Simple curl balances and thermocline depth:
Terms of Sverdrup integration (Curl(Tau) and Tau-x): Tropical Pacific SWCA SWCA (overlay vectors)
Curl terms from ECMWF: Mean Annual cycle Annual cycle anonymous
Curl(Tau/f) components: Mean: SWCA Pacific 1 cpy harmonic: Stack Overlay Detail SWCA
Compare transports: Ekman vs XBT Geostrophic Sverdrup, Ekman, Geostrophic (all from winds) Magnitudes
Ekman pumping:Annual cycle correlation: d(Z20)/dt vs Curl
Statistics of the Ekman pumping balance terms
Compare Curl to d(Z20)/dt harmonics (vectors): Curl(Tau) and d(Z20)/dt Curl(Tau/f) and d(Z20)/dt
Same comparison from K90 XBTs: SWCA Whole N tropical Pacific
d(Z20)/dt as a fn of (x,t) at different latitudes (pos = downwelling)
Compare Curl(Tau)/(f*rho)
Compare Curl and Z20 as a fn of (y,t) at 100°-94°W
Mean thermocline from winds and Sverdrup balance (Entirely within Ferret: jnl 95 -> 97)
Compare damping times for Sverdrup balance (Obs Z20 vs from winds): FSU winds. H&R winds.
-> Link to Sverdrup calculation page
-> Link to Rossby wave model page