FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2885388317> ?p ?o ?g. }

• W2885388317 endingPage "78" @default.
• W2885388317 startingPage "64" @default.
• W2885388317 abstract "Based on daily maximum temperature (Tmax), daily minimum temperature (Tmin) and daily precipitation collected from 1867 meteorological stations in China from 1961 to 2015, the spatiotemporal variations in temperature and precipitation extremes and their associations with large-scale atmospheric and oceanic circulation patterns were analyzed using linear trend analysis, Pearson correlation analysis and Mann-Kendall method. Results indicate that both the maximum Tmin (TNx) and the minimum Tmin (TNn) had increased significantly at rates of 0–0.5 °C and 0.2–1.0 °C per decade respectively in most of China, whereas the trends in the maximum Tmax (TXx) and the minimum Tmax (TXn) were not significant, resulting in a decrease of diurnal temperature range (DTR) at rates of 0–0.7 °C per decade in most of northeastern China, northern China and western China. The percentage changes in TXn and TNn were much higher than those of TXx and TNx. For precipitation indices, simple daily intensity index (SDII) and extremely wet-day precipitation (R99p) had increased at rates of 0.10 mm/day and 2.6 mm per decade respectively, but the trends of maximum 1-day precipitation (Rx1day), maximum 5-day precipitation (Rx5day) and total wet-day precipitation (PRCPTOT) were not significant in China. The spatial trends of five precipitation indices were also not significant in almost the whole of China. Higher percentage changes of precipitation indices were mainly appeared in western China. Most of climatic indices had positive correlation with Atlantic multidecadal oscillation (AMO) and negative correlation with East Atlantic/Western Russia (EA/WR). The variations of TXx and TNx were more related to the variability of AMO and EA/WR in China, and those of TXn and TNn were more associated with the Arctic oscillation (AO) in northeastern China, northern China and northern Xinjiang. The variations of precipitation indices were not significantly related to the circulation patterns in the vast majority of China." @default.
• W2885388317 created "2018-08-22" @default.
• W2885388317 creator A5006691049 @default.
• W2885388317 creator A5037062669 @default.
• W2885388317 creator A5058091698 @default.
• W2885388317 creator A5082720626 @default.
• W2885388317 creator A5088170512 @default.
• W2885388317 date "2019-08-01" @default.
• W2885388317 modified "2023-10-17" @default.
• W2885388317 title "Changes in the temperature and precipitation extremes in China during 1961–2015" @default.
• W2885388317 cites W1475046854 @default.
• W2885388317 cites W1913722913 @default.
• W2885388317 cites W1923883847 @default.
• W2885388317 cites W1975571057 @default.
• W2885388317 cites W1976413921 @default.
• W2885388317 cites W1978896016 @default.
• W2885388317 cites W1983460777 @default.
• W2885388317 cites W1990635923 @default.
• W2885388317 cites W1995349031 @default.
• W2885388317 cites W2000679372 @default.
• W2885388317 cites W2007489277 @default.
• W2885388317 cites W2009947463 @default.
• W2885388317 cites W2015137132 @default.
• W2885388317 cites W2017405272 @default.
• W2885388317 cites W2020297738 @default.
• W2885388317 cites W2021973688 @default.
• W2885388317 cites W2026776617 @default.
• W2885388317 cites W2031009006 @default.
• W2885388317 cites W2039200886 @default.
• W2885388317 cites W2040740595 @default.
• W2885388317 cites W2050969011 @default.
• W2885388317 cites W2053735647 @default.
• W2885388317 cites W2056606453 @default.
• W2885388317 cites W2056619885 @default.
• W2885388317 cites W2060350073 @default.
• W2885388317 cites W2082319382 @default.
• W2885388317 cites W2085315592 @default.
• W2885388317 cites W2090367398 @default.
• W2885388317 cites W2093578704 @default.
• W2885388317 cites W2101003198 @default.
• W2885388317 cites W2129068257 @default.
• W2885388317 cites W2134104608 @default.
• W2885388317 cites W2142546117 @default.
• W2885388317 cites W2151377141 @default.
• W2885388317 cites W2176774719 @default.
• W2885388317 cites W2239353230 @default.
• W2885388317 cites W2286181713 @default.
• W2885388317 cites W2304126200 @default.
• W2885388317 cites W2313575986 @default.
• W2885388317 cites W2460749911 @default.
• W2885388317 cites W2516748092 @default.
• W2885388317 cites W2591173330 @default.
• W2885388317 cites W2593293539 @default.
• W2885388317 cites W2593810587 @default.
• W2885388317 cites W2622427083 @default.
• W2885388317 cites W2702199532 @default.
• W2885388317 cites W2729186703 @default.
• W2885388317 cites W2738034153 @default.
• W2885388317 cites W2765115937 @default.
• W2885388317 cites W2769041836 @default.
• W2885388317 cites W2793250537 @default.
• W2885388317 cites W2796073907 @default.
• W2885388317 cites W905826617 @default.
• W2885388317 doi "https://doi.org/10.1016/j.quaint.2018.08.008" @default.
• W2885388317 hasPublicationYear "2019" @default.
• W2885388317 type Work @default.
• W2885388317 sameAs 2885388317 @default.
• W2885388317 citedByCount "24" @default.
• W2885388317 countsByYear W28853883172019 @default.
• W2885388317 countsByYear W28853883172020 @default.
• W2885388317 countsByYear W28853883172021 @default.
• W2885388317 countsByYear W28853883172022 @default.
• W2885388317 countsByYear W28853883172023 @default.
• W2885388317 crossrefType "journal-article" @default.
• W2885388317 hasAuthorship W2885388317A5006691049 @default.
• W2885388317 hasAuthorship W2885388317A5037062669 @default.
• W2885388317 hasAuthorship W2885388317A5058091698 @default.
• W2885388317 hasAuthorship W2885388317A5082720626 @default.
• W2885388317 hasAuthorship W2885388317A5088170512 @default.
• W2885388317 hasConcept C107054158 @default.
• W2885388317 hasConcept C11308688 @default.
• W2885388317 hasConcept C126322002 @default.
• W2885388317 hasConcept C127313418 @default.
• W2885388317 hasConcept C153294291 @default.
• W2885388317 hasConcept C166957645 @default.
• W2885388317 hasConcept C167678106 @default.
• W2885388317 hasConcept C17093552 @default.
• W2885388317 hasConcept C191935318 @default.
• W2885388317 hasConcept C205649164 @default.
• W2885388317 hasConcept C2985831756 @default.
• W2885388317 hasConcept C2988405389 @default.
• W2885388317 hasConcept C39432304 @default.
• W2885388317 hasConcept C49204034 @default.
• W2885388317 hasConcept C71924100 @default.
• W2885388317 hasConcept C91586092 @default.
• W2885388317 hasConceptScore W2885388317C107054158 @default.
• W2885388317 hasConceptScore W2885388317C11308688 @default.
• W2885388317 hasConceptScore W2885388317C126322002 @default.

• next