1 edition of A Numerical Study of the Forcing Mechanisms of the Leeuwin Current System found in the catalog.
A Numerical Study of the Forcing Mechanisms of the Leeuwin Current System
2002 by Storming Media .
Written in English
|The Physical Object|
The Leeuwin current, the intensity of which depends on the Southern Oscillation Index, and westerly winds are the main causes of variation in the level of settlement of rock lobster pueruli off Western Australia, and are therefore indirectly responsible for variations in lobster catches (Pearce & Phillips, ; Caputi & Brown, ).Cited by: 5. The Leeuwin Current is one of the greatest biogeographic influences on Western Australia's marine environments, bringing a flow of tropical water down the coast. The current is strongest and closest to the coast during autumn and winter, in the absence of opposing southerly winds and the associated nearshore northward flowing Cape and Ningaloo. Dynamics of the Leeuwin Current, and an observational reconstruction of the Leeuwin Current System. 2pm-3pm, Thursday, March 3. Red Centre RC, University of NSW. Ryo Furue, (University of Hawaii) CCRC Atlantic meridional overturning circulation and Southern Ocean. 2pm-3pm, Wednesday, March 2. Jon Petch (UK Met Office) CAWCR. online version of the program book. Please click the following link to download and install: When you are finished installing, please return to this window and PRESS.
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A numerical study of the eddying characteristics of the Leeuwin Current System Article in Deep Sea Research Part I Oceanographic Research Papers 55(3) March with 15 Reads. Numerical modelling of the mean flow characteristics of the Leeuwin Current System Article in Deep Sea Research Part II Topical Studies in Oceanography 54().
A numerical study of the mesoscale eddy dynamics of the Leeuwin current system Ailbhe Travers () The morphology and dynamics of low-energy, sheltered, sandy beaches (joint supervision with Dr I Eliot) Emma Gale () The hydrodynamics of intermittently closing and opening lakes and lagoons (joint supervision with Dr D Hamilton and Dr R.
In International Geophysics, Most ocean modeling, whether global or regional, is done with atmospheric forcing assumed to be known a priori and hence prescribable independently. For hindcasts (simulations of past events, for which atmospheric data are available), certain process studies, and climatological type simulations, this does not prove to.
Published Papers. Hamilton, K., At the dawn of global climate modeling: The strange case of the Leith Atmosphere Model. Hist. Geo- Space Sci., 11, 1.
Introduction. The dominant ocean current along Western Australia (WA) is the Leeuwin Current (LC) (Godfrey and Ridgway,Smith et al., ), a warm poleward flow of tropical other eastern boundary currents (e.g., the Benguela and Humboldt Currents at similar latitudes), the poleward flow of the LC suppresses the persistent upwelling of cool, Cited by: This reference work is available as a limited print edition and online via ScienceDirect.
The online version of this reference work provides the breadth and depth of content Elsevier is known for and also offers a great deal more when it comes to flexibility. Leeuwin Current Water (LCW) and Sub-Tropical Surface Water (STSW) were distinguished and a prominent front at ∼30°S characterized by strong eastward flow separated them.
Although zooplankton abundance increased towards the north, the prey field was unevenly distributed with patches of higher prey concentration associated mainly with by: We study the development and evolution of buoyant river plumes on the continental shelf.
Our calculations are based on three‐dimensional numerical simulations, where the river runoff is introduced as a volume of zero salinity water in the continuity equation and mixing is provided by the model's turbulence closure scheme and wind forcing.
Paleoceanographic (paleocean) modeling is the application of analytic or numerical techniques to predict and understand the ocean’s past circulation, biogeochemical interactions, and climate. Paleocean modeling is primarily a tool for exploring the mechanistic functioning of the ocean and for making concrete predictions testable against.
Forcing Mechanisms Predictive capability is usually premised on the identification and understanding of the mechanisms that couple response to forcing. The preceding section has illustrated that the coastal ocean is subjected to forcing over a broad range of periods, ranging from interannual variations in the coupled ocean-atmosphere system.
