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International Journal of Business Marketing and Management (IJBMM)
Volume 4 Issue 4 April 2019, P.P. 36-42
ISSN: 2456-4559
www.ijbmm.com
International Journal of Business Marketing and Management (IJBMM) Page 36
Estimating Impact of Weather Variables on Rice Production in
Tanzania: What is the Contribution of Increase in Planting Area?
Kulyakwave, Peter David1,2,3
, Shiwei Xu1,3*
, Wen Yu1,3
1
Agricultural Information Institute, Chinese Academy of Agricultural Sciences: Beijing, China
2
Department of Research, Training, and Market Development, Tanzania National Service Headquarters Dar Es
Salaam, Tanzania.
3
Key Laboratory of Digital Agricultural Early-Warning Technology, Ministry of Agriculture, Beijing, China.
Abstract-Emphasis on the impact of weather contribution to crop production in the developing world is of
crucial as far as the agricultural sector is concerned. Meanwhile, the relationship between weather and rice
production continues to create interest in Tanzania agricultural development. The upsurge in both income and
population in developing cities carters for more food demand, whereas, the supply side is not sufficient to
balance with the demand. In this paper, we estimated the impacts of weather parameters on rice production with
respect to planting area variations in Tanzania. We used weather time series data including rainfall, maximum
and minimum temperature, and sunshine data from 1981 to 2017, and rice production time series data from the
Mbeya region of Tanzania. Time series data were tested for stationarity properties by use of extended ADF
the Augment Dickey-Fuller test for time series data Stationarity. Moreover, the series proved to exhibit a long
run relationship by Johansen Cointegration test at their first level I (1) with the possibility of having the linear
combination. Regression results revealed that increase in unit rainfall than normal moisture required decrease
mean rice production by 13%, however, through stepwise regression other metrological elements including
mean maximum and minimum temperature, and sunshine had inferior significance on rice production. Most
importantly, an increase in unit planting area was revealed to increase rice production by 41%.
I. Introduction
Tanzania relies on agricultural outputs as primary sources of food to feed the growing
population (Rugumamu, 2014). There are enough shreds of evidence on, and from the fact that the entire
population depends on agriculture outputs including; cereals products such as maize, rice, wheat, sorghum and
etc (Mkonda & He, 2016: Ngailo, Mwakasendo, Kisandu, & Tippe, 2016). It is reported that almost above 80%
of the populations live in the rural areas in which their major economic activities is crop production followed by
animal keeping (Tanzania Invest, 2018). Moreover, the sector is dominated by small scale farmers from the rural
environment which plays duo impacts as producers, traders and consumers at the same time (Mtongori, Stordal,
& Benestad, 2016). To date, agricultural sector contributes to about 35% of country‟s GDP and has been for a
long time referred as the backbone of national economic development (Tanzania Invest, 2018; Wilson & Lewis,
2015; ). In additional, agriculture in Tanzania provides more than 67% of total employment especially to the
rural population which forms above 75% of the total country‟s population (Carlos & Jorge, 2015).
Rice is farmed in various areas of the country but dominated by the Southern Highland regions
including Mbeya, however, other regions such as Shinyanga, Mwanza, Arusha, Kilimanjaro also produce a
substantial amount of rice (Rowhani, Lobell, Linderman, & Ramankutty, 2011; Makoi, 2016). On the other
hand, Agriculture in Tanzania is controlled by meteorological conditions since is a rain-fed farming
system (Call, 2017; Ngailo, Mwakasendo, Kisandu, & Tippe, 2016) where irrigations mechanization is almost
non-existed (FAO, 2014). Continuing reliance on rain-fed rice farming system (WWF, 2010), always becomes
sensitive to any magnitude change in weather. In this regard, any deviations from normal weather condition
especially rainfall, sunshine, and temperature bring significant impacts on rice productions as well as food
security. Meanwhile, rice production requires optimal weather conditions for development from sowing to
harvest, however, any periodic variation of weatherfrom season to the season and or year to year poses
uncertainty to rice production, and food security in the country. With this fact, it is of paramount important to
have a clear understanding of potential impacts of meteorological variables on rice production and significant of
varying the planting area.
Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of
International Journal of Business Marketing and Management (IJBMM) Page 37
On the other hand, weather variability as an environmental factor diverge consumer needs, preference,
and demand (RICE Flagship project, 2017), and consequently fail to trade off. Consumers demand and
preferences on rice characteristics like the aroma, quality and safety shifts as a result of management
changes including the use of weather tolerance seeds, chemicals, and also irrigation practices which upsurges
the gap between consumers and producers. Likewise, as a result of weather shock incidences as evidenced in
various areas makes farmers react by opting crops choices, land allocations due to past weather shocks (Salazar-
Espinoza, Jones, & Tarp, 2015). Under-estimating the impacts from shocks is a major factor to poor
production (Podleśny & Podleśna, 2011), as a result, it increases farmers sensitivity towards crop productions
thereby shifting to other economic activities which are non-productive in the rural environments (Salazar-
Espinoza et al., 2015).
Various approaches tointensifyrice subsector in Tanzania have so far been put in place aiming at
production and productivity fortification, and hunger suppression. However, to the moment the environment
approach has indeed received less attention as an important factor to be considered. However, there are few
studies embracing the total long term effect resulting from climate change but with short weather, impacts have
not adequately covered. Therefore, the current research targeted to understand on how weather variation
including rainfall, sunshine, maximum, and minimum temperatures affect rice production in Tanzania and
specifically in the study region. Additionally, the study also intended to investigate how variations in farm size
under production could combine with weather to influence rice production and productivity. On the other aspect,
apart from achieving stated aims an understanding of the core relationship between weather variables and
planted area with rice production could help the small scale rice farmers on productions forecasting and
predictions.
II. Materials and Methodology
2.1 Type of Data and Data sources
The Panel data pertaining to rice production, planted area, and weather variables are included in this
study. We obtained rice production data series for the study region for the past 36 years (1981-2017) from the
Tanzania government agencies including: Tanzania Ministry of Agriculture, Food security and Cooperative
(MAFC), Ministry of Industry and Trade (MOIT), and National Bureau of Statistics (NBS). The Meteorological
data including average monthly rainfall (mm), average monthly maximum and minimum temperature (o
C), and
average sunshine (hrs) for the same duration of 36 years were sourced from the Tanzania Meteorological
Agency.
2.2 Methodology
2.2.1 Profile of the Study region
Mbeya is among the oldest region located in the Southern Highlands of Tanzania. It is situated between latitude
70 and 90 31‟ to the south of equator and longitude 320 and 350 east of Greenwich. The region is among the
leading in term of agricultural outputs in Tanzania (Makoi, 2016). The climate is hugely affected by both
physiology and altitude. Rice production is among the major agricultural activities undertaken in the region, in
addition, other crops include maize, wheat, banana, beans, and many others are also farmed. Statistics revealed
that the statistics show that in the Southern Highlands area under rice production in about 24% of the total
National area under rice production. In addition, about 33% of the National rice outputs isfrom this region alone,
and, for Mbeya alone an area under rice production is about 135,215 ha. Being in the tropical area, the region
receives rainfall which varies between 650mm and 1200mm though experience dry and cold spell between June
and September. The tropical climate, rainfall distribution, and variations in temperature favour rice production,
however, rice cultivation is undertaken in the large area of the region including Mbarali and Kyela Districts.
III. Stationarity of time series data and Cointegration
We started by verifying if the time series data are stationary by applying Augmented Dickey (1979)
fuller (ADF) regression model. The extended ADF is widely used to check for unit root test by the aid of OL
regression model. Basically, we used two hypotheses during testing for a unit root in time series as; H0: ρ = 0
(Existence of unit root), H1: ρ <0 (No unit root). We also proved by using the ADF test for Unit root test. ADF
test uses calculated statistic t as absolute values and compares with the ADF critical values at 1%, 5% and 10%
as an absolute value. If the OLS regression statistics t is greater than any one or all critical values then we had
enough confidence to reject the H0 and accept the Alternate hypothesis H1.
