Log in

Relevant bibliographies by topics / Upwelling and innershelf circulation

Contents

Journal articles
Dissertations / Theses
Books
Book chapters
Conference papers

Academic literature on the topic 'Upwelling and innershelf circulation'

Author: Grafiati

Published: 4 June 2021

Last updated: 6 February 2022

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Upwelling and innershelf circulation.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Upwelling and innershelf circulation"

1

Zhou, Tiehan, Marvin A. Geller, and Kevin Hamilton. "The Roles of the Hadley Circulation and Downward Control in Tropical Upwelling." Journal of the Atmospheric Sciences 63, no. 11 (2006): 2740–57. http://dx.doi.org/10.1175/jas3770.1.

Full text

Abstract:

Abstract Several idealized models of tropical upwelling are presented in order to clarify the roles of the nonlinear Hadley circulation and extratropical wave driving. In particular, it is shown that the Hadley circulation and wave-driven circulation interact to determine the nature of tropical upwelling. The authors explain several observed features such as maximum upwelling in the summer subtropics and the annual variation of the upwelling.

APA, Harvard, Vancouver, ISO, and other styles

2

Chen, Sih-Yu, and Shih-Nan Chen. "Generation of Upwelling Circulation under Downwelling-Favorable Wind within Bottom-Attached, Buoyant Coastal Currents." Journal of Physical Oceanography 47, no. 10 (2017): 2499–519. http://dx.doi.org/10.1175/jpo-d-16-0271.1.

Full text

Abstract:

AbstractA two-dimensional modeling study by Moffat and Lentz recently reported that downwelling-favorable wind can induce cross-shore upwelling circulation within a bottom-attached, buoyant coastal current. Here, we extend the problem to three dimensions. The driving mechanism and the sensitivity for the upwelling circulation are studied, using a primitive equation ocean model and an analytical model. After the initial downwelling adjustment that steepens the isopycnals and compresses the coastal current, the cross-shore flow can switch to steady upwelling circulation. This reverse circulation

APA, Harvard, Vancouver, ISO, and other styles

3

Schott, Friedrich A. "Shallow overturning circulation of the Western Indian Ocean." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 363, no. 1826 (2005): 143–49. http://dx.doi.org/10.1098/rsta.2004.1483.

Full text

Abstract:

The Indian Ocean differs from the other two oceans in not possessing an eastern equatorial upwelling regime. Instead, the upwelling occurs dominantly in the northwestern Arabian Sea and, to a lesser degree, around the Indian subcontinent. Subduction, on the other hand, occurs dominantly in the Southern Hemisphere. The result is a shallow Cross–Equatorial Cell connecting both regimes. The northward flow at thermocline levels occurs as part of the Somali Current and the southward upper–layer return flow is carried by the Ekman transports that are directed southward in both hemispheres. The main

APA, Harvard, Vancouver, ISO, and other styles

4

Wang, Guihua, Rui Xin Huang, Jilan Su, and Dake Chen. "The Effects of Thermohaline Circulation on Wind-Driven Circulation in the South China Sea." Journal of Physical Oceanography 42, no. 12 (2012): 2283–96. http://dx.doi.org/10.1175/jpo-d-11-0227.1.

Full text

Abstract:

Abstract The dynamic influence of thermohaline circulation on wind-driven circulation in the South China Sea (SCS) is studied using a simple reduced gravity model, in which the upwelling driven by mixing in the abyssal ocean is treated in terms of an upward pumping distributed at the base of the upper layer. Because of the strong upwelling of deep water, the cyclonic gyre in the northern SCS is weakened, but the anticyclonic gyre in the southern SCS is intensified in summer, while cyclonic gyres in both the southern and northern SCS are weakened in winter. For all seasons, the dynamic influenc

APA, Harvard, Vancouver, ISO, and other styles

5

Bednorz, Ewa, Marek Półrolniczak, Bartosz Czernecki, and Arkadiusz M. Tomczyk. "Atmospheric Forcing of Coastal Upwelling in the Southern Baltic Sea Basin." Atmosphere 10, no. 6 (2019): 327. http://dx.doi.org/10.3390/atmos10060327.

