Reality: We both agree that warmer air can hold and
transport more moisture.
Not exact matches
This material allows for better airflow which helps aid in
transporting moisture away from the body, leaving you a baby
more comfortable.
When the jet stream does that, it
transports more heat and
moisture up into the Arctic, which heats the Arctic
more, which make the jet stream even wavier — another vicious cycle related to disappearance of sea ice.
Something even the UVic model can
more or less do is to demonstrate that you don't get anything remotely resembling the LGM in the tropics and SH unless you include the CO2 effect — though I suspect that the tropical results are very much contaminated by inadequacies in the diffusive representation of heat and
moisture transport.
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Taking the slow increase of precipitation with temperature as a given, the
more rapid increase of boundary layer humidity implies that the rate of
transport of
moisture from the boundary layer to higher levels where it rains out must go down.
For one thing turbulence instantly screws it up in the real world,
moisture content screws it up, lateral
transport screws it up, topology screws it up, the non-uniform temperature of the ground screws it up — the real atmosphere is constantly being kicked around between nearly isothermal and nearly DALR on any vertical column, with the actual measured thermal lapse rate rarely deviating by
more than 10 - 20 % from isothermal on an actual vertical sounding of the atmosphere.
The extra boost from the warmer water is adding even
more energy into this storm system, increasing the availability and
transport of
moisture toward land and producing
more efficient wind gusts to the surface.
But, much
more important, models are not intended to predict well all the remaining physical variables of the weather - climate system that are all local in their essence: 3D - temperature (atmosphere and ocean), precipitation, 3D - wind (and ocean currents), 3D - radiance, 3D - cloudness, 3D -
moisture content, 3D - aerosol concentration and
transport, etc, etc, etc...
The strong poleward atmospheric heat and
moisture transport may be one reason why the West Antarctic and Peninsula climate appears to be
more strongly coupled with regional sea ice concentration and extent anomalies than does the East Antarctic (e.g. Jacobs and Comiso 1997; Weatherly et al. 1991).