1. Introduction
This paper explores the determinants and implied economic impacts of climate change adaptation strategies in the context of traditional pastoralism. Pastoralism is a source of livelihoods for millions of inhabitants in developing countries. Pastoral societies inhabit arid and semi-arid environments where climate change is supposed to increase the likelihood of a rise in the frequency and intensity of droughts and floods. The level and nature of their exposure is often believed to be different from those communities living in mixed agricultural systems, which often remain the central focus and policy priority areas of national governments. Pastoralist communities are generally expected to be among the most affected groups, and hence will need access to resources and services that help them cope with impending catastrophic shocks, protect their livelihood assets and increase their resilience [
1]. The adverse impact of climate change is thought to be more severe in developing countries because of their heavy dependence on natural resources and constrained capacity to adapt to climate-induced shifts. Climate variability and change is often recognized as a major threatening factor to food security in areas of the world that are largely dependent on rain-fed agricultural production systems [
2]. The poorest and marginalized communities are especially the most vulnerable group within these countries due to their very limited ability to embrace adaptive choices [
3]. Countries in the Horn of Africa are often considered to be among the most vulnerable, but are also considered to be the least prepared for adverse global environmental change in the word [
4]. In the Horn region, Ethiopia has been typically considered as a home of famine, especially beginning from the last three decades of the 20th century, principally as a result of increasing vulnerability to extreme events that relate to changing climatic conditions. The pastoralist peoples, inhibiting the low land areas of the country, with the harsh and precarious conditions of limited livelihood choices in their settings, have particularly become increasingly vulnerable to persistent poverty in recent decades partly due to their recurrent exposure to the adverse effects of climate variability and change.
Climate change is a key issue in any development debate seriously concerned with the future of pastoralism. The likely impact of predicted weather extremes even raises the question of the sustainability of pastoralism as a viable livelihood system. Brooks [
5] underlines that views on the impact of climate change on pastoralism are quite simplistic and polarized. The extreme of these is represented by the pessimistic scenario of the collapse of fragile pastoral livelihood systems and consequent massive outmigration of the destitute. Increased temperature and more critical drought conditions would likely erode the natural capital (resource) base of sustainable pastoralism which will be manifested though scarcity of pasture and water resources. This resource scarcity, it is argued, in addition to massive pastoral poverty, is considered to trigger severe resource competition and violent conflicts among pastoralist communities. In contrast, the more general notion is based on the long recognized feature of pastoralism as a system of adaptations. Pastoralists are thought to be natural adaptors provided that they are free from negative external interference and are able to inhabit an enabling policy environment of suitable support services [
6,
7,
8]. Pastoralist response in this case is based on an adoption of a variety of strategies. Nevertheless, despite this feature of pastoralism as a system of human creative adaptations to hostile climate factors of dryland ecosystems, pastoral livelihoods have rather become increasingly vulnerable to climate change impacts due to the eroded adaptive capacities of pastoralist communities as a result of prolonged marginalization and harmful external interventions, which are often generally exhibited by superficially imposed dissonant institutions, environmentally unsound programme implementations and bad governance.
Traditional pastoralism typically represents a resilient and unique system of adaptations in a dynamic process of unpredictable climatic variability and continuous human interactions with the natural environment in dryland ecosystems. Pastoral adaptations and climate-induced innovative coping mechanisms are strategically embedded in the indigenous social structures and resource management value systems [
1]. However, the case of global climate change, expressed in terms of increased temperature and shifts in patterns of precipitation, is a new challenge to the world of pastoralism. The possible negative welfare effect of global climate change is an added dimension to the already prevailing crisis in the pastoral livelihood system, which is substantially driven by non-climatic factors of internal and external pressures of change such as population growth, bad governance and shrinking rangeland areas lost to competing activities [
9,
10,
11,
12]. Therefore, the impact of climate change and variability on African pastoral systems could be severe because of the already prevailing exposure of being practiced under marginal environments of considerable water stress [
13]. The scale of climate change impacts may differ across regions, but it is quite crucial for research to focus on these fragile dryland environments in order to inform sound policy decisions.
