The Structure of Water Mass, Salt, and Temperature Transports Within Intermediate Depths of the Western Tropical Atlantic Ocean
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Chapter 8 the Pacific Ocean After These Two Lengthy Excursions Into
Chapter 8 The Pacific Ocean After these two lengthy excursions into polar oceanography we are now ready to test our understanding of ocean dynamics by looking at one of the three major ocean basins. The Pacific Ocean is not everyone's first choice for such an undertaking, mainly because the traditional industrialized nations border the Atlantic Ocean; and as science always follows economics and politics (Tomczak, 1980), the Atlantic Ocean has been investigated in far more detail than any other. However, if we want to take the summary of ocean dynamics and water mass structure developed in our first five chapters as a starting point, the Pacific Ocean is a much more logical candidate, since it comes closest to our hypothetical ocean which formed the basis of Figures 3.1 and 5.5. We therefore accept the lack of observational knowledge, particularly in the South Pacific Ocean, and see how our ideas of ocean dynamics can help us in interpreting what we know. Bottom topography The Pacific Ocean is the largest of all oceans. In the tropics it spans a zonal distance of 20,000 km from Malacca Strait to Panama. Its meridional extent between Bering Strait and Antarctica is over 15,000 km. With all its adjacent seas it covers an area of 178.106 km2 and represents 40% of the surface area of the world ocean, equivalent to the area of all continents. Without its Southern Ocean part the Pacific Ocean still covers 147.106 km2, about twice the area of the Indian Ocean. Fig. 8.1. The inter-oceanic ridge system of the world ocean (heavy line) and major secondary ridges. -
Ocean Circulation and Climate: a 21St Century Perspective
Chapter 13 Western Boundary Currents Shiro Imawaki*, Amy S. Bower{, Lisa Beal{ and Bo Qiu} *Japan Agency for Marine–Earth Science and Technology, Yokohama, Japan {Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA {Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, USA }School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, Hawaii, USA Chapter Outline 1. General Features 305 4.1.3. Velocity and Transport 317 1.1. Introduction 305 4.1.4. Separation from the Western Boundary 317 1.2. Wind-Driven and Thermohaline Circulations 306 4.1.5. WBC Extension 319 1.3. Transport 306 4.1.6. Air–Sea Interaction and Implications 1.4. Variability 306 for Climate 319 1.5. Structure of WBCs 306 4.2. Agulhas Current 320 1.6. Air–Sea Fluxes 308 4.2.1. Introduction 320 1.7. Observations 309 4.2.2. Origins and Source Waters 320 1.8. WBCs of Individual Ocean Basins 309 4.2.3. Velocity and Vorticity Structure 320 2. North Atlantic 309 4.2.4. Separation, Retroflection, and Leakage 322 2.1. Introduction 309 4.2.5. WBC Extension 322 2.2. Florida Current 310 4.2.6. Air–Sea Interaction 323 2.3. Gulf Stream Separation 311 4.2.7. Implications for Climate 323 2.4. Gulf Stream Extension 311 5. North Pacific 323 2.5. Air–Sea Interaction 313 5.1. Upstream Kuroshio 323 2.6. North Atlantic Current 314 5.2. Kuroshio South of Japan 325 3. South Atlantic 315 5.3. Kuroshio Extension 325 3.1. -
Variability of the Southern Antarctic Circumpolar Current Front North of South Georgia
Journal of Marine Systems 37 (2002) 87–105 www.elsevier.com/locate/jmarsys Variability of the southern Antarctic Circumpolar Current front north of South Georgia Sally E. Thorpe a,b,*, Karen J. Heywood a, Mark A. Brandon b,1, David P. Stevens c aSchool of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK bBritish Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK cSchool of Mathematics, University of East Anglia, Norwich NR4 7TJ, UK Received 14 December 2000; received in revised form 15 November 2001; accepted 19 March 2002 Abstract South Georgia ( f 54jS, 37jW) is an island in the eastern Scotia Sea, South Atlantic that lies in the path of the Antarctic Circumpolar Current (ACC). The southern