FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3010410033> ?p ?o ?g. }

• W3010410033 endingPage "767" @default.
• W3010410033 startingPage "751" @default.
• W3010410033 abstract "Abstract Quasi-vertical profiles (QVPs) obtained from a database of U.S. WSR-88D data are used to document polarimetric characteristics of the melting layer (ML) in cold-season storms with high vertical resolution and accuracy. A polarimetric technique to define the top and bottom of the ML is first introduced. Using the QVPs, statistical relationships are developed to gain insight into the evolution of microphysical processes above, within, and below the ML, leading to a statistical polarimetric model of the ML that reveals characteristics that reflectivity data alone are not able to provide, particularly in regions of weak reflectivity factor at horizontal polarization Z H . QVP ML statistics are examined for two regimes in the ML data: Z H ≥ 20 dB Z and Z H < 20 dB Z . Regions of Z H ≥ 20 dB Z indicate locations of MLs collocated with enhanced differential reflectivity Z DR and reduced copolar correlation coefficient ρ hv , while for Z H < 20 dB Z a well-defined ML is difficult to discern using Z H alone. Evidence of large Z DR up to 4 dB, backscatter differential phase δ up to 8°, and low ρ hv down to 0.80 associated with lower Z H (from −10 to 20 dB Z ) in the ML is observed when pristine, nonaggregated ice falls through it. Positive correlation is documented between maximum specific differential phase K DP and maximum Z H in the ML; these are the first QVP observations of K DP in MLs documented at S band. Negative correlation occurs between minimum ρ hv in the ML and ML depth and between minimum ρ hv in the ML and the corresponding enhancement of Z H (Δ Z H = Z H max − Z H rain )." @default.
• W3010410033 created "2020-03-13" @default.
• W3010410033 creator A5024731507 @default.
• W3010410033 creator A5028629919 @default.
• W3010410033 creator A5058577510 @default.
• W3010410033 date "2020-04-01" @default.
• W3010410033 modified "2023-09-27" @default.
• W3010410033 title "A Polarimetric Radar Analysis of Ice Microphysical Processes in Melting Layers of Winter Storms Using S-Band Quasi-Vertical Profiles" @default.
• W3010410033 cites W1522112144 @default.
• W3010410033 cites W1892011713 @default.
• W3010410033 cites W1963491287 @default.
• W3010410033 cites W1967088861 @default.
• W3010410033 cites W1967223524 @default.
• W3010410033 cites W1967518463 @default.
• W3010410033 cites W1971901404 @default.
• W3010410033 cites W1976523267 @default.
• W3010410033 cites W1977069605 @default.
• W3010410033 cites W1986125626 @default.
• W3010410033 cites W1987780302 @default.
• W3010410033 cites W2001049707 @default.
• W3010410033 cites W2044525751 @default.
• W3010410033 cites W2053430295 @default.
• W3010410033 cites W2059484708 @default.
• W3010410033 cites W2061790496 @default.
• W3010410033 cites W2061792766 @default.
• W3010410033 cites W2074445881 @default.
• W3010410033 cites W2083088168 @default.
• W3010410033 cites W2086262081 @default.
• W3010410033 cites W2089195393 @default.
• W3010410033 cites W2090147764 @default.
• W3010410033 cites W2090380481 @default.
• W3010410033 cites W2102404891 @default.
• W3010410033 cites W2102675572 @default.
• W3010410033 cites W2108994921 @default.
• W3010410033 cites W2125680768 @default.
• W3010410033 cites W2126090229 @default.
• W3010410033 cites W2131291464 @default.
• W3010410033 cites W2151210446 @default.
• W3010410033 cites W2161486819 @default.
• W3010410033 cites W2161663834 @default.
• W3010410033 cites W2162568555 @default.
• W3010410033 cites W2169445778 @default.
• W3010410033 cites W2256742118 @default.
• W3010410033 cites W2259421489 @default.
• W3010410033 cites W2300479417 @default.
• W3010410033 cites W2563243459 @default.
• W3010410033 cites W2614650722 @default.
• W3010410033 cites W2757149491 @default.
• W3010410033 cites W2760784711 @default.
• W3010410033 cites W2761279999 @default.
• W3010410033 cites W2944568008 @default.
• W3010410033 cites W2946293825 @default.
• W3010410033 cites W2972671039 @default.
• W3010410033 doi "https://doi.org/10.1175/jamc-d-19-0128.1" @default.
• W3010410033 hasPublicationYear "2020" @default.
• W3010410033 type Work @default.
• W3010410033 sameAs 3010410033 @default.
• W3010410033 citedByCount "13" @default.
• W3010410033 countsByYear W30104100332020 @default.
• W3010410033 countsByYear W30104100332021 @default.
• W3010410033 countsByYear W30104100332022 @default.
• W3010410033 countsByYear W30104100332023 @default.
• W3010410033 crossrefType "journal-article" @default.
• W3010410033 hasAuthorship W3010410033A5024731507 @default.
• W3010410033 hasAuthorship W3010410033A5028629919 @default.
• W3010410033 hasAuthorship W3010410033A5058577510 @default.
• W3010410033 hasBestOaLocation W30104100331 @default.
• W3010410033 hasConcept C105306849 @default.
• W3010410033 hasConcept C105795698 @default.
• W3010410033 hasConcept C108597893 @default.
• W3010410033 hasConcept C120665830 @default.
• W3010410033 hasConcept C121332964 @default.
• W3010410033 hasConcept C127313418 @default.
• W3010410033 hasConcept C147789679 @default.
• W3010410033 hasConcept C153294291 @default.
• W3010410033 hasConcept C185592680 @default.
• W3010410033 hasConcept C191486275 @default.
• W3010410033 hasConcept C196937547 @default.
• W3010410033 hasConcept C205049153 @default.
• W3010410033 hasConcept C2778465081 @default.
• W3010410033 hasConcept C2780092901 @default.
• W3010410033 hasConcept C28493345 @default.
• W3010410033 hasConcept C30354325 @default.
• W3010410033 hasConcept C30475298 @default.
• W3010410033 hasConcept C33923547 @default.
• W3010410033 hasConcept C39432304 @default.
• W3010410033 hasConcept C41008148 @default.
• W3010410033 hasConcept C44280652 @default.
• W3010410033 hasConcept C554190296 @default.
• W3010410033 hasConcept C555944384 @default.
• W3010410033 hasConcept C62520636 @default.
• W3010410033 hasConcept C62649853 @default.
• W3010410033 hasConcept C76155785 @default.
• W3010410033 hasConcept C91586092 @default.
• W3010410033 hasConceptScore W3010410033C105306849 @default.
• W3010410033 hasConceptScore W3010410033C105795698 @default.
• W3010410033 hasConceptScore W3010410033C108597893 @default.
• W3010410033 hasConceptScore W3010410033C120665830 @default.

• next