BEGIN:VCALENDAR VERSION:2.0 PRODID:-//18.83.4.138//NONSGML kigkonsult.se iCalcreator 2.20// CALSCALE:GREGORIAN METHOD:PUBLISH X-FROM-URL:http://oceans.mit.edu X-WR-TIMEZONE:America/New_York BEGIN:VTIMEZONE TZID:America/New_York X-LIC-LOCATION:America/New_York BEGIN:STANDARD DTSTART:20171105T020000 TZOFFSETFROM:-0400 TZOFFSETTO:-0500 RDATE:20181104T020000 TZNAME:EST END:STANDARD BEGIN:DAYLIGHT DTSTART:20180311T020000 TZOFFSETFROM:-0500 TZOFFSETTO:-0400 TZNAME:EDT END:DAYLIGHT END:VTIMEZONE BEGIN:VEVENT UID:83rrcno47f5rumaeclvp2d6114@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150505T150000 DTEND;TZID=America/New_York:20150505T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Amala Mahadevan\, WHOI. ‘Eddy-driven subduction of particulate orga nic carbon and oxygen from the North Atlantic spring bloom ‘. Clark 507. URL:http://oceans.mit.edu/event/amala-mahadevan-whoi-eddy-driven-subduction -of-particulate-organic-carbon-and-oxygen-from-the-north-atlantic-spring-b loom-clark-507 END:VEVENT BEGIN:VEVENT UID:ub84g3og21o7js7ossrvn7saig@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:The Brazil Current is probably the least known and explored of the western boundary currents of the world ocean. In this talk\, we offer an overview of research carried out at the Oceanographic Institute of the University of São Paulo (IOUSP) on this current system's pattern\, water m asses and mesoscale variability. By blending small quasi-synoptic data set s\, mooring data and simple process-oriented modeling\, we propose an exte nsion of the seminal work by Henry Stommel (1965). The BC system is descri bed from its site of origin (~15S) to where its starts to separate from th e continental margin\, south of 35S. DTSTART;TZID=America/New_York:20150512T150000 DTEND;TZID=America/New_York:20150512T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Ilson da Silveira\, Universidade de São Paulo. ‘The Brazil Current revisited: Beyond Stommel’s (1965) pioneering insights’. Clark 507. URL:http://oceans.mit.edu/event/ilson-da-silveira-universidade-de-sao-paulo -the-brazil-current-revisited-beyond-stommels-1965-pioneering-insights-cla rk-507 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nThe Brazil Curre nt is probably the least known and explored of the western boundary curren ts of the world ocean. In this talk\, we offer an overview of research car ried out at the Oceanographic Institute of the University of São Paulo (IO USP) on this current system's pattern\, water masses and mesoscale variabi lity. By blending small quasi-synoptic data sets\, mooring data and simple process-oriented modeling\, we propose an extension of the seminal work b y Henry Stommel (1965). The BC system is described from its site of origin (~15S) to where its starts to separate from the continental margin\, sout h of 35S. END:VEVENT BEGIN:VEVENT UID:giej4fotj8s93pcbu6239r3et8@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:The impact of the North Atlantic Oscillation (NAO) on the Atlan tic Meridional Overturning Circulation (AMOC) and large-scale climate is a ssessed using simulations with three different climate models. Perturbatio n experiments are conducted in which a pattern of anomalous heat flux corr esponding to the NAO is added to the model ocean\; in companion experiment s no such flux is added. Differences between the experiments illustrate ho w the model ocean and climate system respond to the NAO. A positive phase of the NAO tends to strengthen the AMOC by extracting heat from the subpol ar gyre\, thereby increasing deepwater formation\, horizontal density grad ients\, and the AMOC. The flux forcings have the spatial structure of the observed NAO\, but the amplitude of the forcing varies sinusoidally in tim e with distinct periods varying from 2 to 200 years. The response of the A MOC to NAO variations is small at short time scales\, but increases up to the dominant time scale of internal AMOC variability (20-30 years for the models used). The amplitude of the response of the AMOC\, and associated o ceanic heat transport\, is approximately constant as the timescale of the forcing is increased further. In contrast\, the response of other properti es\, such as hemispheric surface air temperature or Arctic sea ice\, conti nues to increase as the time scale of the forcing becomes progressively lo nger. The larger response of temperature and sea ice at progressively long er time scales is associated with an increased impact of radiative feedbac k processes. The impact of the NAO-induced AMOC variations extends to the Southern Ocean as well\, inducing variations in surface and interior ocean properties. This relationship results in some skill in decadal prediction of aspects of the Southern Ocean. DTSTART;TZID=America/New_York:20150519T150000 DTEND;TZID=America/New_York:20150519T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Tom Delworth\, GFDL. ‘The impact of the North Atlantic Oscillation on climate through its influence on the Atlantic Meridional Overturning Ci rculation’. Clark 201. URL:http://oceans.mit.edu/event/tom-delworth-gfdl-the-impact-of-the-north-a tlantic-oscillation-on-climate-through-its-influence-on-the-atlantic-merid ional-overturning-circulation-clark-201 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nThe impact of th e North Atlantic Oscillation (NAO) on the Atlantic Meridional Overturning Circulation (AMOC) and large-scale climate is assessed using simulations w ith three different climate models. Perturbation experiments are conducted in which a pattern of anomalous heat flux corresponding to the NAO is add ed to the model ocean\; in companion experiments no such flux is added. Di fferences between the experiments illustrate how the model ocean and clima te system respond to the NAO. A positive phase of the NAO tends to strengt hen the AMOC by extracting heat from the subpolar gyre\, thereby increasin g deepwater formation\, horizontal density gradients\, and the AMOC. The f lux forcings have the spatial structure of the observed NAO\, but the ampl itude of the forcing varies sinusoidally in time with distinct periods var ying from 2 to 200 years. The response of the AMOC to NAO variations is sm all at short time scales\, but increases up to the dominant time scale of internal AMOC variability (20-30 years for the models used). The amplitude of the response of the AMOC\, and associated oceanic heat transport\, is approximately constant as the timescale of the forcing is increased furthe r. In contrast\, the response of other properties\, such as hemispheric su rface air temperature or Arctic sea ice\, continues to increase as the tim e scale of the forcing becomes progressively longer. The larger response o f temperature and sea ice at progressively longer time scales is associate d with an increased impact of radiative feedback processes. The impact of the NAO-induced AMOC variations extends to the Southern Ocean as well\, in ducing variations in surface and interior ocean properties. This relations hip results in some skill in decadal prediction of aspects of the Southern Ocean. END:VEVENT BEGIN:VEVENT UID:6ccmrqqsetuqttr3b0u5iohm7o@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150526T150000 DTEND;TZID=America/New_York:20150526T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Ken Brink\, WHOI. ‘Continental shelf baroclinic instability with fl uctuating wind forcing’. Clark 507 URL:http://oceans.mit.edu/event/ken-brink-whoi-continental-shelf-baroclinic -instability-with-fluctuating-wind-forcing-clark-507 END:VEVENT BEGIN:VEVENT UID:1mhk2k6n73243epihbavrpp13c@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150602T150000 DTEND;TZID=America/New_York:20150602T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Uriel Zajaczkovski\, Scripps. ‘Southern Ocean eddies: propagation\, energy sources and the role of topography’. Clark 507. URL:http://oceans.mit.edu/event/uriel-zajaczkovski-scripps-southern-ocean-e ddies-propagation-energy-sources-and-the-role-of-topography-clark-507 END:VEVENT BEGIN:VEVENT UID:poltmskhe21j1ic87v76rhesf8@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150609T150000 DTEND;TZID=America/New_York:20150609T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Young-Oh Kwon\, WHOI. ‘Year-to-year re-outcropping of Eighteen Degr ee Water in an eddy-resolving ocean simulation’. Clark 201. URL:http://oceans.mit.edu/event/young-oh-kwon-whoi-year-to-year-re-outcropp ing-of-eighteen-degree-water-in-an-eddy-resolving-ocean-simulation-clark-2 01 END:VEVENT BEGIN:VEVENT UID:daes58s3elgu9tgm8pvh74aa30@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150616T150000 DTEND;TZID=America/New_York:20150616T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Tom Connolly\, WHOI. ‘Surface waves and exchange across the inner s helf’. Clark 507. URL:http://oceans.mit.edu/event/tom-connolly-whoi-surface-waves-and-exchang e-across-the-inner-shelf-clark-507 END:VEVENT BEGIN:VEVENT UID:41i45du12hj9p5elhg8b88rab8@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150618T140000 DTEND;TZID=America/New_York:20150618T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Sanjeeva Balasuriya\, University of Adelaide. ‘Flow barriers and fl ux in unsteady flows’. Clark 201 URL:http://oceans.mit.edu/event/sanjeeva-balasuriya-university-of-adelaide- flow-barriers-and-flux-in-unsteady-flows-clark-201 END:VEVENT BEGIN:VEVENT UID:rt5o22uqg1jm1jk48nkek6b99c@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150623T150000 DTEND;TZID=America/New_York:20150623T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Larry Pratt\, WHOI. ‘Resonant stirring and mixing in an idealized m odel of an eddy’. Clark 507. URL:http://oceans.mit.edu/event/larry-pratt-whoi-resonant-stirring-and-mixi ng-in-an-idealized-model-of-an-eddy-clark-507 END:VEVENT BEGIN:VEVENT UID:54vndurckkf737eknmjqml0j58@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150625T140000 DTEND;TZID=America/New_York:20150625T150000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Pierre-Yves Passaggia\, UNC. ‘Bifurcation and global stability anal ysis of horizontal convection.’ Clark 507 URL:http://oceans.mit.edu/event/pierre-yves-passaggia-unc-bifurcation-and-g lobal-stability-analysis-of-horizontal-convection-clark-507 END:VEVENT BEGIN:VEVENT UID:ehlikb3q0cnm611oo4gq9jvj70@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150630T150000 DTEND;TZID=America/New_York:20150630T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Raffaele Ferrari\, MIT. ‘Turning ocean mixing upside down’. Clark 5 07. URL:http://oceans.mit.edu/event/raffaele-ferrari-mit-turning-ocean-mixing-u pside-down-clark-507 END:VEVENT BEGIN:VEVENT UID:v64t7cuibqlarnl27an3i6beb4@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150707T150000 DTEND;TZID=America/New_York:20150707T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Tom Sanford and Ren-Chieh Lien\, APL-UW. ‘The Hunt for the Elusive Vortical Mode’. Clark 507 URL:http://oceans.mit.edu/event/tom-sanford-and-ren-chieh-lien-apl-uw-the-h unt-for-the-elusive-vortical-mode-clark-507 END:VEVENT BEGIN:VEVENT UID:8ruuglad8cl6d9snsskla1o4d8@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:Mixing in near-integrable flows with a clear separation of time or spacial scales is notoriously difficult to achieve. In many flows the intrinsic symmetries create invariant surfaces that act as barriers to cha otic advection and mixing. Thus\, a key to efficient mixing is to add to t he original (symmetric) flow a certain kind of perturbation that destroys those symmetries. In the present talk we discuss a quantitative long-time theory of mixing due to the presence of resonances in 3-D near-integrable Stokes flows. The resonance phenomena\, such as scattering on resonance\, capture into resonance\, and separatrix crossings\, involving different co mponents of the original flow and the perturbation may destroy the invaria nt surfaces\, paving a way to the large-scale mixing in a big fraction of the fluid flow. We explain the extend and the rate of mixing in terms of t he evolution of the adiabatic invariants of the system. We show that when the leading phenomenon is scattering on resonances or separatrix crossings \, the resulting mixing can be described in terms of a single 1-D diffusio n-type equation\, with parameters of the diffusion equation defined by the averaged statistics of a single passage through resonance or separatrix. DTSTART;TZID=America/New_York:20150709T140000 DTEND;TZID=America/New_York:20150709T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Dmitri Vainchtein\, Temple University. ‘Resonances and Mixing in Mu lti-scale Flows’. Clark 201 URL:http://oceans.mit.edu/event/dmitri-vainchtein-temple-university-resonan ces-and-mixing-in-multi-scale-flows-clark-201 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nMixing in near-i ntegrable flows with a clear separation of time or spacial scales is notor iously difficult to achieve. In many flows the intrinsic symmetries create invariant surfaces that act as barriers to chaotic advection and mixing. Thus\, a key to efficient mixing is to add to the original (symmetric) flo w a certain kind of perturbation that destroys those symmetries. In the pr esent talk we discuss a quantitative long-time theory of mixing due to the presence of resonances in 3-D near-integrable Stokes flows. The resonance phenomena\, such as scattering on resonance\, capture into resonance\, an d separatrix crossings\, involving different components of the original fl ow and the perturbation may destroy the invariant surfaces\, paving a way to the large-scale mixing in a big fraction of the fluid flow. We explain the extend and the rate of mixing in terms of the evolution of the adiabat ic invariants of the system. We show that when the leading phenomenon is s cattering on resonances or separatrix crossings\, the resulting mixing can be described in terms of a single 1-D diffusion-type equation\, with para meters of the diffusion equation defined by the averaged statistics of a s ingle passage through resonance or separatrix. END:VEVENT BEGIN:VEVENT UID:k2a6v78es75p0tkb85oep69808@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150714T150000 DTEND;TZID=America/New_York:20150714T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Laura Slivinski\, WHOI. ‘Applications of Lagrangian Data Assimilati on to Katama Bay\, MA’. Clark 507. URL:http://oceans.mit.edu/event/laura-slivinski-whoi-applications-of-lagran gian-data-assimilation-to-katama-bay-ma-clark-507 END:VEVENT BEGIN:VEVENT UID:trl8okotv6pj6iin45vtmlc4jo@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150716T140000 DTEND;TZID=America/New_York:20150716T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Alex Soloviev\, Nova Southeastern U. ‘3D Dynamics of the Near-Surfa ce Layer of the Ocean: Field and Computational Fluid Dynamics Experiments’ . Clark 201 URL:http://oceans.mit.edu/event/alex-soloviev-nova-southeastern-u-3d-dynami cs-of-the-near-surface-layer-of-the-ocean-field-and-computational-fluid-dy namics-experiments-clark-201 END:VEVENT BEGIN:VEVENT UID:dmbu7fjup8o2vqslmj9ambf1j4@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:The interaction between an Antarctic Circumpolar Current-like c hannel flow and a continental shelf break is considered using eddy-permitt ing simulations of a quasi-geostrophic and a primitive equation model. The experimental setup is motivated by the continental shelf of the West Anta rctica Peninsula. Numerical experiments are performed to study how the wid th and slope of an idealized continental shelf topography affect the chara cteristics of the flow. The main focus is on the regime where the shelf br eak width is slightly greater than the eddy scale. In this regime\, a stro ng baroclinic jet develops on the shelf break due to the locally stabilizi ng effect of the topographic slope. The velocity of this jet is set at fi rst order by the gradient of the background barotropic geostrophic contour s\, which is dominated by the slope of the topography. At statistical equi librium\, an aperiodic cycle is observed. Initially\, over a long stable p eriod\, an upper-layer jet develops over the shelf break. Once the vertica l shear reaches the critical condition for baroclinic instability\, the je t becomes unstable and drifts away from the shelf break. The cross-shelf m ixing is intrinsically linked with the jet drifting\, as most of the merid ional flux occurs during this instability period. Investigation of the zon al momentum budget reveals that a strong Reynolds stress divergence invers ion across the jet is associated with a drifting event\, accelerating one flank of the jet and decelerating the other. The hypothesis that jet drift ing may be due to one flank of the jet being more baroclinically unstable than the other\, is tested using topographic profiles with variable curvat ures. DTSTART;TZID=America/New_York:20150721T150000 DTEND;TZID=America/New_York:20150721T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Alon Stern\, GFDL/Princeton U. ‘Instability and mixing of zonal jet s along an idealized continental shelf break’. Clark 201 URL:http://oceans.mit.edu/event/alon-stern-gfdlprinceton-u-instability-and- mixing-of-zonal-jets-along-an-idealized-continental-shelf-break-clark-201 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nThe interaction between an Antarctic Circumpolar Current-like channel flow and a continent al shelf break is considered using eddy-permitting simulations of a quasi- geostrophic and a primitive equation model. The experimental setup is moti vated by the continental shelf of the West Antarctica Peninsula. Numerical experiments are performed to study how the width and slope of an idealize d continental shelf topography affect the characteristics of the flow. The main focus is on the regime where the shelf break width is slightly great er than the eddy scale. In this regime\, a strong baroclinic jet develops on the shelf break due to the locally stabilizing effect of the topograph ic slope. The velocity of this jet is set at first order by the gradient o f the background barotropic geostrophic contours\, which is dominated by t he slope of the topography. At statistical equilibrium\, an aperiodic cycl e is observed. Initially\, over a long stable period\, an upper-layer jet develops over the shelf break. Once the vertical shear reaches the critica l condition for baroclinic instability\, the jet becomes unstable and drif ts away from the shelf break. The cross-shelf mixing is intrinsically link ed with the jet drifting\, as most of the meridional flux occurs during th is instability period. Investigation of the zonal momentum budget reveals that a strong Reynolds stress divergence inversion across the jet is assoc iated with a drifting event\, accelerating one flank of the jet and decele rating the other. The hypothesis that jet drifting may be due to one flank of the jet being more baroclinically unstable than the other\, is tested using topographic profiles with variable curvatures. END:VEVENT BEGIN:VEVENT UID:4f5ihduahg5bhbga9um5b86788@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150728T150000 DTEND;TZID=America/New_York:20150728T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Georgy Manucharyan\, WHOI. ‘Wind-driven halocline dynamics of the B eaufort Gyre’. Clark 507. URL:http://oceans.mit.edu/event/georgy-manucharyan-whoi-wind-driven-halocli ne-dynamics-of-the-beaufort-gyre-clark-507 END:VEVENT BEGIN:VEVENT UID:qbhtrfh7gkrf198ofdo4clhslc@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150804T150000 DTEND;TZID=America/New_York:20150804T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Alexey Fedorov\, Yale. ‘The “super” El Nino of 2014 that never happ ened and global warming hiatus.’ Clark 507 URL:http://oceans.mit.edu/event/alexey-fedorov-yale-the-super-el-nino-of-20 14-that-never-happened-and-global-warming-hiatus-clark-507 END:VEVENT BEGIN:VEVENT UID:h6ko2jrbvbfstkfmkb98v7et3c@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150811T150000 DTEND;TZID=America/New_York:20150811T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Wilken-Jon von Appen\, Alfred Wegener Institute. ‘Seasonal cycle of mesoscale instability of the West Spitsbergen Current’. Clark 507. URL:http://oceans.mit.edu/event/wilken-jon-von-appen-alfred-wegener-institu te-seasonal-cycle-of-mesoscale-instability-of-the-west-spitsbergen-current -clark-507 END:VEVENT BEGIN:VEVENT UID:ls6o7ub8auc2jkb0g616sie9l4@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150818T150000 DTEND;TZID=America/New_York:20150818T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Trevor McDougall\, U. New South Wales\, ‘How does the deep ocean ma nage to achieve upwelling since the interior diapycnal velocity is downwar ds? and\, On the thermodynamics of seawater and frazil ice’\, Clark 5 07 URL:http://oceans.mit.edu/event/trevor-mcdougall-u-new-south-wales-how-does -the-deep-ocean-manage-to-achieve-upwelling-since-the-interior-diapycnal-v elocity-is-downwards-and-on-the-thermodynamics-of-seawater-and-frazil-i END:VEVENT BEGIN:VEVENT UID:kiuh038rfcblv51dkiso35vac0@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150824T140000 DTEND;TZID=America/New_York:20150824T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Louis Clement\, LDEO. ‘Generation of internal waves by eddies impin ging at the western boundary of the North Atlantic’. Clark 201. URL:http://oceans.mit.edu/event/louis-clement-ldeo-generation-of-internal-w aves-by-eddies-impinging-at-the-western-boundary-of-the-north-atlantic-cla rk-201 END:VEVENT BEGIN:VEVENT UID:4fir0ubk8l1knopuj9k02c8rhg@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150825T150000 DTEND;TZID=America/New_York:20150825T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:John Marshall\, MIT. ‘Response of the ocean to volcanic eruptions’. Clark 507. URL:http://oceans.mit.edu/event/john-marshall-mit-response-of-the-ocean-to- volcanic-eruptions-clark-507 END:VEVENT BEGIN:VEVENT UID:494vrr1rgff3hm9ok3dnii7u0o@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150915T150500 DTEND;TZID=America/New_York:20150915T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Magdalena Andres\, WHOI. ‘Line W and SYNOP: Does Deep Cyclogenesis under Gulf Stream Meanders Influence the DWBC?’. Clark 507 URL:http://oceans.mit.edu/event/magdalena-andres-whoi-line-w-and-synop-does -deep-cyclogenesis-under-gulf-stream-meanders-influence-the-dwbc-clark-507 END:VEVENT BEGIN:VEVENT UID:jobcn33na9eg6af2iiso54alf0@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150922T150500 DTEND;TZID=America/New_York:20150922T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:X. San Liang\, Nanjing Institute of Meteorology. ‘Rigorous causalit y quantification between time series and applications to ocean data analys is’. Clark 507. URL:http://oceans.mit.edu/event/x-san-liang-nanjing-institute-of-meteorolog y-rigorous-causality-quantification-between-time-series-and-applications-t o-ocean-data-analysis-clark-507 END:VEVENT BEGIN:VEVENT UID:nll8o321cqot543r1th5heb75c@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20150929T150500 DTEND;TZID=America/New_York:20150929T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:M. Dolores Pérez-Hernández\, WHOI. ‘The Canary Basin contribution t o the seasonal cycle of the Atlantic Meridional Overturning Circulation a t 26ºN’. Clark 507. URL:http://oceans.mit.edu/event/m-dolores-perez-hernandez-whoi-the-canary-b asin-contribution-to-the-seasonal-cycle-of-the-atlantic-meridional-overtur ning-circulation-at-26on-clark-507 END:VEVENT BEGIN:VEVENT UID:u4umqbrbhtpeipp8vktes60ics@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:Clark 507 DTSTART;TZID=America/New_York:20151006T150500 DTEND;TZID=America/New_York:20151006T160000 LOCATION:the western Nordic Seas under changing atmospheric conditions'. Cl ark 507 SEQUENCE:0 SUMMARY:Kjetil Våge\, U. Bergen. ‘Wintertime convection in the western Nord ic Seas under changing atmospheric conditions’. Clark 507 URL:http://oceans.mit.edu/event/kjetil-vage-u-bergen-wintertime-convection- in-the-western-nordic-seas-under-changing-atmospheric-conditions-clark-507 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nClark 507 END:VEVENT BEGIN:VEVENT UID:87t795erdc0ok67ga6as2sgk2o@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151013T150500 DTEND;TZID=America/New_York:20151013T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Kerry Cook\, U. Texas Austin. ‘The West African Monsoon: Dynamics o f the monsoon jump and recent trends’. Clark 507. URL:http://oceans.mit.edu/event/kerry-cook-u-texas-austin-the-west-african- monsoon-dynamics-of-the-monsoon-jump-and-recent-trends-clark-507 END:VEVENT BEGIN:VEVENT UID:mei5e2dv5n7tve4rmlg1f0fkic@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151015T140000 DTEND;TZID=America/New_York:20151015T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Femke de Jong\, Duke. ‘Eddies in the Labrador Sea: Part 2’ Clark 20 1 URL:http://oceans.mit.edu/event/femke-de-jong-duke-eddies-in-the-labrador-s ea-part-2-clark-201 END:VEVENT BEGIN:VEVENT UID:br1kst6f32gqppv5fj4969cdhg@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151020T150500 DTEND;TZID=America/New_York:20151020T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Ali Mashayek\, MIT. ‘Topographic Enhancement of Vertical Mixing in the Southern Ocean’. Clark 201 URL:http://oceans.mit.edu/event/ali-mashayek-mit-topographic-enhancement-of -vertical-mixing-in-the-southern-ocean-clark-201 END:VEVENT BEGIN:VEVENT UID:mba735734800bulmbrcdtbpe9g@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151027T150500 DTEND;TZID=America/New_York:20151027T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Joern Callies\, MIT. ‘The Role of Mixed Layer Instabilities in Subm esoscale Turbulence’. Clark 507 URL:http://oceans.mit.edu/event/joern-callies-mit-the-role-of-mixed-layer-i nstabilities-in-submesoscale-turbulence-clark-507 END:VEVENT BEGIN:VEVENT UID:ia3l3itiv88dpcsbmjid098k84@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151103T150500 DTEND;TZID=America/New_York:20151103T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:PO postdocs\, ‘5 minute introductions.’ Clark 201. URL:http://oceans.mit.edu/event/po-postdocs-5-minute-introductions-clark-20 1 END:VEVENT BEGIN:VEVENT UID:klvkq3t4adb3j87tla2e1i55to@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151110T150500 DTEND;TZID=America/New_York:20151110T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Susan Wijffles\, CSIRO. ‘Detecting the footprint of anthropogenic c limate forcing in the ocean’. Clark 507. URL:http://oceans.mit.edu/event/susan-wijffles-csiro-detecting-the-footprin t-of-anthropogenic-climate-forcing-in-the-ocean-clark-507 END:VEVENT BEGIN:VEVENT UID:h7groh3m547b89r8c6t3joqhuo@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151112T140000 DTEND;TZID=America/New_York:20151112T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Hedinn Valdimarsson\, Marine Research Institute. ‘Oceanography in I celandic waters’. Clark 201 URL:http://oceans.mit.edu/event/hedinn-valdimarsson-marine-research-institu te-oceanography-in-icelandic-waters-clark-201 END:VEVENT BEGIN:VEVENT UID:m5o658pdgk6iqnnhfrkdh1s7to@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151117T150500 DTEND;TZID=America/New_York:20151117T160000 SEQUENCE:0 SUMMARY:Robert Todd\, WHOI. ‘Potential vorticity structure in the North Atl antic western boundary current from underwater glider observations’ Clark 507 URL:http://oceans.mit.edu/event/robert-todd-whoi-potential-vorticity-struct ure-in-the-north-atlantic-western-boundary-current-from-underwater-glider- observations-clark-507 END:VEVENT BEGIN:VEVENT UID:hrpjs445bd351fal8s4ns2n4vs@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151119T140000 DTEND;TZID=America/New_York:20151119T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Gaetan Lerisson\, Ecole Polytechnique. ‘Effect of mean current on t he stability of internal gravity waves’. Clark 201 URL:http://oceans.mit.edu/event/gaetan-lerisson-ecole-polytechnique-effect- of-mean-current-on-the-stability-of-internal-gravity-waves-clark-201 END:VEVENT BEGIN:VEVENT UID:jujo1pden2a0fc03a4lf43e1f4@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151203T140000 DTEND;TZID=America/New_York:20151203T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Jesse Cusack\, National Oceanography Center Southampton. ‘Isopycnal spice variance in the deep ACC’. Clark 201. URL:http://oceans.mit.edu/event/jesse-cusack-national-oceanography-center-s outhampton-isopycnal-spice-variance-in-the-deep-acc-clark-201 END:VEVENT BEGIN:VEVENT UID:vavb7716jhdup6bbspjogo9668@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20151208T150500 DTEND;TZID=America/New_York:20151208T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Viviane Menezes\, WHOI. ‘The circulation of the Indian Ocean: Unusu al effect of salinity’. Clark 507. URL:http://oceans.mit.edu/event/viviane-menezes-whoi-the-circulation-of-the -indian-ocean-unusual-effect-of-salinity-clark-507 END:VEVENT BEGIN:VEVENT UID:u5uvgtcmulcp7lehapbrqe3h6c@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160119T150500 DTEND;TZID=America/New_York:20160119T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Jim Bisagni\, U Mass Dartmouth. ‘Salinity variability along the eas tern continental shelf of the Unites States and Canada\, 1973-2013’. Clark 507. URL:http://oceans.mit.edu/event/jim-bisagni-u-mass-dartmouth-salinity-varia