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Dryland changes under different levels of global warming
Abstract
Drylands are vital ecosystems which cover almost 47% of the Earth's surface, hosting 39% of the global population. Dryland areas are highly sensitive to climatic changes and substantial impacts are foreseen under a warming climate. Many studies have examined the evolution of drylands in the future highlighting the need for improved capability of climate models to simulate aridity. The present study takes advantage of new higher resolution climate projections by the HadGEM3A Atmosphere Global Climate Model using prescribed time varying SSTs and sea ice, provided by a range of CMIP5 climate models under RCP8.5. The aim of the higher resolution models is to examine the benefit of the improved representation of atmospheric processes in the dryland research and to see where these results lie in the range of results from previous studies using the original CMIP5 ensemble. The transient response of aridity from the recent past until the end of the 21st century was examined as well as the expansion of global drylands under specific levels of global warming (1.5 °C, 2 °C and 4 °C). Dryland changes were further assessed at the watershed level for a number of major global river basins to discuss implications on hydrological changes and land degradation. The areal coverage of drylands could increase by an additional 7% of the global land surface by 2100 under high end climate change. At a 4 °C warmer world above pre-industrial, 11.2% of global land area is projected to shift towards drie…
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“30% of the approximately 46% (±0.8%) of the global land area defined as drylands are grassy ecosystems (22)(23)(24).”
From Restoring Degraded Lands (2021) · cites this paper as [22]
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“Under the background of global warming (Williams et al., 2020), the dryland area will continue to expand (Feng & Fu, 2013; Lickley & Solomon, 2018), from 40% (Huang et al., 2016) of the global terrestrial ecosystem currently to 47% by the end of the 21st century (Koutroulis, 2019).”
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“5 concentration scenario, 2% of the global land area is projected to shift towards drier types and 4.24% to wetter at a 4 C warmer world above pre-industrial levels (Koutroulis, 2019).”
BackgroundInfluentialTowards an understanding of future range shifts in lichens and mosses under climate change
Mallen-Cooper, M., Rodríguez-Caballero, E., Eldridge, D., Weber, B., Büdel, B., Höhne, H., & Cornwell, W. (2022) · Journal of Biogeography · doi:10.1111/jbi.14542 · Cited by 39
Pérez‐Guzmán, L., Acosta-Martínez, V., Phillips, L., & Mauget, S. (2020) · Applied Soil Ecology · doi:10.1016/j.apsoil.2019.103487 · Cited by 39
Ibrahim, A., Al-Fatesh, A., Khan, W., Kasim, S., Abasaeed, A., Fakeeha, A., Bonura, G., & Frusteri, F. (2019) · International journal of hydrogen energy · doi:10.1016/j.ijhydene.2019.09.014 · Cited by 39
Blin, N., Hausner, M., Leray, S., Lowry, C., & Suárez, F. (2022) · Journal of Hydrology: Regional Studies · doi:10.1016/j.ejrh.2022.100996 · Cited by 38
Future projection of droughts in Morocco and potential impact on agriculture.
Gumus, V., Moçayd, N. E., Seker, M., & Seaid, M. (2024) · Journal of Environmental Management · doi:10.1016/j.jenvman.2024.122019 · Cited by 38
Vegetation as the catalyst for water circulation on global terrestrial ecosystem.
Chen, J., Shao, Z.-F., Deng, X.-J., Huang, X., & Dang, C.-Y. (2023) · Science of the Total Environment · doi:10.1016/j.scitotenv.2023.165071 · Cited by 38
Zhao, Y., Chang, C., Zhou, X., Zhang, G., & Wang, J. (2023) · Journal of Environmental Management · doi:10.1016/j.jenvman.2023.119419 · Cited by 37
Li, S., & He, S. (2021) · Agricultural and Forest Meteorology · doi:10.1016/j.agrformet.2021.108767 · Cited by 38
Climate Change and Potential Demise of the Indian Deserts
Rajesh, P., & Goswami, B. (2022) · Earth's Future · doi:10.1029/2022ef003459 · Cited by 36
“Interestingly, many modeling studies indicate that Global Warming (GW) is expected to cause precipitation to decrease in most semi-arid regions, and vegetation-albedo feedback is likely to lead to the expansion of the global deserts (Koutroulis, 2019; Liu & Xue, 2020; Wetherald & Manabe, 2002; Zeng & Yoon, 2009).”
