Sentences with phrase «of diabatic»

This is the opposite of a diabatic process, where there is heat transfer.»

Wang, T. Vukicevic, G. Leoncini, T. Matsui, C. Castro, D. Niyogi, C.M. Kishtawal, A. Biazar, K. Doty, R.T. McNider, U. Nair, and W.K. Tao, 2007: Satellite - based model parameterization of diabatic heating.

The origins of the delayed increases in global surface temperature accompanying El Niño events and the implications for the role of diabatic processes in El Niño — Southern Oscillation (ENSO) are explored.

Diabatic temperature changes on the other hand can occur in the form of diabatic heating or diabatic cooling.

The tendency for clouds to form where air is going up creates an asymmetry of diabatic heating in a wave (see figure below).

Not exact matches

Regional diabatic heating can also cause atmospheric teleconnections that influence regional climate thousands of kilometers away from the point of forcing.

Vertical structure and physical processes of the Madden - Julian Oscillation: Linking hindcast fidelity to simulated diabatic heating and moistening, Journal of Geophysical Research - Atmospheres.

Vertical structure and diabatic processes of the Madden - Julian Oscillation: Biases and uncertainties at short range, Journal of Geophysical Research - Atmospheres, 120 (10): 4749 -4763.

Idealized horizontal profiles of vertical velocity (left) and diabatic heating (right) to illustrate how convective heating is asymmetric in an atmospheric wave.

With regard to the diabatic process the exchange of radiation in and out reaches thermal equilibrium relatively quickly (leaving Earth's oceans out of the scenario for current purposes) and once the temperature rise within the atmosphere has occurred then equilibrium has been achieved and energy in at TOA will match energy out.

Essentially, the adiabatic and diabatic loops must always match each other on any given planet at equilibrium because they are then of equal size and run at equal speed but are of opposite sign.

Essentially, an adiabatic process is one where temperature changes can occur without addition or removal of energy and a diabatic process is one where temperature changes can only occur as a result of the addition and or removal of energy.

As long as the AAL is a closed loop and kept independent of the Solar Diabatic Loop (SDL) then system equilibrium is maintained however high the surface temperature might rise.

Here is a simplified summary of the nature of, and differences, between diabatic and adiabatic processes.

(i) If one increases GHGs to slow down energy flow through the diabatic loop thereby warming that loop there will be an increase in PE relative to KE within the adiabatic loop instead of a change in the constant.

I have encountered much confusion about the relevance of so called diabatic and adiabatic processes in the minds of both alarmed proponents of Anthropogenic Global Warming (AGW) and in the minds of many sceptics.

(ii) If one decreases GHGs to speed up the energy flow through the diabatic loop thereby cooling that loop there will be a reduction in PE relative to KE within the adiabatic loop instead of a change in the constant.

The evolution of global mean surface temperatures, zonal means and fields of sea surface temperatures, land surface temperatures, precipitation, outgoing longwave radiation, vertically integrated diabatic heating and divergence of atmospheric energy transports, and ocean heat content in the Pacific is documented using correlation and regression analysis.

Quantify the magnitude, location, and physical mechanisms associated with interior diapycnal mixing in the ocean, which contribute to the diabatic AMOC, and evaluate the realism of current GCMs in this regard.

However, we can measure the temperature and estimate how it changes as a result of air flowing over an area, and then calculate the «leftover» residual temperature tendency to get an idea of how diabatic processes (i.e. convection and radiation) are heating the atmosphere.

Forced Rossby waves occur as a response of the midtroposhere and high - troposphere atmospheric circulation to the external diabatic and orographic forcing (25, 39, 40), which arises, e.g., from the thermal contrast between land and oceans as well as from mountain ranges.

This study investigates the features of eastward extension of the South Asian high (SAH) and its connection with diabatic heating and rainfall over eastern Asia on subseasonal time scales.

A further complication is that regional diabatic heating results in nonlinear long - distance communication of convergence and divergence fields, often referred to as teleconnections.

Quantify the magnitude, location, and physical mechanisms associated with interior diapycnal mixing in the ocean, which contribute to the diabatic AMOC, and evaluate the realism of current ocean GCMs in this regard.

For example, see The Diabatic and Nonlinear Aspects of the El Nino - Southern Oscillation: Implications for its Past and Future Behavior (Sun 2009).