In addition, the long term relationship between data was established. More so, Interaction of variables
creates equilibrium and disequilibrium in the long run. Likewise, Johansen cointegration was performed to test
Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of
International Journal of Business Marketing and Management (IJBMM) Page 38
the relationship exhibited by the variables in the long run. More precisely, the cointegration is conducted at their
level of I (1) order series. We, therefore, hypothesized that H0: there is no cointegration relationship between
variables and H1: H0 is not true such that there are cointegration equations. Thus, the test was done at a 5%
level of significance. The Johansen cointegration test revealed that there is a maximum of two cointegration
equations which can be exhibited by the series hence rejected the null hypothesis. The result thus depicts the
possibilities of having long run combination of variables in the model as has also proved by using Johansen test
(1988)(Hjalmar son& Österholm, 2010).
IV. Characteristics of the Panel Data
The descriptive characteristics of the panel data considered for the study are presented in Table 1. The average
rice production is 2528.2 („000‟kg/ha/year). The minimum and maximum production obtained was 200 and
8582 (“000” kg/ha/year) respectively. The mean, minimum and maximum rainfall received during growing to
harvest season (January to July) each year measured in a monthly base is 123.3, 66.8, and 81.3 millimeters. The
mean, minimum and maximum temperature (maximum) was 23.2, 21.9, and 24.2 (oC). However, other
important weather parameters are shown in( Table 1) including area planted (ha).
Table 1. Results for descriptive statistics of all variables
Variable Obs Mean Std. Dev. Minimum Maximum
Rice production (“000”kg/ha) 35 2528.2 1449.1 200.0 8452.0
Area “ha” 35 43.1 18.7 12.2 81.3
Average rainfall (mm) 37 123.3 30.3 66.8 181.7
Average maximum Temperature
(o
C)
37 23.2 0.5 21.9 24.2
Average Temperature minimum
(o
C)
37 11.1 0.5 9.9 12.3
Average Sunshine 37 7.8 0.5 6.8 8.7
V. Estimating model for weather variables impact on rice production
Rice productions involve interactions of various variables including both the natural and non-natural
parameters. The natural parameters include weather variables such as rainfall, temperatures, and sunshine to
mention a few while non-natural variables are like technology, capital, labor and many others. More so, the
relationship between variables influences rice production as well as productivity in a particular environment. In
order to estimate the impacts of weather on rice production, an econometric model was designed using OLS
regression equation. The relationship between rice productions as dependent variable is established with average
rainfall, average maximum and minimum temperature, sunshine, time, and also the size of planting area
equation (1). Using a stepwise regression both rainfall and planting area confirm to show positive impacts on
rice production in the study areas.
𝑦𝑟 = 𝛼0 + 𝛼1 𝐴𝑟𝑓 + 𝛼2 𝐴𝑡𝑚𝑎𝑥 + 𝛼3 𝐴𝑡𝑚𝑖𝑛 + 𝛼4 𝐴𝑠𝑠 + 𝛼5 𝐴𝑎𝑟𝑒𝑎 + 𝛼6 𝑡𝑖𝑚𝑒 + 𝜀𝑡 (1)
Where, yris the rice production, 𝛼0 is a constant term, 𝛼1is a coefficient for rainfall variable denoted as Arf, 𝛼2
is a coefficient for maximum temperature variable denoted as Atmax, 𝛼3 is coefficient for temperature
minimum denoted as Atmin,𝛼4 is coefficient of sunshine denoted as Ass, 𝛼5is coefficient of planting area
denoted as Area, 𝛼6 is a coefficient of time trend variabledenoted as time in years, and 𝜀𝑡 is an error term.
Henceforth, after we performed a stepwise regression we obtained equation (2).
𝑦𝑟 = 𝛼0 + 𝛼1 𝐴𝑟𝑓 + 𝛼2 𝐴𝑎𝑟𝑒𝑎 + 𝜀𝑡 (2)
Whereas, 𝛼0 constant, 𝛼1is a coefficient for rainfall denoted as Arf, 𝛼2is coefficient of planting area denoted as
Area, and 𝜀𝑡 is an error term.
VI. Stationarity checking for both rainfall and area variables
Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of
International Journal of Business Marketing and Management (IJBMM) Page 39
Before we used the equation described in the model (2) for the analysis the authors performed the
stationarity test by using the Dickey & Fuller, (1979) method. Our intention was to eliminate the unit root if
exist in the respective time series data which could end up with spurious equations. The underlined hypotheses
for the test are H0: 𝜌 = 0“there is unit root”, and 𝜌 => 0“no unit root”. Therefore, the true models are
described in following equations 3-5.