Full text

Abstract:

This study analyzes the atmospheric forcing of upwelling occurrence along differently oriented coastlines of the southern Baltic Sea basin. The mean daily sea surface temperature (SST) data from the summer seasons (June–August) of the years 1982–2017 made the basis for the detection of upwelling cases. For the atmospheric part of the analysis, monthly indices of four macroscale circulation patterns were used: North Atlantic Oscillation (NAO), Scandinavian (SCAND), East Atlantic (EA) and East Atlantic/Western Russia (EATL/WRUS). In order to identify the local airflows and wind conditions, zonal

APA, Harvard, Vancouver, ISO, and other styles

6

Katsman, Caroline A. "Impacts of Localized Mixing and Topography on the Stationary Abyssal Circulation." Journal of Physical Oceanography 36, no. 8 (2006): 1660–71. http://dx.doi.org/10.1175/jpo2925.1.

Full text

Abstract:

Abstract Stommel and coworkers calculated the stationary, geostrophic circulation in the abyssal ocean driven by prescribed sources (representing convective downwelling sites) and sinks (slow, widespread upwelling through the thermocline). The applied basin geometries were highly idealized with nearly uniform upwelling and gradual bottom slopes. In this paper, the classical Stommel–Arons theory for the abyssal circulation is extended by introducing pronounced bathymetry in the form of a midocean ridge and strongly enhanced upwelling in the vicinity of this ridge, modeled after direct observati

APA, Harvard, Vancouver, ISO, and other styles

7

Bednorz, Ewa, Marek Półrolniczak, and Arkadiusz M. Tomczyk. "Regional circulation patterns inducing coastal upwelling in the Baltic Sea." Theoretical and Applied Climatology 144, no. 3-4 (2021): 905–16. http://dx.doi.org/10.1007/s00704-021-03539-7.

Full text

Abstract:

AbstractAtmospheric feedback involved in the occurrence of coastal upwelling in a small semi-enclosed sea basin, i.e., the Baltic Sea, was analysed, and the regional circulation conditions triggering upwelling in different coastal sections were identified. Upwelling in the summer season (June–August, years 1982–2017) was recognized on the basis of sea surface temperature patterns. Circulation conditions were defined using (1) the established daily indices of zonal and meridional airflow and (2) the synoptic situation at sea level distinguished by applying rotated principal component analysis t

APA, Harvard, Vancouver, ISO, and other styles

8

Largier, John L. "Upwelling Bays: How Coastal Upwelling Controls Circulation, Habitat, and Productivity in Bays." Annual Review of Marine Science 12, no. 1 (2020): 415–47. http://dx.doi.org/10.1146/annurev-marine-010419-011020.

Full text

Abstract:

Bays in coastal upwelling regions are physically driven and biochemically fueled by their interaction with open coastal waters. Wind-driven flow over the shelf imposes a circulation in the bay, which is also influenced by local wind stress and thermal bay–ocean density differences. Three types of bays are recognized based on the degree of exposure to coastal currents and winds (wide-open bays, square bays, and elongated bays), and the characteristic circulation and stratification patterns of each type are described. Retention of upwelled waters in bays allows for dense phytoplankton blooms tha

APA, Harvard, Vancouver, ISO, and other styles

9

Hogg, Andrew McC, Paul Spence, Oleg A. Saenko, and Stephanie M. Downes. "The Energetics of Southern Ocean Upwelling." Journal of Physical Oceanography 47, no. 1 (2017): 135–53. http://dx.doi.org/10.1175/jpo-d-16-0176.1.

Full text

Abstract:

AbstractThe ocean’s meridional overturning circulation is closed by the upwelling of dense, carbon-rich waters to the surface of the Southern Ocean. It has been proposed that upwelling in this region is driven by strong westerly winds, implying that the intensification of Southern Ocean winds in recent decades may have enhanced the rate of upwelling, potentially affecting the global overturning circulation. However, there is no consensus on the sensitivity of upwelling to winds or on the nature of the connection between Southern Ocean processes and the global overturning circulation. In this s

APA, Harvard, Vancouver, ISO, and other styles

10

Troitskaya, Elena, Vadim Blinov, Vyacheslav Ivanov, et al. "Cyclonic circulation and upwelling in Lake Baikal." Aquatic Sciences 77, no. 2 (2014): 171–82. http://dx.doi.org/10.1007/s00027-014-0361-8.

