Focus on deep and shallow convection, and turbulence - cmmap

More documents

Recommendations

Info

High-Resolution Simulation of Shallow-to-Deep Convection Transition over Land (Khairoutdinov and Randall 2006) Figure 8. PDF of cloud size as a function of height shown for three different simulation times. Mean and standard deviations are shown by the white and yellow lines, respectively. 150 km x 150 km, 100 m grid size, 6 h
Grid-size dependence in a large domain LES •RICO trade wind cumulus case: 19 Jan 2005 •Control simulation: 100 m horizontal grid size, 40 km x 40 km domain, 24 h simulation •Grid-size dependence simulations: 500 m, 1000 m, 2000 m, 4000 m horizontal grid sizes, otherwise unchanged from control •Next: stereo images of clouds at 12 h
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: Proposed Evaluation Methods •Benc
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 and 36: 5000 4500 4000 Cloud Water Mixing R
Page 37: Proposed Evaluation Methods •Obse

Focus on deep and shallow convection, and turbulence - cmmap

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?