𝑦𝑡𝑦 = 𝑦𝑡𝑦−1 + 𝑢𝑡 (3)
Where, 𝑦𝑡𝑦 is the rice for Mbeya region at time t, 𝑦𝑡𝑦−1 is the rice production at time t-1, and 𝑢𝑡is an error term
at time t.
𝑦𝑡𝑟 = 𝑦𝑡𝑟−1 + 𝑢𝑡𝑟 (4)
Whereby;𝑦𝑡𝑟 is rainfall variable for Mbeya at time t, 𝑦𝑡𝑟−1 is rainfall for Mbeya at time𝑡𝑟 − 1, and 𝑢𝑡 is an
error term at time t.
𝑦𝑡𝑎 = 𝑦𝑡𝑎−1 + 𝑢𝑡𝑟 (5)
Whereby;𝑦𝑡𝑎 is area planted rice in Mbeya at time t, 𝑦𝑡𝑎−1 is an area planted rice for Mbeya region at time
𝑡𝑟𝑎 − 1, and 𝑢𝑡 is an independent error term at time t.
VII. Augmented Dickey and Fuller Stationarity test for rice production Mbeya region
Table 2.dfuller production, reg
Dickey-Fuller test for unit root Number of obs = 34
---------- Interpolated Dickey-Fuller ---------
Test 1% Critical 5% Critical 10% Critical
StatisticValue Value Value
Z(t) -4.821 -3.689 -2.975 -2.619
MacKinnon approximate p-value for Z(t) = 0.0000
D.production Coef. Std. Err. tP>|t| [95% Conf. Interval]
production
L1. -.8593911 .1782449 -4.82 0.000 -1.222464-.4963182
_cons 2205.635 508.3602 4.34 0.000 1170.139 3241.131
The results dictate that Dfuller t-statistics was -4.821 (in absolute value), which is greater than the
critical values at 1%, 5%, and 10%. Also from the result P-value = 0.000 which means we have enough reasons
to reject null hypothesis at .05 significance level. Hence the rice productiondata are stationary series.
VIII. Augmented Dickey and Fuller Stationarity test for planted area in Mbeya region
Table 3. dfuller area, reg
Dickey-Fuller test for unit root Number of obs = 34
---------- Interpolated Dickey-Fuller ---------
Test 1% Critical 5% Critical 10% Critical
Statistic Value Value Value
------------------------------------------------------------------------------
Z(t) -2.661 -3.689 -2.975 -2.619
MacKinnon approximate p-value for Z(t) = 0.0810
D.
Area Coef. Std. Err. tP>|t| [95% Conf. Interval]
L1. -.3735319 .1403539 -2.66 0.012 -.6594234 -.0876403
_cons 17.26563 6.453911 2.68 0.012 4.119445 30.41182
The results show that Dfuller T-statistics is 2.661 (in absolute value), which is greater than the critical value at
10% (Significant) but less than critical values at 1% and 5% in absolute values. Therefore, we have failed to
Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of
International Journal of Business Marketing and Management (IJBMM) Page 40
reject the null hypothesis that the series data are not stationary at 0.05 significant levels. So, we had to perform a
second difference of the series data.
Table 4.dfuller darea, reg
Dickey-Fuller test for unit root Number of obs = 34
---------- Interpolated Dickey-Fuller ---------
Test 1% Critical 5% Critical 10% Critical
Statistic Value Value Value
Z(t) -6.135 -3.689 -2.975 -2.619
MacKinnon approximate p-value for Z(t) = 0.0000
D.darea Coef. Std. Err. t P>|t| [95% Conf. Interval]
darea
L1. -1.321712 .2154422 -6.13 0.000 -1.760553 -.8828703
_cons .1252123 3.438219 0.04 0.971 -6.87821 7.128635
Therefore, thedfuller T-statistics = -6.135 (in absolute value), which is greater than the critical values at 1%, 5%,
and 10% in absolute values. Then, we have enough reasons to reject the null hypothesis the series are not
stationary at 0.05 significant levels. Hence, we conclude by accepting the alternative hypothesis that the series is
stationary after second difference at 0.05 significant levels.
