These currents are located on
the western side of every ocean basin.
Warm currents transport heat from lower latitudes poleward and tend to occur on
the western sides of oceans.
As shown here for the North Atlantic but also true for all ocean basins, the ocean surface slope is steeper on
the western side of an ocean basin than on the eastern side.
Not exact matches
That is the boundary on the
Western side, it goes all the way down, it cuts across Graphic Road to Nkrumah Circle Area and then the Southern border
of that will be the Atlantic
Ocean.
The study reports that glaciers flowing to the coast on the
western side of the Peninsula show a distinct spatial correlation with
ocean temperature patterns, with those in the south retreating rapidly but those in the north showing little change.
The
western side of the mountain offers stunning views
of the town, port,
ocean, and several outlying islands.
Oceans Rest is situated in the picturesque sea
side village
of Vlees Bay, in the
Western Cape.
Boasting the highest number
of ocean -
side holes in the
Western Hemisphere, the 72 - par Playa Grande Golf Course affords panoramic mountain - to - sea views.
The hooks will be required starting May 5 ahead
of the spring spawning season in the Gulf
of Mexico for the bluefin that frequent the
western side of the Atlantic
Ocean.
The Humboldt Current Large Marine Ecosystem (off Chile and Peru), the Benguelan Current LME (Namibia and South Africa), the Canary Current LME (Morocco), are the other main upwelling ecosystems, all driven by similar oceanographic and atmospheric processes, all on the eastern
sides of ocean basins (
western sides of continents).
The aforementioned high - amplitude ridging in the Gulf
of Alaska and the associated «blocked» flow over the Pacific
Ocean has led to an accumulation
of very cold air on its downstream
side over
western Canada.
As a result
of this juxtaposition
of cold air and warm air, the eastern
sides of continents and the
western fringes
of oceans in middle and high latitudes are the preferred locations for extratropical storm development.
Owing to the enhanced descent
of air over the eastern parts
of the
oceans, landmasses adjacent to these areas (typically the
western sides of continents) tend to be deserts, such as those found in northwestern and southwestern Africa and along
western coastal Mexico.
But unlike those cycles, which create a standing pattern
of warmth on one
side of the tropical Pacific, the MJO is nearly continuous, creating a migrating cluster
of storms that spawns over the
western Indian
Ocean and moves eastward at 15 — 30 kilometers per hour.
Overall, this study reveals a unique susceptibility
of the Antarctic coastal
ocean to remote wind perturbations, particularly subsurface
ocean temperatures on the
western side of the peninsula.
My understanding
of Richard Seager's point is that even without a Gulf - Stream - like current, the eastern
side of middle latitude
ocean basins will be warmer than their
western flanks and continental Europe would be warmer than North America at the same latitude.
Transport
of surface waters toward the
western boundary
of the
ocean basins causes the
ocean - surface slope to be steeper on the
western side (versus eastern
side)
of a gyre (in either hemisphere).