The number of cloud droplets formed at the cloud base depends on both the properties of aerosol particles and the updraft velocity of an air parcel at the cloud base. As the spatial scale of updrafts is too small to be resolved in global atmospheric models. the updraft velocity is commonly parameterised based on the available turbulent kinetic energy. Here we present alternative metho... https://www.freeebookfinder.com/product-category/fr-sweatshirts/