Evaluation of the HadISST1 and NSIDC 1850 onward sea ice datasets with a focus on the Barents-Kara seas

In recent years, long-term continuous sea-ice datasets have been developed, and they cover the periods before and after the satellite era. How these datasets differ from one another before the satellite era, and whether one is more reliable than the other, is important but unclear because the sea-ic...

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Bibliographic Details
Published in:Atmospheric and Oceanic Science Letters
Main Authors: WANG Rui-Bo, LI Shuanglin, HAN Zhe
Format: Article in Journal/Newspaper
Language:English
Published: KeAi Communications Co., Ltd. 2018
Subjects:
Evaluation
sea-ice dataset
NSIDC
Hadley Centre
proxy
Environmental sciences
GE1-350
Oceanography
GC1-1581
Franz Josef Land
National Snow and Ice Data Center
Novaya Zemlya
Sea ice
Online Access:https://doi.org/10.1080/16742834.2018.1504599
https://doaj.org/article/0385eecf3dc04ab4a33164b7b849e459
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Summary:In recent years, long-term continuous sea-ice datasets have been developed, and they cover the periods before and after the satellite era. How these datasets differ from one another before the satellite era, and whether one is more reliable than the other, is important but unclear because the sea-ice record before 1979 is sparse and not continuous. In this letter, two sets of sea-ice datasets are evaluated: one is the HadISST1 dataset from the Hadley Centre, and the other is the SIBT1850 (Gridded Monthly Sea Ice Extent and Concentration, from 1850 Onward) dataset from the National Snow and Ice Data Center (NSIDC). In view of its substantial importance for climate, the winter sea ice in the Barents and Kara seas (BKS) is of particular focus. A reconstructed BKS sea-ice extent (SIE) is developed using linear regression from the mean of observed surface air temperature at two adjacent islands, Novaya Zemlya and Franz Josef Land (proxy). One validation illustrates that the proxy is substantially coherent with the BKS sea-ice anomaly in the observations and the CMIP5 (phase 5 of the Coupled Model Intercomparison Project) historical experiments. This result indicates that the proxy is reasonable. Therefore, the establishment of the reconstructed BKS SIE is also reasonable. The evaluation results based on the proxy suggest that the sea-ice concentration prior to the satellite era in the NSIDC dataset is more realistic and reliable than that in the Hadley Centre dataset, and thus is more appropriate for use.

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