Global sensitivity experiments of the radiative forcing due to mineral aerosols
By G. Myhre, F. Stordal. 2001
137 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/e4087663317253f80d7778b90c862e5f37d6f55f
How researchers see this paper
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In Atmospheric Science
- Oleg Dubovik
- Didier Tanré
- Alexander Smirnov
- Michael Schulz
- J. Haywood
- Peter N. Francis
- Y. Balkanski
- M. Glew
In Global and Planetary Change
- Oleg Dubovik
- Didier Tanré
- Alexander Smirnov
- Michael Schulz
- J. Haywood
- Peter N. Francis
- Y. Balkanski
- M. Glew
Citations in the corpus
- Aerosol properties over bright-reflecting source regions (2004, background): “Several recent papers have modeled the direct forcing of such aerosols using optical properties of aerosols compiled from various measurements [29], [33].”
- Comparison of size and morphological measurements of coarse mode dust particles from Africa (2003, background): “bility [e.g., Patterson, 1981; Tegen and Lacis, 1996; Claquin et al., 1998; Schulz et al., 1998; Myhre and Stordal, 2001], and vertical distribution and transport mechanisms”
- Reevaluation of Mineral aerosol radiative forcings suggests a better agreement with satellite and AERONET data (2006, methodology): “The filled blue squares indicate measurements that were collected by Patterson et al. [1977] between 300 and 700 nm and by Volz [1973] for wavelengths greater than 2500 nm.”
- Radiative properties and direct effect of Saharan dust measured by the C‐130 aircraft during Saharan Dust Experiment (SHADE): 2. Terrestrial spectrum (2003, background): “Myhre and Stordal [2001] found a terrestrial radiative forcing of between 0.”
- Radiative properties and direct radiative effect of Saharan dust measured by the C-130 aircraft during SHADE: 1. Solar spectrum (2003, methodology): “particles as evidenced by the modeling studies ofMyhre and Stordal [2001] and Woodward [2001].”
- Saharan dust absorption and refractive index from aircraft-based observations during SAMUM 2006 (2009, background): “…magnitude and even the sign of the dust radiative forcing depend on the optical properties of the dust, on its vertical distribution, on the presence of clouds and on the albedo of the underlying surface (Sokolik and Toon, 1996; Tegen et al., 1996; Liao and Seinfeld, 1998; Myhre and Stordal, 2001).”
- Modeling the radiative impact of mineral dust during the Saharan Dust Experiment (SHADE) campaign (2003, methodology): “[37] In the work of Myhre and Stordal [2001] a large number of sensitivity calculations of the radiative forcing due to mineral dust were performed, pointing to refractive indices as a major source to the large uncertainty. In addition to the calculations performed using the refractive indices deriv”