Background: The complexity of the distribution patterns of drought and soil water balance across various regions raises questions about how the mechanism of drought events responds to climate anomalies. The research aims to determine the climate anomaly pattern of maize drought levels based on land water balance with FAO Penman Monteith evapotranspiration value estimates in Gorontalo district, Indonesia. This research was carried out from April to August 2020. Methods: The research location was in Limboto subdistrict, Gorontalo Province, Indonesia. The material in this research is climate data from 1997 to 2016 (20 years) including rainfall, solar radiation, maximum and minimum air temperature, exposure time, air humidity and wind speed. The tools in this research are sample rings, Belgi drills, GPS, documentation tools. The method used is the drought index analysis method and the water adequacy index based on the FAO Penman Monteith evapotranspiration method. Result: El Nino and La Nina climate anomaly patterns occur every 5 to 7 year recurring period. The highest level of drought with strong drought status occurred during the El Nino anomaly in 1997-1998 for 8 months and this triggered a decrease in harvested area and corn production with a coefficient of reduction in vulnerable production category. La Niña climate anomaly years 1999 and 2007 had an impact on low accumulation potential of water loss with highest level of drought weak status and this triggered an increase in harvested area and corn production with a coefficient of reduction in very resistant production category.
Read full abstract