2012
DOI: 10.1080/01431161.2012.720739
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Validation of MODIS, MISR, OMI, and CALIPSO aerosol optical thickness using ground-based sunphotometers in Hong Kong

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Cited by 19 publications
(9 citation statements)
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“…The data analyzes were supported with observations from a Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) mounted onboard a Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite (Wong et al 2013). In addition, a Hybrid Single Particle Lagrangian Integrated Trajectory Model (HYSPLIT) (Draxler and Rolph 2010) is used to describe the origin of the air masses.…”
Section: Other Datamentioning
confidence: 99%
“…The data analyzes were supported with observations from a Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) mounted onboard a Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite (Wong et al 2013). In addition, a Hybrid Single Particle Lagrangian Integrated Trajectory Model (HYSPLIT) (Draxler and Rolph 2010) is used to describe the origin of the air masses.…”
Section: Other Datamentioning
confidence: 99%
“…Note that differences exist between MISR and MODIS derived AOD also. This is mainly due to the different procedures followed by the two sensors for retrieval of AOD (Prasad and Singh, 2007;Cheng et al, 2012;Wong et al, 2013).…”
Section: Methodsmentioning
confidence: 99%
“…This study uses level 2.0 quality assured and cloud screened AERONET data from Lahore and Karachi stations for years 2006-2013. AERONET AOD level 2.0 data from NASA website was downloaded with in ± 30 minutes of the satellite pass time for Lahore and Karachi stations [17] and compared with satellite based AOD extracted at 5x5 pixel (spatial) window over Lahore and Karachi's AERONET stations. This data was used to validate the satellite based AOD retrieved from MODIS, MISR, OMI and CALIPSO at spatial resolutions of 550 nm, 558 nm, 532 nm and 342nm respectively (Table 1).…”
Section: Data Used and Applied Research Methodologymentioning
confidence: 99%
“…MISR sensor was launched into polar Earth orbit aboard the Terra spacecraft in December 1999 to provide an AOD product (MISR_AM1_AS_AEROSOL) at spatial resolution of 17.1 km 2 on every 17 days [26]. Another sensor OMI with advance viewing capabilities is an inheritor of instruments such as the Total Ozone Mapping Spectrometer (TOMS) and provides an AOD product OMI_Aura_L3_OMAEROe at a spatial resolution of 27.8 km 2 [17]. Unlike previous sensors, CALIPSO provides vertical profiles of aerosol loading as well along with spatial and optical properties of aerosols and clouds at footprint of 5 km 2 in form of its AOD product (CAL_LID_L2_05kmAPro_Prov_V3) [27].…”
Section: Data Used and Applied Research Methodologymentioning
confidence: 99%
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