ACC front (SACCF), one of three major fronts associated with the ACC, wraps anticyclonically around South Georgia and then retroflects north of the island. This paper investigates temporal variability in the position of the SACCF north of South Georgia that is likely to have an effect on the South Georgia ecosystem by contributing to the variability in local krill abundance. A meridional hydrographic section that crossed the SACCF three times demonstrates that the SACCF is associated with a geopotential anomaly of 4.5 J kg À 1 in the eastern Scotia Sea. A high resolution (1/4j  1/4j) map of historical geopotential anomaly shows the mean position of the SACCF retroflection north of South Georgia to be at 36jW, 400 km further east than in previous work. It also reveals temporal variability associated with the SACCF in the South Georgia region. -
Downloaded 09/25/21 10:39 PM UTC 1028 JOURNAL of PHYSICAL OCEANOGRAPHY VOLUME 33
MAY 2003 SLOYAN ET AL. 1027 The Paci®c Cold Tongue: A Pathway for Interhemispheric Exchange* BERNADETTE M. SLOYAN,1 GREGORY C. JOHNSON, AND WILLIAM S. KESSLER NOAA/Paci®c Marine Environmental Laboratory, Seattle, Washington (Manuscript received 29 January 2002, in ®nal form 28 October 2002) ABSTRACT Mean meridional upper-ocean temperature, salinity, and zonal velocity sections across the Paci®c Ocean between 88S and 88N are combined with other oceanographic and air±sea ¯ux data in an inverse model. The tropical Paci®c Ocean can be divided into three regions with distinct circulation patterns: western (1438E± 1708W), central (1708±1258W), and eastern (1258W±eastern boundary). In the central and eastern Paci®c the downward limbs of the shallow tropical cells are 15(613) 3 106 m3 s 21 in the north and 20(611) 3 106 m3 s21 in the south. The Paci®c cold tongue in the eastern region results from diapycnal upwelling through all layers of the Equatorial Undercurrent, which preferentially exhausts the lightest (warmer) layers of the Equatorial Undercurrent [10(66) 3 106 m3 s21] between 1258 and 958W, allowing the denser (cooler) layers to upwell [9(64) 3 106 m3 s21] east of 958W and adjacent to the American coast. An interhemispheric exchange of 13(613) 3 106 m3 s 21 between the southern and northern Paci®c Ocean forms the Paci®c branch of the Paci®c± Indian interbasin exchange. Southern Hemisphere water enters the tropical Paci®c Ocean via the direct route at the western boundary and via an interior (basin) pathway. However, this water moves irreversibly into the North Paci®c by upwelling in the eastern equatorial Paci®c and air±sea transformation that drives poleward interior transport across 28N. -
Equatorial Ocean Currents
i KNAUSSTRIBUTE An Observer's View of the Equatorial Ocean Currents Robert H. Weisbeq~ University qf South Florida • St. Petersbm X, Florida USA Introduction The equator is a curious place. Despite high solar eastward surface current that flows halfway around the radiation that is relatively steady year-round, oceanog- Earth counter to the prevailing winds. raphers know to pack a sweater when sailing there. Curiosity notwithstanding, we study these equatori- Compared with the 28°C surface temperatures of the al ocean circulation features because they are adjacent tropical waters, the eastern halves of the equa- fundamental to the Earth's climate system and its vari- torial Pacific or Atlantic Oceans have surface ations. For instance, the equatorial cold tongue in the temperatures up to 10°C colder, particularly in boreal Atlantic (a band of relatively cold water centered on the summer months. The currents are equally odd. equator), itself a circulation induced feature, accounts Prevailing easterly winds over most of the tropical for a factor of about 1.5 increase in heat flux from the Pacific and Atlantic Oceans suggest westward flowing southern hemisphere to the northern hemisphere. In the currents. Yet, eastward currents oftentimes outweigh Pacific, the inter-annual variations in the cold tongue those flowing toward the west. Motivation for the first temperature are the ocean's part of the E1 Nifio- quantitative theory of the large scale, wind driven Southern Oscillation (ENSO) which affects climate and ocean circulation, in fact, came -