As an initial phase of this project we have taken the southeast region of the Australian seabed as our study area. The seabed responses to current climate and possible future climatic conditions over the next 50 yr have been simulated for the first time by a state-of-the-art numerical.
Lin, and S.-P. Xie, Tropical cyclone-induced ocean response: A comparative study of the South China Sea and tropical Northwest Pacific Ocean.
Climate, 28, The oceans cover 70% of the Earth's surface, and are critical components of Earth's climate system. This new edition of Encyclopedia of Ocean Sciences summarizes the breadth of knowledge about them, providing revised, up to date entries as well coverage of.
Unfortunately, this book can't be printed from the OpenBook. If you need to print pages from this book, we recommend downloading it as a PDF.
Visit to get more information about this book, to buy it in print, or to download it as a free PDF. Abstract. This chapter deals mostly with the dynamics of discrete vortices in a two-layer fluid and has the following structure.
First, two vortices (a simplest heton) are used to demonstrate the characteristic features of a system of baroclinic vortices, after which, the results of analytical and numerical studying of vortex ensembles are studied, starting from relatively Cited by: 2. In this study we present a multiproxy data set spanning the Early to Late Pliocene (~ to Ma) from International Ocean Discovery Program (IODP) Expedition Site U (Gallagher et al., ), situated on the Australian northwest shelf (NWS) within the path of the Leeuwin Current (LC), and directly influenced by the ITF (D'Adamo et Cited by: 5.
Furue R, Guerreiro K, Phillips HE, McCreary Jr JP, Bindoff NL, 'On the Leeuwin Current System and its linkage to zonal flows in the South Indian Ocean as inferred from a gridded hydrography', Journal of Physical Oceanography, 47 pp.
ISSN () [Refereed Article] DOI: /JPO-D The oceans cover 70% of the Earth’s surface, and are critical components of Earth’s climate system. This new edition of Encyclopedia of Ocean Sciences summarizes the breadth of knowledge about them, providing revised, up to date entries as well coverage of new topics in the field.
New and expanded sections include microbial ecology, high latitude systems and the. The LC is a poleward eastern boundary current driven by an alongshore pressure gradient, generated through the transport of warmer, lower salinity water into the tropical Indian Ocean by the Indonesian Throughflow [9,10,11].It is augmented with contributions from the central South Indian Counter Current (SICC) and the Holloway Current in the shelf region around 20°–23° S.
The tidal current was quite strong in the study area. The current speeds ranged from to m/s during the spring tide, which increased landward and had the spatial pattern with stronger.
Effect of salinity on density in the Leeuwin Current System. JGR,A numerical investigation of the annual variability in the Gulf of California. JPO, Leeuwin Current observations on the Australian North West Shelf, May-June DSR, This constitutes the first quantitative assessment of Leeuwin Current pathways within an offline, year integration time, eddy-resolving global ocean model simulation.
Along the Leeuwin Current's pathway we find a mean poleward transport of Sv in which the tropical sources account for % of the transport. An extensive survey of the Leeuwin Current system collected plankton samples using µm nets (down to m depth) over shelf ( m), Leeuwin Current ( m) and oceanic ( m) stations from 22°S to 34°S.
Sampling was conducted in May to coincide with peak Leeuwin Current flow and biological activity. We found that the thermal forcing of the Tropical Indian Ocean and Tropical Western Pacific warming are the underlie mechanisms, which were both verified by numerical sensitivity experiments.
Especially, we found the Northern Australia was cooling in contrast to the rapid warming climate, which is an example of independence of the regional. Ezer T. Thattai B. Kjerfve and W. Heyman On the variability of the flow along the Meso-American Barrier Reef System: A numerical model study of the influence of the Caribbean Current and eddies Ocean Dynamics 55 doi:.
You can write a book review and share your experiences. Other readers will always be interested in your opinion of the books you've read.
