Articles | Volume 13, issue 6
https://doi.org/10.5194/tc-13-1661-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-1661-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Comparison of ERA5 and ERA-Interim near-surface air temperature, snowfall and precipitation over Arctic sea ice: effects on sea ice thermodynamics and evolution
Caixin Wang
CORRESPONDING AUTHOR
Department of Research and Development, Norwegian Meteorological Institute, 9293 Tromsø, Norway
Research Department, Fram Centre, Norwegian Polar Institute, P.O. Box 6606 Langnes, 9296 Tromsø, Norway
Robert M. Graham
Research Department, Fram Centre, Norwegian Polar Institute, P.O. Box 6606 Langnes, 9296 Tromsø, Norway
Keguang Wang
Department of Research and Development, Norwegian Meteorological Institute, 9293 Tromsø, Norway
Sebastian Gerland
Research Department, Fram Centre, Norwegian Polar Institute, P.O. Box 6606 Langnes, 9296 Tromsø, Norway
Mats A. Granskog
Research Department, Fram Centre, Norwegian Polar Institute, P.O. Box 6606 Langnes, 9296 Tromsø, Norway
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Latest update: 14 Dec 2024
Short summary
A warm bias and higher total precipitation and snowfall were found in ERA5 compared with ERA-Interim (ERA-I) over Arctic sea ice. The warm bias in ERA5 was larger in the cold season when 2 m air temperature was < −25 °C and smaller in the warm season than in ERA-I. Substantial anomalous Arctic rainfall in ERA-I was reduced in ERA5, particularly in summer and autumn. When using ERA5 and ERA-I to force a 1-D sea ice model, the effects on ice growth are very small (cm) during the freezing period.
A warm bias and higher total precipitation and snowfall were found in ERA5 compared with...