The DOI matches its Crossref record; 49 of the 50 references it cites were found in a registry or an index.
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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“Drought is a major natural hazard determined by water availability being significantly below normal conditions for a region (Sheffield et al. 2012).”
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“Latest drought trend studies (Sheffield et al. 2012; Vicente-Serrano et al. 2014) and drought scenarios under possible climate change predictions (e.g., Cook et al. 2014) depend on indices that take into consideration evapotranspiration and precipitation such as the reconnaissance drought index…”
BackgroundMa, S., Zhou, T., Angélil, O., & Shiogama, H. (2017) · Journal of Climate · doi:10.1175/jcli-d-16-0636.1 · Cited by 54
“1 and MIROC5 simulations.”
InfluentialDehghan, S., Salehnia, N., Sayari, N., & Bakhtiari, B. (2020) · Journal of Arid Land · doi:10.1007/s40333-020-0095-5 · Cited by 54
Extreme weather events in Europe: preparing for climate change adaptation
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Modeling the response of soil moisture to climate variability in the Mediterranean region
Mimeau, L., Tramblay, Y., Brocca, L., Massari, C., Camici, S., & Finaud‐Guyot, P. (2021) · Hydrology and earth system sciences · doi:10.5194/hess-25-653-2021 · Cited by 53
Ortíz-Gómez, R., Flowers-Cano, R. S., & Medina-García, G. (2022) · Water Resources Management · doi:10.1007/s11269-022-03154-9 · Cited by 53
Simulated climatology and evolution of aridity in the 21st century
Lin, L., Gettelman, A., Feng, S., & Fu, Q. (2015) · Journal of Geophysical Research Atmospheres · doi:10.1002/2014jd022912 · Cited by 53
“Various methods were developed to estimate the PET, but the Penman-Monteith (PM) equation is regarded as the most reliable PET algorithm under all climatic conditions [Jensen et al., 1990; Donohue et al., 2010; Dai, 2011; Sheffield et al., 2012].”
MethodGanguly, A. R., Kodra, E., Agrawal, A., Banerjee, A., Boriah, S., Chatterjee, S., Chatterjee, S., Choudhary, A., Das, D., Faghmous, J. H., et al. (2014) · Nonlinear processes in geophysics · doi:10.5194/npg-21-777-2014 · Cited by 54
“Two recent papers on droughts, one published in Nature Climate Change (Dai, 2013) and another in Nature (Sheffield et al., 2012), offered diametrically opposite insights.”
BackgroundSmerdon, J. E., Cook, B. I., Cook, E. R., & Seager, R. (2015) · Journal of Climate · doi:10.1175/jcli-d-14-00417.1 · Cited by 53
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“There is longstanding and active debate in the literature about the strengths and weaknesses of different drought indices (e.g. VicenteSerrano et al., 2010; Sheffield et al., 2012; Joetzjer et al., 2013).”
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Fu, Q., Lin, L., Huang, J., Feng, S., & Gettelman, A. (2016) · Journal of Geophysical Research Atmospheres · doi:10.1002/2015jd024075 · Cited by 53
“We obtain PET using the Penman-Monteith algorithm [Shuttleworth, 1993; Allen et al., 1998], which is physically based and is superior to empirical formulations [Donohue et al., 2010; Dai, 2011; Sheffield et al., 2012].”
MethodAadhar, S., & Mishra, V. K. (2019) · Environmental Research Letters · doi:10.1088/1748-9326/ab4862 · Cited by 53
Landfalling Droughts: Global Tracking of Moisture Deficits From the Oceans Onto Land
Herrera-Estrada, J. E., & Diffenbaugh, N. S. (2020) · Water Resources Research · doi:10.1029/2019wr026877 · Cited by 53
“Still, the use of simple PET models in PDSI and SPEI can cause biased drought estimates (Sheffield et al., 2012).”