Assessing the economic impacts of changing climatic conditions and their interactions with other driving forces of livelihoods vulnerability has remained a relatively neglected area of research in the context of pastoralist systems [
14]. The burgeoning literature on the assessment of the economic impact of climate change in agriculture has almost exclusively focused on crop agriculture and mixed farming systems [
15,
16,
17,
18]. Nevertheless, the issue of adverse long-term effects and persistent poverty implications of extreme weather shocks and associated multiple drivers has been a subject of recent investigation in our study area [
9,
19]. Also, Angassa and Oba [
20] point to external interventions and induced adaptation strategies, which are indicated to have triggered scarcities by undermining the efficacy of traditional strategies of natural resource management and patterns of land use, as significant drivers of vulnerability to catastrophic assets shocks during drought years. However, there is a need for more systematic inquiry into the nature and economic impacts of adaptation practices, the challenges of local adaptive responses, and long-term welfare implications of specific adaptation options in the context of traditional pastoralism. In addition to individual adaptation options ascertained at household level, there are several public measures and scattered efforts that can be identified in the context of the need to enhance pastoralist adaptive capacity to climate change. Not all individual adaptation measures to climate variability and public actions in pastoral areas are constructive and sustainable. Some can be destructive to the extent that they may increase pastoralist vulnerability. Therefore, a critical and systematic appraisal of current individual adaptive behavior and public measures in pastoral areas is essentially justifiable in view of the need to design policies and selectively promote innovative practices that can enhance pastoralist adaptive capacities. The focus of this paper is on the empirical analysis of individual household adaptation behavior and the implied impacts of embraced adaptation measures on household income in southern Ethiopian rangelands.
The rest of this paper is organized as follows. The next section introduces the study area and data sources.
Section 3 presents the extent of climate variability and pastoralist perception about long-term climate change in the Borana pastoral area of southern Ethiopia.
Section 4 provides a descriptive account of identified climate-induced pastoralist core adaptive strategies.
Section 5 is devoted to econometric analysis of the determinants and implications of selected adaptation strategies embraced by pastoral households in the study area. Concluding remarks are given in
Section 6.
3. General Trends of Climate Variability in Borana Rangelands
The general trends and pastoralist perception of climate variability in the study area are broadly assessed in this section. This is based on the important consideration that pastoralist adaptation choice is largely influenced by changing climatic conditions and underlying local perceptions. We start with the presentation of the nature and extent of climate variability based on the last four decades’ climatic data records of three major meteorological stations currently managed by the Ethiopian Meteorological Service Agency in the Borana region.
Table 1 shows a summary of the average annual rate of change in temperature trends recorded at the Negelle station. Very regular and consistent temperature records are available only for Negelle, which is the oldest and fairly consistently managed station in the region. Other stations have significant periodic interruptions and irregular temperature records of considerably missing data points. Therefore, based on Negelle station temperature records, the average temperature in the area has significantly followed an upward trend with an average annual rate of increase of 0.3% in the last 50 years. With an estimated annual rate of increase of 0.35% in the 1980–2012 period, this long-term change in average temperature appears to have been more pronounced in the recent decades (these growth rate figures, estimated by using the semi-long transformation model, are statistically significant at a 1% level). A further general picture of long-term trend in the average temperature is additionally provided in
Figure 1.
Table 1.
Average annual rate of change in temperature trends in Borana area.
Table 1.
Average annual rate of change in temperature trends in Borana area.
Station | Period | Average Annual Growth Rate (%) * |
---|
Negelle | 1964–2012 | 0.3 ψ |
1980–2012 | 0.35 ψ |
Figure 1.
Negelle station long-term average annual temperature trends. Source: Created based on Ethiopian Meteorological Service Agency records (unpublished raw data).
Figure 1.
Negelle station long-term average annual temperature trends. Source: Created based on Ethiopian Meteorological Service Agency records (unpublished raw data).
Figure 2 shows the erratic nature of rainfall in the Borana rangelands. All the three stations keep both temperature and precipitation records. The rainfall records are more regular and consistent than the observed irregular and scanty temperature data points particularly observed at Moyale and Yabello stations. It can be seen, especially from trends in the Moyale and Negelle station records, that the area has on the average experienced a long-term declining trend in mean annual rainfall in the last several decades. The highest rainfall record for the last four decades was 1382 mm in 1972 which was recorded at Negelle station. It was a year of the second highest (913 mm) record for Yabello station (the highest record for Yabello station in the last 30 years was 986 mm in 2012). The second highest rainfall record was observed a decade later in the early 1980s, which was 1309 mm for Negelle station in 1981 and 1171 mm for Moyale in 1982. The 1972 recorded rainfall level appears to have never been attained at the three stations for the past 40 years. The Borana pastoral area in the last four decades has on the average experienced rather a long-term decline in rainfall with increasing incidence of periodic droughts. The lowest rainfall at the three stations was in 1999, which was 309, 359, and 372 mm for Moyale, Negelle, and Yabello, respectively. It was a period of the catastrophic drought that ravaged the entire Borana region at the turn of the century.
Figure 2.
Trends in mean annual rainfall in three major stations. Source: Created based on Ethiopian Meteorological Service Agency records (unpublished raw data).
Figure 2.
