The standardized precipitation index (SPI) is a foundational tool for drought assessment. However, its application is constrained by complex probability distribution selection and mandatory normal transformation. To overcome these limitations, this study introduces a systematic framework that uses the Anderson–Darling test to optimize distribution selection. This approach refines drought evaluation through the actual precipitation index (API). By using untransformed precipitation data, the API enables a more direct climatic assessment. Results demonstrated strong consistency between the API and SPI across upper northern Thailand. Both indices successfully detected the 2011 regional floods and the 2015-2016 El Niño drought. Comparatively, the API demonstrated superior sensitivity to moisture saturation, particularly in Chiang Mai, Nan, and Phayao. Furthermore, spatial dynamic analysis using regular vine (R-vine) copulas identified Lampang as the primary regional hub. Lampang governs the central cluster (Chiang Mai, Lamphun, and Phrae) and mediates dependencies between Phayao and Chiang Rai. Nevertheless, localized geographic interactions create substantial concurrent extreme rainfall risks for the Chiang Mai–Lamphun pair. Because it preserves physical rainfall units, the API facilitates more actionable risk management than the SPI. Consequently, integrating R-vine copulas within the API framework is strongly recommended. This integration enhances spatial rainfall modeling, early warning systems, and adaptive water resource management, ultimately supporting climate resilience and sustainable development in vulnerable regions.
Citation: Kritdilada Luanmuang, Manad KhamKong, Nawapon Nakharutai, Pimwarat Srikummoon. Optimal distribution selection and spatial drought modeling in upper northern Thailand using an integrated actual precipitation index and regular vine copula framework[J]. AIMS Mathematics, 2026, 11(6): 16788-16810. doi: 10.3934/math.2026689
The standardized precipitation index (SPI) is a foundational tool for drought assessment. However, its application is constrained by complex probability distribution selection and mandatory normal transformation. To overcome these limitations, this study introduces a systematic framework that uses the Anderson–Darling test to optimize distribution selection. This approach refines drought evaluation through the actual precipitation index (API). By using untransformed precipitation data, the API enables a more direct climatic assessment. Results demonstrated strong consistency between the API and SPI across upper northern Thailand. Both indices successfully detected the 2011 regional floods and the 2015-2016 El Niño drought. Comparatively, the API demonstrated superior sensitivity to moisture saturation, particularly in Chiang Mai, Nan, and Phayao. Furthermore, spatial dynamic analysis using regular vine (R-vine) copulas identified Lampang as the primary regional hub. Lampang governs the central cluster (Chiang Mai, Lamphun, and Phrae) and mediates dependencies between Phayao and Chiang Rai. Nevertheless, localized geographic interactions create substantial concurrent extreme rainfall risks for the Chiang Mai–Lamphun pair. Because it preserves physical rainfall units, the API facilitates more actionable risk management than the SPI. Consequently, integrating R-vine copulas within the API framework is strongly recommended. This integration enhances spatial rainfall modeling, early warning systems, and adaptive water resource management, ultimately supporting climate resilience and sustainable development in vulnerable regions.
| [1] | Office of Agricultural Economics (OAE), Agricultural Statistics of Thailand, Bangkok, Thailand: Ministry of Agriculture and Cooperatives, 2020. Available from: https://oae.go.th/home/article/386. |
| [2] |
T. A. Räsänen, P. Someth, H. Lauri, J. Koponen, J. Sarkkula, M. Kummu, Observed river discharge changes due to hydropower operations and climate variability in the Mekong Basin, J. Hydrol., 545 (2017), 28–41. https://doi.org/10.1016/j.jhydrol.2016.12.023 doi: 10.1016/j.jhydrol.2016.12.023
|
| [3] | M. Khamkong, P. Bookkamana, Development of statistical models for maximum daily rainfall in upper northern region of Thailand, Chiang Mai J. Sci., 42 (2015), 1044–1053. |
| [4] | T. B. McKee, N. J. Doesken, J. Kleist, The relationship of drought frequency and duration to time scales, Proceedings of the 8th Conference on Applied Climatology, Anaheim, CA, USA: American Meteorological Society, 1993,179–184. |
| [5] |
