Land use/cover dynamics and its drivers in Gelda catchment, Lake Tana watershed, Ethiopia
© The Author(s) 2017
Received: 30 July 2016
Accepted: 1 January 2017
Published: 14 January 2017
The demand for meeting local food production has caused farmlands to expand at the cost of natural forests and grasslands in the Ethiopian highlands. However, empirical evidences on rate and patterns of LULC dynamics, and major driving forces in highlands of Ethiopia at catchment level were rare to contribute to design effective land management options. This study was to analyze the rate and patterns of LULC dynamics, and identify major driving forces in the Gelda catchment.
Six different LULC maps derived from aerial photographs and Landsat images were produced, and comparisons were made. The results indicated that the study catchment has undergone significant LULC alterations and transformations since late 1950s. Farmlands and settlement were expanded by 57.7% while shrubs, forests and grasslands were declined by 18.6, 83.8 and 53.5% over the entire study period, respectively. The magnitude of initial grasslands and farmlands converted into degraded land seems small; however these can significantly cause an irreversible damage to the soil resources. The combinations of land reform of 1975, forest development and villagization program 1980s, civil war, frequent changes in political structure, and population pressure were the major driving forces of LULC change.
Therefore, the GIS and remote sensing based change detection matrix analysis technique could provide useful baseline information to understand the spatiotemporal patterns of land use transitions caused by the major driving forces thereby sustainable land management planning is possible.
Local changes in land use and land cover (LULC) affect life support functions and human livelihoods (Lambin et al. 2001; Lambin and Geist 2006). It has diverse environmental impacts by negatively affecting water supply, reservoir storage capacity, agricultural productivity and ecology of a region (Sharma et al. 2011). In most developing countries, the demands for meeting local food production caused agricultural lands expansion at the expense of natural forests and grasslands (Lambin et al. 2003). Local level studies undertaken in highlands of Ethiopia suggest that a presence of significant LULC changes were caused by a combination of varying factors depending on each locality condition (Hassen et al. 2015; Eyayu et al. 2009; Woldeamlak and Sterk 2005; Eleni et al. 2013; Mohammed 2011; Woldeamlak 2002).
Increased deforestation and poor farm management practices has led to accelerated soil erosion and land degradation in the Ethiopian highlands (Mohammed et al., 2005; Hurni et al. 2005; Hassen et al. 2015). These are, particularly, common in areas where high population pressure exists whose livelihoods directly depend on the exploitation of natural resources in rural areas (Woldeamlak and Sterk 2005). Farmland/settlements and bushlands/degraded lands were expanding appreciably, while grasslands and forest areas have been diminished largely driven by population pressures, economic factors and policy issues (Woldeamlak 2002; Getachew et al. 2011; Tsehaye and Mohammed 2013; Eleni et al. 2013; Hassen et al. 2015; Alemu et al. 2015). Similarly, significant expansions of urban built-up were accompanied by substantial decline in forest, grass and shrub lands (Mohammed 2011). These studies supported that LULC changes have implications for environmental degradation such as soil erosion, soil quality deterioration, decreasing available water and the subsequent drying-out of water reservoirs.
Increasing rates of forest conversion, unsustainable agricultural land use and severe soil erosion are the major factors characterizing land degradation in the highlands of Ethiopia (Mekuria 2005). Despite efforts made to overcome deforestation and the resulting land degradation in Ethiopia, as EFAP 1993, the extent of forests was much higher from 40% at the beginning of the twentieth century, 16% in the 1950s, 3.1% by 1982, only 2–3% in 1990s, and 3.56% in 2004 (Badege 2001; Wubalem 2012). That means, although the attempts to rehabilitate areas under intense deforestation and degraded as part of national campaign to conserve soil and water in different parts of Ethiopia have been done; success has been limited to date. Accordingly, some remnant stands of natural forests are mainly confined to religious sites, along rivers and streams, and on peaks of hills where crop cultivation is difficult in the highlands of Ethiopia (Warra et al. 2013). This is due to the fact that agriculture and rural settlement has remained the predominant and ever expanding LULC classes between 1965 and 2007 caused by a variety of natural and man-made drivers of change.
