Ukrainian Antarctic Journal

Vol 21 No 2(27) (2023): Ukrainian Antarctic Journal
Articles

Variability of extreme precipitation in West Antarctica and its response to the Amundsen Sea Low changes

L. Pysarenko
Ukrainian Hydrometeorological Institute of the State Emergency Service of Ukraine and the National Academy of Sciences of Ukraine, Kyiv, 03028, Ukraine; State Institution National Antarctic Scientific Center of the Ministry of Education and Science of Ukraine, Kyiv, 01601, Ukraine
D. Pishniak
State Institution National Antarctic Scientific Center of the Ministry of Education and Science of Ukraine, Kyiv, 01601, Ukraine
M. Savenets
Ukrainian Hydrometeorological Institute of the State Emergency Service of Ukraine and the National Academy of Sciences of Ukraine, Kyiv, 03028, Ukraine
Spectrograms of the signal emitted from Vernadsky and received onboard RV Noosfera after reflection from the ionosphere, the black line shows the X component of the geomagnetic field measured at the Vernadsky AIA station. See paper Zalizovski et al. 2024 (page 195). Photo by S. Glotov and from the archive of the SI NASC
Published December 31, 2023
Keywords
  • atmospheric pressure,
  • glacier basin,
  • ice shelf,
  • precipitation,
  • 95th percentile of precipitation
How to Cite
Pysarenko, L., Pishniak, D., & Savenets, M. (2023). Variability of extreme precipitation in West Antarctica and its response to the Amundsen Sea Low changes. Ukrainian Antarctic Journal, 21(2(27), 175-189. https://doi.org/10.33275/1727-7485.2.2023.716

Abstract

Changes in precipitation extremes over West Antarctica and the Antarctic Peninsula belong to the observed consequences of current climate change. We discuss the spatio-temporal patterns of extreme precipitation and their relationships with the Amundsen Sea Low (ASL) parameters. Based on the ERA5 reanalysis data, the 95th percentile of daily precipitation totals was estimated and linked to the ASL parameters over the main glacier basins in the region. The 95th percentile of precipitation varied from 5 mm to over 40 mm over the region, showing higher values along the coastline and reaching the maximum over the west coast of the Antarctic Peninsula. The tendencies of extreme precipitation vary from –3 to 4 mm per decade and enhance the observed spatial distribution differences. On average, extreme precipitation events covered 4.7–4.9% of the basins’ area. All dependencies had a well-detected seasonality. Both total and extreme precipitation varied under the ASL fluctuations, showing significant average-to-strong correlations. The ASL shifts to the west caused a decrease in precipitation over the Amundsen Sea and an increase over the Antarctic Peninsula. The ASL deepening (lower atmospheric pressure of the system) resulted in a precipitation decrease over the Getz Ice Shelf and a precipitation increase over the western part of the Antarctic Peninsula. There are two regions with opposite responses of precipitation to the ASL changes: the western part over the Getz Ice Shelf with nearby marine areas, and the eastern part covering the Antarctic Peninsula, Pine Island glaciers, the Abbot Ice Shelf, and the Bellingshausen Sea. The obtained results are crucial for our understanding of extreme precipitation occurrences over West Antarctica in recent decades under climate change.

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