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Published byAnnabelle Morris Modified over 9 years ago
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Direct aerosol radiative forcing based on combined A-Train observations and comparisons to IPCC-2007 results Jens Redemann, Y. Shinozuka, M. Vaughan, P. Russell, M. Kacenelenbogen, J. Livingston, O. Torres, L. Remer BAERI – SRI - NASA Langley - NASA Ames – NASA Goddard - UMBC http://geo.arc.nasa.gov/AATS-website/ email: Jens.Redemann-1@nasa.govJens.Redemann-1@nasa.gov
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Goals and Motivation Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions MODIS OMI CALIOP Goal: To use A-Train aerosol obs to constrain aerosol radiative properties to calculate observationally- based F aerosol (z) and its uncertainty
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Target: F aerosol (z) + F aerosol (z) Constraints/Input: - MODIS AOD (7/2 ) + AOD - OMI AAOD (388 nm) + AAOD - CALIPSO ext (532, 1064 nm) + ext - CALIPSO back (532, 1064 nm) + back Retrieval: ext (, z) + ext ssa (, z) + ssa g (, z) + g Aerosol models: 7 fine and 3 coarse mode models and refractive indices for bi-modal log-normal size distribution → 100 combinations Free parameters: N fine, N coarse Rtx code Comparison: CERES F clear Airborne F clear Comparison: AERONET AOD, ssa, g Airborne test bed data Approach Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions Input &Spatial Sampling Constraints/Input: - MODIS AOD (7/2 ) + AOD - OMI AAOD (388 nm) + AAOD - CALIPSO ext (532, 1064 nm) + ext - CALIPSO back (532, 1064 nm) + back
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Aerosol models: Based on field observations, optimized to span observed range of ssa vs. EAE and lidar ratio vs. EAE Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions
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Minimize X and select top 3% solutions with : retrieved parameters : observables : uncertainties in obs. : weighting factors Metric: Simple weighted cost function x i = AOD 550nm (±0.03±5%) AOD 1240 nm (±0.03±5%) - MODIS AAOD 388 nm ±(0.05+30%) - OMI 532 ±(0.1Mm -1 sr -1 +30%), - CALIOP Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions
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Sample retrieval Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions
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OMAERUV (Torres group)OMAERO (KNMI group) AOD 388nm ssa 388nm Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions Representativeness of input - 1
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions Representativeness of input - 2 OMAERO data collocated with MODIS and CALIOP is a reasonable representation of global OMAERO over ocean OMAERUV data collocated with MODIS and CALIOP is a poor representation of global OMAERUV over ocean
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions AOD & ssa comparisons to AERONET - Ocean ssa 441nm Positive bias in input ssa data is removed in MOC retrieval AOD 500nm
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions AOD & ssa comparisons to AERONET - Land Positive bias in input ssa data is removed in MOC retrieval ssa 441nm AOD 500nm
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions ssa 550nm AOD 550nm AOD and ssa distribution
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions AOD and ssa distribution ssa 400nm 550nm 2200nm AOD 400nm 550nm 2200nm
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions Maps of TOA and surface DARF – MODIS snow-free, gap-filled albedo parameters (8-day res.) Black-sky albedo (0.3-5 m) at solar noon, Day 185, 2007
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions Maps of TOA and surface DARF TOA Surface
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions Comparisons of DARF to previous results Seasonal clear-sky DARF results at TOA and SFC from models and observations [W/m 2 ] after CCSP, adapted from Yu et al. 2006.
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Goals & Motivation Approach Technical details Input & Spatial sampling Aerosol models Metric Sample retrieval Representativeness of input Results AOD & ssa comparisons to AERONET AOD and ssa distribution Maps of TOA and surface DARF Comparisons of DARF to previous results Conclusions Conclusions This data set: – –Provides a PURELY observational estimate of clear-sky DARF(z) that compares favorably with previous observationally-based estimates and better with model based estimates at TOA – –Is based on stringently quality-screened, instantaneously collocated level 2 MODIS AOD (7/2 ), OMI AAOD at 388nm, and CALIOP aerosol backscatter at 532nm – –Is based on aerosol models that are consistent with suborbital obs – –Uses OMAERUV over land and OMAERO over ocean (because of representativeness of their subsampling) – –Contains 12 months (2007) of aerosol extinction, ssa and g as f(t, lat, long,, z) – –Agrees better with AERONET in terms of ssa(441nm) than input OMI+MODIS data – –Uses CALIOP layer heights to constrain OMAERUV AAOD – –Provides uncertainty estimates based on range of aerosol models that are consistent with observation within their uncertainties Future work: – –Utilize MODIS DB and/or MAIAC data – –Cover all of the available collocated MODIS, OMI, CALIOP data (June 2006-Dec. 2008) – –All-sky DARF by running retrievals with limited input
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