The major driving forces of human-induced change in LULC form a complex system of dependencies, interactions and feedback loops at different spatiotemporal scales (Agarwal et al. 2002; Verheye 2007). These complexity calls for multidisciplinary analyses, primarily focused on biophysical attributes (e.g. topographic or soil type), and wide range of socio-economic drivers of change (Veldkamp and Lambin 2001). Driving force of landscape change is determined by the spatiotemporal and institutional scale of the system under study (Bürgi et al. 2004). These driving forces of landscape change involve land cover (climate, topography and soil characteristics) and land use (human induced) processes, such as natural (biophysical) and man-made driving forces, i.e., socioeconomic, political, technological, and cultural (Bürgi et al. 2004; Sherbinin 2002; Lambin et al. 2001). Cultural or man-made drivers may also trigger events as important as biophysical drivers (Lambin et al. 2003).
The mounting pressures on the natural forest, shrubs and grasslands by unsustainable land uses, in the study area, have witnessed spatiotemporal changes in LULC patterns. However, studies of LULC dynamics using change detection analysis to explain the land use transition, i.e., net loss and/or gain of each LULC classes over space and time at this level are rare in the northwestern highlands of Ethiopia. This study is, therefore, crucial for researchers to contribute on the limited literature on the subject by providing empirical evidences on rate and patterns, and major driving forces of LULC dynamics in highlands of Ethiopia at catchment level; which can contribute to design effective land management options. It can also provide insights into the major contributors of land use transitions and a baseline study for examining their implications on soil erosion potential, soil characteristics and suitability status of the land for sustainable rainfed agriculture in the highlands of Ethiopia. Therefore, the main purpose of this analysis is to provide empirical evidences on rate and patterns, and identify major driving forces of LULC dynamics at watershed level; and thereby designing a more effective land management options will be possible.
Materials and methods
Study area description
The altitude ranges from 1780 to 2481 meters above sea level. The slope gradient is dominated by gentle slope (0–7.6%) covering about 48.5% (12,682 ha) and moderately steep (7.7–16%) with 37.13% (9714 ha) of the catchment. The steep (16.2–30.2%) and very steep (>30.3%) slope gradients cover about 11.22% (2936 ha) and 3% (787 ha) respectively, commonly found in the southeastern and southern corners of the catchment. Gleysols (54.9%) and Nitisols (30.5%) form the major soil types of the catchment (FAO 1997). Gleyosols are poorly drained with seasonal water accumulation (Driessen and Deckers 2001). The other soils are commonly found on the sloping lands.
As evidenced from protected areas like churches and grave yards, climatic–climax vegetation found in the area include Juniperus procera (locally tid), Hagenia abyssinica (locally called kosso); Albizia gummifera (Sassa); Podocarpus falcatus (Zigba); Cordia africana (wanza); and Ficus vasta (Warka). Field observation also indicated that non-indigenous tree species like Cupressocyparis leylandii (yeferenj Tid), Acacia sieberiana (Yefereng Girar) and Eucalyptus spp. (Bahir zaf) are expanding.
Subsistence rainfed crop production with supplementary traditional irrigation and livestock husbandry are the main sources of livelihood. Dera wereda ARD office (2013) showed that the commonly grown crops in the catchment include barley (Hordeum vulgare L.), maize (Zea mays L.), teff (Eragrotis teff), noug (Guizotia abyssinica), and finger millet (Eleusin coracana).
