Not exact matches
Shallow coral reefs from the water's
surface to 30 - 40 metres depth are the tip of the iceberg that comprises the
ocean's extensive coral ecosystem.
This interaction may occur anywhere in the
ocean, in particular in regions where
surface - gravity waves interact as they reflect from continental shelf breaks, where the deep - sea suddenly faces a much
shallower shoreline.
Whereas the nodules are scattered across the deep abyssal plains of the
oceans, hundreds of miles from shore and typically three miles or more below the
surface, many of the sulfide deposits are close to a coastline; also, they are always on undersea mountains and therefore located in much
shallower water.
Whipped up by
surface winds and girded by the Coriolis effect (produced by Earth's rotation), eddies may grow to several hundred kilometers in diameter and are known to transport heat, chemicals and biology throughout the
oceans»
shallower depths.
A report about U.S. oil and gas exploration in the Arctic published last month by the National Petroleum Council found most drilling opportunities under America's jurisdiction are less than 100 meters below the
ocean's
surface, more
shallow - than - standard depths in other drill regions, like the Gulf of Mexico.
The increased wave action reaches down and stirs up sediments on
shallow continental shelves, releasing radium and other chemicals that are carried up to the
surface and swept away into the open
ocean by currents such as the Transpolar Drift.
The entire
ocean — from the depths to the
shallows — gets its oxygen supply from the
surface, either directly from the atmosphere or from phytoplankton, which release oxygen into the water through photosynthesis.
Venus may have had a
shallow liquid - water
ocean and habitable
surface temperatures for up to 2 billion years of its early history, according to computer modeling of the planet's ancient climate by scientists at NASA's Goddard Institute for Space Studies (GISS) in New York.
The carbon in the atmosphere,
ocean, on the
surface, life, and other
shallow, near
surface reservoirs accounts for only about 10 % of Earth's carbon.
According to computer modelling, the planet Venus could have once been habitable, hosting a
shallow - water
ocean, and
surface temperatures hospitable to life.
The
shallow depth, by the way, would be ideal for Kamino - style
ocean platforms, allowing construction of covered cities at the
ocean surface, where armies of clones could march and drill in peace.
Vivid soft corals and gorgonian fans are a highlight here combined with colorful
shallow coral gardens to explore during your safety stop Koh Phi Phi is as fabulous below the
ocean's
surface as it is above it.
Close to shore, every island is surrounded by
shallow coral reefs that are just a few feet below the
ocean's
surface.
I would claim that the
surface temperature — which is a comparatively easy thing to measure — is a relevant test of climate physics because a lot of the
ocean response is indeed determined by the relatively
shallow mixed layer.
A given chunk of water moves because of the net forces on it, and so a net northward transfer of water not driven by friction must require that the average isobar
surfaces slope downwards in the
shallow ocean as you go north.
The concern, as I understand it, is that pathways in the latter areas can bring undissolved methane up to the seabed
surface, and from there it can make it way through the
shallow water column into the
ocean surface.
And that's part of the reason oil companies are drilling a mile beneath the
surface of the
ocean — because we're running out of places to drill on land and in
shallow water.
Due to the Antarctic Refrigerator Effect, the deep
oceans continued to cool, and the thermocline that separates warm
surface water from cooler deep waters became increasingly more
shallow.
Venus may have had a
shallow liquid - water
ocean and habitable
surface temperatures for up to 2 billion years of its early history.
I suspect that larger tidal currents over
shallow water mix
ocean heat up to the
surface to keep these waters covered by water or dangerously thin ice.
«Previous observations have pointed to large methane plumes being released from the seabed in the relatively
shallow sea off the northern coast of Siberia, but the latest findings were made far away from land in the deep, open
ocean where the
surface is usually capped by ice.»
When many modern families of animals developed in a hot greenhouse world in which a warm
ocean and land filled most of earths
surface with fertile
shallow seas and vast tropical jungles.
An enhanced AMOC leads to a stronger cyclonic circulation north of the Gulf Stream and a southward shift of the Gulf Stream path, which results in
shallower isopycnals (
surfaces of constant density in
ocean) in the Gulf Stream front.
The dissipative friction force is a viscous friction between the
surface mixed layer and the deeper
ocean layers or the
shallow continental shelf.
Presumably, the theorized massive movement of heat from
shallow surface waters to deep regions of the Atlantic and Southern
Oceans remains an active process.
That the slowdown in
surface warming has been concentrated in the
ocean -
surface (and
shallow -
ocean) temperatures has led a number of scientists (including the Met Office) to posit that the pause in
ocean surface warming may be driven in part by increased heat uptake in the deep
ocean.
Increased carbon dioxide has already lowered the pH of the
surface ocean; this is expected to have a negative effect on survival of plankton, the base of the marine food chain, and the growth and health of corals, which form biodiverse reefs in
shallow waters of the Hawaiian Islands and Florida, and deep reefs in Alaska and the Southeast U.S. Invasive species are increasingly being recognized.
It looks like the sub-sea permafrost is failing due to warmer
ocean temperatures and allowing methane to escape; because the Siberian Sea is very
shallow the methane isn't oxidized as it travels to the
surface.
It doesn't even appear to be enough to raise the temperature of the
shallow surface layer by more than a fraction of a degree to say nothing of imparting any significant warmth to the other 90 % of the volume of the global
ocean below the thermocline (400 + meters deep).
If I remember my
ocean circulation correctly, the exchange between the deep
ocean and the
surface /
shallow ocean takes place at only a few regions.