Small scale mixing in coastal areas
|
|
- Sylvia Lang
- 5 years ago
- Views:
Transcription
1 Spice in coastal areas 1, Jody Klymak 1, Igor Yashayaev 2 University of Victoria 1 Bedford Institute of Oceanography 2 19 October, 2015
2 Spice Lateral stirring on scales less than the Rossby radius are rarely observed. Labrador Sea has large salinity contracts between the Labrador Current and the main basin. Goal1: Improving understanding of upper ocean by examining transects in the Labrador Sea (Part A).
3 Spice Lateral stirring on scales less than the Rossby radius are rarely observed. Labrador Sea has large salinity contracts between the Labrador Current and the main basin. Goal1: Improving understanding of upper ocean by examining transects in the Labrador Sea (Part A). Goal2: Understanding the mechanisms of the enhanced submesoscale activity in the winter mixed layer using ADCP data (Part B).
4 Moving Vessel Profiler Moving Vessel Profiler Collecting data sets from both shallow (100m) and deep water( Maximum-800m) Primary function: Without the need to stop the vessel Spice Figure: The MVP deployed from a typical vessel collecting three sets of profile data Figure: It shows the path of the Free Fall Fish for a typical cast.
5 Spice Figure: Locations of data with Survey A section noted by the black arrow MVP can capture both lateral and vertical information; Downcasts were used for the ; Vertical and horizontal resolution are 0.5m and 6.5km, respectively; The ship s speed is 6m/s on average.
6 Spice: γ = sgn(t T )(α 2 (T T ) 2 + β 2 (S S) 2 ) 1 2 Spice Figure: Temperature-salinity plot from SurveyA. Color dots indicate distance along the line, with red indicating south and gray shows north. Black curves is the mean for the section used to calculate spice along isopycnals. Figure: a) Salinity and b) temperature along Survey A plotted at the mean depth of the isopycnals with isopycnals contoured in black lines c) Spice,, plotted on isopycnal depths.
7 Spice statistics: Lateral decorrelation length scale The length scales reflect the size of eddies stirring the fluid Spice Figure: Lateral lag correlations for high-passed (λ less than 50km ) spice along isopycnals. Individual traces are in grey, and the average for the depth bin is colored. The short black line represents the decorrelation scale, which is defined as when the mean trace first drop below a lag correlation of 0.1.
8 Spice statistics: Spice spectra Spice Indicate what physical processes are stirring the tracer along isopycnals Figure: Spectra of lateral spice variation based on different depth bins, normalized by large-scale spice gradient. The dashed lines are power law fit over wavenumber range cpkm to 0.04 cpkm. The deep spectra is redder with depth, which indicates that more dissipation of lateral variance with depth The redder spectra in depth is the opposite of the trend predicted by QG/SQG theory What is happened here?
9 Spice statistics: PDF of lateral spice gradient Spice Peaked pdf compared with normal distribution Fontogenesis is acting sharpen small scale gradients. Other spice statistics: Figure: PDF of normalized spice gradient with two depth bins of m and m.
10 Spice statistics: PDF of lateral spice gradient Spice Peaked pdf compared with normal distribution Fontogenesis is acting sharpen small scale gradients. Other spice statistics: Lateral displacement; Figure: PDF of normalized spice gradient with two depth bins of m and m.
11 Spice statistics: PDF of lateral spice gradient Spice Peaked pdf compared with normal distribution Fontogenesis is acting sharpen small scale gradients. Other spice statistics: Lateral displacement; Vertical de-coherence length scales Figure: PDF of normalized spice gradient with two depth bins of m and m.
12 Part B : ADCP Spice
13 Part B: Observational transection Spice N N N N 47.5 N W W W W W Figure: Maps showing LineP line.
14 Part B: Observational results Spice Depth[m] U (Along track) Distance from LineP Depth[m] V (Across track) Distance from LineP Figure: Along track (U) and across track (V) velocities in the upper 500m.
15 Part B: Observational results Spice Power spectrum density (m 3 s 2 ) Cu: Along track power spectra k 2 Cu Wavenumber k x [cpkm] Cv: Across track power spectra k 2 Cv Wavenumber k x [cpkm] Figure: Power spectrum of observed transverse (a) and longitudinal (b) kinetic energy at depth of 152m.
