Impacts of climate and land use/cover changes on streamflow at Kibungo sub-catchment, Tanzania

Lusajo Henry Mfwango; Tenalem Ayenew; Henry F Mahoo

doi:10.1016/j.heliyon.2022.e11285

Impacts of climate and land use/cover changes on streamflow at Kibungo sub-catchment, Tanzania

Heliyon. 2022 Oct 26;8(11):e11285. doi: 10.1016/j.heliyon.2022.e11285. eCollection 2022 Nov.

Authors

Lusajo Henry Mfwango^{1

2}, Tenalem Ayenew³, Henry F Mahoo⁴

Affiliations

¹ Africa Centre of Excellence for Water Management (ACEWM), College of Natural and Computational Sciences, Addis Ababa University, P.O. Box 1176, Ethiopia.
² Water Institute (W.I.), P. O. Box 35059, Dar es Salaam, Tanzania.
³ School of Earth Sciences, Addis Ababa University, P.O. Box 1176, Ethiopia.
⁴ Department of Agriculture Engineering and Land Planning, Sokoine University of Agriculture, Tanzania.

Abstract

The impacts of changing climate and land use/cover on streamflow in the Kibungo sub-catchment were evaluated using the Soil and Water Assessment Tool (SWAT). Rainfall, minimum, and maximum temperature data for six stations from the ensemble mean of the RCMs (RCA4, RACMO22T, CCLM4-8-17) were used under RCP 4.5 and RCP 8.5. The homogeneity and trend test were used to detect the change point and identify the pattern in the annual time series, respectively. Land Change Modeler (LCM) was used to predict land use maps of 2040 and 2070 from historical maps. Streamflow was simulated for 2021-2040 and 2041-2070 based on the homogeneity test results. The model calibration (2009-2016) and validation (2009-2016) for streamflow were successful. The homogeneity test detects a change point in 2040. A significant decrease in annual rainfall by 22.9 mm/yr (RCP 4.5) and 57 mm/yr (RCP 8.5) for 2021-2040 and an insignificant decrease was obtained during 2041-2070 under both emission scenarios. The annual temperature increased insignificantly by 0.004 °C/yr under RCP 4.5 while a significant increase of 0.21 °C/yr under RCP 8.5 was observed for 2021-2040. For 2041-2070, a significant increase of 0.016 °C/yr (RCP 4.5) and 0.045 °C/yr (RCP 8.5) was observed. The change in land use/cover resulted in increasing the build-up area (84%), agricultural fields (55.6%), and a decrease in the forest area (10.5%) during 2021-2040. During 2041-2070, the build-up area increased by 32.1%, the agricultural field by 36%, and the forest area decreased by 11%. Streamflow decreased significantly by 65.4 m³/yr (RCP 4.5) and 195.9 m³/yr (RCP 8.5) from 2021 to 2040. An insignificant decrease of 13.7 m³/s (RCP 4.5) and 7.63 m³/s (RCP 8.5) was observed during 2041-2070. This study provides an insight to the managers, planners, and policymakers on environmental protection/conservation for sustainable utilization of water resources at the Kibungo sub-catchment.

Keywords: Climate change; Kibungo sub-catchment; Land use/cover change; SWAT model; Streamflow simulation.