MethodEvidence for intensification of meteorological droughts in Oman over the past four decades
Kenawy, A. E., Buloshi, A. A., Al‐Awadhi, T., Nasiri, N. A., Navarro‐Serrano, F., Al-Hatrushi, S., Robaa, S. M., Domínguez‐Castro, F., McCabe, M. F., Schuwerack, P.-M., et al. (2020) · Atmospheric Research · doi:10.1016/j.atmosres.2020.105126 · Cited by 53
Identifying Causal Interactions Between Groundwater and Streamflow Using Convergent Cross‐Mapping
Bonotto, G., Peterson, T. J., Fowler, K., & Western, A. W. (2022) · Water Resources Research · doi:10.1029/2021wr030231 · Cited by 52
Tracking Interannual Streamflow Variability with Drought Indices in the U.S. Pacific Northwest
Abatzoglou, J. T., Barbero, R., Wolf, J. W., & Holden, Z. A. (2014) · Journal of Hydrometeorology · doi:10.1175/jhm-d-13-0167.1 · Cited by 53
“…drought indices that incorporate PET may yield divergent trajectories in a warming climate between temperature- and energybased estimates of PET (Donohue et al. 2010; Sheffield et al. 2012), further emphasizing the need to quantify the effectiveness of different flavors of a single drought index.”
BackgroundHistorical gridded reconstruction of potential evapotranspiration for the UK
Tanguy, M., Prudhomme, C., Smith, K., & Hannaford, J. (2018) · Earth system science data · doi:10.5194/essd-10-951-2018 · Cited by 52
“, 2009) or the Palmer Drought Severity Index (Palmer, 1965), different formulations of PET have a significant impact on the result (Beguería et al., 2013; Sheffield et al., 2012; Stagge et al., 2014).”
BackgroundPrăvălie, R., SÎRODOEV, I. G., Patriche, C. V., Roșca, B., Piticar, A., Bandoc, G., Sfîcă, L., Tişcovschi, A., Dumitrașcu, M., Chifiriuc, M. C., et al. (2019) · Agricultural Systems · doi:10.1016/j.agsy.2019.102767 · Cited by 52
Coastal defence techniques and climate change: a review
Foti, E., Musumeci, R. E., & Stagnitti, M. (2020) · RENDICONTI LINCEI · doi:10.1007/s12210-020-00877-y · Cited by 52
Jiang, R., Liang, J., Zhao, Y., Wang, H. E., Xie, J., Lu, X., & Li, F. (2021) · Scientific Reports · doi:10.1038/s41598-021-93328-z · Cited by 51
Sharifi, A., Mirabbasi, R., Nasr-Esfahani, M. A., Haghighi, A. T., & Nafchi, R. F. (2021) · Journal of Hydrology · doi:10.1016/j.jhydrol.2021.127045 · Cited by 51
Zhang, Y., Hao, Z., Zhang, X., & Hao, F. (2021) · Environmental Research Letters · doi:10.1088/1748-9326/ac43e0 · Cited by 52
“Following Sheffield et al (2012), we also mask out Greenland and desert regions (precipitation less than 0.5 mm d−1) without calculation of dry events (with approximately zero mean precipitation), since a percentile-based drought index is meaningless in these regions (Dunn et al 2020).”
MethodInfluentialDrought adaptive microbes as bioinoculants for the horticultural crops
Kour, D., Khan, S. S., Kaur, T., Kour, H., Singh, G., Yadav, A. N., & Yadav, A. N. (2022) · Heliyon · doi:10.1016/j.heliyon.2022.e09493 · Cited by 51
“Specifically, in the Tropics and Subtropics, drought has become more rampant and is anticipated to exacerbate its duration and severity (Sheffield et al., 2012).”
BackgroundSpatial patterns of European droughts under a moderate emission scenario
Spinoni, J., Naumann, G., & Vogt, J. (2015) · Advances in science and research · doi:10.5194/asr-12-179-2015 · Cited by 51
Zhao, X. H., Hong, W., Liang, S., Zhou, T., He, B., Tang, B., & Wu, D. (2015) · Remote Sensing · doi:10.3390/rs71014039 · Cited by 51
“Although PDSI is described as an index overestimating the magnitude of drought [49], and the average over the region may hide strong sub-regional anomalies, this evaluation is useful to highlight general relationships.”
