05/09/2026
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CRITICAL SOIL MOISTURE DEFICIT PERSISTS NATIONWIDE
βLatest soil moisture data shows deep subsoil drought conditions remaining at critical to extreme levels across extensive areas of Luzon, Visayas, and Mindanao.
βAFFECTED PROVINCES BY DROUGHT SEVERITY
(Categorized based on the highest drought intensity level present within any part of the province)
π΄ βEXCEPTIONAL TO EXTREME
βͺοΈ MINDANAO: Agusan del Norte, Agusan del Sur, Basilan, Bukidnon, Cotabato (North Cotabato), Davao City, Davao de Oro, Davao del Norte, Davao del Sur, Davao Occidental, Davao Oriental, Lanao del Norte, Lanao del Sur, Maguindanao del Norte, Maguindanao del Sur, Misamis Occidental, Misamis Oriental, Sarangani, South Cotabato, Sultan Kudarat, Surigao del Norte, Surigao del Sur, Zamboanga City, Zamboanga del Norte, Zamboanga del Sur, Zamboanga Sibugay
βͺοΈ VISAYAS: Bohol, Capiz, Cebu, Eastern Samar, Iloilo, Leyte, Negros Occidental, Negros Oriental, Northern Samar, Samar, Southern Leyte
βͺοΈ LUZON: Catanduanes, Isabela, Masbate, Nueva Vizcaya, Quirino, Sorsogon
π βMODERATE TO SEVERE
βͺοΈ MINDANAO: Camiguin, Dinagat Islands, Sulu
βͺοΈ VISAYAS: Aklan, Siquijor
βͺοΈ LUZON: Albay, Camarines Norte, Camarines Sur, Cagayan, Oriental Mindoro, Palawan, Quezon, Romblon, Marinduque
π‘βMINOR TO MILD
βͺοΈ MINDANAO: Tawi-Tawi
βͺοΈ VISAYAS: Guimaras, Biliran
βͺοΈ LUZON: Aurora, Apayao, Batangas, Kalinga, Mountain Province
βDROUGHT SEVERITY LEGEND EXPLANATION
ββͺοΈ Exceptional to Extreme (Red to Dark Red): Severe to critical subsoil moisture depletion. Crops face severe stress or total wilting, groundwater tables drop significantly, and river flows decrease drastically.
βͺοΈ Moderate to Severe (Orange to Dark Orange): Substantial moisture deficits in root zones, causing noticeable crop stress, reduced agricultural yields, and declining reservoir levels.
βͺοΈ Minor to Mild (Yellow to Light Orange): Early-stage moisture deficiency or dry conditions, serving as a warning sign of potential drought development if dry weather persists.
βWHY LOCAL RAIN DOES NOT MEAN DROUGHT IS OVER
ββͺοΈ Root-Zone Moisture Deficit: Drought intensity models calculate deep soil moisture levels (0β40 cm and 0β100 cm depths) where agricultural crops and aquifers draw water.
βͺοΈ Surface Wetting vs. Subsoil Saturation: Brief rain showers or localized thunderstorms only moisten the outermost layer of topsoil, which quickly evaporates in sunny weather without penetrating deep into the subsoil.
βͺοΈ Sustained Recovery Required: Overcoming deep hydrological drought requires consecutive weeks of consistent, soaking rainfall to fully recharge underground aquifers and restore root-zone water reserves.
βSOURCE: Windy.com / CzechGlobe (Drought Intensity Model)
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