Preprints
https://doi.org/10.5194/egusphere-2025-1247
https://doi.org/10.5194/egusphere-2025-1247
25 Mar 2025
 | 25 Mar 2025
Status: this preprint is open for discussion and under review for Earth System Dynamics (ESD).

Storylines of Future Drought in the Face of Uncertain Rainfall Projections: a New Zealand Case Study

Hamish Lewis, Luke J. Harrington, Peter B. Gibson, and Neelesh Rampal

Abstract. Robust increases in temperatures will occur globally across the twenty-first century; however, for some regions, sign changes in rainfall remain uncertain. Navigating this uncertainty is crucial in addressing drought-related challenges faced by climate-exposed sectors. New Zealand represents these challenges, exhibiting significant model uncertainty in warm-season rainfall change. Here, we examine how temperature-driven increases in potential evapotranspiration interact with contrasting storylines of future rainfall to explore drought outcomes for New Zealand. In our drying storyline, we find that increasing temperatures accompanied by less rainfall bring forward the onset of drought several months and delay its termination. In the wetting storyline, increases in rainfall partly offset the temperature-induced drying effect, leading to minor reductions in soil moisture. Examining extreme years, the average hydrological year in the future becomes comparable to the driest years of the current climate, while the worst future events exhibit unprecedented drought severity.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
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Hamish Lewis, Luke J. Harrington, Peter B. Gibson, and Neelesh Rampal

Status: open (until 17 May 2025)

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Hamish Lewis, Luke J. Harrington, Peter B. Gibson, and Neelesh Rampal
Hamish Lewis, Luke J. Harrington, Peter B. Gibson, and Neelesh Rampal

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Short summary
Global temperatures will continue to increase over twenty-first century; in contrast to rainfall, where the sign of change is unknown in some regions, such as New Zealand. These uncertain rainfall projections have great implications for future drought. In a wetter future, the increases in rainfall offset some of the temperature induced drying, leading to a small increase in drought severity. In a drier future the reduction in rainfall exacerbates the drying due to increasing temperatures.
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