Focus on deep and shallow convection, and turbulence - cmmap

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5000 4500 4000 Rain Water Mixing Ratio 100 m 500 m 1000 m 2000 m 4000 m 3500 height (m) 3000 2500 2000 1500 1000 500 0 0 1 2 3 4 5 6 7 rain water mixing ratio (g/kg) x 10 !3 Figure 4:
Proposed Evaluation Methods •Observational datasets •High-resolution cloud properties from satellites: MODIS, ISCCP, etc •Vertical structure of clouds: CloudSat, ARM MMCR, TRMM •High-resolution hourly precipitation from rain gage and unbiased radar •Surface mesonet observations of T, RH, p, u, v •Aircraft-based measurements during field experiments
Page 1 and 2: Focus on deep and
Page 3 and 4: from Arakawa and Jung (2003)
Page 5 and 6: Boundary layers in deep precipitati
Page 7 and 8: Outline of this talk •Introductio
Page 9 and 10: Science Issues Representation of th
Page 11 and 12: Boundary-layer Clouds in a Multisca
Page 13 and 14: Continental shallow cumuli (ARM) LE
Page 15 and 16: Proposed Evaluation Methods •Benc
Page 17 and 18: Grid-size dependence in a large dom
Page 19 and 20: 500 m
Page 21 and 22: 2000 m
Page 23 and 24: 100 m
Page 25 and 26: 1000 m
Page 27 and 28: 4000 m
Page 29 and 30: Avg’d to 500 m log 10 of Liquid W
Page 31 and 32: 1000 m log 10 of Liquid Water Path
Page 33 and 34: last 6 hrs 100 m 500 m 1000 m 2000
Page 35: 5000 4500 4000 Cloud Water Mixing R

Focus on deep and shallow convection, and turbulence - cmmap

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