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• W2029322549 startingPage "n/a" @default.
• W2029322549 abstract "[1] An intercomparison of six cloud-resolving and large-eddy simulation models is presented. This case study is based on observations of a persistent mixed-phase boundary layer cloud gathered on 7 May, 1998 from the Surface Heat Budget of Arctic Ocean (SHEBA) and First ISCCP Regional Experiment - Arctic Cloud Experiment (FIRE-ACE). Ice nucleation is constrained in the simulations in a way that holds the ice crystal concentration approximately fixed, with two sets of sensitivity runs in addition to the baseline simulations utilizing different specified ice nucleus (IN) concentrations. All of the baseline and sensitivity simulations group into two distinct quasi-steady states associated with either persistent mixed-phase clouds or all-ice clouds after the first few hours of integration, implying the existence of multiple states for this case. These two states are associated with distinctly different microphysical, thermodynamic, and radiative characteristics. Most but not all of the models produce a persistent mixed-phase cloud qualitatively similar to observations using the baseline IN/crystal concentration, while small increases in the IN/crystal concentration generally lead to rapid glaciation and conversion to the all-ice state. Budget analysis indicates that larger ice deposition rates associated with increased IN/crystal concentrations have a limited direct impact on dissipation of liquid in these simulations. However, the impact of increased ice deposition is greatly enhanced by several interaction pathways that lead to an increased surface precipitation flux, weaker cloud top radiative cooling and cloud dynamics, and reduced vertical mixing, promoting rapid glaciation of the mixed-phase cloud for deposition rates in the cloud layer greater than about 1 − 2 × 10−5 g kg−1 s−1 for this case. These results indicate the critical importance of precipitation-radiative-dynamical interactions in simulating cloud phase, which have been neglected in previous fixed-dynamical parcel studies of the cloud phase parameter space. Large sensitivity to the IN/crystal concentration also suggests the need for improved understanding of ice nucleation and its parameterization in models." @default.
• W2029322549 created "2016-06-24" @default.
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• W2029322549 date "2011-02-01" @default.
• W2029322549 modified "2023-10-01" @default.
• W2029322549 title "Intercomparison of cloud model simulations of Arctic mixed-phase boundary layer clouds observed during SHEBA/FIRE-ACE" @default.
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• W2029322549 cites W1968855589 @default.
• W2029322549 cites W1974829366 @default.
• W2029322549 cites W1974930472 @default.
• W2029322549 cites W1991466717 @default.
• W2029322549 cites W1996323808 @default.
• W2029322549 cites W2008575785 @default.
• W2029322549 cites W2010554983 @default.
• W2029322549 cites W2014741650 @default.
• W2029322549 cites W2015328318 @default.
• W2029322549 cites W2015772592 @default.
• W2029322549 cites W2018066911 @default.
• W2029322549 cites W2018909690 @default.
• W2029322549 cites W2019895406 @default.
• W2029322549 cites W2020718223 @default.
• W2029322549 cites W2021575707 @default.
• W2029322549 cites W2022158302 @default.
• W2029322549 cites W2023453422 @default.
• W2029322549 cites W2026675755 @default.
• W2029322549 cites W2029838360 @default.
• W2029322549 cites W2029853075 @default.
• W2029322549 cites W2031314322 @default.
• W2029322549 cites W2038868034 @default.
• W2029322549 cites W2042556449 @default.
• W2029322549 cites W2045272432 @default.
• W2029322549 cites W2048978228 @default.
• W2029322549 cites W2049170372 @default.
• W2029322549 cites W2050069633 @default.
• W2029322549 cites W2051722342 @default.
• W2029322549 cites W2052201417 @default.
• W2029322549 cites W2053918385 @default.
• W2029322549 cites W2055457852 @default.
• W2029322549 cites W2065450476 @default.
• W2029322549 cites W2069291319 @default.
• W2029322549 cites W2075162893 @default.
• W2029322549 cites W2075975755 @default.
• W2029322549 cites W2076790609 @default.
• W2029322549 cites W2078122547 @default.
• W2029322549 cites W2079622917 @default.
• W2029322549 cites W2080964149 @default.
• W2029322549 cites W2083458282 @default.
• W2029322549 cites W2089876101 @default.
• W2029322549 cites W2092354469 @default.
• W2029322549 cites W2095853260 @default.
• W2029322549 cites W2096112487 @default.
• W2029322549 cites W2103164730 @default.
• W2029322549 cites W2104663386 @default.
• W2029322549 cites W2110059481 @default.
• W2029322549 cites W2110770653 @default.
• W2029322549 cites W2114883075 @default.
• W2029322549 cites W2115466864 @default.
• W2029322549 cites W2119621743 @default.
• W2029322549 cites W2125765412 @default.
• W2029322549 cites W2132742519 @default.
• W2029322549 cites W2134835764 @default.
• W2029322549 cites W2138884861 @default.
• W2029322549 cites W2139215874 @default.
• W2029322549 cites W2143117507 @default.
• W2029322549 cites W2150322550 @default.
• W2029322549 cites W2158536070 @default.
• W2029322549 cites W2160456125 @default.
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• W2029322549 cites W2170409344 @default.
• W2029322549 cites W2175438141 @default.
• W2029322549 cites W2175748926 @default.
• W2029322549 cites W2178052315 @default.
• W2029322549 cites W2495857162 @default.
• W2029322549 cites W3081006245 @default.
• W2029322549 cites W4254835330 @default.
• W2029322549 doi "https://doi.org/10.1029/2011ms000066" @default.
• W2029322549 hasPublicationYear "2011" @default.
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