FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2039608628> ?p ?o ?g. }

• W2039608628 endingPage "2460" @default.
• W2039608628 startingPage "2437" @default.
• W2039608628 abstract "Abstract This paper describes idealized simulations of a squall line observed on 20 June 2007, in central Oklahoma. Results are compared with measurements from dual-polarization radar and surface disdrometer. The baseline model configuration qualitatively reproduces key storm features, but underpredicts precipitation rates and generally overpredicts median volume raindrop diameter. The sensitivity of model simulations to parameterization of raindrop breakup is tested under different low-level (0–2.5 km) environmental vertical wind shears. Storm characteristics exhibit considerable sensitivity to the parameterization of breakup, especially for moderate (0.0048 s−1) shear. Simulations with more efficient breakup tend to have higher domain-mean precipitation rates under both moderate and higher (0.0064 s−1) shear, despite the smaller mean drop size and hence lower mass-weighted fall speed and higher evaporation rate for a given rainwater content. In these runs, higher evaporation leads to stronger cold pools, faster propagation, larger storm size, greater updraft mass flux (but weaker convective updrafts at mid- and upper levels), and greater total condensation that compensates for the increased evaporation to give more surface precipitation. The impact of drop breakup on mass-weighted fall speed is also important and leads to a nonmonotonic response of storm characteristics (surface precipitation, cold pool strength, etc.) to changes in breakup efficiency under moderate wind shear. In contrast, the response is generally monotonic at higher wind shear. Interactions between drop breakup, convective dynamics, cold pool intensity, and low-level environmental wind shear are also described in the context of “Rotunno–Klemp–Weisman (RKW) theory,” which addresses how density currents evolve in sheared environments." @default.
• W2039608628 created "2016-06-24" @default.
• W2039608628 creator A5006780848 @default.
• W2039608628 creator A5020516922 @default.
• W2039608628 creator A5086723313 @default.
• W2039608628 creator A5089665922 @default.
• W2039608628 date "2012-08-01" @default.
• W2039608628 modified "2023-09-30" @default.
• W2039608628 title "Sensitivity of a Simulated Midlatitude Squall Line to Parameterization of Raindrop Breakup" @default.
• W2039608628 cites W1481811138 @default.
• W2039608628 cites W1966213179 @default.
• W2039608628 cites W1967580646 @default.
• W2039608628 cites W1969451133 @default.
• W2039608628 cites W1976653998 @default.
• W2039608628 cites W1976989782 @default.
• W2039608628 cites W1979316171 @default.
• W2039608628 cites W1980764896 @default.
• W2039608628 cites W1982665211 @default.
• W2039608628 cites W1984041426 @default.
• W2039608628 cites W1986358484 @default.
• W2039608628 cites W1988589244 @default.
• W2039608628 cites W1994162645 @default.
• W2039608628 cites W2005092043 @default.
• W2039608628 cites W2009050609 @default.
• W2039608628 cites W2009314250 @default.
• W2039608628 cites W2010279778 @default.
• W2039608628 cites W2010498097 @default.
• W2039608628 cites W2015559976 @default.
• W2039608628 cites W2016583669 @default.
• W2039608628 cites W2016898261 @default.
• W2039608628 cites W2017045507 @default.
• W2039608628 cites W2018624638 @default.
• W2039608628 cites W2021595836 @default.
• W2039608628 cites W2023308405 @default.
• W2039608628 cites W2024445106 @default.
• W2039608628 cites W2033060029 @default.
• W2039608628 cites W2033961722 @default.
• W2039608628 cites W2034005226 @default.
• W2039608628 cites W2035706748 @default.
• W2039608628 cites W2048171182 @default.
• W2039608628 cites W2049009264 @default.
• W2039608628 cites W2050335471 @default.
• W2039608628 cites W2057204830 @default.
• W2039608628 cites W2063680893 @default.
• W2039608628 cites W2066433058 @default.
• W2039608628 cites W2069461995 @default.
• W2039608628 cites W2070158856 @default.
• W2039608628 cites W2074283713 @default.
• W2039608628 cites W2074507622 @default.
• W2039608628 cites W2077038911 @default.
• W2039608628 cites W2087262003 @default.
• W2039608628 cites W2096671520 @default.
• W2039608628 cites W2096696769 @default.
• W2039608628 cites W2099459620 @default.
• W2039608628 cites W2101902804 @default.
• W2039608628 cites W2102890156 @default.
• W2039608628 cites W2104484944 @default.
• W2039608628 cites W2106292919 @default.
• W2039608628 cites W2107413761 @default.
• W2039608628 cites W2110129650 @default.
• W2039608628 cites W2110796569 @default.
• W2039608628 cites W2114883075 @default.
• W2039608628 cites W2115466864 @default.
• W2039608628 cites W2115792892 @default.
• W2039608628 cites W2132094274 @default.
• W2039608628 cites W2134897899 @default.
• W2039608628 cites W2155420241 @default.
• W2039608628 cites W2156040521 @default.
• W2039608628 cites W2157092104 @default.
• W2039608628 cites W2157747676 @default.
• W2039608628 cites W2161486819 @default.
• W2039608628 cites W2165749813 @default.
• W2039608628 cites W2172352847 @default.
• W2039608628 cites W2172458149 @default.
• W2039608628 cites W2173020645 @default.
• W2039608628 cites W2174378052 @default.
• W2039608628 cites W2175231548 @default.
• W2039608628 cites W2178395904 @default.
• W2039608628 cites W4230250764 @default.
• W2039608628 cites W4376848726 @default.
• W2039608628 doi "https://doi.org/10.1175/mwr-d-11-00283.1" @default.
• W2039608628 hasPublicationYear "2012" @default.
• W2039608628 type Work @default.
• W2039608628 sameAs 2039608628 @default.
• W2039608628 citedByCount "74" @default.
• W2039608628 countsByYear W20396086282012 @default.
• W2039608628 countsByYear W20396086282013 @default.
• W2039608628 countsByYear W20396086282014 @default.
• W2039608628 countsByYear W20396086282015 @default.
• W2039608628 countsByYear W20396086282016 @default.
• W2039608628 countsByYear W20396086282017 @default.
• W2039608628 countsByYear W20396086282018 @default.
• W2039608628 countsByYear W20396086282019 @default.
• W2039608628 countsByYear W20396086282020 @default.
• W2039608628 countsByYear W20396086282021 @default.
• W2039608628 countsByYear W20396086282022 @default.
• W2039608628 countsByYear W20396086282023 @default.
• W2039608628 crossrefType "journal-article" @default.

• next