Revisiting temperature sensitivity: How does Antarctic precipitation change with temperature?

With progressing global warming, snowfall in Antarctica is expected to increase, which could counteract or even temporarily overcompensate ice-sheet mass losses through increased ice discharge, calving and melting. For sea-level projections it is therefore vital to understand the processes determini...

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Main Authors: Nicola, Lena, Notz, Dirk, Winkelmann, Ricarda
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-2022-254
https://tc.copernicus.org/preprints/tc-2022-254/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd108477 2023-05-15T13:38:41+02:00 Revisiting temperature sensitivity: How does Antarctic precipitation change with temperature? Nicola, Lena Notz, Dirk Winkelmann, Ricarda 2023-01-02 application/pdf https://doi.org/10.5194/tc-2022-254 https://tc.copernicus.org/preprints/tc-2022-254/ eng eng doi:10.5194/tc-2022-254 https://tc.copernicus.org/preprints/tc-2022-254/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-2022-254 2023-01-09T17:22:43Z With progressing global warming, snowfall in Antarctica is expected to increase, which could counteract or even temporarily overcompensate ice-sheet mass losses through increased ice discharge, calving and melting. For sea-level projections it is therefore vital to understand the processes determining snowfall changes in Antarctica. Here we revisit the relationship between Antarctic temperature changes and precipitation changes, identifying and explaining regional differences and deviations from the theoretical approach based on the Clausius-Clapeyron relationship. Analysing the latest estimates from global (CMIP6) and regional (RACMO2.3) model projections, we find an average increase of 5.5 % in annual precipitation over Antarctica per degree of warming, with a minimum sensitivity of 2 % K -1 near Siple Coast, and a maximum sensitivity > 10 % K -1 at the East Antarctic Plateau region. This large range can be explained by the prevailing climatic conditions, with local temperatures determining the Clausius-Clapeyron sensitivity that is counteracted in some regions by the prevalence of the coastal wind regime. We compare different approaches of deriving the sensitivity factor, which in some cases can lead to sensitivity changes of up to 7 % for the same model. Importantly, local sensitivity-factors are found to be strongly dependent on the warming level, suggesting that some ice-sheet models which base their precipitation estimates on parameterizations derived from these sensitivity factors might overestimate warming-induced snowfall changes, particularly in high-emission scenarios. This would have consequences for Antarctic sea-level projections for this century and beyond. Text Antarc* Antarctic Antarctica Ice Sheet Copernicus Publications: E-Journals Antarctic Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917) Siple Coast ENVELOPE(-155.000,-155.000,-82.000,-82.000)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description With progressing global warming, snowfall in Antarctica is expected to increase, which could counteract or even temporarily overcompensate ice-sheet mass losses through increased ice discharge, calving and melting. For sea-level projections it is therefore vital to understand the processes determining snowfall changes in Antarctica. Here we revisit the relationship between Antarctic temperature changes and precipitation changes, identifying and explaining regional differences and deviations from the theoretical approach based on the Clausius-Clapeyron relationship. Analysing the latest estimates from global (CMIP6) and regional (RACMO2.3) model projections, we find an average increase of 5.5 % in annual precipitation over Antarctica per degree of warming, with a minimum sensitivity of 2 % K -1 near Siple Coast, and a maximum sensitivity > 10 % K -1 at the East Antarctic Plateau region. This large range can be explained by the prevailing climatic conditions, with local temperatures determining the Clausius-Clapeyron sensitivity that is counteracted in some regions by the prevalence of the coastal wind regime. We compare different approaches of deriving the sensitivity factor, which in some cases can lead to sensitivity changes of up to 7 % for the same model. Importantly, local sensitivity-factors are found to be strongly dependent on the warming level, suggesting that some ice-sheet models which base their precipitation estimates on parameterizations derived from these sensitivity factors might overestimate warming-induced snowfall changes, particularly in high-emission scenarios. This would have consequences for Antarctic sea-level projections for this century and beyond.
format Text
author Nicola, Lena
Notz, Dirk
Winkelmann, Ricarda
spellingShingle Nicola, Lena
Notz, Dirk
Winkelmann, Ricarda
Revisiting temperature sensitivity: How does Antarctic precipitation change with temperature?
author_facet Nicola, Lena
Notz, Dirk
Winkelmann, Ricarda
author_sort Nicola, Lena
title Revisiting temperature sensitivity: How does Antarctic precipitation change with temperature?
title_short Revisiting temperature sensitivity: How does Antarctic precipitation change with temperature?
title_full Revisiting temperature sensitivity: How does Antarctic precipitation change with temperature?
title_fullStr Revisiting temperature sensitivity: How does Antarctic precipitation change with temperature?
title_full_unstemmed Revisiting temperature sensitivity: How does Antarctic precipitation change with temperature?
title_sort revisiting temperature sensitivity: how does antarctic precipitation change with temperature?
publishDate 2023
url https://doi.org/10.5194/tc-2022-254
https://tc.copernicus.org/preprints/tc-2022-254/
long_lat ENVELOPE(-83.917,-83.917,-75.917,-75.917)
ENVELOPE(-155.000,-155.000,-82.000,-82.000)
geographic Antarctic
Siple
Siple Coast
geographic_facet Antarctic
Siple
Siple Coast
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2022-254
https://tc.copernicus.org/preprints/tc-2022-254/
op_doi https://doi.org/10.5194/tc-2022-254
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