Full text

APA, Harvard, Vancouver, ISO, and other styles

More sources

Dissertations / Theses on the topic "Upwelling and innershelf circulation"

1

Cheung, Yee Ying. "Modeling upwelling circulation over continental shelf in the northern South China sea /." View abstract or full-text, 2006. http://library.ust.hk/cgi/db/thesis.pl?AMCE%202006%20CHEUNG.

Full text

APA, Harvard, Vancouver, ISO, and other styles

2

Rodríguez, Cruz Elisabet. "Circulation patterns of Ría de Pontevedra under upwelling and downwelling conditions." Master's thesis, Universidade de Aveiro, 2017. http://hdl.handle.net/10773/23481.

Full text

Abstract:

Mestrado em Ciências do Mar e da Atmosfera<br>Circulation patterns inside some of the Rías Baixas have been widely studied, but this is not the case of the Ría de Pontevedra. Through this thesis, we try to enhance the knowledge about the circulation pattern of this Ría. A ROMS-AGRIF system con guration was used in this study. This con guration was validated through the comparison with weekly temperature and salinity data measured by INTECMAR. The analysis done in this work is based on the study of three representative events of the circulation patterns: one upwelling event and two downw

APA, Harvard, Vancouver, ISO, and other styles

3

Ndoye, Siny. "Fonctionnement dynamique du centre d'upwelling Sud-Sénégalais : approche par la modélisation réaliste et l'analyse d'observations satellite de température de surface de la mer." Thesis, Paris 6, 2016. http://www.theses.fr/2016PA066372/document.

Full text

Abstract:

L’extrémité sud du système du courant des Canaries comprend un centre d’upwelling (résurgence localisée d’eaux froides sous l’action de vents favorables) qui a jusqu’ici reçu peu d’attention. Ma thèse porte sur la dynamique de ce centre d’upwelling sud Sénégal ou SSUC (Southern Senegal Upwelling Center en anglais). Elle s’intéresse donc à la circulation et à la structure thermohaline sur le large plateau sud-sénégalais, entre la côte et _100-200 km au large en se focalisant sur la période d’upwelling (Novembre-Mai). Une des particularités de la zone est la séparation entre la zone d’upwelling

APA, Harvard, Vancouver, ISO, and other styles

4

Osborn, Timothy J. "Internally-generated variability in some ocean models on decadal to millennial timescales." Thesis, University of East Anglia, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.297045.

Full text

APA, Harvard, Vancouver, ISO, and other styles

5

Yulaeva, Elena Valentinovna. "On the mechanism of the large-scale seasonally varying upwelling in the region of the tropical tropopause /." Thesis, Connect to this title online; UW restricted, 1997. http://hdl.handle.net/1773/10092.

Full text

APA, Harvard, Vancouver, ISO, and other styles

6

Austin, Jay Alan. "Wind-driven circulation on a shallow, stratified shelf." Thesis, Massachusetts Institute of Technology, 1998. http://hdl.handle.net/1721.1/58538.

Full text

Abstract:

Thesis (Ph. D.)--Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), February 1999.<br>Includes bibliographical references (leaves 235-243).<br>A detailed examination of the development of a deep convection event observed in the Greenland Sea in 1988-89 is carried out through a combination of modeling, scale estimates, and data analysis. We develop a prognostic one-dimensional mixed layer model which is coupled to a thermodynamic ice model. Our model contains a represe

APA, Harvard, Vancouver, ISO, and other styles

7

Kounta, Diop Lala. "Le rôle de la dynamique océanique et atmosphérique en Atlantique Nord sur le fonctionnement de l'upwelling ouest-africain." Electronic Thesis or Diss., Sorbonne université, 2019. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2019SORUS649.pdf.

Full text

Abstract:

Cette thèse avait pour objectif de mieux comprendre le rôle de la dynamique océanique et atmosphérique régionale sur le fonctionnement de l’upwelling ouest africain. La première partie est consacrée à l’étude du cycle saisonnier, de la dynamique et de l’origine des masses d’eau du courant de bord qui alimente l’upwelling ouest africain. Ce courant est situé sur la pente continentale et est dénommé WABC (pour West African poleward Boundary Current en anglais). Son lien avec la circulation à l’échelle de l’Atlantique Tropical Nord Est (ATNE) est aussi étudié. Les résultats obtenus sont principal

APA, Harvard, Vancouver, ISO, and other styles

8

Di, Nezio Pedro N. "Climate Response of the Equatorial Pacific to Global Warming." Scholarly Repository, 2008. http://scholarlyrepository.miami.edu/oa_theses/157.

