FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2099964024> ?p ?o ?g. }

• W2099964024 abstract "This modeling study compares the performance of eight single‐column models (SCMs) and four cloud‐resolving models (CRMs) in simulating shallow frontal cloud systems observed during a short period of the March 2000 Atmospheric Radiation Measurement (ARM) intensive operational period. Except for the passage of a cold front at the beginning of this period, frontal cloud systems are under the influence of an upper tropospheric ridge and are driven by a persistent frontogenesis over the Southern Great Plains and moisture transport from the northwestern part of the Gulf of Mexico. This study emphasizes quantitative comparisons among the model simulations and with the ARM data, focusing on a 27‐hour period when only shallow frontal clouds were observed. All CRMs and SCMs simulate clouds in the observed shallow cloud layer. Most SCMs also produce clouds in the middle and upper troposphere, while none of the CRMs produce any clouds there. One possible cause for this is the decoupling between cloud condensate and cloud fraction in nearly all SCM parameterizations. Another possible cause is the weak upper tropospheric subsidence that has been averaged over both descending and ascending regions. Significantly different cloud amounts and cloud microphysical properties are found in the model simulations. All CRMs and most SCMs underestimate shallow clouds in the lowest 125 hPa near the surface, but most SCMs overestimate the cloud amount above this layer. These results are related to the detailed formulations of cloud microphysical processes and fractional cloud parameterizations in the SCMs, and possibly to the dynamical framework and two‐dimensional configuration of the CRMs. Although two of the CRMs with anelastic dynamical frameworks simulate the shallow frontal clouds much better than the SCMs, the CRMs do not necessarily perform much better than the SCMs for the entire period when deep and shallow frontal clouds are present." @default.
• W2099964024 created "2016-06-24" @default.
• W2099964024 creator A5000932395 @default.
• W2099964024 creator A5001975042 @default.
• W2099964024 creator A5015027683 @default.
• W2099964024 creator A5022865217 @default.
• W2099964024 creator A5036495659 @default.
• W2099964024 creator A5037095156 @default.
• W2099964024 creator A5037160914 @default.
• W2099964024 creator A5041284859 @default.
• W2099964024 creator A5045080588 @default.
• W2099964024 creator A5045217069 @default.
• W2099964024 creator A5046085404 @default.
• W2099964024 creator A5050226800 @default.
• W2099964024 creator A5050610593 @default.
• W2099964024 creator A5059436319 @default.
• W2099964024 creator A5065538907 @default.
• W2099964024 creator A5067439693 @default.
• W2099964024 creator A5067533658 @default.
• W2099964024 creator A5073905819 @default.
• W2099964024 creator A5090022060 @default.
• W2099964024 creator A5090432729 @default.
• W2099964024 date "2005-04-21" @default.
• W2099964024 modified "2023-10-17" @default.
• W2099964024 title "Modeling springtime shallow frontal clouds with cloud-resolving and single-column models" @default.
• W2099964024 cites W1966596601 @default.
• W2099964024 cites W1966825857 @default.
• W2099964024 cites W1969523186 @default.
• W2099964024 cites W1974605993 @default.
• W2099964024 cites W1983408938 @default.
• W2099964024 cites W1987257833 @default.
• W2099964024 cites W2004044275 @default.
• W2099964024 cites W2005906181 @default.
• W2099964024 cites W2015559976 @default.
• W2099964024 cites W2017429567 @default.
• W2099964024 cites W2018166027 @default.
• W2099964024 cites W2019059884 @default.
• W2099964024 cites W2026824899 @default.
• W2099964024 cites W2027872029 @default.
• W2099964024 cites W2028091784 @default.
• W2099964024 cites W2034834825 @default.
• W2099964024 cites W2042058640 @default.
• W2099964024 cites W2044918207 @default.
• W2099964024 cites W2046762519 @default.
• W2099964024 cites W2052559311 @default.
• W2099964024 cites W2055407199 @default.
• W2099964024 cites W2059471972 @default.
• W2099964024 cites W2065339245 @default.
• W2099964024 cites W2074435632 @default.
• W2099964024 cites W2080964149 @default.
• W2099964024 cites W2083787882 @default.
• W2099964024 cites W2090785751 @default.
• W2099964024 cites W2105503137 @default.
• W2099964024 cites W2110431927 @default.
• W2099964024 cites W2110796569 @default.
• W2099964024 cites W2127192903 @default.
• W2099964024 cites W2132742519 @default.
• W2099964024 cites W2133673175 @default.
• W2099964024 cites W2135901729 @default.
• W2099964024 cites W2136850383 @default.
• W2099964024 cites W2140343068 @default.
• W2099964024 cites W2146208162 @default.
• W2099964024 cites W2148233761 @default.
• W2099964024 cites W2150946542 @default.
• W2099964024 cites W2155113355 @default.
• W2099964024 cites W2156618689 @default.
• W2099964024 cites W2158669608 @default.
• W2099964024 cites W2159859889 @default.
• W2099964024 cites W2173752470 @default.
• W2099964024 cites W2174038884 @default.
• W2099964024 cites W2174442245 @default.
• W2099964024 cites W2174648193 @default.
• W2099964024 cites W2176416142 @default.
• W2099964024 cites W2176681310 @default.
• W2099964024 cites W2179198649 @default.
• W2099964024 cites W2180136486 @default.
• W2099964024 cites W4253843360 @default.
• W2099964024 doi "https://doi.org/10.1029/2004jd005153" @default.
• W2099964024 hasPublicationYear "2005" @default.
• W2099964024 type Work @default.
• W2099964024 sameAs 2099964024 @default.
• W2099964024 citedByCount "54" @default.
• W2099964024 countsByYear W20999640242012 @default.
• W2099964024 countsByYear W20999640242013 @default.
• W2099964024 countsByYear W20999640242014 @default.
• W2099964024 countsByYear W20999640242015 @default.
• W2099964024 countsByYear W20999640242016 @default.
• W2099964024 countsByYear W20999640242017 @default.
• W2099964024 countsByYear W20999640242018 @default.
• W2099964024 countsByYear W20999640242020 @default.
• W2099964024 countsByYear W20999640242021 @default.
• W2099964024 countsByYear W20999640242023 @default.
• W2099964024 crossrefType "journal-article" @default.
• W2099964024 hasAuthorship W2099964024A5000932395 @default.
• W2099964024 hasAuthorship W2099964024A5001975042 @default.
• W2099964024 hasAuthorship W2099964024A5015027683 @default.
• W2099964024 hasAuthorship W2099964024A5022865217 @default.
• W2099964024 hasAuthorship W2099964024A5036495659 @default.
• W2099964024 hasAuthorship W2099964024A5037095156 @default.
• W2099964024 hasAuthorship W2099964024A5037160914 @default.

• next