16 Part B: Observational results Helmholtz decomposition: Spice PSD m (a) k m (b) k m (c) k K ψ : non-divergent k 3 K φ : divergent wavenumber[cpkm 1 ] K ψ : non-divergent k 3 K φ : divergent wavenumber[cpkm 1 ] K ψ : non-divergent k 3 K φ : divergent wavenumber[cpkm 1 ] Figure: ADCP KE spectrum for three layers: (a) m, (b) m, and (c) m. The figure shows along-track (blue line) and across-track (green line) KE spectra, and the spectral decomposition into horizontally rotational (red line) and divergent components (cyan line).
17 Whether there is a seasonal cycle for the submesoscale in the upper mixed layer? Spice
18 Spice Whether there is a seasonal cycle for the submesoscale in the upper mixed layer? How the seasonality in the submesoscale turbulence affects the exchanges of the nutrients between the nutrient-depleted mixed layer and the nutrient-rich thermocline?
19 Spice Whether there is a seasonal cycle for the submesoscale in the upper mixed layer? How the seasonality in the submesoscale turbulence affects the exchanges of the nutrients between the nutrient-depleted mixed layer and the nutrient-rich thermocline? Applying these methodology for modelling data (Youyu Lu).
20 Spice
that individual/local amplitudes of Ro can reach O(1).
Supplementary Figure. (a)-(b) As Figures c-d but for Rossby number Ro at the surface, defined as the relative vorticity ζ divided by the Coriolis frequency f. The equatorial band (os-on) is not shown due
More informationLateral Mixing Progress Report November 8, 2012
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Lateral Mixing Progress Report November 8, 2012 Jody Klymak School of Earth and Ocean Sciences University of Victoria P.O.
More informationDecomposing kinetic energy along Line P in the Pacific ocean. Manman Wang B.Sc., Ocean University of China, 2012
Decomposing kinetic energy along Line P in the Pacific ocean by Manman Wang B.Sc., Ocean University of China, 2012 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master
More informationmeso to submesoscale!
meso to submesoscale! horizontal wavenumber spectra! in Drake Passage Cesar B Rocha*! Teresa K Chereskin* Sarah T Gille* Dimitris Menemenlis+ * : SIO, UC San Diego +: JPL, NASA Snapshot of surface relative
More information2013 Annual Report for Project on Isopycnal Transport and Mixing of Tracers by Submesoscale Flows Formed at Wind-Driven Ocean Fronts
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. 2013 Annual Report for Project on Isopycnal Transport and Mixing of Tracers by Submesoscale Flows Formed at Wind-Driven
More informationFinescale Water-Mass Variability from ARGO Profiling Floats
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Finescale Water-Mass Variability from ARGO Profiling Floats Eric Kunze Applied Physics Lab, University of Washington 1013
More informationLateral Mixing Progress Report November 8, 2012
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Lateral Mixing Progress Report November 8, 2012 Jody Klymak School of Earth and Ocean Sciences University of Victoria P.O.
More informationSeismic Reflection Methods for Study of the Water Column
Contribution MS number 581 for Encyclopedia of Ocean Sciences Seismic Reflection Methods for Study of the Water Column Ilker Fer Bjerknes Centre for Climate Research, and Geophysical Institute University
More informationGoals of this Chapter
Waves in the Atmosphere and Oceans Restoring Force Conservation of potential temperature in the presence of positive static stability internal gravity waves Conservation of potential vorticity in the presence
More informationDISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Lateral Mixing
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Lateral Mixing Eric A. D Asaro APL/UW 1013 NE 40 th Str Seattle, WA 98105 phone: (206) 685-2982 fax: (206) 543-6785 email:
More informationprimitive equation simulation results from a 1/48th degree resolution tell us about geostrophic currents? What would high-resolution altimetry
Scott 2008: Scripps 1 What would high-resolution altimetry tell us about geostrophic currents? results from a 1/48th degree resolution primitive equation simulation Robert B. Scott and Brian K. Arbic The
More informationSIO 210: Data analysis
