Abstract

Abstract The effects of longwave radiation in a small cumulus cloud are investigated by a combination of a three-dimensional radiative transfer model as well as a slab-symmetric cloud dynamics model. The calculations indicate that longwave radiative cooling substantially enhances the maximum cloud water content. For a run in an environment without wind shear, the maximum increase reaches 96%. The total cloud water content was also increased somewhat (maximum 20%). The effects of longwave cooling at different stages of development of the simulated cloud were further examined and analyzed. In the initial stage of the development, the augmentation of cloud water content near the cloud top and sides is traced mainly to the direct effect of longwave radiative cooling on cloud microphysics (i.e., radiative cooling reduces the local temperature and hence the saturation water vapor pressure, which leads to additional condensation). In the mature stage of the cloud, the increase of total cloud water content arises...

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call