Arctic ocean freshwater in CMIP6 ensembles: Declining sea ice, increasing ocean storage and export
The Arctic has undergone dramatic changes in sea ice cover and the hydrologic cycle, both of which strongly impact the freshwater storage in, and export from, the Arctic Ocean. Here we analyze Arctic freshwater storage and fluxes in seven climate models from the Coupled Model Intercomparison Project...
Published in: | Journal of Geophysical Research: Oceans |
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Other Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2021
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Online Access: | https://doi.org/10.1029/2020JC016930 |
id |
ftncar:oai:drupal-site.org:articles_24930 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) |
op_collection_id |
ftncar |
language |
English |
description |
The Arctic has undergone dramatic changes in sea ice cover and the hydrologic cycle, both of which strongly impact the freshwater storage in, and export from, the Arctic Ocean. Here we analyze Arctic freshwater storage and fluxes in seven climate models from the Coupled Model Intercomparison Project Phase 6 (CMIP6) and assess their performance over the historical period (1980-2000) and in two future emissions scenarios, SSP1-2.6 and SSP5-8.5. Similar to CMIP5, substantial differences exist between the models' Arctic mean states and the magnitude of their 21st century storage and flux changes. In the historical simulation, most models disagree with observations over 1980-2000. In both future scenarios, the models show an increase in liquid freshwater storage and a reduction in solid storage and fluxes through the major Arctic gateways (Bering Strait, Fram Strait, Davis Strait, and the Barents Sea Opening) that is typically larger for SSP5-8.5 than SSP1-2.6. The liquid fluxes are driven by both volume and salinity changes, with models exhibiting a change in sign (relative to 1980-2000) of the freshwater flux through the Barents Sea Opening by mid-century, little change in the Bering Strait flux, and increased export from the remaining straits by the end of the 21st century. In the straits west of Greenland (Nares, Barrow, and Davis straits), the models disagree on the behavior of the liquid freshwater export in the early-to-mid 21st century due to differences in the magnitude and timing of a simulated decrease in the volume flux. 1852977 |
author2 |
Zanowski, Hannah (author) Jahn, Alexandra (author) Holland, Marika M. (author) |
format |
Article in Journal/Newspaper |
title |
Arctic ocean freshwater in CMIP6 ensembles: Declining sea ice, increasing ocean storage and export |
spellingShingle |
Arctic ocean freshwater in CMIP6 ensembles: Declining sea ice, increasing ocean storage and export |
title_short |
Arctic ocean freshwater in CMIP6 ensembles: Declining sea ice, increasing ocean storage and export |
title_full |
Arctic ocean freshwater in CMIP6 ensembles: Declining sea ice, increasing ocean storage and export |
title_fullStr |
Arctic ocean freshwater in CMIP6 ensembles: Declining sea ice, increasing ocean storage and export |
title_full_unstemmed |
Arctic ocean freshwater in CMIP6 ensembles: Declining sea ice, increasing ocean storage and export |
title_sort |
arctic ocean freshwater in cmip6 ensembles: declining sea ice, increasing ocean storage and export |
publishDate |
2021 |
url |
https://doi.org/10.1029/2020JC016930 |
long_lat |
ENVELOPE(158.167,158.167,-81.450,-81.450) |
geographic |
Arctic Arctic Ocean Barents Sea Bering Strait Greenland Nares |
geographic_facet |
Arctic Arctic Ocean Barents Sea Bering Strait Greenland Nares |
genre |
Arctic Arctic Arctic Ocean Barents Sea Bering Strait Davis Strait Fram Strait Greenland Sea ice |
genre_facet |
Arctic Arctic Arctic Ocean Barents Sea Bering Strait Davis Strait Fram Strait Greenland Sea ice |
op_relation |
Journal of Geophysical Research: Oceans--J. Geophys. Res. Oceans--2169-9275--2169-9291 Arctic Ocean freshwater storage and fluxes from CMIP6 model ensembles 1950-2100--10.18739/A2154DQ22 CCCma CanESM5-CanOE model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.10269 CCCma CanESM5 model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.3610 CCCma CanESM5 model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.3696 CMIP6 simulations of the CNRM-CERFACS based on CNRM-CM6-1 model for CMIP experiment historical--10.22033/ESGF/CMIP6.4066 CNRM-CERFACS CNRM-CM6-1 model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.4184 CNRM-CERFACS CNRM-CM6-1 model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.4224 IPSL IPSL-CM6A-LR model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.5195 IPSL IPSL-CM6A-LR model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.5262 IPSL IPSL-CM6A-LR model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.5271 MIROC MIROC6 model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.5603 MIROC MIROC6 model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.5743 MIROC MIROC6 model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.5771 MOHC UKESM1.0-LL model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.6113 MOHC UKESM1.0-LL model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.6333 MOHC UKESM1.0-LL model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.6405 MPI-M MPI-ESM1.2-LR model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.6595 MPI-M MPI-ESM1.2-LR model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.6690 MPI-M MPI-ESM1.2-LR model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.6705 NCAR CESM2 model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.7627 NCAR CESM2 model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.7746 NCAR CESM2 model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.7768 HannahZanowski/CMIP6_ArcticFW: Arctic FW Storage and Fluxes in CMIP6 Models--10.5281/zenodo.4606856 articles:24930 doi:10.1029/2020JC016930 ark:/85065/d7cj8j0q |
