Articles | Volume 17, issue 4
https://doi.org/10.5194/acp-17-2741-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-2741-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Microphysical properties of frozen particles inferred from Global Precipitation Measurement (GPM) Microwave Imager (GMI) polarimetric measurements
Universities Space Research Association, Columbia, MD, USA
Climate and Radiation Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Dong L. Wu
Climate and Radiation Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
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- Microwave and submillimeter wave scattering of oriented ice particles M. Brath et al. 10.5194/amt-13-2309-2020
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- A Prognostic Nested k-Nearest Approach for Microwave Precipitation Phase Detection over Snow Cover Z. Takbiri et al. 10.1175/JHM-D-18-0021.1
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- Angular-Dependent Polarized Characteristics of Surface Emissivity at 150 GHz Over Saharan and Taklimakan Deserts X. Xie et al. 10.1109/TGRS.2022.3195206
- First results from an uncooled LWIR polarimeter for cubesat deployment K. Hart et al. 10.1117/1.OE.59.7.075103
- Satellites See the World’s Atmosphere S. Ackerman et al. 10.1175/AMSMONOGRAPHS-D-18-0009.1
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- A Comprehensive Machine Learning Study to Classify Precipitation Type over Land from Global Precipitation Measurement Microwave Imager (GPM-GMI) Measurements S. Das et al. 10.3390/rs14153631
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Latest update: 08 Nov 2024
Short summary
Under certain temperature or aerodynamic conditions, ice crystals prefer to orient along certain directions. The preferred orientation direction of non-spherical ice particles would result in a difference in the satellite remote sensing using different polarized channels. This paper studies this polarization difference using the Global Precipitation Measurement Microwave Imager, where we can infer the dominant ice particle orientation and shape factors from passive remote sensing measures.
Under certain temperature or aerodynamic conditions, ice crystals prefer to orient along certain...
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