Not exact matches
It is producing a «Submaran»: an unmanned device that can float on the
surface of the
ocean and also
drive 200 meters under the water to monitor pipelines,
currents, temperature or whatever a customer might want.
This is to be expected because the spin - up of the wind -
driven ocean circulation speeds up the
currents (Ekman transport) which carry heat out of the tropics in the near -
surface layers toward the subtropical
ocean gyres.
If the NAO were
driving an
ocean current that contains higher SST's and more saline
surface water into the Arctic region, I suspect it would be a possible correlation that salinity may be playing a part in the Arctic ice loss.
It's always worth remembering that the other end of the AMOC involves two main factors: (1) vorticity - mixing of heat from
surface waters into the deep abyssal
ocean (which decreases density causing the Atlantic Deep Water to start rising above the colder Antarctic Bottom Water) and (2) the wind -
driven upwelling around the Antarctic Circumpolar
Current.
Many of the
surface currents of the world
oceans (i.e., the
ocean «gyres» which appear as rotating horizontal
current systems in the upper
ocean) are
driven by the wind, however, the sinking in the Arctic is related to the buoyancy forcing (effects that change either the temperature or salinity of the water, and hence its buoyancy).
For example, atmospheric carbon dioxide grew by approximately 30 % during the transition from the most recent cold glacial period, about 20,000 years ago, to the
current warm interglacial period; the corresponding rate of decrease in
surface ocean pH,
driven by geological processes, was approximately 50 times slower than the
current rate
driven largely by fossil fuel burning.
Surface currents are largely wind -
driven, although the rotation of the earth, the presence of continents, and the
oceans» internal dynamics also have a strong influence.
In contrast to the wind -
driven currents, the THC is not confined to
surface waters but can be regarded as a big overturning of the world
ocean, from top to bottom.
I do understand that the winds are
driven by the uneven heating of the earth and, in turn, the winds effect
surface currents, but the
oceans of water, with it's peculiar properties, have an outsized effect.
15 Heat Transport in the Biosphere The unequal heating of Earth's
surface drives winds and
ocean currents transport heat throughout the biosphere Winds form because warm air tends to rise and cool air tends to sink air that is heated near the equator rises
After entering the Atlantic
Ocean, the
surface waters join the wind -
driven currents in the Atlantic, becoming saltier by evaporation under the intense tropical sun.
Oceanic
currents are largely
driven by the
surface wind stress; hence the large - scale atmospheric circulation is important to understanding the
ocean circulation.
This empirical finding contradicts Spencer's hypothesis that cloud cover changes are
driving global warming, but is consistent with our
current understanding of the climate:
ocean heat is exchanged with the atmosphere, which causes
surface warming, which alters atmospheric circulation, which alters cloud cover, which impacts
surface temperature.
Hamish Pritchard prepares us, «In most places in Antarctica, we can't explain the ice - shelf thinning through melting of snow at the
surface, so it has to be
driven by warm
ocean currents melting them from below.
This wind distribution
drives a system of
surface currents in the uppermost 100 metres of the
ocean.
wind and
ocean surface currents are as much or possibly even more important than temperature in
driving sea ice variability.
The induced
current around the equator would
drive the atmosphere and
surface ocean currents simultaneously, although being lighter, the atmosphere might show a change before
ocean currents.
Physically, it is difficult to see how
ocean temperatures can cause a consistent pattern of winds high up into the atmosphere while we have a very good physical explanation of how the winds can
drive the
surface ocean currents and temperature.
They also
drive the great
surface ocean currents such as the Gulf Stream: which is why ideas that these
currents could stop due to changes in water temperature is absurd.
In places
surface water sinks —
driving deep
ocean currents — and in others it upwells.
Heat transfer into the deep
oceans is pretty much all mechanically
driven by «circulation» factors, so a cooling of the southern
oceans due to changes in
surface winds and
currents would tend to change deep
ocean uptake.
Currents that move through the upper ocean then dive down to depth may move some of the surface heat to the deeper waters, especially where the currents have dived not just from cooling water (hot water would tend to go up, cold water would tend to go down) but because it is driven in «conveyor» systems which may run counter to expectations of where water should go when considering only local conditions, and especially, if the water is dropping because of an increase in s
Currents that move through the upper
ocean then dive down to depth may move some of the
surface heat to the deeper waters, especially where the
currents have dived not just from cooling water (hot water would tend to go up, cold water would tend to go down) but because it is driven in «conveyor» systems which may run counter to expectations of where water should go when considering only local conditions, and especially, if the water is dropping because of an increase in s
currents have dived not just from cooling water (hot water would tend to go up, cold water would tend to go down) but because it is
driven in «conveyor» systems which may run counter to expectations of where water should go when considering only local conditions, and especially, if the water is dropping because of an increase in salinity.
The westerlies of middle latitudes and the trade winds of the tropics
drive the most prominent features of
ocean surface motion, large - scale roughly circular
current systems elongated in the east - west direction known as gyres.