Institute of 0 Oceanographic Sciences ^ Deacon Laboratory
Fee Institute of 0 Oceanographic Sciences ^ Deacon Laboratory INTERNAL DOCUMENT No. 327 Parameterization versus resolution: a review P D Killworth, K D5ds & S R Thompson 1994 Natural Environment Research Council c 0 C" r INSTITUTE OF OCEANOGRAPHIC SCIENCES DEACON LABORATORY INTERNAL DOCUMENT No. 327 Parameterization versus resolution: a review P D Killworth, K Dods & S R Thompson 1994 ' • • Wormley Godalming Surrey GU8 SUB UK . \ Tel +44-(0)428 684141 v. Telex 858833 OCEANS G # Telefax +44-{0)428 683066 DOCUMENT DATA SHEET DjSTE KILLWORIH, P D, DOOS, K & THOMPSON, S R 1994 7771^ Parameterization versus resolution: a review. ^(EFERENCE Institute of OceanograpMc Sciences Deacon Laboratory, Internal Document, No. 327, 43pp. (Unpublished manuscript) ABSTRACT This review outlines our current knowledge of the effects of resolution on ocean general circulation models used for climate studies. Comparisons are made between the marginally eddy-resolving models currently in use. Poleward heat flux is the quantity which it is most vital to obtain accurately in order that coupled atmosphere-ocean models will function correctly. This quantity has consistent values over a wide range of resolutions, although its longitudinal distribution may vary. Other quantities, such as eddy energy, depend heavily on resolution and only show signs of asymptoting to some 'correct' value for extremely fine resolution. Grid resolution should be balanced between the horizontal and vertical, in the sense that the parameter Nh/E, should be of order unity, where N is the buoyancy frequency, f the Coriolis parameter, and h and L are the vertical and horizontal spacings respectively. A simple numerical representation of the Eady problem shows that erroneous instabilities can occur if this quantity differs noticeably from unity. -
Why Are There Agulhas Rings?
APRIL 1999 PICHEVIN ET AL. 693 Why Are There Agulhas Rings? THIERRY PICHEVIN SHOM/CMO, Brest, France DORON NOF Department of Oceanography and the Geophysical Fluid Dynamics Institute, The Florida State University, Tallahassee, Florida JOHANN LUTJEHARMS Department of Oceanography, University of Cape Town, Rondebosch, South Africa (Manuscript received 31 March 1997, in ®nal form 7 May 1998) ABSTRACT The recently proposed analytical theory of Nof and Pichevin describing the intimate relationship between retro¯ecting currents and the production of rings is examined numerically and applied to the Agulhas Current. Using a reduced-gravity 1½-layer primitive equation model of the Bleck and Boudra type the authors show that, as the theory suggests, the generation of rings from a retro¯ecting current is inevitable. The generation of rings is not due to an instability associated with the breakdown of a known steady solution but rather is due to the zonal momentum ¯ux (i.e., ¯ow force) of the Agulhas jet that curves back on itself. Numerical experiments demonstrate that, to compensate for this ¯ow force, several rings are produced each year. Since the slowly drifting rings need to balance the entire ¯ow force of the retro¯ecting jet, their length scale is considerably larger than the Rossby radius; that is, their scale is greater than that of their classical counterparts produced by instability. Recent observations suggest a correlation between the so-called ``Natal Pulse'' and the production of Agulhas rings. As a by-product of the more general retro¯ection experiments, the pulse issue is also examined numerically using two different representations for the pulses. -
Upper-Level Circulation in the South Atlantic Ocean
