ORIGINAL RESEARCH article

Front. Mar. Sci.

Sec. Physical Oceanography

Volume 12 - 2025 | doi: 10.3389/fmars.2025.1558240

This article is part of the Research TopicPhysical Processes in the Arctic Ocean and Their Effects on Climate and Marine EcosystemView all 8 articles

Sea Ice Decline in the Eastern Arctic Results in Expansion of the Freshened Surface Layer

Provisionally accepted
Vladimir RogozhinVladimir Rogozhin1,2*Alexander OsadchievAlexander Osadchiev1,3*Alexander SavinAlexander Savin3Ekaterina KuskovaEkaterina Kuskova4Anton GeorgievAnton Georgiev5Olga KonovalovaOlga Konovalova2,5
  • 1P.P. Shirshov Institute of Oceanology (RAS), Moscow, Russia
  • 2Marine Research Center, Lomonosov Moscow State University, Moscow, Moscow Oblast, Russia
  • 3Moscow Institute of Physics and Technology, Dolgoprudny, Moscow Oblast, Russia
  • 4Vizard LLC, Moscow, Russia
  • 5Faculty of Biology, Lomonosov Moscow State University, Moscow, Moscow Oblast, Russia

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In this study, we report an anomalously large freshened surface layer in the Eastern Arctic during icefree season in 2019. This freshened surface layer is formed by river discharge and sea ice meltwater and is also referred to as the Lena plume, due to the Lena River discharge is its major freshwater source. Based on in situ and satellite data, we demonstrate that in August-September 2019 the Lena plume extended from the Lena Delta in the west to the Wrangel Island in the east, i.e., its zonal extent was approximately 2000 km. The area of the Lena plume varied between 750 000 and 870 000 km 2 during this period, which is 1.5 times greater than the assessment of its maximal area in previous years, albeit they were often hindered by the presence of sea ice coverage.The main reasons for this anomalous spreading of the Lena plume are the following. First, intense sea ice melting in the Eastern Arctic in 2019 provided a significantly greater volume of meltwater inflow to the freshened surface layer, as compared to other years. Second, sea ice cleared out of the Laptev and East Siberian seas by the beginning of August and September 2019 respectively, and these seas remained free of ice during for 2 to 3 months (longer ice-free period occurred only in 2007 and 2020).Three months of favorable wind forcing on the Lena plume in July-September 2019 caused its anomalously extensive eastward and northward expansion, together with changes in the vertical structure of the Lena plume. This plume expansion affected the composition of phytoplankton communities, with the intrusion of freshwater species in the eastern part of the East Siberian Sea. The reported expansion of the large Lena plume under favorable sea ice and wind conditions provides the

Keywords: river plume, Sea surface layer, wind forcing, sea ice conditions, meltwater, Phytoplankton communities, Lena River, Eastern Arctic

Received: 09 Jan 2025; Accepted: 08 Apr 2025.

Copyright: © 2025 Rogozhin, Osadchiev, Savin, Kuskova, Georgiev and Konovalova. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

* Correspondence:
Vladimir Rogozhin, P.P. Shirshov Institute of Oceanology (RAS), Moscow, Russia
Alexander Osadchiev, Moscow Institute of Physics and Technology, Dolgoprudny, 141700, Moscow Oblast, Russia

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Supplementary Material