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Heat flux variations in the eastern Norwegian Atlantic Current toward the Arctic from moored instruments, 1995–2005
Author(s) -
Orvik Kjell Arild,
Skagseth Øystein
Publication year - 2005
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2005gl023487
Subject(s) - heat flux , anomaly (physics) , flux (metallurgy) , the arctic , current (fluid) , norwegian , environmental science , climatology , arctic , oceanography , atmospheric sciences , geology , physics , heat transfer , materials science , thermodynamics , linguistics , philosophy , metallurgy , condensed matter physics
An extraordinary warming of the Atlantic inflow to the Norwegian Sea toward the Arctic is observed over the last decade. In light of that we investigate the seasonal and interannual variations of the heat flux in the eastern Norwegian Atlantic Current (NwASC) using moored temperature (T)‐ and current (v) measurements in the Svinøy section (62°N); 1995–2005. By splitting the heat flux anomaly (vT)′ into v′ and T′ (, : 10‐year means; v′T′ negligible), we examine the relative contributions from variations in v and T. The dominating seasonal signal coincides almost completely with v′, whilst T′ has a minor modulating effect. On the interannual timescale the heat‐flux anomaly also coincides with v′, while T′ contributes significantly to the long term trend. There is a downward 10‐year trend in the velocity field of 3.9 cm s −1 (12%), combined with a 1°C increase in temperature, resulting in a constant heat flux.