The impact of temperature errors on perceived humidity supersaturation

Details The impact of temperature errors on perceived humidity supersaturation The impact of temperature errors on perceived humidity supersaturation

Jul 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30qsc11b&link_type=abstract

Geophysical Research Letters, Volume 30, Issue 14, pp. ASC 11-1, CiteID 1759, DOI 10.1029/2003GL017691

Computer Science

Sound

4

Global Change: Remote Sensing, Global Change: Water Cycles (1836), Global Change: Instruments And Techniques, Meteorology And Atmospheric Dynamics: General Or Miscellaneous

Scientific paper

A Monte Carlo method is used to study the propagation of temperature uncertainties into relative humidity with respect to ice (RH i ) calculated from specific humidity. For a flat specific humidity distribution and Gaussian temperature uncertainties the resulting RH i distribution drops exponentially at high RH i values-much slower than a Gaussian. This agrees well with the RH i distribution measured by the Microwave Limb Sounder (MLS), which means that such remotely measured RH i distributions can be explained, at least partly, by temperature uncertainties.

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