Mesoscale Eddy Influence on Upper.Ocean Chlorophyll Variability ...

′ ′

U ′ wind = αSST ′
α =0.32
−→
τ
−→ −→
U ′ wind = αSST ′
α =0.32
WE = 1
ρf ∇×−→ τ

U ′ wind = αSST ′
α =0.32
−→
τ
−→ −→
U ′ wind = αSST ′
α =0.32
WE = 1
ρf ∇×−→ τ

U ′ wind = αSST ′
α =0.32
−→
τ
−→ −→
U ′ wind = αSST ′
α =0.32
WE = 1
ρf ∇×−→ τ

−→
u
−→
a
u o
−→
τ = ρCD|urel| −→ u rel
−→ u rel = −→ u a − −→ u o
WE = 1
ρf ∇×−→ τ

−→
u
−→
a
u o
−→
τ = ρCD|urel| −→ u rel
−→ u rel = −→ u a − −→ u o
WE = 1
ρf ∇×−→ τ

−→
u
−→
a
u o
−→
τ = ρCD|urel| −→ u rel
−→ u rel = −→ u a − −→ u o
WE = 1
ρf ∇×−→ τ

−→
u
−→
a
u o
−→
τ = ρCD|urel| −→ u rel
−→ u rel = −→ u a − −→ u o
WE = 1
ρf ∇×−→ τ

WE = 1
ρf ∇×−→ τ

WE = 1
ρf ∇×−→ τ

WE = 1
ρf ∇×−→ τ

WE = 1
ρf ∇×−→ τ

WE = 1
ρf ∇×−→ τ