op_rights |
Copyright 2021 American Geophysical Union. |
op_doi |
https://doi.org/10.1029/2020JC016930 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
126 |
container_issue |
4 |
_version_ |
1796302295690903552 |
spelling |
ftncar:oai:drupal-site.org:articles_24930 2024-04-14T08:05:38+00:00 Arctic ocean freshwater in CMIP6 ensembles: Declining sea ice, increasing ocean storage and export Zanowski, Hannah (author) Jahn, Alexandra (author) Holland, Marika M. (author) 2021-04 https://doi.org/10.1029/2020JC016930 en eng Journal of Geophysical Research: Oceans--J. Geophys. Res. Oceans--2169-9275--2169-9291 Arctic Ocean freshwater storage and fluxes from CMIP6 model ensembles 1950-2100--10.18739/A2154DQ22 CCCma CanESM5-CanOE model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.10269 CCCma CanESM5 model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.3610 CCCma CanESM5 model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.3696 CMIP6 simulations of the CNRM-CERFACS based on CNRM-CM6-1 model for CMIP experiment historical--10.22033/ESGF/CMIP6.4066 CNRM-CERFACS CNRM-CM6-1 model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.4184 CNRM-CERFACS CNRM-CM6-1 model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.4224 IPSL IPSL-CM6A-LR model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.5195 IPSL IPSL-CM6A-LR model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.5262 IPSL IPSL-CM6A-LR model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.5271 MIROC MIROC6 model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.5603 MIROC MIROC6 model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.5743 MIROC MIROC6 model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.5771 MOHC UKESM1.0-LL model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.6113 MOHC UKESM1.0-LL model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.6333 MOHC UKESM1.0-LL model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.6405 MPI-M MPI-ESM1.2-LR model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.6595 MPI-M MPI-ESM1.2-LR model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.6690 MPI-M MPI-ESM1.2-LR model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.6705 NCAR CESM2 model output prepared for CMIP6 CMIP historical--10.22033/ESGF/CMIP6.7627 NCAR CESM2 model output prepared for CMIP6 ScenarioMIP ssp126--10.22033/ESGF/CMIP6.7746 NCAR CESM2 model output prepared for CMIP6 ScenarioMIP ssp585--10.22033/ESGF/CMIP6.7768 HannahZanowski/CMIP6_ArcticFW: Arctic FW Storage and Fluxes in CMIP6 Models--10.5281/zenodo.4606856 articles:24930 doi:10.1029/2020JC016930 ark:/85065/d7cj8j0q Copyright 2021 American Geophysical Union. article Text 2021 ftncar https://doi.org/10.1029/2020JC016930 2024-03-21T18:00:26Z The Arctic has undergone dramatic changes in sea ice cover and the hydrologic cycle, both of which strongly impact the freshwater storage in, and export from, the Arctic Ocean. Here we analyze Arctic freshwater storage and fluxes in seven climate models from the Coupled Model Intercomparison Project Phase 6 (CMIP6) and assess their performance over the historical period (1980-2000) and in two future emissions scenarios, SSP1-2.6 and SSP5-8.5. Similar to CMIP5, substantial differences exist between the models' Arctic mean states and the magnitude of their 21st century storage and flux changes. In the historical simulation, most models disagree with observations over 1980-2000. In both future scenarios, the models show an increase in liquid freshwater storage and a reduction in solid storage and fluxes through the major Arctic gateways (Bering Strait, Fram Strait, Davis Strait, and the Barents Sea Opening) that is typically larger for SSP5-8.5 than SSP1-2.6. The liquid fluxes are driven by both volume and salinity changes, with models exhibiting a change in sign (relative to 1980-2000) of the freshwater flux through the Barents Sea Opening by mid-century, little change in the Bering Strait flux, and increased export from the remaining straits by the end of the 21st century. In the straits west of Greenland (Nares, Barrow, and Davis straits), the models disagree on the behavior of the liquid freshwater export in the early-to-mid 21st century due to differences in the magnitude and timing of a simulated decrease in the volume flux. 1852977 Article in Journal/Newspaper Arctic Arctic Arctic Ocean Barents Sea Bering Strait Davis Strait Fram Strait Greenland Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Arctic Ocean Barents Sea Bering Strait Greenland Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Journal of Geophysical Research: Oceans 126 4 |