Matches in SemOpenAlex for { <https://semopenalex.org/work/W3205726262> ?p ?o ?g. }
- W3205726262 endingPage "248" @default.
- W3205726262 startingPage "227" @default.
- W3205726262 abstract "Abstract Changes in precipitation seasonality or the distribution of precipitation have important impacts on hydrological extremes (e.g., floods or droughts). Precipitation extremes have been widely reported to increase with global warming; however, the variability and mechanism of precipitation seasonality have not been well quantified in China. Here, we explore the multiscale variability in precipitation seasonality from 1960 to 2018 in China. A seasonality index of precipitation is defined to quantify the precipitation seasonality with a lower value indicating a more even distribution throughout a year. The seasonality index increases from southeastern to northwestern China, with a decrease in the annual mean precipitation, a later timing of the wet season, and a shorter wet season duration. The seasonality index decreases from 1960 to 2018 in China, accompanied by the increasing duration of wet season, especially in northern climate-sensitive basins, such as the Northwest River, Hai River, and Songliao River basins. In the Northwest River basin, for example, the observed significant decrease in the seasonality index (~0.02 decade −1 ) from 1960 to 2018 is consistent with a significant decrease in the ratio of annual maximum 10-day precipitation to annual precipitation, which is confirmed by their significant positive correlation ( R = 0.72; p = 0). El Niño–Southern Oscillation (ENSO) dominates interannual fluctuations and spatial patterns of precipitation seasonality in China. In El Niño years, the precipitation seasonality index decreases across China except for the Yangtze River basin, with broad increases in annual precipitation." @default.
- W3205726262 created "2021-10-25" @default.
- W3205726262 creator A5009394525 @default.
- W3205726262 creator A5048849178 @default.
- W3205726262 creator A5071308361 @default.
- W3205726262 creator A5087913492 @default.
- W3205726262 date "2022-01-01" @default.
- W3205726262 modified "2023-10-14" @default.
- W3205726262 title "Reduction in Precipitation Seasonality in China from 1960 to 2018" @default.
- W3205726262 cites W1452618852 @default.
- W3205726262 cites W1574976822 @default.
- W3205726262 cites W1785409029 @default.
- W3205726262 cites W1795688558 @default.
- W3205726262 cites W1812730403 @default.
- W3205726262 cites W1887193019 @default.
- W3205726262 cites W1966186652 @default.
- W3205726262 cites W1970103377 @default.
- W3205726262 cites W1973110714 @default.
- W3205726262 cites W1983123344 @default.
- W3205726262 cites W1988493564 @default.
- W3205726262 cites W1992661975 @default.
- W3205726262 cites W2000218464 @default.
- W3205726262 cites W2000755878 @default.
- W3205726262 cites W2009690705 @default.
- W3205726262 cites W2012138111 @default.
- W3205726262 cites W2018764772 @default.
- W3205726262 cites W2029993861 @default.
- W3205726262 cites W2042933397 @default.
- W3205726262 cites W2051483247 @default.
- W3205726262 cites W2052692754 @default.
- W3205726262 cites W2055422189 @default.
- W3205726262 cites W2056163179 @default.
- W3205726262 cites W2069460427 @default.
- W3205726262 cites W2071485587 @default.
- W3205726262 cites W2075793519 @default.
- W3205726262 cites W2103888668 @default.
- W3205726262 cites W2128628509 @default.
- W3205726262 cites W2130557413 @default.
- W3205726262 cites W2138408792 @default.
- W3205726262 cites W2138680286 @default.
- W3205726262 cites W2158112716 @default.
- W3205726262 cites W2158535548 @default.
- W3205726262 cites W2162606350 @default.
- W3205726262 cites W2165641465 @default.
- W3205726262 cites W2234594242 @default.
- W3205726262 cites W2255287630 @default.
- W3205726262 cites W2265765003 @default.
- W3205726262 cites W2276270457 @default.
- W3205726262 cites W2290653984 @default.
- W3205726262 cites W2299979294 @default.
- W3205726262 cites W2306704302 @default.
- W3205726262 cites W2318680928 @default.
- W3205726262 cites W2328573691 @default.
- W3205726262 cites W2335706095 @default.
- W3205726262 cites W2398251484 @default.
- W3205726262 cites W2399488999 @default.
- W3205726262 cites W2491513442 @default.
- W3205726262 cites W2509078861 @default.
- W3205726262 cites W2544051602 @default.
- W3205726262 cites W2548253312 @default.
- W3205726262 cites W2556345248 @default.
- W3205726262 cites W2582873487 @default.
- W3205726262 cites W2588490232 @default.
- W3205726262 cites W2606154988 @default.
- W3205726262 cites W2733580920 @default.
- W3205726262 cites W2735706617 @default.
- W3205726262 cites W2742211115 @default.
- W3205726262 cites W2751568030 @default.
- W3205726262 cites W2765294988 @default.
- W3205726262 cites W2765349378 @default.
- W3205726262 cites W2768413744 @default.
- W3205726262 cites W2773582012 @default.
- W3205726262 cites W2785818389 @default.
- W3205726262 cites W2790240715 @default.
- W3205726262 cites W2791708206 @default.
- W3205726262 cites W2792444893 @default.
- W3205726262 cites W2793414713 @default.
- W3205726262 cites W2793521721 @default.
- W3205726262 cites W2793629918 @default.
- W3205726262 cites W2801966091 @default.
- W3205726262 cites W2806504306 @default.
- W3205726262 cites W2810239705 @default.
- W3205726262 cites W2828472803 @default.
- W3205726262 cites W2885645126 @default.
- W3205726262 cites W2887688776 @default.
- W3205726262 cites W2888304208 @default.
- W3205726262 cites W2896173661 @default.
- W3205726262 cites W2901008040 @default.
- W3205726262 cites W2905138547 @default.
- W3205726262 cites W2910862611 @default.
- W3205726262 cites W2921069043 @default.
- W3205726262 cites W2921652195 @default.
- W3205726262 cites W2922633580 @default.
- W3205726262 cites W2943739006 @default.
- W3205726262 cites W2944607176 @default.
- W3205726262 cites W2946264511 @default.
- W3205726262 cites W2946371073 @default.
- W3205726262 cites W2948694578 @default.