Trends in mean annual rainfall in three major stations. Source: Created based on Ethiopian Meteorological Service Agency records (unpublished raw data).
The trends and long-term seasonal variability of rainfall conditions in the area are summarized in
Table 2. The region to a great extent appears to have experienced substantial declines in the main (
ganna) season rainfall over the last three decades. However, despite the general long-term declines in the region’s annual precipitations, the average rate of change for the short (
hagaya) season was positive in the 2000 decade as compared to the previous periods. The average increase in
hagaya rainfall has been particularly considerable to compensate for the average declines in the main season rainfalls at Yabello station. This apparently minor movement might have motivated a comment by one of our elder informants: “
hagaya and
ganna rains recently seemed to have moved in a direction of swapping their positions”. However, the feeble apparent gains in
hagaya rainfall have never been enough to sufficiently and reliably compensate for the considerable absolute declines in the
region’s main (
ganna) rainfalls.
With the observed rate of increases in the estimated coefficients of variations (CV), the general trends in the region’s average rainfalls rather appear to indicate a condition of shifts towards more unpredictability. Quite considerably, the variability of short (
hagaya) rainfalls has generally increased over the decades, which indicates their expected conventional unpredictability. The level of this variability is apparently higher at Yabello and Moyale stations, which have exhibited considerable average gains in their short season precipitations (
Table 2). Therefore, this monitorable general movement apparently signals that, in addition to the overall secular decline, the trends in annual rainfall in Borana rangelands might have taken a shift towards the direction of even more unpredictability.
Table 3 indicates that the ratio of short (
hagaya) rainfalls in the total annual precipitations has considerably increased in recent decades. The ratio of
hagaya rainfall in the total annual precipitation in the 2000s was 37%, and this was an increase from a decade average of 27% in the 1980s with an average rate of change of 17%. The upward trend in these ratios seemingly indicate the increasing significance of
hagaya season in the Borana rangelands though it is in fact largely a result of substantial declines in the main (
ganna) season rainfalls.
Table 2.
Trends in seasonal rainfall variability in Borana rangelands.
Table 2.
Trends in seasonal rainfall variability in Borana rangelands.
Station | Averages and Coefficients of Variation (CV) | Rate of Change (%) |
---|
1970s | 1980s | 1990s | 2000s | 2000s/1970s | 2000s/1980s |
---|
Negelle Station | | | | | | |
Annual | | | | | | |
Average (mm) | 899 | 788 | 651 | 654 | −10.1 | −4.5 |
Main season | | | | | | |
Average (mm) | 486 | 515 | 393 | 380 | −8.0 | −7.3 |
CV | 0.32 | 0.38 | 0.39 | 0.34 | 2.0 | −2.7 |
Short season | | | | | | |
Average (mm) | 316 | 241 | 197 | 224 | −10.8 | −1.8 |
CV | 0.36 | 0.30 | 0.46 | 0.42 | 5.3 | 8.8 |
Moyale Station | | | | | | |
Annual | | | | | | |
Average (mm) | * | 719 | 503 | 504 | * | −8.5 |
Main season | | | | | | |
Average (mm) | * | 478 | 223 | 246 | * | −15.3 |
CV | * | 0.45 | 0.34 | 0.38 | * | −4.1 |
Short season | | | | | | |
Average (mm) | * | 171 | 190 | 195 | * | 3.3 |
CV | * | 0.48 | 1.2 | 0.69 | * | 9.5 |
Yabello Station | | | | | | |
Annual | | | | | | |
Average (mm) | * | 530 | 541 | 604 | * | 3.3 |
Main season | | | | | | |
Average (mm) | * | 314 | 299 | 301 | * | −1.1 |
CV | * | 0.39 | 0.24 | 0.45 | * | 3.6 |
Short season | | | | | | |
Average (mm) | * | 133 | 158 | 195 | * | 10.0 |
CV | * | 0.48 | 0.70 | 0.58 | * | 4.8 |
Table 3.
Trends in the ratios of short (hagaya) rainfalls by decade.
Table 3.
Trends in the ratios of short (hagaya) rainfalls by decade.
Station | Mid to late 1960s Average | 1970s Average | 1980s Average | 1990s Average | 2000s Average | % Change 2000s/1980s |
---|
Negelle | 0.35 | 0.36 | 0.31 | 0.31 | 0.38 | 10 |
Moyale | na | * | 0.25 | 0.34 | 0.38 | 24 |
Yabello | * | * | 0.25 | 0.27 | 0.35 | 18 |
Average | * | * | 0.27 | 0.31 | 0.37 | 17 |
The foregoing analysis broadly reveals that, except for the recorded trends at Yabello station, there is an observed tendency of long-term declines in the region’s average annual rainfalls with increasing sign of unpredictability. Here, it may be important take up an important issue of ascertaining whether pastoralist perceptions of climate change correspond with the actually recorded climate variability in the region. Pastoral households were asked whether or not they have noticed any change in the climatic conditions in terms of changing trends in temperature and rainfall in the last two decades. Nearly 95% of the interviewed pastoral households (N = 281) perceived that the average temperature in the area has increased, while the average rainfall has reportedly decreased, in the last several decades. A clear deviation, however, was observed between local perception and recorded rainfall trends at Yabello station.
