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LBA/Physical Climate. Moist Convection in the Amazon. Things models should do that LBA data has pointed out. easterlies/westerlies and convection land features effects on convection forest vs non-forest topography river vs land. Rondônia 1999 850 hPa zonal wind - CPTEC.
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LBA/Physical Climate Moist Convection in the Amazon
Things models should do that LBA data has pointed out • easterlies/westerlies and convection • land features effects on convection • forest vs non-forest • topography • river vs land
Summers of 1980 to 1999 Carvalho et al , 2002
Summers of 1980 to 1999 Carvalho et al , 2002
Petersen, 2000 Blakeslee,2000 Blakeslee, 2000
Hourly rainfall rate from TOGA radar Anagnostou & Morales, 2002
GOES Hourly average cloud fraction TOGA
Time of first radar echoes S-Pol Jan/Feb 1999 westerlies easterlies 6:20 7:20 8:20 9:20 10:20 11:20 12:20 Local Time
TRMM-LBA Region: Forest vs. Non-Forest FOREST TOGA Profiler NON-FOREST SPOL Carey et al 2001
TRMM-LBA Region: Topography “Elevated” >= 223 m “Non-Elevated” < 223 m Carey et al 2001
Effects of Deforestation on Rain Rate Statistics Carey et al 2001
TRMM-LBA: Effect of land type on rainfall statistics KEY: Fractional Rain Duration = % of grid boxes for land type category with rain (R > 0) Fractional Grid Coverage = % of all grid boxes for land type category Ru = Unconditional Mean Rain Rate Rc = Conditional Mean Rain Rate NE = Non Elevated (< 223 m) E = Elevated ( 223 m) F = Forested NF = Non Forested Carey et al 2001
Effects of Deforestation on Cumulative Rain Depth Carey et al 2001
Land Effects on Rain Depth Carey et al 2001
Effects of Elevation on Rain Depth Carey et al 2001
Elevated Only Forested Non-Forested Forested Non-Forested Non-Elevated Only Carey et al 2001
23 July 2001 Tapajós (from Pindobal to Boim and back) 28 July 2001 Tapajós & Amazonas (red line: temperature where the two rivers merge)
West East South AWS Jamaraquá 24 July / 1 August 2001 North
Pressure (mb) Winds at Belterra radiosonde
Winds and potential temperature Belterra radiosonde