FESOM model results

control: the hindcast simulation using interannually varying atmospheric forcing (IAVF). AO: In the Arctic Ocean the IAVF is used. Outside the Arctic Ocean the normal year forcing (NYF) is used. The NYF is repeatedly used for every year. nAO:In the Arctic Ocean the NYF is used. Outside the Arctic Oc...

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Bibliographic Details
Main Authors: Zhang, Wenhao, Wang, Qiang, Wang, Xuezhu, Danilov, Sergey
Format: Dataset
Language:unknown
Published: Zenodo 2019
Subjects:
Arctic
Arctic Ocean
Bering Strait
The ''Y''
Online Access:https://dx.doi.org/10.5281/zenodo.2648156
https://zenodo.org/record/2648156
Description
Summary:control: the hindcast simulation using interannually varying atmospheric forcing (IAVF). AO: In the Arctic Ocean the IAVF is used. Outside the Arctic Ocean the normal year forcing (NYF) is used. The NYF is repeatedly used for every year. nAO:In the Arctic Ocean the NYF is used. Outside the Arctic Ocean the IAVF is used. AO_w: the same as AO but the atmospheric buoyancy forcing in the Arctic Ocean is changed to the NYF. nAO_w: the same as nAO but the atmospheric buoyancy forcing outside the Arctic Ocean is changed to the NYF. vtransp: volume transport through Bering Strait. fwtransp: freshwater transport through Bering Strait. Htransp: heat transport through Bering Strait. slp_yr: annual mean sea level pressure. ssh_yr: annual mean sea surface high. Ekmantransp_tx: Ekman transport component in the x direction. Ekmantransp_ty: Ekman transport component in the y direction. min: years with low Bering Strait throughflow. max: years with high Bering Strait throughflow. temp_diff_0-50m: the difference of temperature between years with high and low Bering Strait throughflow. salt_diff_0-50m: the difference of salinity between years with high and low Bering Strait throughflow.

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