Not exact matches
Once a year, they migrate from the
deep ocean to shallow
water along the Pacific Coast of North America.
El Nino's mass of warm
water puts a lid on the normal currents of cold,
deep water that typically rise to the surface
along the equator and off the coast of Chile and Peru, said Stephanie Uz,
ocean scientist at Goddard Space Flight Center in Greenbelt, Maryland.
During the spring and summer months,
deep ocean water rich in carbon dioxide periodically wells up
along the California coast when surface
waters are pushed offshore by strong winds.
Sardines thrived here, feeding on the rich blooms of plankton fertilized by nutrients carried
along by rising
deep ocean waters.
Most of the deposits, some small and some large, are buried in or below permafrost and sediments in the
ocean bottom
along continental margins — where shallow offshore
waters slope down toward the
deeper ocean floor.
The waves that run
along shallow continental shelves are much larger than those over the
deep ocean, and so the force applied by the standing waves is also larger in shallow
water.
In the North West US
along the Pacific Coast the oyster industry has been having a hard time for the last two or three years, partly because of
ocean acidification, which is related with the upwelling of
deep water.
From
deep water fishing to whale watching...
along with sightseeing and enjoying the spectacular BC scenery and
ocean wilderness off the northwest coast of Vancouver Island.
eadler2 January 10, 2015 at 5:54 pm ... When
ocean surface temperatures cool, due to a La Nina, the warmer surface
water is mixed
deeper into the
ocean and cooler
ocean water flows
along the surface of the Pacific.
When
ocean surface temperatures cool, due to a La Nina, the warmer surface
water is mixed
deeper into the
ocean and cooler
ocean water flows
along the surface of the Pacific.
When the wind - driven
ocean circulation is intense, such as during the negative phase of the IPO & La Nina, there is strong upwelling of cold
deep water along the equator, and
along the eastern coasts of the continents.
Our results suggest that the majority of the world's
deep water is not transported back to the surface
along the current systems of the standard great
ocean conveyor (GOC).
Dense
water sinks and can form
deep water currents that flow
along the
ocean floor or on another layer of denser
water.
The JGR paper is full of «might have», «may have», «could have» caveats
along with «Its comparison with available bottom
water measurements shows reasonably good agreement, indicating that
deep ocean warming below 700 m might have contributed 1.1 mm / yr to the global mean SLR or one - third of the altimeter - observed rate of 3.11 ± 0.6 mm / yr over 1993 — 2008.»
For a long time people thought that
ocean pH was regulated ultimately by reactions between
deep seawater and sediments, but as Walt Allensworth February 5, 2015 at 3:08 pm, says there are so many black, and clear, vents
along the midocean ridges spewing acidic
water, that these probably maintain
ocean pH instead.
Since
ocean water can't travel on the time - scales predicated by the models the scientists conceived to record these measurements (less than 10 - 20 years), they think that energy is transferred instead
along a
deep pressure wave.
Being denser than warm
water it then sank and flowed out
along the bottom of the
ocean in
deep ocean currents, eventually filling the depths of the
ocean basins around the world.