FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2533438009> ?p ?o ?g. }

• W2533438009 endingPage "2252" @default.
• W2533438009 startingPage "2239" @default.
• W2533438009 abstract "Abstract. This study presents the evaluation of a technique to estimate cloud condensed water content (CWC) in tropical convection from airborne cloud radar reflectivity factors at 94 GHz and in situ measurements of particle size distributions (PSDs) and aspect ratios of ice crystal populations. The approach is to calculate from each 5 s mean PSD and flight-level reflectivity the variability of all possible solutions of m(D) relationships fulfilling the condition that the simulated radar reflectivity factor (T-matrix method) matches the measured radar reflectivity factor. For the reflectivity simulations, ice crystals were approximated as oblate spheroids, without using a priori assumptions on the mass–size relationship of ice crystals. The CWC calculations demonstrate that individual CWC values are in the range ±32 % of the retrieved average CWC value over all CWC solutions for the chosen 5 s time intervals. In addition, during the airborne field campaign performed out of Darwin in 2014, as part of the international High Altitude Ice Crystals/High Ice Water Content (HAIC/HIWC) projects, CWCs were measured independently with the new IKP-2 (isokinetic evaporator probe) instrument along with simultaneous particle imagery and radar reflectivity. Retrieved CWCs from the T-matrix radar reflectivity simulations are on average 16 % higher than the direct CWCIKP measurements. The differences between the CWCIKP and averaged retrieved CWCs are found to be primarily a function of the total number concentration of ice crystals. Consequently, a correction term is applied (as a function of total number concentration) that significantly improves the retrieved CWC. After correction, the retrieved CWCs have a median relative error with respect to measured values of only −1 %. Uncertainties in the measurements of total concentration of hydrometeors are investigated in order to calculate their contribution to the relative error of calculated CWC with respect to measured CWCIKP. It is shown that an overestimation of the concentration by about +50 % increases the relative errors of retrieved CWCs by only +29 %, while possible shattering, which impacts only the concentration of small hydrometeors, increases the relative error by about +4 %. Moreover, all cloud events with encountered graupel particles were studied and compared to events without observed graupel particles. Overall, graupel particles seem to have the largest impact on high crystal number-concentration conditions and show relative errors in retrieved CWCs that are higher than for events without graupel particles." @default.
• W2533438009 created "2016-10-28" @default.
• W2533438009 creator A5016737297 @default.
• W2533438009 creator A5033187323 @default.
• W2533438009 creator A5035770243 @default.
• W2533438009 creator A5042792326 @default.
• W2533438009 creator A5049926850 @default.
• W2533438009 creator A5060224773 @default.
• W2533438009 creator A5062609856 @default.
• W2533438009 creator A5077592032 @default.
• W2533438009 creator A5083129216 @default.
• W2533438009 date "2017-06-13" @default.
• W2533438009 modified "2023-10-14" @default.
• W2533438009 title "Evaluation of radar reflectivity factor simulations of ice crystal populations from in situ observations for the retrieval of condensed water content in tropical mesoscale convective systems" @default.
• W2533438009 cites W1594754229 @default.
• W2533438009 cites W1600730687 @default.
• W2533438009 cites W1613795631 @default.
• W2533438009 cites W1976674106 @default.
• W2533438009 cites W1979514218 @default.
• W2533438009 cites W1979895664 @default.
• W2533438009 cites W1981601556 @default.
• W2533438009 cites W2029646713 @default.
• W2533438009 cites W2044940833 @default.
• W2533438009 cites W2060398853 @default.
• W2533438009 cites W2078522113 @default.
• W2533438009 cites W2091458129 @default.
• W2533438009 cites W2092777356 @default.
• W2533438009 cites W2109291292 @default.
• W2533438009 cites W2110261132 @default.
• W2533438009 cites W2122070295 @default.
• W2533438009 cites W2135239023 @default.
• W2533438009 cites W2136309870 @default.