Data sources and methods of analysis
Time series black-and-white photographic and Landsat satellite images were the main source of input data for the LULC analysis in this study. The 1957 aerial photographic images and 1973 Landsat image were the only oldest remote sensing data available for the study area, but there were no any reference images available between 1957 and 1973. Thus, further subdivisions for LULC analysis between 1957 and 1973 were not possible. Eleven 1 m × 1 m black-and-white scanned photographic images of 1957 by 600 dots per inch (DPI) were obtained from Ethiopian Mapping Agency (EMA). These were used for photogrammetric processing, as well as visual photo-interpretation activities. Materials such as mirror and pocket stereoscopes were employed for stereo viewing during visual interpretations of features on hardcopy pairs of aerial photos. The visual interpretations process using stereoscopes were helpful to substantiate onscreen feature classifications using GIS environment. Subsequently, all photographic images were geometrically corrected based on geo-referenced and 1:50,000 scale topographic map to produce orthorectified images using “Geo Correction Tools” of ArcGIS. Finally, the mosaic image was produced from eleven orthorectified images using “Mosaic Tool” and later “subset image” into the required study area AOI of ERDAS EMAGINE 9.2.
Landsat images were downloaded from Global Land Cover Facility (GLCF) in the USGS archives at Glovis (http://glovis.usgs.gov). Five images were downloaded at about ten years’ interval to easily visualize changes in spatiotemporal LULC patterns. However, some discrepancy ±1 year was considered due to the availability and quality of Landsat images from USGS archives for the study area. Therefore, the Landsat MSS of 1973 (60 m × 60 m), Landsat TM of 1984 and 1995 (30 m × 30 m), Landsat ETM+ of 2004 (30 m × 30 m) and Landsat OLI of 2014 (30 m × 30 m) at path (169 and 170p), and row (52r) images were used. These were preprocessed such as layer stacking, sub-sampling the study area by AOI file, re-sampling of all time-series images into similar ground resolution (30 m × 30 m), gap filling for Landsat 7 SCL-off (2004 and 2014 images), and spectrally enhancing the images before actual image classification process.
The major LULC classes considered in the classification are as given in Table 2. The farm and settlement areas were included in the same land cover as it was difficult to separate these two on the employed images. Likewise, wetland class has been excluded in the classification process as an independent LULC class because this class largely covered with grassland, cultivated fields and forest adjacent to Lake Tana. Consequently, it was difficult to analyze wetlands separately while the area under study is occupied by different LULC classes. About 100 ground control points (GCP) representative of the different LULC classes were taken by a GPS receiver to improve accuracy of classification and to produce thematic land cover maps representative to the entire study period. Field observation was also conducted to substantiate the image classification and analysis.
Accuracy assessment for the classified images
Overall classification accuracy (%)
Overall kappa coefficient
Description of LULC classes identified in Gelda catchment of Lake Tana watershed, Ethiopia
Farmland and settlement
Areas used for crop cultivation, both annuals and perennials, and the scattered rural settlements that are closely associated with the cultivated fields. These were combined into one category as it was difficult to identify the dispersed rural settlements as a separated LULC class where fragmented cultivated land exists around homesteads
Forest areas covered with dense growth of trees that formed nearly closed canopies around religious sites. This category also included plantation forests mixed with regenerating ‘indigenous’ species of trees and bushes
Areas covered with shrubs, bushes and small trees, with little useful wood, mixed with some grasses
Land predominately covered with grasses, forbs, grassy areas
Bare land cover
Bare landscape that has very little or no grass cover due to overgrazing of grasslands
Results and discussion
Land use/cover patterns of Gelda catchment between 1957 and 2014
Farmland and settlement
Bare land cover
Rate of change in LULC between 1957 and 2014 in Gelda catchment
Farmland and settlement
LULC change in the study catchment between 1957 and 1973
Table 4 and Fig. 4 indicated an existence of spatiotemporal transformations in the identified LULC classes. Shrinkage of forest cover was observed between 1957 and 1973, while the other LULC classes showed expansions of their original extent in this early period of analysis. Forest cover was declined by 71.5% (265.2 ha/year) over the time span of 16 years. The shrinkage could be attributed to destruction of natural forests in search for additional farm plots, construction materials and domestic fuel consumption in the study catchment. However, farmland and settlement cover, which accounted the lowest coverage ever in the entire 57 years, but has been extended by 12.9% (73.3 ha/year). Shrubs accounted for 27% of the total area of the catchment in 1957 and expanded by 10.2% (45.5 ha/year). Likewise, grasslands were around 15.8% of the study area and exceptionally increased by 51.7% (134.2 ha/year). These possibly reflect the impacts of deforestations on land use transitions where natural forests are ultimately converted into farmlands, shrubs and grasslands between 1957 and 1973. Actual transformed figures of LULC class to other were not given because change detection matrix analysis was not possible.
