2005
DOI: 10.5194/acp-5-1757-2005
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Supersaturation, dehydration, and denitrification in Arctic cirrus

Abstract: Abstract.A polar cirrus case study is discussed with the help of a one-dimensional model with explicit aerosol and ice microphysics. It is demonstrated that continuous cooling of air in regions with small amounts of ice and slow ice deposition rates of water vapor drives significant in-cloud supersaturations over ice, with potentially important consequences for heterogeneous halogen activation. Radiatively important cloud properties such as ice crystal size distributions are investigated, showing the presence … Show more

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Cited by 24 publications
(42 citation statements)
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“…Additionally, some sensitivity studies are carried out. Second, we simulate a well-documented case of arctic cirrostratus and compare our results with 1-D simulations (Lin et al, 2005;Kärcher, 2005). Kärcher and Lohmann (2002a) used a detailed box model (particle tracking, highly resolved aerosol size distribution) for testing an analytically derived relationship between the maximum possible ice crystal number density, formed by homogeneous nucleation, and vertical velocity.…”
Section: Validation and Discussionmentioning
confidence: 99%
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“…Additionally, some sensitivity studies are carried out. Second, we simulate a well-documented case of arctic cirrostratus and compare our results with 1-D simulations (Lin et al, 2005;Kärcher, 2005). Kärcher and Lohmann (2002a) used a detailed box model (particle tracking, highly resolved aerosol size distribution) for testing an analytically derived relationship between the maximum possible ice crystal number density, formed by homogeneous nucleation, and vertical velocity.…”
Section: Validation and Discussionmentioning
confidence: 99%
“…In this section we compare the performance of our bulk microphysics scheme with the spectrally resolving schemes of Lin et al (2005) and Kärcher (2005) for the case of an arctic cirrostratus triggered by a constant vertical updraught.…”
Section: Formation and Evolution Of An Arctic Cirrostratusmentioning
confidence: 99%
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“…In cirrus with sufficiently high IWC (>0.1-1 mg m −3 ) in the absence of very high ice supersaturations, HNO 3 is redistributed between aerosol and ice particles and uptake in ice dominates dissolution in liquid particles (Kärcher, 2005; . Thermodynamic equilibrium properties of STS aerosol particles containing 0.1 nmol mol −1 H 2 SO 4 as a function of the ice saturation ratio S i for various combinations of the HNO 3 partial pressure p n and T prevailing during the TROCCINOX observations.…”
Section: Nitric Acid Partitioningmentioning
confidence: 99%
“…In what follows we make use of a one-dimensional, cirrus cloud-resolving model with detailed STS aerosol and ice microphysics (Kärcher, 2005).…”
Section: Microphysical Simulationsmentioning
confidence: 99%