3.1. Classification of vegetation cover change
The changes of rangeland vegetation cover from 1992–2019 are presented in Table 3, Figs. 5 and 6 below. In order to assess the changes from remote sensing maps, the total number of pixels for each vegetation cover change map (1992, 1995, 2000, 2005, 2010, 2015 and 2019) was recorded. Among the LULC change classes observed in Teltele rangeland, agricultural land, bare land and bush encroachment land increased, while forest, grassland and wetland on rangelands decreased from 1992–2019. The agriculture land showed an increasing trend of 15.2% (1992–1995), 1.8% (1995–2000), 0.3% (2000–2005), 3% (2005–2010), 19.3% (2010–2015) and 7.6% (2015–2019) with a net change of 39.8% (1992–2019) (Table 3). This means that grassland, natural forest and wetland mainly change into agricultural land at an alarming rate. This is due to the government's current land policies which encouraged the pastoral community to participate in agricultural practice in addition to the scarcity of livestock, since the frequent climatic changes, like drought, challenges the livestock sector and as well as the livelihood of the pastoral community. Therefore, the government encourages the community to reduce their livestock and keep them around their home area by conserving some part of grazing area in the form of ranch and transforming the other part into agricultural. This has caused the degradation of rangeland in the Teltele district. The bush land infestation is also one of the challenging issues on the Teltele rangeland and has changed most of the area into un grazing land covered with the dense bush. The rate of change was 1.4% (1992–1995), 2.4% (1995–2000), 0.1% (2000–2005), 0.5% (2005–2010), 0.4% (2010–2015) and 0.8% (2015–2019) with the net change of 5.5% (1992–2019). The infestation rate was high when the impact of climate change was harsh compared to the other period. From 1995–2000 and 2015–2019 the infestation rate was high; this is due to strong drought (El-Niño) which occurred on the Teltele rangeland in 1999 and 2016 respectively. On the side of agricultural land and bush land encroached area, some part of the land has become a non-functional bare area, which means that the covered rangeland has changed to an area which covered neither by grass vegetation nor crop species. The changing rate was high (5.9%) during the period from 1995–2000 and 2015–2019; this is due to the severe impact of the drought (El-Niño) during the year 1999 and 2016 respectively, followed by 2.5% (1992–1995), 1.4% (2000–2005), 2.1% (2005–2010), 2.7% (2010–2015) with a net change of 14.3% (1992–2019).
Table 3
Land use/land cover classes and changes from 1992–2019 in Teltele rangeland.
LU LC class | Land Cover (km2) | | | | Changes within periods (%) |
1992 | 1995 | 2000 | 2005 | 2010 | 2015 | 2019 | | 1992 -95 | 95 -00 | 00 -05 | 05 -10 | 10 -15 | 15- 19 | 1992-19 |
A | % | A | % | A | % | A | % | A | % | A | % | A | % | % | % | % | % | % | % | % |
AL | 98 | 0.95 | 115.5 | 1.1 | 118 | 1.15 | 118 | 1.1 | 121.5 | 1.2 | 150.5 | 1.5 | 162.9 | 2.5 | 15.2 | 1.8 | 0.3 | 3.0 | 19.3 | 7.6 | 39.8 |
FL | 1382 | 13.5 | 1355.1 | 13 | 1328 | 13.0 | 1320 | 12.9 | 1284 | 12.5 | 1251 | 12.2 | 1212 | 11.8 | -2.0 | -2.0 | − .6 | -2.8 | -2.6 | -3.2 | -14 |
GL | 1009 | 9.85 | 907.6 | 8.8 | 724 | 7.05 | 715.5 | 7.0 | 698.6 | 6.8 | 654 | 6.5 | 620 | 6.0 | -11.4 | -25.4 | -1 | -2.4 | -6.8 | -5.5 | -62.7 |
WL | 30.7 | 0.3 | 27.6 | 0.3 | 21.3 | 0.2 | 20.7 | 0.2 | 19.5 | 0.2 | 18 | 0.1 | 15.2 | 0.15 | -9.8 | -29.5 | -3 | -6.0 | -9.0 | -18.4 | -102 |
BL | 535 | 5.2 | 548.8 | 5.4 | 583 | 5.6 | 591.2 | 5.8 | 604 | 5.9 | 620.6 | 6.0 | 624.3 | 6.1 | 2.5 | 5.9 | 1.4 | 2.1 | 2.7 | 5.9 | 14.3 |
SL | 7201 | 70.2 | 7301 | 71 | 7482 | 73.0 | 7490 | 73 | 7528 | 73.4 | 7561 | 73.7 | 7622 | 74.3 | 1.4 | 2..4 | 0.1 | 0.5 | 0.4 | 0.8 | 5.5 |
Total | 10256 | 100 | 10256 | 100 | 10256 | 100 | 10256 | 100 | 10256 | 100 | 10256 | 100 | 10256 | 100 | | | | | | | |
Note
AL = agricultural land, FL = forest land; GL = grass land, WL = wetland, BL = bare land, SL = shrub land. The pixel number change to Km2 by using the resolution (300 m) or 0.09 km2.