LULC change in the study catchment between 1973 and 1984
LULC change matrix of the study catchment (1973–1984)
Change from LULC 1984 (ha)
Farmland and settlement
Change from LULC 1973 (ha)
Farmland and settlement
The exceptional increment of forests by 20.06% (338.87 ha) was largely due to additional areas obtained from grassland by 13.7% (277.56 ha), farmland and settlement by 18.7% (379.82 ha), and shrubs by 37.75% (765.94 ha) despite some of the original cover was lost largely into farmland and settlement by 52.98% (895.27 ha) and shrubs by 6.97% (117 ha). This suggests that land acquisition from other LULC classes for forest conservation program was in response to initiatives of restoring indigenous trees and forests by the past socialist regime’s forest development program since the establishment of Gelda protected forest in 1980. Similarly, bare land cover also expanded due to major area gain from conversion of grasslands by about 59.2% (119.6 ha), and farmland and settlement by about 29.3% (59.35). The expansion of bare land reflected the impact of unsustainable utilizations of grasslands and farmlands due to overgrazing and land degradation.
Shrinkages were observed in the extent of grasslands by 27.6% (158 ha/year) and shrubs 7.26% (52 ha/year) despite some gains were obtained from other LULC classes (Table 4 and 5). It is because some areas gained areas from different LULC classes could not bring a net expansion in grasslands and shrubs or did not compensate its decline in this second period of analysis. The substantial decline for grasslands were largely contributed by conversion of its original extent into farmland and settlement 30.63% (1929.56 ha) and shrubs by 33.92% (2136.44 ha) despite some gains were observed mainly from farmland and settlement by 38% (1735.59 ha) and shrubs by 19.2% (875.56 ha). This was attributed to land acquisition for farmlands following the downfall of the imperial regime in 1974 and the resulting policy changes at the expense of grazing lands and shrubs. This also showed the increasing demand for farmlands as well as forest development into areas once occupied by grassland. In addition, shrinkage of shrubs were largely due to conversion of its original extent into farmlands and settlement by about 50.2% (3946.1 ha) despite some area gains were observed mainly from grasslands, and farmland and settlement by about 29.3% (2136.44 ha) and 36.48% (2660.21 ha), respectively. This clearly showed that about half of the original shrubland were transformed into farmland and settlement caused by population pressure and changes in land tenure system that transformed landless tenants into land owners.
LULC change in the study catchment between 1984 and 1995
LULC change matrix of the Gelda catchment (1984–1995)
Change from LULC 1995 (ha)
Farmland and settlement
Change from LULC 1984 (ha)
Farmland and settlement
Shrinkages were evident in forest cover 52.6% (97 ha/year) and shrubs 61.63% (408.6 ha/year) despite some area gains were observed from other LULC classes (Tables 4, 6). It was because the area gained from other LULC classes could not satisfy the losses or conversions from their original extent. The dominant reasons that largely contributed to the reduction of forest cover were conversion of its initial extent into farmlands and settlement by about 47.37% (960.98 ha), and shrubs by about 19.26% (390.8 ha) despite some gains from farmland and settlement. It was partly attributed to forced resettlement program between 1987 and 1991. This could be due to forest clearing in search for additional farmlands and new settlement units in socialist regime, particularly during rural resettlement program. The demand for local construction material and fuel wood, and civil war between 1990 and 1991 were the other reasons for forestland decrease. Shrubs have also been diminished as a result of conversion of its initial extent largely into grasslands by about 27% (1975.4 ha) and farmland and settlement by about 53.8% (3925.9 ha) despite some gains in farmland and settlement. It was partly related to political instability and change of political structure of the country, which led to the clearance of shrubs for expansion of farmlands and new settlement centers. These revealed that further vegetation clearance in search for additional farmlands, new settlement units and grazing could eventually transform the initial extents of shrubs.
