Effects of LGM sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites
Stable water isotopes in polar ice cores are widely used to reconstruct past temperature variations over several orbital climatic cycles. One way to calibrate the isotope-temperature relationship is to apply the present-day spatial relationship as a surrogate for the temporal one. However, this meth...
Main Authors: | , , , , , |
---|---|
Format: | Text |
Language: | English |
Published: |
2023
|
Subjects: | |
Online Access: | https://doi.org/10.5194/cp-2023-3 https://cp.copernicus.org/preprints/cp-2023-3/ |
id |
ftcopernicus:oai:publications.copernicus.org:cpd109056 |
---|---|
record_format |
openpolar |
spelling |
ftcopernicus:oai:publications.copernicus.org:cpd109056 2023-05-15T13:38:41+02:00 Effects of LGM sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites Cauquoin, Alexandre Abe-Ouchi, Ayako Obase, Takashi Chan, Wing-Le Paul, André Werner, Martin 2023-01-24 application/pdf https://doi.org/10.5194/cp-2023-3 https://cp.copernicus.org/preprints/cp-2023-3/ eng eng doi:10.5194/cp-2023-3 https://cp.copernicus.org/preprints/cp-2023-3/ eISSN: 1814-9332 Text 2023 ftcopernicus https://doi.org/10.5194/cp-2023-3 2023-01-30T17:22:43Z Stable water isotopes in polar ice cores are widely used to reconstruct past temperature variations over several orbital climatic cycles. One way to calibrate the isotope-temperature relationship is to apply the present-day spatial relationship as a surrogate for the temporal one. However, this method leads to large uncertainties because several factors like the sea surface conditions or the origin and the transport of water vapor influence the isotope-temperature temporal slope. In this study, we investigate how the sea surface temperature (SST), the sea ice extent and the strength of the Atlantic Meridional Overturning Circulation (AMOC) affect these temporal slopes in Greenland and Antarctica for Last Glacial Maximum (LGM, ~21 000 years ago) to preindustrial climate change. For that, we use the isotope-enabled atmosphere climate model ECHAM6-wiso, forced with a set of sea surface boundary condition datasets based on reconstructions (e.g., GLOMAP) or MIROC 4m simulation outputs. We found that the isotope-temperature temporal slopes in East Antarctic coastal areas are mainly controlled by the sea ice extent, while the sea surface temperature cooling affects more the temporal slope values inland. Mixed effects on isotope-temperature temporal slopes are simulated in West Antarctica with sea surface boundary conditions changes, because the transport of water vapor from the Southern Ocean to this area can dampen the influence of temperature on the changes of the isotopic composition of precipitation and snow. In the Greenland area, the isotope-temperature temporal slopes are influenced by the sea surface temperatures very near the coasts of the continent. The greater the LGM cooling off the coast of southeast Greenland, the larger the temporal slopes. The presence or absence of sea ice very near the coast has a large influence in Baffin Bay and the Greenland Sea and influences the slopes at some inland ice cores stations. We emphasize that the extent far south of the sea ice is not so important. On the other hand, ... Text Antarc* Antarctic Antarctica Baffin Bay Baffin Bay Baffin Greenland Greenland Sea ice core Sea ice Southern Ocean West Antarctica Copernicus Publications: E-Journals Antarctic Baffin Bay Greenland Southern Ocean West Antarctica |
institution |
Open Polar |
collection |
Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
Stable water isotopes in polar ice cores are widely used to reconstruct past temperature variations over several orbital climatic cycles. One way to calibrate the isotope-temperature relationship is to apply the present-day spatial relationship as a surrogate for the temporal one. However, this method leads to large uncertainties because several factors like the sea surface conditions or the origin and the transport of water vapor influence the isotope-temperature temporal slope. In this study, we investigate how the sea surface temperature (SST), the sea ice extent and the strength of the Atlantic Meridional Overturning Circulation (AMOC) affect these temporal slopes in Greenland and Antarctica for Last Glacial Maximum (LGM, ~21 000 years ago) to preindustrial climate change. For that, we use the isotope-enabled atmosphere climate model ECHAM6-wiso, forced with a set of sea surface boundary condition datasets based on reconstructions (e.g., GLOMAP) or MIROC 4m simulation outputs. We found that the isotope-temperature temporal slopes in East Antarctic coastal areas are mainly controlled by the sea ice extent, while the sea surface temperature cooling affects more the temporal slope values inland. Mixed effects on isotope-temperature temporal slopes are simulated in West Antarctica with sea surface boundary conditions changes, because the transport of water vapor from the Southern Ocean to this area can dampen the influence of temperature on the changes of the isotopic composition of precipitation and snow. In the Greenland area, the isotope-temperature temporal slopes are influenced by the sea surface temperatures very near the coasts of the continent. The greater the LGM cooling off the coast of southeast Greenland, the larger the temporal slopes. The presence or absence of sea ice very near the coast has a large influence in Baffin Bay and the Greenland Sea and influences the slopes at some inland ice cores stations. We emphasize that the extent far south of the sea ice is not so important. On the other hand, ... |
format |
Text |
author |
Cauquoin, Alexandre Abe-Ouchi, Ayako Obase, Takashi Chan, Wing-Le Paul, André Werner, Martin |
spellingShingle |
Cauquoin, Alexandre Abe-Ouchi, Ayako Obase, Takashi Chan, Wing-Le Paul, André Werner, Martin Effects of LGM sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites |
author_facet |
Cauquoin, Alexandre Abe-Ouchi, Ayako Obase, Takashi Chan, Wing-Le Paul, André Werner, Martin |
author_sort |
Cauquoin, Alexandre |
title |
Effects of LGM sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites |
title_short |
Effects of LGM sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites |
title_full |
Effects of LGM sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites |
title_fullStr |
Effects of LGM sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites |
title_full_unstemmed |
Effects of LGM sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites |
title_sort |
effects of lgm sea surface temperature and sea ice extent on the isotope-temperature slope at polar ice core sites |
publishDate |
2023 |
url |
https://doi.org/10.5194/cp-2023-3 https://cp.copernicus.org/preprints/cp-2023-3/ |
geographic |
Antarctic Baffin Bay Greenland Southern Ocean West Antarctica |
geographic_facet |
Antarctic Baffin Bay Greenland Southern Ocean West Antarctica |
genre |
Antarc* Antarctic Antarctica Baffin Bay Baffin Bay Baffin Greenland Greenland Sea ice core Sea ice Southern Ocean West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Baffin Bay Baffin Bay Baffin Greenland Greenland Sea ice core Sea ice Southern Ocean West Antarctica |
op_source |
eISSN: 1814-9332 |
op_relation |
doi:10.5194/cp-2023-3 https://cp.copernicus.org/preprints/cp-2023-3/ |
op_doi |
https://doi.org/10.5194/cp-2023-3 |
_version_ |
1766109832567324672 |