SIO 210: Data analysis 1. Sampling and error 2. Basic statistical concepts 3. Time series analysis 4. Mapping 5. Filtering 6. Space-time data 7. Water mass analysis 10/8/18 Reading: DPO Chapter 6 Look
More informationSIO 210: Data analysis methods L. Talley, Fall Sampling and error 2. Basic statistical concepts 3. Time series analysis
SIO 210: Data analysis methods L. Talley, Fall 2016 1. Sampling and error 2. Basic statistical concepts 3. Time series analysis 4. Mapping 5. Filtering 6. Space-time data 7. Water mass analysis Reading:
More informationSAMS Gliders: Research Activities
SAMS Gliders: Research Activities Mark Inall, Toby Sherwin, Stuart Cunningham Estelle Dumont, Marie Porter, Dmitry Aleynik Scottish Association for Marine Science Scottish Marine Institute Oban PA37 1QA
More informationLecture 17 ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY. Learning objectives: understand the concepts & physics of
ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY Lecture 17 Learning objectives: understand the concepts & physics of 1. Ekman layer 2. Ekman transport 3. Ekman pumping 1. The Ekman Layer Scale analyses
More informationModeling and Parameterizing Mixed Layer Eddies
Modeling and Parameterizing Mixed Layer Eddies Baylor Fox-Kemper (MIT) with Raffaele Ferrari (MIT), Robert Hallberg (GFDL) Los Alamos National Laboratory Wednesday 3/8/06 Mixed Layer Eddies Part I: Baroclinic
More informationSIO 210 CSP: Data analysis methods L. Talley, Fall Sampling and error 2. Basic statistical concepts 3. Time series analysis
SIO 210 CSP: Data analysis methods L. Talley, Fall 2016 1. Sampling and error 2. Basic statistical concepts 3. Time series analysis 4. Mapping 5. Filtering 6. Space-time data 7. Water mass analysis Reading:
More informationComparison Figures from the New 22-Year Daily Eddy Dataset (January April 2015)
Comparison Figures from the New 22-Year Daily Eddy Dataset (January 1993 - April 2015) The figures on the following pages were constructed from the new version of the eddy dataset that is available online
More informationWave vortex decomposition of one-dimensional ship-track data
J. Fluid Mech. (014), vol. 756, pp. 1007 106. c Cambridge University Press 014 doi:10.1017/jfm.014.488 1007 Wave vortex decomposition of one-dimensional ship-track data Oliver Bühler 1,, Jörn Callies and
More informationDISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Lateral Mixing
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Lateral Mixing Eric A. D Asaro APL/UW 1013 NE 40 th Str Seattle, WA 98105 phone: (206) 685-2982 fax: (206) 543-6785 email:
More informationOcean Dynamics. The Great Wave off Kanagawa Hokusai
Ocean Dynamics The Great Wave off Kanagawa Hokusai LO: integrate relevant oceanographic processes with factors influencing survival and growth of fish larvae Physics Determining Ocean Dynamics 1. Conservation
More informationDISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Lateral Mixing
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Lateral Mixing Eric A. D Asaro APL/UW 1013 NE 40 th Str Seattle, WA 98105 phone: (206) 685-2982 fax: (206) 543-6785 email:
More informationCHAPTER 7 Ocean Circulation Pearson Education, Inc.
CHAPTER 7 Ocean Circulation 2011 Pearson Education, Inc. Types of Ocean Currents Surface currents Deep currents 2011 Pearson Education, Inc. Measuring Surface Currents Direct methods Floating device tracked
More informationInternal Waves in the Vicinity of the Kuroshio Path
Internal Waves in the Vicinity of the Kuroshio Path Ren-Chieh Lien Applied Physics Laboratory University of Washington Seattle, Washington 98105 phone: (206) 685-1079 fax: (206) 543-6785 email: lien@apl.washington.edu
More informationLab 12: El Nino Southern Oscillation
Name: Date: OCN 104: Our Dynamic Ocean Lab 12: El Nino Southern Oscillation Part 1: Observations of the tropical Pacific Ocean during a normal year The National Oceanographic and Atmospheric Administration
More informationA Comparison of Predicted Along-channel Eulerian Flows at Cross- Channel Transects from an EFDC-based Model to ADCP Data in South Puget Sound
A Comparison of Predicted Along-channel Eulerian Flows at Cross- Channel Transects from an EFDC-based Model to ADCP Data in South Puget Sound Skip Albertson, J. A. Newton and N. Larson Washington State
