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.
Research article
| 
23 Feb 2017
Research article |
| 23 Feb 2017
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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- Advances in Atmospheric Radiation: Theories, Models, and Their Applications. Part II: Radiative Transfer Models and Related Applications H. Zhang et al. 10.1007/s13351-024-3089-y
- High-altitude demonstration of LWIR polarimetry using uncooled microbolometers K. Shanks et al. 10.1016/j.jqsrt.2023.108872
- The Characteristics of Precipitation with and without Bright Band in Summer Tibetan Plateau and Central-Eastern China L. Yang et al. 10.3390/rs16193703
- Global monitoring of deep convection using passive microwave observations J. Rysman et al. 10.1016/j.atmosres.2020.105244
- Nonparametric Methodology to Estimate Precipitating Ice from Multiple-Frequency Radar Reflectivity Observations M. Grecu et al. 10.1175/JAMC-D-18-0036.1
- Microwave and submillimeter wave scattering of oriented ice particles M. Brath et al. 10.5194/amt-13-2309-2020
- CoSMIR Performance During the GPM OLYMPEX Campaign R. Kroodsma et al. 10.1109/TGRS.2019.2906039
- 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
- Using passive and active observations at microwave and sub-millimetre wavelengths to constrain ice particle models R. Ekelund et al. 10.5194/amt-13-501-2020
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- Airborne validation of radiative transfer modelling of ice clouds at millimetre and sub-millimetre wavelengths S. Fox et al. 10.5194/amt-12-1599-2019
- 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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- Towards variational retrieval of warm rain from passive microwave observations D. Duncan et al. 10.5194/amt-11-4389-2018
- 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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- Sensitivity of 89–190-GHz Microwave Observations to Ice Particle Scattering R. Chen & R. Bennartz 10.1175/JAMC-D-19-0293.1
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- CloudSat snowfall estimates over Antarctica and the Southern Ocean: An assessment of independent retrieval methodologies and multi-year snowfall analysis L. Milani et al. 10.1016/j.atmosres.2018.05.015
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- The Global Precipitation Measurement (GPM) mission's scientific achievements and societal contributions: reviewing four years of advanced rain and snow observations G. Skofronick‐Jackson et al. 10.1002/qj.3313
- CloudSat-Based Assessment of GPM Microwave Imager Snowfall Observation Capabilities G. Panegrossi et al. 10.3390/rs9121263
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- Representing Precipitation Ice Species With Both Spherical and Nonspherical Particles for Radiative Transfer Modeling of Microphysics‐Consistent Cloud Microwave Scattering Properties S. Sieron et al. 10.1002/2017MS001226
- A general database of hydrometeor single scattering properties at microwave and sub-millimetre wavelengths P. Eriksson et al. 10.5194/essd-10-1301-2018
Latest update: 20 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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