2009
DOI: 10.5194/acp-9-2517-2009
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Parameterization of cloud droplet formation for global and regional models: including adsorption activation from insoluble CCN

Abstract: Abstract. Dust and black carbon aerosol have long been known to exert potentially important and diverse impacts on cloud droplet formation. Most studies to date focus on the soluble fraction of these particles, and overlook interactions of the insoluble fraction with water vapor (even if known to be hydrophilic). To address this gap, we developed a new parameterization that considers cloud droplet formation within an ascending air parcel containing insoluble (but wettable) particles externally mixed with aeros… Show more

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Cited by 116 publications
(219 citation statements)
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“…This effect is observed because FHH particles require less water uptake to reach the critical diameter than κ-KT particles and consequently deplete much less water vapor (Kumar et al, 2009a). Using FHH theory to describe activation of mineral dust will therefore bias estimates of the aerosol indirect effect when mineral dust act as CCN.…”
Section: Conclusion and Atmospheric Implicationsmentioning
confidence: 99%
See 1 more Smart Citation
“…This effect is observed because FHH particles require less water uptake to reach the critical diameter than κ-KT particles and consequently deplete much less water vapor (Kumar et al, 2009a). Using FHH theory to describe activation of mineral dust will therefore bias estimates of the aerosol indirect effect when mineral dust act as CCN.…”
Section: Conclusion and Atmospheric Implicationsmentioning
confidence: 99%
“…According to Kumar et al (2009a), using κ-KT instead of using FHH theory in model parameterizations changes the maximum supersaturations and sensitivity of the cloud droplet number to aerosol variations in parcel model simulations. This effect is observed because FHH particles require less water uptake to reach the critical diameter than κ-KT particles and consequently deplete much less water vapor (Kumar et al, 2009a).…”
Section: Conclusion and Atmospheric Implicationsmentioning
confidence: 99%
“…Equations (A1) and (A2) consider only Köh-ler theory for computation of CCN. The impact of water adsorption onto insoluble particles such as dust can also be treated with a similar formalism (Kumar et al, 2009). The second step is achieved by finding an approximate solution to the equation describing the supersaturation tendency in the ascending air parcel, which can be written as…”
Section: Adjoint Developmentmentioning
confidence: 99%
“…The development of the adjoint of the Fountoukis and Nenes (2005) parameterization (FN), as well as that for the adsorption activation parameterization of Kumar et al (2009), is described in full detail in Karydis et al (2012b). Briefly, because the computation of N d in FN is achieved by iterative solution of Eq.…”
Section: A1 Fn and Fn-il Parameterizationsmentioning
confidence: 99%
“…The potential of soot particles to act as cloud condensation nuclei (CCN) or ice nuclei (IN) is also modified by the aging process. The aging of mineral dust particles changes their capability to act as IN or CCN (Kumar et al, 2009). Therefore, the explicit treatment of the aging process is an important process that should not be neglected.…”
Section: Aerosol Mixing State and Chemical Aging Of Particlesmentioning
confidence: 99%