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Strong inertial currents and marginal internal wave stability in the central North Sea
Author(s) -
van Haren Hans,
Maas Leo,
Zimmerman J. T. F.,
Ridderinkhof Herman,
Malschaert Hans
Publication year - 1999
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 - 10.1029/1999gl002352
Subject(s) - internal tide , internal wave , abyssal zone , geology , inertial wave , mixing (physics) , atmospheric sciences , water column , oceanography , geophysics , physics , wave propagation , mechanical wave , longitudinal wave , quantum mechanics
Solar insolation stabilizes the water column and suppresses vertical exchange. Observations from the central North Sea clearly show that increased heating in summer is accompanied by enhanced de‐stabilizing vertical current differences (shear), surprisingly to such extent that the equilibrium state is marginally stable. Under calm weather conditions, the shear is predominantly generated by near‐inertial motions while the internal wave spectrum primarily results from nonlinear interaction between the dominating tidal and near‐inertial motions. In terms of the associated enhanced vertical mixing across the largest vertical temperature gradients, shelf seas are not different from the abyssal ocean, despite the proximity to energy sources near boundaries in the former. By the lack of sufficiently strong wind‐ and tidal‐mixing this internal mixing is considered to be responsible for the diapycnal transport of nutrients leading to the observed increase in near‐surface values and triggering the late‐summer phytoplankton bloom.