Heterogeneous Correlation Mapping between Rainfall Variability in Lake Toba and Indian Ocean Sea Surface Temperature

Main Article Content

Mohamad Khoirun Najib
Sri Nurdiati

Abstract

Rainfall variability in the Lake Toba watershed of North Sumatra is influenced by large-scale ocean–atmosphere in-teractions, particularly those involving sea surface temperatures (SST) in the Indian Ocean. This study applies Heterogeneous Correlation Mapping (HCM) to examine the spatially varying relationship between monthly rainfall at 13 meteorological stations and SST over the Indian Ocean warm pool (5°S–10°N, 60°E–80°E) during 1981–2014. Singular Value Decomposition (SVD) is employed to extract dominant coupled modes of SST–rainfall variability. Results indicate that a six-month lag yields the strongest coupling, with the leading mode explaining 88.5% of the total variance. A clear spatial heterogeneity is observed: stations such as Lumban Julu and Silaen exhibit stronger SST–rainfall correlations, while others show weaker responses, likely due to topographic and local climatic modulation. These findings underscore the importance of accounting for spatial and temporal structures in hydroclimatic teleconnection analysis and offer insights for improving seasonal rainfall prediction in mountainous tropical regions

Article Details

How to Cite
Najib, M. K., & Nurdiati, S. (2026). Heterogeneous Correlation Mapping between Rainfall Variability in Lake Toba and Indian Ocean Sea Surface Temperature. (IJCSAM) International Journal of Computing Science and Applied Mathematics, 12(1), 7–12. https://doi.org/10.12962/j24775401.ijcsam.v12i1.7665
Section
Articles
Author Biographies

Mohamad Khoirun Najib, IPB University

School of Data Science, Mathematics, and Informatics

Sri Nurdiati, IPB University

School of Data Science, Mathematics, and Informatics

References

[1] Y. Chen, F. Y. Teo, S. Y. Wong, A. Chan, C. Weng, and R. A. Falconer, “Monsoonal extreme rainfall in Southeast Asia: A review,” Water, vol. 17, no. 1, p. 5, Jan. 2024.

[2] C. Yao, W. Qian, S. Yang, and Z. Lin, “Regional features of precipitation over Asia and summer extreme precipitation over Southeast Asia and their associations with atmospheric–oceanic conditions,” Meteorology and Atmospheric Physics, vol. 106, no. 1, pp. 57–73, Jan. 2010.

[3] D. Cui, C. Wang, and J. Santisirisomboon, “Characteristics of extreme precipitation over eastern Asia and its possible connections with Asian summer monsoon activity,” International Journal of Climatology, vol. 39, pp. 711–723, 2019.

[4] A. Kurniadi, E. Weller, S.-K. Min, and M.-G. Seong, “Independent ENSO and IOD impacts on rainfall extremes over Indonesia,” Inter-

national Journal of Climatology, vol. 41, no. 6, pp. 3640–3656, 2021.

[5] M. N. Nur’utami and R. Hidayat, “Influences of IOD and ENSO to Indonesian rainfall variability: Role of atmosphere–ocean interaction in the Indo-Pacific sector,” Procedia Environmental Sciences, vol. 33, pp. 196–203, 2016.

[6] H. Irwandi, M. S. Rosid, and T. Mart, “The effects of ENSO, climate change and human activities on the water level of Lake Toba, Indonesia: A critical literature review,” Geoscience Letters, vol. 8, no. 1, p. 21, 2021.

[7] H. Irwandi, N. Pusparini, J. Y. Ariantono, R. Kurniawan, C. A. Tari, and A. Sudrajat, “The influence of ENSO to the rainfall variability in

North Sumatra Province,” in IOP Conference Series: Materials Science and Engineering, vol. 335, no. 1, p. 012055, 2018.

