Sensitivity of multiangle imaging to natural mixtures of aerosols over ocean

By Ralph A. Kahn, P. Banerjee, D. McDonald. 2001

248 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/71ef60bf64585be644bc6ab77d23410c7e7d9aaf

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Citations in the corpus

The value of multiangle measurements for retrieving structurally and radiatively consistent properties of clouds, aerosols, and surfaces (2005, methodology): “A research aerosol retrieval code (Kahn et al., 2001) applied to MISR data obtained an aerosol optical depth of 0.”
Decadal-scale trends in regional aerosol particle properties and their linkage to emission changes (2017, background): “…(275 m 1.1 km) observations at 9 along-track viewing angles in each of 4 visible/near-infrared spectral bands provide nearglobal coverage every 9 d (Diner et al 1998) and sensitivity to particle type over both land and ocean, in addition to total AOD (Kahn et al 2001, Kahn and Gaitley 2015).”
Constraining the magnitude of the global dust cycle by minimizing the difference between a model and observations (2006, methodology): “In addition, MISR retrieves parameters related to particle shape [Kahn et al., 2001].”
Multiangle Imaging Spectroradiometer (MISR) global aerosol optical depth validation based on 2 years of coincident Aerosol Robotic Network (AERONET) observations (2005, methodology): “Standard approaches are adopted for modeling surface Fresnel reflection, wind speed-dependent white caps, and Sun glint contributions, whereas the water-leaving radiance component in the red and near-infrared bands is assumed to be negligible [Martonchik et al., 1998; Kahn et al., 2001b].”
Solar radiation budget and radiative forcing due to aerosols and clouds (2008, methodology): “The Multiangle Imaging Spectroradiometer (MISR) AODs [e.g., Diner et al., 1998; Kahn et al., 2001, 2005] and The D02203 KIM AND RAMANATHAN: SOLAR RADIATION BUDGET AND FORCING 2 of 34 D02203 Moderate resolution Imaging Spectroradiometer (MODIS) AODs [e.g., Kaufman et al., 1997; Tanre et al., 1997;…”
Polarimetric remote sensing of aerosols over land (2009, background): “, 2003], or spectral bands can be used that are immune to variations in the chlorophyll concentration [Kaufman et al., 1997a; Martonchik et al., 1998; Kahn et al., 2001].”
Improved retrievals of carbon dioxide from Orbiting Carbon Observatory-2 with the version 8 ACOS algorithm (2018, background): “However, the use of two fixed aerosol types, types “2b” and “3b” from the Kahn et al. (2001) climatology, did not accurately represent the true global variability of aerosol on the length scales and timescales probed by GOSAT and OCO-2.”
Overview of the CALIPSO Mission and CALIOP Data Processing Algorithms (2009, methodology): “We have adopted an observation-based approach to deﬁning representative aerosol types, as opposed to a synthetic approach (e.g., Kahn et al. 2001).”
Ability of multiangle remote sensing observations to identify and distinguish mineral dust types : Optical models and retrievals of optically thick plumes : Quantifying the radiative and biogeochemical impacts of mineral dust (2005, methodology): “[57] We use the MISR research aerosol retrieval (Figure 10) to compare MISR measurements with modeled radiances [ Kahn et al., 2001a ].”
Aerosol source plume physical characteristics from space-based multiangle imaging (2007, background): “…and spherical versus nonspherical, making possible the separation of about a dozen aerosol air mass types based on particle properties, and allowing us to distinguish plume and background aerosols [Kahn et al., 2001, 2005; Kalashnikova and Kahn, 2006; Chen et al., submitted manuscript, 2006].”