Full text

Abstract:

The climate response of the equatorial Pacific to increased greenhouse gases is investigated using numerical experiments from five climate models participating in the Intergovernmental Panel on Climate Change Fourth Assessment Report. Changes in the heat budget of the surface layer in response to CO2 doubling (2xCO2) are analyzed in experiments with full-coupled ocean dynamics; and compared to experiments with uncoupled ocean dynamics. In full-coupled experiments, weaker ocean zonal currents driven by a slowing down of the Walker circulation reduce the ocean heat flux divergence throughout the

APA, Harvard, Vancouver, ISO, and other styles

9

Silva, Lourval dos Santos. "Condições oceanográficas no canal de São Sebastião: fevereiro de 1994 a março de 1995." Universidade de São Paulo, 1995. http://www.teses.usp.br/teses/disponiveis/21/21132/tde-29012004-131532/.

Full text

Abstract:

Um conjunto de dados hidrográficos e correntométricos foram coletados entre fevereiro/94 e março/95 no Canal de São Sebastião e região costeira adjacente, para o estudo em primeira aproximação de suas variações sazonais. Da análise da rede externa ao canal observou-se um acentuado contraste de salinidade e de temperatura ao redor da Ilha de São Sebastião, bem como movimentos ascendentes a norte da ISS. Já no interior do canal, ficou determinado que correntes para SW indicam a aproximação da ACAS na costa. Os cruzeiros de verão não apresentaram a formação em duas camadas e no inverno as condiçõ

APA, Harvard, Vancouver, ISO, and other styles

10

Ribeiro, Flávia Noronha Dutra. "Padrões das circulações atmosférica e oceânica na região de ressurgência costeira de Cabo Frio." Universidade de São Paulo, 2010. http://www.teses.usp.br/teses/disponiveis/14/14133/tde-28062013-185755/.

Full text

Abstract:

Um modelo oceânico de 1 ½ camadas é desenvolvido e acoplado ao modelo atmosférico tridimensional de meso escala TVM-NH, com a finalidade de estudar a interação entre a circulação atmosférica e o fenômeno de ressurgência costeira na região de Cabo Frio (RJ Brasil). A condição de contorno do modelo oceânico foi testada e provou ser pouco reflexiva. O modelo oceânico demonstrou ser capaz de representar a distribuição espacial e evolução temporal da temperatura da superfície do mar na região de estudo. O modelo acoplado foi então utilizado para estudar a influência conjunta entre a ressurgência

APA, Harvard, Vancouver, ISO, and other styles

More sources

Books on the topic "Upwelling and innershelf circulation"

1

Austin, Jay Alan. Wind-driven circulation on a shallow, stratified shelf. Massachusetts Institute of Technology, Woods Hole Oceanographic Institution, Joint Program in Oceanography/Applied Ocean Science and Engineering, 1998.

Find full text

APA, Harvard, Vancouver, ISO, and other styles

2

Austin, Jay Alan. Wind-driven circulation on a shallow, stratified shelf. Massachusetts Institute of Technology, Woods Hole Oceanographic Institution, Joint Program in Oceanography/Applied Ocean Science and Engineering, 1998.

Find full text

APA, Harvard, Vancouver, ISO, and other styles

3

International Symposium on Vertical Motion in the Equatorial Upper Ocean and its Effects upon Living Resources and the Atmosphere (1985 Paris). Vertical motion in the equatorial upper ocean: Proceedings of the International Symposium on Vertical Motion in the Equatorial Upper Ocean and its Effects upon Living Resources and the Atmosphere, Unesco, Paris, France, 6-10 May 1985. Gauthier-Villars, 1987.

