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Clouds, climate, challenges
Herman Russchenberg
Remote Sensing of the Atmosphere
Earth-atmosphere energy balance
The radiation balance: a status quo
Solar energy
No atmosphere
Too cold to live in
Greenhouse
gases
Too warm to live in
Cooling clouds
Nice in the shade
height
-20 +24 +14
Clouds and climate
Clouds scatter light
Clouds absorb heat
Evaporation cools
Condensation warms
Cooling Warming
A bit about cloud formation
Condensation
level
No aerosols A few aerosols Many aerosols
Moist air parcels
Clouds
rainfall formation
Large droplets:
rainfall
More aerosols
Delayed rainfall
Longer cloud lifetime
Sustained impact
on radiation
DirectwarmingduetoCO2
Responseoftheearth
Additionalwarming
Global warming: state of the art
Short wave fluxes Long wave fluxes
Number concentration
Liquid water content
Optical depth = total extinction of radiation due to absorption and scattering
Example of flux calculations
Neg. Feedback
Pos. Feedback
Present
Perturbed Future
Strong Pos. Feedback
Possible cloud responses to warming
Greenland melt, July 2012
Bennartz et al, 2013, Nature
Impact of thin low level clouds on
surface temperature
How much light reaches the earth?
How much is reflected into space?
How much heat leaves the earth?
How much water condenses or evaporates?
How much water precipitates?
The cloud questions
50 km
50km
Climate grid
Why are clouds so difficult?
Complexity of the problem
Large variety of cloud types
Global information needed
A large range of temporal and spatial scales
A multitude of different physical parameters
How to solve this problem?
Models Observations
Cesar Observatory
Delft University of Technology, KNMI, Wageningen University and Research
Utrecht University, RIVM, ECN, TNO , European Space Agency
Groeten uit Cabauw
Observation of light rain with different instruments
lidar radar
time
height
Why multi-sensor strategies?
short wavelength long wavelength
1.  Cloud thickness
2.  Liquid water content
3.  Droplet size
4.  Number concentration
5.  Vertical profile
What do we have to know?
Case study: water clouds
Assume a cloud model
Cloud base
Cloud top
H
Expected response of radar
Expected response of lidar
Number of droplets
Water content
radar lidar radiometer
Inside stratocumulus
Radar reflection [dBZ]
Total amount of water [g/m^2]
Time [utc]
estimate cloud parameters
Droplet concentration Profile particle size
Courtesy: Christine Brandau
Extinction Optical thickness
radiative properties
Questions
•  Can we use radiation measurements to
evaluate cloud retrievals?
•  What’s the impact of the assumed vertical
cloud profiles on radiation?
Evaluation with radiative closure
•  retrieval of cloud microphysics
•  calculate the surface radiation
•  compare with surface radiation measurements
•  ARM mobile facility, Germany, 2007
•  Cloud radar, ceilometer, microwave radiometer
•  Pyranometer surface irradiance
Models of the vertical cloud structure
Three models for
different vertical
variations within the
cloud
1.  Homogeneous Mixing
2.  Scaled-Adiabatic
Stratified
3. Vertically Uniform
The 3 vertical cloud
models can
reproduce the
radiation at surface
with small biases
Surface radiation closure
Impact of the vertical cloud structure
Three models for different
vertical variations within the
cloud
1.  Homogeneous Mixing
2.  Scaled-Adiabatic Stratified
3. Vertically Uniform
Way of the future: integration
space, ground, air, models
Ice clouds
Water clouds
Mixed phase clouds
drizzle
rainfall
Energy fluxes, evaporation
Water balance
Aerosols
Water vapour
Trace gases
radiation

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