FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2912256305> ?p ?o ?g. }

• W2912256305 endingPage "302" @default.
• W2912256305 startingPage "302" @default.
• W2912256305 abstract "Optical and geometrical characteristics of the cirrus clouds over Naqu (4508 m a.s.l., 31.48° N, 92.06° E), in the Tibetan Plateau were determined from LiDAR and radiosonde measurements performed during the third TIbetan Plateau EXperiment of atmospheric sciences (TIPEX III) campaign from July to August 2014. For the analysis of the temperature dependence, the simultaneous observations with LiDAR and radiosonde were conducted. Cirrus clouds were generally observed ranging from 5.2 km to 12 km above ground level (AGL) (i.e., 9.7 km to 16.5 km a.s.l.), with the midcloud temperatures ranging from −79.7 to −26.0 °C. The cloud thickness generally differed from 0.12 to 2.55 km with a mean thickness of 1.22 ± 0.70 km, and 85.7% of the measurement cases had thickness smaller than 1.5 km. The retrievals of linear particle depolarization ratio, extinction coefficient, and optical depth of cirrus clouds were provided. Moreover, the multiple scattering effect inside of cirrus clouds was corrected. The linear particle depolarization ratio of the cirrus clouds varied from 0.36 to 0.52, with a mean value of 0.44 ± 0.04. The optical depth of the cirrus clouds was between 0.01 and 3 following the scheme of Fernald-Klett method. Sub-visual, thin, and opaque cirrus clouds were observed at 4.76%, 61.90% and 33.34% of the measured cases, respectively. The temperature and thickness dependencies of the optical properties were studied in detail. A maximum cirrus thickness of around 2 km was found at temperatures between −60 and −50 °C. This study shows that the mean extinction coefficient of the cirrus clouds increases with the increase of temperature. Conversely, the measurements indicate that the linear particle depolarization ratio decreases with the increasing temperature. The relationships between the existence of cirrus clouds and the temperature anomaly (temperature difference from the mean value of the temperature during July and August 2014 over Naqu) and deep convective activity are also discussed. The formation of cirrus clouds is investigated and also its apparent relationship with the South Asia High Pressure, the dynamic processes of Rossby wave, and deep convective activity over the Tibetan Plateau. The outgoing longwave radiation of cirrus clouds is calculated with the Fu-Liou model and is shown to increases monotonously with the increase of optical depth." @default.
• W2912256305 created "2019-02-21" @default.
• W2912256305 creator A5009769244 @default.
• W2912256305 creator A5067016266 @default.
• W2912256305 creator A5069071194 @default.
• W2912256305 creator A5075043960 @default.
• W2912256305 date "2019-02-02" @default.
• W2912256305 modified "2023-10-03" @default.
• W2912256305 title "Optical and Geometrical Properties of Cirrus Clouds over the Tibetan Plateau Measured by LiDAR and Radiosonde Sounding during the Summertime in 2014" @default.
• W2912256305 cites W1964230818 @default.
• W2912256305 cites W1970917223 @default.
• W2912256305 cites W1973204902 @default.
• W2912256305 cites W1984046918 @default.
• W2912256305 cites W1984309167 @default.
• W2912256305 cites W1992596079 @default.
• W2912256305 cites W1995515323 @default.
• W2912256305 cites W2001418107 @default.
• W2912256305 cites W2008074672 @default.
• W2912256305 cites W2008594745 @default.
• W2912256305 cites W2017070381 @default.
• W2912256305 cites W2017317164 @default.
• W2912256305 cites W2020598345 @default.
• W2912256305 cites W2032503251 @default.
• W2912256305 cites W2038350547 @default.
• W2912256305 cites W2044318832 @default.
• W2912256305 cites W2045556497 @default.
• W2912256305 cites W2049992443 @default.
• W2912256305 cites W2056952189 @default.
• W2912256305 cites W2071405466 @default.
