Analysis of the Global Microwave Polarization Data of Clouds
| Autor: | Lin Tian, Gail Skofronick-Jackson, Xiping Zeng, Rachael Kroodsma, Amber E. Emory, William S. Olson |
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| Rok vydání: | 2018 |
| Předmět: |
Atmospheric Science
Conical scanning Radiometer 010504 meteorology & atmospheric sciences Ice crystals 010502 geochemistry & geophysics Numerical weather prediction 01 natural sciences Physics::Geophysics law.invention Lidar law Climatology Astrophysics::Earth and Planetary Astrophysics Radar Global Precipitation Measurement Astrophysics::Galaxy Astrophysics Physics::Atmospheric and Oceanic Physics Geology Microwave 0105 earth and related environmental sciences Remote sensing |
| Zdroj: | Journal of Climate. 32:3-13 |
| ISSN: | 1520-0442 0894-8755 |
| DOI: | 10.1175/jcli-d-18-0293.1 |
| Popis: | Information about the characteristics of ice particles in clouds is necessary for improving our understanding of the states, processes, and subsequent modeling of clouds and precipitation for numerical weather prediction and climate analysis. Two NASA passive microwave radiometers, the satellite-borne Global Precipitation Measurement (GPM) Microwave Imager (GMI) and the aircraft-borne Conical Scanning Millimeter-Wave Imaging Radiometer (CoSMIR), measure vertically and horizontally polarized microwaves emitted by clouds (including precipitating particles) and Earth’s surface below. In this paper, GMI (or CoSMIR) data are analyzed with CloudSat (or aircraft-borne radar) data to find polarized difference (PD) signals not affected by the surface, thereby obtaining the information on ice particles. Statistical analysis of 4 years of GMI and CloudSat data, for the first time, reveals that optically thick clouds contribute positively to GMI PD at 166 GHz over all the latitudes and their positive magnitude of 166-GHz GMI PD varies little with latitude. This result suggests that horizontally oriented ice crystals in thick clouds are common from the tropics to high latitudes, which contrasts the result of Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) that horizontally oriented ice crystals are rare in optically thin ice clouds. |
| Databáze: | OpenAIRE |
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