FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2092139027> ?p ?o ?g. }

• W2092139027 endingPage "44" @default.
• W2092139027 startingPage "16" @default.
• W2092139027 abstract "Convective precipitation associated with tropical depression (TD) is one primary type of post-flooding season rainfall in South China (SC). Observations of the Tropical Rainfall Measuring Mission (TRMM) satellite have shown specific diurnal features of convective rainfall in South China, which is somewhat different from that in other seasons or regions of China. Convective precipitation is usually organized into a rainfall band along the southeastern coast of South China in the early morning hours. The rainfall band develops and intensifies quickly in the morning, then moves inland in the afternoon and, finally, diminishes at night. The daily convective rainfall along the coast is much more than that in the inland region, and heavy rainfall is often found along the coast. A long-duration heavy rainfall event associated with tropical depression “Fitow” during the period from 28 August to 6 September 2001, is selected in this study to explore the diurnal feature of convective rainfall and its formation mechanism. Modeling results of the 10-day heavy rainfall event are compared with both rain-gauge observation and satellite-retrieved rainfall. Total precipitation and its spatial distribution, as well as diurnal variations are reasonably simulated and agree well with observations. Further analysis reveals that the development and movement of convective precipitation is mainly related to the land and sea breezes. The anomalous height-latitudinal circulation in the morning-to-noon hours is completely reversed in the afternoon-to-late-evening hours, with the convective rainfall swinging back and forth, following its updraft branch. Sensitivity experiments show that the afternoon convective rainfall in the inland region of SC is caused by the diurnal variation of solar radiation forcing. The mountain range along the coast and the complex topography in the inland region of SC plays a critical role in the enhancement of diurnal convective rainfall everywhere. The formation of a heavy rainfall band along the southeastern coast of SC and the diurnal variation of the rainfall pattern are mainly the results of the land-sea thermal contrast." @default.
• W2092139027 created "2016-06-24" @default.
• W2092139027 creator A5031571760 @default.
• W2092139027 date "2013-12-27" @default.
• W2092139027 modified "2023-10-18" @default.
• W2092139027 title "Diurnal Variation of Rainfall Associated with Tropical Depression in South China and its Relationship to Land-Sea Contrast and Topography" @default.
• W2092139027 cites W1610718871 @default.
• W2092139027 cites W1826780856 @default.
• W2092139027 cites W1975411539 @default.
• W2092139027 cites W1976204417 @default.
• W2092139027 cites W1980817947 @default.
• W2092139027 cites W1981670386 @default.
• W2092139027 cites W1983441418 @default.
• W2092139027 cites W1984559227 @default.
• W2092139027 cites W1986888501 @default.
• W2092139027 cites W1990402820 @default.
• W2092139027 cites W1991730448 @default.
• W2092139027 cites W1994235592 @default.
• W2092139027 cites W1995622703 @default.
• W2092139027 cites W1995626966 @default.
• W2092139027 cites W2000962843 @default.
• W2092139027 cites W2003625681 @default.
• W2092139027 cites W2006704253 @default.
• W2092139027 cites W2011018722 @default.
• W2092139027 cites W2014840824 @default.
• W2092139027 cites W2018256512 @default.
• W2092139027 cites W2019854863 @default.
• W2092139027 cites W2024805570 @default.
• W2092139027 cites W2030989004 @default.
• W2092139027 cites W2032790457 @default.
• W2092139027 cites W2034326114 @default.
• W2092139027 cites W2041200453 @default.
• W2092139027 cites W2042580095 @default.
• W2092139027 cites W2050904974 @default.
• W2092139027 cites W2063074811 @default.
• W2092139027 cites W2068166470 @default.
• W2092139027 cites W2077492770 @default.
• W2092139027 cites W2077712810 @default.
• W2092139027 cites W2078457486 @default.
• W2092139027 cites W2088378381 @default.
• W2092139027 cites W2089488727 @default.
• W2092139027 cites W2091159746 @default.
• W2092139027 cites W2103680334 @default.
• W2092139027 cites W2110904824 @default.
• W2092139027 cites W2117850731 @default.
• W2092139027 cites W2130614332 @default.
• W2092139027 cites W2132065420 @default.
• W2092139027 cites W2134506346 @default.
• W2092139027 cites W2136868324 @default.
• W2092139027 cites W2139940184 @default.
• W2092139027 cites W2143036607 @default.
• W2092139027 cites W2160893981 @default.
• W2092139027 cites W2173631438 @default.
• W2092139027 cites W2174684128 @default.
• W2092139027 cites W2175810071 @default.
• W2092139027 cites W2176395379 @default.
• W2092139027 cites W2178063404 @default.
• W2092139027 cites W2178851890 @default.
• W2092139027 cites W2180139275 @default.
• W2092139027 cites W1988760335 @default.
• W2092139027 doi "https://doi.org/10.3390/atmos5010016" @default.
• W2092139027 hasPublicationYear "2013" @default.
• W2092139027 type Work @default.
• W2092139027 sameAs 2092139027 @default.
• W2092139027 citedByCount "10" @default.
• W2092139027 countsByYear W20921390272015 @default.
• W2092139027 countsByYear W20921390272016 @default.
• W2092139027 countsByYear W20921390272017 @default.
• W2092139027 countsByYear W20921390272018 @default.
• W2092139027 countsByYear W20921390272020 @default.
• W2092139027 countsByYear W20921390272021 @default.
• W2092139027 countsByYear W20921390272022 @default.
• W2092139027 crossrefType "journal-article" @default.
• W2092139027 hasAuthorship W2092139027A5031571760 @default.
• W2092139027 hasBestOaLocation W20921390271 @default.
• W2092139027 hasConcept C107054158 @default.
• W2092139027 hasConcept C10899652 @default.
• W2092139027 hasConcept C11472968 @default.
• W2092139027 hasConcept C120961793 @default.
• W2092139027 hasConcept C121332964 @default.
• W2092139027 hasConcept C126322002 @default.
• W2092139027 hasConcept C127313418 @default.
• W2092139027 hasConcept C1276947 @default.
• W2092139027 hasConcept C136996986 @default.
• W2092139027 hasConcept C153294291 @default.
• W2092139027 hasConcept C167678106 @default.
• W2092139027 hasConcept C186293655 @default.
• W2092139027 hasConcept C19720800 @default.
• W2092139027 hasConcept C205649164 @default.
• W2092139027 hasConcept C2776476923 @default.
• W2092139027 hasConcept C2777864850 @default.
• W2092139027 hasConcept C29141058 @default.
• W2092139027 hasConcept C39432304 @default.
• W2092139027 hasConcept C41008148 @default.
• W2092139027 hasConcept C42935608 @default.
• W2092139027 hasConcept C49204034 @default.
• W2092139027 hasConcept C58650310 @default.
• W2092139027 hasConcept C61939431 @default.

• next