Premium
Summertime coastal current reversal opposing offshore forcing and local wind near the middle east coast of Korea: Observation and dynamics
Author(s) -
Park JaeHyoung,
Chang KyungIl,
Nam SungHyun
Publication year - 2016
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 - 10.1002/2016gl069322
Subject(s) - pressure gradient , submarine pipeline , current (fluid) , pressure gradient force , geology , oceanography , wind stress , forcing (mathematics) , buoy , boundary current , climatology , sea breeze , temperature gradient , buoyancy , ocean current , environmental science , meteorology , geography , physics , quantum mechanics
A 6 year long current measurement at a buoy station off the middle east coast of Korea reveals an equatorward reversal of coastal current in summer opposing poleward local wind stress and offshore boundary current. The current reversal extends about 40 km offshore from the coast and is concurrent with warming and freshening of water column. Estimates of the depth‐averaged alongshore momentum balance suggest a major balance between the alongshore pressure gradient and the lateral friction. Sources of the pressure gradient for the summertime current reversal are identified as the alongshore buoyancy gradient driven by the wind curl gradient and the prevalence of warmer and lower salinity water in the north. Alongshore pressure gradient and velocity induced by the wind curl gradient are quantified, which yields the observed seasonal current reversal.