Thermal Overturning Circulation in an Arctic Pond

Abstract In a 1.2‐m‐deep arctic permafrost pond, early‐summer bottom‐water renewal was dominated by thermal overturning circulation, rather than wind‐driven overturning or vertical turbulent mixing. Three high‐resolution current profilers measured turbulent dissipation rates. Three dense temperature...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Stephen M. Henderson, Sally MacIntyre
Format: Article
Language:English
Published: Wiley 2025-04-01
Subjects:
Online Access:https://doi.org/10.1029/2024GL114541