More informationMean Stream-Coordinate Structure of the Kuroshio Extension First Meander Trough
Mean Stream-Coordinate Structure of the Kuroshio Extension First Meander Trough 6 March, 2008 Penelope J. Howe, Kathleen A. Donohue, and D. Randolph Watts Graduate School of Oceanography University of
More informationSubmesoscale Routes to Lateral Mixing in the Ocean
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Submesoscale Routes to Lateral Mixing in the Ocean Amit Tandon Physics Department, UMass Dartmouth 285 Old Westport Rd
More informationDecadal variability in the Kuroshio and Oyashio Extension frontal regions in an eddy-resolving OGCM
Decadal variability in the Kuroshio and Oyashio Extension frontal regions in an eddy-resolving OGCM Masami Nonaka 1, Hisashi Nakamura 1,2, Youichi Tanimoto 1,3, Takashi Kagimoto 1, and Hideharu Sasaki
More informationThermohaline and wind-driven circulation
Thermohaline and wind-driven circulation Annalisa Bracco Georgia Institute of Technology School of Earth and Atmospheric Sciences NCAR ASP Colloquium: Carbon climate connections in the Earth System Tracer
More informationTurbulence and mixing within anticyclonic eddies in the Mediterranean sea during BOUM experiment
Turbulence and mixing within anticyclonic eddies in the Mediterranean sea during BOUM experiment Yannis Cuypers, Pascale Bouruet-Aubertot, Claudie Marec, Jean-Luc Fuda BOUM Objectives Biogeochimie de l'oligotrophie
More informationBaltic Sea Research Institute
Baltic Sea Research Institute Warnemuende (IOW) Cruise Report No. 44/96/ 04 R/V "A.v.Humboldt" MESODYN Cruise 01 to 12 March 1996 Stolpe Furrow / Baltic Sea This report is based on preliminary data and
More informationWave vortex decomposition of one-dimensional shiptrack
Wave vortex decomposition of one-dimensional shiptrack data The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation As Published
More informationGeneration and Evolution of Internal Waves in Luzon Strait
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Generation and Evolution of Internal Waves in Luzon Strait Ren-Chieh Lien Applied Physics Laboratory University of Washington
More informationSUPPLEMENTARY INFORMATION
Figure S1. Summary of the climatic responses to the Gulf Stream. On the offshore flank of the SST front (black dashed curve) of the Gulf Stream (green long arrow), surface wind convergence associated with
More informationSubmesoscale Dynamics of the South China Sea
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Submesoscale Dynamics of the South China Sea Craig M. Lee Applied Physics Laboratory, 1013 NE 40 th St, Seattle, WA 98105
More informationScalable Lateral Mixing and Coherent Turbulence DRI: Use of an AUV to Quantify Submesoscale Mixing Processes
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Scalable Lateral Mixing and Coherent Turbulence DRI: Use of an AUV to Quantify Submesoscale Mixing Processes Louis Goodman
More informationFRICTION-DOMINATED WATER EXCHANGE IN A FLORIDA ESTUARY
FRICTION-DOMINATED WATER EXCHANGE IN A FLORIDA ESTUARY By KIMBERLY ARNOTT A THESIS PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE
More informationTutorial School on Fluid Dynamics: Aspects of Turbulence Session I: Refresher Material Instructor: James Wallace
Tutorial School on Fluid Dynamics: Aspects of Turbulence Session I: Refresher Material Instructor: James Wallace Adapted from Publisher: John S. Wiley & Sons 2002 Center for Scientific Computation and
More informationWinds and Global Circulation
Winds and Global Circulation Atmospheric Pressure Winds Global Wind and Pressure Patterns Oceans and Ocean Currents El Nino How is Energy Transported to its escape zones? Both atmospheric and ocean transport
More informationSimulation of Lagrangian Drifters in the Labrador Sea
Simulation of Lagrangian Drifters in the Labrador Sea Roland W. Garwood Jr. and Ramsey R. Harcourt Department of Oceanography Naval Postgraduate School 833 Dyer Rd Rm 328 Monterey, CA 93943-5193 phone:
More informationDIAMIX an experimental study of diapycnal deepwater mixing in the virtually tideless Baltic Sea
BOREAL ENVIRONMENT RESEARCH 7: 363 369 ISSN 1239-6095 Helsinki 23 December 2002 2002 DIAMIX an experimental study of diapycnal deepwater mixing in the virtually tideless Baltic Sea Anders Stigebrandt 1),