[8] A. Olita, A. Ribotti, R. Sorgente, L. Fazioli, and A. Perilli, “SLA–chlorophyll-a variability and covariability in the Algero-Provenc¸al Basin (1997–2007) through combined use of EOF and wavelet analysis of satellite data,” Ocean Dynamics, vol. 61, no. 1, pp. 89–102, 2011.

[9] S. Nurdiati, F. Bukhari, M. T. Julianto, M. K. Najib, and N. Nazria, “Heterogeneous correlation map between estimated ENSO and IOD

from ERA5 and hotspot in Indonesia,” Jambura Geoscience Review, vol. 3, no. 2, pp. 65–72, Jul. 2021.

[10] A. Mulsandi, Y. Koesmaryono, R. Hidayat, A. Faqih, and A. Sopaheluwakan, “Detecting Indonesian monsoon signals and related features using space–time singular value decomposition (SVD),” Atmosphere, vol. 15, no. 2, p. 187, 2024.

[11] R. E. Benestad, A. Mezghani, J. Lutz, A. Dobler, K. M. Parding, and O. A. Landgren, “Various ways of using empirical orthogonal functions for climate model evaluation,” Geoscientific Model Development, vol. 16, no. 10, pp. 2899–2913, 2023.

[12] A. Hannachi, Patterns Identification and Data Mining in Weather and Climate. Cham, Switzerland: Springer, 2021.

[13] Z. Qiao, C. Wu, N. Huang, X. Xu, Z. Sun, and X. Sun, “Spatio-temporal structure of the urban thermal environment in Beijing based on an empirical orthogonal function,” Journal of Spatial Science, vol. 63, no. 2, pp. 297–310, 2018.

[14] C. A. Chesner, “Geologic studies of the Toba supereruption source caldera, Indonesia,” Journal of Volcanology and Geothermal Research, vols. 239–240, pp. 1–12, 2012. https://doi.org/10.1016/j.jvolgeores.2012.06.018

[15] R. I. Lukman and I. Ridwansyah, “Kajian kondisi morfometri dan beberapa parameter stratifikasi perairan Danau Toba,” Jurnal Limnotek, vol. 18, no. 2, pp. 83–96, 2011.

[16] M. Williams, “Climate change in Lake Toba, Indonesia,”Quaternary International, vol. 258, pp. 149–158, 2012. https://doi.org/10.1016/j.quaint.2011.06.005

[17] A. Navarra and V. Simoncini, A Guide to Empirical Orthogonal Functions for Climate Data Analysis. Dordrecht, The Netherlands: Springer, 2010, ch. 4.

[18] S. Nurdiati, E. Khatizah, M. K. Najib, and R. R. Hidayah, “Analysis of rainfall patterns in Kalimantan using fast Fourier transform (FFT) and empirical orthogonal function (EOF),” in Journal of Physics: Conference Series, vol. 1796, no. 1, p. 012053, 2021.

[19] A. H. Monahan, J. C. Fyfe, M. H. P. Ambaum, D. B. Stephenson, and G. R. North, “Empirical orthogonal functions: The medium is the message,” Journal of Climate, vol. 22, no. 24, pp. 6501–6514, 2009.

[20] M. K. Najib, S. Nurdiati, and A. Sopaheluwakan, “Copula-based joint distribution analysis of the ENSO effect on the drought indicators over Borneo fire-prone areas,” Modeling Earth Systems and Environment, vol. 8, no. 2, pp. 2817–2826, 2022.

[21] M. K. Najib, S. Nurdiati, and A. Sopaheluwakan, “Multivariate fire risk models using copula regression in Kalimantan, Indonesia,” Natural Hazards, vol. 113, no. 2, pp. 1263–1283, 2022.

[22] E. Aldrian and R. D. Susanto, “Identification of three dominant rainfall regions within Indonesia and their relationship to sea surface temperature,” International Journal of Climatology, vol. 23, no. 12, pp. 1435–1452, 2003, doi: 10.1002/joc.950.