Relative impacts of sea ice loss and atmospheric internal variability on winter Arctic to East Asian surface air temperature based on large-ensemble simulations with NorESM2

There is no consensus as to whether the cooling trend and the frequent severe mid-latitude winters in the 1990s and 2000s are induced by the Arctic changes. One key factor in this respect is the relative impacts of Arctic sea ice loss (referred to as signal) and the atmospheric internal variability...

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Main Author: He, Shengping
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Published: Zenodo 2023
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Online Access:https://doi.org/10.5281/zenodo.7961969
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spelling ftzenodo:oai:zenodo.org:7961969 2024-09-15T18:19:06+00:00 Relative impacts of sea ice loss and atmospheric internal variability on winter Arctic to East Asian surface air temperature based on large-ensemble simulations with NorESM2 He, Shengping 2023-05-23 https://doi.org/10.5281/zenodo.7961969 unknown Zenodo https://zenodo.org/communities/eu https://doi.org/10.5281/zenodo.7961968 https://doi.org/10.5281/zenodo.7961969 oai:zenodo.org:7961969 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/other 2023 ftzenodo https://doi.org/10.5281/zenodo.796196910.5281/zenodo.7961968 2024-07-27T06:38:59Z There is no consensus as to whether the cooling trend and the frequent severe mid-latitude winters in the 1990s and 2000s are induced by the Arctic changes. One key factor in this respect is the relative impacts of Arctic sea ice loss (referred to as signal) and the atmospheric internal variability (sometimes behaving as noise). If the signal-to-noise ratio is low, the atmospheric internal variability can easily overwhelm the forced response to Arctic sea ice forcing. In this study, we use reanalysis datasets and three sets of large-ensemble simulations carried out by the Norwegian Earth System Model with a coupled atmosphere-land surface model, forced by seasonal sea ice conditions from preindustrial, present-day, and future periods. The objective is to quantify the relative contributions of Arctic sea ice and unforced atmospheric internal variability to “warm Arctic, cold East Asia” pattern in winters. The datasets used in this study include: (1)The reanalysis data is the European Centre for Medium-Range Weather Forecasts (ECMWF) fifth-generation global atmospheric reanalysis (ERA5), which is publicly available at https://www.ecmwf.int/en/forecasts/dataset/ecmwf-reanalysis-v5. This data was used for Figure 2a, Figure 5c, and Figure 6a Hersbach, Hans, et al. "The ERA5 global reanalysis." Quarterly Journal of the Royal Meteorological Society 146.730 (2020): 1999-2049. DOI: https://doi.org/10.1002/qj.3803 (2) Sateliate observed Arctic sea ice extent index which can be downloaded freely from the National Snow and Ice Data Center: https://nsidc.org/data/seaice_index. This data was used for Figure 2a and Figure 5c. Fetterer, F., K. Knowles, W. N. Meier, M. Savoie, and A. K. Windnagel. 2017, updated daily. Sea Ice Index, Version 3. Boulder, Colorado USA. NSIDC: National Snow and Ice Data Center. DOI: https://doi.org/10.7265/N5K072F8 (3) Forcing fields for the PAMIP experiments are available from the input4MIPs data server at https://esgf-node.llnl.gov/search/input4mips/). This data was used for Figure 1. Smith, D. ... Other/Unknown Material National Snow and Ice Data Center Sea ice Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
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description There is no consensus as to whether the cooling trend and the frequent severe mid-latitude winters in the 1990s and 2000s are induced by the Arctic changes. One key factor in this respect is the relative impacts of Arctic sea ice loss (referred to as signal) and the atmospheric internal variability (sometimes behaving as noise). If the signal-to-noise ratio is low, the atmospheric internal variability can easily overwhelm the forced response to Arctic sea ice forcing. In this study, we use reanalysis datasets and three sets of large-ensemble simulations carried out by the Norwegian Earth System Model with a coupled atmosphere-land surface model, forced by seasonal sea ice conditions from preindustrial, present-day, and future periods. The objective is to quantify the relative contributions of Arctic sea ice and unforced atmospheric internal variability to “warm Arctic, cold East Asia” pattern in winters. The datasets used in this study include: (1)The reanalysis data is the European Centre for Medium-Range Weather Forecasts (ECMWF) fifth-generation global atmospheric reanalysis (ERA5), which is publicly available at https://www.ecmwf.int/en/forecasts/dataset/ecmwf-reanalysis-v5. This data was used for Figure 2a, Figure 5c, and Figure 6a Hersbach, Hans, et al. "The ERA5 global reanalysis." Quarterly Journal of the Royal Meteorological Society 146.730 (2020): 1999-2049. DOI: https://doi.org/10.1002/qj.3803 (2) Sateliate observed Arctic sea ice extent index which can be downloaded freely from the National Snow and Ice Data Center: https://nsidc.org/data/seaice_index. This data was used for Figure 2a and Figure 5c. Fetterer, F., K. Knowles, W. N. Meier, M. Savoie, and A. K. Windnagel. 2017, updated daily. Sea Ice Index, Version 3. Boulder, Colorado USA. NSIDC: National Snow and Ice Data Center. DOI: https://doi.org/10.7265/N5K072F8 (3) Forcing fields for the PAMIP experiments are available from the input4MIPs data server at https://esgf-node.llnl.gov/search/input4mips/). This data was used for Figure 1. Smith, D. ...
format Other/Unknown Material
author He, Shengping
spellingShingle He, Shengping
Relative impacts of sea ice loss and atmospheric internal variability on winter Arctic to East Asian surface air temperature based on large-ensemble simulations with NorESM2
author_facet He, Shengping
author_sort He, Shengping
title Relative impacts of sea ice loss and atmospheric internal variability on winter Arctic to East Asian surface air temperature based on large-ensemble simulations with NorESM2
title_short Relative impacts of sea ice loss and atmospheric internal variability on winter Arctic to East Asian surface air temperature based on large-ensemble simulations with NorESM2
title_full Relative impacts of sea ice loss and atmospheric internal variability on winter Arctic to East Asian surface air temperature based on large-ensemble simulations with NorESM2
title_fullStr Relative impacts of sea ice loss and atmospheric internal variability on winter Arctic to East Asian surface air temperature based on large-ensemble simulations with NorESM2
title_full_unstemmed Relative impacts of sea ice loss and atmospheric internal variability on winter Arctic to East Asian surface air temperature based on large-ensemble simulations with NorESM2
title_sort relative impacts of sea ice loss and atmospheric internal variability on winter arctic to east asian surface air temperature based on large-ensemble simulations with noresm2
publisher Zenodo
publishDate 2023
url https://doi.org/10.5281/zenodo.7961969
genre National Snow and Ice Data Center
Sea ice
genre_facet National Snow and Ice Data Center
Sea ice
op_relation https://zenodo.org/communities/eu
https://doi.org/10.5281/zenodo.7961968
https://doi.org/10.5281/zenodo.7961969
oai:zenodo.org:7961969
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.796196910.5281/zenodo.7961968
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