Temperature‐Dependent Optical Properties of Ice Crystals in the Far‐Infrared Regime

Abstract A database of temperature‐dependent hexagonal ice aggregate optical properties in the far‐infrared (FIR) spectrum is developed to support FIR missions, particularly the current Polar Radiant Energy in the Far InfraRed Experiment and the upcoming Far‐infrared‐Outgoing‐Radiation Understanding and Monitoring. Based on this data set, simulations of the brightness temperatures (BTs) in the 100–667 cm −1 FIR region are conducted for an anvil‐like ice cloud in a tropical atmosphere. The results show nonnegligible impact of ice cloud temperature on simulated BTs, which can be as large as 3 K due to the difference between fixed 160 or 270 K cloud temperature and the benchmark counterpart, varying in accordance with the ambient temperature profile for a cloud residing between 249.6 and 199.6 K. To enhance the accuracy of FIR radiative transfer modeling, it is recommended to incorporate temperature‐dependent optical properties of ice clouds.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-06-18
DOI
https://doi.org/10.1029/2025gl116735
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
0.00

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article

Temperature‐Dependent Optical Properties of Ice Crystals in the Far‐Infrared Regime

Helen Brindley, Ping Xian Yang, Tristan L’Ecuyer, Tiziano Maestri et al.
Geophysical Research Letters
Atmospheric aerosols and clouds
article

Temperature‐Dependent Optical Properties of Ice Crystals in the Far‐Infrared Regime

Helen Brindley, Ping Xian Yang, Tristan L’Ecuyer, Tiziano Maestri, Tong Ren
article en

Abstract

Abstract A database of temperature‐dependent hexagonal ice aggregate optical properties in the far‐infrared (FIR) spectrum is developed to support FIR missions, particularly the current Polar Radiant Energy in the Far InfraRed Experiment and the upcoming Far‐infrared‐Outgoing‐Radiation Understanding and Monitoring. Based on this data set, simulations of the brightness temperatures (BTs) in the 100–667 cm −1 FIR region are conducted for an anvil‐like ice cloud in a tropical atmosphere. The results show nonnegligible impact of ice cloud temperature on simulated BTs, which can be as large as 3 K due to the difference between fixed 160 or 270 K cloud temperature and the benchmark counterpart, varying in accordance with the ambient temperature profile for a cloud residing between 249.6 and 199.6 K. To enhance the accuracy of FIR radiative transfer modeling, it is recommended to incorporate temperature‐dependent optical properties of ice clouds.

Geophysical Research LettersVol. 52(12)
University of Wisconsin–Madison (US), National Centre for Earth Observation (GB), Imperial College London (GB), Texas A&M University (US), University of Bologna (IT)
National Aeronautics and Space Administration
Affordable and clean energy
Openalex Percentile: Top 86%
Atmospheric aerosols and clouds
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