• W2533438009 cites W2139782007 @default.
• W2533438009 cites W2153113147 @default.
• W2533438009 cites W2156857940 @default.
• W2533438009 cites W2159853514 @default.
• W2533438009 cites W2162246342 @default.
• W2533438009 cites W2171093281 @default.
• W2533438009 cites W2176622002 @default.
• W2533438009 cites W2326035820 @default.
• W2533438009 cites W2389277551 @default.
• W2533438009 cites W2418543131 @default.
• W2533438009 cites W2520952949 @default.
• W2533438009 cites W2550614314 @default.
• W2533438009 cites W2977789091 @default.
• W2533438009 doi "https://doi.org/10.5194/amt-10-2239-2017" @default.
• W2533438009 hasPublicationYear "2017" @default.
• W2533438009 type Work @default.
• W2533438009 sameAs 2533438009 @default.
• W2533438009 citedByCount "9" @default.
• W2533438009 countsByYear W25334380092017 @default.
• W2533438009 countsByYear W25334380092019 @default.
• W2533438009 countsByYear W25334380092020 @default.
• W2533438009 countsByYear W25334380092021 @default.
• W2533438009 countsByYear W25334380092022 @default.
• W2533438009 countsByYear W25334380092023 @default.
• W2533438009 crossrefType "journal-article" @default.
• W2533438009 hasAuthorship W2533438009A5016737297 @default.
• W2533438009 hasAuthorship W2533438009A5033187323 @default.
• W2533438009 hasAuthorship W2533438009A5035770243 @default.
• W2533438009 hasAuthorship W2533438009A5042792326 @default.
• W2533438009 hasAuthorship W2533438009A5049926850 @default.
• W2533438009 hasAuthorship W2533438009A5060224773 @default.
• W2533438009 hasAuthorship W2533438009A5062609856 @default.
• W2533438009 hasAuthorship W2533438009A5077592032 @default.
• W2533438009 hasAuthorship W2533438009A5083129216 @default.
• W2533438009 hasBestOaLocation W25334380091 @default.
• W2533438009 hasConcept C121332964 @default.
• W2533438009 hasConcept C125388846 @default.
• W2533438009 hasConcept C127313418 @default.
• W2533438009 hasConcept C153294291 @default.
• W2533438009 hasConcept C159985019 @default.
• W2533438009 hasConcept C192562407 @default.
• W2533438009 hasConcept C204323151 @default.
• W2533438009 hasConcept C39432304 @default.
• W2533438009 hasConcept C40382383 @default.
• W2533438009 hasConcept C41008148 @default.
• W2533438009 hasConcept C554190296 @default.
• W2533438009 hasConcept C62649853 @default.
• W2533438009 hasConcept C76155785 @default.
• W2533438009 hasConcept C91586092 @default.
• W2533438009 hasConceptScore W2533438009C121332964 @default.
• W2533438009 hasConceptScore W2533438009C125388846 @default.
• W2533438009 hasConceptScore W2533438009C127313418 @default.
• W2533438009 hasConceptScore W2533438009C153294291 @default.
• W2533438009 hasConceptScore W2533438009C159985019 @default.
• W2533438009 hasConceptScore W2533438009C192562407 @default.
• W2533438009 hasConceptScore W2533438009C204323151 @default.
• W2533438009 hasConceptScore W2533438009C39432304 @default.
• W2533438009 hasConceptScore W2533438009C40382383 @default.
• W2533438009 hasConceptScore W2533438009C41008148 @default.
• W2533438009 hasConceptScore W2533438009C554190296 @default.
• W2533438009 hasConceptScore W2533438009C62649853 @default.
• W2533438009 hasConceptScore W2533438009C76155785 @default.
• W2533438009 hasConceptScore W2533438009C91586092 @default.
• W2533438009 hasIssue "6" @default.
• W2533438009 hasLocation W25334380091 @default.
• W2533438009 hasLocation W25334380092 @default.

• next