Prog. Oceanog. Vol. 26, pp. 1-73, 1991. 0079 - 6611/91 $0.00 + .50 Printed in Great Britain. All fights reserved. © 1991 Pergamon Press pie Upper-level circulation in the South Atlantic Ocean RAY G. P~-rwtSON and LOTHAR Sa~AMMA lnstitut fiir Meereskunde an der Universitiit Kiel, Diisternbrooker Weg 20, 2300 Kiel 1, F.R.G. Abstract - In this paper we present a literature survey of the South Atlantic's climate and its oceanic upper-layer circulation and meridional beat transport. The opening section deals with climate and is focused upon those elements having greatest oceanic relevance, i.e., distributions of atmospheric sea level pressure, the wind fields they produce, and the net surface energy fluxes. The various geostrophic currents comprising the upper-level general circulation are then reviewed in a manner organized around the subtropical gyre, beginning off southern Africa with the Agulhas Current Retroflection and then progressing to the Benguela Current, the equatorial current system and circulation in the Angola Basin, the large-scale variability and interannual warmings at low latitudes, the Brazil Current, the South Atlantic Cmrent, and finally to the Antarctic Circumpolar Current system in which the Falkland (Malvinas) Current is included. A summary of estimates of the meridional heat transport at various latitudes in the South Atlantic ends the survey. CONTENTS 1. Introduction 2 2. Climatic Elements 2 3. Subtropical and Equatorial Circulation 11 3.1. Agulhas Current Retroflection 11 3.2. Benguela Cmrent 16 3.3. Equatorial Cttrrents 18 3.3.1. Components of the system 18 3.3.2. Angola Basin circulation 26 3.3.3. -
Pliocene Stratigraphy and the Impact of Panama Uplift on Changes in Caribbean and Tropical East Pacific Upper Ocean Stratification (6 – 2.5 Ma)
PLIOCENE STRATIGRAPHY AND THE IMPACT OF PANAMA UPLIFT ON CHANGES IN CARIBBEAN AND TROPICAL EAST PACIFIC UPPER OCEAN STRATIFICATION (6 – 2.5 MA) PLIOZÄNE STRATIGRAPHIE UND DER EINFLUSS DES PANAMA-SEEWEGES AUF DIE STRATIFIZIERUNG DER OBERFLÄCHEN-WASSERMASSEN IN DER KARIBIK UND IM TROPISCHEN OST-PAZIFIK (6 – 2.5 MA) Kumulative Dissertation zur Erlangung des Doktorgrades der Mathematisch-Naturwissenschaftlichen Fakultät der Christian-Albrechts-Universität zu Kiel vorgelegt von Silke Steph Kiel, 2005 PLIOCENE STRATIGRAPHY AND THE IMPACT OF PANAMA UPLIFT ON CHANGES IN CARIBBEAN AND TROPICAL EAST PACIFIC UPPER OCEAN STRATIFICATION (6 – 2.5 MA) PLIOZÄNE STRATIGRAPHIE UND DER EINFLUSS DES PANAMA-SEEWEGES AUF DIE STRATIFIZIERUNG DER OBERFLÄCHEN-WASSERMASSEN IN DER KARIBIK UND IM TROPISCHEN OST-PAZIFIK (6 – 2.5 MA) Kumulative Dissertation zur Erlangung des Doktorgrades der Mathematisch-Naturwissenschaftlichen Fakultät der Christian-Albrechts-Universität zu Kiel vorgelegt von Silke Steph Kiel, 2005 158 pages 52 figures 10 tables 8 appendices Referent: ________________________________________ Koreferent: ________________________________________ Tag der Disputation: ________________________________________ Zum Druck genehmigt, Kiel, den: ________________________________________ Der Dekan: ________________________________________ I ABSTRACT This thesis examines the closure history of the Central American Seaway (CAS) and its effect on changes in ocean circulation and climate during the time interval from ~6 – 2.5 Ma. It was accomplished within the DFG Research Unit "Impact of Gateways on Ocean Circulation, Climate and Evolution" at the University of Kiel. Proxy records from Ocean Drilling Program (ODP) Sites 999 and 1000 (Caribbean), and from ODP Sites 1237, 1239 and 1241 (low-latitude east Pacific) are developed and examined. In addition, previously established proxy data from Atlantic Sites 925/926 (Ceara Rise) and 1006 (western Great Bahama Bank) and from two east Pacific sites (851, 1236) are included for interpretations. -
36- 5. Rotating Flow the General Circulation of the Ocean
