The key physical parameters governing frictional dissipation in a precipitating atmosphere
Precipitation generates small-scale turbulent air flows—the energy of which ultimately dissipates to heat. The power of this process has previously been estimated to be around 2–4 W m−2 in the tropics: a value comparable in magnitude to the dynamic power of global atmospheric circulation. Here it is...
| Autores principales: | , , , , , , |
|---|---|
| Formato: | Journal Article |
| Lenguaje: | Inglés |
| Publicado: |
American Meteorological Society
2013
|
| Materias: | |
| Acceso en línea: | https://hdl.handle.net/10568/95730 |
Ejemplares similares: The key physical parameters governing frictional dissipation in a precipitating atmosphere
- Why does air passage over forest yield more rain?: examining the coupling between rainfall, pressure and atmospheric moisture content
- Comments on "The Tropospheric Land-Sea Warming Contrast as the Driver of Tropical Sea Level Pressure Changes"
- Vegetation Impact on Atmospheric Moisture Transport under Increasing Land-Ocean Temperature Contrasts
- Vegetation impact on atmospheric moisture transport under increasing land-ocean temperature contrasts
- Integrating prediction of precipitation and hydrology for early actions: the InPRHA project within the World Weather Research Programme
- The role of ecosystem transpiration in creating alternate moisture regimes by influencing atmospheric moisture convergence