EGU2020-6575, updated on 15 Mar 2021
https://doi.org/10.5194/egusphere-egu2020-6575
EGU General Assembly 2020
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Spatial and temporal variation of drought patterns over East Africa

Gebremedhin Gebremeskel Haile1,2,3, Qiuhong Tang1,2, Guoyong Leng1, Guoqiang Jia1, Jie Wang1, Diwen Cai1, Siao Sun1, Binod Baniya1, and Qinghuan Zhang1
Gebremedhin Gebremeskel Haile et al.
  • 1Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese, Academy of Sciences, Beijing, China
  • 2University of Chinese Academy of Sciences, Beijing, China
  • 3Tigray Agricultural Research Institute, Mekelle, Ethiopia

Understanding historical patterns of changes in drought is essential for drought adaptation and mitigation.
While the negative impacts of drought over east Africa have attracted increasing attention,
a comprehensive and long-term spatiotemporal assessment of drought is still lacking. Here, we provided
a comprehensive spatiotemporal drought pattern analysis during the period of 1964–2015 over
the GHA. The Standardised Precipitation-Evapotranspiration Index (SPEI) at various timescales (1 month
(SPEI-01), 3 month (SPEI-03), 6 month (SPEI-06), and 12 month (SPEI-12)) was used to investigate drought
patterns on a monthly, seasonal, and interannual basis. The results showed that despite regional differences,
an overall increasing tendency of the drought was observed across the GHA over the past 52 yr, with trends of
change of -0.0017 yr-1, -0.0036 yr-1, -0.0031 yr-1, and -0.0023 yr-1 for SPEI-01, SPEI-03, SPEI-06, and
SPEI-12, respectively. Droughts were more frequent, persistent, and intense in Sudan and Tanzania, while
more severe droughts were found in Somalia, Ethiopia, and Kenya. Droughts occurred frequently before
the 1990 s, and then became intermittent with large-scale impacts occurred during 1973–1974, 1984–
1985, and 2010–2011. A turning point was also detected in 1989, with the SPEI showing a statistically significant
downward trend during 1964–1989 and a non-statistically significant downward trend from 1990
to 2015. Seasonally, droughts exhibited an increasing trend in winter, spring, and summer, but a decreasing
trend in autumn. The research findings have significant implications for drought adaptation and mitigation
strategies through identifying the hotspot regions over east Africa at various timescales. Area-specific
efforts are required to alleviate environmental and societal vulnerabilities to drought events.

How to cite: Haile, G. G., Tang, Q., Leng, G., Jia, G., Wang, J., Cai, D., Sun, S., Baniya, B., and Zhang, Q.: Spatial and temporal variation of drought patterns over East Africa, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6575, https://doi.org/10.5194/egusphere-egu2020-6575, 2020.