5. Analysis of Determinants and Impacts of Pastoralist Adaptation Choices
5.1. The Model
Our simple theoretical departure for the analysis of pastoralist response to long-term climatic variability and change is the notion of pastoral household utility maximization. Here pastoral households are assumed to make rational decision of choosing adaptation measure “m” over adaptation strategy “n” if the expected utility from the former option is greater than that of the latter adaptation option. That is if:
The empirical strategy is based on a range of major pastoral household adaptation choices identified and quantified during the field survey. Using a similar empirical approach to Di Falco
et al. [
18], here pastoralist adaptation to climatic variability is explored by adopting a framework of two-stages setting. (An alternative statistical approach to this specification is to consider those adaptation measures as polytomous choice categories [
17,
21] most commonly analyzed by using Multinomial Logit Models. However, the simple approach we have adopted here is recognized as being more useful in broadly assessing the impacts of adaptation choices in the next step). The pastoralist decision to implement an adaptation strategy (based on the assumption that it generates benefits) is modeled as a binary response outcome. The underlying response behavior in this case can be represented by unobserved (latent) variable (A
i*) capturing the expected benefits from adaptation choice with respect to not adopting, and specified as:
The observed adaptation option Ai = 1 if Ai* > 1, and 0 otherwise. The vector X broadly represents different groups of explanatory factors corresponding to household socio-economic characteristics, climatic variables and other factors such as institutional support services. Therefore, in the adopted first step, factors that significantly play a role in determining the probability of pastoral household adoption of specific adaptation strategies are examined using probit model estimation.
The next associated step roughly explores the effects of climate change adaptation measures on pastoral household income. This is applied by considering selected adaptation strategies of fairly strong connections with major sources of pastoral household revenues, the latter including milk and meat production and non-pastoral adaptations such as cereal cultivation and asset diversification. Predicted values of probit estimates in the first step are generated as a measure of probability of adoption and are included as a dummy variable (Ai = 1 if the identified measure is adopted by household i, and 0 otherwise) in the applied ordinary least square (OLS) model estimation.
Definition and descriptive statistics of the empirical model variables are provided in
Table 5. Selected major pastoral adaptation choices are dependent variables in the first stage estimation. The first category of variables in
Table 5 is associated with a vector of variables of household socio-economic characteristics embraced in Equation (2). These include age of household head (AGE), gender of household head (GENDER), household size (HHSIZE), level of educational (EDUCATION), and livestock size (LVSTKSIZE).
The second category refers to elements of a vector of climate variables represented by locality based approximations of temperature (MAXTEMP) and rainfall (RAINFALL) conditions. Here, in addition to the usual cross-sectional analysis problem of specifically entering individual household level rainfall and temperature observations, our case is found to be quite tricky and more daunting due to the mobile nature of traditional pastoralism. In order to clear this hurdle in the Borana case, we resorted to the unique traditional characterization of
warra (semi-settled)
versus fora (mobile) herd management system in Borana pastoralism. The Borana
warra herd unit is a core division of subsistence herds which is of limited (10–20 km radius) circular movement in the surroundings of semi-settled pastoralist encampments [
26,
29]. Individual household level temperature observations by site were then approximated by average recent records of relatively closer currently operating meteorological stations. The Moyale meteorological station, for example, is within 20 km distance of our Bokola survey site in the area. In other cases, extrapolated records of the fairly widely spread previous (now abandoned) substations of the Southern Rangelands Development Unit (SORDU) were additionally used. The rainfall data used in the empirical model estimation come from the dataset constructed by the Climate Prediction Centre of the National Oceanic and Atmospheric Association (NOAA), which are extracted based on grid measures of the surveyed sites.
Table 5.
Definition and descriptive statistics of model variables.
Table 5.
Definition and descriptive statistics of model variables.