-36- 5. Rotating Flow The general circulation of the ocean (and atmosphere) differs markedly from the flows we typically observe around us and from the solutions that we have discussed so far, because large scale geophysical flows are: (1) dominated by the effects of rotation and (2) are almost inviscid. In this chapter I will introduce a technique to help us decide what terms in the Navier-Stokes equations are important in a given situation, present additional basic concepts and finally apply all that we have learned to the problem of the surface circulation of the oceans. 5.1. Non-dimensionalization In the last chapter, we saw how approximate analyses of partial differential equa- tions can provide insight into the behavior of the solution. Scaling the equations with typ- ical values of the variables also has other uses, most of which begin with the basic con- cept of non-dimensionalization. But before I discuss non-dimensionalization, I want to first consider the effect of variable density on the Navier-Stokes equation. Let → + ρ → ρ + ρ p pH pˆ (z) ˆ ρ where pH and (z) satisfy the hydrostatic equation ∇ =−ρ pH (z)gzˆ If we subtract this equation from the Navier-Stokes equation Du (ρ(z) + ρˆ) =−∇(p + pˆ) − (ρ(z) + ρˆ)gzˆ + µ∇2u Dt H and divide by ρ(z) + ρˆ we obtain Du 1 ρˆ =− ∇pˆ − gzˆ + ν∇2u Dt ρ + ρˆ ρ + ρˆ Note that gravity enters only to the extent that the density deviates from the hydrostatic 1 1 − ρˆ situation. In must cases,ρ ˆ << ρ(z) and = . -
Variability of the South Atlantic Upper Ocean Circulation: a Data
Variability of the South Atlantic upper ocean circulation: a data assimilation experiment with 5 years of Topex/Poseidon altimeter observations Elodie Garnier, Jacques Verron, Bernard Barnier To cite this version: Elodie Garnier, Jacques Verron, Bernard Barnier. Variability of the South Atlantic upper ocean circulation: a data assimilation experiment with 5 years of Topex/Poseidon altimeter observa- tions. International Journal of Remote Sensing, Taylor & Francis, 2003, 24 (5), pp.911-934. 10.1080/01431160210154902. hal-00182964 HAL Id: hal-00182964 https://hal.archives-ouvertes.fr/hal-00182964 Submitted on 13 Jan 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License Variability of the South Atlantic upper ocean circulation: a data assimilation experiment with 5 years of TOPEX/POSEIDON altimeter observations E. GARNIER, J. VERRON and B. BARNIER LEGI, UMR 5519 CNRS, BP 53X, 38041 Grenoble Cedex, France / Abstract. Dynamical interpolation of five years of TOPEX POSEIDON alti-meter data (October 1992–September 1997) is performed in the South Atlantic basin, through the use of a simple quasigeostrophic model and a simple nudging data assimilation technique. The resulting data set is analysed in order to evidence the role of mesoscale eddies on the interannual variability of the South Atlantic ocean circulations. -
Lagrangian Views of the Pathways of the Atlantic Meridional Overturning
REVIE W ARTICLE Lagra ngia n Vie ws of t he Pat h ways of t he Atla ntic 10.1029/2019J C015014 Meridio nal Overt ur ni ng Circ ulatio n S pecial Sectio n: A. Bo wer 1 , S. L ozier 2, 3 , A. Biastoc h 4 , K. Dro ui n 2 , N. Fo u kal 1 , H. F urey 1 , Atla ntic Meridio nal 5 6 2, 7 Overt ur ni ng Circ ulatio n: M. La n k horst , S. R ü hs , a n d S. Zo u Revie ws of Observational and 1 2 Modeling Advances Woods Hole, Oceanographic Institution, Woods Hole, M A, US A, Depart ment of Earth and Ocean Sciences, Duke University, Durha m, N C, US A, 3 No w at Depart ment of Earth and At mospheric Sciences, Georgia Institute of Technology, Atla nta, G A, US A, 4 G E O M A R Hel mholtz Centre for Ocean Research Kiel, Kiel, Ger many, 5 Scri p ps I nstit utio n of Key Poi nts: Ocea nograp hy, U niversity of Califor nia Sa n Diego, La Jolla, C A, US A, 6 Ocea n Fro ntier I nstit ute Dal ho usie U niversity, • Lagra ngia n met hods are critical to Halifax, Nova Scotia, Ca nada, 7 No w at Depart ment of Physical Oceanography, Woods Hole Oceanographic Institution, describi ng t he t hree ‐di m e nsi o n al str uct ure of t he Atla ntic Meridio nal Woods Hole, M A, US A Overt ur ni ng Circ ulatio n • Fl ui d parcel trajectories reveal t he lack of meridio nal co n nectivity i n A bstract The Lagrangian method — w here c urre nt locatio n a nd i ntensity are deter mi ned by tracki ng t he bot h t he s hallo w a nd deep li mbs of move ment of fl o w alo ng its pat h — is t he oldest tec h niq ue for measuri ng t he ocea n circ ulatio n.