Whether you've loved the book or not, if you give your honest and detailed thoughts then people will find new books that are right for them., Free ebooks since Thermohaline circulation (THC) is a part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes.
The adjective thermohaline derives from thermo-referring to temperature and -haline referring to salt content, factors which together determine the density of sea water.
Wind-driven surface currents (such. A Numerical Study of the Effects of Wind Forcing on the Chile Current System.
Journal of Oceanography, 51(5), BATTEEN, M.L., RUTHERFORD, M.J., AND BAYLER, E.J. A numerical study of wind- and thermal-forcing efects on the ocean circulation off western Australia.
Journal of Physical Oceanography, 22(12), Roughan MM; Oke PR; Middleton JH,'A modeling study of the climatological current field and thetrajectories of upwelled particles in the East Australian Current', Journal of Physical Oceanography, vol. 33, pp. - Abstract Variability of the Leeuwin current (LC) off Western Australia is a footprint of interannual and decadal climate variations in the tropical Indo-Pacific.
La Niña events often result in a strengthened LC, high coastal sea levels and unusually warm sea surface temperatures (SSTs), termed Ningaloo Niño. The problem is sufficiently complex that analytic or numerical approaches are necessary to estimate current hazards and explore potential future changes.
n this study. Chris Bull interview for AMSI Winter School in future projections of Australia’s coastal regions depend critically on our understanding of the dynamics of the Leeuwin Current and East Australian Current.
My PhD aims to improve our understanding of the circulation, variability and dynamics of the Leeuwin Current and East Australian. Leeuwin Current Activity Controls Benthic Foraminifera on the Carnarvon Ramp, Western Australia: From Inception to Flow Optimum.
Christian Haller, Pamela Hallock, Albert C. Hine, Christopher G. Smith. Quantifying Depositional Architecture of Basin-Floor Fan Pinchouts: Implications for Improved Stratigraphic Trap Prediction.
Our current study has focused on the mean field and primarily the circulation in the Southern Hemisphere of the Indian Ocean. The circulation in the north Indian Ocean undergoes significant seasonal variations with reversing ocean currents due to strong monsoon wind forcing (Schott et al.
Hence, a different strategy is needed for Cited by: 2. Ocean boundary current systems are key components of the climate system, are home to highly productive ecosystems, and have numerous societal impacts.
Establishment of a global network of boundary current observing systems is a critical part of ongoing development of the Global Ocean Observing System. The characteristics of boundary current systems are reviewed, Cited by: 8.
Contrasting local retention and cross-shore transports of the East Australian Current and the Leeuwin Current and their relative influences on the life histories of small pelagic fishes. Deep-Sea Research Part II: Topical Studies in Oceanography Kamenkovich, A. Hogg, and J.
Peters, On the mechanisms of late 20th century sea-surface temperature trends over the Antarctic Circumpolar Current. Geophys. This study focuses on the improved estimation of mesoscale surface ocean circulation obtained by merging TOPEX/Poseidon (T/P) and ERS‐1 and ‐2 altimeter measurements between OCited by: Estimating the Velocity and Transport of Western Boundary Current Systems: A Case Study of the East Australian Current near Brisbane.
Journal of Atmospheric and Oceanic Technology, 35(6),doi: /JTECH-D. A4D-Var analysis system for theCalifornia Current: A prototype for an operational regional ocean data assimilation system. In L. Xu & S. Park (Eds.), Data assimilation for atmospheric, oceanic.Böning, C.
W., Eden, C., Latif, M., Stramma, L., Brandt, P., Fischer, J., Oschlies, A. and Visbeck, M. () Nordatlantik I - Die Bedeutung des.Submission Title: Exploring Ocean Indicators: Coordinating Efforts to Better Study, Monitor, and Predict Ocean States, Changes, and Processes, Submission Title: Essential Ocean Variables: a Common Focus for Sustained Global Ocean Observing, Submission Title: Investigating the Effect of Ocean Currents on the Surface Stress and Heat Fluxes over .