More informationLoss of Gaussianity in Oceanic Turbulent Flows with Internal Waves and Solitons
Loss of Gaussianity in Oceanic Turbulent Flows with Internal Waves and Solitons Peter C. Chu Naval Ocean Analysis and Prediction Laboratory, Naval Postgraduate School Monterey, California 93940 1 Abstract
More informationthe 2 past three decades
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE2840 Atlantic-induced 1 pan-tropical climate change over the 2 past three decades 3 4 5 6 7 8 9 10 POP simulation forced by the Atlantic-induced atmospheric
More informationDonald Slinn, Murray D. Levine
2 Donald Slinn, Murray D. Levine 2 Department of Civil and Coastal Engineering, University of Florida, Gainesville, Florida College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis,
More informationTracer transport and meridional overturn in the equatorial ocean
OFES workshops, February 2006 Tracer transport and meridional overturn in the equatorial ocean Akio Ishida with Yoshikazu Sasai, Yasuhiro Yamanaka, Hideharu Sasaki, and the OFES members Chlorofluorocarbon
More informationCompensation and Alignment of Thermohaline Gradients in the Ocean Mixed Layer
2214 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 33 Compensation and Alignment of Thermohaline Gradients in the Ocean Mixed Layer RAFFAELE FERRARI Massachusetts Institute of Technology, Cambridge, Massachusetts
More informationWestern North Pacific Integrated Physical-Biogeochemical Ocean Observation Experiment (INBOX)
Western North Pacific Integrated Physical-Biogeochemical Ocean Observation Experiment (INBOX) Toshio Suga (JAMSTEC/Tohoku Univ.) & the INBOX Group: S. Hosoda, R. Inoue, K. Sato, K. Shinya, T. Kobayashi,
More informationInfluence of forced near-inertial motion on the kinetic energy of a nearly-geostrophic flow
Abstract Influence of forced near-inertial motion on the kinetic energy of a nearly-geostrophic flow Stephanne Taylor and David Straub McGill University stephanne.taylor@mail.mcgill.ca The effect of forced
More informationChapter 6. Antarctic oceanography
Chapter 6 Antarctic oceanography The region of the world ocean bordering on Antarctica is unique in many respects. First of all, it is the only region where the flow of water can continue all around the
More information2 Observing the Ocean Ships Navigation The Electronics Era 16
Contents Preface xiii 1 Introduction 1 2 Observing the Ocean 4 2.1 Ships 5 2.2 Navigation 6 2.3 The Preelectronics Era 6 2.4 The Electronics Era 16 2.5 The Rise of Satellites 27 2.6 Intermediate- and Long-Duration
More informationProceedings of Meetings on Acoustics
Proceedings of Meetings on Acoustics Volume 19, 2013 http://acousticalsociety.org/ ICA 2013 Montreal Montreal, Canada 2-7 June 2013 Acoustical Oceanography Session 2aAO: Seismic Oceanography 2aAO8. Current-eddy
More informationThe California current is the eastern boundary current that lies to the west of
I. INTORDUCTION A. California Current System The California current is the eastern boundary current that lies to the west of North America. The California current flows from north, Washington, to south,
More informationWinds and Currents in the Oceans
Winds and Currents in the Oceans Atmospheric Processes Density of air is controlled by temperature, pressure, and moisture content. 1. Warm air is less dense than cold air and moist air is less dense than
More informationLecture 1. Amplitude of the seasonal cycle in temperature
Lecture 6 Lecture 1 Ocean circulation Forcing and large-scale features Amplitude of the seasonal cycle in temperature 1 Atmosphere and ocean heat transport Trenberth and Caron (2001) False-colour satellite
More informationGeneral Comment on Lab Reports: v. good + corresponds to a lab report that: has structure (Intro., Method, Results, Discussion, an Abstract would be
General Comment on Lab Reports: v. good + corresponds to a lab report that: has structure (Intro., Method, Results, Discussion, an Abstract would be a bonus) is well written (take your time to edit) shows
More informationThe role of the midlatitude ocean in sub-seasonal prediction
The role of the midlatitude ocean in sub-seasonal prediction R. Saravanan Xiaohui Ma, Xue Liu, J. Steinweg-Woods J. Kurian, R. Montuoro, P. Chang, I. Szunyogh Yinglai Jia, Ocean University of China J.
