1. Introduction
There is substantial evidence that the mean and extremes of climate variables have been changing in recent decades and that rising atmospheric greenhouse gas concentrations could cause such trends to intensify in the near future [
1]. According to [
1] the case in Africa will be more pronounced than the global average, suggesting warming in all seasons. Studies have reported high variability in rainfall and associated adverse effects of rainfall changes in East Africa [
2]. A study on climate change in Tanzania by [
3] reported a consistent rise in night-time temperatures (Tmin) (0.31 °C/decade) for over fifty years in the Northern Highlands zone of Tanzania.
As temperature increases, its impact on agricultural crops is expected to be remarkably felt with consequences for millions of smallholder farmers, including an increasing burden of agricultural diseases and insect pests. Cash crops such as coffee will be the most affected by climate change [
4]. As already pointed out by [
3] a 1 °C rise in mean minimum (night-time) temperature will cause an annual yield loss of approximately 137 kg of coffee ha
−1 in northern Tanzania.
Coffee is one of Tanzania’s largest export crops [
5], contributing 24% to the annual agricultural foreign exchange earnings and significant tax revenue. The crop contributes about 4% to gross domestic product (GDP), generating an average of US
$100 million annually [
5]. The coffee sub-sector also supports the livelihoods of over 450,000 farm families in 15 regions directly, and over 2.4 million people employed in its value chain indirectly [
6]. The average smallholder coffee productivity ranges between 250 and 300 kg/ha, which is very low compared to the potential yield of over 1000 kg/ha. We hypothesize that climate change may be behind the decline of coffee yields in Tanzania, thus putting coffee production and the livelihoods of coffee farmers at risk [
6]. This is because decrease in rainfall, especially the long rain season and increase in temperature negatively affects the expansion stage, during which rainfall is required to sustain berry development [
3]. Furthermore, drought and increase in temperature results in fruit abortions, increased bean defects, reduced berry growth, and acceleration of ripening, leading to a reduction in coffee yield and quality [
3]. Despite the prevailing trend of decreasing productivity, coffee still makes a significant contribution to smallholder livelihoods that produce 95% of coffee in Tanzania [
6].
Therefore, a better understanding of climate change and variability by smallholder farmers is necessary for designing adaptation strategies and policies to deal with the impacts of climate change on the Tanzanian coffee sub-sector, where 95% of the produced coffee is grown by smallholder farmers. The understanding largely targets the smallholder farmers who are highly vulnerable to climate change because most depend on rain-fed agriculture, cultivating in marginal areas, and lack access to technical or financial support that could help them invest in more climate-resilient agriculture. Different climatic studies show that sub-Saharan Africa is among the worst impacted region by the climate change and thus, a better understanding of how farmers view climate issues is an imperative step toward improving resilience [
7,
8]. Therefore, it can be premised that perceived personal experiences could affect climate change belief and the corresponding adaptation measures taken. It is evident that in areas where farmers lack awareness and knowledge about climate change, their vulnerability has been increasing, causing poor yields, food shortage, and poverty [
9].
Different studies indicate that smallholder farmers have been responding to climate change impacts through a range of interventions, including agronomic practices such as planting shade trees, pruning, planting drought-tolerant varieties, and application of organic fertilizers [
4,
10]. Some researchers have analyzed how farmer’s perceived climate change in Tanzania. [
10], investigated whether or not smallholder farmers in Tanzania perceived climate change across four regions: Iringa, Dodoma, Morogoro, and Tanga. Other studies by [
9,
11] compared smallholders’ perception of climate change with meteorological data across different agro-ecological zones. These studies suggest that farmers have already perceived change in climate conditions. However, these studies were mainly done in arid and semiarid regions of Tanzania where coffee is not the main crop, and when done in Northern and Southern Highland zones, coffee was not taken into account. A study by [
12] explored the perceived impacts of climate variability on coffee and banana farming in the highlands of Moshi rural District. The only drawback from this study was that it did not analyze factors influencing perception of climate change. Different scholars have indicated that the adoption of a particular adaptation method by individual households is influenced by several factors; e.g., in Ethiopia, [
13] and Uganda, [
14] found that farmers’ education, access to extension services and credits, climate information, social capital, and agro-ecological settings had a great influence on farmers’ choice of adaptation strategies to climate change. In Tanzania, [
9] indicates that farmers’ knowledge on climate change is a good base for undertaking effective adaptations. However, farmers’ perceptions of climate change are contextual and location-specific as societies differ in culture, education, demographics, resource endowments, and biophysical and institutional characteristics. This heterogeneity influences the way they perceive changes in their local climate and the way they respond to the change [
15]. Therefore, adaptation strategies of the farmers are linked with their perception of climate change and its impacts [
16].
