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• W2118328181 endingPage "513" @default.
• W2118328181 startingPage "513" @default.
• W2118328181 abstract "Immersion freezing of water and aqueous solutions by particles acting as ice nuclei (IN) is a common process of heterogeneous ice nucleation which occurs in many environments, especially in the atmosphere where it results in the glaciation of clouds. Here we experimentally show, using a variety of IN types suspended in various aqueous solutions, that immersion freezing temperatures and kinetics can be described solely by temperature, T, and solution water activity, a(w), which is the ratio of the vapour pressure of the solution and the saturation water vapour pressure under the same conditions and, in equilibrium, equivalent to relative humidity (RH). This allows the freezing point and corresponding heterogeneous ice nucleation rate coefficient, J(het), to be uniquely expressed by T and a(w), a result we term the a(w) based immersion freezing model (ABIFM). This method is independent of the nature of the solute and accounts for several varying parameters, including cooling rate and IN surface area, while providing a holistic description of immersion freezing and allowing prediction of freezing temperatures, J(het), frozen fractions, ice particle production rates and numbers. Our findings are based on experimental freezing data collected for various IN surface areas, A, and cooling rates, r, of droplets variously containing marine biogenic material, two soil humic acids, four mineral dusts, and one organic monolayer acting as IN. For all investigated IN types we demonstrate that droplet freezing temperatures increase as A increases. Similarly, droplet freezing temperatures increase as the cooling rate decreases. The log10(J(het)) values for the various IN types derived exclusively by Tand a(w), provide a complete description of the heterogeneous ice nucleation kinetics. Thus, the ABIFM can be applied over the entire range of T, RH, total particulate surface area, and cloud activation timescales typical of atmospheric conditions. Lastly, we demonstrate that ABIFM can be used to derive frozen fractions of droplets and ice particle production for atmospheric models of cirrus and mixed phase cloud conditions." @default.
• W2118328181 created "2016-06-24" @default.
• W2118328181 creator A5049444999 @default.
• W2118328181 creator A5072221729 @default.
• W2118328181 date "2013-01-01" @default.
• W2118328181 modified "2023-10-16" @default.
• W2118328181 title "A water activity based model of heterogeneous ice nucleation kinetics for freezing of water and aqueous solution droplets" @default.
• W2118328181 cites W1570025454 @default.
• W2118328181 cites W1587101236 @default.
• W2118328181 cites W1626331569 @default.
• W2118328181 cites W1633474379 @default.
• W2118328181 cites W1644074212 @default.
• W2118328181 cites W1657365528 @default.
• W2118328181 cites W1929218345 @default.
• W2118328181 cites W1964641020 @default.
• W2118328181 cites W1966932620 @default.
• W2118328181 cites W1970378186 @default.
• W2118328181 cites W1974585830 @default.
• W2118328181 cites W1978578998 @default.
• W2118328181 cites W1982413789 @default.
• W2118328181 cites W1982744822 @default.
• W2118328181 cites W1983277381 @default.
• W2118328181 cites W1984436535 @default.
• W2118328181 cites W1984484393 @default.
• W2118328181 cites W1988911477 @default.
• W2118328181 cites W1992981130 @default.
• W2118328181 cites W1993436181 @default.
• W2118328181 cites W1994201258 @default.
• W2118328181 cites W1996666570 @default.
• W2118328181 cites W1997615594 @default.
• W2118328181 cites W1998647656 @default.
• W2118328181 cites W1999919409 @default.
• W2118328181 cites W2003491554 @default.
• W2118328181 cites W2004221212 @default.
• W2118328181 cites W2005056392 @default.
• W2118328181 cites W2011254969 @default.
• W2118328181 cites W2012903065 @default.
• W2118328181 cites W2012908759 @default.
• W2118328181 cites W2016809654 @default.
• W2118328181 cites W2017434004 @default.
• W2118328181 cites W2019059884 @default.
• W2118328181 cites W2021788237 @default.
• W2118328181 cites W2024514869 @default.
• W2118328181 cites W2026111308 @default.
• W2118328181 cites W2029243935 @default.
• W2118328181 cites W2030102203 @default.
• W2118328181 cites W2033099541 @default.
• W2118328181 cites W2033745265 @default.
• W2118328181 cites W2035215452 @default.
• W2118328181 cites W2044753020 @default.
• W2118328181 cites W2045470555 @default.
• W2118328181 cites W2047715735 @default.
• W2118328181 cites W2049892409 @default.
• W2118328181 cites W2051487741 @default.
• W2118328181 cites W2059970437 @default.
• W2118328181 cites W2064375852 @default.
• W2118328181 cites W2064465292 @default.
• W2118328181 cites W2065860216 @default.
• W2118328181 cites W2074847173 @default.
• W2118328181 cites W2075712895 @default.
• W2118328181 cites W2084207432 @default.
• W2118328181 cites W2084759306 @default.
• W2118328181 cites W2086070310 @default.
• W2118328181 cites W2088509007 @default.
• W2118328181 cites W2091601188 @default.
• W2118328181 cites W2093674996 @default.
• W2118328181 cites W2097528821 @default.
• W2118328181 cites W2100365896 @default.
• W2118328181 cites W2103792347 @default.
• W2118328181 cites W2106136566 @default.
• W2118328181 cites W2106365060 @default.
• W2118328181 cites W2109297789 @default.
• W2118328181 cites W2109696661 @default.
• W2118328181 cites W2110062597 @default.
• W2118328181 cites W2110089488 @default.
• W2118328181 cites W2118423529 @default.
• W2118328181 cites W2119101262 @default.
• W2118328181 cites W2120999018 @default.
• W2118328181 cites W2128869037 @default.
• W2118328181 cites W2132077964 @default.
• W2118328181 cites W2136351893 @default.
• W2118328181 cites W2138881777 @default.
• W2118328181 cites W2139774107 @default.
• W2118328181 cites W2148854824 @default.
• W2118328181 cites W2149726954 @default.
• W2118328181 cites W2149861045 @default.
• W2118328181 cites W2150711435 @default.
• W2118328181 cites W2151725382 @default.
• W2118328181 cites W2158897593 @default.
• W2118328181 cites W2160853425 @default.
• W2118328181 cites W2162982522 @default.
• W2118328181 cites W2163867132 @default.
• W2118328181 cites W2166731785 @default.
• W2118328181 cites W2166829885 @default.
• W2118328181 cites W2166978691 @default.
• W2118328181 cites W2167248737 @default.
• W2118328181 cites W2173328836 @default.
• W2118328181 cites W2315009775 @default.

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