Near-bottom water warming in the Laptev Sea in response to atmospheric and sea-ice conditions in 2007.

Hölemann, Jens A. , Kirillov, Sergey, Klagge, Torben, Novikhin, Andrey, Kassens, Heidemarie and Timokhov, Leonid (2011) Near-bottom water warming in the Laptev Sea in response to atmospheric and sea-ice conditions in 2007. Open Access Polar Research, 30 . p. 6425. DOI 10.3402/polar.v30i0.6425.

[thumbnail of 2011_Hoelemann_etal_PolRes_6425-20984-1-PB.pdf]
2011_Hoelemann_etal_PolRes_6425-20984-1-PB.pdf - Published Version
Available under License Creative Commons Attribution Non-commercial.

Download (4MB) | Preview

Supplementary data:


In this paper we present new data from ship-based measurements and two-year observations from moorings in the Laptev Sea along with Russian historical data. The observations from the Laptev Sea in 2007 indicate that the bottom water temperatures on the mid-shelf increased by more than 3°C compared to the long-term mean as a consequence of the unusually high summertime surface water temperatures. Such a distinct increase in near-
bottom temperatures has not been observed before. Remnants of the relatively warm bottom water occupied the mid-shelf from September 2007 until April 2008. Strong polynya activity during March to May 2007 caused more summertime open water and therefore warmer sea surface temperatures in the Laptev Sea. During the ice-free period in August and September 2007, the prevailing cyclonic atmospheric circulation deflected the freshwater plume of the River Lena to the east, which increased the salinity on the mid-shelf north of the Lena Delta. The resulting weaker density stratification allowed more vertical mixing of the water column during storms in late September and early October, leading to the observed warming of the near-bottom layer in the still ice-free Laptev Sea. In summer and autumn 2008, when the density
stratification was stronger and sea surface temperatures were close to the long-term mean, no near-bottom water warming was observed. Warmer water temperatures near the seabed may also impact the stability of the shelf’s submarine permafrost.

Document Type: Article
Additional Information: WOS:000298040800004
Keywords: Siberian Shelf seas; Shelf oceanography; Sea ice; Atmospheric forcing; Siberian Arctic shelf; Thermohaline structure; Hydrography
Research affiliation: OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-P-OZ Paleo-Oceanography
Refereed: Yes
Open Access Journal?: Yes
Publisher: Norwegian Polar Institute
Projects: Polynya, Laptev Sea System
Date Deposited: 04 Dec 2014 11:12
Last Modified: 31 Jan 2023 05:24

Actions (login required)

View Item View Item