We studied a method to retrieve the optical thickness and effective particle radius of water clouds using the split-window
channels and the 8.7-μm channel of Meteosat-8. Valid ranges are approximately from 1 to 9 for optical thickness and
smaller than 18 micron for effective particle radius. The retrieval used the brightness temperature (TBB) and brightness
temperature difference (BTD) between the split windows, as computed with the radiation code RSTAR5b for various
properties of water clouds and vertical profiles of temperature and water vapor. The retrieved cloud parameters were then
compared to those retrieved by the solar reflection method, which employs the 0.6-, 3.9-, and 11- μm channels of
Meteosat-8. Comparison between the two methods revealed that the split-window technique could capture spatial
features for both optical thickness and effective particle radius. The BTD is a good indicator for optical thickness. The
diurnal variation of BTD shows the minimum value (thickest) before sunrise. Further precipitation and optical depth
estimated from TMI/TRMM are compared with optical properties.
Access to the requested content is limited to institutions that have purchased or subscribe to SPIE eBooks.
You are receiving this notice because your organization may not have SPIE eBooks access.*
*Shibboleth/Open Athens users─please
sign in
to access your institution's subscriptions.
To obtain this item, you may purchase the complete book in print or electronic format on
SPIE.org.
INSTITUTIONAL Select your institution to access the SPIE Digital Library.
PERSONAL Sign in with your SPIE account to access your personal subscriptions or to use specific features such as save to my library, sign up for alerts, save searches, etc.