Find full text

APA, Harvard, Vancouver, ISO, and other styles

4

International Symposium on Vertical Motion in the Equatorial Upper Ocean and its Effects upon Living Resources and the Atmosphere (1985 Paris). Vertical motion in the equatorial upper ocean: Proceedings of the International Symposium on Vertical Motion in the Equatorial Upper Ocean and its Effects upon Living Resources and the Atmosphere : Unesco, Paris, France, 6-10 May 1985. Gauthier-Villars, 1987.

Find full text

APA, Harvard, Vancouver, ISO, and other styles

5

Fischer, Williams E., and Adams B. Green. Upwelling: Mechanisms, Ecological Effects and Threats to Biodiversity. Nova Science Publishers, Incorporated, 2014.

Find full text

APA, Harvard, Vancouver, ISO, and other styles

6

The Oceanic Thermohaline Circulation: An Introduction (Atmospheric and Oceanographic Sciences Library). Springer, 2006.

Find full text

APA, Harvard, Vancouver, ISO, and other styles

7

Behera, Swadhin, and Toshio Yamagata. Climate Dynamics of ENSO Modoki Phenomena. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.612.

Full text

Abstract:

The El Niño Modoki/La Niña Modoki (ENSO Modoki) is a newly acknowledged face of ocean-atmosphere coupled variability in the tropical Pacific Ocean. The oceanic and atmospheric conditions associated with the El Niño Modoki are different from that of canonical El Niño, which is extensively studied for its dynamics and worldwide impacts. A typical El Niño event is marked by a warm anomaly of sea surface temperature (SST) in the equatorial eastern Pacific. Because of the associated changes in the surface winds and the weakening of coastal upwelling, the coasts of South America suffer from widespre

APA, Harvard, Vancouver, ISO, and other styles

Book chapters on the topic "Upwelling and innershelf circulation"

1

Walker, Nan D. "Wind and Eddy-Related Shelf/Slope Circulation Processes and Coastal Upwelling in the Northwestern Gulf of Mexico." In Circulation in the Gulf of Mexico: Observations and Models. American Geophysical Union, 2013. http://dx.doi.org/10.1029/161gm21.

Full text

APA, Harvard, Vancouver, ISO, and other styles

2

"Deep upwelling and mixing." In The Oceanic Thermohaline Circulation: An Introduction. Springer New York, 2007. http://dx.doi.org/10.1007/978-0-387-48039-8_9.

Full text

APA, Harvard, Vancouver, ISO, and other styles

3

"Equatorial Circulation, Shallow Overturning, and Upwelling." In Ocean Circulation in Three Dimensions. Cambridge University Press, 2019. http://dx.doi.org/10.1017/9781139015721.008.

Full text

APA, Harvard, Vancouver, ISO, and other styles

4

Álvarez-Borrego, Saul. "Physical Oceanography." In Island Biogeography in the Sea of Cortés II. Oxford University Press, 2002. http://dx.doi.org/10.1093/oso/9780195133462.003.0008.

Full text

Abstract:

The nature of the relationships between physical and biological processes in the ocean is subtle and complex. Not only do the physical phenomena create a structure, such as a shallow, mixed layer or a front, within which biological processes may proceed, but they also influence the rates of biological processes in many indirect ways. In the ocean, physical phenomena control the distribution of nutrients necessary for phytoplankton photosynthesis. Places with higher kinetic energy have higher concentrations of planktonic organisms, and that makes the whole food web richer (Mann and Lazier 1996). For example, in the midriff region of the Sea of Cortés (Tiburón and Ángel de la Guarda; fig. 1.2), tidal currents are strong, and intense mixing occurs, creating a situation similar to constant upwelling. Thus, primary productivity is high, and this area supports large numbers of sea birds and marine mammals (Maluf 1983). The Gulf of California is a dynamic marginal sea of the Pacific Ocean and has been described as an area of great fertility since the time of early explorers. Gilbert and Allen (1943) described it as fabulously rich in marine life, with waters fairly teeming with multitudes of fish, and to maintain these large numbers, there must be correspondingly huge crops of their ultimate food, the phytoplankton. Topographically the gulf is divided into a series of basins and trenches, deepening to the south and separated from each other by transverse ridges (Shepard 1950; fig. 3.1). Input of nutrients into the gulf from rivers is low and has only local coastal effects. The Baja peninsula has only one, very small river, near 27°N; rivers in mainland Mexico and the Colorado River have dams that divert most of the water for agricultural and urban use. The gulf has three main natural fertilization mechanisms: wind-induced upwelling, tidal mixing, and thermohaline circulation. Upwelling occurs off the eastern coast with northwesterly winds (winter conditions from December through May) and off the Baja California coast with southeasterly winds (summer conditions from July through October), with June and November as transition periods (Álvarez-Borrego and Lara- Lara 1991).

