Articles | Volume 9, issue 1
https://doi.org/10.5194/amt-9-9-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/amt-9-9-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The microwave properties of simulated melting precipitation particles: sensitivity to initial melting
University of Maryland Baltimore County, Joint Center for Earth Systems Technology, Baltimore, MD, USA
NASA Goddard Space Flight Center, Code 612, Greenbelt, MD, USA
W. S. Olson
University of Maryland Baltimore County, Joint Center for Earth Systems Technology, Baltimore, MD, USA
NASA Goddard Space Flight Center, Code 612, Greenbelt, MD, USA
G. Skofronick-Jackson
NASA Goddard Space Flight Center, Code 612, Greenbelt, MD, USA
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Cited
17 citations as recorded by crossref.
- 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
- Cautious note on using the discrete dipole approximation for inhomogeneous, spherical scatterers with high optical contrast F. Kanngießer & P. Eriksson 10.1364/OL.463561
- SLALOM: An All-Surface Snow Water Path Retrieval Algorithm for the GPM Microwave Imager J. Rysman et al. 10.3390/rs10081278
- A Machine Learning Snowfall Retrieval Algorithm for ATMS P. Sanò et al. 10.3390/rs14061467
- The GPM Combined Algorithm M. Grecu et al. 10.1175/JTECH-D-16-0019.1
- Radiowave Scattering Characteristics of Melting Layer Measured by a Dual Ka-band Radar System K. NAKAMURA et al. 10.2151/jmsj.2021-053
- The State of Precipitation Measurements at Mid-to-High Latitudes L. Milani & C. Kidd 10.3390/atmos14111677
- Melting Layer Attenuation at Ka‐ and W‐Bands as Derived From Multifrequency Radar Doppler Spectra Observations H. Li & D. Moisseev 10.1029/2019JD030316
- Validation of Microphysical Snow Models Using In Situ, Multifrequency, and Dual‐Polarization Radar Measurements in Finland J. Tyynelä & A. von Lerber 10.1029/2019JD030721
- Two Layers of Melting Ice Particles Within a Single Radar Bright Band: Interpretation and Implications H. Li & D. Moisseev 10.1029/2020GL087499
- Effect of Particle Shape, Density, and Inhomogeneity on the Microwave Optical Properties of Graupel and Hailstones G. Tang et al. 10.1109/TGRS.2017.2726994
- Bulk hydrometeor optical properties for microwave and sub-millimetre radiative transfer in RTTOV-SCATT v13.0 A. Geer et al. 10.5194/gmd-14-7497-2021
- Impacts of Shape Assumptions on Z–R Relationship and Satellite Remote Sensing Clouds Based on Model Simulations and GPM Observations L. Mai et al. 10.3390/rs15061556
- Estimation of Melting-Layer Cooling Rate from Dual-Polarization Radar: Spectral Bin Model Simulations J. Carlin & A. Ryzhkov 10.1175/JAMC-D-18-0343.1
- Evaluation of Higher‐Order Quadrature Schemes in Improving Computational Efficiency for Orientation‐Averaged Single‐Scattering Properties of Nonspherical Ice Particles I. Fenni et al. 10.1029/2020JD034172
- Snowflake Melting Simulation Using Smoothed Particle Hydrodynamics J. Leinonen & A. von Lerber 10.1002/2017JD027909
- A general database of hydrometeor single scattering properties at microwave and sub-millimetre wavelengths P. Eriksson et al. 10.5194/essd-10-1301-2018
17 citations as recorded by crossref.
- 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
- Cautious note on using the discrete dipole approximation for inhomogeneous, spherical scatterers with high optical contrast F. Kanngießer & P. Eriksson 10.1364/OL.463561
- SLALOM: An All-Surface Snow Water Path Retrieval Algorithm for the GPM Microwave Imager J. Rysman et al. 10.3390/rs10081278
- A Machine Learning Snowfall Retrieval Algorithm for ATMS P. Sanò et al. 10.3390/rs14061467
- The GPM Combined Algorithm M. Grecu et al. 10.1175/JTECH-D-16-0019.1
- Radiowave Scattering Characteristics of Melting Layer Measured by a Dual Ka-band Radar System K. NAKAMURA et al. 10.2151/jmsj.2021-053
- The State of Precipitation Measurements at Mid-to-High Latitudes L. Milani & C. Kidd 10.3390/atmos14111677
- Melting Layer Attenuation at Ka‐ and W‐Bands as Derived From Multifrequency Radar Doppler Spectra Observations H. Li & D. Moisseev 10.1029/2019JD030316
- Validation of Microphysical Snow Models Using In Situ, Multifrequency, and Dual‐Polarization Radar Measurements in Finland J. Tyynelä & A. von Lerber 10.1029/2019JD030721
- Two Layers of Melting Ice Particles Within a Single Radar Bright Band: Interpretation and Implications H. Li & D. Moisseev 10.1029/2020GL087499
- Effect of Particle Shape, Density, and Inhomogeneity on the Microwave Optical Properties of Graupel and Hailstones G. Tang et al. 10.1109/TGRS.2017.2726994
- Bulk hydrometeor optical properties for microwave and sub-millimetre radiative transfer in RTTOV-SCATT v13.0 A. Geer et al. 10.5194/gmd-14-7497-2021
- Impacts of Shape Assumptions on Z–R Relationship and Satellite Remote Sensing Clouds Based on Model Simulations and GPM Observations L. Mai et al. 10.3390/rs15061556
- Estimation of Melting-Layer Cooling Rate from Dual-Polarization Radar: Spectral Bin Model Simulations J. Carlin & A. Ryzhkov 10.1175/JAMC-D-18-0343.1
- Evaluation of Higher‐Order Quadrature Schemes in Improving Computational Efficiency for Orientation‐Averaged Single‐Scattering Properties of Nonspherical Ice Particles I. Fenni et al. 10.1029/2020JD034172
- Snowflake Melting Simulation Using Smoothed Particle Hydrodynamics J. Leinonen & A. von Lerber 10.1002/2017JD027909
- A general database of hydrometeor single scattering properties at microwave and sub-millimetre wavelengths P. Eriksson et al. 10.5194/essd-10-1301-2018
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Latest update: 31 Aug 2024
Short summary
This research explores, through simulations, how a realistically shaped snowflake aggregate begins the melting process and how microwave-based satellite observations are sensitive to those initial stages of melting. Using highly detailed physical models, and high-precision numerical models, we can accurately simulate the sensitivity of observations to this critical transition from dry snow to melting snow. This research improves on existing models, providing an accurate measurement basis.
This research explores, through simulations, how a realistically shaped snowflake aggregate...