Changes between the periods were calculated as:
Where, A = recent land use/ land area in Km2; B = previous area of land use/ land cover in Km2, and data from 1992 used as a base.
On the contrary, the rangeland area covered with natural forests, grassland and wetlands decreased during the period under study. The loss of grassland, forest and wetlands is mainly attributed to increased agricultural activities, bush infestation and expansion of bare areas, as illustrated on the remote sensing map (Fig. 6 and Table 3). Grassland decreased by 11.4% (1992–1995), 25.4% (1995–2000), 1.1% (2000–2005), 2.4% (2005–2010), 6.8% (2010–2015) and 5.5% (2015–2019) with a net change of 62.7% from 1992–2019 (Table 3). Wetland part of Teltele rangeland decreased by 9.8% (1992–1995), 29.5% (1995–2000), 3% (2000–2005), 6% 2005–2010), 9% (2010–2015) and 18.4% (2015–2019) with net change of 102% from 1992–2019. The net change of wetland indicated that more than half (50%) part of the wetland occurred during 1992 change to other land use type either agricultural land, bare land, bush encroached area or others. The most significant change in terrain observed in grassland and wetlands parts of Teltele rangeland occurred during the period from 1995–2000 and 2015–2019, this is due to climate change impact (El-Niño) that happened on the Teltele rangeland in 1999 and 2016 respectively. The natural forest part of the rangeland also decreased by 2% (1992–2000), 0.6% (2000–2005), 2.8% (2005–2010), 2.6% (2010–2015) and 3.2% (2015–2019) with a net change of 14% from 1992–2019. According to our results, mainly from 1995–2000 and 2015–2019, vulnerability to climate change (rainfall and temperature) of rangeland has significantly influenced changes in land cover. The rainfall trend in the study area has a significant impact on the rangeland degradation and also on the livestock dynamics on the Teltele rangeland area. This means that due to the shift from wetland to other land use part like agricultural and infested with bush plant species, water scarcity was currently one of the major problems in the study area. Thus, resulted in the decline of the livestock.
3.2. Land use and land cover change transition matrix from 1992–2019
The rate of change trend has shown periodic fluctuations in the Teltele rangeland area. The LULC transitions are the result of either natural factor or human mismanagement of resources during the last almost three decades of the study period. In order to calculate the transition matrix for our case, we overlaid the remote sensing map of 1992 to that of 2019 to generate the matrix which was used to calculate the area of gains, losses and persistence between LULC types [43]. The LULC change directions for the study area from one type to another that have been calculated using Microsoft excel are shown in the transition probability matrix (Fig. 7 and Table 4) below.
The values indicated in bold color across the table indicate that the part of LULC type staying unchanged from one type to another from 1992–2019, whereas the rest of the value indicate that LULC changed from one type to another within a time interval from 1992–2019. The change detection statistics showed that over 28 years (1992–2019), 35.842% of the grassland, 47.9% of the wetland, 9.8% of the forest land, 1.9% of the agricultural land, 2.8% of the bare area, and 0.2% of the shrub land area were changed to other LULC classes, where we compared the LULC type identified in1992 with 2019 (Table 4). This indicates that only 64.2% of grassland, 52.1% of wetland, 90.2% of forestland, 97.2% of bare land, 98.1% of agricultural land and 99.8% of shrub land remained within the same LULC types in 2019. The major change was observed in grassland, wetland and forestland area and mainly transformed to agricultural land, bare land and shrub land LULC types (Table 4 from 2019 year), which is similar to the findings of [44]. As shown in Fig. 7, the majority of grassland, wetland and forestland have decreased (negative change), whereas the agricultural land, bare land and shrub land have increased (positive change). This indicated that in 2019 (nowadays) the rangeland has degraded due to factors like expansion of farming practices, infestation of bush and shrub invasive plant species, and bare area expansion due to factors like flooding and high wind (climate change) in combination with different anthropogenic factors.
