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The main moisture flux sources in SAMS and evolution of the system. Iracema F.A.Cavalcanti Daniel R. Andres Adma Raia Silvio Nilo Henrique Barbosa. CPTEC/INPE. Models and simulations. AGCM CPTEC/COLA T62L28 (~200 km) 10 years simulation (1982-1991) 50 years simulation (using 1980-2002)
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The main moisture flux sources in SAMS and evolution of the system Iracema F.A.Cavalcanti Daniel R. Andres Adma Raia Silvio Nilo Henrique Barbosa CPTEC/INPE
Models and simulations • AGCM CPTEC/COLA T62L28 (~200 km) • 10 years simulation (1982-1991) • 50 years simulation (using 1980-2002) • Eta Regional Model (40 km) • DJF simulation (1996-2000)
1996 to 2000 DJF SIMULATION Eta Regional Model 40 km Downscale from CPTEC/COLA AGCM precipitation MOISTURE FLUX Moisture flux
EL NINO CPTEC/COLA AGCM
LA NINA CPTEC/COLA AGCM
EL NINO 82/83- LA NINA 88/89 CPTEC/COLA AGCM
PRECIPITATION DIURNAL CYCLE DJF 06 GMT 12 GMT 00 GMT 18 GMT
DJF WIND FLOW AT 850 hPa 12 GMT 06 GMT 18 GMT 00 GMT
Submonthly monsoon variability LLJ ZCAS Dependence on the low level flow
DJF 10 YEARS AVERAGE GRELL ENSEMBLE CONVECTION SCHEME MCGA CPTE/COLA
MONTHLY AND SEASONAL CHANGES • MONTHLY CHANGES OF MOISTURE FLUX : LARGE DIFFERENCES IN DJF AND JJA. • MOISTURE FLUX FROM NORTH AND SOUTH ATLANTIC OCEAN TO THE AMAZON REGION AND THEN TO CENTRAL AND SOUTHEAST BRAZIL AND FROM SOUTH ATLANTIC DIRECTLY TO SE, IN DJF. • IN JJA THE MOISTURE FLUX IS DIRECTED FROM ATLANTIC OCEAN TO NORTHWEST S.A.
CHANGES IN MOISTURE FLUX /WIND FLOW AT LOW LEVELS • DIURNAL SCALE • SUBMONTHLY SCALE • SEASONAL SCALE • INTERANNUAL SCALE • INTRASEASONAL SCALE ?
ACKNOWLEDGEMENTS VAMOS/CLIVAR, JOSS/UCAR