BackgroundBrasil, J. B., Guerreiro, M. S., de Andrade, E. M., Palácio, H. A. D. Q., Medeiros, P., & Ribeiro, J. C. (2022) · Sustainability · doi:10.3390/su14031721 · Cited by 36
Li, S., He, S., Xu, Z., Liu, Y., & von Bloh, W. (2023) · CATENA · doi:10.1016/j.catena.2022.106767 · Cited by 35
Soil health in Latin America and the Caribbean
Poppiel, R. R., Cherubin, M. R., Novais, J. J., & Demattê, J. A. M. (2025) · Communications Earth & Environment · doi:10.1038/s43247-025-02021-w · Cited by 46
“…lower SHI in northwestern Brazil most in fl uenced by climate factors (area under high pressure of deserti fi cation 41 – 43 ; intermediate SHI in the Amazon basin signed to vegetation biomass dynamics; middle-low SHI in Central Brazil caused by soil exposure from…”
Brazilian Dry Forest (Caatinga) Response To Multiple ENSO: the role of Atlantic and Pacific Ocean
Pereira, M. P. S., Mendes, K. R., Justino, F. B., do Couto-Santos, F. R., da Silva, A. S., da Silva, D. F., & Malhado, A. C. M. (2019) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2019.135717 · Cited by 45
Climate Resilient Development Pathways in Global Drylands
Stringer, L., Simpson, N., Schipper, E., & Eriksen, S. (2022) · Anthropocene Science · doi:10.1007/s44177-022-00027-z · Cited by 30
“…Change and Development in the Drylands Dryland areas are the hyper-arid, arid, semi-arid and dry sub-humid areas of the planet that cover about 45–47% of the Earth’s land area (Koutroulis 2019), and are inhabited by around a third of the world’s population: c.3 billion people (van der Esch et al.”
BackgroundAlary, V., Lasseur, J., Frija, A., & Gautier, D. (2022) · Agricultural Systems · doi:10.1016/j.agsy.2022.103389 · Cited by 30
Large variations in afforestation-related climate cooling and warming effects across short distances
Rohatyn, S., Rotenberg, E., Tatarinov, F. A., Carmel, Y., & Yakir, D. (2023) · Communications Earth & Environment · doi:10.1038/s43247-023-00678-9 · Cited by 31
“Since the ‘break-even time’ increases with aridity, and may exceed the expected forests life cycles, our results indicate that shifts such as predicted by Koutroulis 19 may result in corresponding shifts in the potential climate change mitigation benefits of forestation actions in drylands.”
ResultPotential distribution of three types of ephemeral plants under climate changes
Zhang, L., Liu, H.-L., Zhang, H.-X., Chen, Y.-F., Zhang, L.-W., Kudusi, K., Taxmamat, D., & Zhang, Y.-M. (2022) · Frontiers in Plant Science · doi:10.3389/fpls.2022.1035684 · Cited by 28
“, 2017), especially in the mid-latitude arid regions, where there are precipitation changes and temperature increases because of climate change, such as reduced precipitation and increased evaporation (Koutroulis, 2019).”
BackgroundLiu, Q., & Shi, T.-G. (2019) · Sustainability · doi:10.3390/su11154160 · Cited by 28
“The environmental problems following those pressures, such as global warming [5], soil erosion [6], desertification [7], environment pollution [8], and loss of biodiversity [9], have changed the ecosystem structure and process, decreased the ecosystem service value, and posed great threats to region sustainable develo…”
BackgroundInfluentialPrecise ecological restoration under water diversions-groundwater-ecosystem interactions in drylands
Liu, Q., Wang, G.-Y., Gui, D.-W., Liu, Y.-F., Abd-Elmabod, S. K., & Wei, G. (2023) · Journal of Hydrology · doi:10.1016/j.jhydrol.2023.130601 · Cited by 27
Desertification dynamics in China’s drylands under climate change
Meng-Tian, H. U. A. N. G., & Pan-mao, Z. (2023) · Advances in Climate Change Research · doi:10.1016/j.accre.2023.05.001 · Cited by 27
Spatial Shift of Aridity and Its Impact on Land Use of Syria
Houmsi, M. R., Shiru, M., Nashwan, M. S., Ahmed, K., Ziarh, G. F., Shahid, S., Chung, E., & Kim, S. (2019) · Sustainability · doi:10.3390/su11247047 · Cited by 27
“Koutroulis [14] projected a 7% increase in global drylands in the last part of the present century while Feng and Fu [15] projected an increase of 10%.”
BackgroundThe role of climate, vegetation, and soil factors on carbon fluxes in Chinese drylands
Liu, Z., Chen, Z., Yu, G.-R., Zhang, W., Zhang, T., & Han, L. (2023) · Frontiers in Plant Science · doi:10.3389/fpls.2023.1060066 · Cited by 26
“Drylands cover 41% of the global land surface (Feng and Fu, 2013) and sustain 38% of the world’s population (Koutroulis, 2019).”
