Brief communication: Two-year MRR observations at Great Wall Station, Antarctic Peninsula region

Abstract. We report a two-year record (March 2024–February 2026) of Micro Rain Radar (MRR) observations at Great Wall Station in the Antarctic Peninsula region. After quality control, near-surface precipitation and snowfall were identified during 32 % and 21 % of the observation time, respectively. Median snowfall radar reflectivity is approximately 9 dBZ and exhibits minimal variation with height, likely due to frequent shallow snowfall. Strong winds are associated with reduced low-level median radar reflectivity below approximately 1 km. We further developed a localized Ze (equivalent radar reflectivity) – S (snowfall rate) parameterization and identified systematic underestimation of cumulative snowfall profiles in ERA5 products.

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Publication Details

Journal
˜The œcryosphere
Published
2026-07-23
DOI
https://doi.org/10.5194/tc-20-4049-2026
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
0.00

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Brief communication: Two-year MRR observations at Great Wall Station, Antarctic Peninsula region

Minghu Ding, Haoran Li, Junmei Lü, Biao Tian et al.
˜The œcryosphere
Cryospheric studies and observations
article

Brief communication: Two-year MRR observations at Great Wall Station, Antarctic Peninsula region

Minghu Ding, Haoran Li, Junmei Lü, Biao Tian, Jiayi Sun, Wenqian Zhang
article en

Abstract

Abstract. We report a two-year record (March 2024–February 2026) of Micro Rain Radar (MRR) observations at Great Wall Station in the Antarctic Peninsula region. After quality control, near-surface precipitation and snowfall were identified during 32 % and 21 % of the observation time, respectively. Median snowfall radar reflectivity is approximately 9 dBZ and exhibits minimal variation with height, likely due to frequent shallow snowfall. Strong winds are associated with reduced low-level median radar reflectivity below approximately 1 km. We further developed a localized Ze (equivalent radar reflectivity) – S (snowfall rate) parameterization and identified systematic underestimation of cumulative snowfall profiles in ERA5 products.

˜The œcryosphereVol. 20(7)
Ministry of Education (CL), Chinese Academy of Meteorological Sciences (CN)
National Natural Science Foundation of China, Chinese Academy of Meteorological Sciences
Openalex Percentile: Top 12%
Cryospheric studies and observations
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