Therefore, the current study contributes to the rapidly advancing climate change and farmers’ perception literature by providing practical evidence of the climate trends according to farmers’ perceptions and factors affecting perception in the two major Arabica coffee-growing areas of Tanzania. The results will also be used as one step toward the formulation of climate change adaptation strategies specific for coffee in Tanzania and beyond. The research explores the possibility of increasing coffee production sustainably through improved agronomic practices for adaptation to climate change in the Northern and Southern Highlands of Tanzania by assessing farmer’s perceptions and determining which factors influence their perceptions.
3. Results
3.1. Characteristics of the Households
Among the 242 sampled households, 90% were headed by men and 10% were headed by women. Respondents from Northern Highlands zone were of the age group between 41 and 70 years, while those of the Southern Highlands zone was dominated by those between 41 and 60 years (
Appendix A,
Table A1).
Chi-square results indicate that variations in farmer’s age across the districts were significant, χ2(26, N = 242) = 30.98, p < 0.05. The land-holding size also significantly varied across the districts χ2(26, N = 242) = 22, p < 0.01. The majority of the respondents from the Northern Highlands zone had a farm size between 0.5 and 1ha, while those from the Southern Highlands zone had farm sizes between 1 and 2 ha. The study also showed significant variations (p < 0.05) of the respondent’s education level between the districts, χ2(36, N = 242) = 62.13, p < 0.05. On the other hand, respondents had farming experience between 20 and 39 years with significant variations χ2(36, N = 242) = 26.5, p < 0.05 among the districts.
Results also indicate significant variations between male and female respondents in terms of time aware of climate change (
p < 0.1) and sex of the household head (
p < 0.01) (
Table 3). There were also lack of significant variations (
p > 0.05) in terms of education level, access to climate information and extension services between male and female respondents.
Similarly, in the Northern Highlands zone, the Chi-square test indicated a lack of significant variations (
p > 0.05) in terms of education level and access to extension services between male and female respondents. However, significant variations between male and female respondents were observed in the time aware of climate change (
p < 0.05), sex of the household head (
p < 0.01), and access to climate information (
p < 0.1)(
Table 4). Most of the respondents (89%) were aware of climate change, while 11% did not know what climate change is. Among the subset of 89%, 146 (91%) of the respondents were from the Northern Highlands and 69 (85%) from the Southern Highlands.
Significant variations between time aware of climate change, sex of the household head, access to climate information and the perceptions of temperature increase and rainfall decrease were also observed in the Southern (
Table 5) and Northern (
Table 6) Highlands zones. Furthermore, out of 242 respondents, 79% had access to climate information mostly through media such as TV, radio, and mobile phones. On the other hand, there were significant differences (t = 1.9367,
p < 0.01) among farming households with access to climate information in the Northern Highlands zone (76%) as compared to those in the Southern Highlands zone (86%). Among the 242 respondents, 163(67%) farmers perceived climate change by a way of change in intensity of the climate variables (increase in temperature and decrease in rainfall). There was also significant difference (t = 7.636,
p < 0.01) between respondents with positive perceptions of climate change (increase in temperature and decrease in rainfall) and those with negative perceptions of climate change. However, there was no significant difference (t = 1.0316,
p > 0.05) between farmers with positive perceptions of climate change in the Northern (70%) and those from the Southern Highlands zone (63%).
3.2. Comparing Smallholder Farmers’ Perception with Meteorological Data
Farmers’ perceptions were compared with the results of the historical trends from meteorological data.