bility-along-the-eastern-continental-shelf-of-the-unites-states-and-canada -1973-2013-clark-507 END:VEVENT BEGIN:VEVENT UID:6ak8j8naldca65bnmt2ehch300@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160126T150500 DTEND;TZID=America/New_York:20160126T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Maike Sonnewald\, MIT. ‘Ocean model utility dependence on horizonta l resolution’. Clark 507. URL:http://oceans.mit.edu/event/maike-sonnewald-mit-ocean-model-utility-dep endence-on-horizontal-resolution-clark-507 END:VEVENT BEGIN:VEVENT UID:gag64q6k4rppibofnun8nmvlno@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160202T150500 DTEND;TZID=America/New_York:20160202T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Tom Haine\, Johns Hopkins. ‘Denmark Strait overflow kinematics’. Cl ark 507. URL:http://oceans.mit.edu/event/tom-haine-johns-hopkins-denmark-strait-over flow-kinematics-clark-507 END:VEVENT BEGIN:VEVENT UID:5fnr4l7t9jcg1cq0nvcksbs8qg@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160209T150500 DTEND;TZID=America/New_York:20160209T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Anthony Kirincich\, WHOI. ‘The importance of lateral variability on exchange across the inner shelf’. Clark 507 URL:http://oceans.mit.edu/event/anthony-kirincich-whoi-the-importance-of-la teral-variability-on-exchange-across-the-inner-shelf-clark-507 END:VEVENT BEGIN:VEVENT UID:tnsjcpeh5qpej4g2icjak6f0u8@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160216T150500 DTEND;TZID=America/New_York:20160216T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:‘Meet the PO students’. Clark 507. URL:http://oceans.mit.edu/event/meet-the-po-students-clark-507-2 END:VEVENT BEGIN:VEVENT UID:9m1u51acc0ha532q6dquijc7ds@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160223T150500 DTEND;TZID=America/New_York:20160223T160000 SEQUENCE:0 SUMMARY:Canceled URL:http://oceans.mit.edu/event/canceled END:VEVENT BEGIN:VEVENT UID:4ae98dvnh95t652m37nklmqlfc@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160301T150500 DTEND;TZID=America/New_York:20160301T160000 SEQUENCE:0 SUMMARY:Debasis Sengupta\, Indian Inst. Sci. ‘Monsoon rain\, river runoff\, and Bay of Bengal salinity’. Clark 507 URL:http://oceans.mit.edu/event/debasis-sengupta-indian-inst-sci-monsoon-ra in-river-runoff-and-bay-of-bengal-salinity-clark-507 END:VEVENT BEGIN:VEVENT UID:s4j6kjemhi47ev09qa7prtjtm0@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160307T110000 DTEND;TZID=America/New_York:20160307T120000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Shota Katsura\, U Tokyo. ‘Structure and variation of upper ocean sa linity in the subtropical Pacific: North Pacific tropical water and barrie r layer.’ Clark 507. URL:http://oceans.mit.edu/event/shota-katsura-u-tokyo-structure-and-variati on-of-upper-ocean-salinity-in-the-subtropical-pacific-north-pacific-tropic al-water-and-barrier-layer-clark-507 END:VEVENT BEGIN:VEVENT UID:22hu9k0u8jjgnrpu4lg2gkdiag@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160308T150500 DTEND;TZID=America/New_York:20160308T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Joseph D’Addezio\, U. South Carolina. ‘Air-sea interactions in the Seychelles-Chagos thermocline ridge’. Clark 507. URL:http://oceans.mit.edu/event/joseph-daddezio-u-south-carolina-air-sea-in teractions-in-the-seychelles-chagos-thermocline-ridge-clark-507 END:VEVENT BEGIN:VEVENT UID:r7o3ktjdrjovecuut3l7vomdk0@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160315T150500 DTEND;TZID=America/New_York:20160315T160000 LOCATION:Carriage House SEQUENCE:0 SUMMARY:‘What are we up to? Talks by three PO faculty’. Carriage House URL:http://oceans.mit.edu/event/what-are-we-up-to-talks-by-three-po-faculty -carriage-house END:VEVENT BEGIN:VEVENT UID:poi0rvbl4kq6oo9cemk8l7is7c@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160322T150500 DTEND;TZID=America/New_York:20160322T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Steve Lentz\, WHOI. ‘The Middle Atlantic Bight cold pool revisited. ’ Clark 507. URL:http://oceans.mit.edu/event/steve-lentz-whoi-the-middle-atlantic-bight- cold-pool-revisited-clark-507 END:VEVENT BEGIN:VEVENT UID:523p1g4f1vs8mkp1i8dv84q2n8@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160405T150500 DTEND;TZID=America/New_York:20160405T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Anna FitzMaurice\, Princeton U. ‘The Southern Ocean overturning cir culation and its relation to Antarctic sea ice extent’. Clark 507. URL:http://oceans.mit.edu/event/anna-fitzmaurice-princeton-u-the-southern-o cean-overturning-circulation-and-its-relation-to-antarctic-sea-ice-extent- clark-507 END:VEVENT BEGIN:VEVENT UID:lfgcefe5ln0kol3j3am3qd8l3k@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160412T150500 DTEND;TZID=America/New_York:20160412T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Ken Brink\, WHOI. ‘Cooling\, winds and eddies over the continental shelf’. Clark 507. URL:http://oceans.mit.edu/event/ken-brink-whoi-cooling-winds-and-eddies-ove r-the-continental-shelf-clark-507 END:VEVENT BEGIN:VEVENT UID:q9ls49jii8h2tm8pej80hlu6rk@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160419T150500 DTEND;TZID=America/New_York:20160419T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Mike Spall\, WHOI. ‘Offshore decay scale of cold upwelled SST’. Cla rk 201 URL:http://oceans.mit.edu/event/mike-spall-whoi-offshore-decay-scale-of-col d-upwelled-sst-clark-201 END:VEVENT BEGIN:VEVENT UID:549mtpoqbotab2bts869uq6fog@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160425T140500 DTEND;TZID=America/New_York:20160425T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Matthew Alford\, SIO. ‘Observing the generation\, propagation and d issipation of internal waves in the ocean.’ Clark 201. URL:http://oceans.mit.edu/event/matthew-alford-sio-observing-the-generation -propagation-and-dissipation-of-internal-waves-in-the-ocean-clark-201 END:VEVENT BEGIN:VEVENT UID:3gs0l1b0k3j83gt5h6gg0gdp2o@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160426T150500 DTEND;TZID=America/New_York:20160426T160000 LOCATION:Carriage House SEQUENCE:0 SUMMARY:Hyodae Seo\, WHOI. ‘Eddy-driven air-sea interaction in the Californ ia Current System’. Carriage House. URL:http://oceans.mit.edu/event/hyodae-seo-whoi-eddy-driven-air-sea-interac tion-in-the-california-current-system-carriage-house END:VEVENT BEGIN:VEVENT UID:o9fe33h9rkfjhve2qpvaqem2bo@google.com DTSTAMP:20180503T083649Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160503T150500 DTEND;TZID=America/New_York:20160503T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Susan Wijffels\, CSIRO. ‘Towards understanding the Indonesian Throu ghflow and its variability’. Clark 507. URL:http://oceans.mit.edu/event/susan-wijffels-csiro-towards-understanding- the-indonesian-throughflow-and-its-variability-clark-507 END:VEVENT BEGIN:VEVENT UID:hltebk9pl3i849e9kbv2cq7di0@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160510T150500 DTEND;TZID=America/New_York:20160510T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Luca Centurioni\, SIO. ‘Near-surface circulation of the North West Pacific Ocean and interaction with the China Seas’. Clark 507 URL:http://oceans.mit.edu/event/luca-centurioni-sio-near-surface-circulatio n-of-the-north-west-pacific-ocean-and-interaction-with-the-china-seas-clar k-507 END:VEVENT BEGIN:VEVENT UID:hq3t95rbns58me6c0dcqc97ei8@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160517T150500 DTEND;TZID=America/New_York:20160517T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Nick Beaird\, WHOI. ‘Fingerprints of ocean-glacier interaction arou nd Greenland’. Clark 201. URL:http://oceans.mit.edu/event/nick-beaird-whoi-fingerprints-of-ocean-glac ier-interaction-around-greenland-clark-201 END:VEVENT BEGIN:VEVENT UID:v0tonlt37us3kd0pv7l1mquob4@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160519T140500 DTEND;TZID=America/New_York:20160519T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Charlie Eriksen\, U. Washington. ‘Deepglider observations of full-d epth flow structure from Bermuda to the Western Boundary’. Clark 201. URL:http://oceans.mit.edu/event/charlie-eriksen-u-washington-deepglider-obs ervations-of-full-depth-flow-structure-from-bermuda-to-the-western-boundar y-clark-201 END:VEVENT BEGIN:VEVENT UID:3j02b94am2l3qceptmr4qt26n0@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160524T150500 DTEND;TZID=America/New_York:20160524T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Sarah Purkey\, LDEO. ‘Regional and global rates of ocean mass addit ion between 1996-2006 from a full depth sea level rise budget’. Clark 201. URL:http://oceans.mit.edu/event/sarah-purkey-ldeo-regional-and-global-rates -of-ocean-mass-addition-between-1996-2006-from-a-full-depth-sea-level-rise -budget-clark-201 END:VEVENT BEGIN:VEVENT UID:9742fscbf75i0m39vma3775v9k@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160526T140500 DTEND;TZID=America/New_York:20160526T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Dan Amrhein\, MIT/WHOI. ‘Towards ocean state estimation at the Last Glacial Maximum’. Clark 201 URL:http://oceans.mit.edu/event/dan-amrhein-mitwhoi-towards-ocean-state-est imation-at-the-last-glacial-maximum-clark-201 END:VEVENT BEGIN:VEVENT UID:311aue6cmfctjj86m9soa7grfk@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160531T150500 DTEND;TZID=America/New_York:20160531T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Ke Chen\, WHOI. ‘Heat balance and temperature variability in the No rtheast US coastal ocean’. Clark 507. URL:http://oceans.mit.edu/event/ke-chen-whoi-heat-balance-and-temperature-v ariability-in-the-northeast-us-coastal-ocean-clark-507 END:VEVENT BEGIN:VEVENT UID:6csf0g15afmesb3h2b8lpmpp7k@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160602T140500 