LULC change in the study catchment between 1995 and 2004
Land use and cover change matrix of the Gelda catchment (1995–2004)
Change from LULC 2004 (ha)
Farmland and settlement
Change from LULC 1995 (ha)
Farmland and settlement
Table 7 also revealed that reductions were observed in farmland and settlement, and bare land because the added areas from other LULC classes could not be adequate to compensate the losses. Exceptional shrinkage was observed in farmland and settlement cover by about 14.6% (263.78 ha/year) possibly due to tough measures taken by the government to restore areas which were under forests, shrubs, grazing lands and those farmlands not suitable for agriculture (Table 4). The dominant contributors of the existing decline in farmland and settlement was associated with the conversions of its initial extent into grasslands by about 25.4% (4125.97 ha) and shrubs by about 6.7% (1097.79 ha) despite some area was largely gained from grasslands (Table 7). The areas previously occupied by farmlands and villages were declined following refusal of forced settlement and inadequate reaction from the transitional government in early 1990s. However, tough measures on land restoration were taken at the end of this study period that substantially reduced areas occupied by farmlands. Despite the fact that bare land constituted a very small spatial extent in the watershed, its original extent was decreased as much as 24.9% at the rate of 10.5 ha/year (Table 4). The decline was contributed mainly by the conversion of the initial extent into grasslands by about 54.8% (208.8 ha). This indicated that once the area is out of production and physically unsuitable for either of human uses, the area were exempted from any human contact and eventually recovered largely into grasslands.
LULC change in the study catchment between 2004 and 2014
Land use and cover change detection matrix of the Gelda catchment (2004-2014)
Change to LULC 2014 (ha)
Farmland and settlement
Change from LULC 2004 (ha)
Farmland and settlement
Slight decline was observed in forest cover by 23.1% (28.8 ha/y) while the highest was in grazing lands by 75.65% (600 ha/year) between 2004 and 2014 (Table 4). These shrinkages were evident because some areas gained from other LULC classes were not adequate to compensate the losses from their initial extent (Table 8). Decline in forest cover was largely attributed to its conversion into farmland and settlement by about 43.5% (543.3 ha) and shrubs by about 8.5% (106.4 ha) despite some area gain from the classes of shrubs by 10.7% (102.6 ha), and farmland and settlement by 26.1% (250 ha). In this study period, various levels of vegetation clearance in search for farmlands and household consumption have possibly transformed the original forest cover into farmlands and shrubs. Similarly, reduction in grassland covers were mostly caused by conversion of its initial extent into shrubs by about 42% (3377.97 ha), and farmland and settlement by about 41.1% (3259.98 ha) despite some gains from other LULC classes. This was possibly associated to land encroachment for agriculture and land restoration which was not suitable for grazing into shrubs.
LULC change in the study catchment between 1957 and 2014
Rate of change of LULC for the past 57 years (1957–2014)
Farmland and settlement
Rate of changes
Major drivers of land use and cover dynamics
The LULC dynamics in the study area largely depend on dynamic relationships among population and policy/institutional factors, but the effect of natural factors such as climate over small area and short periods of time may not felt as such.