BackgroundKashyap, R., Kuttippurath, J., & Patel, V. K. (2025) · GIScience & Remote Sensing · doi:10.1080/15481603.2025.2483458 · Cited by 25
“In the context of global warming, majority of semi-arid regions are expanding (Huang et al. 2017) and vegetation-albedo feedback will contribute to the expansion of deserts on a global scale (Koutroulis 2019; Zeng and Yoon 2009; IPCC 2021).”
Hirwa, H., Li, F., Qiao, Y., Measho, S., Muhirwa, F., Tian, C., Leng, P., Ingabire, R., Itangishaka, A. C., Chen, G., et al. (2022) · Frontiers in Environmental Science · doi:10.3389/fenvs.2022.851249 · Cited by 42
“Ultimately, model simulations and other evidence clearly show that continued global warming will make the earth’s drylands drier over time (Overpeck and Udall, 2010; Huang et al., 2012; Feng and Fu, 2013; Koutroulis, 2019).”
BackgroundCavalcante, A. D. M. B., & Sampaio, A. C. G. (2022) · Journal of Arid Environments · doi:10.1016/j.jaridenv.2022.104725 · Cited by 25
(2022) · Climate Change and Land · doi:10.1017/9781009157988.003 · Cited by 23
Global blind spots in soil health research overlap with environmental vulnerability hotspots
Cherubin, M. R., Pinheiro, C. R., Souza, L. F. N., Canisares, L., Ferreira, T. O., Cerri, C. E., Minasny, B., & Smith, P. (2025) · Communications Earth & Environment · doi:10.1038/s43247-025-02663-w · Cited by 24
“Such ari-di fi cation is expected to result in a global expansion of drylands by up to 6.9% 54 predominantly in the developing regions 55 , exacerbating its socio-economic vulnerability.”
InfluentialHow will drought evolve in global arid zones under different future emission scenarios?
Wu, F., Yang, X.-L., Yuan, X., Ren, L.-L., Yuan, S.-S., Yuan, F., Jiang, S.-H., Liu, Y., & Zhang, H.-S. (2024) · Journal of Hydrology: Regional Studies · doi:10.1016/j.ejrh.2024.101661 · Cited by 24
Significant influences of extreme climate on autumn phenology in Central Asia grassland
Gao, X.-Y., Tao, Z.-X., & Dai, J.-H. (2023) · Ecological Indicators · doi:10.1016/j.ecolind.2023.111056 · Cited by 24
Advancing the Evidence Base of Future Warming Impacts on Human Mobility in African Drylands
Thalheimer, L., Williams, D., Geest, K., & Otto, F. (2021) · Earth's Future · doi:10.1029/2020ef001958 · Cited by 24
“4 of 10 In a warmer world, drylands are expanding globally (IPCC, 2018) while high population growth in drylands exposes more people to climate hazards (Koutroulis, 2019).”
BackgroundInfluentialMeasurements and modeling of hydrological responses to summer pruning in dryland apple orchards
Ye, M., Zhao, X.-N., Biswas, A., Huo, G., Yang, B., Zou, Y.-F., Siddique, K., & Gao, X.-D. (2021) · doi:10.1016/j.jhydrol.2020.125651 · Cited by 23
Mıynat, M. E., & Argun, H. (2020) · doi:10.1016/j.ijhydene.2020.03.118 · Cited by 23
Allam, A., Moussa, R., Najem, W., & Bocquillon, C. (2020) · Hydrology and Earth System Sciences · doi:10.5194/hess-24-4503-2020 · Cited by 23
Ventura‐Rojas, P. D., González-Romero, A., Moreno, C. E., & Sosa, V. (2024) · Mammal Review · doi:10.1111/mam.12372 · Cited by 22
Zareian, M. (2021) · Journal of Hydro-environment Research · doi:10.1016/j.jher.2021.01.004 · Cited by 22
Wendt, C. F., Ceia-Hasse, A., Nunes, A., Verble, R., Santini, G., Boieiro, M., & Branquinho, C. (2021) · Scientific Reports · doi:10.1038/s41598-021-82059-w · Cited by 22
Imaging Spectroscopy for Conservation Applications
Seeley, M. M., & Asner, G. P. (2021) · Remote Sensing · doi:10.3390/rs13020292 · Cited by 28
“Drylands Dryland ecosystems cover nearly half of the global land area [74], and approximately three billion people, or nearly 40% of the global population, live in dryland ecosystems [75].”
BackgroundMazurana, L., Bittencourt, P. R. S., Scremin, F. R., Neves, A., & Possan, E. (2021) · Journal of Thermal Analysis and Calorimetry · doi:10.1007/s10973-020-10436-0 · Cited by 31
Hissan, R. U., Shafiq, H., Nassani, A., Parveen, N., Hussain, B., & Radulescu, M. (2024) · Environment, Development and Sustainability · doi:10.1007/s10668-024-05224-x · Cited by 21
“LDD can also lead to a reduction in biodiversity and poverty around the world (Koutroulis, 2019 ).”
