An analysis of potential cloud artifacts in MODIS over ocean aerosol optical thickness products
By Jianglong Zhang, J. Reid, Brent N. Holben. 2005
185 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/d34e28ab0e7feb548de54679eeef82e5b5b5673e
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In Atmospheric Science
- Johannes Quaas
- G. Feingold
- N. Bellouin
- Martin Wild
- Daniel Rosenfeld
- Bjorn Stevens
- P. Stier
- Ulrike Lohmann
In Global and Planetary Change
- Johannes Quaas
- G. Feingold
- N. Bellouin
- Martin Wild
- Daniel Rosenfeld
- Bjorn Stevens
- P. Stier
- Ulrike Lohmann
Citations in the corpus
- The invigoration of deep convective clouds over the Atlantic: aerosol effect, meteorology or retrieval artifact? (2010, background): “Nevertheless it has been shown that the MODIS AOD retrievals may contain residual artifacts introduced by clouds (Kaufman et al., 2005d; Zhang et al., 2005), by 3-D effects near clouds (Marshak et al.”
- Bounding Global Aerosol Radiative Forcing of Climate Change (2020, background): “In addition, sam-924 pling the aerosol radiative properties in close vicinity to clouds leads to errors (Christensen925 et al., 2017) due to the humidity-swelling of the aerosol (Quaas et al., 2010) and926 misclassification of cloud as aerosols (J. Zhang et al., 2005).927 2.”
- Interpreting the cloud cover – aerosol optical depth relationship found in satellite data using a general circulation model (2009, background): “Also, spurious clouds might be un-detected by the retrieval algorithm in regions identified as clear and thus used for an AOD retrieval (“cloud contamination”; Kaufman et al., 2005b; Zhang et al., 2005; Tian et al., 2008).”
- A simple model for the cloud adjacency effect and the apparent bluing of aerosols near clouds (2008, background): “[2] Numerous studies based on satellite observations have reported a positive correlation between cloud amount and aerosol optical thickness (AOT) [e.g., Sekiguchi et al., 2003; Loeb and Manalo-Smith, 2005; Ignatov et al., 2005; Zhang et al., 2005; Kaufman et al., 2005a; Matheson et al., 2005].”
- Satellite-based estimate of the direct and indirect aerosol climate forcing (2008, background): “It must be noted that in particular the interpretation of the often-found positive relationship between cloud fraction and AOD as a representation of the cloud lifetime aerosol effect is largely debated [Kaufman et al., 2005c; Loeb and Manalo-Smith, 2005; Zhang et al., 2005; Lohmann et al., 2006].”
- Aerosol-cloud interaction inferred from MODIS satellite data and global aerosol models (2006, background): “Residual cloud contamination in the aerosol retrievals has been suggested to be a cause for the increase in cloud cover with AOD (Zhang et al., 2005), but Kaufman et al.”
- Global observations of aerosol‐cloud‐precipitation‐climate interactions (2014, background): “Even distant clouds can bias the retrieval of aerosol properties [Zhang et al., 2005] due to radiation scattered into the pixel of interest.”