Statistics from BNPB (2019) indicate that between 2010-2018 around 87% of all natural disasters in Indonesia were related to hydrometeorology. The region is primarily associated with high rainfall accumulation. However, rainfall intensity regularly fluctuates and seasonal droughts do occur (Bonal et al. 2016). In the Maritime Continent, droughts can be attributed to a narrower Intertropical Convergence Zone (ITCZ) during some periods (Xavier et al. 2020). There is also a strong connection between droughts and Indonesian fires with type of El Niño and phase of the Indian Ocean Dipole (Pan et al. 2018). According to Meteorology, Climatology, and Geophysical Agency (BMKG), about 92% of Indonesia experienced drought in 2019 due to the El Niño cycle that began at the end of 2018 (Indonesian Red Cross, 2019).
BNPB, 2019: Indonesian National Agency for Disaster Countermeasure (Badan Nasional Penanggulangan Bencana (BNPB)). http:/bnpb.cloud/dibi/tabel1b (Accessed March 15, 2019).
Bonal, D., B. Burban, C. Stahl, F. Wagner, and B. Hérault, 2016: The response of tropical rainforests to drought—lessons from recent research and future prospects. Ann. For. Sci., https://doi.org/10.1007/s13595-015-0522-5.
Xavier, P., and Coauthors, 2020: Seasonal Dependence of Cold Surges and their Interaction with the Madden–Julian Oscillation over Southeast Asia. J. Clim., https://doi.org/10.1175/jcli-d-19-0048.1.
Pan, X., M. Chin, C. M. Ichoku, and R. D. Field, 2018: Connecting Indonesian Fires and Drought With the Type of El Niño and Phase of the Indian Ocean Dipole During 1979–2016. J. Geophys. Res. Atmos., https://doi.org/10.1029/2018JD028402.
Meteorological drought is a condition in which rainfall has decreased compared to the average. Hydrological drought occurs when low water supply becomes evident.
Different definitions which were applied to the rainfall data are described below.