APA, Harvard, Vancouver, ISO, and other styles

5

Dolman, Han. "The Carbon Cycle." In Biogeochemical Cycles and Climate. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780198779308.003.0009.

Full text

Abstract:

The chapter first shows carbon dioxide variability over long geological timescales. The current stocks and fluxes of carbon are then given, for the whole planet and for the atmosphere, ocean and land separately. The main flows of carbon in the ocean, through the biological pump (via uptake through photosynthesis) and the physical pump (via involving chemical transformation uptake in water and production of carbonate), and on land, through photosynthesis (Gross Primary Production) and respiration leading to Net Primary Production, Net Ecosystem Production and Net Biome Production and through the storage of carbon in biomass, are described. Next, carbon interactions during the Paleocene–Eocene Thermal Maximum and glacial–interglacial transitions, thought to involve changes in ocean circulation and upwelling, are examined. The key changes from anthropogenic perturbation of the natural carbon cycle are shown to be due to fossil fuel burning and land-use change (deforestation). The effects of the carbon–climate feedback on temperature and carbon stocks are also shown.

APA, Harvard, Vancouver, ISO, and other styles

6

"Island in the Stream: Oceanography and Fisheries of the Charleston Bump." In Island in the Stream: Oceanography and Fisheries of the Charleston Bump, edited by George R. Sedberry, John C. Mcgovern, and Oleg Pashuk. American Fisheries Society, 2001. http://dx.doi.org/10.47886/9781888569230.ch1.

Full text

Abstract:

<em>Abstract.</em>—The Charleston Bump is a complex bottom feature of great topographic relief located southeast of Charleston, South Carolina. This bottom feature deflects the Gulf Stream offshore in the South Atlantic Bight, and establishes permanent and temporary eddies, gyres, and associated upwellings in the warm Gulf Stream flow. Thermal fronts associated with Gulf Stream deflection, and die bottom feature itself, are believed to be attractive to large pelagic fishes, or result in concentrations of larvae, juveniles, and prey for larger fish. Upwelling in the region supports early life history stages of important fishery species. Deflection of the Gulf Stream may also play a direct or indirect role in transport of early life stages toward, or away from, nursery areas. Sea surface temperatures (SSTs) influenced by the Gulf Stream response to the Charleston Bump appear to have a role in determining recruitment success in gag <em> Mycteroperca microlepis, </em>a continental shelf reef fish. Relative cohort strength in gag was correlated (r = 0.89) to SST at 33°30'N, 78°30' W. Variability in conditions mat affect recruitment of larvae and juveniles, combined with heavy fishing pressure on prespawning adults, may result in recruitment failure in gag. In addition to strongly influencing circulation patterns in the South Atlantic Bight, die rugged bottom topography of the Bump is an important habitat and spawning ground for wreckfish <em> Polyprion americanus </em>and supports die U.S. fishery for this species. As a result, die Bump is an essential habitat for this species in U.S. waters. A geographic analysis of commercial pelagic longline logbook data shows mat die Charleston Bump is an area of concentrated commercial fishing effort, and that pelagic longline fisheries also concentrate along fronts at die edges of Gulf Stream gyres and eddies downstream. The "Charleston Bump Complex" of rough bottom topography and dynamic oceanography is an essential habitat for wreckfish and highly migratory pelagic fishes, and may influence recruitment success in some continental shelf fishes.

APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Upwelling and innershelf circulation"

1

Suursaar, Ü. "Interpretation of Doppler effect-based vertical velocity measurements in the coastal waters of Estonia, Baltic Sea: possible influence of upwelling, Langmuir circulation and turbidity." In FLUID STRUCTURE INTERACTION 2009. WIT Press, 2009. http://dx.doi.org/10.2495/fsi090181.

Full text

APA, Harvard, Vancouver, ISO, and other styles

We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!