Figure 3 shows farmers’ perceptions of changing in rainfall amount categorized based on their respective districts. Many famers (above 70%) felt declining rainfall in their areas, with the exception of farming households from Mbinga districts where only 62% had a similar feeling of rainfall decline. Looking at the meteorological data from two districts one from Northern Highlands zone (Hai) and another from the Southern Highlands zone (Mbozi), we find that approximately half of the years within the study period experienced below average annual rainfall.
The average rainfall amount for Lyamungo was 1447.79 mm, while the highest average annual rainfall was 2194 mm recorded in 2006 and the lowest was 670 mm recorded in 1989. For the case of Mbimba, the average rainfall amount was 1342.79 mm, the highest average annual rainfall was 1693 mm recorded in 1994, while the lowest was 630 mm recorded in 1981.
Figure 4a,b reveal that there is persistent high variability in annual rainfall based on a 5-year moving average. The 5-year moving average trend lines are not consistent throughout the 40-year period. The RAI for Lyamungo indicates that in the first and second decades, only five years respectively recorded an average rainfall above the average for the entire period. In the third decade and fourth decades, only 4 and 3 years respectively recorded an average rainfall above the average of the 40-year period. On the other hand, the RAI for Mbimba reveal that in the first and second decades, six years recorded an average rainfall above the average for the entire period. In the third decade and fourth decades, only 3 and 2 years respectively recorded above-average rainfall of the 40-year period. Hence, the fourth decade (2009–2018) was the driest of all four decades in both sites.
The majority of coffee farmers (more than 70%) from both the Northern and Southern Highlands felt an increase in temperature with the exception of Mbinga district, where only 67.7% of farmers perceived an increase in temperature (
Figure 5). In the study period, the mean temperature for Lyamungo and Mbimba were 19.85 °C and 18.76 °C, respectively. Temperature values for the 40-year period were erratic, as indicated in
Figure 6a,b. The highest average temperature for the four decades at Lyamungo was 20.47 °C, which was recorded in 2012, while the lowest for the period was 18.45 °C in 1979. At Mbimba, the highest average annual temperature was 20.5 °C recorded in 2010, while the lowest was 17.45 °C recorded in 2001. The yearly averages at Lyamungo (Hai district) from 2003 to 2018 were all above the average, while at Mbimba (Mbozi district), they were above from 2005 to 2018 for the 40-year period under study. Hence, the mean temperatures at Lyamungo (Northern Highlands zone) and Mbimba (Southern Highlands zone) have been increasing during the study period.
3.3. Perceived Impacts of Climate Change on Coffee Farming
Farming households noted climate change impact in terms of reduction of coffee yield (89%), increased crop insect pest (79%), increase crop diseases (63%), late coffee flowering (63%), and crop failure due to water shortage (59%). Variations in climate change impacts across the two zones were significant (
p < 0.05) except for reduction in coffee yield (
p > 0.05) (
Table 7).
Another climate change impact pointed out by coffee farming households was prolonged harvesting period, which significantly varied, χ
2(9, N = 242) = 49.85,
p < 0.01 across the two zones (
Figure 7).
On the other hand, there were significant positive associations (
p < 0.05) among the increase in temperature, decrease in rainfall, and most of the climate change impacts mentioned by respondents (
Table 8). There was also a significant negative association (
p < 0.05) between increases in coffee insect pest and diseases with reduction in rainfall. However, a lack of significant association (
p > 0.05) between late coffee flowering and increase in temperature was also observed. Reduction in yield as a result of climate change was reported to be significantly higher among male households than the female households.
Table 9 below indicates the results of the logistic regression model of farmers’ perceptions of climate change. Male-led households positively perceived climate change (
p < 0.01) more than female-headed households. Positive perception of climate change was significantly influenced by farmers who were trained up to standard seven (
p < 0.05), and form four (
p < 0.1). Furthermore, farmers with more farming experience were also more likely to have positive perceptions of climate change than farmers with low farming experience (
p < 0.1). On the other hand, farmers who have experienced crop failure due to water shortage are more likely to have positive perceptions of climate change than farmers without such experience (
p < 0.01). Farmers’ access to climate information also increases the probability of perceiving climate change positively (
p < 0.01). A positive perception of climate change was also significantly influenced by farmers who heard about climate change two years ago and five years ago (
p < 0.01).
