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Using Atrain observations to evaluate clouds in CAM

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Using A-train observations to evaluate clouds in CAM. Jennifer Kay (NCAR/CSU) ... Thanks to Hugh Morrison (NCAR) Active instruments such as radar or lidar ... – PowerPoint PPT presentation

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Title: Using Atrain observations to evaluate clouds in CAM


1
Using A-train observations to evaluate clouds in
CAM
  • Jennifer Kay (NCAR/CSU)
  • Andrew Gettelman (NCAR)
  • Thanks to Hugh Morrison (NCAR)

2
Spaceborne radar and lidar 101
  • Active instruments such as radar or lidar
  • emit a pulse.
  • The pulse is either reflected back to the
    instrument, continues downward, or is absorbed
    and lost.
  • The reflected signal is a measure of vertical
    cloud and aerosol structure.



CloudSats 94 GHz (3 mm) radar measures cloud
particles, raindrops, and snowflakes. CALIPSOs
532/1064 nm lidar measures aerosols and thin
clouds.



3
CloudSat and CALIPSO Data Sampling
4
Global Zonal Mean Cloud Fraction(CloudSatCALIPSO
)
More data plots http//www.cgd.ucar.edu/cms/jenka
y/
5
The A-train satellite data provide a unique view
of Arctic clouds.
DJF Low Cloud Maps
CloudSatCALIOP (radarlidar)
ISCCP D2 (infrared)
Warren (surface obs.)
6
How do we use CloudSat data to evaluate CAMs
clouds?
  • Important factors to consider
  • How do we define a cloud? (radar sensitivity)
  • - Are these data representative? (short data
    record)
  • Clear advantages of CloudSat data
  • first measure of global cloud vertical structure
  • measured cloud quantities such as dBZ can be
    directly compared to simulated model cloud
    quantities (w/MG microphysics)

7
The importance of cloud definition
JJA low cloud cover
8
Variability in the short CloudSat record
Western Arctic cloud reductions from 2007 to 2006
are associated with differing atmospheric
circulation patterns.
9
Overall GoalApple-to-Apple ComparisonsCloudSat
vs. CAM-dev
CAM-dev ? CAM 3.6 ? CAM 3.5 MG microphysics
empirical radar reflectivity simulator 3 years,
6-hourly output
Some important cloud definitions cloud ? -30 dBZ
lt cloud lt 10 dBZ cloud fraction ? cloud / total
-cloud fraction can be by-profile or
by-height
  • TODAY, preliminary comparisons of
  • Global low cloud cover
  • Global high cloud cover
  • dBZ-ht histograms, cloud profiles in specific
    regions

10
JJA Low Cloud Fraction Maps
CloudSat Observations (1-3 km, by-profile)
CAM 3.6 (1-3 km, by-profile)
11
DJF High Cloud Fraction Maps
CloudSat Observations (7-22 km, by-profile)
CAM 3.6 (7-22 km, by-profile)
12
Tropical Comparison(CFAD, Cloud fraction
by-height)
13
Sub-tropics Comparison(CFAD, Cloud fraction
by-height)
14
Mid-Latitude Storm Track (CFAD, Cloud fraction
by-height)
15
Future Plans
Conclusions
  • CloudSat data are a unique tool for evaluating
    the representation of clouds in next-generation
    climate models.
  • Cloud definition is key to useful comparisons.
  • Much more work to be done
  • Add CFMIP ISCCP/CloudSat/CALIPSO simulator to
    CAM
  • Use DART to constrain CAM dynamics, look at
    clouds
  • Actively engage with model evaluation efforts
    for CAM4

PLUG Does your work incorporate model-obs cloud
comparisons? I can provide cloud data to help you
evaluate model performance E-mail me
(jenkay_at_ucar.edu) or Talk to me later.
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