Variable | Description | Mean | SD |
---|
AGE | Age of household head | 54 | 16.7 |
GENDER | Dummy for gender of household head, 1 if male; 0 otherwise | 0.86 | 0.40 |
HHSIZE | Household size | 6 | |
EDUCATION | Household head level of education in years | 0.28 | 1.1 |
LVSTKSIZE | Livestock size in a standardized unit (TLU) * | 12 | 17 |
SHKSURINDEX | Shock survival index (see text for explanation) | 1.12 | 1.02 |
EXTENVIST | Dummy for regular visit by government extension agent, 1 if yes; 0 otherwise | 0.71 | 0.46 |
FREQUTRAINP | Frequency of participation in government or NGO training & orientation programs (0 = none; 1 = a few times; 3 = frequently) | 1.2 | 1.1 |
CREDITACESS | Dummy for access to formal credit, 1 if yes; 0 otherwise | 0.16 | 0.36 |
MLOCALEADER | Dummy for membership in local government leadership structure, 1 if yes; 0 otherwise | 0.17 | 0.38 |
DISTDISTCAP | Distance from district capital (km) | 23 | 14.4 |
RAINFALL | Average annual rainfall (mm) based on NOAA dataset | 301.7 | 39.4 |
MAXTEMP | Maximum temperature based on extrapolated recorded temperature at stations closer to sample site | 29 | 2.65 |
PRANGESTATUS | Dummy for perceived range status in the locality, 1 if degraded; 0 otherwise | 91 | 29 |
AREACULTVD | Area cultivated in sangas (4 sangas = 1 hectare) | 2.3 | 3.3 |
WCRATIO | Workers-Consumers ratio in the household (household composition) | 0.5 | 0.2 |
The variable SHKSURINDEX (shock survival index) is included here in order to capture the effects of past recurrent exposure to climate-induced shocks in addition to the usual variables of current rainfall and temperature conditions. It is a ratio of current stock size to the highest reportedly attained pre-shock livestock holding multiplied by frequency of exposure to catastrophic shocks [
9]. The frequency of exposure is measured by the reported number of times the respondent pastoral household experienced drought-related substantial livestock losses in the past.
The other set of variables included in the empirical model are institutional support variables represented by access to regular extension visit (EXTENVIST), frequency of participation in organized government and NGO training and orientation programmes (FREQUTRAINP), and access to formal credit (CREDITACESS). Other included explanatory variables are household head membership in local government leadership structure (MLOCALEADER), distance from district capital (DISTDISTCAP) and perceived range status of most frequently used local range ecology (PRANGESTATUS).
5.2. Empirical Results and Discussion
Probit regression results of the determinants of pastoral household selected adaptation choices are presented in
Table 6. These are estimated functions of pastoral household adaptation choice decisions represented by the relationship specified in Equation (2). The estimated results generally indicate that the likelihood of pastoral household adoption of the selected major adaptation options is significantly explained by age, gender, wealth status, degree of pastoral household shock resilience, and climatic variables. It is found that the probability of adjustment in pastoral practices of increased mobility and adoption of more camels significantly decreases with age. This clearly signifies that it is the younger pastoral households that have more of the energy to move around the rangelands in the event of shock and climatic risks, and that the older generations of Borana pastoralists are likely to be more hesitant in embracing camel pastoralism than the recent cohorts. The strategy of asset diversification in the form of conversion of livestock assets into urban-based physical investments is, as expected, significantly explained by the size of livestock ownership. The likelihood of adoption of high-return adaptation measure is also found to be positively and significantly related to household head membership in local government leadership structure.
Table 6.
Probit regression results of pastoral household selected adaptation choices.
Table 6.
Probit regression results of pastoral household selected adaptation choices.
