calipso validation and data quality improvement
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CALIPSO VALIDATION and DATA QUALITY IMPROVEMENT. EECLAT T0, J. Pelon. Data quality Improvement. - PowerPoint PPT PresentationTRANSCRIPT
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CALIPSO VALIDATION and DATA QUALITY IMPROVEMENT
EECLAT T0, J. Pelon
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V4 L1 products to include new calibrations of 532 nighttime (stratospheric aerosols, new GEOS 5.7 met data) and 532 daytime (signal slope correction, D/N calibration) and 1064 nm (D+N, reference scene selection)
Data quality Improvement
Example of results at 1064 nm for a one month test performed at LaRC
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Elaboration of V4 L2 products under discussion
Continuation of Validation effort (impact of calibration, new products)
Aerosol characterization (regional and global)
Cloud characterization using CALIOP/IIR
Improvement of Cloud microphysical products in V4
Ongoing Case studies and statistical analyses for further characterization of processes at the regional and global scales (aerosol transport, dust, radiative impacts …)
Data quality Improvement
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Analysis of Cloud Properties
Cloud properties in V3 : - Structure, OD and IWC (CALIOP)- e, OD, IWP (IIR/CALIOP)
New MODIS coll. 6 with cloud models leading to reduced ODs in better agreement with IIR
Discussion on changes in Lidar ratio for CALIOP OD retrieval (+15 -20 %)
Josset et al., JGR, 2012
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IIR and CALIOP cirrus OD
Single-layered semi-transparent clouds, altitude > 7km, randomly oriented ice (CALIOP flag), 5-km resolution, ocean, all latitudes,
day, January 2008-2011.
• CALIOP data : Lidar ratio=31.5 and Multiple scattering factor=0.6
• Expected: IIR « absorption » ODeff ~ 0.5 x CALIOP total visible OD
CALIOP OD/IIR ODeff = 2.0 +/-10% in agreement with expectations and sensitivity studies.
Sensitivity of IIR retrievals: good agreement with CALIOP down to ODs smaller than 0.05
Garnier et al, ILRC, 2012
Expected
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Analysis of Cloud Properties
Cloud properties in V3 : - Structure, OD and IWC (CALIOP)- e, OD, IWP (IIR/CALIOP)
New results on Cloud Microphysics from Combined CALIPSO INSTRUMENTS (IIR + CALIOP) + RTM taking advantage of IR-lidar complementarities for Day & Night analyses)
Release of L2b cloud particle size & IWP products,
Results presented in JAMC Part II (Garnier et al., submitted 2012)
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IIR IWP for High dense clouds
January 2009 D+N
First L3 IIR test products obtained at ICAREto be part of CALIPSO L3 cloud product
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IWC values directly derived from Deff and AODs using CALIOP Single-layered semi-transparent cloud, altitude > 7km, T° < 233K, data over ocean, all latitudes, Day+Night
White solide line: from CIRCLE 2 campaign in Europe (Mioche et al, JGR, 2010)Green triangles from ARM & TOGA-COARE (McFarquhar et al., 2003)
January 2011
IWC = f(extinction) from IIR in good agreement with in situ
IWC/ext (Heymsfield et al, GRL, 2005) used in Version 3 CALIOP shows larger values
IWC Analysis from IIR
Garnier et al., JAMC, subm. 2012
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