The impact of the melting layer on the passive microwave cloud scattering signal observed from satellites: A study using TRMM microwave passive and active measurements

Author:

Galligani V. S.1,Prigent C.1,Defer E.1,Jimenez C.1,Eriksson P.2

Affiliation:

1. Laboratoire d'Etudes du Rayonnement et de la Matière en Astro-physique (LERMA), Centre National de la Recherche Scientifique; Observatoire de Paris; Paris France

2. Department of Earth and Space Sciences; Chalmers University of Technology; Gothenburg Sweden

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Reference50 articles.

1. Armstrong , R. L. M. J. Brodzik 2005 Northern hemisphere EASE-grid weekly snow cover and sea ice extent version 3 (Boulder, CO: National snow and ice data center, Digital Media) http://nsidc.org/data/nsidc-0046. html

2. Rain type classification algorithm for TRMM precipitation radar;Awaka;Geoscience and Remote Sensing, 1997. IGARSS'97. Remote Sensing-A Scientific Vision for Sustainable Development,1997

3. Constraining microwave brightness temperatures by radar bright band observations;Battaglia;J. Atmos. Oceanic Technol.,2003

4. The effect of the melting layer on the microwave emission of clouds over the ocean;Bauer;J. Atmos. Sci.,1999

5. Combined cloud-microwave radiative transfer modeling of stratiform rainfall;Bauer;J. Atmos. Sci.,2000

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