b 0 =0
Post on 22-Jan-2016
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b0=0 b0>0
2p + [(2*H*b0)/(d*|f0|)] ∂xp + [2/d] f0/|f0| ∂yt(x) = 0
Sverdrup interior
Stommel boundary
-p(x,y)t(x)
Vorticity:
f+ x = const.fconst
xconst
fconst
xconstf+ x = const.f+
x-
f-
x+
f-plane: b-plane:
Vorticity tendencies due to1. Planetary b-effect:
Vorticity tendencies due to2. Wind-stress Curl:
Vorticity tendencies due to3. Friction:
Total vorticity tendencies:
f+ x = const.f+
x-
f-
x+
West East
-1.0 (-9.0) +1.0 (+0.9)
-1.0 (-1.0) -1.0 (-1.0)
+0.1 (+10) +0.1 (+0.1)
-1.9 (0.0) +0.1 (0.0)
Stommel, H., 1951: An elementary explanation of why ocean currents are strongest in the West, BAMS, 32, 21-23.
Modeled Sea Surface Temperature
Gulfstream
http://science.hq.nasa.gov/oceans/physical/OSC.html
http://www.atmos.washington.edu/~hakim/542/barotropic.html
Barotropic Instability of a Shear Flow (Gaussian Strip of Vorticity):
y
x
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