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Little change in global drought over the past 60 years
Abstract
Drought is expected to increase in frequency and severity in the future as a result of climate change, mainly as a consequence of decreases in regional precipitation but also because of increasing evaporation driven by global warming. Previous assessments of historic changes in drought over the late twentieth and early twenty-first centuries indicate that this may already be happening globally. In particular, calculations of the Palmer Drought Severity Index (PDSI) show a decrease in moisture globally since the 1970s with a commensurate increase in the area in drought that is attributed, in part, to global warming. The simplicity of the PDSI, which is calculated from a simple water-balance model forced by monthly precipitation and temperature data, makes it an attractive tool in large-scale drought assessments, but may give biased results in the context of climate change. Here we show that the previously reported increase in global drought is overestimated because the PDSI uses a simplified model of potential evaporation that responds only to changes in temperature and thus responds incorrectly to global warming in recent decades. More realistic calculations, based on the underlying physical principles that take into account changes in available energy, humidity and wind speed, suggest that there has been little change in drought over the past 60 years. The results have implications for how we interpret the impact of global warming on the hydrological cycle and its extremes, and may help to explain why palaeoclimate drought reconstructions based on tree-ring data diverge from the PDSI-based drought record in recent years.
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“Two recent studies published in Nature Climate Change 25 and Nature 26 came to opposing conclusions about whether there are noticeable changes in drought trends as a result of climate change.”
From A Big Data Guide to Understanding Climate Change: The Case for Theory-Guided Data Science (2014) · cites this paper as [26]
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“This point has been verified by recent studies (Sheffield et al., 2012; Li et al., 2014).”
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“The use of different drought proxies for the ranking of drought events is problematic because the chosen proxies (e.g., precipitation, evapotranspiration), together with the time scale, strongly affect the ranking (Vidal et al. 2010; Sheffield et al. 2012).”
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Multi-criterion model ensemble of CMIP5 surface air temperature over China
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Legacies of La Niña: North American monsoon can rescue trees from winter drought
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“…main criticism of the SPI is that its calculation is based only on precipitation data knowing that other relevant variables as temperature, evapotranspiration, solar radiation or wind speed among others can have an important role when a drought event is developing (Dai 2012, Sheffield et al. 2012).”
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“Essentially, temperature-based methods perform well because T is correlated with radiation and humidity at monthly timescale (Sheffield et al., 2012).”
BackgroundMethodEarly warning information, farmers’ perceptions of, and adaptations to drought in China
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“Among the several types of extreme weather events driven by climate change, drought has become a worldwide concern (Sheffield et al. 2012).”
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“From a viewpoint of global scale, Sheffield et al. (2012) has suggested little changes of drought in the past decades using the Penman–Monteith method.”
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Kumar, A., Kumar, S., Rautela, K. S., Shekhar, S., Ray, T., & Thangavel, M. (2023) · Journal of Water and Climate Change · doi:10.2166/wcc.2023.280 · Cited by 39
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“The TW equation may not be the best approach to estimate PET in drought monitoring because it is overly dependent on T (Sheffield et al., 2012), and previous studies have shown that T is not the only factor that influences PET (or even the most important factor) (Roderick & Farquhar, 2002).”
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“The former provides a better estimate due to its more comprehensive physics [4,14] but it is data intensive and requires more input data that are not usually readily available.”
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“However, Sheffield et al. (2012) also recognized their limitations of lack of observations for validation, and thus, the results need to be verified by other independent analyses.”
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“Regional environmental change is often slow, with ecosystem changes in biotic and abiotic conditions unfolding over decades, centuries or millennia (Renberg et al., 1993; Sheffield et al., 2012).”
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Sensitivity of discharge projections to potential evapotranspiration estimation in Northern Tunisia
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“Several studies show that the impacts of climate change on discharge depend on the PET formula used (Seiller and Anctil 2016; Bae et al. 2011; SpernaWeiland et al. 2012).”
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“There are also notable uncertainties in soil moisture trends during historical periods based on both model simulations and observations (Dai, 2013; Sheffield et al., 2012).”
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Crescimento e produtividade de cultivares e linhagens de amendoim submetidas a déficit hídrico
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An overview of US state drought plans: crisis or risk management?