BackgroundFifty years since Monteith's 1965 seminal paper: the emergence of global ecohydrology
Dolman, A. J., Miralles, D. G., & de Jeu, R. (2014) · Ecohydrology · doi:10.1002/eco.1505 · Cited by 51
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“…drought at global or continental scales for present and future climate (Andreadis et al. 2005; Sheffield and Wood 2008a, b; Shukla and Wood 2008; Sheffield et al. 2009, 2012; Dai 2011, 2013; Hannaford et al. 2013; Prudhomme et al. 2011; Stahl et al. 2011; Corzo Perez et al. 2011; Wehner et al.…”
BackgroundSpraggs, G., Oldham, L., Jones, P. D., & Ede, P. (2015) · Journal of Hydrology · doi:10.1016/j.jhydrol.2015.01.015 · Cited by 51
Variability of temperature extremes in the Yellow River basin during 1961–2011
Liang, K., Bai, P., Li, J., & Liu, C. (2014) · Quaternary International · doi:10.1016/j.quaint.2014.02.007 · Cited by 49
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“Drought has occurred in most places of the world, including wet and humid regions [5,6], and it is expected to increase in frequency and severity due to decreasing precipitation and increasing evapotranspiration driven by global warming [7–10].”
BackgroundRobust drying and wetting trends found in regions over China based on Köppen climate classifications
Chen, T., Zhang, H., Chen, X., Hagan, D. F. T., Wang, G., Gao, Z., & Shi, T. (2017) · Journal of Geophysical Research Atmospheres · doi:10.1002/2016jd026168 · Cited by 51
“For example, usually, PDSI using PMmethod tends to exhibit less drying trends than PDSI using THmethod under global warming due to their differences in temperature sensitivities [Dai, 2013; Sheffield et al., 2012; Zhang et al., 2016].”
BackgroundMethodInfluentialDominant variables of global air pollution-climate interaction: Geographic insight
Feng, H., Zou, B., Wang, J., & Gu, X. (2019) · Ecological Indicators · doi:10.1016/j.ecolind.2018.12.038 · Cited by 51
A 250‐Year European Drought Inventory Derived From Ensemble Hydrologic Modeling
Moravec, V., Markonis, Y., Rakovec, O., Kumar, R., & Hanel, M. (2019) · Geophysical Research Letters · doi:10.1029/2019gl082783 · Cited by 51
“…al., 2016), and the rest of the world (Kelley et al., 2015; van Dijk et al., 2013), have sparked debate about how changes in drought occurrence and characteristics are related to climatic variability (e.g., Hanel et al., 2018; Hisdal et al., 2001; Seneviratne et al., 2012; Sheffield et al., 2012).”
BackgroundKim, D., Lee, W., Kim, S. T., & Chun, J. A. (2019) · Water Resources Research · doi:10.1029/2019wr024991 · Cited by 51
“For instance, the controversy over global drought trends (Dai, 2013a; Sheffield et al., 2012; Trenberth et al., 2014) originated from the discrepancy in potential ET estimates.”
BackgroundA near‐term drought assessment using hydrological and climate forecasting in the Mekong River Basin
Kang, H., & Sridhar, V. (2020) · International Journal of Climatology · doi:10.1002/joc.6860 · Cited by 50
“Drought indices are commonly used for historical drought assessments (Sheffield et al., 2012), drought forecasting (Cancelliere et al.”
BackgroundClimate-induced salinization may lead to increased lake nitrogen retention
Jiang, X., Liu, C., Hu, Y., Shao, K., Tang, X., Zhang, L., Gao, G., & Qin, B. (2022) · Water Research · doi:10.1016/j.watres.2022.119354 · Cited by 50
Havens, K. E., & Steinman, A. D. (2013) · Environmental Management · doi:10.1007/s00267-013-0189-3 · Cited by 50
“the validity of this simple approach (e.g., Lofgren et al. 2011; Milly and Dunne 2011; Scheffield et al. 2012).”
MethodNorth American Pancontinental Droughts in Model Simulations of the Last Millennium*
Coats, S., Cook, B. I., Smerdon, J. E., & Seager, R. (2014) · Journal of Climate · doi:10.1175/jcli-d-14-00634.1 · Cited by 50
“There are multiple ways to compute PET, with the ideal method being Penman–Monteith (PM), which includes the effect of the vapor pressure deficit along with the impact of RNET (a more detailed treatment of PM PDSI can be found in Sheffield et al. 2012; Cook et al. 2014a; Smerdon et al. 2015).”
MethodGlobal meteorological drought – Part 1: Probabilistic monitoring
Dutra, E., Wetterhall, F., Giuseppe, F. D., Naumann, G., Barbosa, P., Vogt, J., Pozzi, W., & Pappenberger, F. (2014) · Hydrology and earth system sciences · doi:10.5194/hess-18-2657-2014 · Cited by 50
“Evapotranspiration can amplify drought events (Teuling et al., 2013), but care should be taken when using simple calculations of potential evapotranspiration (Sheffield et al., 2012).”
