FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4385803399> ?p ?o ?g. }

• W4385803399 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> Observations of vertical wind in Chongqing, a typical mountainous city in China, are important, but sparse and have low resolution. To obtain more wind profile data, this study matched the Aeolus track with ground-based wind observation sites in Chongqing in 2021. Based on the obtained results, verification and quality control studies were conducted on the wind observations of a wind profile radar (WPR) with radiosonde (RS) data, and a comparison of the Aeolus Mie-cloudy and Rayleigh-clear wind products with WPR data was then performed. The conclusions can be summarized as follows: (1) A clear correlation between the wind observations of WPR and RS was found, with a correlation coefficient (R) of 69.92 %. Their root-mean-square deviation increased with height but decreased by 3–4 km. (2) After quality control of Gaussian filtering (GF) and empirical orthogonal function construction (EOFc, G = 87.23 %) of the WPR data, the R between the WPR and RS reached 76.00 % and 95.44 %, respectively. The vertical distribution showed that GF could better retain the characteristics of WPR wind observations, but with limited improvement in decreasing deviations, whereas EOFc performed better in decreasing deviations, but considerably modified the original characteristics of the wind field, especially regarding intensive vertical wind shear in strong convective weather processes. (3) In terms of the differences between the Aeolus and WPR data, 56.0 % and 67.8 % deviations were observed between ±5 m/s for Rayleigh-clear and Mie-cloudy winds vs. WPR winds, respectively. Vertically, the mean differences of both Rayleigh-clean and Mie-cloudy winds versus WPR winds appeared below 1.5 km, which is attributed to the prevailing quiet and small winds within the boundary layer in Chongqing, such that the movement of molecules and aerosols is mostly affected by irregular turbulence. Additionally, large mean differences of 4–8 km for Mie-cloudy versus WPR winds may be related to the high content of cloud liquid water in the middle troposphere, influenced by the topography of the Tibetan Plateau. (4) The differences in both Rayleigh-clear and Mie-cloudy versus WPR winds had changed. Deviations of 58.9 % and 59.6 % were concentrated between ±5m/s for Rayleigh-clear versus WPR winds with GF and EOFc quality control, respectively. In contrast, 69.1 % and 70.2 % of deviations appeared between ±5 m/s for Rayleigh-clear versus WPR and EOFc WPR winds, respectively. These results shed light on the comprehensive applications of multi-source wind profile data in mountainous cities or areas with sparse ground-based wind observations." @default.
• W4385803399 created "2023-08-15" @default.
• W4385803399 date "2023-08-15" @default.
• W4385803399 modified "2023-10-14" @default.
• W4385803399 title "Comment on amt-2023-152" @default.
• W4385803399 doi "https://doi.org/10.5194/amt-2023-152-rc1" @default.
• W4385803399 hasPublicationYear "2023" @default.
• W4385803399 type Work @default.
• W4385803399 citedByCount "0" @default.
• W4385803399 crossrefType "peer-review" @default.
• W4385803399 hasBestOaLocation W43858033991 @default.
• W4385803399 hasConcept C105795698 @default.
• W4385803399 hasConcept C119599485 @default.
• W4385803399 hasConcept C11999413 @default.
• W4385803399 hasConcept C127413603 @default.
• W4385803399 hasConcept C135558025 @default.
• W4385803399 hasConcept C13724139 @default.
• W4385803399 hasConcept C153294291 @default.
• W4385803399 hasConcept C154718420 @default.
• W4385803399 hasConcept C161067210 @default.
• W4385803399 hasConcept C205649164 @default.
• W4385803399 hasConcept C22679943 @default.
• W4385803399 hasConcept C2780092901 @default.
• W4385803399 hasConcept C33923547 @default.
• W4385803399 hasConcept C39432304 @default.
• W4385803399 hasConcept C78600449 @default.
• W4385803399 hasConceptScore W4385803399C105795698 @default.
• W4385803399 hasConceptScore W4385803399C119599485 @default.
• W4385803399 hasConceptScore W4385803399C11999413 @default.
• W4385803399 hasConceptScore W4385803399C127413603 @default.
• W4385803399 hasConceptScore W4385803399C135558025 @default.
• W4385803399 hasConceptScore W4385803399C13724139 @default.
• W4385803399 hasConceptScore W4385803399C153294291 @default.
• W4385803399 hasConceptScore W4385803399C154718420 @default.
• W4385803399 hasConceptScore W4385803399C161067210 @default.
• W4385803399 hasConceptScore W4385803399C205649164 @default.
• W4385803399 hasConceptScore W4385803399C22679943 @default.
• W4385803399 hasConceptScore W4385803399C2780092901 @default.
• W4385803399 hasConceptScore W4385803399C33923547 @default.
• W4385803399 hasConceptScore W4385803399C39432304 @default.
• W4385803399 hasConceptScore W4385803399C78600449 @default.
• W4385803399 hasLocation W43858033991 @default.
• W4385803399 hasOpenAccess W4385803399 @default.
• W4385803399 hasPrimaryLocation W43858033991 @default.
• W4385803399 hasRelatedWork W1785986414 @default.
• W4385803399 hasRelatedWork W2020847322 @default.
• W4385803399 hasRelatedWork W2051151250 @default.
• W4385803399 hasRelatedWork W2130522552 @default.
• W4385803399 hasRelatedWork W2154551423 @default.
• W4385803399 hasRelatedWork W2392819665 @default.
• W4385803399 hasRelatedWork W2804195220 @default.
• W4385803399 hasRelatedWork W3148099466 @default.
• W4385803399 hasRelatedWork W4312511354 @default.
• W4385803399 hasRelatedWork W829829611 @default.
• W4385803399 isParatext "false" @default.
• W4385803399 isRetracted "false" @default.
• W4385803399 workType "peer-review" @default.