The researchers also found that larval behavior enhances the persistence of these network connections, when compared to passive
transport by the ocean currents.
Cameron has been studying how and why this energy
transport by ocean currents affects the global climate.
Variations in SST due to variations in heat
transport by ocean currents or diffusion into the thermocline are neglected while contributions by changes in evaporation, turbulent transfer, and surface radiation are estimated as being proportional to the anomalous air - sea temperature difference.
Not exact matches
«We established a means to study viral populations within more complex communities and found that surface
ocean viruses were passively
transported on
currents and that population abundances were structured
by local environmental conditions,» said Sullivan, associate professor in the Department of Ecology and Evolutionary Biology and member of the BIO5 Institute.
«We established a means to study viral populations within more complex communities and found that surface
ocean viruses were passively
transported on
currents and that population abundances were structured
by local environmental conditions,» said Sullivan, associate professor in the Department of Ecology and Evolutionary Biology and a member of the BIO5 Institute.
By analogy, a warmer world wouldn't be rainier (or cloudier); it's an imperfect analogy, because rain isn't absolutely correlated with cloudiness, and lateral transport of energy by ocean, air, and latent heat currents in and out of the E & W Pacific Ocean areas won't scale to global warmi
By analogy, a warmer world wouldn't be rainier (or cloudier); it's an imperfect analogy, because rain isn't absolutely correlated with cloudiness, and lateral
transport of energy
by ocean, air, and latent heat currents in and out of the E & W Pacific Ocean areas won't scale to global warmi
by ocean, air, and latent heat currents in and out of the E & W Pacific Ocean areas won't scale to global wa
ocean, air, and latent heat
currents in and out of the E & W Pacific
Ocean areas won't scale to global wa
Ocean areas won't scale to global warming
The mercury - enriched waters then enter a long - range eastward
transport by large
ocean circulation
currents,» said USGS scientist and coauthor David Krabbenhoft.
WHOI scientists were involved in the recently reported study of rapid draining of glacier meltwater lakes, but WHOI is also studying the
transport of carbon sediments
by ocean currents.
On the other hand, the budgeting of salinity implicit in the
ocean model used
by Hatun et al. may not properly account for river run - off (freshens the water),
transport from the Pacific, the Canadian Archipelago, the East Greenland
current, or melting processes.
One, she says, «clearly and authoritatively describes the complex interactions among
ocean dynamics and heat
transport, sea ice dynamics forced both
by atmospheric winds and
ocean currents, and atmospheric thermodynamic forcing in determining recent variations in multi-year sea ice extent.
JC comment: This paper clearly and authoritatively describes the complex interactions among
ocean dynamics and heat
transport, sea ice dynamics forced both
by atmospheric winds and
ocean currents, and atmospheric thermodynamic forcing in determining recent variations in multi-year sea ice extent.
Transport of heat
by winds and
ocean currents
6 Climate is caused
by many factors including: Trapping of heat
by the atmosphere Latitude
Transport of heat
by winds and
ocean currents
Conversely, during low solar activity during the Little Ice Age,
transport of warm water was reduced
by 10 % and Arctic sea ice increased.17 Although it is not a situation I would ever hope for, if history repeats itself, then natural climate dynamics of the past suggest, the
current drop in the sun's output will produce a similar cooler climate, and it will likely be detected first as a slow down in the poleward
transport of
ocean heat.22 Should we prepare for this possibility?
Also described in the post: surface waters with ENSO - induced anomalies in the South Atlantic should be
transported northward into the North Atlantic
by ocean currents.
Here, we have shown that this warming was associated and presumably initiated
by a major increase in the westerly to south - westerly wind north of Norway leading to enhanced atmospheric and
ocean heat
transport from the comparatively warm North Atlantic
Current through the passage between northern Norway and Spitsbergen into the Barents Sea.»
In the tropics
oceans absorb energy on average before it is
transported poleward
by currents and generally given up to the atmosphere.
These anomalies are then
transported by major
ocean currents to locations where the stored energy is released into the atmosphere, altering atmospheric pressure and moisture patterns that can ultimately affect regional precipitation.
Or exactly how much heating of the equatorial
ocean gets
transported to the poles
by ocean currents.
The zonal integral (east to west) of wind stress curl across an
ocean basin is proportional to the western boundary
current transport (i.e., the
transport responsible for the dominant part of the poleward heat flux
by the
ocean).