top of page

Clouds

    Clouds are formed from water vapor condensation on cloud condensation nuclei (CCN) or deposition on ice nuclei (IN). In the field, clouds can be monitored by ground-based (e.g. radars and ceilometers) and satellite-based (e.g. CloudSat) remote-sensing instruments over a long term. They can also be surveyed by air-borne instruments during field campaigns. The global cloud radiative effects on current and future climate are evaluated by numerical models. The best estimate on the present-day net cloud radiative forcing is -20 W m^-2. Currently, clouds are not well-represented in climate models, either due to the coarse resolution of models or due to poor understanding in key cloud processes. In Chapter 7 of IPCC AR5, the following aspects of cloud studies are assessed:

 

 

bottom of page