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 increased ice-sheet mass losses caused by increased ice discharge and melting. For sea-level projections it is therefore vital to understand the processes determ...

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Main Authors: Nicola, Lena, Notz, Dirk, Winkelmann, Ricarda
Format: Text
Language:English
Published: Katlenburg-Lindau : EGU 2023
Subjects:
910
Online Access:https://dx.doi.org/10.34657/13713
https://oa.tib.eu/renate/handle/123456789/14691
id ftdatacite:10.34657/13713
record_format openpolar
spelling ftdatacite:10.34657/13713 2024-09-15T17:47:33+00:00 Revisiting temperature sensitivity: how does Antarctic precipitation change with temperature? ... Nicola, Lena Notz, Dirk Winkelmann, Ricarda 2023 https://dx.doi.org/10.34657/13713 https://oa.tib.eu/renate/handle/123456789/14691 en eng Katlenburg-Lindau : EGU Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Antarctica Siple Coast West Antarctica climate conditions CMIP plateau precipitation climatology snow cover temperature effect 910 article article-journal Text ScholarlyArticle 2023 ftdatacite https://doi.org/10.34657/13713 2024-07-03T10:25:24Z With progressing global warming, snowfall in Antarctica is expected to increase, which could counteract or even temporarily overcompensate increased ice-sheet mass losses caused by increased ice discharge 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, Coupled Model Intercomparison Project Phase 6) 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 of > 10 % K-1 at the East Antarctic plateau region. This large range can be explained by the prevailing climatic ... Text Antarc* Antarctic Antarctica Ice Sheet West Antarctica DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Antarctica
Siple Coast
West Antarctica
climate conditions
CMIP
plateau
precipitation climatology
snow cover
temperature effect
910
spellingShingle Antarctica
Siple Coast
West Antarctica
climate conditions
CMIP
plateau
precipitation climatology
snow cover
temperature effect
910
Nicola, Lena
Notz, Dirk
Winkelmann, Ricarda
Revisiting temperature sensitivity: how does Antarctic precipitation change with temperature? ...
topic_facet Antarctica
Siple Coast
West Antarctica
climate conditions
CMIP
plateau
precipitation climatology
snow cover
temperature effect
910
description With progressing global warming, snowfall in Antarctica is expected to increase, which could counteract or even temporarily overcompensate increased ice-sheet mass losses caused by increased ice discharge 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, Coupled Model Intercomparison Project Phase 6) 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 of > 10 % K-1 at the East Antarctic plateau region. This large range can be explained by the prevailing climatic ...
format Text
author Nicola, Lena
Notz, Dirk
Winkelmann, Ricarda
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? ...
publisher Katlenburg-Lindau : EGU
publishDate 2023
url https://dx.doi.org/10.34657/13713
https://oa.tib.eu/renate/handle/123456789/14691
genre Antarc*
Antarctic
Antarctica
Ice Sheet
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
West Antarctica
op_rights Creative Commons Attribution 4.0 International
CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.34657/13713
_version_ 1810496965608210432