CAPS v1.0: An improved regional coupled modeling system for Arctic sea ice and climate simulation and prediction

The updated Coupled Arctic Prediction System (CAPS) is evaluated, which is built on new versions of Weather Research and Forecasting model (WRF), the Regional Ocean Modeling System (ROMS), the Community Ice CodE (CICE), and a data assimilation based on the Local Error Subspace Transform Kalman Filte...

Full description

Bibliographic Details
Main Authors: Yang, Chao-Yuan, Liu, Jiping, Chen, Dake
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/gmd-2021-220
https://gmd.copernicus.org/preprints/gmd-2021-220/
id ftcopernicus:oai:publications.copernicus.org:gmdd95825
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:gmdd95825 2023-05-15T14:47:08+02:00 CAPS v1.0: An improved regional coupled modeling system for Arctic sea ice and climate simulation and prediction Yang, Chao-Yuan Liu, Jiping Chen, Dake 2021-07-12 application/pdf https://doi.org/10.5194/gmd-2021-220 https://gmd.copernicus.org/preprints/gmd-2021-220/ eng eng doi:10.5194/gmd-2021-220 https://gmd.copernicus.org/preprints/gmd-2021-220/ eISSN: 1991-9603 Text 2021 ftcopernicus https://doi.org/10.5194/gmd-2021-220 2021-07-19T16:22:28Z The updated Coupled Arctic Prediction System (CAPS) is evaluated, which is built on new versions of Weather Research and Forecasting model (WRF), the Regional Ocean Modeling System (ROMS), the Community Ice CodE (CICE), and a data assimilation based on the Local Error Subspace Transform Kalman Filter. A set of Pan-Arctic prediction experiments with improved/changed physical parameterizations in WRF, ROMS and CICE as well as different configurations are performed for the year 2018 to assess their impacts on the predictive skill of Arctic sea ice at seasonal timescale. The key improvements of WRF, including cumulus, boundary layer, and land surface schemes, result in improved simulation in near surface air temperature and downward radiation. The major changes of ROMS, including tracer advection and vertical mixing schemes, lead to improved evolution of the predicted total ice extent (particularly correcting the late ice recovery issue in the previous CAPS), and reduced biases in sea surface temperature. The changes of CICE, that include improved ice thermodynamics and assimilation of new sea ice thickness product, have noticeable influences on the predicted ice thickness and the timing of ice recovery. Results from the prediction experiments suggest that the updated CAPS can better predict the evolution of total ice extent compared with its predecessor, though the predictions still have certain biases at the regional scale. We further show that the CAPS can remain skillful beyond the melting season, which may have potential values for stakeholders making decisions for socioeconomical activities in the Arctic. Text Arctic Sea ice Copernicus Publications: E-Journals Arctic
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The updated Coupled Arctic Prediction System (CAPS) is evaluated, which is built on new versions of Weather Research and Forecasting model (WRF), the Regional Ocean Modeling System (ROMS), the Community Ice CodE (CICE), and a data assimilation based on the Local Error Subspace Transform Kalman Filter. A set of Pan-Arctic prediction experiments with improved/changed physical parameterizations in WRF, ROMS and CICE as well as different configurations are performed for the year 2018 to assess their impacts on the predictive skill of Arctic sea ice at seasonal timescale. The key improvements of WRF, including cumulus, boundary layer, and land surface schemes, result in improved simulation in near surface air temperature and downward radiation. The major changes of ROMS, including tracer advection and vertical mixing schemes, lead to improved evolution of the predicted total ice extent (particularly correcting the late ice recovery issue in the previous CAPS), and reduced biases in sea surface temperature. The changes of CICE, that include improved ice thermodynamics and assimilation of new sea ice thickness product, have noticeable influences on the predicted ice thickness and the timing of ice recovery. Results from the prediction experiments suggest that the updated CAPS can better predict the evolution of total ice extent compared with its predecessor, though the predictions still have certain biases at the regional scale. We further show that the CAPS can remain skillful beyond the melting season, which may have potential values for stakeholders making decisions for socioeconomical activities in the Arctic.
format Text
author Yang, Chao-Yuan
Liu, Jiping
Chen, Dake
spellingShingle Yang, Chao-Yuan
Liu, Jiping
Chen, Dake
CAPS v1.0: An improved regional coupled modeling system for Arctic sea ice and climate simulation and prediction
author_facet Yang, Chao-Yuan
Liu, Jiping
Chen, Dake
author_sort Yang, Chao-Yuan
title CAPS v1.0: An improved regional coupled modeling system for Arctic sea ice and climate simulation and prediction
title_short CAPS v1.0: An improved regional coupled modeling system for Arctic sea ice and climate simulation and prediction
title_full CAPS v1.0: An improved regional coupled modeling system for Arctic sea ice and climate simulation and prediction
title_fullStr CAPS v1.0: An improved regional coupled modeling system for Arctic sea ice and climate simulation and prediction
title_full_unstemmed CAPS v1.0: An improved regional coupled modeling system for Arctic sea ice and climate simulation and prediction
title_sort caps v1.0: an improved regional coupled modeling system for arctic sea ice and climate simulation and prediction
publishDate 2021
url https://doi.org/10.5194/gmd-2021-220
https://gmd.copernicus.org/preprints/gmd-2021-220/
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-2021-220
https://gmd.copernicus.org/preprints/gmd-2021-220/
op_doi https://doi.org/10.5194/gmd-2021-220
_version_ 1766318276395139072