• W2912256305 cites W2073029903 @default.
• W2912256305 cites W2080054311 @default.
• W2912256305 cites W2085028454 @default.
• W2912256305 cites W2086916879 @default.
• W2912256305 cites W2087199341 @default.
• W2912256305 cites W2094202907 @default.
• W2912256305 cites W2098536579 @default.
• W2912256305 cites W2104915604 @default.
• W2912256305 cites W2105301940 @default.
• W2912256305 cites W2113814850 @default.
• W2912256305 cites W2120114636 @default.
• W2912256305 cites W2120182313 @default.
• W2912256305 cites W2124085558 @default.
• W2912256305 cites W2128182792 @default.
• W2912256305 cites W2131113592 @default.
• W2912256305 cites W2147024476 @default.
• W2912256305 cites W2155232959 @default.
• W2912256305 cites W2176500283 @default.
• W2912256305 cites W2177359352 @default.
• W2912256305 cites W2178914096 @default.
• W2912256305 cites W2211145027 @default.
• W2912256305 cites W2324374695 @default.
• W2912256305 cites W2470224965 @default.
• W2912256305 cites W2470467603 @default.
• W2912256305 cites W2572088766 @default.
• W2912256305 cites W2793416893 @default.
• W2912256305 doi "https://doi.org/10.3390/rs11030302" @default.
• W2912256305 hasPublicationYear "2019" @default.
• W2912256305 type Work @default.
• W2912256305 sameAs 2912256305 @default.
• W2912256305 citedByCount "8" @default.
• W2912256305 countsByYear W29122563052020 @default.
• W2912256305 countsByYear W29122563052022 @default.
• W2912256305 countsByYear W29122563052023 @default.
• W2912256305 crossrefType "journal-article" @default.
• W2912256305 hasAuthorship W2912256305A5009769244 @default.
• W2912256305 hasAuthorship W2912256305A5067016266 @default.
• W2912256305 hasAuthorship W2912256305A5069071194 @default.
• W2912256305 hasAuthorship W2912256305A5075043960 @default.
• W2912256305 hasBestOaLocation W29122563051 @default.
• W2912256305 hasConcept C111368507 @default.
• W2912256305 hasConcept C11999413 @default.
• W2912256305 hasConcept C121332964 @default.
• W2912256305 hasConcept C127313418 @default.
• W2912256305 hasConcept C134306372 @default.
• W2912256305 hasConcept C153294291 @default.
• W2912256305 hasConcept C2779185125 @default.
• W2912256305 hasConcept C2779345167 @default.
• W2912256305 hasConcept C2780030769 @default.
• W2912256305 hasConcept C2781448682 @default.
• W2912256305 hasConcept C27896171 @default.
• W2912256305 hasConcept C33923547 @default.
• W2912256305 hasConcept C39432304 @default.
• W2912256305 hasConcept C51399673 @default.
• W2912256305 hasConcept C55510283 @default.
• W2912256305 hasConcept C62649853 @default.
• W2912256305 hasConcept C91586092 @default.
• W2912256305 hasConceptScore W2912256305C111368507 @default.
• W2912256305 hasConceptScore W2912256305C11999413 @default.
• W2912256305 hasConceptScore W2912256305C121332964 @default.
• W2912256305 hasConceptScore W2912256305C127313418 @default.
• W2912256305 hasConceptScore W2912256305C134306372 @default.
• W2912256305 hasConceptScore W2912256305C153294291 @default.
• W2912256305 hasConceptScore W2912256305C2779185125 @default.
• W2912256305 hasConceptScore W2912256305C2779345167 @default.
• W2912256305 hasConceptScore W2912256305C2780030769 @default.
• W2912256305 hasConceptScore W2912256305C2781448682 @default.
• W2912256305 hasConceptScore W2912256305C27896171 @default.
• W2912256305 hasConceptScore W2912256305C33923547 @default.

• next