BackgroundYang, Q., Ma, Z., Zheng, Z., & Duan, Y. (2017) · Advances in Atmospheric Sciences · doi:10.1007/s00376-017-6313-1 · Cited by 50
Liu, M., Adam, J. C., Richey, A., Zhu, Z., & Myneni, R. B. (2018) · Journal of Hydrology · doi:10.1016/j.jhydrol.2018.07.068 · Cited by 51
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“…ΔET/P over China observed after considering that the reservoir water storage is consistent with the changes in the determining factors of ET [Douville et al., 2013; Jung et al., 2010; Lin et al., 2012; Miralles et al., 2014; Sheffield et al., 2012; Tang et al., 2011;Wang, 2014;Wang et al., 2012a].”
ResultThe use of range size to assess risks to biodiversity from stochastic threats
Murray, N., Keith, D. A., Bland, L. M., Nicholson, E., Regan, T. J., Rodrı́guez, J. P., & Bedward, M. (2017) · Diversity and Distributions · doi:10.1111/ddi.12533 · Cited by 56
“Spatially explicit stochastic threats such as extreme drought (Allen et al., 2010; Sheffield et al., 2012), disease outbreak (Fisher et al., 2012), coral bleaching (Hoegh-Guldberg et al., 2007), fires (Stephens et al., 2013; Nowacki & Abrams, 2015), invasion of alien species (Blackburn et al.,…”
BackgroundSimulated changes in aridity from the last glacial maximum to 4xCO 2
Greve, P., Roderick, M. L., & Seneviratne, S. I. (2017) · Environmental Research Letters · doi:10.1088/1748-9326/aa89a3 · Cited by 50
“Additionally, thegeneralized conclusionofmore arid conditions in a warmer world is challenged by large uncertainties underlying observed and projected aridity changes (Sheffield et al 2012, Greve et al 2014, Greve and Seneviratne 2015).”
BackgroundSelf-citationCarbon–water flux coupling under progressive drought
Boese, S., Jung, M., Carvalhais, N., Teuling, A. J., & Reichstein, M. (2019) · Biogeosciences · doi:10.5194/bg-16-2557-2019 · Cited by 50
“Climate change is expected to exacerbate existing water scarcities, with a particular increase 20 of drought events expected in Mediterranean regions (Hoerling et al., 2012; Sheffield et al., 2012).”
BackgroundDroughts in the area of Poland in recent centuries in the light of multi-proxy data
Przybylak, R., Oliński, P., Koprowski, M., Filipiak, J., Pospieszyńska, A., Chorążyczewski, W., Puchałka, R., & Dąbrowski, H. P. (2020) · Climate of the past · doi:10.5194/cp-16-627-2020 · Cited by 56
“For example, Sheffield et al. (2012) argue that overestimation of the rate of change of global droughts is related to the shortcomings (simplifications) of the Palmer Drought Severity Index (PDSI) used for this purpose.”
BackgroundLe, M., Kim, H., Moon, H., Zhang, R., Lakshmi, V., & Nguyen, L. B. (2020) · Journal of Hydrology Regional Studies · doi:10.1016/j.ejrh.2020.100767 · Cited by 49
Ansari, R., & Grossi, G. (2022) · Natural hazards and earth system sciences · doi:10.5194/nhess-22-287-2022 · Cited by 48
Drought risk and water resources assessment in the Beijing-Tianjin-Hebei region, China
Li, Q., Chen, L., & Xu, Y. (2022) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2022.154915 · Cited by 49
Variability and trends in global drought
McCabe, G. J., & Wolock, D. M. (2015) · Earth and Space Science · doi:10.1002/2015ea000100 · Cited by 48
Twidwell, D., Wonkka, C. L., Taylor, C. A., Zou, C. B., Twidwell, J. J., & Rogers, W. E. (2013) · Applied Vegetation Science · doi:10.1111/avsc.12044 · Cited by 48
“This PDSI method can overestimate changes in drought occurring over time because it uses a simplified model of evapotranspiration (Sheffield et al. 2012).”
