2021
DOI: 10.1016/j.wace.2021.100405
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A decision tree approach to identify predictors of extreme rainfall events – A case study for the Fiji Islands

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Cited by 3 publications
(6 citation statements)
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“…For example, the 20CR‐derived annual TC numbers in the entire South Pacific Ocean basin, as well as in the two sub‐regions east and west of the 170° E longitude, have underestimation biases in representing observed TC numbers from the SPEArTC dataset (Figure 1). Note that we have divided the South Pacific basin into two sub‐regions from ~170° E as they have opposite response to effects of ENSO variability (Chand & Walsh, 2009, 2011, 2012; Chand et al, 2010, 2013, 2020; Dowdy et al, 2012; Magee et al, 2017; Magee & Kiem, 2020; Maru et al, 2018; Ramsay et al, 2012; Sharma, Magee, & Verdon‐Kidd, 2021; Sharma, Verdon‐Kidd, & Magee, 2021).…”
Section: Resultsmentioning
confidence: 99%
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“…For example, the 20CR‐derived annual TC numbers in the entire South Pacific Ocean basin, as well as in the two sub‐regions east and west of the 170° E longitude, have underestimation biases in representing observed TC numbers from the SPEArTC dataset (Figure 1). Note that we have divided the South Pacific basin into two sub‐regions from ~170° E as they have opposite response to effects of ENSO variability (Chand & Walsh, 2009, 2011, 2012; Chand et al, 2010, 2013, 2020; Dowdy et al, 2012; Magee et al, 2017; Magee & Kiem, 2020; Maru et al, 2018; Ramsay et al, 2012; Sharma, Magee, & Verdon‐Kidd, 2021; Sharma, Verdon‐Kidd, & Magee, 2021).…”
Section: Resultsmentioning
confidence: 99%
“…The Graphical Interpretation of Tracks (GrIT) technique (Diamond et al, 2012) was used to establish some novel quality control and duplicate track detection processes in the development of SPEArTC. Hence, it considered more appropriate for TC frequency studies from around 1950 onwards for the South Pacific (e.g., Magee et al, 2016, 2017; Sharma, Verdon‐Kidd, Magee, 2021) compared with other observational data sources.…”
Section: Data Definitions and Methodsmentioning
confidence: 99%
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“…One common metric used to quantify extreme precipitation is the 95th percentile of the cumulative daily precipitation distribution [47], which was the definition used in this study. The 95th percentile metric has been used extensively in analysis of extreme events (e.g., [48][49][50][51]).…”
Section: Methodsmentioning
confidence: 99%