Explanatory Variables | Mobility | Drought-Tolerant Species (Camel) | Private Enclosures | Asset Diversification |
---|
Cereal Cultivation | Cereals & Fodder |
---|
AGE | −0.0152 *** | −0.0263 *** | −0.0122 * | −0.0131 ** | −0.0125 |
| (0.0053) | (0.0064) | (0.0070) | (0.0062) | (0.0088) |
GENDER | −0.0752 | 0.0236 | 0.8017 *** | 0.2979 | −0.7543** |
| (0.1935) | (0.2256) | (0.3049) | (0.2785) | (0.3404) |
HHSIZE | 0.0556 | 0.1141 ** | 0.0434 | 0.0513 | −0.0505 |
| (0.0435) | (0.0461) | (0.0458) | (0.0411) | (0.0615) |
EDUCATION | 0.0041 | 0.0548 | −0.1241 | −0.0632 | 0.1078 |
| (0.0679) | (0.0785) | (0.0978) | (0.0791) | (0.0930) |
LVSTKSIZE | 0.0359 ** | 0.0203 *** | 0.0020 | 0.0185 *** | 0.0910 *** |
| (0.0155) | (0.0078) | (0.0080) | (0.0069) | (0.0189) |
SHKSURINDEX | 0.3279 *** | 0.4314 *** | 0.1835 | 0.2048** | 0.0197 |
| (0.1122) | (0.1018) | (0.1188) | (0.1032) | (0.1330) |
EXTENVISIT | −0.3608 | −0.3852 | 0.4796 | 0.2595 | −0.2859 |
| (0.2276) | (0.2718) | (0.3597) | (0.3250) | (0.4433) |
FREQTRAINP | 0.1397 | 0.0121 | 0.2354 * | 0.2431 ** | 0.1290 |
| (0.0897) | (0.1046) | (0.1207) | (0.1060) | (0.1639) |
CREDITACCESS | −0.4384 | −0.5139 * | 0.5495 | 0.0708 | −0.7191 |
| (0.2718) | (0.2705) | (0.3425) | (0.2833) | (0.4654) |
MLOCALEADER | 0.1059 | −0.1941 | −0.3080 | 0.1301 | 0.7236 ** |
| (0.2589) | (0.2679) | (0.2996) | (0.2605) | (0.3341) |
DISTDISTCAP | −0.0156 | −0.0318 ** | −0.0241 * | −0.0269 ** | −0.0244 |
| (0.0111) | (0.0129) | (0.0142) | (0.0128) | (0.0227) |
RAINFALL | 0.0117 *** | 0.0238 *** | 0.0276 *** | 0.0208 *** | 0.0012 |
| (0.0037) | (0.0041) | (0.0044) | (0.0041) | (0.0069) |
MAXTEMP | 0.2901 *** | −0.0804 | −0.7609*** | −0.4560 *** | −0.3075 * |
| (0.1109) | (0.1182) | (0.1352) | (0.1069) | (0.1791) |
PRANGESTATUS | 0.0719 | 0.4131 | −0.7115 * | −0.5864 * | 0.2983 |
| (0.2852) | (0.3332) | (0.4228) | (0.3302) | (0.4653) |
CONSTANT | −11.389 *** | −4.961 | 13.306 *** | 6.183 | 7.301 |
| (4.199) | (4.288) | (4.641) | (3.979) | (7.038) |
Wald χ2(14) | 67.91 | 81.17 | 122.42 | 107.26 | 71.08 |
N | 281 | 281 | 281 | 281 | 281 |
Pseudo R2 | 0.22 | 0.31 | 0.56 | 0.32 | 0.56 |
The probability of adoption of increased mobility as a survival strategy in the growing circumstances of recurrent climatic shocks is very significantly explained by wealth status and level of climatic shocks survival. The poor and the stockless generally tend to settle for opportunistic cereal cultivation or move to peri-urban location in search of relief assistance and other non-pastoral opportunities than moving in the rangelands. It also appears that adaptation choice and capacity is rather more significantly explained by dynamically exhibited degree of pastoral household shock resilience, which is rather measured here by considering the degree of survival in recurrent exposure to climate-induced shocks as an alternative to using the levels of current temperature and rainfall conditions alone. This is quite important in the context of mobile pastoralism because in our case current temperature and rainfall conditions are rather found to be more logical and consistent in explaining the pastoralist recent involvements in dryland cropping than modification of traditional pastoral practices. It is quite logical to observe from the estimated relationship that increased mobility is significantly associated with high temperature. However, the apparently positive relationship between mobility and annual rainfall conditions in a specific locality is perhaps quite inconsistent with common expectations. Some of the respondents may have rather experienced inter-locality shifts in their current encampments while their response to the question of increased mobility considerably signifies their dynamic perception of relative trends in the recent past. The status of local range ecology and associated sustained availability of pasture are crucial factors for pastoral mobility rather than only current level of local rainfall conditions in specific localities.
In addition to the significance of age, the decision to adopt more camel is very significantly explained by the size of livestock ownership and degree of climate-induced shock survival. The recently increasing prohibitive cost of adoption of drought-tolerant species (camel) implies that it is only the wealthy households that can more productively diversify the composition of their herd species portfolios as a hedge against the current condition of increasing climate-induced risks of livelihood deteriorations. The estimated positive relationship between local rainfall conditions and the level of household camel holding rather largely indicates the observed less dominance of this species in the pastoral herd portfolio of sampled households from the more arid Dilo district predominantly characterized by small ruminant production in addition to cattle. The expected future trend is that the prevailing long-term declines in average rainfalls in Borana rangelands would generally imply the adoption of drought-tolerant livestock species such as camel, albeit the increasing restrictive pressure of soaring adaptation costs. However, the current status in camel holding is partly influenced by the experience of past tradition and the often observed location-specific predominance of camel adoption, which, in addition to the particular case of suitability of existing range ecology, is substantially shaped by the degree of Borana exposure to the breeding practices and experience of other adjacent camel rearing pastoral groups in the area.