MethodSpatiotemporal variability of four precipitation-based drought indices in Xinjiang, China
Li, Y., Yao, N., Şahin, S., & Appels, W. M. (2016) · Theoretical and Applied Climatology · doi:10.1007/s00704-016-1827-5 · Cited by 48
“Among them, there are an array of standardized indices that allow for drought characterization at different timescales, such as standardized precipitation index (SPI), standardized precipitation evapotranspiration index (SPEI), and standardized runoff index (SRI) (McKee et al. 1993; Shukla and Wood 2008; Beguería et a…”
BackgroundMethodXu, G., Liu, X., Trouet, V. M., Treydte, K. S., Wu, G., Chen, T., Sun, W., An, W., Wang, W., Zeng, X., et al. (2018) · Climate Dynamics · doi:10.1007/s00382-018-4215-2 · Cited by 48
“An enhanced understanding of drought variability is therefore crucial for sustainable development in arid regions (Sheffield et al. 2012).”
BackgroundQuintana‐Seguí, P., Barella-Ortiz, A., Sanfiz, S., & Miguez‐Macho, G. (2019) · Water Resources Management · doi:10.1007/s11269-018-2160-9 · Cited by 48
Benefits of Arbuscular Mycorrhizal Fungi Application to Crop Production under Water Scarcity
Posta, K., & Duc, N. H. (2019) · IntechOpen eBooks · doi:10.5772/intechopen.86595 · Cited by 48
“Nonetheless, ongoing climate change supposed to amplify the frequency and severity of drought in different regions of the globe [1] can wipe out the so far achievements.”
Future changes in Aridity Index at two and four degrees of global warming above preindustrial levels
Wang, X., Jiang, D., & Lang, X. (2020) · International Journal of Climatology · doi:10.1002/joc.6620 · Cited by 50
“Given that the above method tends to depict more severe drought (Dai, 2011; Sheffield et al., 2012), and that, in reality, PET not only responds to air temperature but also to the aerodynamic and radiative controls”
MethodInfluentialInvestigation of variable threshold level approaches for hydrological drought identificationPreprint
Beyene, B. S., Loon, A. F. V., Lanen, H. A. J. V., & Torfs, P. J. J. F. (2014) · doi:10.5194/hessd-11-12765-2014 · Cited by 48
The relationship between drought activity and vegetation cover in Northwest China from 1982 to 2013
Jiang, Y., Wang, R., Qing, P., Wu, X., Ning, H., & Li, C. (2018) · Natural Hazards · doi:10.1007/s11069-018-3282-3 · Cited by 47
“…researchers have claimed that there is little difference between SPEI and PDSI whether using Penman–Monteith algorithms or Thornthwaite algorithms (Sheffield et al. 2012), but the Penman–Monteith method is more accurate because more meteorological data are involved, and more factors are…”
MethodQuantifying Flash Droughts Over China From 1980 to 2017
Fu, K., & Wang, K. (2022) · Journal of Geophysical Research Atmospheres · doi:10.1029/2022jd037152 · Cited by 47
“The Palmer drought severity index (PDSI) and standardized precipitation index (SPI) are the indices most commonly used to quantify traditional droughts (Dai, 2013; Feng et al., 2011, 2008; Palmer, 1965; Sheffield et al., 2012; S. Yuan & Quiring, 2014).”
Yang, P., Zhai, X., Huang, H., Zhang, Y., Zhu, Y., Shi, X., Zhou, L., & Fu, C. (2023) · Atmospheric Research · doi:10.1016/j.atmosres.2023.106753 · Cited by 47
Characterizing present and future drought changes over eastern China
Chen, H., & Sun, J. (2017) · International Journal of Climatology · doi:10.1002/joc.4987 · Cited by 47
Increasing drought has been observed by SPEI_pm in Southwest China during 1962–2012
Wang, Z., Li, J., Lai, C., Huang, Z., Zhong, R., Zeng, Z., & Chen, X. (2017) · Theoretical and Applied Climatology · doi:10.1007/s00704-017-2152-3 · Cited by 47
“To address these problems, Beguería et al. (2014) recommended use of a more robust Penman–Monteith (PM) equation to compute the reference ET (ET0), shown to be a more accurate and comprehensive approach (Sheffield et al. 2012).”
