Convective momentum transport

Convective momentum transport is an atmospheric event that involves an exchange of momentum, usually due to vertical motion (convection) associated with clouds.

The essential processes responsible for cloud convective momentum transport in the tropics are:

The vertical momentum advection due to subsidence of environmental air compensating cloud mass flux.
The detrainment of excess momentum from clouds.
The convection induced pressure gradient force.

References

Meteorological data and variables

General	Adiabatic processes Advection Buoyancy Lapse rate Lightning Surface solar radiation Surface weather analysis Visibility Vorticity Wind Wind shear

Condensation	Cloud Cloud condensation nuclei (CCN) Fog Convective condensation level (CCL) Lifted condensation level (LCL) Precipitation Water vapor

Convection	Convective available potential energy (CAPE) Convective inhibition (CIN) Convective instability Convective momentum transport Convective temperature (T_c) Equilibrium level (EL) Free convective layer (FCL) Helicity K Index Level of free convection (LFC) Lifted index (LI) Maximum parcel level (MPL) Bulk Richardson number (BRN)

Temperature	Dew point (T_d) Dew point depression Dry-bulb temperature Equivalent temperature (T_e) Forest fire weather index Haines Index Heat index Humidex Humidity Relative humidity (RH) Mixing ratio Potential temperature (θ) Equivalent potential temperature (θ_e) Sea surface temperature (SST) Thermodynamic temperature Vapor pressure Virtual temperature Wet-bulb temperature Wet-bulb potential temperature Wind chill

Pressure	Atmospheric pressure Baroclinity Barotropicity Pressure gradient Pressure-gradient force (PGF)

This article is issued from Wikipedia - version of the 8/25/2015. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.

Convective momentum transport

See also

References