- PII
- S30346487S0002351525030085-1
- DOI
- 10.7868/S3034648725030085
- Publication type
- Article
- Status
- Published
- Authors
- Volume/ Edition
- Volume 61 / Issue number 3
- Pages
- 377-387
- Abstract
- The circulation features of the Siberian shelf in the period from 1985 to 2014 are studied using numerical large-scale model of ocean and sea ice circulation and atmospheric reanalysis data. It is shown that in the last two decades the residence time of river tracers in the shelf area has 2–4 times decreased. The most likely reason for this reduction is an increase in the duration of the ice-free period, combined with the prevailing wind effect, favorable for transport of tracers into the deep part of the Arctic Ocean.
- Keywords
- Северный Ледовитый океан шельфовые моря траектории трассеров сибирские реки речной сток арктическая осцилляция океана
- Date of publication
- 01.03.2025
- Year of publication
- 2025
- Number of purchasers
- 0
- Views
- 36
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