BackgroundMethodProgress in understanding drought tolerance: from alleles to cropping systems
Varshney, R. K., Tuberosa, R., & Tardieu, F. (2018) · Journal of Experimental Botany · doi:10.1093/jxb/ery187 · Cited by 47
“Although it is uncertain whether episodes of drought will be more severe with climate change (Sheffield et al., 2012), their prevalence and year-to-year variability are major features in future modelling scenarios (Sun et al.”
BackgroundDaily SPEI Reveals Long-term Change in Drought Characteristics in Southwest China
Jia, Y., Zhang, B., & Ma, B. (2018) · Chinese Geographical Science · doi:10.1007/s11769-018-0973-3 · Cited by 47
Impacts of potential evapotranspiration on drought phenomena in different regions and climate zones
Um, M., Kim, Y., Park, D., Jung, K., Wang, Z., Kim, M. M., & Shin, H. (2019) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2019.135590 · Cited by 47
Kyatengerwa, C., Kim, D., & Choi, M. (2019) · Journal of Hydrology · doi:10.1016/j.jhydrol.2019.124348 · Cited by 48
Shi, L., Feng, P., Wang, B., Liu, D. L., & Yu, Q. (2020) · Journal of Hydrology · doi:10.1016/j.jhydrol.2020.125394 · Cited by 47
“Moreover, this equation leads to an overestimation of ETp with increasing air temperature and might not be suitable for climate change studies (Sheffield et al., 2012).”
BackgroundMethodZhao, X., Xia, H., Liu, B., & Jiao, W. (2022) · Remote Sensing · doi:10.3390/rs14071570 · Cited by 47
Drought over Southeast Asia and Its Association with Large-Scale Drivers
Phan‐Van, T., Nguyen, P. N. B., Ngo‐Duc, T., Vu‐Minh, T., Le, P. V. V., Trinh‐Tuan, L., Nguyen‐Thi, T., Pham‐Thanh, H., & Tran-Quang, D. (2022) · Journal of Climate · doi:10.1175/jcli-d-21-0770.1 · Cited by 46
Kang, Y., Guo, E., Wang, Y., Bao, Y., Bao, Y., Mandula, N., Runa, A., Gu, X., & Jin, L. (2022) · Journal of Hydrology · doi:10.1016/j.jhydrol.2022.128296 · Cited by 48
Zhang, F., Cui, N., Guo, S., Yue, Q., Jiang, S., Zhu, B., & Yu, X. (2023) · Agricultural Water Management · doi:10.1016/j.agwat.2023.108293 · Cited by 46
Methodological differences in projected potential evapotranspiration
McAfee, S. A. (2013) · Climatic Change · doi:10.1007/s10584-013-0864-7 · Cited by 47
Quej, V. H., Almorox, J., Arnaldo, J. A., & Moratiel, R. (2018) · Journal of Hydrologic Engineering · doi:10.1061/(asce)he.1943-5584.0001747 · Cited by 46
Lin, L., Gettelman, A., Xu, Y., Wu, C., Wang, Z., Rosenbloom, N. A., Bates, S. C., & Dong, W. (2019) · Geoscientific model development · doi:10.5194/gmd-12-3773-2019 · Cited by 46
“Note,30 5 however, that rainfall in the reanalysis products such as JRA55 and MERRA2 is dependent on the reanalysis model physics, and it is well-known that there is large uncertainty among various observational datasets [Sheffield et al., 2012; Trenberth et al., 2014].”
BackgroundProjected Drought Conditions over Southern Slope of the Central Himalaya Using CMIP6 Models
Sharma, S., Hamal, K., Khadka, N., Ali, M., Subedi, M., Hussain, G., Ehsan, M. A., Saeed, S., & Dawadi, B. (2021) · Earth Systems and Environment · doi:10.1007/s41748-021-00254-1 · Cited by 46
Projected Meteorological Drought over Asian Drylands under Different CMIP6 Scenarios
Li, H., Li, Z., Chen, Y., Liu, Y., Hu, Y., Sun, F., & Kayumba, P. M. (2021) · Remote Sensing · doi:10.3390/rs13214409 · Cited by 45
“This formulation incorporates the effects of thermal and dynamic factors such as temperature, solar and infrared radiation, humidity, and wind speed variations on evapotranspiration [4,37].”