Plant biomass allocation is mediated by precipitation use efficiency in arid and semiarid ecosystems
Feng, S., Ding, J., Zhan, T., Zhao, W., & Pereira, P. (2022) · Land Degradation and Development · doi:10.1002/ldr.4455 · Cited by 25
“Furthermore, the continuous expansion of arid and semiarid land under a changing climate (Feng & Fu, 2013; Huang et al., 2016; Koutroulis, 2019) will largely alter human welfare and affect the achievement of sustainable development goals (Yin et al., 2021).”
BackgroundCatalytic pyrolysis of pine bark over Ni/SiO2 in a CO2 atmosphere
Lee, T., Jung, S., Kim, K.-H., & Kwon, E. (2021) · Energy · doi:10.1016/j.energy.2021.119827 · Cited by 21
Controlling gully- and revegetation-induced dried soil layers across a slope-gully system.
Zhang, C.-C., Wang, Y.-Q., & Shao, M. (2020) · Science of the Total Environment · doi:10.1016/j.scitotenv.2020.142444 · Cited by 21
Song, Y.-F., Lu, Y.-J., Liu, T.-J., Li, H.-P., Yue, Z.-W., Liu, H.-W., & Gao, T.-M. (2020) · doi:10.1016/j.ecoleng.2020.105834 · Cited by 21
Zhang, G., Chen, X., Zhou, Y., Zhao, H., Jin, Y., Luo, Y., Chen, S., Wu, X., Pan, Z., & An, P. (2023) · Journal of Hydrology · doi:10.1016/j.jhydrol.2023.129939 · Cited by 21
Oliveira, A. D. F. N., de Sousa, L. I. S., da Costa, V. A. S., de Andrade, J. V. D., Lima, L. A. L., de Sales, P. A. F., da Silva, D. F., Pereira, A. P. D. A., & Melo, V. M. M. (2021) · Microbiology Research · doi:10.1016/j.micres.2021.126893 · Cited by 20
Corre, L., Ribes, A., Bernus, S., Drouin, A., Morin, S., & Soubeyroux, J. (2025) · Climate Services · doi:10.1016/j.cliser.2025.100553 · Cited by 19
Gumus, V., & Seker, M. (2024) · Hydrological Sciences Journal · doi:10.1080/02626667.2024.2364712 · Cited by 19
“Similarly, Koutroulis (2019) observed that climate change, characterized by reduced precipitation and increased PET, would exacerbate droughts and expand their impact areas across the Southern Mediterranean region under various warming scenarios (+1.5, +2, +4°C).”
InfluentialSlightly Enhanced Drought in the Yellow River Basin Under Future Warming Scenarios
Li, C., Kattel, G., Zhang, J., Shang, Y.-J., Gnyawali, K., Zhang, F., & Miao, L. (2022) · Social Science Research Network · doi:10.2139/ssrn.4052312 · Cited by 19
Future summer warming pattern under climate change is affected by lapse-rate changes
Brogli, R., Sørland, S. L., Kröner, N., & Schär, C. (2021) · Weather and Climate Dynamics · doi:10.5194/wcd-2-1093-2021 · Cited by 19
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Chen, L.-J., Li, C., Zhang, Z., Feng, Q., Xi, H.-Y., Guo, R., Zhang, C., & Wei, Y.-X. (2023) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104323 · Cited by 18
Metadata
- Authors
- Koutroulis, A. G.
- Affiliations
- Technical University of Crete (GR)
- Corresponding author
- Koutroulis, Aristeidis G.
- Venue
- Science of The Total Environment
- Publisher
- Elsevier BV
- Published
- 2019-03
- Volume
- 655
- Pages
- 482-511
- ISSN
- 0048-9697 (ISSN-L)
- OpenAlex
- W2901145303
- Cited by
- 294
- References
- 0
- Citations by year
- 2026: 29 · 2025: 41 · 2024: 51 · 2023: 40 · 2022: 52 · 2021: 44 · 2020: 25 · 2019: 12
- FWCI
- 11.86
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- The Science of The Total Environment (publishedVersion)
- PubMed (publishedVersion)
- Funders
- Seventh Framework Programme (603864)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Environmental Science › Global and Planetary Change › Hydrology and Drought Analysis
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate Change and Environmental Impact
- Keywords
- arid regions, aridity, global warming, climate change projections, CMIP5, RCP8.5, dryland expansion, land degradation, river basins, hydrological change, 1.5°C target, climate model resolution
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