Deep
moist atmospheric convection controls the development of major weather systems like hurricanes, drives the global transport of energy within the climate system and strongly influences the uncertainty of projected climate change.
More information: Miyamoto, Y., Kajikawa, Y., Yoshida, R., Yamaura, T., Yashiro, H. & Tomita, H. Deep
moist atmospheric convection in a subkilometer global simulation.
Not exact matches
The physics that must be included to investigate the
moist greenhouse is principally: (i) accurate radiation incorporating the spectral variation of gaseous absorption in both the solar radiation and thermal emission spectral regions, (ii)
atmospheric dynamics and
convection with no specifications favouring artificial
atmospheric boundaries, such as between a troposphere and stratosphere, (iii) realistic water vapour physics, including its effect on
atmospheric mass and surface pressure, and (iv) cloud properties that respond realistically to climate change.
It reflects reductions in lapse rates, which in the tropics reflect reductions in the
moist - adiabatic lapse rate to which
moist convection tends to restore
atmospheric temperature profiles.