Local spatial variability in the occurrence of summer precipitation in the Sør Rondane Mountains, Antarctica

During the austral summer 2019/2020, three vertically pointing K-band Doppler profilers (Micro Rain Radar PRO, MRR-PRO) were deployed along a transect across the Sør Rondane Mountains, directly south of the scientific base Princess Elisabeth Antarctica. The MRR-PRO devices were placed at locations c...

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Main Authors: Ferrone, Alfonso, Vignon, Étienne, Zonato, Andrea, Berne, Alexis
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-490
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-490/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere110224 2023-12-24T10:09:50+01:00 Local spatial variability in the occurrence of summer precipitation in the Sør Rondane Mountains, Antarctica Ferrone, Alfonso Vignon, Étienne Zonato, Andrea Berne, Alexis 2023-11-24 application/pdf https://doi.org/10.5194/egusphere-2023-490 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-490/ eng eng doi:10.5194/egusphere-2023-490 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-490/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-490 2023-11-27T17:24:18Z During the austral summer 2019/2020, three vertically pointing K-band Doppler profilers (Micro Rain Radar PRO, MRR-PRO) were deployed along a transect across the Sør Rondane Mountains, directly south of the scientific base Princess Elisabeth Antarctica. The MRR-PRO devices were placed at locations corresponding to different stages of the interaction between the complex terrain and the typical flow associated with precipitating systems. The radar measurements, alongside information from the ERA5 reanalysis and a set of high-resolution Weather Research and Forecasting (WRF) simulations, have been used to study the spatial variability in snowfall across the transect. Radar observations reveal differences in the frequency of occurrence of virga and surface precipitation above the transect. An analysis of the WRF outputs reveals the presence of a relatively dry layer above the radar locations, reaching a constant altitude of 3.5 km above mean sea level. Due to the complex terrain, the depth of the layer varies across the transect, affecting sublimation and the occurrence of virgae. Combined information from the ERA5 reanalysis, the WRF simulations, and ground-level measurements suggests that orographic lifting enhances precipitation above the highest mountain peaks. Finally, the analysis of the succession of virga and surface precipitation above the sites shows that, in most cases, they represent different stages of the same large-scale events. This study reveals the significant spatial variability in the occurrence of precipitation in a region of complex terrain, emphasizing the importance of collecting snowfall measurements in the mountainous regions of the Antarctic continent. Text Antarc* Antarctic Antarctica Copernicus Publications: E-Journals Antarctic Austral Sør Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) Sør-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) The Antarctic
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description During the austral summer 2019/2020, three vertically pointing K-band Doppler profilers (Micro Rain Radar PRO, MRR-PRO) were deployed along a transect across the Sør Rondane Mountains, directly south of the scientific base Princess Elisabeth Antarctica. The MRR-PRO devices were placed at locations corresponding to different stages of the interaction between the complex terrain and the typical flow associated with precipitating systems. The radar measurements, alongside information from the ERA5 reanalysis and a set of high-resolution Weather Research and Forecasting (WRF) simulations, have been used to study the spatial variability in snowfall across the transect. Radar observations reveal differences in the frequency of occurrence of virga and surface precipitation above the transect. An analysis of the WRF outputs reveals the presence of a relatively dry layer above the radar locations, reaching a constant altitude of 3.5 km above mean sea level. Due to the complex terrain, the depth of the layer varies across the transect, affecting sublimation and the occurrence of virgae. Combined information from the ERA5 reanalysis, the WRF simulations, and ground-level measurements suggests that orographic lifting enhances precipitation above the highest mountain peaks. Finally, the analysis of the succession of virga and surface precipitation above the sites shows that, in most cases, they represent different stages of the same large-scale events. This study reveals the significant spatial variability in the occurrence of precipitation in a region of complex terrain, emphasizing the importance of collecting snowfall measurements in the mountainous regions of the Antarctic continent.
format Text
author Ferrone, Alfonso
Vignon, Étienne
Zonato, Andrea
Berne, Alexis
spellingShingle Ferrone, Alfonso
Vignon, Étienne
Zonato, Andrea
Berne, Alexis
Local spatial variability in the occurrence of summer precipitation in the Sør Rondane Mountains, Antarctica
author_facet Ferrone, Alfonso
Vignon, Étienne
Zonato, Andrea
Berne, Alexis
author_sort Ferrone, Alfonso
title Local spatial variability in the occurrence of summer precipitation in the Sør Rondane Mountains, Antarctica
title_short Local spatial variability in the occurrence of summer precipitation in the Sør Rondane Mountains, Antarctica
title_full Local spatial variability in the occurrence of summer precipitation in the Sør Rondane Mountains, Antarctica
title_fullStr Local spatial variability in the occurrence of summer precipitation in the Sør Rondane Mountains, Antarctica
title_full_unstemmed Local spatial variability in the occurrence of summer precipitation in the Sør Rondane Mountains, Antarctica
title_sort local spatial variability in the occurrence of summer precipitation in the sør rondane mountains, antarctica
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-490
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-490/
long_lat ENVELOPE(25.000,25.000,-72.000,-72.000)
ENVELOPE(25.000,25.000,-72.000,-72.000)
geographic Antarctic
Austral
Sør Rondane Mountains
Sør-Rondane
The Antarctic
geographic_facet Antarctic
Austral
Sør Rondane Mountains
Sør-Rondane
The Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-490
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-490/
op_doi https://doi.org/10.5194/egusphere-2023-490
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