Hysteresis and irreversibility of global drought patterns in response to CO 2 mitigation efforts
Bibliographic Data
| ID | 15550719 |
|---|---|
| Authors | Sanjit Kumar Mondal (0000-0002-2118-6858, Chinese Academy of Sciences, corresponding author), Soon‐Il An (0000-0002-0003-429X, Pohang University of Science and Technology), Seung‐Ki Min (0000-0002-6749-010X, Pohang University of Science and Technology), Tong Jiang (0009-0003-3536-5309, Nanjing University), Buda Su (0000-0003-0510-4397, Nanjing University), Seungmok Paik (0000-0003-3655-4227, Seoul National University), Soong‐Ki Kim (0000-0001-6586-780X, Planetary Science Institute) |
| Year | 2025 |
| Volume | 20 |
| Issue | 8 |
| Pages | 084047-084047 |
| Publication date | 2025-06-19 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Environmental Research Letters (JOURNAL) |
| Journal identifiers | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Publisher | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/ade608 |
| OpenAlex | W4411443372 |
| Language | EN |
| References cited | 59 |
Drought is expected to intensify with rising CO 2 , but its behavior under CO 2 mitigation, remains uncertain. The response of the climate system to CO 2 variation exhibits hysteresis and irreversibility, highlighting the difficulty of recovery and the potential for long-lasting impacts. We investigated the hysteresis and reversibility of global drought and the associated underlying drivers. The Community Earth System Model 2 was used to simulate CO 2 changes: linear increases, decreases (i.e. net negative), and restoration to the initial level. This paper incorporates three well-established indices based on atmospheric, meteorological and soil moisture data to reflect drought. Here, we show that drought is dominant during the CO 2 decrease phase, leading to strong hysteresis with irreversible behavior over more than half of the global land cover. The robust irreversible changes in drought are concentrated in specific areas, i.e. hotspots, covering over 11% of the global land and are particularly pronounced in Northern Africa, Southwest Russia, and Central America. A decrease in precipitation drives drought during the CO 2 increase phase, while an enhanced vapor pressure deficit (VPD) exacerbates it during the CO 2 decrease phase. This increased VPD exacerbates drought hysteresis by raising potential evapotranspiration. Our findings suggest that only CO 2 reduction is not enough to effectively mitigate drought impacts, rather advanced water management strategies are essential
Atmospheric sciences · Biology · Climate change · Climatology · Evapotranspiration · Geography · Hysteresis · Land cover · Land use · Meteorology · Precipitation · Water content · Atmospheric and Environmental Gas Dynamics · Climate variability and models · Environmental Science · Hydrology and Drought Analysis · Ecology · Geology
Early-warning signals for critical transitions
Tipping elements in the Earth's climate system
Little change in global drought over the past 60 years
The Community Earth System Model Version 2 (Cesm2)
A Multiscalar Drought Index Sensitive to Global Warming
Summary for Policymakers
Hysteresis of the Earth system under positive and negative CO 2 emissions
On the proportionality between global temperature change and cumulative CO 2 emissions during periods of net negative CO 2 emissions
Reversibility in an Earth System model in response to CO 2 concentration changes
| Citation velocity | historical |
|---|---|
| Highly cited | No |