Active Raman sounding of the earth's water vapor field.
The typically weak cross-sections characteristic of Raman processes has historically limited their use in atmospheric remote sensing to nighttime application. However, with advances in instrumentation and techniques, it is now possible to apply Raman lidar to the monitoring of atmospheric water vapor, aerosols and clouds throughout the diurnal cycle. Upper tropospheric and lower stratospheric measurements of water vapor using Raman lidar are also possible but are limited to nighttime and require long integration times. However, boundary layer studies of water vapor variability can now be performed with high temporal and spatial resolution. This paper will review the current state-of-the-art of Raman lidar for high-resolution measurements of the atmospheric water vapor, aerosol and cloud fields. In particular, we describe the use of Raman lidar for mapping the vertical distribution and variability of atmospheric water vapor, aerosols and clouds throughout the evolution of dynamic meteorological events. The ability of Raman lidar to detect and characterize water in the region of the tropopause and the importance of high-altitude water vapor for climate-related studies and meteorological satellite performance are discussed.
Tratt
David M
DM
NASA Earth Science Technology Office, Greenbelt, MD 20771, USA. dtratt@esto.gsfc.nasa.gov
Whiteman
David N
DN
Demoz
Belay B
BB
Farley
Robert W
RW
Wessel
John E
JE
D000531:Altitude; D018534:Earth, Planet; D008685:Meteorological Concepts; D013059:Spectrum Analysis, Raman; D014867:Water / Q000737:chemistry*
D014867:Water