IX. Results and Discussion
The results revealed that out of six independent variables regressed by average rice production only
rainfall and the area was significant for the model as shown in equation (2).Therefore, it was revealed that rice
production in the study area is affected by the average rainfall (mm) and average planting area (ha) for the
whole farming seasons.According to our results, it illustrates that increase in unit rainfall above the average
amount required was likely to decrease rice production by 13%(Table 5).The study demonstrated thatrice
requires an optimal amount of rainfall during the growth period but any deviations from the optimal plant
requirement lead to poor yields. Similar findings wereobserved by Horie(2006)as he studiedthe effect of rainfall
and cropping intensity on rice. Asada and Matsumoto ( 2015) also revealed that an increase of rainfall above the
required amount could reduce rice yield and rice in the Ganges-Brahmaputra Basin. Among the two important
rice producer districts, Mbarali district is reported to receive less rainfall thanthe Kyela district, however, the
former was superior in terms of rice production due to the existence of small irrigation schemes which are less
developed (Ngailo et al, 2016). Therefore, availability of irrigation technology in the locality could help farmers
to have a decent water plan according to plant requirement than rain-water which is beyond famers‟ control.
More specific the result draws attention on the overall effect of rainfall in whole growing season from
sowing to mature, however, it may be reported otherwise when is to be considered at different stages of plant
growth. A similar result is reported by (Ali, Paliwal, Kumar, & Kumar, 2017) on the effect of rainfall on
different growth stages of rice in India. For example, during transplanting more rainfall is required to facilitate
plant development but similar quantitycould bedetrimental to rice during pollination, grain filling, maturity,and
also duringthe harvesting process.
Table 5. Rice production estimates from OLS regression
Production Coef. Std. Err t P>|t| [95% Conf. Interval]
area 41.42415 12.26956 3.38 0.002 16.43187 66.41643
avrf -12.87381 7.839164 -1.64 0.110 -28.84166 3.094049
_cons 2304.758 960.7709 2.40 0.022 347.7313 4261.784
F=0.0066 R-squared =0.2696Adj R-squared = 0.2240DW (3, 35)= 2.150584
Meanwhile, the result from (Table 5) shows that an increase in unit farm area (ha) increases rice production by
41%and wassignificant at 0.05% level. The findings indicate that farmers could reap more rice outputs if
increase in planting area was his best choice. This implies that there is a need for farmers to increase their farm
Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of
International Journal of Business Marketing and Management (IJBMM) Page 41
size in order to attain optimal rice productions in the study area. A Similar result was reported by (van Ittersum
et al, 2016),as they commented thatupsurge in cropping area remains the main option for small scale farmers to
increase their crop production in Sub-Sahara Africa Tanzania inclusive.In addition, the rice production model
reveals that apart from roles played by rainfall, and the variations of an area,rice productionwas also facilitated
by other variables such as technology advancement such as seeds, machinery, insecticides and herbicides, soil
characteristics, and other management practices which in combination contribute to rice production.
X. Conclusion
The study used an econometric approach basically the OLSregression to determine the estimates for
rice production in the Mbeya region of Tanzania. The results revealed that rice production is highly affected by
variations in both rainfall and planting area. To be more specific, an increase in unit mean rainfall above normal
plants requirement in the farming season decrease rice production by 13%. In addition, increases in planting
area by one unit revealed to an increase rice production by 41%. However, the results create an alert that
increases in population will demand more land for both agricultural and other human activities,therefore, there is
a high possibility ofincreasing land pressure in the study area. It is suggested that more studies be undertaken
especially on land management with relationship to crops production. In addition, the government should also
have an eye look on land tenure systems that will have a harmonious relationship among land usersespecially
farmers and animal keepers, since, farmers best desires are to maximize rice production by increasing their farm
size.
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Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the Contribution of Increase in Planting Area?

