A composite El Niño
FORCING:
- The 6 El Niños chosen (over Taux at 0°,170°W)
- (x,t) Hofmullers of composite Tau and Curl in latitude bands: Southern hemisphere Northern hemisphere
- RMS (maps) of composite forcing: Taux Tauy Curl -d(Taux)/dy d(Tauy)/dx f^s/BCurl(tau)+Taux
- RMS about composite: Taux Tauy
- Time series at 160°E-160°W: Curl Overlay Tau vectors Taux Overlay Tau vectors
RMS Curl: Plain Overlay N and S hemisphere Smooth y=sbx:5
- Sequential maps every 3 months:
- The composite: Yr -1 Yr 0 Yr +1 Combined (html)
(Different style of wind vectors: Yr 0 Yr +1)
- Compare climatology of stress and curl:
- Mean Include divergence Individual derivative terms
- Seasonal values (sequential maps): Totals (Different style) Anomalies
- Seasonal cycle at 160°E-160°W
- Wind divergence
- OND Yr 0 compared to climatology: Curl Divergence
- Can features be traced to the western boundary? Combined (WB origins) (2-month chunks)
- Looking at the 6 events individually:
- RMS: Taux Tauy Correlation: Taux Tauy
- Quantities averaged over 160°E-160°W:
Actual values: Taux Tauy Curl Differences: Taux Tauy
Vectors: Differences from composite Overlay composite Overlay curl
- Sequence maps of all 6 events
- Variance ellipses, showing the variability among the 6 events and significance of the means.
Subjectively divided into 6 periods:
(Mar/Oct yr-1, Nov yr-1/Feb yr0, Mar/Jun yr0, Jul/Oct yr0, Nov yr0/Apr yr+1, May/Aug yr+1)
- Individual gifs
- Combined jpgs (1-3) Combined jpgs (4-6)
Combined pdfs (1-3) Combined pdfs (4-6)
- Plain and bold vectors only: gifs Stacked: pdf: 1-3 4-6 jpg: 1-3 4-6
SOLUTION:
- The Rossby model forced with the composite El Niño:
(Forcing was assumed to be zero before and after the 3-year composite.)
- Sequential maps of solutions:
- 24-month damping, c_k=3.5: Yr -1 Yr 0 Yr +1 Yr +2 Yr +3 Yr _4 Combined
- No damping, c_k=3.5: Yr -1 Yr 0 Yr +1 Yr +2 Yr +3 Yr _4 Combined
- Zonal transports: 24-month damping No damping
- RMS RW solution at 160°E-160°W Overlay N and S hemisphere
- RW solution along the western boundary:
- c_k=3.5 m/s: D=24 (Yrs -1 to +2) D=99 (Yrs -1 to +2)
- c_k=2.5 m/s: D=24 (Yrs -1 to +2) D=99 (Yrs -1 to +2)
- Zonal currents arriving at the WB: c=3.5/D=24 c=3.5/D=99 c=2.5/D=24 c=2.5/D=99
- Hofmullers of forcing and solution at each latitude
- (y,t) sections of h_RW and u_RW at various longitudes: 140°W 160°W 180° Western boundary
- Map of Rossby zonal transport during JFM Yr +1
- Mean incoming zonal transport at the WB
- Later work done in connection with interannual ORCA paper (see its page):
- Rossby h and u at the western boundary: h u
- Godfrey WBC from composite El Niño forcing
- Southern hemisphere: Years -1 to +2 To year +3
- Northern hemisphere: Years -1 to +3
- Total WBC, N and S hemisphere Exclude 1°S-1°N
- Complete WB solution: h, with (U_RW,WBC) vectors
- RMS of Rossby solution (compare N and S hemisphere):
h at 160°E-160°W WBC transport V_rw,ek,tot,wbc
- Meridional transport (WBC and zonally-integrated interior V):
- Line plots: 28.5°S-23.5°S 22.5°S-17.5°S 16.5°S-11.5°S 10.5°S-5.5°S
- Shaded fields (y,t): Southern hemisphere Northern hemisphere
- Include V_ekman: Southern hemisphere Northern hemisphere
- Interior V_rw,ekman,total in 20°longitude bands (Open browser wide)
- Interior V_rw,ekman,total in longitude bands (Open browser wide)
- Winds along the eastern boundary: Taux Tauy
- Rossby wave travel time across the basin
- Composite El Niño Rossby quantities on the equator: h
WBC transport arriving at the equator: 0.5°S/N 1.5°S/N Equatorial h due to WBC convergence
- A Kelvin wave solution with the composite winds:
- h U
- Compare the Rossby solution relative to the western boundary: h Difference
- Movies of the Rossby solution:
- h and (u,v) vectors (1.4Mb)
- Vrw,Vek,Vtot (2Mb)
- V shade, (u,v) vectors (2Mb)
- V shade (poleward/Eqward) and (u,v) vectors (2Mb)
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