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“Sheffield et al. (2012) argue that this expected increased intensity of drought is overestimated because of those advocates’ simplified method of projection.”
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“Recently, contrasting conclusions were drawn about global drought climatology (Sheffield et al. 2012; Dai 2013).”
Evaluation of CMIP5 Global Climate Models over the Volta Basin: Precipitation
Agyekum, J., Annor, T., Lamptey, B., Quansah, E., & Agyeman, R. Y. K. (2018) · Advances in Meteorology · doi:10.1155/2018/4853681 · Cited by 36
“A decrease in the amount of precipitation may lead to drought [3, 4], while an increase can cause flooding [5].”
BackgroundSpatio-temporal variations in extreme drought in China during 1961–2015
Zhang, J., & Shen, Y. (2019) · Journal of Geographical Sciences · doi:10.1007/s11442-019-1584-3 · Cited by 37
Intensification of historical drought over China based on a multi‐model drought index
Han, X., Wu, J., Zhou, H., Liu, L., Yang, J., Shen, Q., & Wu, J. (2020) · International Journal of Climatology · doi:10.1002/joc.6527 · Cited by 37
Pettit, J. M., Voelker, S. L., DeRose, R. J., & Burton, J. I. (2020) · Global Change Biology · doi:10.1111/gcb.15274 · Cited by 37
Song, Y., Tian, J., Linderholm, H. W., Wang, C., Ou, Z., & Chen, D. (2020) · International Journal of Climatology · doi:10.1002/joc.6885 · Cited by 37
“Several studies have examined changes to drought and the degree to which these are driven by global warming (Dai, 1998; Ma et al., 2004; Sheffield and Wood, 2008; Qian, 2011; Wang et al., 2011; Sheffield et al., 2012; Dai, 2013; Trenberth et al., 2014; Dai and Zhao, 2016).”
BackgroundRobust historical evapotranspiration trends across climate regimes
Hobeichi, S., Abramowitz, G., & Evans, J. P. (2021) · Hydrology and earth system sciences · doi:10.5194/hess-25-3855-2021 · Cited by 37
Indicators of climate change impacts on the water cycle and water management
Peters‐Lidard, C. D., Rose, K. C., Kiang, J. E., Strobel, M. L., Anderson, M. L., Byrd, A. R., Kolian, M. J., Brekke, L. D., & Arndt, D. S. (2021) · Climatic Change · doi:10.1007/s10584-021-03057-5 · Cited by 37
“Although the PDSI was a landmark in the development of drought indices, it is not without limitations (Heim Jr. 2002; Sheffield et al. 2012).”
BackgroundMyronidis, D., & Theofanous, N. (2021) · Stochastic Environmental Research and Risk Assessment · doi:10.1007/s00477-021-02015-y · Cited by 37
Reducing Climate Change Induced Flood at the Cost of Hydropower in the Lancang‐Mekong River Basin
Yun, X., Tang, Q., Sun, S., & Wang, J. (2021) · Geophysical Research Letters · doi:10.1029/2021gl094243 · Cited by 37
Zona, D., Lipson, D. A., Richards, J. H., Phoenix, G. K., Liljedahl, A., Ueyama, M., Sturtevant, C., & Oechel, W. C. (2014) · Biogeosciences · doi:10.5194/bg-11-5877-2014 · Cited by 39
“Large parts of Alaska and Canada have been subjected to a substantial drying over the last 50 years (as shown by the increase in the Palmer Drought Severity Index using the Penman–Monteith equation, PDSI-PM, Sheffield et al., 2012).”
BackgroundMethodInter-annual and spatial variability of Hamon potential evapotranspiration model coefficients
McCabe, G. J., Hay, L. E., Bock, A., Markstrom, S. L., & Atkinson, R. D. (2014) · Journal of Hydrology · doi:10.1016/j.jhydrol.2014.12.006 · Cited by 36
“This is an interesting result given that several previous studies have argued that temperature-based PET models such as the Hamon model over-estimate PET (Milly and Dunne, 2011; Sheffield et al., 2012).”
