gsfc. glaciation level and vertical profile of droplet size associated with cloud-aerosol...
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![Page 1: GSFC. Glaciation Level and Vertical Profile of Droplet Size Associated with Cloud-Aerosol Interactions (D. Rosenfeld) Clean Polluted](https://reader036.vdocuments.mx/reader036/viewer/2022062422/56649efa5503460f94c0c0ef/html5/thumbnails/1.jpg)
GSFC
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GSFC
Glaciation Level and Vertical Profile of Droplet Glaciation Level and Vertical Profile of Droplet Size Associated with Cloud-Aerosol InteractionsSize Associated with Cloud-Aerosol Interactions
(D. (D. Rosenfeld)Rosenfeld)
Glaciation Level and Vertical Profile of Droplet Glaciation Level and Vertical Profile of Droplet Size Associated with Cloud-Aerosol InteractionsSize Associated with Cloud-Aerosol Interactions
(D. (D. Rosenfeld)Rosenfeld)
Clean Polluted
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GSFC
Glaciation Level and Vertical Glaciation Level and Vertical Profile of Droplet Size Profile of Droplet Size
Associated Associated with Cloud-Aerosol with Cloud-Aerosol
InteractionsInteractions(D. Rosenfeld)(D. Rosenfeld)
Glaciation Level and Vertical Glaciation Level and Vertical Profile of Droplet Size Profile of Droplet Size
Associated Associated with Cloud-Aerosol with Cloud-Aerosol
InteractionsInteractions(D. Rosenfeld)(D. Rosenfeld)
Clean
Clean Cases
Polluted Cases
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GSFC
Scientific Scenario for CLAIM-3D:Scientific Scenario for CLAIM-3D:Scientific Scenario for CLAIM-3D:Scientific Scenario for CLAIM-3D:
Today, Microphysical Effects on Clouds:
•Studied from Cloud Top with many assumptions
•With complicated/limited in situ aircraft measurements.
The CLOUD SCANNER add:•Instantaneous measurements of the cloud vertical profile of microphysics, thermodynamic phase, and cloud 3D properties
•Simultaneous measurements of aerosol properties
Today, Microphysical Effects on Clouds:
•Studied from Cloud Top with many assumptions
•With complicated/limited in situ aircraft measurements.
The CLOUD SCANNER add:•Instantaneous measurements of the cloud vertical profile of microphysics, thermodynamic phase, and cloud 3D properties
•Simultaneous measurements of aerosol properties
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GSFC
Cloud Scanner Measurements Cloud Scanner Measurements During the LBA/SMOCC/Racci During the LBA/SMOCC/Racci
Experiment 2002Experiment 2002
Cloud Scanner Measurements Cloud Scanner Measurements During the LBA/SMOCC/Racci During the LBA/SMOCC/Racci
Experiment 2002Experiment 2002
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GSFC
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GSFC
350 nm) 2500
Ice
Water
350 (nm) 2500
Ice
Water
Ice
Water
Ice
Water
Ice
Water
Clear Sky
Clo
ud
Su
rfac
e
ice
water
Glaciation Level
Clear Sky
Clo
ud
Su
rfac
e
ice
water
Glaciation Level
350 (nm) 2500
Prototype Results
•Thermodynamic Phase •Droplet Size
•Temperature •Aerosol Type + Amount
Aircraft Proof of Concept Aircraft Proof of Concept Cloud Side MeasurementsCloud Side Measurements
Cloud Top
Cloud Base
Glaciation
Conceptual Model
Mixed Phase
5
15
25
35
45
55
0 10 20 30 40 50
Effective Radius (um)
clo
ud
hei
gh
t (A
.U.)
5
15
25
35
45
55
0 2 4 6 8 10 12 14
reflectances 2.1 and 2.25um (A.U.)
clo
ud
hei
gh
t (A
.U.)
Retrieved Eff. Radius
Refl. 2.10um
Refl. 2.25um
0 Effective Radius (m) 50
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GSFC
King et. all 1997King et. all 1997King et. all 1997King et. all 1997
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GSFC
Reflectances from Side and Top of a
Cylindrical Cloud ( z=50, x=30)
0
1
2
3
4
5
6
7
8
0 0.2 0.4 0.6 0.8 1
Reflectance
hei
ght
(km
) Cloud Top
Cloud Side
2.1 m
0.66m
o = 60, = 40
3-D Radiative Transfer Studies:
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GSFC
v=60,
v=180
v=60,v=0
o=60,o=0
v=0,v=0
0 2 4 6
0
2
4
6
x (km)
y (km)
0.00 0.25 0.50 0.75 1.00
v=60,v=902 4 6
2
4
6
x (km)
y (km)
0 25 50 75 100 125 150optical depth
A. Marshak – 3D Cloud Simulation
Input (optical depth)Output
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GSFC
100km
Default Simple Scanning ModeThe instrument points towards the illuminated side of the clouds and scans as the satellite moves (see simple scan movie). An extra feature and also descope option can be a second simple camera (between 1 to 3 visible wavelengths for parallax observations of the cloud structure).
Additional 1- view angle for
Parallax(also for descope option)
Multi Spectral Cloud ScannerView direction
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GSFC
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GSFC
100km
Geometry of the Multi-Angle ScanThe instrument view angle changes from forward to backward geometries as it scans a
selected region (see full scan movie)
~ 400km
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GSFC
~ 400km
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GSFC
CLAIM-3D Observing Geometry CLAIM-3D Observing Geometry (fig 1)(fig 1)
CLAIM-3D Observing Geometry CLAIM-3D Observing Geometry (fig 1)(fig 1)
Side viewSide view
International collaboration:Enhanced Polder
International collaboration:Enhanced Polder
Cloud ScannerCloud
Scanner
3D view3D view
Min. 100km swath
Cloud Structure And
Vegetation Hot Spot
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GSFC
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GSFC
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GSFC
TMI ImageTMI Image
60dg View 60dg View angleangle
Courtesy of Antony Courtesy of Antony DavisDavis
TMI ImageTMI Image
60dg View 60dg View angleangle
Courtesy of Antony Courtesy of Antony DavisDavis
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GSFC
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GSFC