2020
DOI: 10.1371/journal.pone.0238709
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Investigating variations of precipitation concentration in the transitional zone between Qinling Mountains and Loess Plateau in China: Implications for regional impacts of AO and WPSH

Abstract: Changes in precipitation patterns greatly impact regional drought/flood risk management and utilization of water resources. The main purpose of this paper was to investigate spatio-temporal variability of precipitation concentration in the transitional zone between Qinling Mountains (QDM), Guanzhong Plain (GZP) and the Loess Plateau (LPNS) in China, using monthly-scale precipitation concentration index (PCI) and daily-scale concentration index (CI) from daily rainfall records. The Mann-Kendall method was emplo… Show more

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Cited by 18 publications
(9 citation statements)
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“…The spatial distribution of precipitation within the QRB was obtained by using the widely-used ordinary kriging interpolation method [37], which was reported to exhibit optimal precision and results for the interpolation of precipitation in the YR [38]. Figure 2 displays the spatial pattern of the average annual precipitation from 2006 to 2016.…”
Section: Precipitationmentioning
confidence: 99%
“…The spatial distribution of precipitation within the QRB was obtained by using the widely-used ordinary kriging interpolation method [37], which was reported to exhibit optimal precision and results for the interpolation of precipitation in the YR [38]. Figure 2 displays the spatial pattern of the average annual precipitation from 2006 to 2016.…”
Section: Precipitationmentioning
confidence: 99%
“…Global warming is intensifying the global hydrological cycle, making the wet and dry seasons more contrasting and more intense, while the frequency of sub seasonal precipitation is decreasing [ [20] , [21] , [22] ]. Rainy/dry periods or consecutive periods of rainy/dry days can be used to describe local weather patterns [ 23 ].…”
Section: Introductionmentioning
confidence: 99%
“…From 1960 to 2015, extreme precipitation events in the Qinling Mountains decreased, while their intensity increased, with change rates of 35.1 and −7.1 mm/10a in the north and south, respectively [8,9]. Most studies on extreme precipitation events in the Qinling Mountains have focused on annual and seasonal variations, influencing factors, and change trends during historical periods [10][11][12], paying little attention to future precipitation changes in the Qinling Mountains. At present, the consistency of research results on future precipitation in the Qinling Mountains is poor.…”
Section: Introductionmentioning
confidence: 99%