  • 1. International Journal of Business Marketing and Management (IJBMM) Volume 4 Issue 4 April 2019, P.P. 36-42 ISSN: 2456-4559 www.ijbmm.com International Journal of Business Marketing and Management (IJBMM) Page 36 Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the Contribution of Increase in Planting Area? Kulyakwave, Peter David1,2,3 , Shiwei Xu1,3* , Wen Yu1,3 1 Agricultural Information Institute, Chinese Academy of Agricultural Sciences: Beijing, China 2 Department of Research, Training, and Market Development, Tanzania National Service Headquarters Dar Es Salaam, Tanzania. 3 Key Laboratory of Digital Agricultural Early-Warning Technology, Ministry of Agriculture, Beijing, China. Abstract-Emphasis on the impact of weather contribution to crop production in the developing world is of crucial as far as the agricultural sector is concerned. Meanwhile, the relationship between weather and rice production continues to create interest in Tanzania agricultural development. The upsurge in both income and population in developing cities carters for more food demand, whereas, the supply side is not sufficient to balance with the demand. In this paper, we estimated the impacts of weather parameters on rice production with respect to planting area variations in Tanzania. We used weather time series data including rainfall, maximum and minimum temperature, and sunshine data from 1981 to 2017, and rice production time series data from the Mbeya region of Tanzania. Time series data were tested for stationarity properties by use of extended ADF the Augment Dickey-Fuller test for time series data Stationarity. Moreover, the series proved to exhibit a long run relationship by Johansen Cointegration test at their first level I (1) with the possibility of having the linear combination. Regression results revealed that increase in unit rainfall than normal moisture required decrease mean rice production by 13%, however, through stepwise regression other metrological elements including mean maximum and minimum temperature, and sunshine had inferior significance on rice production. Most importantly, an increase in unit planting area was revealed to increase rice production by 41%. I. Introduction Tanzania relies on agricultural outputs as primary sources of food to feed the growing population (Rugumamu, 2014). There are enough shreds of evidence on, and from the fact that the entire population depends on agriculture outputs including; cereals products such as maize, rice, wheat, sorghum and etc (Mkonda & He, 2016: Ngailo, Mwakasendo, Kisandu, & Tippe, 2016). It is reported that almost above 80% of the populations live in the rural areas in which their major economic activities is crop production followed by animal keeping (Tanzania Invest, 2018). Moreover, the sector is dominated by small scale farmers from the rural environment which plays duo impacts as producers, traders and consumers at the same time (Mtongori, Stordal, & Benestad, 2016). To date, agricultural sector contributes to about 35% of country‟s GDP and has been for a long time referred as the backbone of national economic development (Tanzania Invest, 2018; Wilson & Lewis, 2015; ). In additional, agriculture in Tanzania provides more than 67% of total employment especially to the rural population which forms above 75% of the total country‟s population (Carlos & Jorge, 2015). Rice is farmed in various areas of the country but dominated by the Southern Highland regions including Mbeya, however, other regions such as Shinyanga, Mwanza, Arusha, Kilimanjaro also produce a substantial amount of rice (Rowhani, Lobell, Linderman, & Ramankutty, 2011; Makoi, 2016). On the other hand, Agriculture in Tanzania is controlled by meteorological conditions since is a rain-fed farming system (Call, 2017; Ngailo, Mwakasendo, Kisandu, & Tippe, 2016) where irrigations mechanization is almost non-existed (FAO, 2014). Continuing reliance on rain-fed rice farming system (WWF, 2010), always becomes sensitive to any magnitude change in weather. In this regard, any deviations from normal weather condition especially rainfall, sunshine, and temperature bring significant impacts on rice productions as well as food security. Meanwhile, rice production requires optimal weather conditions for development from sowing to harvest, however, any periodic variation of weatherfrom season to the season and or year to year poses uncertainty to rice production, and food security in the country. With this fact, it is of paramount important to have a clear understanding of potential impacts of meteorological variables on rice production and significant of varying the planting area.
