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EPIC 2001 Workshop, September 2003, Boulder, Colorado

EPIC 2001 Workshop, September 2003, Boulder, Colorado

EPIC 2001 Workshop, September 2003, Boulder, Colorado. Major atmospheric focus in EPIC2001 cold tongue region: Latitude-height structure and dynamics in lower troposphere. Robust observed features compared to NCEP GDAS. Deepening cloud-topped mixed layer as air flows over SST front.

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329 views • 22 slides
MLS Cloud Forcing: IWC validation & Cloud Feedback Determination

MLS Cloud Forcing: IWC validation & Cloud Feedback Determination

MLS Cloud Forcing: IWC validation & Cloud Feedback Determination. MLS Science Team Teleconference: June 8, 2006 Dan Feldman Jonathan Jiang Hui Su Yuk Yung. Cloud Forcing Intro. Clouds are a prominent radiative feedback mechanism with substantial impact on SW and LW radiative budget

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346 views • 19 slides
Update on the 2-moment stratiform cloud microphysics scheme in CAM

Update on the 2-moment stratiform cloud microphysics scheme in CAM

Update on the 2-moment stratiform cloud microphysics scheme in CAM. Hugh Morrison and Andrew Gettelman National Center for Atmospheric Research CCSM Atmospheric Model Working Group Meeting Feb 12, 2008 Thanks to Steve Ghan (PNNL). History. Development began after 2006 AMWG meeting.

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300 views • 17 slides
Update on the 2-moment stratiform cloud microphysics scheme in CAM

Update on the 2-moment stratiform cloud microphysics scheme in CAM

Update on the 2-moment stratiform cloud microphysics scheme in CAM. Hugh Morrison and Andrew Gettelman National Center for Atmospheric Research CCSM Atmospheric Model Working Group Meeting Feb 12, 2008 Thanks to Steve Ghan (PNNL). History. Development began after 2006 AMWG meeting.

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285 views • 17 slides
MLS Cloud Forcing: IWC validation & Cloud Feedback Determination

MLS Cloud Forcing: IWC validation & Cloud Feedback Determination

MLS Cloud Forcing: IWC validation & Cloud Feedback Determination. MLS Science Team Teleconference: June 15, 2006 Dan Feldman Jonathan Jiang Hui Su Yuk Yung. Cloud Forcing Intro. Clouds are a prominent radiative feedback mechanism with substantial impact on SW and LW radiative budget

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316 views • 15 slides
Cloud-climate feedbacks: what we think we know and why we think we know it

Cloud-climate feedbacks: what we think we know and why we think we know it

Cloud-climate feedbacks: what we think we know and why we think we know it. David Mansbach 14 April 2006. ?T 2 4. ?T 2 4. T 2 <T 0 (slightly). T 1 <T 0. ?T 1 4. ?T 1 4. ?T 0 4. Clouds, in general and today Greenhouse effect, albedo effect, and satellite measurements

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Solar cloud forcing = Rs - Rs 0 Longwave cloud forcing = Rl - Rl 0 Compare buoy cloud forcing to

Solar cloud forcing = Rs - Rs 0 Longwave cloud forcing = Rl - Rl 0 Compare buoy cloud forcing to

Surface Cloud Forcing in the East Pacific Stratus Deck/Cold Tongue/ITCZ Complex Meghan F. Cronin (NOAA PMEL) Nicholas A. Bond (JISAO PMEL/UW) Chris Fairall (NOAA ETL) Robert A. Weller (WHOI) submitted to J. Climate. Solar cloud forcing = Rs - Rs 0 Longwave cloud forcing = Rl - Rl 0

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177 views • 6 slides

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