The probability of practicing the recently growing pervasive strategy of private enclosures for cereal cultivation is negatively related to age, and positively associated with gender. The older household heads rather either stick to their conservative feelings about dryland tilling or significantly lack the required labor power for land preparations. Cereal cultivation in the Borana rangelands, as detailed elsewhere, is generally a gender-biased operation [
30]. The estimated results, as commonly expected, also indicate that pastoralist adoption of the practice of cereal cultivation decreases with level of aridity and increasing temperature. Correspondingly, in addition to level of aridity and temperature conditions, household range enclosure for the double purpose of cereal cultivation and fodder production is significantly explained by the size of stock ownership.
An important result in
Table 6 is that institutional support mechanisms such as rural credit access and regular extension visits appear to have no effect on pastoral household choice of the selected adaptation measures. This suggests, at least, the partial ineffectiveness of these institutions in southern Ethiopian rangelands. Perhaps, except for the health programs, the existing extension services are largely less development-oriented at the household level. About 39% of our survey respondents indicated to have received visits by government agents but a significant component of these contacts are largely for tax collection and for local political and security matters rather than effective developmental advice. The frequency of participation in organized orientation programs is significantly associated with private land enclosures for dryland farming, and for the double purpose of cereal cultivation and fodder production. This result is consistent with the fairly observed recent recommendations by some governmental and non-governmental agents for household stockpiling of hay required to minimize the problem of feed shortages encountered during dry periods. However, private rangeland enclosures for this purpose may significantly imply negative repercussions due to the inbuilt incompatibility of this measure with the more ecologically sound broad strategy of extensive pastoralism on communal pasturelands in dryland ecosystems.
The estimated model results in
Table 7 are presented in accordance with our further aim of the need to roughly explore the effects of selected adaptation strategies well associated with pastoral production and household income. Quite notably, the previously discussed remaining strategies of pastoralists increasingly resorting to low-return activity engagements are generally related to the tendency of dropping out of pastoralism [
31]. As it can be seen, the results indicate that, except for the strategy of private land enclosures for cereal cultivation, all other adaptation measures are found to be significantly positive for the achievement of increased net household income in Borana rangelands. Therefore, the strategies of increased pastoral mobility, preference for more drought-tolerant species (camel) and conversion of livestock capital assets into urban-based physical capital investments have considerable positive implications for sustainable household food security in the region. The estimated model results interestingly reveal the apparent incompatibility of the implications of these findings and current negative views on pastoral mobility and corresponding vigorous stance of planned pastoralist sedentarization. The estimated results rather suggest that increased mobility has more significantly positive food security implication for an average Borana household than sedentarized cereal cultivation. The relationship between household income and climate variables of increasing temperature and precipitation in the rangelands is found to be significantly negative. The estimated result of a negative relationship between precipitation and pastoral household income may well appear quite inconceivable. But it might be partly explained by the general tendency of a shift towards increasing use of fragile rangeland soils for a relatively low-return cereal cultivation, which could involve a negative repercussion of rangeland degradation and reduced livestock productivity [
20,
24]. However, for drawing a strong and valid inference, the predictions with respect to these variables of current temperature and rainfall conditions in a cross-sectional context may be fairly mooted. This is partly due to the possible complex productivity influences of the diverse range of ecological conditions of the Borana mobile pastoral mode of production, but it remains to be a matter of further investigation.
Table 7.
The relationship between net income and selected adaptation choices.
Table 7.
The relationship between net income and selected adaptation choices.