DTEND;TZID=America/New_York:20160602T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Emily Shroyer\, OSU. ‘Seasonal connections between Nares Strait and Petermann Glacier: Linking the sea ice\, ocean\, and ice shelf’. Clark 20 1. URL:http://oceans.mit.edu/event/emily-shroyer-osu-seasonal-connections-betw een-nares-strait-and-petermann-glacier-linking-the-sea-ice-ocean-and-ice-s helf-clark-201 END:VEVENT BEGIN:VEVENT UID:93f9r7o5941q3i16b4f896k94g@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160607T140500 DTEND;TZID=America/New_York:20160607T150000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Ben Harden\, SEA / WHOI. ‘Upstream sources of the Denmark Strait Ov erflow: Observations from a high-resolution mooring array’. Clark 507 URL:http://oceans.mit.edu/event/ben-harden-sea-whoi-upstream-sources-of-the -denmark-strait-overflow-observations-from-a-high-resolution-mooring-array -clark-507 END:VEVENT BEGIN:VEVENT UID:gkv4r8gf8a4et6b0j3gv6v97es@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160613T140500 DTEND;TZID=America/New_York:20160613T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Aneesh Subramanian\, Oxford. ‘Stochastic multi-scale atmospheric mo deling: A route to improved forecasts for the tropics’. Clark 201 URL:http://oceans.mit.edu/event/aneesh-subramanian-oxford-stochastic-multi- scale-atmospheric-modeling-a-route-to-improved-forecasts-for-the-tropics-c lark-201 END:VEVENT BEGIN:VEVENT UID:3raohdtt0amh0qdepqmn6fogvc@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160614T150500 DTEND;TZID=America/New_York:20160614T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Allan Clarke\, FSU. ‘El Nino and La Nina freshwater jets in the Wes tern Equatorial Pacific’. Clark 507 URL:http://oceans.mit.edu/event/allan-clarke-fsu-el-nino-and-la-nina-freshw ater-jets-in-the-western-equatorial-pacific-clark-507 END:VEVENT BEGIN:VEVENT UID:siiejfvsuusc696b9mn5d9548c@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160621T150500 DTEND;TZID=America/New_York:20160621T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Eleanor Frajka-Williams\, NOC Southampton. ‘Reconciling observation s of the Atlantic MOC variability’. Clark 507. URL:http://oceans.mit.edu/event/eleanor-frajka-williams-noc-southampton-rec onciling-observations-of-the-atlantic-moc-variability-clark-507 END:VEVENT BEGIN:VEVENT UID:09kcvbspgd4itfcvcjifak8hc8@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160628T150500 DTEND;TZID=America/New_York:20160628T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Amy Bower\, WHOI. ‘The Charlie-Gibbs Fracture Zone: A crossroads of the Atlantic Meridional Overturning circulation’. Clark 507. URL:http://oceans.mit.edu/event/amy-bower-whoi-the-charlie-gibbs-fracture-z one-a-crossroads-of-the-atlantic-meridional-overturning-circulation-clark- 507 END:VEVENT BEGIN:VEVENT UID:bn7m1k9vk79tp9m7e1htbncfe8@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160705T150500 DTEND;TZID=America/New_York:20160705T160000 SEQUENCE:0 SUMMARY:Cancelled URL:http://oceans.mit.edu/event/cancelled-11 END:VEVENT BEGIN:VEVENT UID:up0ef34ufndv9scjuf9klh5a40@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160707T140500 DTEND;TZID=America/New_York:20160707T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Ivan Ovsyannikov\, U. Bremen. ‘Cubic homoclinic tangencies and reso nances in two-dimensional symplectic maps.’ Clark 201. URL:http://oceans.mit.edu/event/ivan-ovsyannikov-u-bremen-cubic-homoclinic- tangencies-and-resonances-in-two-dimensional-symplectic-maps-clark-201 END:VEVENT BEGIN:VEVENT UID:n47nbc41hk0kdqqln6kmpq62j0@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160712T150500 DTEND;TZID=America/New_York:20160712T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Dujuan Kang\, Rutgers. ‘Understanding the energetics and variabilit y of the Gulf Stream and associated eddies’. Clark 507. URL:http://oceans.mit.edu/event/dujuan-kang-rutgers-understanding-the-energ etics-and-variability-of-the-gulf-stream-and-associated-eddies-clark-507 END:VEVENT BEGIN:VEVENT UID:fc9e3vli5rib7om4li6igbe748@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160719T150500 DTEND;TZID=America/New_York:20160719T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Leo Maas\, NIOZ. ‘Wave attractors.’ Clark 507. URL:http://oceans.mit.edu/event/leo-maas-nioz-wave-attractors-clark-507 END:VEVENT BEGIN:VEVENT UID:s9cm0kk8jtbvockni5mtqlqehc@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160726T150500 DTEND;TZID=America/New_York:20160726T160000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Ruth Musgrave\, MIT. ‘Tidally driven mixing: breaking lee waves\, h ydraulic jumps and the influence of subinertial internal tides’. Clark 201 URL:http://oceans.mit.edu/event/ruth-musgrave-mit-tidally-driven-mixing-bre aking-lee-waves-hydraulic-jumps-and-the-influence-of-subinertial-internal- tides-clark-201 END:VEVENT BEGIN:VEVENT UID:hdf4esh5ft68j02h66btncki88@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160802T150500 DTEND;TZID=America/New_York:20160802T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Robert Nazarian\, Princeton U. ‘Internal wave scattering in idealiz ed and realistic continental slope canyons’. Clark 507 URL:http://oceans.mit.edu/event/robert-nazarian-princeton-u-internal-wave-s cattering-in-idealized-and-realistic-continental-slope-canyons-clark-507 END:VEVENT BEGIN:VEVENT UID:p5nnqgmsclu5vo0vka0bs9vguo@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160809T150500 DTEND;TZID=America/New_York:20160809T160000 SEQUENCE:0 SUMMARY:Alexey Fedorov\, Yale. ‘The Pacific meridional overturning circulat ion (PMOC) in past warm climates’. Clark 507. URL:http://oceans.mit.edu/event/alexey-fedorov-yale-the-pacific-meridional- overturning-circulation-pmoc-in-past-warm-climates-clark-507 END:VEVENT BEGIN:VEVENT UID:9gdjbotdmi1p2u08hol3ikuj6s@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160811T140500 DTEND;TZID=America/New_York:20160811T150500 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Dhruv Balwada\, FSU. ‘A lagrangian view of oceanic turbulence’. Cla rk 201 URL:http://oceans.mit.edu/event/dhruv-balwada-fsu-a-lagrangian-view-of-ocea nic-turbulence-clark-201 END:VEVENT BEGIN:VEVENT UID:jvp05jffnc5hpifussa90sq1i4@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160816T150500 DTEND;TZID=America/New_York:20160816T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Georgy Manucharayan\, Cal Tech. ‘Emergence of a multi-decadal eddy- memory mode and its impacts on the Beaufort Gyre variability’. Clark 201 URL:http://oceans.mit.edu/event/georgy-manucharayan-cal-tech-emergence-of-a -multi-decadal-eddy-memory-mode-and-its-impacts-on-the-beaufort-gyre-varia bility-clark-201 END:VEVENT BEGIN:VEVENT UID:tulevvipqa4u7sq6fdi56gq1uc@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160818T140500 DTEND;TZID=America/New_York:20160818T150500 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Rui Xin Huang\, WHOI. ‘Adiabatic motions in the ocean and extended isopycnal analysis’. Clark 201 URL:http://oceans.mit.edu/event/rui-xin-huang-whoi-adiabatic-motions-in-the -ocean-and-extended-isopycnal-analysis-clark-201 END:VEVENT BEGIN:VEVENT UID:gci0lam9v6bhe39fj9geiqplsk@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160823T150500 DTEND;TZID=America/New_York:20160823T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:John Toole\, WHOI. ‘Moored observations of the Deep Western Boundar y Current in the northwest Atlantic: 2004-2014’. Clark 507. URL:http://oceans.mit.edu/event/john-toole-whoi-moored-observations-of-the- deep-western-boundary-current-in-the-northwest-atlantic-2004-2014-clark-50 7 END:VEVENT BEGIN:VEVENT UID:cul0rka7hkld97rbptua1p4450@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160830T150500 DTEND;TZID=America/New_York:20160830T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Cancelled URL:http://oceans.mit.edu/event/cancelled-8 END:VEVENT BEGIN:VEVENT UID:a1fg33o5c5j0q16149aamnv5pg@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160906T150500 DTEND;TZID=America/New_York:20160906T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Alain de Verneil\, Mediterranean Inst. Oceanography. ‘Biological tr acer structure in the surface ocean: Effects of mesoscale forcing from the regional to sub-mesoscale’. Clark 507 URL:http://oceans.mit.edu/event/alain-de-verneil-mediterranean-inst-oceanog raphy-biological-tracer-structure-in-the-surface-ocean-effects-of-mesoscal e-forcing-from-the-regional-to-sub-mesoscale-clark-507 END:VEVENT BEGIN:VEVENT UID:hnv2cijmd9pglo4enh8kaghedc@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160913T150500 DTEND;TZID=America/New_York:20160913T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Malcolm Scully\, WHOI. ‘Observations of the transfer of energy and momentum to the oceanic surface boundary layer beneath breaking waves.’ Cl ark 507. URL:http://oceans.mit.edu/event/malcolm-scully-whoi-observations-of-the-tra nsfer-of-energy-and-momentum-to-the-oceanic-surface-boundary-layer-beneath -breaking-waves-clark-507 END:VEVENT BEGIN:VEVENT UID:cs642cgnq9ccod34j0oo1ageg4@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160920T150500 DTEND;TZID=America/New_York:20160920T160000 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Viviane Menezes\, WHOI. ‘Accelerated freshening of Antarctic Bottom Waters over the last decade (2007-2016) in the Southern Indian Ocean’. Cl ark 507 URL:http://oceans.mit.edu/event/viviane-menezes-whoi-accelerated-freshening -of-antarctic-bottom-waters-over-the-last-decade-2007-2016-in-the-southern -indian-ocean-clark-507 END:VEVENT BEGIN:VEVENT UID:1s62fulcc4qrfrtkt5ajr7624g@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20160927T150500 DTEND;TZID=America/New_York:20160927T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Raffaele Ferrari\, MIT. ‘A model of the ocean overturning circulati on with two closed basins and a reentrant channel’. Clark 507 URL:http://oceans.mit.edu/event/raffaele-ferrari-mit-a-model-of-the-ocean-o verturning-circulation-with-two-closed-basins-and-a-reentrant-channel-clar k-507 END:VEVENT BEGIN:VEVENT UID:u7d38v147utkgtt0vr2lcjgffc@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161004T150500 DTEND;TZID=America/New_York:20161004T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Mohamad M. Nasr-Azadani\, UCSB. ‘Gravity currents in sheared and st ratified ambients: Numerical Simulations and vorticity modeling’. Clark 50 7 URL:http://oceans.mit.edu/event/mohamad-m-nasr-azadani-ucsb-tbd-clark-507 END:VEVENT BEGIN:VEVENT UID:j9on34pntp5s1upjojfldlb080@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161011T150500 DTEND;TZID=America/New_York:20161011T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Jian Zhao\, WHOI. ‘Mesoscale process in the Iceland Basin’. Clark 5 07 URL:http://oceans.mit.edu/event/jian-zhao-whoi-mesoscale-process-in-the-ice land-basin-clark-507 END:VEVENT BEGIN:VEVENT UID:di719bd44rdc10pg1jv5hlmvhg@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161013T140500 DTEND;TZID=America/New_York:20161013T150500 SEQUENCE:0 SUMMARY:Masatoshi Miyamoto\, U. Tokyo. ‘Characteristics and mechanisms of d eep mesoscale variability south of the Kuroshio Extension’. Clark 201 URL:http://oceans.mit.edu/event/masatoshi-miyamoto-u-tokyo-characteristics- and-mechanisms-of-deep-mesoscale-variability-south-of-the-kuroshio-extensi on-clark-201 END:VEVENT BEGIN:VEVENT UID:rdql31vrbpqiqslenbmvlupcj4@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161018T150500 DTEND;TZID=America/New_York:20161018T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Chris Piecuch\, Atmospheric and Environmental Research. ‘Inter annu al sea level changes on the North American Northeast Coast: Influence of l ocal atmospheric forcing’. Clark 507 URL:http://oceans.mit.edu/event/chris-piecuch-atmospheric-and-environmental -research-inter-annual-sea-level-changes-on-the-north-american-northeast-c oast-influence-of-local-atmospheric-forcing-clark-507 END:VEVENT BEGIN:VEVENT UID:dodrmf8dhrhm3e1ubac371jveo@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161025T150500 DTEND;TZID=America/New_York:20161025T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Karl Helfrich\, WHOI. ‘Instabilities of internal solitary waves’. C lark 507. URL:http://oceans.mit.edu/event/karl-helfrich-whoi-instabilities-of-interna l-solitary-waves-clark-507 END:VEVENT BEGIN:VEVENT UID:bpof1cjcge4mclu6vhgipc8hko@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161101T150500 DTEND;TZID=America/New_York:20161101T160500 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Henrik Soiland\, Inst. Marine Research. ‘The Lofoten Basin Eddy – a permanent feature of the Norwegian Sea’. Clark 201 URL:http://oceans.mit.edu/event/henrik-soiland-inst-marine-research-the-lof oten-basin-eddy-a-permanent-feature-of-the-norwegian-sea-clark-201 END:VEVENT BEGIN:VEVENT UID:rjr0jhqqa4vuokkj0ktj5bcago@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161108T150500 DTEND;TZID=America/New_York:20161108T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Xiaolin Zhang\, FSU. ‘On the Dynamical Relationship Between Equator ial Pacific Surface Currents\, Zonally-Averaged Equatorial Sea Level and E l Nino Prediction’. Clark 507 URL:http://oceans.mit.edu/event/xiaolin-zhang-fsu-on-the-dynamical-relation ship-between-equatorial-pacific-surface-currents-zonally-averaged-equatori al-sea-level-and-el-nino-prediction-clark-507 END:VEVENT BEGIN:VEVENT UID:201i0785oebclspj16qn89c9l0@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161115T150500 DTEND;TZID=America/New_York:20161115T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Sanjiv Ramachandran\, U. Mass Dartmouth. ‘Submesoscale processes in shallow\, stratified layers: observations from the Bay of Bengal during t he winter monsoon’. Clark 507 URL:http://oceans.mit.edu/event/sanjiv-ramachandran-u-mass-dartmouth-submes oscale-processes-in-shallow-stratified-layers-observations-from-the-bay-of -bengal-during-the-winter-monsoon-clark-507 END:VEVENT BEGIN:VEVENT UID:qsqa1mgrgh6pq3droobvhhr4g4@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161122T150500 DTEND;TZID=America/New_York:20161122T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Cancelled URL:http://oceans.mit.edu/event/cancelled-6 END:VEVENT BEGIN:VEVENT UID:qn510o9eftfon0877oph272tj0@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161129T150500 DTEND;TZID=America/New_York:20161129T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Mathieu Dever\, Dalhousie U. ‘Investigating the dynamics of a buoya nt coastal current using observations and a simple conceptual model’. Clar k 507. URL:http://oceans.mit.edu/event/open-3 END:VEVENT BEGIN:VEVENT UID:1vqdas7rpailo65d73688bl5c4@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161206T150500 DTEND;TZID=America/New_York:20161206T160500 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Terry Joyce\, WHOI. ‘On the slowing of the Deep Western Boundary Cu rrent southeast of Cape Cod: 2004-2014’. Clark 201 URL:http://oceans.mit.edu/event/open-5 END:VEVENT BEGIN:VEVENT UID:sji490aa80k4cd6l4v0ttdtk38@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161213T150500 DTEND;TZID=America/New_York:20161213T160500 SEQUENCE:0 SUMMARY:Cancelled URL:http://oceans.mit.edu/event/open-7 END:VEVENT BEGIN:VEVENT UID:41na9ve8oeu1kk3je5sdgjnagg@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161220T150500 DTEND;TZID=America/New_York:20161220T160500 SEQUENCE:0 SUMMARY:Cancelled URL:http://oceans.mit.edu/event/cancelled-10 END:VEVENT BEGIN:VEVENT UID:nhrv0urv9c3lpmtbhugav1qbio@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20161227T150500 DTEND;TZID=America/New_York:20161227T160500 SEQUENCE:0 SUMMARY:Cancelled URL:http://oceans.mit.edu/event/cancelled-7 END:VEVENT BEGIN:VEVENT UID:dkrhgngl4lmoe03n3bqn1s1ssg@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170103T150500 DTEND;TZID=America/New_York:20170103T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Cancelled URL:http://oceans.mit.edu/event/cancelled-5 END:VEVENT BEGIN:VEVENT UID:n2a24r058dp3p713notb7hrm2g@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170110T150500 DTEND;TZID=America/New_York:20170110T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Young-Oh Kwon\, WHOI. ‘North Atlantic Blocking Variability and Role of the Atlantic Multidecadal Oscillation’. Clark 507 URL:http://oceans.mit.edu/event/young-oh-kwon-whoi-north-atlantic-blocking- variability-and-role-of-the-atlantic-multidecadal-oscillation-clark-507 END:VEVENT BEGIN:VEVENT UID:diijpup835rtbtl3bb36rfguso@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:Lateral mixing by mesoscale eddies is widely recognized as a cr ucial mechanism for the global ocean circulation and the associated heat/s alt/tracer transports. The Salinity in the Upper Ocean Processes Study (SP URS) confirmed the importance of eddy mixing for the surface salinity fiel ds even in the center of the subtropical gyre of the North Atlantic. We fo cus on the global salinity maxima due to their role as indicators for glob al changes in the hydrological cycle as well as providing the source water masses for the shallow overturning circulation.\nWe introduce a novel app roach to estimate the contribution of eddy mixing to the global sea surfac e salinity maxima. Using a global 2D tracer experiments in a 1/10 degree M ITgcm setup driven by observed surface velocities\, we analyze the effect of eddy mixing using a water mass framework\, thus focussing on the diffus ive flux across surface isohalines. This enables us to diagnose temporal v ariability on seasonal to inter annual time scales\, revealing regional di fferences in the mechanism causing temporal variability.Sensitivity experi ments with various salinity backgrounds reveal robust inter annual variabi lity caused by changes in the surface velocity fields potentially forced b y large scale climate. DTSTART;TZID=America/New_York:20170117T150500 DTEND;TZID=America/New_York:20170117T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Julius Busecke\, LDEO. ‘Temporal variability in eddy mixing in the global subtropics’. Clark 507. URL:http://oceans.mit.edu/event/julius-busecke-ldeo-temporal-variability-in -eddy-mixing-in-the-global-subtropics-clark-507 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nLateral mixing b y mesoscale eddies is widely recognized as a crucial mechanism for the glo bal ocean circulation and the associated heat/salt/tracer transports. The Salinity in the Upper Ocean Processes Study (SPURS) confirmed the importan ce of eddy mixing for the surface salinity fields even in the center of th e subtropical gyre of the North Atlantic. We focus on the global salinity maxima due to their role as indicators for global changes in the hydrologi cal cycle as well as providing the source water masses for the shallow ove rturning circulation.