Exact(6)
The data were collected after two consecutive rainfall events.
That is, EOF1 mainly shows consecutive rainfall variations from late May to mid-December, which are characterized by the onset and withdrawal of the southwest monsoon.
In particular, the influence on retention time of the possibility of water mixing from consecutive rainfall events, due to the pre-filling of the storage capacity from previous runoffs has been investigated.
The difference in rainfall amount between 3- and the 4-day consecutive rainfall is found to be less up to the 60-year return periods and increasing differential amount is observed for the remaining return periods.
The surface layer at an initially unsaturated state (2000 kPa ± 500 kPa) imbibed water made available from May through August by rainfall events and lost that water between consecutive rainfall events.
The fundamental data execution was carried out using the Mann-Kendall test (Mann 1945; Kendall 1975) and auto-correlation function (ACF) analysis to verify the maximum 24 h consecutive rainfall which is convenient for regional frequency analysis.
Similar(54)
The curve corresponding to LP III distribution shows low Chi-square values for 2- to 5-day consecutive rainfalls.
Table 1 shows the maximum rainfall amount for the 10-, 50- and 100-year return periods for 1- to 5-day consecutive rainfalls.
The analysis of results indicate that the there is a significant difference in rainfall amount between the 10-year and 50-year return periods for 1- to 5-day consecutives rainfall.
The frequency distribution procedure of maximum consecutive hour rainfall data in a homogeneous region consist of similar quantile distribution (Dalrymple 1960).
The maximum consecutive hour rainfall data was analyzed using L-moments approach, to study the spatial homogeneity, probability distributions and as well as regional frequency estimates.
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