S. M. Vicente-Serrano, S. Beguería, J. I. López-Moreno, A multiscalar drought index sensitive to global warming: the SPEI, J. Climate, 23 (2010), 1696–1718. https://doi.org/10.1175/2009JCLI2909.1 doi: 10.1175/2009JCLI2909.1
|
| [6] |
J. H. Stagge, L. M. Tallaksen, L. Gudmundsson, A. F. Van Loon, K. Stahl, Candidate distributions for climatological drought indices, Int. J. Climatol., 35 (2015), 4027–4040. https://doi.org/10.1002/joc.4267 doi: 10.1002/joc.4267
|
| [7] |
T. Chaito, M. Khamkong, Analyzing runoff variability index in northern Thailand using length-biased Weibull-Rayleigh distribution, AIMS Math., 10 (2025), 14539–14559. https://doi.org/10.3934/math.2025655 doi: 10.3934/math.2025655
|
| [8] |
Q. Zhang, C. Y. Xu, Z. Zhang, Observed changes of drought/wetness episodes in the Pearl River basin, China, using the standardized precipitation index and aridity index, Theor. Appl. Climatol., 98 (2009), 89–99. https://doi.org/10.1007/s00704-008-0095-4 doi: 10.1007/s00704-008-0095-4
|
| [9] |
F. Yusof, F. Hui-Mean, J. Suhaila, Z. Yusop, K. Ching-Yee, Rainfall characterisation by application of standardised precipitation index (SPI) in Peninsular Malaysia, Theor. Appl. Climatol., 115 (2014), 503–516. https://doi.org/10.1007/s00704-013-0918-9 doi: 10.1007/s00704-013-0918-9
|
| [10] |
J. Almedeij, Drought analysis for Kuwait using standardized precipitation index, Sci. World J., 2014 (2014), 451841. https://doi.org/10.1155/2014/451841 doi: 10.1155/2014/451841
|
| [11] |
Z. Şen, M. Almazroui, Actual precipitation index (API) for drought classification, Earth Syst. Environ., 5 (2021), 59–70. https://doi.org/10.1007/s41748-021-00201-0 doi: 10.1007/s41748-021-00201-0
|
| [12] |
F. Laio, G. Di Baldassarre, A. Montanari, Model selection techniques for the frequency analysis of hydrological extremes, Water Resour. Res., 45 (2009), W07416. https://doi.org/10.1029/2007WR006666 doi: 10.1029/2007WR006666
|
| [13] |
H. Akaike, A new look at the statistical model identification, IEEE Trans. Autom. Control., 19 (1974), 716–723. https://doi.org/10.1109/TAC.1974.1100705 doi: 10.1109/TAC.1974.1100705
|
| [14] |
H. Zhang, L. Chen, V. P. Singh, Flood frequency analysis using generalized distributions and entropy-based model selection method, J. Hydrol., 595 (2021), 125610. https://doi.org/10.1016/j.jhydrol.2020.125610 doi: 10.1016/j.jhydrol.2020.125610
|
| [15] |
H. Wu, M. D. Svoboda, M. J. Hayes, D. A. Wilhite, F. Wen, Appropriate application of the standardized precipitation index in arid locations and dry seasons, Int. J. Climatol., 27 (2007), 65–79. https://doi.org/10.1002/joc.1371 doi: 10.1002/joc.1371
|
| [16] |
K. Luanmuang, M. Kamkhong, N. Nakharutai, P. Srikummoon, An analysis of drought in the upper northern of Thailand using actual precipitation index, AIP Conf. Proc., 3123 (2024), 020012. https://doi.org/10.1063/5.0223852 doi: 10.1063/5.0223852
|
| [17] |
X. Chen, Q. Shao, C. Y. Xu, J. Zhang, L. Zhang, C. Ye, Comparative study on the selection criteria for fitting flood frequency distribution models with emphasis on upper-tail behavior, Water, 9 (2017), 320. https://doi.org/10.3390/w9050320 doi: 10.3390/w9050320
|
| [18] |
S. Morid, V. Smakhtin, M. Moghaddasi, Comparison of seven meteorological indices for drought monitoring in Iran, Int. J. Climatol., 26 (2006), 971–985. https://doi.org/10.1002/joc.1264 doi: 10.1002/joc.1264
|
| [19] | M. Abramowitz, I. A. Stegun, Handbook of mathematical functions with formulas, graphs, and mathematical tables, New York, NY, USA: Dover Publications, 1965. |
| [20] |
T. Chaito, M. Khamkong, A modified Box and Cox power transformation to determine the standardized precipitation index, Songklanakarin J. Sci. Technol., 40 (2018), 867–877. https://doi.org/10.14456/sjst-psu.2018.91 doi: 10.14456/sjst-psu.2018.91
|
| [21] |
T. Chaito, M. Khamkong, P. Murnta, Appropriate transformation techniques to determine a modified standardized precipitation index for the Ping River in northern Thailand, EnvironmentAsia, 12 (2019), 32–42. https://doi.org/10.14456/ea.2019.43 doi: 10.14456/ea.2019.43
|
| [22] |
A. K. Dey, D. Kundu, Discriminating among the log-normal, Weibull, and generalized exponential distributions, IEEE Trans. Reliab., 58 (2009), 416–424. https://doi.org/10.1109/TR.2009.2019494 doi: 10.1109/TR.2009.2019494
|
| [23] | Upper Northern Region Irrigation Hydrology Center, Rainfall data. Available from: http://www.hydro-1.net/. |
| [24] |
J. Dißmann, E. C. Brechmann, C. Czado, D. Kurowicka, Selecting and estimating regular vine copulae and application to financial returns, Comput. Stat. Data Anal., 59 (2013), 52–69. https://doi.org/10.1016/j.csda.2012.08.010 doi: 10.1016/j.csda.2012.08.010
|