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Global exposure of population and land-use to meteorological droughts under different warming levels and SSPs: a CORDEX-based study.
Spinoni, J., P. Barbosa, E. Bucchignani, J. Cassano, T. Cavazos, A. Cescatti, J.H. Christensen, O.B. Christensen, E. Coppola, J.P. Evans, G. Forzieri, B. Geyer, F. Giorgi, D. Jacob, J. Katzfey, T. Koenigk, R. Laprise, C.J. Lennard, M. Levent Kurnaz, D. Li, M. Llopart, N. McCormick, G. Naumann, G. Nikulin, T. Ozturk, H.-J. Panitz, R.P. da Rocha, S.A. Solman, J. Syktus, F. Tangang, C. Teichmann, R. Vautard, J.V. Vogt, K. Winger, G. Zittis, A. Dosio
International Journal of Climatology, 41(15), 6825-6853, doi: 10.1002/joc.7302, 2021.
Abstract
Global warming is likely to cause a progressive drought increase in some
regions, but how population and natural resources will be affected is still
underexplored. This study focuses on global population, forests, croplands and
pastures exposure to meteorological drought hazard in the 21st century,
expressed as frequency and severity of drought events. As input, we use a large
ensemble of climate simulations from the Coordinated Regional Climate
Downscaling Experiment (CORDEX), population projections from the NASA-
SEDAC dataset and land-use projections from the Land-Use Harmonization
2 project for 1981–2100. The exposure to drought hazard is presented for five
Shared Socioeconomic Pathways (SSP1-SSP5) at four Global Warming Levels
(GWLs: 1.5C to 4 C). Results show that considering only Standardized Precip-
itation Index (SPI; based on precipitation), the SSP3 at GWL4 projects the larg-
est fraction of the global population (14%) to experience an increase in drought
frequency and severity (versus 1981–2010), with this value increasing to 60% if
temperature is considered (indirectly included in the Standardized
Precipitation-Evapotranspiration Index, SPEI). With SPEI, considering the
highest GWL for each SSP, 8 (for SSP2, SSP4, SSP5) and 11 (SSP3) billion peo-
ple, that is, more than 90%, will be affected by at least one unprecedented
drought. For SSP5 at GWL4, approximately 2 × 106 km2 of forests and crop-
lands (respectively, 6% and 11%) and 1.5 × 106 km2 of pastures (19%) will be
exposed to increased drought frequency and severity according to SPI, but for
SPEI this extent will rise to 17 × 106 km2 of forests (49%), 6 × 106 km2 of pas-
tures (78%) and 12 × 106 km 2 of croplands (67%), being mid-latitudes the most
affected. The projected likely increase of drought frequency and severity signif-
icantly increases population and land-use exposure to drought, even at low
GWLs, thus extensive mitigation and adaptation efforts are needed to avoid the
most severe impacts of climate change.
Key Figure
Figure 11. Population and
land-use progressive exposure to
significant increase of both DF and DS
at different GWLs under the SSP5
scenario, according to SPI (left) and
SPEI (right). White represents areas
with population below 1 inhabitant/
km2 and land-use below 5% over the
grid point.
This page is maintained by Jason Evans |
Last updated 22 April 2023
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