\nWe introduce a novel approach to estimate the contr ibution of eddy mixing to the global sea surface salinity maxima. Using a global 2D tracer experiments in a 1/10 degree MITgcm setup driven by obser ved surface velocities\, we analyze the effect of eddy mixing using a wate r mass framework\, thus focussing on the diffusive flux across surface iso halines. This enables us to diagnose temporal variability on seasonal to i nter annual time scales\, revealing regional differences in the mechanism causing temporal variability.Sensitivity experiments with various salinity backgrounds reveal robust inter annual variability caused by changes in t he surface velocity fields potentially forced by large scale climate. END:VEVENT BEGIN:VEVENT UID:0c6arp1d01o746e526qphr8ntk@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170119T140500 DTEND;TZID=America/New_York:20170119T150500 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Carina Bringedal\, U. Bergen. ‘Idealized models for wind driven var iations in an overturning circulation’. Clark 201. URL:http://oceans.mit.edu/event/carina-bringedal-u-bergen-idealized-models- for-wind-driven-variations-in-an-overturning-circulation-clark-201 END:VEVENT BEGIN:VEVENT UID:b2cucnmv3pe11dr4k3lgc1nj1c@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170124T150500 DTEND;TZID=America/New_York:20170124T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:David Nieves\, WHOI. ‘Non-hydrostatic\, rapidly rotating and stably stratified flows’. Clark 507 URL:http://oceans.mit.edu/event/david-nieves-whoi-non-hydrostatic-rapidly-r otating-and-stably-stratified-flows-clark-507 END:VEVENT BEGIN:VEVENT UID:nol9amv4bcuebgiunj177dn9q0@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170131T150500 DTEND;TZID=America/New_York:20170131T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Rhys Parfitt\, WHOI. ‘To what extent do oceanic frontal zones affec t mid-latitude weather and climate?’. Clark 507. URL:http://oceans.mit.edu/event/rhys-parfitt-whoi-to-what-extent-do-oceanic -frontal-zones-affect-mid-latitude-weather-and-climate-clark-507 END:VEVENT BEGIN:VEVENT UID:t5ke92ulk1dnd2rbqjqu41l4as@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170207T150500 DTEND;TZID=America/New_York:20170207T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Tom Rossby\, URI. ‘Currents\, fluxes and the MOC between Cape Farew ell and Scotland’. Clark 507. URL:http://oceans.mit.edu/event/tom-rossby-uri-currents-fluxes-and-the-moc- between-cape-farewell-and-scotland-clark-507 END:VEVENT BEGIN:VEVENT UID:me9klcq795qiesh92ut2brjc4g@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170214T150500 DTEND;TZID=America/New_York:20170214T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Kate Lowry\, WHOI. ‘The influence of sea ice and hydrography on phy toplankton bloom dynamics in the Chukchi Sea’. Clark 507 URL:http://oceans.mit.edu/event/open-9 END:VEVENT BEGIN:VEVENT UID:usev2apv2hqk7s86sv039o2bf4@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170216T140500 DTEND;TZID=America/New_York:20170216T150000 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Steingrimur Jonsson\, U. Akureyri. ‘Study of water exchange\, circu lation and oxygen levels in a small fjord in Iceland following the death o f 52 thousand tons of herring’. Clark 201 URL:http://oceans.mit.edu/event/steingrimur-jonsson-university-of-akureyri- tbd-clark-201 END:VEVENT BEGIN:VEVENT UID:hn0vrl3v3khlk6nb701l05d7ac@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170221T150500 DTEND;TZID=America/New_York:20170221T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Matthew Falder\, U. Birmingham. ‘Sharp transition from internal wav es to stratified turbulence observed in seismic reflection images’. Clark 507 URL:http://oceans.mit.edu/event/matthew-falder-u-birmingham-sharp-transitio n-from-internal-waves-to-stratified-turbulence-observed-in-seismic-reflect ion-images-clark-507 END:VEVENT BEGIN:VEVENT UID:vt5avemev1nv2u36npr0hkdqg4@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:The Brewer-Dobson circulation\, the meridional overturning of m ass in the stratosphere\, is important for the distribution of gases in th e stratosphere\, such as ozone and water vapor\, which impact surface clim ate. I will present a theory that relates the ideal tracer 'age of air' to this circulation strength. Age can be determined from certain trace gases \, and I have applied the theory to obtain the first data-based estimate o f the global meridional overturning circulation of the stratosphere. When I compare this to models and reanalysis data\, I find substantial disagree ment. I will then show how age of air provides enough information to deter mine the full circulation by deriving a quantitative relationship between the age distribution and the adiabatic component of the circulation. DTSTART;TZID=America/New_York:20170228T150500 DTEND;TZID=America/New_York:20170228T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Marianna Linz\, MIT/WHOI. ‘A theory for calculating the strength of the stratospheric circulation from age’. Clark 507 URL:http://oceans.mit.edu/event/marianna-linz-mitwhoi-a-theory-for-calculat ing-the-strength-of-the-stratospheric-circulation-from-age-clark-507 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nThe Brewer-Dobso n circulation\, the meridional overturning of mass in the stratosphere\, i s important for the distribution of gases in the stratosphere\, such as oz one and water vapor\, which impact surface climate. I will present a theor y that relates the ideal tracer 'age of air' to this circulation strength. Age can be determined from certain trace gases\, and I have applied the t heory to obtain the first data-based estimate of the global meridional ove rturning circulation of the stratosphere. When I compare this to models an d reanalysis data\, I find substantial disagreement. I will then show how age of air provides enough information to determine the full circulation b y deriving a quantitative relationship between the age distribution and th e adiabatic component of the circulation.\n END:VEVENT BEGIN:VEVENT UID:lora794199g0vou53mqqarjl7k@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170307T150500 DTEND;TZID=America/New_York:20170307T160500 SEQUENCE:0 SUMMARY:Jake Gebbie\, Irina Rypina and Amala Mahadevan\, WHOI. From Circula tion to Mixing — Some Vignettes of Physical Oceanography. Clark 201 URL:http://oceans.mit.edu/event/reserved-3 END:VEVENT BEGIN:VEVENT UID:di3t8ip1keifimq60bi5cjnl2s@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170314T150500 DTEND;TZID=America/New_York:20170314T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Bernadette Sloyan\, CSIRO. ‘Sustained Ocean Observations: the role of the OOPC (Ocean Observations Physics and Climate panel)’. Clark 507 URL:http://oceans.mit.edu/event/bernadette-sloyan-csiro-tbd-clark-507 END:VEVENT BEGIN:VEVENT UID:oma9kf030v4ftord9je507b98o@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170321T150500 DTEND;TZID=America/New_York:20170321T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Cancelled URL:http://oceans.mit.edu/event/open-2 END:VEVENT BEGIN:VEVENT UID:ff3a92mf45iu10cje3af9r9mqo@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170328T150500 DTEND;TZID=America/New_York:20170328T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Sylvia Cole\, WHOI. ‘Momentum transfer in the Arctic marginal ice z one’. Clark 507 URL:http://oceans.mit.edu/event/open-14 END:VEVENT BEGIN:VEVENT UID:9h0jovectfkaab2napoa62gnkk@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170404T150500 DTEND;TZID=America/New_York:20170404T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Joseph LaCasce\, University of Oslo. ‘The vertical structure of Ros sby waves’. Clark 507 URL:http://oceans.mit.edu/event/joseph-lacasce-university-of-oslo-the-verti cal-structure-of-rossby-waves-clark-507 END:VEVENT BEGIN:VEVENT UID:89gv4i0rhdeo0bse4sf5f2elmg@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170411T150500 DTEND;TZID=America/New_York:20170411T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Thomas Kilpatrick\, SIO. ‘Satellite observations of convection–wind coupling’. Clark 507 URL:http://oceans.mit.edu/event/open-6 END:VEVENT BEGIN:VEVENT UID:j6njfjc73iuk9abfq9qde001tg@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170418T150500 DTEND;TZID=America/New_York:20170418T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Allan Clarke\, FSU. ‘On the relationship of near-surface flow\, Sto kes drift and wind stress’. Clark 507 URL:http://oceans.mit.edu/event/allan-clarke-fsu-tbd-clark-507 END:VEVENT BEGIN:VEVENT UID:dcvaefdedl9v3knqs5dl1celbo@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:The Intertropical Convergence Zone (ITCZ)\, also known as the d oldrums\, is the area just north of the equator where the northeast and so utheast trade winds converge. We discuss the role of the ocean in pushing the ITCZ northwards away from the equator and in modulating its meridional migrations. DTSTART;TZID=America/New_York:20170425T150500 DTEND;TZID=America/New_York:20170425T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:John Marshall\, MIT. ‘Inter-hemispheric asymmetries in climate: Oce ans and the Inter-tropical Convergence Zone’. Clark 507 URL:http://oceans.mit.edu/event/open X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nThe Intertropica l Convergence Zone (ITCZ)\, also known as the doldrums\, is the area just north of the equator where the northeast and southeast trade winds converg e. We discuss the role of the ocean in pushing the ITCZ northwards away fr om the equator and in modulating its meridional migrations. END:VEVENT BEGIN:VEVENT UID:20170502T150500-02mm6q7uplh244fa4f7at8slfk_R20170502T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170502T150500 DTEND;TZID=America/New_York:20170502T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Jack Whitehead\, WHOI. ‘Dimensions of continents and oceans – water has carved a perfect cistern’. Clark 507 URL:http://oceans.mit.edu/event/reserved-7 END:VEVENT BEGIN:VEVENT UID:02mm6q7uplh244fa4f7at8slfk@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170502T150500 DTEND;TZID=America/New_York:20170502T160500 LOCATION:Clark 507 RRULE:FREQ=WEEKLY;UNTIL=20170502T190459Z;BYDAY=TU SEQUENCE:0 SUMMARY:OPEN URL:http://oceans.mit.edu/event/open-4 END:VEVENT BEGIN:VEVENT UID:02mm6q7uplh244fa4f7at8slfk_R20170502T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170502T150500 DTEND;TZID=America/New_York:20170502T160500 EXDATE;TZID=America/New_York:20170502T150500 