More informationHomework 5: Background Ocean Water Properties & Stratification
14 August 2008 MAR 110 HW5: Ocean Properties 1 Homework 5: Background Ocean Water Properties & Stratification The ocean is a heterogeneous mixture of water types - each with its own temperature, salinity,
More informationJ2.6 SONAR MEASUREMENTS IN THE GULF STREAM FRONT ON THE SOUTHEAST FLORIDA SHELF COORDINATED WITH TERRASAR-X SATELLITE OVERPASSES
J2.6 SONAR MEASUREMENTS IN THE GULF STREAM FRONT ON THE SOUTHEAST FLORIDA SHELF COORDINATED WITH TERRASAR-X SATELLITE OVERPASSES Chris Maingot 1, Alexander Soloviev 1, Silvia Matt 1, Mikhail Gilman 1,
More informationPhysical Oceanographic Context of Seamounts. Pierre Dutrieux Department of Oceanography, University of Hawai'i at Manoa, Honolulu, Hawai'i
Physical Oceanographic Context of Seamounts Pierre Dutrieux Department of Oceanography, University of Hawai'i at Manoa, Honolulu, Hawai'i PEW Workshop, October 2007 Seamounts: definitions submarine topographic
More informationStratification of the Ocean Boundary Surface Layer - year-long observations with gliders
Stratification of the Ocean Boundary Surface Layer - year-long observations with gliders Ayah Lazar 1,2 Andrew Thompson 2 Gillian Damerell 3 Karen Heywood 3 Christian Buckingham 4 Alberto Naveira Garabato
More informationCruise and Data Report: R/V Shana Rae operations in support of April 2015 AirSWOT campaign, April 17-20, 2015
Cruise and Data Report: R/V Shana Rae operations in support of April 2015 AirSWOT campaign, April 17-20, 2015 J. Thomas Farrar, Benjamin Hodges, Sebastien Bigorre Physical Oceanography Department Woods
More informationNational Oceanography Centre. Research & Consultancy Report No. 36
National Oceanography Centre Research & Consultancy Report No. 36 State of the eastern North Atlantic subpolar gyre: The Extended Ellett Line Programme Annual Report No. 1 N P Holliday 1, S Cunningham
More informationOn the horizontal variability of the upper ocean
On the horizontal variability of the upper ocean Daniel L. Rudnick Scripps Institution of Oceanography, La Jolla, California Abstract. The last decade has seen a tremendous increase in the number and quality
More informationisopycnal outcrop w < 0 (downwelling), v < 0 L.I. V. P.
Ocean 423 Vertical circulation 1 When we are thinking about how the density, temperature and salinity structure is set in the ocean, there are different processes at work depending on where in the water
More information3. Midlatitude Storm Tracks and the North Atlantic Oscillation
3. Midlatitude Storm Tracks and the North Atlantic Oscillation Copyright 2006 Emily Shuckburgh, University of Cambridge. Not to be quoted or reproduced without permission. EFS 3/1 Review of key results
More informationFigure 1: Two schematic views of the global overturning circulation. The Southern Ocean plays two key roles in the global overturning: (1) the
Figure 1: Two schematic views of the global overturning circulation. The Southern Ocean plays two key roles in the global overturning: (1) the Antarctic Circumpolar Current connects the ocean basins, establishing
More informationROSSBY WAVE PROPAGATION
ROSSBY WAVE PROPAGATION (PHH lecture 4) The presence of a gradient of PV (or q.-g. p.v.) allows slow wave motions generally called Rossby waves These waves arise through the Rossby restoration mechanism,
More informationThe Physical Context for Thin Layers in the Coastal Ocean
The Physical Context for Thin Layers in the Coastal Ocean David M. Fratantoni Physical Oceanography Department Woods Hole Oceanographic Institution Woods Hole, MA 02543 phone: (508) 289-2908 fax: (508)
More informationmeters, we can re-arrange this expression to give
Turbulence When the Reynolds number becomes sufficiently large, the non-linear term (u ) u in the momentum equation inevitably becomes comparable to other important terms and the flow becomes more complicated.
