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This study explores methods to improve convective sensitivity to tropospheric relative humidity, presented by Richard Neale (NCAR) and Brian Mapes (RSMAS, University of Miami) at the AMWG Meeting on March 20, 2006. The research focuses on analyzing moisture sensitivity in the free troposphere, emphasizing the role of entrainment and cloud microphysics. Results indicate significant improvements in rainfall predictions for JJA (June-July-August), with reductions in systematic errors in precipitation forecasting and enhancements in the representation of diurnal rainfall cycles.
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Improving Convective Sensitivity to Tropospheric Relative Humidity Richard Neale (NCAR) and Brian Mapes (RSMAS, University of Miami) AMWG Meeting, Mar 20, 2006
Free Troposphere Altitude PBL 0 Moisture sensitivity + Undilute Dilute Entraining Plume -Cloud water (1 g/kg) -Freezing below 273K -Entrainment chosen Pseudoadiabatic Ascent -No cloud water -No freezing -No entrainment (but implied) 0.2 X 100% + 0.8 X RHclr = 1.0 X 10% => RHclr = -12.5%
Dilute Undilute JJA FV 2x2.5 1979-1988 Dilute minus GPCP Undilute - GPCP Dilute Undilute
Undilute minus ERS Dilute minus ERS
Dilute Undilute
CAPT CCCP-ARM ParametrizationTestbed Dilute Undilute
Dilute Variance of 5-day ave rainfall Undilute
Dilute ENSO Warm minus Cold DJF Prect. Undilute
Amplitude of Diurnal Cycle (mm/day) (JJA 1984) CAM3 (T85) 3B42 TRMM TMI/PR
Local Time of Daily Rainfall Max CAM3 (T85) 3B42 TRMM TMI/PR
Overall JJA significant improvements (DJF some improvements Africa/Australia rainfall) -Reduction in S. Indian Ocean ITCZ -Enhanced Asian-Monsoon rainfall -Reduced twin ITCZ bias -Improved tropospheric humidity, MSE structure -Decrease in large Pacific high PSL error -Reduction in amplitude of diurnal cycle of rainfall/increased night-time rainfall -More realistic balance of convective/stratiform rainfall -CAPT tests, < half the error through day 5 forecast -ENSO wider Pacific equatorial signal (tentative) -Enhanced subseasonal variability (too much?) Some deterioration -Indian monsoon precipitation excess -South Atlantic circulation pattern -No change or slightly earlier diurnal cycle rainfall maximum