EXDATE;TZID=America/New_York:20170509T150500 EXDATE;TZID=America/New_York:20170516T150500 LOCATION:Clark 507 RRULE:FREQ=WEEKLY;UNTIL=20170530T190459Z;BYDAY=TU SEQUENCE:0 SUMMARY:Reserved. URL:http://oceans.mit.edu/event/reserved-2 END:VEVENT BEGIN:VEVENT UID:20170509T150500-02mm6q7uplh244fa4f7at8slfk_R20170502T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170509T150500 DTEND;TZID=America/New_York:20170509T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Viviane Menezes\, WHOI. ‘Air-Sea Interaction\, Water Mass Formation and Ocean Circulation — From warm-salty (Red Sea) to cold-fresh waters (S outhern Ocean)’. Clark 507 URL:http://oceans.mit.edu/event/reserved-6 END:VEVENT BEGIN:VEVENT UID:20170516T150500-02mm6q7uplh244fa4f7at8slfk_R20170502T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170516T150500 DTEND;TZID=America/New_York:20170516T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Robert Todd\, WHOI. ‘New views of the Gulf Stream’. Clark 507 URL:http://oceans.mit.edu/event/reserved END:VEVENT BEGIN:VEVENT UID:20170523T150500-02mm6q7uplh244fa4f7at8slfk_R20170502T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170523T150500 DTEND;TZID=America/New_York:20170523T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Nick Beaird\, WHOI. ‘Production\, Export\, and Oceanic Impacts of G reenland’s glacial meltwater’. Clark 201 URL:http://oceans.mit.edu/event/reserved-4 END:VEVENT BEGIN:VEVENT UID:02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170530T150500 DTEND;TZID=America/New_York:20170530T160500 EXDATE;TZID=America/New_York:20170613T150500 EXDATE;TZID=America/New_York:20170627T150500 EXDATE;TZID=America/New_York:20170704T150500 EXDATE;TZID=America/New_York:20170711T150500 EXDATE;TZID=America/New_York:20171226T150500 LOCATION:Clark 507 RRULE:FREQ=WEEKLY;UNTIL=20171226T200500Z;BYDAY=TU SEQUENCE:0 SUMMARY:OPEN URL:http://oceans.mit.edu/event/open-24 END:VEVENT BEGIN:VEVENT UID:20170530T150500-02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170530T150500 DTEND;TZID=America/New_York:20170530T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Ruth Musgrave\, MIT. ‘ The generation of Rossby waves and wake eddi es by small islands’. Clark 507 URL:http://oceans.mit.edu/event/reserved-5 END:VEVENT BEGIN:VEVENT UID:20170606T150500-02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170606T150500 DTEND;TZID=America/New_York:20170606T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Christopher Piecuch\, AER. ‘A Bayesian Perspective on Recent Mean S ea Level Changes along the United States East Coast’. Clark 507 URL:http://oceans.mit.edu/event/robert-todd-whoi-tbd-clark-507 END:VEVENT BEGIN:VEVENT UID:0o6l8uh32k8iu2p22cd5ggjhks@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:I will demonstrate the tools that allow to perform analytic\, i .e. mathematically rigorous\, proofs of chaos in various models. This incl udes the proof of the birth of the Lorenz attractor in the Lorenz model. I n future\, the further development of such tools and criteria will be very useful for the study of applied problems. DTSTART;TZID=America/New_York:20170608T140500 DTEND;TZID=America/New_York:20170608T150500 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Ivan Ovsyannikov\, U. Bremen. ‘Analytic proof of chaotic regimes in dynamical models’. Clark 271 URL:http://oceans.mit.edu/event/ivan-ovsyannikov-u-bremen-analytic-proof-of -chaotic-regimes-in-dynamical-models-clark-201 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nI will demonstra te the tools that allow to perform analytic\, i.e. mathematically rigorous \, proofs of chaos in various models. This includes the proof of the birth of the Lorenz attractor in the Lorenz model. In future\, the further deve lopment of such tools and criteria will be very useful for the study of ap plied problems. END:VEVENT BEGIN:VEVENT UID:20170613T150500-02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170613T150500 DTEND;TZID=America/New_York:20170613T160500 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Georgy Manucharyan\, CalTech. ‘The role of mesoscale eddies in the Ekman-driven variability of the Beaufort Gyre’. Clark 201 URL:http://oceans.mit.edu/event/xinfeng-liang-u-south-florida-tbd-clark-507 END:VEVENT BEGIN:VEVENT UID:20170620T150500-02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION:Observations show that the upper ocean has been warming since t he 1970s\, and it is usually attributed to global warming that is associat ed with the increasing concentration of greenhouse gases in the atmosphere . The global ocean is implicitly considered as a passive heat reservoir\, and it is assumed that the ocean was in equilibrium with the atmosphere be fore the anthropogenic global warming had occurred. However\, the global o cean is a dynamically active heat exchanger involving processes of various temporal and spatial scales and has a memory of thousands of years. Not o nly the heat exchange between ocean and atmosphere but the vertical heat f lux passing the lower face of the upper ocean contribute to the changes in the observed upper ocean heat content. In this talk\, I will present the mean and the bidecadal change of the ocean vertical heat flux as well as t he related physical processes from a dynamically consistent and data-const rained ocean state estimate - ECCO (Estimating the Circulation & Climate o f the Ocean). Implications of the vertical redistribution of ocean heat on the changes of the upper and deep ocean heat contents\, particularly the recently much-debated global warming 'hiatus'\, will also be discussed. DTSTART;TZID=America/New_York:20170620T150500 DTEND;TZID=America/New_York:20170620T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Xinfeng Liang\, U. South Florida. ‘Vertical Redistribution of the G lobal Oceanic Heat Content’. Clark 507 URL:http://oceans.mit.edu/event/xinfeng-liang-u-south-florida-tbd-clark-507 -2 X-ALT-DESC;FMTTYPE=text/html:\\n\\n\\n\\n\\nObservations sho w that the upper ocean has been warming since the 1970s\, and it is usuall y attributed to global warming that is associated with the increasing conc entration of greenhouse gases in the atmosphere. The global ocean is impli citly considered as a passive heat reservoir\, and it is assumed that the ocean was in equilibrium with the atmosphere before the anthropogenic glob al warming had occurred. However\, the global ocean is a dynamically activ e heat exchanger involving processes of various temporal and spatial scale s and has a memory of thousands of years. Not only the heat exchange betwe en ocean and atmosphere but the vertical heat flux passing the lower face of the upper ocean contribute to the changes in the observed upper ocean h eat content. In this talk\, I will present the mean and the bidecadal chan ge of the ocean vertical heat flux as well as the related physical process es from a dynamically consistent and data-constrained ocean state estimate - ECCO (Estimating the Circulation & Climate of the Ocean). Implications of the vertical redistribution of ocean heat on the changes of the upper a nd deep ocean heat contents\, particularly the recently much-debated globa l warming 'hiatus'\, will also be discussed. END:VEVENT BEGIN:VEVENT UID:20170627T150500-02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170627T150500 DTEND;TZID=America/New_York:20170627T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Alison Macdonald\, WHOI. ‘A 2011-2015 Fukushima Tracer Perspective on North Pacific Mode Water Circulation’. Clark 507 URL:http://oceans.mit.edu/event/alison-macdonald-whoi-a-2011-2015-fukushima -tracer-perspective-on-north-pacific-mode-water-circulation-clark-507 END:VEVENT BEGIN:VEVENT UID:lkesstjn8205ioc4aknguoemgo@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170706T020500 DTEND;TZID=America/New_York:20170706T030500 SEQUENCE:0 SUMMARY:Takashi Ijichin\, University of Tokyo. ‘Evaluation of mixing coeffi cients in the deep ocean’. Clark 201 URL:http://oceans.mit.edu/event/takashi-ijichin-university-of-tokyo-evaluat ion-of-mixing-coefficients-in-the-deep-ocean-clark-201 END:VEVENT BEGIN:VEVENT UID:20170711T150500-02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170711T150500 DTEND;TZID=America/New_York:20170711T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Tom Farrar\, WHOI. ‘TBD’. Clark 507 URL:http://oceans.mit.edu/event/tom-farrar-whoi-tbd-clark-507 END:VEVENT BEGIN:VEVENT UID:20170718T150500-02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170718T150500 DTEND;TZID=America/New_York:20170718T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Andreas Thurnherr\, LDEO. ‘TBD’. Clark 507 URL:http://oceans.mit.edu/event/andreas-thurnherr-ldeo-tbd-clark-507 END:VEVENT BEGIN:VEVENT UID:uuvh70g3tlchlo4hdgv7ckruvs@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170720T140500 DTEND;TZID=America/New_York:20170720T150500 SEQUENCE:0 SUMMARY:Lisa Beal\, U. Miami. ‘TBD’. Clark 201. URL:http://oceans.mit.edu/event/lisa-beal-u-miami-tbd-clark-201 END:VEVENT BEGIN:VEVENT UID:bkm5rpdofo7qrkm5dlv8r374io@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170727T140500 DTEND;TZID=America/New_York:20170727T150500 LOCATION:Clark 201 SEQUENCE:0 SUMMARY:Christopher Wolfe\, Stony Brook University. ‘TBD’. Clark 201 URL:http://oceans.mit.edu/event/christopher-wolfe-stony-brook-university-tb d-clark-201 END:VEVENT BEGIN:VEVENT UID:20170801T150500-02mm6q7uplh244fa4f7at8slfk_R20170530T190500@google.com DTSTAMP:20180503T083650Z CATEGORIES;LANGUAGE=en-US:WHOI Seminar | Physical Oceanography CONTACT: DESCRIPTION: DTSTART;TZID=America/New_York:20170801T150500 DTEND;TZID=America/New_York:20170801T160500 LOCATION:Clark 507 SEQUENCE:0 SUMMARY:Alexey Fedorov\, Yale University. ‘TBD’. Clark 507 URL:http://oceans.mit.edu/event/alexey-fedorov-yale-university-tbd-clark-50 7 END:VEVENT END:VCALENDAR