Sentences with phrase «advection through»

When the Nares Strait and NWP ice breaks up, that thick ice will be highly susceptible to advection through those passages.

Not exact matches

Arctic winter formation has been largely hit by advection from cyclones easily punching through what was once a mighty fortress of cold air living in a physical symbiosis with much thicker sea ice.

If monsoon winds get weaker, condensation and therefore latent heat release through precipitation are reduced (moisture - advection feedback, Fig. 1 A).

In response to the latent heat release, thermal energy is transported out of the region through large - scale advection and synoptic processes.

Heating by latent heat release and cooling through heat advection compensate each other, and both decrease with decreasing winds (or equivalently, land — ocean temperature difference ΔT; see Eq.

Nares Strait Recent ice advection patterns; warm water advances into the Arctic from the Atlantic; ice distribution patterns: all of these things show that conditions continue to be advantageous for export of ice through Fram Strait.

Although latent heat release through precipitation warms the atmospheric column, direct advection of heat is cooling it.

«Regression maps of SIM during the wintertime (January — March) AO index show 1) an increase in ice advection away from the coast of the East Siberian and Laptev Seas, which should have the effect of producing more new thin ice in the coastal flaw leads; 2) a decrease in ice advection from the western Arctic into the eastern Arctic; and 3) a slight increase in ice advection out of the Arctic through Fram Strait.

The net power flowing through a square meter per unit path via advection (is this what you mean by molecular flow?)

It is described by Here, a1 is a fixed heat capacity, which we approximate as the effective heat capacity per unit area of a 75 m ocean mixed layer; a3 corresponds to a doubling of atmospheric CO2 levels causing a forcing of 3.74 W m − 2; and C0 is the pre-industrial concentration of CO2 [30]; a0 and a2 are both able to vary, and control the climate sensitivity, and rate of advection of heat through the thermocline, respectively.

The difference is that the warming of the Western Antarctica Peninsula was known and is easily explained through atmospheric circulation dynamics — regional warm air advection patterns.

Since we can not measure any individual forcing directly in the atmosphere, the models draw upon results of laboratory experiments in passing sunlight through chambers in which atmospheric constituents are artificially varied; such experiments are, however, of limited value when translated into the real atmosphere, where radiative transfers and non-radiative transports (convection and evaporation up, advection along, subsidence and precipitation down), as well as altitudinal and latitudinal asymmetries, greatly complicate the picture.

Perhaps taking the time to familiarize oneself with the atmospheric circulation patterns of the area will show that it is perfectly normal, natural and expected that those particles reach Antarctica through warm air advection pathways... Just look at a satellite animation.