Results 191 to 200 of about 852,517 (245)

Physiology and Survival of Intertidal Calcifiers in Two Contrasting Upwelling Systems. [PDF]

open access: yesEcol Evol
Hernández-Dauval A   +3 more
europepmc   +1 more source

Microbiota responses to environmental stress in mobile and sessile marine invertebrates: evidence for the effect of dissolved oxygen variations. [PDF]

open access: yesFront Microbiol
Valenzuela-Muñoz V   +7 more
europepmc   +1 more source

The Arabian Seas: a window into future oceans -physical, biogeochemical, and ecological dynamics in unique marginal environments. [PDF]

open access: yesNatl Sci Rev
Zhan P   +19 more
europepmc   +1 more source

Global Climate Change and Intensification of Coastal Ocean Upwelling

open access: yesScience, 1990
A mechanism exists whereby global greenhouse warning could, by intensifying the alongshore wind stress on the ocean surface, lead to acceleration of coastal upwelling.
Andrew Bakun
exaly   +2 more sources
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A documentary proxy for coastal upwelling

2023
Coastal upwelling is a process in which sea water from intermediate depths emerges along the west coast of continents in response to the intensity of the alongshore component of the wind. These areas are economically relevant as upwelled water is rich in nutrients, creating regions of great interest for fisheries.Quantifying upwelling intensity at ...
David Gallego   +4 more
openaire   +1 more source

A Cyclesonde View of Coastal Upwelling

Journal of Physical Oceanography, 1976
Abstract In August 1973, 320 vertical profiles of temperature and horizontal velocity were recorded during a 64 h period by an array of three Cyclesondes in the coastal upwelling region off Oregon. The mean interior along-shore velocity was geostrophic and a linear function of density, with a near-surface, equatorward jet at mid-shelf, and a poleward ...
Walter R. Johnson   +2 more
openaire   +1 more source

A Numerical Model of Coastal Upwelling

Journal of Physical Oceanography, 1972
Abstract A wind-driven model of coastal upwelling induced into a stratified, rotating ocean is solved numerically. The circulation is on an f plane and longshore variations are neglected. A multilevel model is derived, but only solutions for a two-layer model are discussed. A longshore baroclinic surface jet is discovered.
James J. O'Brien, H. E. Hurlburt
openaire   +1 more source

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