Mixed-phase clouds, thin cirrus clouds, and OLR over the tropics: observations, retrievals, and radiative impacts

dc.contributorDessler, Andrew E.
dc.contributorYang, Ping
dc.creatorLee, Joonsuk
dc.date.accessioned2010-01-15T00:15:43Z
dc.date.accessioned2010-01-16T02:20:03Z
dc.date.accessioned2017-04-07T19:56:51Z
dc.date.available2010-01-15T00:15:43Z
dc.date.available2010-01-16T02:20:03Z
dc.date.available2017-04-07T19:56:51Z
dc.date.created2007-08
dc.date.issued2009-06-02
dc.description.abstractThe tropics is a very important region in terms of earth?s radiation budget because the net radiative heating is largest in the tropics and that surplus energy is redistributed by the circulations of oceans and atmospheres. Moreover, a large number of clouds are formed by deep convection and convergence of water vapor. Thus, it is very important to understand the radiative energy balance of the tropics and the effect of clouds on the radiation field. For mixed-phase clouds, error analyses pertaining to the inference of effective particle sizes and optical thicknesses are performed. Errors are calculated with respect to the assumption of a cloud containing solely liquid or ice phase particles. The analyses suggest that the effective particle size inferred for a mixed-phase cloud can be underestimated (or overestimated) if a pure liquid phase (or pure ice phase) is assumed for the cloud, whereas the corresponding cloud optical thickness can be overestimated (or underestimated). The analyses of optical depth and fraction of occurrence for thin cirrus clouds showed that about 40% of pixels flagged as clear-sky contain detectible thin cirrus clouds. The regions of high occurrence and large optical depth located around deep convection showed seasonal variations. The thin cirrus clouds occur more frequently with larger optical depth in the northern (southern) hemisphere during spring and summer (autumn and winter). The net cloud radiative forcing by thin cirrus clouds is positive at the top of atmosphere and is negative at the bottom of atmosphere. The difference in OLR between measurement and model is 4.2 Wm-2 for September 2005. The difference is smaller in moist regions and larger in drier regions. OLR increases with increasing surface temperatures up to 300 K but decreases at surface temperatures larger than 300 K due to the strong absorption of increased water vapor. In summary, if the surface temperature is lower than the threshold of convection (300 K), temperature is a dominant factor in OLR and if the surface temperature is larger than 300 K, OLR is strongly influenced by water vapor.
dc.identifier.urihttp://hdl.handle.net/1969.1/ETD-TAMU-1897
dc.language.isoen_US
dc.subjectcirrus
dc.subjectOLR
dc.subjectraiative impacts
dc.titleMixed-phase clouds, thin cirrus clouds, and OLR over the tropics: observations, retrievals, and radiative impacts
dc.typeBook
dc.typeThesis

Files

Collections