Although the overall demographic data for the study catchment was not possible to obtain following catchment boundaries, the data were compiled according to administrative structure where the catchment is almost entirely found. The demographic data were limited to three census reports of Ethiopia in 1984, 1994 and 2007; but LULC analyses were between 1957 and 2014. Thus, demographic data were used to see trends of population changes in the study area over larger portion of the study period so that comparison can be made possible among LULC change and population pressure. The data indicated that the total population of Dera wereda was increased from 204,962 in 1984; 212,341 in 1994 to 248,464 in 2007 at an average annual growth rate of 3.6 and 16.9% respectively (CSA 1991, 1995, 2008). This revealed that population pressure on the land resources increased the demand for farmlands, settlements, fuel wood, and construction materials. The census reports also indicated that most of the total population in the were da (>90%) resides in the rural areas where households largely depend on land resources as means of livelihood. This caused expansion of farmlands into shrubs, forests and grasslands; overgrazing; deforestation for household energy consumption and income; and declined arable land percapita in rural areas. These suggest that population growth is a major driving force in LULC dynamics of Gelda catchment. This is consistent with the previous studies in the highlands of Ethiopia (Woldeamlak 2002; Wubalem 2012; Hurni 1988; Mekuria 2005; Tsehaye and Mohammed 2015; Hassen et al. 2015). However, direct field observation and informal interview indicated that the scarcity of forest products for household consumption forced the local population to plant trees around homesteads and protect forests in areas not usable for agriculture in recent times. The expansion of farmlands and bare land in the study area were presumably attributed to the impacts of population pressure mainly in search of additional farmlands, overgrazing and poor farming practices. Sociopolitical influences, especially inse-curity of land tenure; disincentives among farmers for conservation programs; taking some land out of production and placing more pressure on existing farm and grasslands have discouraged farmers from investing in soil conservation practices since 1984 in the study area.
Institutional and policy factors
Ethiopia has undertaken many institutional and policy changes regarding land resources management following major changes in political and government structures in 1974, 1974 and 1991. These frequent changes in political and government structures were responsible for successive changes in land resource use and administrative frameworks in Ethiopia, which intern resulted in successive LULC changes in the study area. The major institutional and policy factors responsible for changes in LULC change were the downfall of the imperial regime followed by land reform of 1975 where farmlands were given to landless tenants confiscated from landlords, and clearing forest and shrubs. The forest restoration and plantations program of socialist regime since early 1980s using food-for-work program was another policy factor where success to date is rare due to lower local community involvement. The resettlement program between 1987 and 1990; civil war between 1990 and 1991; downfall of socialist regime; and the resulting legal vacuum in natural resource conservation attributed to the clearance of shrubs and forest cover. The 1997 land redistribution in Amhara region that aimed at ensuring social justice and responding to population change was another factor despite its failure to fully satisfy the ever increasing demand for farmlands and settlement.
There have been substantial LULC changes in Gelda catchment of northwestern highlands of Ethiopia driven mainly by population pressure institutional and policy factors. The existing expansions of traditional farming practices into grasslands, natural vegetations and marginal lands eventually led to a decrease in fodder availability and gradual soil quality deterioration. The decline in grassland forced the local community to keep their cattle on bare lands and shrubs, particularly during the cropping season. The institutional and policy reforms over the entire study period have contributed to changes the legal and policy frameworks of land resource management and ownerships in the country. These changes could have implications for sustainable agricultural resource management and the livelihood of the local community. As a result, off-farm activities and soil fertility improvement are essential to reduce the adverse impacts of population pressure on natural resource base. Improved land management practices such as applying soil and water conservation techniques and improved agricultural inputs could improve agricultural production. Likewise, local involvement in natural resource management and the existence of clear land tenure policies are critical for sustainable land use. Alternative energy sources for household energy consumption and environmental education are also imperative. Therefore, the change detection matrix analysis in GIS and remote sensing could provide useful baseline information to understand the spatiotemporal patterns of land use transitions and major contributors of LULC change caused by the major driving forces thereby sustainable land management planning is possible.
EEH has conceived of the study. He has also participated in the design of the study, carried out the data collection, GIS and remote sensing based analysis of data, and performed the statistical analysis. MA has participated in the sequence alignment of the draft manuscript. He also participated in its design and coordination, and helped to draft and edits the manuscript. All authors read and approved the final manuscript.