More information2. Measurements of suspended sediment concentrations from ADCP backscatter in strong currents
2. Measurements of suspended sediment concentrations from ADCP backscatter in strong currents Lucas M. Merckelbach 1 and H. Ridderinkhof 2 1 Helmholtz-Zentrum Geesthacht, D-21502 Germany, email: lucas.merckelbach@hzg.de
More informationCarbon pathways in the South Atlantic
Carbon pathways in the South Atlantic Olga T. Sato, Ph.D. Paulo Polito, Ph.D. olga.sato@usp.br - polito@usp.br Oceanographic Institute University of São Paulo Olga Sato and Paulo Polito (IOUSP) Carbon
More informationEarly Student Support for a Process Study of Oceanic Responses to Typhoons
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Early Student Support for a Process Study of Oceanic Responses to Typhoons Ren-Chieh Lien Applied Physics Laboratory University
More informationWater mass formation, subduction, and the oceanic heat budget
Chapter 5 Water mass formation, subduction, and the oceanic heat budget In the first four chapters we developed the concept of Ekman pumping, Rossby wave propagation, and the Sverdrup circulation as the
More informationSMS 303: Integrative Marine
SMS 303: Integrative Marine Sciences III Instructor: E. Boss, TA: A. Palacz emmanuel.boss@maine.edu, 581-4378 5 weeks & topics: diffusion, mixing, tides, Coriolis, and waves. Pre-class quiz. Mixing: What
More informationEddy-Mixed Layer Interactions in the Ocean
Eddy-Mixed Layer Interactions in the Ocean The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation As Published Publisher Ferrari,
More informationThe production and dissipation of compensated thermohaline variance by mesoscale stirring
The production and dissipation of compensated thermohaline variance by mesoscale stirring K. Shafer Smith Center for Atmosphere Ocean Science Courant Institute of Mathematical Sciences New York University
More informationObservation of Oceanic Structure around Tosa-Bae Southeast of Shikoku
Journal of Oceanography Vol. 50, pp. 543 to 558. 1994 Observation of Oceanic Structure around Tosa-Bae Southeast of Shikoku YOSHIHIKO SEKINE, HARUKI OHWAKI and MOTOYA NAKAGAWA Institute of Oceanography,
More informationField Observations of an Internal Ship Wake in the Saguenay Fjord
Field Observations of an Internal Ship Wake in the Saguenay Fjord Daniel Bourgault, Institut des sciences de la mer de Rimouski, Rimouski, Québec, Canada Peter Galbraith, Maurice Lamontagne Institute,
More informationJohn Steffen and Mark A. Bourassa
John Steffen and Mark A. Bourassa Funding by NASA Climate Data Records and NASA Ocean Vector Winds Science Team Florida State University Changes in surface winds due to SST gradients are poorly modeled
More informationGeostrophic Current Analysis through the CenCal Box
Geostrophic Current Analysis through the CenCal Box LT Sean P. Yemm OC357 Winter Quarter, 23 I. Introduction A. California Current System The California Current System is composed of numerous jets, filaments,
More informationBay of Bengal Surface and Thermocline and the Arabian Sea
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Bay of Bengal Surface and Thermocline and the Arabian Sea Arnold L. Gordon Lamont-Doherty Earth Observatory of Columbia
More informationPassive Scalars in Stratified Turbulence
GEOPHYSICAL RESEARCH LETTERS, VOL.???, XXXX, DOI:10.1029/, Passive Scalars in Stratified Turbulence G. Brethouwer Linné Flow Centre, KTH Mechanics, SE-100 44 Stockholm, Sweden E. Lindborg Linné Flow Centre,
More informationUsing Dye to Study Lateral Mixing in the Ocean: 100 m to 1 km
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Using Dye to Study Lateral Mixing in the Ocean: 100 m to 1 km Murray D. Levine Oregon State University College of Earth,
More informationThe World Ocean. Pacific Ocean 181 x 10 6 km 2. Indian Ocean 74 x 10 6 km 2. Atlantic Ocean 106 x 10 6 km 2
The World Ocean The ocean and adjacent seas cover 70.8% of the surface of Earth, an area of 361,254,000 km 2 Pacific Ocean 181 x 10 6 km 2 Indian Ocean 74 x 10 6 km 2 Atlantic Ocean 106 x 10 6 km 2 Oceanic
More informationEquatorial Deep Jets and Abyssal Mixing in the Indian Ocean
APRIL 2002 DENGLER AND QUADFASEL 1165 Equatorial Deep Jets and Abyssal Mixing in the Indian Ocean MARCUS DENGLER Institut für Meereskunde an der Universität Kiel, Kiel, Germany DETLEF QUADFASEL Niels Bohr
More informationParameterizing Eddy Heat Flux in a 1/10 Ocean. Simulation: A Wavenumber Perspective
Parameterizing Eddy Heat Flux in a 1/10 Ocean Simulation: A Wavenumber Perspective Alexa Griesel Sarah T. Gille Janet Sprintall Julie L. McClean Scripps Institution of Oceanography, La Jolla Mathew E.
