Ocean Heat Transport Into the Barents Sea: Distinct Controls on the Upward Trend and Interannual Variability. Issue 22 (20th November 2019)

• Record Type: Journal Article
• Authors: Wang, Qiang; Wang, Xuezhu; Wekerle, Claudia; Danilov, Sergey; Jung, Thomas; Koldunov, Nikolay; Lind, Sigrid; Sein, Dmitry; Shu, Qi; Sidorenko, Dmitry
• Is Part Of: Geophysical research letters. Volume 46:Issue 22(2019)
• Page Start: 13180
• Page End: 13190
• Publication Date: 2019-11-20
• Subjects: Barents Sea -- Atlantic Water -- heat transport -- subpolar North Atlantic -- wind forcing -- Nordic Seas; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1029/2019GL083837
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: Ocean heat transport through the Barents Sea Opening (BSO) has strong impacts on the Barents Sea ice extent and the climate. In this paper we quantified the contributions from different atmospheric forcing components to the trend and interannual variability of the BSO heat transport. Ocean‐ice model simulations were conducted in which the interannual variation of atmospheric forcing was maintained only in or outside the Arctic in two different simulations. The sum of their BSO heat transport anomalies reasonably replicated the trend and variability from a hindcast simulation. The upward trend of the BSO heat transport mainly stems from the increasing ocean temperature in the subpolar North Atlantic. For the interannual variability, the local wind and upstream forcing are similarly important. The location of the Atlantic Water boundary current in the Nordic Seas, influenced by the cyclonic atmospheric circulation, is crucial in determining part of the BSO inflow variability. Key Points: Forcing responsible for the trend and interannual variability of ocean heat transported into the Barents Sea is disentangled The upward trend of the heat inflow stems from warming in the subpolar North Atlantic, while local wind accounts for half of its variance The location of the Atlantic Water boundary current relative to the Barents Sea entrance is crucial in determining the heat inflow