BackgroundMethodDeng, S., Liu, S., & Mo, X. (2021) · Journal of Hydrology · doi:10.1016/j.jhydrol.2021.127170 · Cited by 45
Persistent humid climate favored the Qin and Western Han Dynasties in China around 2,200 y ago
Qin, C., Yang, B. J., Bräuning, A., Ljungqvist, F. C., Osborn, T. J., Валерьевич, Ш. В., He, M., Kang, S., Schneider, L., Esper, J., et al. (2024) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.2415294121 · Cited by 47
Severity, duration and frequency of drought in SE England from 1697 to 2011
Todd, B., Macdonald, N., Chiverrell, R. C., Caminade, C., & Hooke, J. M. (2013) · Climatic Change · doi:10.1007/s10584-013-0970-6 · Cited by 45
Changes in the frequency and severity of hydrological droughts over Ethiopia from 1960 to 2013
Kenawy, A. E., McCabe, M. F., Vicente-Serrano, S. M., López‐Moreno, J. I., & Robaa, S. M. (2016) · Cuadernos de Investigación Geográfica · doi:10.18172/cig.2931 · Cited by 45
“Although Sheffield et al. (2012) have suggested little change in the global drought over the past 60 years, other research has also highlighted the potential implications of future climate changes on drought frequency and severity (Sheffield and Wood, 2008; Dai, 2011), with changes likely to…”
BackgroundSpatial and temporal patterns of drought in the Continental U.S. during the past century
Ge, Y., Apurv, T., & Cai, X. (2016) · Geophysical Research Letters · doi:10.1002/2016gl069660 · Cited by 50
“…(which has been found to bemore physically realistic and based on more diverse input data than the Thornthwaite equation) [Dai, 2013; Sheffield et al., 2012]; (b) the data sets use self-calibration method for PDSI calculation [Wells et al., 2004], in which PDSI is calibrated using…”
MethodZhao, G., Gao, H., Kao, S., Voisin, N., & Naz, B. S. (2018) · Journal of Hydrology · doi:10.1016/j.jhydrol.2018.05.037 · Cited by 45
Economy-wide impact of drought induced productivity losses
Kilimani, N., Heerden, J. H. V., Bohlmann, H. R., & Roos, L. (2018) · Disaster Prevention and Management An International Journal · doi:10.1108/dpm-05-2018-0155 · Cited by 45
Impact of climate model resolution on soil moisture projections in central-western Europe
van der Linden, E. C., Haarsma, R., & van der Schrier, G. (2019) · Hydrology and earth system sciences · doi:10.5194/hess-23-191-2019 · Cited by 45
Zhang, A., Jia, G., & Wang, H. (2019) · Environmental Research Letters · doi:10.1088/1748-9326/ab005e · Cited by 45
“Ensemble usage of multi-source data has been widely adopted to reduce uncertainty in climate studies (Sheffield et al 2012, Reddington et al 2017).”
Jiang, D., Li, Z., Luo, Y., & Xia, Y. (2020) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2020.143682 · Cited by 45
Neto, A. A. M., Niu, G., Roy, T., Tyler, S. W., & Troch, P. A. (2020) · Communications Earth & Environment · doi:10.1038/s43247-020-00056-9 · Cited by 45
Rahman, K. U., Shang, S., & Zohaib, M. (2021) · Remote Sensing · doi:10.3390/rs13091662 · Cited by 45
“Therefore, the insufficiency of RGs for monitoring droughts has been addressed in a number of studies [20,29,30], which is emphasizing on application and development of continuous precipitation datasets for drought assessment [19].”
BackgroundPrediction of Reservoir Storage Anomalies in India
Tiwari, A. D., & Mishra, V. K. (2019) · Journal of Geophysical Research Atmospheres · doi:10.1029/2019jd030525 · Cited by 44
“Since PET estimations can have uncertainty (Sheffield et al., 2012), we compared PET estimates for a few locations and found that the Hargreaves method provides similar estimates that are obtained from the Penman‐Monteith method.”
MethodTemporal Scaling of Streamflow Elasticity to Precipitation: A Global Analysis
Zhang, Y., Viglione, A., & Blöschl, G. (2022) · Water Resources Research · doi:10.1029/2021wr030601 · Cited by 50
Babaousmail, H., Ayugi, B. O., Rajasekar, A., Zhu, H., Oduro, C., Mumo, R., & Ongoma, V. (2022) · Atmosphere · doi:10.3390/atmos13050741 · Cited by 44
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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