Table 4
Land use and land cover change transition matrices from 1992–2019
| 2019 |
| Classes | AL | | FL | | GL | | WL | | BL | | SL | | G. Total | |
| A(km2) | A (%) | A(km2) | A (%) | A(km2) | A (%) | A(km2) | A (%) | A(km2) | A (%) | A(km2) | A (%) | A(km2) | A (%) |
1992 19 92 | AL | 96.18 | 0.94 | 0.59 | 0.006 | 0.11 | 0.001 | 0 | 0 | 0.1 | 0 | 0.43 | 0.004 | 98 | 1.0 |
FL | 12.56 | 0.16 | 1,246.6 | 12.15 | 0.12 | 0.001 | 0 | 0 | 58.4 | 0.57 | 64.28 | 0.626 | 1,382 | 13.50 |
GL | 7.98 | 0.08 | 0.314 | 0.003 | 647.31 | 6.31 | 1.6 | 0.02 | 41.93 | 0.41 | 309.38 | 3.016 | 1,009.00 | 9.8 |
WL | 8.39 | 0.08 | 0 | 0 | 5.8 | 0.056 | 16 | 0.16 | 0.11 | 0.001 | 0 | 0 | 30.7 | 0.3 |
BL | 16.31 | 0.16 | 0.04 | 0.003 | 0 | 0 | 0.4 | 0.003 | 520 | 5.07 | 0 | 0 | 535 | 5.2 |
SL | 9.19 | 0.1 | 3.82 | 0.04 | 0.66 | 0.005 | 0 | 0 | 0.18 | 0.002 | 7,186.96 | 70.07 | 7,201.00 | 70.2 |
G. Total | 150.61 | 1.52 | 1,251.40 | 12.2 | 654 | 6.34 | 18 | 0.18 | 620.72 | 6.05 | 7,561.50 | 73.73 | 10,256 | 100 |
Note
AL = agricultural land, FL = forest land, GL = grassland, BL = bare land, SL = shrub land, WL = wetland G. total = grand total, A = area.
The major factors related to the growing challenges of maintaining a livestock-based livelihood system in the face of changing land use and recurring droughts [45]. However, Pastoralists in the study area are conscious of the potential threat of invasive plant species and often, the removal of most shrubs and trees not preferred by livestock on their rangeland had negative impact on the native grass species [46].
3.3. Forage biomass production dynamics
The present study was tried to assess the biomass production status of forage grass species in Teltele rangeland area using different land cover types. According to the results, the total dry biomass production across all land use types was 3,094 and 1,090.6 kg/ha from grassland, 178 and 101 kg/ha from agricultural land, 1,907 and 475.6 kg/ha from forestlan241 and 119 kg/ha from shrubland, 97.2 and 19 kg/ha from bare land and 1,978.3and 483.7 kg/ha from wetland were recorded during wet and dry season respectively (Fig. 8). When we have found seasonal impact in all land use types 64.8% (grass land), 43.3% (agricultural land), 75.1% (forest land), 50.6% (shrub land), 80.5% (bare land) and 75.5% (wet land) more or higher dry biomass production during the wet season as compared to the dry season.
Rainfall is the main determinant factor for forage production in all land use type [47, 48]. When we have seen the amount of forage in different land use/cover types, the grasslands had the highest average amount of forage biomass of 2,092.3 kg/ha followed by wetland with 1,231 kg/ha, forest with 1,191.3 kg/ha, shrub land with 180 kg/ha, agricultural land with 139.5 kg/ha and bare land with 58.1 kg/ha (Fig. 8). This source of variation and dynamics of the forage biomass in the Teltele rangeland is due to a great influence of land use land cover change on the quantity of dry biomass recovered as well as the quantity of fresh weight forage in a given area. Further, the results showed that there was a significant interaction between the season and land cover types with forage biomass production dynamics in the study area and this result is in agreement with [49, 50]. From this we can understand that transition from grazing area (grassland) to other land use type had a significant impact on the reduction of forge biomass production and this was the current major problem on Teltele rangeland resulted to the decline of livestock and scarcity of income in the pastoralist livelihood. The expansion of agricultural land, bush land and bare land area have harmful effects on the forage production dynamics, but the expansion of agricultural land is more problematic in our study site, which is consistent with the data reported by [47, 51].
