Role of Atlantification in Enhanced Primary Productivity in the Barents Sea

Abstract Recent changes in the Arctic sea‐ice are strongly influenced by the recent increase in heat transport from vigorous Atlantic inflows, so‐called Atlantification. This Atlantification can induce physical and ecological changes near the Atlantic gateway. Here, we used the observational data se...

Full description

Bibliographic Details
Published in:Earth's Future
Main Authors: Kyung‐Min Noh, Ji‐Hoon Oh, Hyung‐Gyu Lim, Hajoon Song, Jong‐Seong Kug
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:https://doi.org/10.1029/2023EF003709
https://doaj.org/article/54ae7a2f72ce4204b99e1c2c9141878e
Description
Summary:Abstract Recent changes in the Arctic sea‐ice are strongly influenced by the recent increase in heat transport from vigorous Atlantic inflows, so‐called Atlantification. This Atlantification can induce physical and ecological changes near the Atlantic gateway. Here, we used the observational data sets and 26 Earth system models to estimate Atlantic water intrusion, and firstly suggest the impact of Atlantification on marine productivity in the Barents Sea in a warming climate, especially on boreal spring. In a warming climate, the heat transport across the Barents Sea Opening (BSO) is projected to be enhanced (45.5 ± 34.9 TW) by the end of the 21st century compared to the present climate. This poleward intrusion of the Atlantic water is likely to increase productivity with the largest increase in spring (70%). In a warming climate, the productivity is enhanced by Atlantification‐induced changes in physical states—ocean temperature, circulations, stratification, and sea‐ice. Based on inter‐model analyses, we estimated that the Atlantification can explain approximately 26% of the productivity changes in the Barents Sea. Thus, Atlantification is critical for future changes in biological productivity and physical states over the Arctic Ocean.