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Please use this identifier to cite or link to this item: http://hdl.handle.net/2014/40384

Title: Biases in total precipitable water vapor climatologies from Atmospheric Infrared Sounder and Advanced Microwave Scanning Radiometer
Authors: Fetzer, Eric J.
Lambrigtsen, Bjorn H.
Eldering, Annmarie
Aumann, Hartmut H.
Chahine, Moustafa T.
Keywords: remote sounding
water vapor
Atmospheric Infrared Sounder (AIRS)
validation
clouds
Issue Date: 26-Apr-2006
Publisher: American Geophysical Union
Citation: Journal Of Geophysical Research, Vol. 111, D09S16, doi:10.1029/2005JD006598, 2006
Abstract: We examine differences in total precipitable water vapor (PWV) from the Atmospheric Infrared Sounder (AIRS) and the Advanced Microwave Scanning Radiometer (AMSR-E) experiments sharing the Aqua spacecraft platform. Both systems provide estimates of PWV over water surfaces. We compare AIRS and AMSR-E PWV to constrain AIRS retrieval uncertainties as functions of AIRS retrieved infrared cloud fraction. PWV differences between the two instruments vary only weakly with infrared cloud fraction up to about 70%. Maps of AIRS-AMSR-E PWV differences vary with location and season. Observational biases, when both instruments observe identical scenes, are generally less than 5%. Exceptions are in cold air outbreaks where AIRS is biased moist by 10–20% or 10–60% (depending on retrieval processing) and at high latitudes in winter where AIRS is dry by 5–10%. Sampling biases, from different sampling characteristics of AIRS and AMSR-E, vary in sign and magnitude. AIRS sampling is dry by up to 30% in most high-latitude regions but moist by 5–15% in subtropical stratus cloud belts. Over the northwest Pacific, AIRS samples conditions more moist than AMSR-E by a much as 60%. We hypothesize that both wet and dry sampling biases are due to the effects of clouds on the AIRS retrieval methodology. The sign and magnitude of these biases depend upon the types of cloud present and on the relationship between clouds and PWV. These results for PWV imply that climatologies of height-resolved water vapor from AIRS must take into consideration local meteorological processes affecting AIRS sampling.
URI: http://hdl.handle.net/2014/40384
Appears in Collections:JPL TRS 1992+

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