Spatiotemporal climate variability and trends in the Upper Gelana Watershed, northeastern highlands of Ethiopia

Sileshi Tadesse; Asnake Mekuriaw; Mohammed Assen

Heliyon (Mar 2024)

Spatiotemporal climate variability and trends in the Upper Gelana Watershed, northeastern highlands of Ethiopia

Sileshi Tadesse,
Asnake Mekuriaw,
Mohammed Assen

Affiliations

Sileshi Tadesse: Department of Geography and Environmental Studies, Addis Ababa University, P.O.Box 1176, Addis Ababa, Ethiopia; Department of Geography and Environmental Studies, Kotebe University of Education, P.O.Box 31248, Addis Ababa, Ethiopia; Corresponding author. Department of Geography and Environmental Studies, Addis Ababa University, P.O.Box 1176, Addis Ababa, Ethiopia.
Asnake Mekuriaw: Department of Geography and Environmental Studies, Addis Ababa University, P.O.Box 1176, Addis Ababa, Ethiopia
Mohammed Assen: Department of Geography and Environmental Studies, Addis Ababa University, P.O.Box 1176, Addis Ababa, Ethiopia

Journal volume & issue: Vol. 10, no. 5
p. e27274

Abstract

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The aim of this study was to evaluate the performance of CHIRPS and TAMSAT satellite rainfall data over the Upper Gelana watershed, where gauged meteorological data to understand the nature of the climate are scarce. In addition, variability and trends in rainfall and temperature were examined from 1983 to 2021. To evaluate satellite rainfall, categorical and continuous validation statistics were used. Trends were analyzed using Mann-Kendall, Sen's Slope estimator, and innovative trend analysis (ITA) methods. The study also utilized time-series geostatistical analysis techniques. The validation statistics show that TAMSAT performs better on the daily timescale, while the two products have comparable performance on the monthly timescale. TAMSAT was chosen for rainfall analysis because of its higher resolution and performance. The results reveal high inter-annual spatiotemporal variability and strong irregularities in monthly rainfall. The Mann-Kendall test indicates statistically significant positive trends in kiremt and annual rainfall, but belg rainfall exhibits an insignificant negative trend. In the kiremt season, we found a 96.1, 101.6, and 104.8 mm decadal rate of rainfall increment in the lower weina dega (LWD), upper weina dega (UWD), and dega agroecological zones, respectively. In contrast, belg season rainfall declined by 16.4, 16.2, and 14.0 mm per decade in the LWD, UWD, and dega agroecology zones, respectively. The pixel-wise trend analysis also revealed trends and magnitudes of monthly, seasonal, and annual rainfall that vary across the study area. In both LWD and UWD annual minimum and maximum temperatures, respectively, showed significant decreasing and increasing trends, but in dega agroecology the trends were insignificant. The findings of rainfall and temperature trends using the ITA method demonstrated its ability to discover some hidden trends that were not detected by the MK test.

Published in Heliyon

ISSN: 2405-8440 (Online)
Publisher: Elsevier
Country of publisher: United Kingdom
LCC subjects: Science: Science (General); Social Sciences: Social sciences (General)
Website: https://www.cell.com/heliyon/home

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