2020
DOI: 10.1016/j.wace.2020.100265
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Spatio-temporal analysis of rainfall extremes in the flood-prone Nagavali and Vamsadhara Basins in eastern India

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Cited by 44 publications
(24 citation statements)
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“…This inconsistency still exists when considering the IMD dataset (Supplementary Table 5). Note that there have been significant increasing trends in frequency and intensity of extreme heavy rainfall over central and southern India since 1950 where regional climates are controlled by the Asian monsoon system (Krishnan et al, 2015;Roxy et al, 2017;Venkata Rao et al, 2020) (i.e., the core monsoon zones). Interestingly, despite a poor station coverage over the Maritime Continent, we find significant positive trends in four out of six datasets.…”
Section: Discussionmentioning
confidence: 99%
“…This inconsistency still exists when considering the IMD dataset (Supplementary Table 5). Note that there have been significant increasing trends in frequency and intensity of extreme heavy rainfall over central and southern India since 1950 where regional climates are controlled by the Asian monsoon system (Krishnan et al, 2015;Roxy et al, 2017;Venkata Rao et al, 2020) (i.e., the core monsoon zones). Interestingly, despite a poor station coverage over the Maritime Continent, we find significant positive trends in four out of six datasets.…”
Section: Discussionmentioning
confidence: 99%
“…The trends in datasets can either be monotonic, where a variable consistently increases or decreases through time, or a step trend, where abrupt changes in data may occur at a specific time. Various studies on trend analysis of climate parameters [11][12][13][15][16][17][18][19][21][22][23], used the two non-parametric tests known as the Mann-Kendall trend test, and Theil-Sen slope test, to detect significant trends, and to quantify the magnitude of trends, respectively.…”
Section: Trend Analysismentioning
confidence: 99%
“…A set of standard measurements of the extreme climate indices based daily precipitation, and daily (minimum and maximum) temperatures were provided by the Expert Team on Climate Change Detection and Indices (ETCCDI) [9,10]. For the past two decades, studies on trend analysis of ETCCDI indices [11][12][13][14][15][16][17][18][19][20][21][22][23], has been widely performed in different regions around the globe, through the use of Mann-Kendall (MK) trend test [24][25][26] and Theil-Sen (TS) slope estimator [27,28], both tests are rank-based non-parametric tests, that are insensitive to outliers and missing data. These recent studies were analyzed based on various temporal scales, ranging from annual [11][12][13][14][15][16][17][18][19][20][21][22][23], seasonal [13,[17][18][19], and monthly [19] time scales.…”
Section: Introductionmentioning
confidence: 99%
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“…On the other hand, as a result of global warming the capacity of the atmosphere to hold water has been increased which lead to an increase in the global precipitation [4][5][6][7][8][9]. In this context, a common way to have a knowledge of future extreme precipitation events is to investigate the trend in the longduration time series of historical records [10][11][12][13][14][15][16][17][18][19][20][21][22]. On the other hand, using the outputs of climate models such as global circulation models (GCMs) can provide a more reliable and more realistic picture of the future.…”
Section: Introductionmentioning
confidence: 99%