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- W2111877314 abstract "Abstract. Transport and scavenging of chemical constituents in deep convection is important to understanding the composition of the troposphere and therefore chemistry-climate and air quality issues. High resolution cloud chemistry models have been shown to represent convective processing of trace gases quite well. To improve the representation of sub-grid convective transport and wet deposition in large-scale models, general characteristics, such as species mass flux, from the high resolution cloud chemistry models can be used. However, it is important to understand how these models behave when simulating the same storm. The intercomparison described here examines transport of six species. CO and O3, which are primarily transported, show good agreement among models and compare well with observations. Models that included lightning production of NOx reasonably predict NOx mixing ratios in the anvil compared with observations, but the NOx variability is much larger than that seen for CO and O3. Predicted anvil mixing ratios of the soluble species, HNO3, H2O2, and CH2O, exhibit significant differences among models, attributed to different schemes in these models of cloud processing including the role of the ice phase, the impact of cloud-modified photolysis rates on the chemistry, and the representation of the species chemical reactivity. The lack of measurements of these species in the convective outflow region does not allow us to evaluate the model results with observations." @default.
- W2111877314 created "2016-06-24" @default.
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- W2111877314 date "2007-09-18" @default.
- W2111877314 modified "2023-10-14" @default.
- W2111877314 title "Cloud-scale model intercomparison of chemical constituent transport in deep convection" @default.
- W2111877314 cites W101515339 @default.
- W2111877314 cites W1548588257 @default.
- W2111877314 cites W1592769740 @default.
- W2111877314 cites W1936252359 @default.
- W2111877314 cites W1963794911 @default.
- W2111877314 cites W1966222331 @default.
- W2111877314 cites W1966825857 @default.
- W2111877314 cites W1973686544 @default.
- W2111877314 cites W1975249766 @default.
- W2111877314 cites W1976391619 @default.
- W2111877314 cites W1980930774 @default.
- W2111877314 cites W1983780973 @default.
- W2111877314 cites W1985963141 @default.
- W2111877314 cites W1988541977 @default.
- W2111877314 cites W1990091723 @default.
- W2111877314 cites W1996954261 @default.
- W2111877314 cites W1999642386 @default.
- W2111877314 cites W2001732717 @default.
- W2111877314 cites W2005133875 @default.
- W2111877314 cites W2006569933 @default.
- W2111877314 cites W2011124381 @default.
- W2111877314 cites W2011397260 @default.
- W2111877314 cites W2013257604 @default.
- W2111877314 cites W2015559976 @default.
- W2111877314 cites W2018474532 @default.
- W2111877314 cites W2023049043 @default.
- W2111877314 cites W2023828029 @default.
- W2111877314 cites W2023969734 @default.
- W2111877314 cites W2029219658 @default.
- W2111877314 cites W2031514487 @default.
- W2111877314 cites W2032873217 @default.
- W2111877314 cites W2033053636 @default.
- W2111877314 cites W2034480362 @default.
- W2111877314 cites W2040015943 @default.
- W2111877314 cites W2044178884 @default.
- W2111877314 cites W2045356894 @default.
- W2111877314 cites W2048978228 @default.
- W2111877314 cites W2049222284 @default.
- W2111877314 cites W2050880342 @default.
- W2111877314 cites W2052461507 @default.
- W2111877314 cites W2053918385 @default.
- W2111877314 cites W2054768071 @default.
- W2111877314 cites W2056151389 @default.
- W2111877314 cites W2057556768 @default.
- W2111877314 cites W2058682766 @default.
- W2111877314 cites W2063182155 @default.
- W2111877314 cites W2067023524 @default.
- W2111877314 cites W2069063204 @default.
- W2111877314 cites W2070381285 @default.
- W2111877314 cites W2071532248 @default.
- W2111877314 cites W2073026744 @default.
- W2111877314 cites W2075045398 @default.
- W2111877314 cites W2075639255 @default.
- W2111877314 cites W2075691614 @default.
- W2111877314 cites W2078112693 @default.
- W2111877314 cites W2084258143 @default.
- W2111877314 cites W2088521789 @default.
- W2111877314 cites W2089308144 @default.
- W2111877314 cites W2093932464 @default.
- W2111877314 cites W2095427266 @default.
- W2111877314 cites W2095528175 @default.
- W2111877314 cites W2096648653 @default.
- W2111877314 cites W2097929307 @default.
- W2111877314 cites W2098024464 @default.
- W2111877314 cites W2112043279 @default.
- W2111877314 cites W2118594737 @default.
- W2111877314 cites W2127192903 @default.
- W2111877314 cites W2128659379 @default.
- W2111877314 cites W2129225156 @default.
- W2111877314 cites W2146009258 @default.
- W2111877314 cites W2147670100 @default.
- W2111877314 cites W2153160115 @default.
- W2111877314 cites W2174609735 @default.
- W2111877314 cites W2176500283 @default.
- W2111877314 cites W2180415739 @default.
- W2111877314 cites W2198360252 @default.