3.4. Linkage of forage biomass with NDVI value
The value of the normalized difference vegetation index (NDVI) of the general Teltele rangeland showed that, while the annual rainfall was high the NDVI value was high. These values were higher in 2004 (0.8628 and 0.1023) and lower in 2000 (0.7826 and 0.0943) (Fig. 9). The relatively high NDVI value was observed, when the annual rainfall was high and in contrary the annual temperature was low. In addition, if the rainfall pattern was good, the forage biomass production was showed a better result as compared with those years with lower annual rainfall. There is generally a link between the value of aboveground forage greenness (NDVI) and forage biomass and the linkage varied with the season and land use/cover types (Fig. 10).
This implies that there is a direct correlation between rainfall, vegetation greening and biomass production in Teltele rangeland. If the rainfall was high, the vegetation cover of rangeland would be better as compared to the period when the rainfall was low or drought and from this, it can be understood that the greenery was also highly related with the losses of vegetation cover. Our result, directly in line with the data reported by [4]. The overall rangeland vegetation cover analysis and change detection showed remarkable grassland vegetation cover changes across the study site. The greatest change was the decrease in the grassland and wetland proportion of rangeland vegetation and the increase in the cropland and bush infested areas.
The above (Fig. 10), indicates that the NDVI value from 1992–2019 has shown both decreasing and increasing trend. The NDVI value of agricultural land, forestland and shrub land showed an upward trend from 1992–2019, whereas the NDVI value of bare land, wetland and grassland showed a downward trend. The lowest NDVI value was recorded in 2000 across almost in all LULC types followed with 2019. This is because of the severe drought (El-Niño) occurred in 1999 and 2016 respectively and the scarcity of forage was also observed in this time and this indicates the direct linkage of NDVI value with forage biomass production at certain grazing sites. As we have seen from Figs. 6 and 7 and Table 3, the LULC types of agricultural land, shrub land increased due to change in some grassland, forestland and wetland and the NDVI value also showed an upward trend. This told us that the greenery of those areas was better compared with other LULC types from 1992–2019. The trend of the NDVI value of agricultural land use type was 0.621(1992), 0.620 (1995), 0.618 (2000), 0.651 (2005), 0.635 (2010), 0.664 (2015) and 0.668 (2019) with a net change in NDVI value increased by 0.047 (6.9%) from 1992–2019. The NDVI modified values of Shrub land were 0.626, 0.624, 0.631, 0.669, 0.673, 0.695 and 0.698 for the year 1992, 1995, 2000, 2005, 2010, 2015 and 2019 receptively with a net increase value of 0.072 (11.5%) compared 1992 with 2019. NDVI values of Forest land use also showed an increase value 0.589, 0.591, 0.593, 0.616, 0.650, 0.666 and 0.667 for the year 1992, 1995, 2000, 2005, 2010, 2015 and 2019 respectively with a net increase value 0.078 (13.2%) between 1992 and 2019. This is not related to the forest land, but rather indicates that the forest species found in 2019 showed better greenery performance compared to the forest found in 1992, even though the area coverage declined and changed to other types of land like agricultural land and shrub lands. When we have seen the change in NDVI value for grassland, the wetland showed a downward trend. For grassland the NDVI values were 0.538, 0.517, 0.499, 0.477, 0.463, 0.456 and 0.445 for the year 1992, 1995, 2000, 2005, 2010, 2015 and 2019 respectively with a deceasing NDVI net value of 0.093 (17.3%) as compared 1992 with 2019. The NDVI values of wetland were 0.467, 0.428, 0.305, 0.377, 0.361, 0.353 and 0.354 for the years 1992, 1995, 2000, 2005, 2010, 2015 and 2019 respectively with a decreasing NDVI net value of 0.113 (24.2%). From this we can understand that both the grassland and wetland in Teltele rangeland have been replaced by other land use types and that the grassland greenery and the amount of water have been highly affected by climatic and anthropogenic factors. The forage biomass production showed a decline pattern from 1992–2019, according to the data obtained from the respondent (Table 5) and filed data (Fig. 8) due to the different driving factors and this is also directly related with the NDVI values. The significant linkage observed between NDVI and LULC changes, was used to estimate the forage biomass production trends across the rangeland compared to each LULC type [51, 52, 53].