More informationROLES OF THE OCEAN MESOSCALE IN THE LATERAL SUPPLY OF MASS, HEAT, CARBON AND NUTRIENTS TO THE NORTHERN HEMISPHERE SUBTROPICAL GYRE
ROLES OF THE OCEAN MESOSCALE IN THE LATERAL SUPPLY OF MASS, HEAT, CARBON AND NUTRIENTS TO THE NORTHERN HEMISPHERE SUBTROPICAL GYRE AYAKO YAMAMOTO 1*, JAIME B. PALTER 1,2, CAROLINA O. DUFOUR 1,3, STEPHEN
More informationLagrangian Statistics in Nonhydrostatic and QG turbulence Baylor Fox-Kemper (Brown)
Lagrangian Statistics in Nonhydrostatic and QG turbulence Baylor Fox-Kemper (Brown) LAPCOD, Schoodic Pt., ME 7/28/15 Sponsor: GoMRI/CARTHE P. E. Hamlington, L. P. Van Roekel, BFK, K. Julien, and G. P.
More informationSAMPLE CHAPTERS UNESCO EOLSS WAVES IN THE OCEANS. Wolfgang Fennel Institut für Ostseeforschung Warnemünde (IOW) an der Universität Rostock,Germany
WAVES IN THE OCEANS Wolfgang Fennel Institut für Ostseeforschung Warnemünde (IOW) an der Universität Rostock,Germany Keywords: Wind waves, dispersion, internal waves, inertial oscillations, inertial waves,
More informationAnalysis of Subsurface Velocity Data from the Arctic Ocean
Analysis of Subsurface Velocity Data from the Arctic Ocean Albert J. Plueddemann 202A Clark Lab, MS-29 Woods Hole Oceanographic Institution Woods Hole, MA 02541-1541 ph: (508) 289-2789, fax: (508) 457-2163
More informationA multi-proxy study of planktonic foraminifera to identify past millennialscale. climate variability in the East Asian Monsoon and the Western Pacific
This pdf file consists of all pages containing figures within: A multi-proxy study of planktonic foraminifera to identify past millennialscale climate variability in the East Asian Monsoon and the Western
More information5. Two-layer Flows in Rotating Channels.
5. Two-layer Flows in Rotating Channels. The exchange flow between a marginal sea or estuary and the open ocean is often approximated using two-layer stratification. Two-layer models are most valid when
More informationHow to form halocline water?
How to form halocline water? Atlantic water - cannot form Halocline water simply by mixing (Aagaard, 1981) Surface Water Adapted from Steele and Boyd, 1998 ADVECTIVE HC Temp Fresh Salty Aagaard et al,
More informationLecture 20 ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY
ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY Lecture 20 Learning objectives: should be able to apply mixed layer temperature equation to explain observations; understand buoyancy forcing & salinity
More informationObservation and dynamics of baroclinic eddies southeast of Okinawa Island
Observation and dynamics of baroclinic eddies southeast of Okinawa Island Xiao-Hua Zhu 1, Jea-Hun Park 2 and Daji Huang 1 1 Second Institute of Oceanography, State Oceanic Administration, China 2 Graduate
More informationBefore we consider two canonical turbulent flows we need a general description of turbulence.
Chapter 2 Canonical Turbulent Flows Before we consider two canonical turbulent flows we need a general description of turbulence. 2.1 A Brief Introduction to Turbulence One way of looking at turbulent
More informationAssessment of the performance of a turbulence closure model: along the tidally-influenced Kaipara River to the estuary, NZ
Assessment of the performance of a turbulence closure model: along the tidally-influenced Kaipara River to the estuary, NZ Berengere S. Dejeans 1, Julia C. Mullarney 2, Iain T. MacDonald 3 and Glen M.
More informationUsing a Broadband ADCP in a Tidal Channel. Part II: Turbulence
1568 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 16 Using a Broadband ADCP in a Tidal Channel. Part II: Turbulence YOUYU LU* AND ROLF G. LUECK School of Earth and Ocean Sciences, University of
More informationFor example, for values of A x = 0 m /s, f 0 s, and L = 0 km, then E h = 0. and the motion may be influenced by horizontal friction if Corioli
Lecture. Equations of Motion Scaling, Non-dimensional Numbers, Stability and Mixing We have learned how to express the forces per unit mass that cause acceleration in the ocean, except for the tidal forces
More information