The authors are grateful to Addis Ababa University (Addis Ababa, Ethiopia) and University of Gondar (Gondar, Ethiopia) for their financial and operational support to conduct this research. This study was also made possible by a research grant awarded to the first author by Association of African Universities (Accra, Ghana).We also thank the local farmers in the study area for their cooperation and understanding during field work. The paper has been benefited largely from anonymous reviewers.
The authors declare that they have no competing interests.
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- Agarwal C, Green GM, Grove JM, Evans TP, Schweik CM (2002) A review and assessment of land-use change models: dynamics of space, time, and human choice. General Technical Report NE-297, Newtown Square, pp 1–61View ArticleGoogle Scholar
- Alemu B, Garedew E, Eshetu Z, Kassa H (2015) Land use and land cover changes and associated driving forces in north western lowlands of Ethiopia. Int Res J Agric Sci Soil Sci 5(1):28–44View ArticleGoogle Scholar
- Badege B (2001) Defforestation and land degradation in the ethiopian highlands: strategy for physical recovery. Northeast Afr Stud 8(1):7–26View ArticleGoogle Scholar
- Bürgi M, Hersperger A, Schneeberger N (2004) Driving forces of landscape change—current and new directions. Landsc Ecol 19:857–868View ArticleGoogle Scholar
- CSA (1991) The population and housing census of Ethiopia: results at a country level (1984). Office of population and housing census commission. Central Statistical Authority (CSA), Addis AbabaGoogle Scholar
- CSA (1995) The population and housing census of Ethiopia: results at a country level (1994). Office of population and housing census commission. Central Statistical Authority (CSA), Addis AbabaGoogle Scholar
- CSA (2008) The population and housing census of Ethiopia: results at a country level (2007). Office of population and housing census commission. Central Statistical Authority (CSA), Addis AbabaGoogle Scholar
- Dera wereda ARD office. (2013). Dera Wereda ARD office report of 2013. Anbessame, Amhara NRS, Ethiopia (Unpublished)Google Scholar
- Eleni Y, Wolfgang W, Michael E, Dagnachew L, Günter B (2013) Identifying land use/cover dynamics in the koga catchment, Ethiopia, from multi-scale data, and implications for environmental change. ISPRS Int J Geo Inf 2:302–323View ArticleGoogle Scholar
- Eyayu M, Heluf G, Tekalign M, Mohammed A (2009) Effects of land-use change on selected soil properties in the tara gedam catchment and adjacent agro-ecosystems, North West Ethiopia. Ethiop J Nat Res 11:35–62Google Scholar
- FAO (1997) The digital soil and terrain database of East Africa (SEA): notes on the Arc/info files, Version 1.0. Land and Water Development Division, Food and Agriculture Organization (FAO), RomeGoogle Scholar
- Driessen P, Deckers J (2001) Lecture notes on the major soils of the World. World Soil Reports 94 (eds). Food and Agriculture organization (FAO), RomeGoogle Scholar
- Getachew F, Heluf G, Kibebew K, Birru Y, Bobe B (2011) Analysis of land use/land cover changes in the Debre-Mewi watershed at the upper catchment of the Blue Nile Basin, Northwest Ethiopia. J Biodivers Environ Sci 1(6):184–198Google Scholar
- GSE (1996). Geological map of Ethiopia. Scale 1:2,000,000. Addis Ababa, Ethiopia. Ministry of Mines, Geological Survey of Ethiopia, second editionsGoogle Scholar
- Hassen MY, Mohammed A, Assefa M, Tena A (2015) Detecting land use/land cover changes in the Lake Hayq (Ethiopia) drainage basin, 1957–2007. Lakes Reserv 20:1–18View ArticleGoogle Scholar