BackgroundResultSawada, Y., Koike, T., & Jaranilla‐Sanchez, P. A. (2014) · Water Resources Research · doi:10.1002/2013wr014847 · Cited by 36
Methodological Approaches to Projecting the Hydrologic Impacts of Climate Change*
Lofgren, B. M., Gronewold, A. D., Acciaioli, A., Cherry, J., Steiner, A. L., & Watkins, D. (2013) · Earth Interactions · doi:10.1175/2013ei000532.1 · Cited by 36
Dissecting indices of aridity for assessing the impacts of global climate change
Girvetz, E. H., & Zganjar, C. (2014) · Climatic Change · doi:10.1007/s10584-014-1218-9 · Cited by 36
“There is evidence showing that the modified Thornthwaite equation could overestimate the increase in PET due to climate change, whereas the Hargreaves method provides a fairly unbiased assessment of climate change when compared to the Penman-Monteith method (Burke and Brown, 2008; Kingston et al., 2009; Sheffield et a…”
A New Time-varying Concept of Risk in a Changing Climate
Sarhadi, A., Ausín, M. C., & Wiper, M. P. (2016) · Scientific Reports · doi:10.1038/srep35755 · Cited by 36
Atmospheric dynamics drive most interannual U.S. droughts over the last millennium
Erb, M. P., Emile‐Geay, J., Hakim, G. J., Steiger, N., & Steig, E. J. (2020) · Science Advances · doi:10.1126/sciadv.aay7268 · Cited by 36
“For the LMR, PDSI is calculated in the model prior using the PenmanMonteith method for estimating the potential evapotranspiration component (31) and then reconstructed in the past through data assimilation alongside other climate variables (Materials and Methods).”
Evaluation of evapotranspiration deficit index for agricultural drought monitoring in North China
Wu, R., Liu, Y., & Xing, X. (2021) · Journal of Hydrology · doi:10.1016/j.jhydrol.2021.126057 · Cited by 36
Spatial and temporal drought projections of northwestern Turkey
Yeşilköy, S., & Şaylan, L. (2022) · Theoretical and Applied Climatology · doi:10.1007/s00704-022-04029-0 · Cited by 36
The Combined Impacts of ENSO and IOD on Global Seasonal Droughts
Yin, H., Wu, Z., Fowler, H. J., Blenkinsop, S., He, H., & Li, Y. (2022) · Atmosphere · doi:10.3390/atmos13101673 · Cited by 36
Spatiotemporal drought variability of the eastern Tibetan Plateau during the last millennium
Deng, Y., Gou, X., Gao, L., Yang, M., & Zhang, F. (2016) · Climate Dynamics · doi:10.1007/s00382-016-3433-8 · Cited by 36
“Besides, it has used the Thornthwaite equation to compute potential evapotranspiration, which may have overestimated the drought severity in the context of global warming (Sheffield et al. 2012).”
Method
Metadata
- Authors
- Sheffield, J., Wood, E. F., & Roderick, M. L.
- Affiliations
- Princeton University (US)
- Australian National University (AU)
- Corresponding author
- Sheffield, Justin
- Venue
- Nature
- Published
- 2012-11
- Volume
- 491
- Issue
- 7424
- Pages
- 435-438
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W2015522309
- Cited by
- 1,978
- References
- 50
- Citations by year
- 2026: 97 · 2025: 126 · 2024: 131 · 2023: 162 · 2022: 188 · 2021: 196 · 2020: 174 · 2019: 159 · 2018: 160 · 2017: 139 · 2016: 144 · 2015: 121 · 2014: 110 · 2013: 66 · 2012: 3
- FWCI
- 79.51
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Nature (publishedVersion)
- PubMed (publishedVersion)
- RePEc: Research Papers in Economics (submittedVersion)
- ePrints Soton (University of Southampton) (submittedVersion)
- ANU Open Research (Australian National University) (submittedVersion)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Hydrology and Drought Analysis
- Physical Sciences › Environmental Science › Global and Planetary Change › Plant Water Relations and Carbon Dynamics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Keywords
- global drought, Palmer Drought Severity Index, drought trends, potential evaporation, global warming, water cycle, drought indices, climate change impacts, water balance modeling
- MeSH terms
- Models, Theoretical, Temperature, Time Factors, Droughts, Global Warming
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