Explanatory Variables | Dependent Variable: Net Household Income |
---|
Mobility | Drought Tolerant Species (Camel) | Private Enclosures | Asset Diversification |
---|
Cereal Cultivation | Fodder & Cereal |
---|
Adaptation Choice | 4311.3 ** | 4838.9 ** | 2630.5 | 7932.1 *** | 13986.8 *** |
(1711.5) | (1933.3) | (1838 ) | (2073.6) | (3936.1) |
LVSTKSIZE | 874.9 *** | 886.3 *** | 910.7 *** | 869.5 *** | 776.2 *** |
(34.1) | (32.3) | (30.6) | (32.1) | (49.0) |
AREACULTVD | 330.8* | 338.5* | 292.7 | 165.7 | 371.5 ** |
(172.9) | (172.5) | (186.9) | (178.9) | (169.1) |
HHSIZE | 38.6 | −2.9 | 71.9 | 8.6 | 153.5 |
(215.5) | (218.8) | (217.5) | (211.9) | 210.7 |
WCRATIO | 7758.9*** | 6695.3 ** | 7190.8 *** | 7123.6 *** | 6979.9 *** |
(2571.6) | (2578.2) | (2587.3) | (2529.0) | (2539.2) |
RAINFALL | −68.9 *** | −73.2 *** | −67.7 *** | −76.9 *** | −54.2 *** |
(20.9) | (21.3) | (21.5) | (20.8) | (20.4) |
MAXTEMP | −1894 *** | −1452.5 *** | −1104.2 ** | −1405.4 *** | −1210.4 ** |
(520.7) | (471.8) | (496.9) | (462.6) | (464.8) |
CONSTATNT | 72,850.7 *** | 62,911.5 *** | 49,909.7 *** | 62,312 *** | 50,477.6 *** |
(19,985.9) | (18,911.5) | (19,017.9) | (18,449.7) | (18,433.6) |
F(7, 273) | 150.81 | 150.75 | 147.89 | 156.44 | 155.08 |
P-value | 0.000 | 0.000 | 0.000 | 0.000 | 0.000 |
N | 281 | 281 | 281 | 281 | 281 |
R2 | 0.79 | 0.79 | 0.79 | 0.80 | 0.80 |
6. Concluding Remarks
This paper examines household climate adaptation strategies and their implied impacts on pastoral household income in southern Ethiopian rangelands. The recorded trend of climate variability in the last four decades is found to correspond with pastoralist perception of climate change in the region. The average temperature fairly followed a general upward trend in recent decades while the existing rainfall records, in accordance with the pastoralist perception, substantially signify that the region has experienced secular declines in average rainfall with significant signs of more unpredictability.
It is quite naive to attribute the pastoral crisis in southern Ethiopian rangelands, and consequent pastoralist adaptation response mechanisms, entirely to a factor of climate variability and change. However, as discussed elsewhere [
9], the influences of climate-induced recurrent shocks have been profoundly sharp to aggravate the effects of a host of internal and external factors, including government interventions, which have dynamically implied shifts in pastoralist livelihood strategies. The pastoralist adaptive response mechanisms have generally involved the strategies of adjustment in pastoral practices and shifts to non-pastoral livelihoods. Despite the existing restrictive pressures, increased pastoral mobility still remains to be a viable strategy of sustainable pastoralism in the present context of climate-induced risks and pastoral livelihood vulnerability. In a related front, the Borana pastoralists appear to have gradually modified their traditional stance against camel pastoralism in recent decades as a result of the increasing need to diversify their herd portfolios in favor of drought-tolerant species. These adjustments in pastoral practices are apparently quite helpful in the sense that they are found to exhibit statistically significant positive implications for increased pastoral household income. However, the recent pastoralist growing interest to embrace drought-tolerant species (camel), in the prevailing circumstance of climate-induced growing local food insecurity, is evidently faced with the problem of soaring camel prices driven by competitive international market pressures. It is a critical trade-off which should be fairly considered by policy makers in designing regional food security strategies and current programme interventions.
The pastoralist non-pastoral adaptation strategies in recent decades are found to be highly dominated by the less rewarding competitive pressures of private rangeland enclosures for opportunistic cereal cultivation and growing involvement of the poor in low-return activities. Only a small percentage of the surveyed pastoral households have managed to convert their livestock assets into relatively high-return non-pastoral undertakings as an adaptive risk management response. The strategy of asset diversification, in the form of transfer of surplus from the pastoral economy to urban-based non-pastoral investment ventures, in the face of currently increasing challenges of climate-induced co-variate shocks, is a significantly desirable risk management and developmental option in the area. All the same, a serious gap in the present state of institutional services provided by external agents in the area is their critical inadequacy of offering commercially-oriented skill training and related rigorous capacity building assistance at the household level. The conventional wisdom is arguably inclined to present a case for existing support actions by external agents to be substantially directed to target the poor. However, it is also crucial to refocus attention to strongly emphasize wealthy and medium stock owners in core support interventions, given the existing reality of catastrophic co-variate shocks which could typically eat into the entire capital asset base of the pastoral mode of production and subsequent rise in the likelihood of widespread pastoralist destitution.
The predominant strategy of private land enclosures for cereal cultivation is seemingly consistent with the ill-informed government stance of pastoralist sedentarization though it is found to have potentially insignificant contribution to average pastoral household food security. However, government strategies that discourage pastoral mobility but promote range privatization for cereal cultivation in the present context of climate-induced recurrent shocks in southern Ethiopian rangelands would ironically negate the goal of achieving sustainable livelihoods in this naturally susceptible environment. Local administrators and community leaders should rather discourage opportunistic and harmful individual adaptation measures such as private rangeland enclosures by wealthy stock owners, an act that is quite inconsistent with the naturally extensive system of adaptation of traditional pastoralism.