Quantitative Contributions of Climate Change and Human Activities to Vegetation Changes in the Upper White Nile River

Vegetation changes in the Upper White Nile River (UWNR) are of great significance to the maintenance of local livelihoods, the survival of wildlife, and the protection of species habitats. Based on the GIMMS NDVI3g and MODIS normalized difference vegetation index (NDVI) data, the temporal and spatia...

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Main Authors: Bo Ma, Shanshan Wang, Christophe Mupenzi, Haoran Li, Jianye Ma, Zhanbin Li
Format: Article
Language:English
Published: MDPI AG 2021-09-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/13/18/3648
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spelling doaj-7e23ba392b7e414cb9c339959bbdc4a82021-09-26T01:17:06ZengMDPI AGRemote Sensing2072-42922021-09-01133648364810.3390/rs13183648Quantitative Contributions of Climate Change and Human Activities to Vegetation Changes in the Upper White Nile RiverBo Ma0Shanshan Wang1Christophe Mupenzi2Haoran Li3Jianye Ma4Zhanbin Li5State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, ChinaDepartment of Environmental Information Systems, Faculty of Environmental Studies, University of Lay Adventists of Kigali, K K 508 St., Kigali P.O. Box 6392, RwandaState Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, ChinaVegetation changes in the Upper White Nile River (UWNR) are of great significance to the maintenance of local livelihoods, the survival of wildlife, and the protection of species habitats. Based on the GIMMS NDVI3g and MODIS normalized difference vegetation index (NDVI) data, the temporal and spatial characteristics of vegetation changes in the UWNR from 1982 to 2020 were analyzed by a Theil-Sen median trend analysis and Mann-Kendall test. The future trend of vegetation was analyzed by the Hurst exponential method. A partial correlation analysis was used to analyze the relationship of the vegetation and climate factors, and a residual trend analysis was used to quantify the influence of climate change and human activities on vegetation change. The results indicated that the average NDVI value (0.75) of the UWNR from 1982 to 2020 was relatively high. The average coefficient of variation for the NDVI was 0.059, and the vegetation change was relatively stable. The vegetation in the UWNR increased 0.013/10 year on average, but the vegetation degradation in some areas was serious and mainly classified as agricultural land. The results of a future trend analysis showed that the vegetation in the UWNR is mainly negatively sustainable, and 62.54% of the vegetation will degrade in the future. The NDVI of the UWNR was more affected by temperature than by precipitation, especially on agricultural land and forestland, which were more negatively affected by warming. Climate change and human activities have an impact on vegetation changes, but the spatial distributions of the effects differ. The relative impact of human activities on vegetation change accounted for 64.5%, which was higher than that of climate change (35.5%). Human activities, such as the large proportion of agriculture, rapid population growth and the rapid development of urbanization were the main driving forces. Establishing a cross-border drought joint early warning mechanism, strengthening basic agricultural research, and changing traditional agricultural farming patterns may be effective measures to address food security and climate change and improve vegetation in the UWNR.https://www.mdpi.com/2072-4292/13/18/3648vegetation changeclimate changehuman activitiesthe Upper White Nile RiverEast Africa
collection DOAJ
language English
format Article
sources DOAJ
author Bo Ma
Shanshan Wang
Christophe Mupenzi
Haoran Li
Jianye Ma
Zhanbin Li
spellingShingle Bo Ma
Shanshan Wang
Christophe Mupenzi
Haoran Li
Jianye Ma
Zhanbin Li
Quantitative Contributions of Climate Change and Human Activities to Vegetation Changes in the Upper White Nile River
Remote Sensing
vegetation change
climate change
human activities
the Upper White Nile River
East Africa
author_facet Bo Ma
Shanshan Wang
Christophe Mupenzi
Haoran Li
Jianye Ma
Zhanbin Li
author_sort Bo Ma
title Quantitative Contributions of Climate Change and Human Activities to Vegetation Changes in the Upper White Nile River
title_short Quantitative Contributions of Climate Change and Human Activities to Vegetation Changes in the Upper White Nile River
title_full Quantitative Contributions of Climate Change and Human Activities to Vegetation Changes in the Upper White Nile River
title_fullStr Quantitative Contributions of Climate Change and Human Activities to Vegetation Changes in the Upper White Nile River
title_full_unstemmed Quantitative Contributions of Climate Change and Human Activities to Vegetation Changes in the Upper White Nile River
title_sort quantitative contributions of climate change and human activities to vegetation changes in the upper white nile river
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2021-09-01
description Vegetation changes in the Upper White Nile River (UWNR) are of great significance to the maintenance of local livelihoods, the survival of wildlife, and the protection of species habitats. Based on the GIMMS NDVI3g and MODIS normalized difference vegetation index (NDVI) data, the temporal and spatial characteristics of vegetation changes in the UWNR from 1982 to 2020 were analyzed by a Theil-Sen median trend analysis and Mann-Kendall test. The future trend of vegetation was analyzed by the Hurst exponential method. A partial correlation analysis was used to analyze the relationship of the vegetation and climate factors, and a residual trend analysis was used to quantify the influence of climate change and human activities on vegetation change. The results indicated that the average NDVI value (0.75) of the UWNR from 1982 to 2020 was relatively high. The average coefficient of variation for the NDVI was 0.059, and the vegetation change was relatively stable. The vegetation in the UWNR increased 0.013/10 year on average, but the vegetation degradation in some areas was serious and mainly classified as agricultural land. The results of a future trend analysis showed that the vegetation in the UWNR is mainly negatively sustainable, and 62.54% of the vegetation will degrade in the future. The NDVI of the UWNR was more affected by temperature than by precipitation, especially on agricultural land and forestland, which were more negatively affected by warming. Climate change and human activities have an impact on vegetation changes, but the spatial distributions of the effects differ. The relative impact of human activities on vegetation change accounted for 64.5%, which was higher than that of climate change (35.5%). Human activities, such as the large proportion of agriculture, rapid population growth and the rapid development of urbanization were the main driving forces. Establishing a cross-border drought joint early warning mechanism, strengthening basic agricultural research, and changing traditional agricultural farming patterns may be effective measures to address food security and climate change and improve vegetation in the UWNR.
topic vegetation change
climate change
human activities
the Upper White Nile River
East Africa
url https://www.mdpi.com/2072-4292/13/18/3648
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