3.5. Socio-Demographic Characteristics of Respondents
The gender, occupation and level of education of the respondents were some of the main demographic characteristics that the respondents considered for this study.
From the above (Fig. 11), we can understand that the gender proportion also took into account and included 75% of males and 25% of females of the total number of participants. This distribution made it possible to understand the perception and coping method dynamics of forage production and of male and female pastoralists. The majority of the respondents (39.2%) were aged between 31–40 years followed by 51–60 years (23.3%) and the age distribution used to evacuate the level of understanding of the general pattern of the study area and the change trend of both forage production and LULC change types during the study period from 1992–2019. Then, the level of education is one of the basic factors on the socio-economic practice within a family and as we have seen from the above figure, the majority of pastoralists (46.7%) were illiterates followed by primary education (33.3%) level. This is because of lack of infrastructure and awareness in the pastoral community based on the data obtained from the respondents and, to some extent, the situation has occurred in the same way with other parts of the country. As a result, most of the livelihood community that depends on livestock occupation has been dispossessed, and this was the major factor causing most of the pastoralists source of income to depend on livestock rearing (54.2%), followed by the management of their own business alongside (20%). In general, from the results of the focus group discussion interviews, we can understand that the introduction of privatized resources (enclosures) had caused shortages of communal grazing areas and limited animal mobility. Thus, the situation affected the socio-economic structure and encouraged pastoralists to diversify their livelihoods with crop production because livestock had become uncertain, which causes the major factor in LULC change of grass land to agricultural land. This result directly related with the data reported by [4].
3.6. Driver of change of vegetation land cover and forage biomass
According to the data obtained from group discussion and interviews, the major drivers which influenced the change in land use-land cover and forage biomass production dynamics in Teltele rangeland, the bush infestation ranked as the primary reason (25.8%), followed by drought (20%) and expansion of agricultural practice (15%), increment of the population both human and livestock in the district (12.5%) without additional land provided (Table 5). Government policies have also had their own impact on the livelihoods of pastoralists, in Teltele, which promote the transformation of rangeland into cultivated land and restrict the movement of pastoralists who were traditionally used to coping with the impact of climate change. And also, existence of different insects that eat and damage the forage species (6.7%) and poor pastoralist interaction are also another driving force for change of land use/cover and also forging biomass product in the study area. But there is still a big gap under the term of land use/cover change factors, rather the pastoral community liked that it was due to God's plan and to nature which could be intended to punish us. This was an indicator of community’s low awareness of the climate change with which the whole world is grappling with and our data are consisted with the data reported by [54]. In addition, undermining traditional land use practice also have a direct impact on LULC changes in Teltele [55, 56, 57]. Local communities claimed that traditional (customary) laws had become weak and that this has contributed to the observed LULC changes in the area. For example, rotation programs for seasonal grazing areas had been planned and maintained for the specified communities for extended periods [58]. In general, regarding to the Ethiopian's land-use policies and plans, a paper recently presented at the annual World Bank conference noted that because of a lack of a coherent policy use of land, the deterioration of land resources has been documented in the country [59, 60], which is similar to the opinions expressed by the respondents.
Table 5
Pastoralist perception related to drivers that cause land use/cover and forge biomass change in Teltele rangeland.
No. | Driving factors | Number of respondents | Percentage (%) |
1. | Drought | 24 | 20 |
2. | Increase population number | 15 | 12.5 |
3. | Poor social- interaction | 6 | 5 |
4. | Bush infestation | 31 | 25.8 |
5 | Agricultural expansion | 18 | 15 |
6. | Government policies | 13 | 10.8 |
7. | Insects and disease | 8 | 6.7 |
8. | Gods plan and nature | 5 | 4.2 |
| Total | 120 | 100 |
For sustainable use of pastures in the district of Teltele, an awareness of the pastoral community on land use policies, respectful of the environment and regulating the growth of the human and animal population, was absolutely necessary.