Sea-ice-loss slowdown modulates the sea surface salinification in the Kara–Laptev Seas since the 2008 summer

Abstract Recent studies have revealed the slowed Arctic sea-ice loss, but its climate effect on the ocean system remains unclear. By examining reanalysis datasets, we illustrate a paradoxical regime shift characterized by sustained ice loss and surface salinification in the Kara–Laptev Seas (KLS) du...

Full description

Bibliographic Details
Published in:Environmental Research Letters
Main Authors: Yi, Daling Li, Fan, Ke, He, Shengping, Wang, Peng
Other Authors: National Key Research and Development Program of China, National Natural Science Foundation of China, Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory, Southern Marine Science and Engineering Guangdong Laboratory, Natural Science Foundation of Guangdong Province, Research Council of Norway, MAPARC
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2024
Subjects:
Online Access:http://dx.doi.org/10.1088/1748-9326/ad5fa7
https://iopscience.iop.org/article/10.1088/1748-9326/ad5fa7
https://iopscience.iop.org/article/10.1088/1748-9326/ad5fa7/pdf
Description
Summary:Abstract Recent studies have revealed the slowed Arctic sea-ice loss, but its climate effect on the ocean system remains unclear. By examining reanalysis datasets, we illustrate a paradoxical regime shift characterized by sustained ice loss and surface salinification in the Kara–Laptev Seas (KLS) during boreal summer since 2008. A notable phase transition from surface freshening during one period (1997–2008) with rapid sea-ice melting to salinification during another period (2009–2020) with gentle sea-ice melting has been identified in the KLS. Using a mixed-layer salinity budget, we characterized quantitatively the role of ice melting in driving salinification across different seas. We show that the salinification observed post-2008 mainly arises from the weakened summer sea-ice-ocean freshwater input, particularly the localized reduction in ice volume during June–August. This recent salinification in the KLS likely maintains a relatively stable state in the thinner seasonal sea-ice prevailing in the new Arctic.