Western Intensification Subtropical gyres are asymmetric & have intense WBC’s Western...
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Transcript of Western Intensification Subtropical gyres are asymmetric & have intense WBC’s Western...
Western Intensification
• Subtropical gyres are asymmetric & have intense WBC’s
• Western intensification is created by the conservation of angular momentum in gyre
• Friction driven boundary current is formed along the western sidewall
• Maintains the total vorticity of a circulating water parcel
Wind Torque in Gyres
Need process to balance the constant addition of negative
wind torque
Curl of the wind stress…
• Model of steady subtropical gyre
• Includes rotation and horizontal friction
f = constant
f = 2 sin
Stommel’s Experiments
Stommel’s Experiments
• Stommel showed combination of horizontal friction & changes in Coriolis parameter lead to a WBC
• Need to incorporate both ideas into an explanation of western intensification
Western Intensification
• Imagine a parcel circuiting a subtropical gyre
• As a parcel moves, it gains negative vorticity (wind stress curl)
• Gyre cannot keep gaining vorticity or it will spin faster and faster
• Need process to counteract the input of negative vorticity from wind stress curl
Western Intensification
• Conservation of potential vorticity (f + )/D
Assume depth D is constant (barotropic ocean)
Friction (i.e., wind stress curl) can alter (f + )
• In the absence of friction
Southward parcels gain to compensate reduction in f
Northward parcels lose to compensate increase in f
Western Intensification
• Friction plays a role due to
wind stress curl (input of -)
sidewall friction (input of +)
+
+
WBC EBC
Western Intensification
• In a symmetric gyre,
Southward: wind stress input of - is balanced
+ inputs by ’s in latitude & sidewall friction
Northward: ’s in latitude result in an input of -
along with the wind stress input of -
This is NOT balanced by + by sidewall friction
Need an asymmetric gyre to increase sidewall friction in the northward flow!!
Western Intensification
• In a symmetric gyre,
Southward: wind stress input of - is balanced
+ inputs by ’s in latitude & sidewall friction
Northward: ’s in latitude result in an input of -
along with the wind stress input of -
This is NOT balanced by + by sidewall friction
Need an asymmetric gyre to increase sidewall friction in the northward flow!!
Western Intensification
• In a asymmetric gyre,
Southward: wind stress input of - is balanced +
inputs by ’s in latitude & sidewall friction
Northward: ’s in latitude result in an input of -
along with the wind stress input of -
This IS balanced by LARGE + from sidewall friction
Total vorticity balance is satisfied & we have an asymetric gyre
Role of Wind Stress Curl
• Spatial ’s in wind stress control where Ekman transports converge
• Where changes in w = 0, the convergence
of Ekman transports = 0
• This sets the boundaries of gyres
• My = 1/(f/y) curl w = (1/) curl w
-> Sverdrup dynamics
Western Intensification• Intense WBC’s create a source of positive
vorticity that maintains total vorticity balance
• Creates asymmetric gyres & WBC’s
• Boundary currents are like boundary layers
• Wind stress curl & ’s in Coriolis parameter with latitude are critical elements
• Can be extended to quantitatively predict water mass transport (Sverdrup theory)