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Delineation of homogeneous hydrometeorological regions using wavelet‐based global fuzzy cluster analysis
Author(s) -
Bharath R.,
Srinivas V. V.
Publication year - 2015
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.4318
Subject(s) - hydrometeorology , wavelet , evapotranspiration , climatology , cluster analysis , univariate , computer science , statistics , multivariate statistics , environmental science , precipitation , econometrics , meteorology , geography , mathematics , geology , artificial intelligence , ecology , biology
Identification of homogeneous hydrometeorological regions (HMRs) is necessary for various applications. Such regions are delineated by various approaches considering rainfall and temperature as two key variables. In conventional approaches, formation of regions is based on principal components ( PCs )/statistics/indices determined from time series of the key variables at monthly and seasonal scales. An issue with use of PCs for regionalization is that they have to be extracted from contemporaneous records of hydrometeorological variables. Therefore, delineated regions may not be effective when the available records are limited over contemporaneous time period. A drawback associated with the use of statistics/indices is that they do not provide effective representation of the key variables when the records exhibit non‐stationarity. Consequently, the resulting regions may not be effective for the desired purpose. To address these issues, a new approach is proposed in this article. The approach considers information extracted from wavelet transformations of the observed multivariate hydrometeorological time series as the basis for regionalization by global fuzzy c ‐means clustering procedure. The approach can account for dynamic variability in the time series and its non‐stationarity (if any). Effectiveness of the proposed approach in forming HMRs is demonstrated by application to India, as there are no prior attempts to form such regions over the country. Drought severity‐area‐frequency ( SAF ) curves are constructed corresponding to each of the newly formed regions for the use in regional drought analysis, by considering standardized precipitation evapotranspiration index ( SPEI ) as the drought indicator.