The smaller branch is advected eastward onto the North Icelandic shelf where the Atlantic water mixes with the colder waters of the East Icelandic Current, an offshoot from the cold East Greenland Current. ❋ Unknown (2009)
Low salinity waters and sea ice are subsequently advected through Fram Strait and the Canadian Archipelago into the convective regions of the North Atlantic. ❋ Unknown (2009)
In the northern Bering and southern Chukchi Seas, primary production occurs over a shallow shelf (50 to 200 m) and as the zooplankton and bacterioplankton cannot fully deplete this carbon source, it is either transferred to the benthos or advected downstream [17]. ❋ Unknown (2009)
Brine release during sea-ice formation increases the density of surface waters which then sink and are advected from the shelf to basin interiors, transporting CO2 into the halocline and deeper waters. ❋ Unknown (2009)
Sea ice from the Arctic Ocean is transported out through Fram Strait and advected southward by the East Greenland Current to cover the entire east coast of Greenland, although in mild winters it does not reach the southern tip of Greenland. ❋ Unknown (2009)
However mature the status of stand-alone sea-ice dynamics modeling, some AOGCMs still employ a simple, so-called "free drift" scheme that only allows ice to be advected with ocean currents. ❋ Unknown (2009)
Bond et al. [10] identified events when icebergs originating from Greenland were more strongly advected into the North Atlantic and proposed that changes in insolation may have been the cause. ❋ Unknown (2009)
Beginning in the Greenland Sea in 1968, significant quantities of freshwater were advected via Denmark Strait into the Subpolar Gyre. ❋ Unknown (2009)
SO2 aerosol has a much shorter lifetime and stays relatively close to its source, but it can be advected considerable distances. ❋ Unknown (2006)
It is likely larger than this since many of the records are from the ocean which are typically less sensitive to temperature change than landmasses, and further, adiabatic cooling of marine air advected over land masses would result from the ❋ Nigel Williams (2010)
That increased surface warmth is also available to be advected poleward by air currents. ❋ Unknown (2009)
Elsewhere, the West Coast would see clearing skies and warmer conditions Tuesday as the trough advected eastward. ❋ Unknown (2009)
There are some deviations - in particular, warming is concentrated near the surface at higher latitudes in winter because the surface is where the ice-albedo feedback occurs and the temperature profile is generally stable to convection (air gets heat advected from lower latitudes) - the tropical warming is greatest in the mid-to-upper troposphere because of changes in the moist adiabatic lapse rate (neutrally stable to moist convection); also, changes in surface evaporation and night-time cooling on land, etc … ❋ Unknown (2009)
