Investigation of Vegetation Cover Change in Sudan by Using Modis Data
- 1 State Key Laboratory of Cryospheric Sciences/Tian Shan Glaciological Station, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
- 2 State Key Laboratory of Cryospheric Sciences/Tian Shan Glaciological Station, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
- 3 Department of Forest Protection and Conservation, Faculty of Forestry, University of Khartoum, Shambat, Sudan
- 4 Division of Hydrology Water-Land Resources, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
- 5 State Key Laboratory of Cryospheric Sciences/Tian Shan Glaciological Station, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
- 6 State Key Laboratory of Cryospheric Sciences/Tian Shan Glaciological Station, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
- 7 College of Geography and Environmental Science, Northwest Normal University, Lanzhou, China
Abstract
The aim of this research paper is to investigate the land cover changes in Sudan during the period 2001-2013 by using the MODIS data and to identify climatic factors influencing the land cover. SPSS v 17 software was used to investigate the correlation of climatic factors with vegetation cover; also ArcGIS v 10.2 software was used to analyze the NDVI data. The results indicate that the monthly average time scale, NDVI value curve distribution during the year, July to October as the center to both sides of decreasing vegetation cover in other months. In the spatial distribution of mean NDVI in Sudan, a high value was found in the southern part. On the other hand, a low value of vegetation cover was found in northern part. NDVI spaces mean presenting features values: autumn followed by summer then winter. By calculation of average annual and seasonal-NDVI values, it was deduced that the main vegetation cover type was increasing in winter and summer seasons at the rates of 0.014/10a and 0.008/10a, respectively. While winter-NDVI was decreasing the rate of 0.001/10a and 0.026/10a in autumn and on the annual scale, respectively. Annual NDVI showed a significant degradation (area = 12705.7 km 2 , 0.5% of total area) in the middle and eastern parts and significant improvement (area = 22485.4 km 2 , 0.9 % of the total area) in the southern part of the country due to the increase in precipitation and decrease in temperature. Mean summer and autumn-NDVI showed a significant difference 0.01% significance level with mean summer and autumn precipitation (correlation coefficients = 0.955 and 0.953, respectively). While there was a significantly negative relationship between mean summer and autumn-NDVI with mean summer and autumn temperature at 0.01% significance level (correlation coefficients = − 0.270 and − 0.820, respectively).
- Peter, J.L. (1983) Sub-Saharan Rainfall Update for 1982: Continued Drought. Journal of Climatology, 3, 419-422. http://onlinelibrary.wiley.com/doi/10.1002/joc.3370030410/full
- UNEP (1992) World Atlas of Desertification. Edward Arnold, Sevenoaks, 68 p.
- Zakieldeen, S.A. (2007) Vulnerability in Sudan. Tiempo Bulletin 62. Online bulletin at: http://www.tiempocyberclimate.org
- El Sammani, M. (1978) Gaps in the Water Provision Map of the Sudan. Sudan Notes and Records, 59, 97-106.
- King’uyu, S.M., Ogallo, L.A. and Anyamba, E.K. (2000) Recent Trends of Minimum and Maximum Surface Temperatures over Eastern Africa. Journal of Climate, 13, 2876-2886. https://doi.org/10.1175/1520-0442(2000)013 2.0.CO;2
- Eldredge, E. Khalil, S.E., Nicholds, N., Abdalla, A.A. and Rydjeski, D. (1988) Changing Rainfall Patterns in Western Sudan. Journal of climatology, 8, 45-53. http://onlinelibrary.wiley.com/doi/10.1002/joc.3370080105/full
- Walsh, R.P.D., Hulme, M. and Campbell, M.D. (1988) Recent Rainfall Changes and Their Impact on Hydrology and Water Supply in the Semi-Arid Zone of the Sudan, The Geographical Journal, 154, 181-198. https://doi.org/10.2307/633845
- Ayoub, A.T., (1998) Extent, Severity and Causative Factors of Land Degradation in the Sudan. Journal of Arid Environments, 38, 397-409. http://www.sciencedirect.com/science/article/pii/S0140196397903463
- Yagoub, Y.E., Li, Z., Musa, O.S., Wang, F., Anjum, .M.N., Bo, Z. and Ding-min, J. (2017) Detection Of Drought Pattern in Sudan Using Standardized Precipitation-Evapotranspiration Index (SPEI). International Journal of Recent Advances in Multidisciplinary Research, 4, 2546-2554. http://www.ijramr.com/sites/default/files/issues-pdf/1348.pdf
- Yagoub, Y.E., Bo, Z., Ding-min, J., Jahelnabi, A.E. and Fadoul, S.M. (2015) Land Use and Land Cover Change in Northeast Gadarif State: Case of El Rawashda Forest, Sudan. Journal of Geographic Information System, 7, 140-157. https://doi.org/10.4236/jgis.2015.72013
- Yagoub, Y.E., Musa, O.S., Siddig, A.A., Bo, Z., Li, Z. and Wang, F. (2017) Assessing the Impacts of Land Use Changes on Vegetation Cover in Eastern Sudan. International Journal of Research in Agricultural Sciences, 4, 70-75. https://ijras.org/administrator/components/com_jresearch/files/publications /IJRAS_505__FINAL.pdf
- UNESCO (1977) United Nations Educational, Scientific and Cultural Organization. Map of the World Distribution of Arid Regions. MAB Technical Notes 7, Paris.