Development and Effects of the Northward-Displaced ITCZ
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1 Development and Effects of the Northward-Displaced ITCZ Shang-Ping Xie IPRC, University of Hawaii First satellite cloud climatology (January ) WES & low-cloud feedback Northward displaced ITCZ Consequences: (1) equatorial annual cycle; (2) asymmetric ocean circulation. Brightness
2 Calm and Tornado Halley 1686 Eq Halley wrote about the ITCZ: it were improper to say there is any Trade Winds, or yet a Variable; for it seems condemned to perpetual Calms, attended with terrible Thunder and Lightning, and Rains so frequent, that our Navigators from thence call this part of the Sea the Rains.
3 NS asymmetry in East Pacific: Nicaragua (12N): 1208 Peru (12S): 11 mm/yr vs mm
4 Outgoing longwave radiation (OLR) in the Western Hemisphere Month Mitchell and Wallace (1992, JC)
5 Precip & SST(>27 o C) Tropical convection is confined to SST > 27 o C. Manabe et al. (1974, JAS) A secondary rainbelt forms just south of the equator around April when a secondary maximum of sea surface temperature appears in the Southern Hemisphere. The monthly charts of brightness, compiled by Tayler and Winston (1968), as observed by satellites, is most pronounced around April in qualitative agreement with the features of the model atmosphere.
6 Chicken & Egg Wind-Evaporation-SST (WES) Feedback Equator Xie & Philander (1994, Tellus )
7 Two-strip model for WES feedback Eq T N V Atmosphere T S Ocean σ = f (aα)/ε coupling coefficient Continental forcing triggers WES, displacing ITCZ.
8 Tilted coastline breaks the equatorial symmetry Downwelling Eq Upwelling
9 Continental asymmetry excites a westward-traveling coupled wave front. Xie and Saito, J. Climate (2001)
10 Westward control by continental geometry Xie & Saito (2001, J. Clim ) SST Land Land
11 Cloud effects COADS annual mean deep cloud Low cloud cools the SE ocean low cloud Strength meridional asymmetry
12 Consequence 1: Annual cycle SST 165W, 20N Galapagos, 90W, Eq
13 SST: Mean (>26 o C) & Annual Harmonic Xie (2004, in Hadley Circulation )
14 Equatorial Annual Cycle T u v Why annual? Why Strong in the east? Why propagate westward?
15 North ITCZ V Annual V Semi-annual 0 Annual V in both cases
16 Temperature along equator SST & u at Eq Veq 2 4
17 Consequence 2: Asymmetries in ocean circulation: North Equatorial Countercurrent (NECC) Annual-mean surface currents based on ship drift. K: Kuroshio, G: Gulf Stream, N and S: North and South Equatorial Currents, B: Brazil Current, and H: Humboldt Current. (WH05)
18 Asymmetry in ocean currents ITCZ
19 17S Subtropical cells Equatorial upwelling as manifested in SST minimum Cold/salty water converges onto the equator to compensate the upwelling, along the thermocline from the subtropics. The ventilation and upwelling maintain a sharp thermocline in the equatorial oceans. Eq 20N
20 Sea surface temperature observed by satellite infrared sensors Europe's heating system: warmer Gulf Stream (red) transports heat north while cold deep water flows south underneath (blue).
21 Rapid Climate Change Ice sheet discharge Gulf Stream shut down Ice sheet discharge
22 Close connection between the subpolar and tropical North Atlantic Cariaco Basin north of South America Wet tropical South America Warm Greenland Peterson et al. (2000, Science) Chiang (2004, Hadley circulation book)
23 Water-hosing response (Yr ) A. Timmermann, Y Okumura, et al GFDL_CM2.1 SST & wind stress NCAR CCSM2 Meridional (WES) mode & reduced NS asymmetry Southward displaced ITCZ, indicating a role of AMOC
24 January Summary Coupled (WES/cloud) feedback Northward-displaced ITCZ Continental geometry AMOC Equatorial annual cycle Circulation asymmetry (NECC)
25 First AGCM with a hydrological cycle & seasonal cycle SST-forced double ITCZ Manabe et al. (1974, JAS) A secondary rainbelt forms just south of the equator around April when a secondary maximum of sea surface temperature appears in the Southern Hemisphere. The monthly charts of brightness, compiled by Tayler and Winston (1968), as observed by satellites, is most pronounced around April in qualitative agreement with the features of the model atmosphere.
26 Bjerknes feedback & zonal asymmetry SST & Precip Z20
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