3.4. Farmers’ Responses to Climate Change
Soil and water conservation practices comprised the use of terraces, cut-off drains, and mulching. The results indicated that 67 (28%) households used terraces in their coffee fields. This includes 49% from the Northern Highlands zone and 46% from the Southern Highlands zone. On the other hand, 31% of the respondents were using cut-off drains, which include 30% from the Northern Highlands zone and 37% from the Southern Highlands zone. Households that applied mulch in their coffee fields constituted 89%. Irrigation practice was the least adopted practice in the study area; only 31 (13%) households out of 242 were irrigating their coffee fields. This involved 27(17%) households from the Northern Highlands zone and 4 (5%) from the Southern Highlands zone. Dominant planted trees are Grevillea robusta, Persea americana, Albizia spp., and Cordia africana. The results also indicated that 41% of the farming households had started planting coffee varieties, which are tolerant to Coffee Berry Disease (CBD) and Coffee Leaf Rust Disease (CLR). However, still, of the majority of the farmers, 119 (73%) who perceived climate change still planted old coffee varieties, which are susceptible to CBD and CLR diseases.
From the surveyed soil nutrients sources, organic manure was the most widely applied nutrient source. About 55% of the farming households who perceived climate change used organic fertilizer, while 56% of those who did not perceive climate change were also using organic fertilizer. There was also significant differences (
p < 0.05) in terms of most of the agronomic practices between the Northern and Southern Highlands zones with the exception of cut-off drains, which were not significantly different between the two zones (
p > 0.05) (
Table 10).
3.5. Factors Influencing Household Decisions to Adapt to Climate Change
Household decisions to adapt to climate change were significantly influenced by the gender of the household head, farm size, education level, farming experience, access to climate information, access to extension services, and time aware of climate change in different ways (
Table 11). The probability of male-headed household to plant disease-tolerant varieties was higher than that of a female-headed household (
β = 0.981,
p < 0.05). Farming experience negatively influenced the adoption of disease-tolerant varieties (
β =
p < 0.05). There is a positive relationship between farmers with larger farm size and the adoption of disease-tolerant varieties (
β = 0.233,
p < 0.05) and carrying out soil and water conservation methods through the use of terraces (
β = 0.303,
p < 0.01), unlike for farmers possessing small farm sizes. However, larger farm sizes decreased the probability of using mulches (
β = −0.208,
p < 0.05).
From
Table 11 above, access to extension services significantly enhanced the adoption of planting shading trees (
β = 1.054,
p < 0.05), using cut-off drains (
β = 0.698,
p < 0.05), soil fertility management (β = 0.868,
p < 0.05), and terraces (
β = 0.759,
p < 0.05) rather than those who use these practices without access to extension services. Access to climate information significantly influenced the use of terraces (
β = 0.772
p < 0.1) and cut-off drains (
β = 1.054
p < 0.05). The adoption of irrigation practice was significantly influenced by farmers who were trained up to form four (
β = 2.669,
p < 0.05), form six (
β = 3.728,
p < 0.05), and university (
β = 3.07,
p < 0.1). Recent climate change awareness significantly (
β =
p < 0.05) influenced the use irrigation practices and intensification of routine activities (pruning insect pest control and disease control).
5. Conclusions
The results demonstrated that coffee farmers from the Northern and Southern Highland of Tanzania have experienced changes in climate (increase in temperature and decrease in rainfall). Moreover, climate change has already impacted coffee production in terms of reduction in yield, increase in coffee insect pests and diseases, late flowering, prolonged harvesting, and total crop failure in more adverse conditions. Climate change will continue to affect farmers’ livelihood unless adaptation measures are taken. Recent awareness of climate change, access to climate change information, education level and the sex of the household head, and farming experience are factors affecting farmers’ climate change perceptions. Smallholder farmers have been responding to unpredictable weather patterns in different ways with their level of response being influenced by the gender of the household head, education level, farming experience, farm size, access to extension services, and time aware of climate change information. Based on these results, it is recommended to enhance access to timely and accurate weather information together with developing institutions that enhances access to education and extension services. Each group of farmers with different levels of education should also be trained or advised in a different way. The focus of education or training should be on attenuating the impacts of climate change through relevant adaptation measures in each coffee-growing region. The findings of this study are also applicable to other areas growing coffee under similar conditions.