Toward a warmer Arctic Ocean: Spreading of the early 21st century Atlantic Water warm anomaly along the Eurasian Basin margins

We document through the analysis of 2002–2005 observational data the recent Atlantic Water (AW) warming along the Siberian continental margin due to several AW warm impulses that penetrated into the Arctic Ocean through Fram Strait in 1999–2000. The AW temperature record from our long-term monitorin...

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Bibliographic Details
Published in:Journal of Geophysical Research
Main Authors: Dmitrenko, Igor A., Polyakov, Igor V., Kirillov, Sergey A., Timokhov, Leonid A., Frolov, Ivan E., Sokolov, Vladimir T., Simmons, Harper L., Ivanov, Vladimir V., Walsh, David
Format: Article in Journal/Newspaper
Language:English
Published: AGU (American Geophysical Union) 2008
Subjects:
Arctic
Arctic Ocean
Laptev Sea
Fram Strait
laptev
Lomonosov Ridge
Online Access:https://oceanrep.geomar.de/id/eprint/719/
https://oceanrep.geomar.de/id/eprint/719/1/351_Dmitrenko_2008_TowardAWarmerArcticOcean_Artzeit_pubid10515.pdf
https://doi.org/10.1029/2007JC004158
Description
Summary:We document through the analysis of 2002–2005 observational data the recent Atlantic Water (AW) warming along the Siberian continental margin due to several AW warm impulses that penetrated into the Arctic Ocean through Fram Strait in 1999–2000. The AW temperature record from our long-term monitoring site in the northern Laptev Sea shows several events of rapid AW temperature increase totaling 0.8°C in February–August 2004. We hypothesize the along-margin spreading of this warmer anomaly has disrupted the downstream thermal equilibrium of the late 1990s to earlier 2000s. The anomaly mean velocity of 2.4–2.5 ± 0.2 cm/s was obtained on the basis of travel time required between the northern Laptev Sea and two anomaly fronts delineated over the Eurasian flank of the Lomonosov Ridge by comparing the 2005 snapshot along-margin data with the AW pre-1990 mean. The magnitude of delineated anomalies exceeds the level of pre-1990 mean along-margin cooling and rises above the level of noise attributed to shifting of the AW jet across the basin margins. The anomaly mean velocity estimation is confirmed by comparing mooring-derived AW temperature time series from 2002 to 2005 with the downstream along-margin AW temperature distribution from 2005. Our mooring current meter data corroborate these estimations.

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