- Hurni H (1988) Degradation and conservation of the resources in the Ethiopian highlands. Mt Res Dev 8(2/3):123–130View ArticleGoogle Scholar
- Hurni H (1998) Agroecological belts of Ethiopia: explanatory notes on three maps at a scale of 1:1,000,000. Soil Conservation Research Programme, Addis AbabaGoogle Scholar
- Hurni H, Kebede T, Gete Z (2005) The implications of changes in population, land use, and land management for surface runoff in the upper Nile basin area of Ethiopia. Mt Res Dev 25(2):147–154View ArticleGoogle Scholar
- Lambin EF, Geist HJ (2006) Land use and land cover change: local processes and global impacts. Springer, BerlinView ArticleGoogle Scholar
- Lambin EF et al (2001) The causes of land-use and land-cover change: moving beyond the myths. Glob Environ Chang 11:261–269View ArticleGoogle Scholar
- Lambin EF, Geist HJ, Lepers E (2003) Dynamics of land-use and land-cover change in tropical regions. Annu Rev Environ Res 28:205–241View ArticleGoogle Scholar
- Lillesand TM, Kiefer RW (1994) Remote sensing and image interpretation. Wiley, New YorkGoogle Scholar
- Mekuria AD (2005) Forest conversion–soil degradation–farmers’ perception nexus: implications for sustainable land use in the southwest of Ethiopia. Cuvillier Verlag Göttingen, Ecol Dev Ser, p 26Google Scholar
- Mohammed A (2011) Land use/cover dynamics and its implications in the dried lake Alemaya watershed, eastern Ethiopia. J Sustain Dev Afr 13(4):1–18Google Scholar
- Mohammed A, Le Roux PA, Barker CH, Heluf G (2005) Soils of Jelo micro-catchment in the chercher highlands of eastern Ethiopia: I morphological and physicochemical properties. Alemaya, EthiopiaGoogle Scholar
- Sharma A, Tiwari KN, Bhadoria PBS (2011) Effect of land use land cover change on soil erosion potential in an agricultural watershed. Environ Monit Assess 173:789–801View ArticleGoogle Scholar
- Sherbinin A (2002) A CIESIN thematic guide to land-use and land-cover change (LUCC). Columbia University, PalisadesGoogle Scholar
- Tsehaye G, Mohammed A (2013) Effects of slope aspect and vegetation types on selected soil properties in a dryland Hirmi watershed and adjacent agro-ecosystem, northern highlands of Ethiopia. Afr J Ecol 52:1–8Google Scholar
- Tsehaye G, Mohammed A (2015) Land use/land cover dynamics and their driving forces in the Hirmi watershed and its adjacent agro-ecosystem, highlands of Northern Ethiopia. J Land Use Sci 10(1):81–94View ArticleGoogle Scholar
- Veldkamp A, Lambin EF (2001) Predicting land-use change. Agric Ecosyst Environ 85:1–6View ArticleGoogle Scholar
- Verheye WH (2007) Factors affecting land use and land cover change, Volume 1. In: Briassoulis, land use, land cover and soil sciences (9). MytiliniGoogle Scholar
- Warra HH, Mohammed AA, Nicolau MD (2013) Spatio-temporal impact of socio-economic practices on land use/land cover in the kasso catchment, bale mountains, Ethiopia. Scientific Annals of “Alexandru Ioan Cuza” University of IAŞI, Volume LIX, no.1, S. II C, Geography series, 1–26Google Scholar
- Woldeamlak B (2002) Land cover dynamics since the 1950s in chemoga watershed, Blue Nile Basin. Mt Res Dev 22(3):263–269View ArticleGoogle Scholar
- Woldeamlak B, Sterk G (2005) Dynamics in land cover and its effect on stream flow in the chemoga watershed, blue Nile basin, Ethiopia. Hydrol Process 19:445–458View ArticleGoogle Scholar
- Wubalem T (2012) The status of forestry development in Ethiopia: challenges and opportunities. National dialog on sustainable agricultural intensification in ethiopia and its role on the climate resilient green economy initiative in Ethiopia July 23rd and 24th, 2012, ILRI Campus, Addis AbabaGoogle Scholar