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March 2005VAMOS/MESA Evaluation of a Nested Model Ensemble Climatology for South America: Annual Cycle, Interannual Variability and Rainy Season Onset Anji Seth (Sara Rauscher and Brant Liebmann) International Research Institute for Climate Prediction
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March 2005VAMOS/MESA Testing a nested model for variability/predictability Hindcasts ( ‘ perfect forcing ’ ) 1.Extreme Seasons [Seth and Rojas (2003); Rojas and Seth (2003); Seth et al. (2004)] RegCM2 / CCM3 2.Sensitivity Studies [Seth and Rojas (2003); Rauscher et al. (2005)] Surface & Domain RegCM2 / CCM3; Domain RegCM3 / ECHAM4.5 3.Nested Model Ensemble Climatology [Seth et al. (2005)] Convection Grell / Emanuel RegCM Simulations Reanalyses GCM Observed SST
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March 2005VAMOS/MESA Outline Experiments Results from Reanalyses and ECHAM driven RegCM/Grell Annual cycle Interannual variability Rainy season onset Reanalyses driven RegCM/Emanuel Grell - Emanuel differences ECHAM driven RegCM/Emanuel Preliminary Conclusions
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March 2005VAMOS/MESA Models and Experiments 1. RegCM3/Grell (Giorgi et al., 2005) Convection (Grell 1993) A-S (stability) closure Ocean (Zeng et al., 1998) BATS (Dickinson et al, 1993) Domain: 111x138x18 Resolution: 80 km Period: Jan 1982 - Dec 1998 Boundary Conditions: NCEP/NCAR ECHAM4.5 (ensemble) 2. RegCM3/Emanuel Emanuel (1991, 1999) Jan 1996 - Dec 1998 AmazonNordeste Monsoon Southeast
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March 2005VAMOS/MESA 1982-1996 Annual Cycle: Lat-Pentad Precipitation: 65W-40W CMAP NN-RegCMECHAMEC-RegCM
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March 2005VAMOS/MESA 1996-98 Precipitation (mm/day Amazon MonsoonSoutheast Nordeste
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March 2005VAMOS/MESA 1996-1998 Precipitation CMAP RegCM GRELL JFMJAS
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March 2005VAMOS/MESA 1982-1996 FMAM Nordeste Preca vs. SSTa CMAP ECHAM NN-RegCM EC-RegCM
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March 2005VAMOS/MESA 1982-1996 NDJ Southeast Preca vs. SSTa CMAP ECHAM NN-RegCMEC-RegCM
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March 2005VAMOS/MESA Calculation of Onset and Withdrawal (Liebmann and Marengo, 2001) R(n) = daily climatological rainfall R = annual mean daily rain rate day 0 = starting day of summation (within dry season - Jul 1) Objective method This definition is local because it depends on the climatology of each region of interest. The onset date can change depending on the start date of the summation. ONSETWITHDRAWAL Daily Precipitation Anomaly Sum of Daily Precipitation Anomalies
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March 2005VAMOS/MESA Mean Date of Onset, Withdrawal, and Length of Rainy Season: July 1982- June 1996
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March 2005VAMOS/MESA Northeast Onset, Withdrawal, and Length of Rainy Season: July 1982- June 1996
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March 2005VAMOS/MESA 1996-1998 Precipitation CMAP JFM JAS RegCM/EMANUEL RegCM/GRELL
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March 2005VAMOS/MESA 1996-98 Precipitation (mm/day) Amazon Monsoon Nordeste Southeast
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March 2005VAMOS/MESA 1996-98 Amazon Precipitation (mm/day)Surface Air Temperature (°C) Evapotranspiration (mm/day)Surface Sensible Heat Flux (W/m^2)
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March 2005VAMOS/MESA Specific Humidity and Temp: Amazon
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March 2005VAMOS/MESA 1996-1998 JFM SLP GRELL, EMANUEL Reanalyses
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March 2005VAMOS/MESA 1996-1998 JFM Vertically Integrated Moisture tranport GRELL EMANUEL
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March 2005VAMOS/MESA 96-98 Nordeste: Prec, Ts, ET, H
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March 2005VAMOS/MESA 1996-1998 Precipitation CMAP JFM JAS ECHAMECHAM-RegCM/EMANUEL
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March 2005VAMOS/MESA 1996-98 Precipitation (mm/day) AmazonNordeste MonsoonSoutheast
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March 2005VAMOS/MESA Discussion Annual Cycle - RegCM/Grell captures the seasonal cycle in Northeast, Monsoon and Southeast, but exhibits a substantial dry bias in Amazon. Interannual Variability - Northeast variability is well captures by the model versions. The Southeast relationship to ENSO is weak at best in RegCM/Grell. Rainy season onset - Onset is well simulated in Northeast and Southeast (better than GCM). Monsoon region onset not as good. Emanuel Scheme - improves the large scale circulation (SLP, winds, moisture transport) and precipitation in Amazon. Improves annual cycle in Northeast, Amazon, Southeast. Too wet in Monsoon.
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March 2005VAMOS/MESA
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March 2005VAMOS/MESA GrellEmanuel closure Destabilization ratePrognostic quasi- equilibrium Modifies by Mass flux Downdrafts? yes comment Simple cloud modelBouyancy sorting and mixing hypothesis
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March 2005VAMOS/MESA Rainfall anomalies in Nordeste, 1850-1995 Rainfall, SLP, Surface wind anomalies SST and Surface wind anomalies Wallace et al., 1998
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March 2005VAMOS/MESA CLIVAR/VAMOS, Kousky/Halpert Features of South American Warm Season Rains
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March 2005VAMOS/MESA
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March 2005VAMOS/MESA South America: Population Density coastal populations ecosystem diversity arid Nordeste: 60% rural Southeast: population And economic center, agricultural breadbasket
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March 2005VAMOS/MESA JanJul (Nicolini et al. 2002)
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March 2005VAMOS/MESA FMAM 1983 (Rojas and Seth 2003) FMAM 1985 1985-1983 CMAPCCM3CCM3>RegCM2
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March 2005VAMOS/MESA 96-98 Southeast: Prec,Ts, ET, SH
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March 2005VAMOS/MESA 96-98 Monsoon: Prec,Ts,ET,H
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March 2005VAMOS/MESA Temperature (ºC): Amazon, Nordeste Monsoon, Southeast
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March 2005VAMOS/MESA Specific Humidity: Amazon, Nordeste Monsoon, Southeast
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March 2005VAMOS/MESA Monthly Evolution of the 6 mm/day Isohyet (Onset Period) 1982-1996 Monthly Climatology
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March 2005VAMOS/MESA Monthly Evolution of the 6 mm/day Isohyet (Withdrawal Period) 1982-1996 Monthly Climatology
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March 2005VAMOS/MESA Precipitation Onset and Withdrawal: Definitions in Monsoon Regions Wind-based Amount or accumulation of precipitation (or OLR as a precipitation proxy) –e.g., Kousky (1988) Onset occurs when: –climatological OLR falls below 240 W m -2 in a given pentad AND –10 of 12 previous pentads have OLR > 240 W m -2 –10 of 12 subsequent pentads have OLR < 240 W m -2 Non-local Sensitive to threshold criteria
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March 2005VAMOS/MESA Monsoon Region Onset, Withdrawal, and Length of Rainy Season: July 1982- June 1996
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March 2005VAMOS/MESA Southeast Region Onset, Withdrawal, and Length of Rainy Season: July 1982- June 1996
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