Probabilistic quantification of global drought risk amplification from temperature-enhanced evapotranspiration under climate change
Akinwale T. Ogunrinde , Paul Adigun , Xian Xue , Koji Dairaku , Sabab Ali Shah , Ifeoluwa S. Adawa
Geoscience Frontiers ›› 2026, Vol. 17 ›› Issue (2) : 102235
Droughts pose escalating threats to global water security, agriculture, and socioeconomic stability amid anthropogenic climate change, with projections indicating an increase in frequency, duration, and severity driven by altered precipitation patterns and amplified evaporative demand. This study introduces a probabilistic framework to quantify drought risk amplification, employing the Risk Ratio (RR) methodology integrated with extreme value theory and non-parametric inference. Utilizing multi-model ensemble (MME) from the Coupled Model Intercomparison Project Phase 6 (CMIP6) under Shared Socioeconomic Pathways (SSP2-4.5 and SSP5-8.5), we evaluate changes in drought characteristics—duration, frequency, and severity — via the Standardized Precipitation Evapotranspiration Index (SPEI) at 3- and 12-month timescales for near-future (NF) and far-future (FF) periods. Our analyses reveal pervasive global intensification, with over 90% of land grids exhibiting positive severity shifts under SSP5-8.5 in the FF, attributed to atmospheric evaporative demand, which accounts for approximately 44% of the trends in SPEI. Threshold-stratified RR assessments reveal nonlinear escalations at higher percentiles (P90 vs. P75), compressing the return periods of extreme events by 20%-30% under high-emission scenarios. Regional hotspots, including the Amazon basin, sub-Saharan Africa, southwestern North America, and Central Asian drylands, exhibit frequency risks that are 4-fold or more amplified, signaling transitions to chronic water stress and potential ecosystem tipping points. These findings underscore the dominance of thermodynamic drivers in drought dynamics, advocating for emissions mitigation to curtail risks by 15%-25% under moderate pathways. By addressing uncertainties in non-stationary regimes, this framework provides adaptive strategies for resilient water management, offering policymakers critical insights to mitigate cascading impacts on global food security and biodiversity in a warming world.
Drought risk amplification / Climate change projections / CMIP6 models / Standardized Precipitation Evapotranspiration Index (SPEI) / Risk Ratio methodology / Atmospheric evaporative demand
| [1] |
|
| [2] |
|
| [3] |
ASCE, 2005. The ASCE Standardized Reference Evapotranspiration Equation. ASCE, Reston, VA, pp. 59. https://doi.org/10.1061/9780784408056. |
| [4] |
|
| [5] |
|
| [6] |
|
| [7] |
|
| [8] |
|
| [9] |
|
| [10] |
|
| [11] |
|
| [12] |
|
| [13] |
|
| [14] |
|
| [15] |
|
| [16] |
|
| [17] |
|
| [18] |
|
| [19] |
Geneva Environment Network, 2025. Desertification, Land Degradation and Drought, and the Role of Geneva. |
| [20] |
|
| [21] |
|
| [22] |
|
| [23] |
|
| [24] |
IPCC, 2021. Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge Univ. Press, Cambridge, United Kingdom and New York, NY, USA, 2392 pp. https://doi.org/10.1017/9781009157896. |
| [25] |
IPCC, 2022. Climate Change 2022: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. https://www.ipcc.ch/report/ar6/wg2/ (accessed 2 November 2025). |
| [26] |
|
| [27] |
|
| [28] |
|
| [29] |
|
| [30] |
|
| [31] |
|
| [32] |
|
| [33] |
|
| [34] |
|
| [35] |
|
| [36] |
|
| [37] |
|
| [38] |
|
| [39] |
|
| [40] |
|
| [41] |
|
| [42] |
|
| [43] |
|
| [44] |
|
| [45] |
|
| [46] |
|
| [47] |
|
| [48] |
|
| [49] |
|
| [50] |
|
| [51] |
|
| [52] |
|
| [53] |
|
| [54] |
|
| [55] |
|
| [56] |
|
| [57] |
|
| [58] |
|
| [59] |
|
| [60] |
|
| [61] |
|
| [62] |
|
| [63] |
|
| [64] |
UNCCD, 2022. Drought in Numbers 2022: Restoration for readiness and resilience. Bonn: United Nations Convention to Combat Desertification. November 2025). |
| [65] |
|
| [66] |
|
| [67] |
|
| [68] |
|
| [69] |
|
| [70] |
|
| [71] |
|
| [72] |
WMO, 2017. WMO guidelines on the calculation of climate normals. WMO-No. 1203. Geneva: World Meteorological Organization. November 2025). |
| [73] |
WMO,2021. WMO atlas of mortality and economic losses from weather, climate and water extremes (1970-2019). WMO-No. 1267. Geneva: World Meteorological Organization. November 2025). |
| [74] |
World Weather Attribution, 2024. Climate change, not El Niño, main driver of exceptional drought in highly vulnerable Amazon River Basin. World Weather Attribution. November 2025). |
| [75] |
|
| [76] |
|
| [77] |
|
| [78] |
|
| [79] |
|
| [80] |
|
| [81] |
|
| [82] |
|
| [83] |
|
/
| 〈 |
|
〉 |