Aerosol cloud precipitation interactions. Part 1. The nature and sources of cloud-active aerosols

By M. Andreae, Daniel Rosenfeld. 2008

1,574 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/4c3aab2710921662cd6883baf845b383e078b5f7

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Markku Kulmala
2. Ulrich Pöschl
3. P. Mcmurry
4. Tuukka Petäjä
5. V. Kerminen
6. Martin Wild
7. M. Andreae
8. Renyi Zhang

In Global and Planetary Change

1. Markku Kulmala
2. Ulrich Pöschl
3. Martin Wild
4. M. Andreae
5. V. Kerminen
6. P. Mcmurry
7. N. Bellouin
8. Daniel Rosenfeld

Citations in the corpus

• Natural aerosol direct and indirect radiative effects (2013, background): “Furthermore, natural aerosol contributes to aerosol background concentrations [ Andreae , 2008], the quanti fi cation of which is a prerequisite for accurate assessments of impacts of anthropogenic aerosol on clouds and climate [ Menon et al ., 2002; Schmidt et al ., 2012].”
• Formation of highly hygroscopic soot aerosols upon internal mixing with sulfuric acid vapor (2009, background): “The change in hygroscopicity of soot particles during aging has an important influence on their atmospheric residence time, optical properties, and cloud-forming potential [Andreae and Rosenfeld, 2008].”
• Global observations of aerosol‐cloud‐precipitation‐climate interactions (2014, background): “The few available estimates of preindustrial aerosol background levels over land are highly uncertain [Andreae, 2007; Andreae and Rosenfeld, 2008].”
• Constraining the aerosol influence on cloud fraction (2016, background): “As expected, sulphate and organic matter show a relatively strong AOD-CDNC-CF relationship, due to their properties as CCN [Andreae and Rosenfeld, 2008].”
• Global distribution of the effective aerosol hygroscopicity parameter for CCN activation (2010, background): “Based on a review of observational data, Andreae and Rosenfeld (2008) suggested that continental and marine aerosols on average tend to cluster into relatively narrow ranges of effective hygroscopicity (continental κ =0.3±0.1; marine κ =0.7±0.2).”
• Cloud condensation nuclei in pristine tropical rainforest air of Amazonia: size-resolved measurements and modeling of atmospheric aerosol composition and CCN activity (2009, neutral): “1; Andreae, 2009) confirm earlier studies suggesting that aerosol particle number and size are the major predictors for the variability of the CCN concentration in continental boundary layer air, followed by particle composition and hygroscopicity as relatively minor modulators (Feingold et al., 200”
• Competition between water uptake and ice nucleation by glassy organic aerosol particles (2014, background): “Atmospheric aerosol particles influence climate through affecting the earth’s radiation budget directly by scattering and absorbing light, and indirectly by acting as nuclei for cloud droplets and ice crystals (Yu et al., 2006; Andreae and Rosenfeld, 2008; IPCC, 2013).”
• Understanding Hail in the Earth System (2020, background): “…recently, given that CCN can have a substantial influence on the microphysical properties of water and ice clouds, which in turn may affect the processes that lead to the formation of hail (Andreae & Rosenfeld, 2008; Fan et al., 2013; Lebo & Morrison, 2014; Liu & Niu, 2010; Rosenfeld et al., 2008).”
• Cloud condensation nuclei production associated with atmospheric nucleation: a synthesis based on existing literature and new results (2012, background): “Understanding the relation between aerosol and their precursor emissions, atmospheric aerosol particle populations, clouds and, eventually, climate is not possible without quantification of the sources responsible for atmospheric CCN (Andreae and Rosenfeld, 2008; Carslaw et al., 2010).”
• The ice nucleation ability of one of the most abundant types of fungal spores found in the atmosphere (2010, neutral): “, 2003; Pruppacher and Klett, 1997), soot (Andreae and Rosenfeld, 2008; K ärcher et al., 2007), crystalline salts (Abbatt et al.”
• Aerosol Mixing State: Measurements, Modeling, and Impacts (2019, background): “Common particle types are mostly primary (soot, organic carbon, biomass burning, mineral dust, sea salt, and industrial; Andreae & Rosenfeld, 2008; Prather et al., 2008).”