
Equatorial Upwelling and Sinking in a Zonal Ocean with Lateral Mixing
Author(s) -
Hidaka Koji
Publication year - 1961
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1961.tb06825.x
Subject(s) - upwelling , geology , zonal and meridional , mixing (physics) , pressure gradient , viscosity , horizontal and vertical , mechanics , motion (physics) , geodesy , geophysics , classical mechanics , oceanography , physics , thermodynamics , quantum mechanics
Summary The two‐dimensional dynamical equations were solved and an expression for the vertical motion was derived by assuming a balance between the pressure gradient, Coriolis and frictional forces. The frictional forces consist of terms of both vertical and lateral mixing. Isovels of the upwelling and sinking in a meridional section were obtained, assuming the magnitudes of the coefficients of the horizontal and vertical viscosities to be 10 8 and 10 2 c. g. s. respectively. The resulting vertical motion of water seems to be more intense than expected. But the result is quite flexible and reasonable values of vertical motion may be obtained by a proper choice of both the horizontal and vertical viscosity coefficients.