2016
DOI: 10.3390/rs8050421
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Development, Production and Evaluation of Aerosol Climate Data Records from European Satellite Observations (Aerosol_cci)

Abstract: Producing a global and comprehensive description of atmospheric aerosols requires integration of ground-based, airborne, satellite and model datasets. Due to its complexity, aerosol monitoring requires the use of several data records with complementary information

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Cited by 184 publications
(176 citation statements)
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References 69 publications
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“…The main output variables are dust optical depth at 10 and 11 15 µm (and 550 nm). Initial results and validation performance are provided in (Popp et al, 2016).…”
Section: Iasi (Infrared Atmospheric Sounding Interferometer)mentioning
confidence: 99%
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“…The main output variables are dust optical depth at 10 and 11 15 µm (and 550 nm). Initial results and validation performance are provided in (Popp et al, 2016).…”
Section: Iasi (Infrared Atmospheric Sounding Interferometer)mentioning
confidence: 99%
“…A climatology (Kinne et al, 2006) is used to constrain chemical composition of the aerosol components at 1° x 1° latitude-longitude grid, while the method retrieves aerosol size and optical thickness on a 10 km grid. The algorithm has been developed from initial 25 prototype (Bevan et al, 2012) under the Aerosol CCI program, and results and validation performance for version 4.21 are provided in Popp et al (2016). The version used here (V4.3) differs from that summarized in Popp et al (2016) by improvements in retrieval of coarse/fine mode fraction, and improved cloud screening over ocean in the region of dense plumes, resulting in approximately 10% greater coverage, with small improvement in correlation against AERONET (AErosol RObotic NETwork) values.…”
Section: (A)atsr ((Advanced) Along Track Scanning Radiometer)mentioning
confidence: 99%
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“…The aerosol data came from the monthly means of the Aerosol Climate Change Initiative (CCI) v4.21 Advanced Along-Track Scanning Radiometer (AATSR) Climate Data Record (CDR), processed with the Swansea algorithm [42], provided at a spatial resolution of one degree. The water vapor data was obtained from the monthly means of the Satellite Application Facility on Climate Monitoring (CM SAF) CDR, based on the Advanced Television Infrared Observation Satellite (TIROS)-N Operational Vertical Sounder (ATOVS) [43], provided at a spatial resolution of 90 km.…”
Section: Atmospheric Correctionmentioning
confidence: 99%