  • 2. Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of International Journal of Business Marketing and Management (IJBMM) Page 37 On the other hand, weather variability as an environmental factor diverge consumer needs, preference, and demand (RICE Flagship project, 2017), and consequently fail to trade off. Consumers demand and preferences on rice characteristics like the aroma, quality and safety shifts as a result of management changes including the use of weather tolerance seeds, chemicals, and also irrigation practices which upsurges the gap between consumers and producers. Likewise, as a result of weather shock incidences as evidenced in various areas makes farmers react by opting crops choices, land allocations due to past weather shocks (Salazar- Espinoza, Jones, & Tarp, 2015). Under-estimating the impacts from shocks is a major factor to poor production (Podleśny & Podleśna, 2011), as a result, it increases farmers sensitivity towards crop productions thereby shifting to other economic activities which are non-productive in the rural environments (Salazar- Espinoza et al., 2015). Various approaches tointensifyrice subsector in Tanzania have so far been put in place aiming at production and productivity fortification, and hunger suppression. However, to the moment the environment approach has indeed received less attention as an important factor to be considered. However, there are few studies embracing the total long term effect resulting from climate change but with short weather, impacts have not adequately covered. Therefore, the current research targeted to understand on how weather variation including rainfall, sunshine, maximum, and minimum temperatures affect rice production in Tanzania and specifically in the study region. Additionally, the study also intended to investigate how variations in farm size under production could combine with weather to influence rice production and productivity. On the other aspect, apart from achieving stated aims an understanding of the core relationship between weather variables and planted area with rice production could help the small scale rice farmers on productions forecasting and predictions. II. Materials and Methodology 2.1 Type of Data and Data sources The Panel data pertaining to rice production, planted area, and weather variables are included in this study. We obtained rice production data series for the study region for the past 36 years (1981-2017) from the Tanzania government agencies including: Tanzania Ministry of Agriculture, Food security and Cooperative (MAFC), Ministry of Industry and Trade (MOIT), and National Bureau of Statistics (NBS). The Meteorological data including average monthly rainfall (mm), average monthly maximum and minimum temperature (o C), and average sunshine (hrs) for the same duration of 36 years were sourced from the Tanzania Meteorological Agency. 2.2 Methodology 2.2.1 Profile of the Study region Mbeya is among the oldest region located in the Southern Highlands of Tanzania. It is situated between latitude 70 and 90 31‟ to the south of equator and longitude 320 and 350 east of Greenwich. The region is among the leading in term of agricultural outputs in Tanzania (Makoi, 2016). The climate is hugely affected by both physiology and altitude. Rice production is among the major agricultural activities undertaken in the region, in addition, other crops include maize, wheat, banana, beans, and many others are also farmed. Statistics revealed that the statistics show that in the Southern Highlands area under rice production in about 24% of the total National area under rice production. In addition, about 33% of the National rice outputs isfrom this region alone, and, for Mbeya alone an area under rice production is about 135,215 ha. Being in the tropical area, the region receives rainfall which varies between 650mm and 1200mm though experience dry and cold spell between June and September. The tropical climate, rainfall distribution, and variations in temperature favour rice production, however, rice cultivation is undertaken in the large area of the region including Mbarali and Kyela Districts. III. Stationarity of time series data and Cointegration We started by verifying if the time series data are stationary by applying Augmented Dickey (1979) fuller (ADF) regression model. The extended ADF is widely used to check for unit root test by the aid of OL regression model. Basically, we used two hypotheses during testing for a unit root in time series as; H0: ρ = 0 (Existence of unit root), H1: ρ <0 (No unit root). We also proved by using the ADF test for Unit root test. ADF test uses calculated statistic t as absolute values and compares with the ADF critical values at 1%, 5% and 10% as an absolute value. If the OLS regression statistics t is greater than any one or all critical values then we had enough confidence to reject the H0 and accept the Alternate hypothesis H1. In addition, the long term relationship between data was established. More so, Interaction of variables creates equilibrium and disequilibrium in the long run. Likewise, Johansen cointegration was performed to test
  • 3. Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of International Journal of Business Marketing and Management (IJBMM) Page 38 the relationship exhibited by the variables in the long run. More precisely, the cointegration is conducted at their level of I (1) order series. We, therefore, hypothesized that H0: there is no cointegration relationship between variables and H1: H0 is not true such that there are cointegration equations. Thus, the test was done at a 5% level of significance. The Johansen cointegration test revealed that there is a maximum of two cointegration equations which can be exhibited by the series hence rejected the null hypothesis. The result thus depicts the possibilities of having long run combination of variables in the model as has also proved by using Johansen test (1988)(Hjalmar son& Österholm, 2010). IV. Characteristics of the Panel Data The descriptive characteristics of the panel data considered for the study are presented in Table 1. The average rice production is 2528.2 („000‟kg/ha/year). The minimum and maximum production obtained was 200 and 8582 (“000” kg/ha/year) respectively. The mean, minimum and maximum rainfall received during growing to harvest season (January to July) each year measured in a monthly base is 123.3, 66.8, and 81.3 millimeters. The mean, minimum and maximum temperature (maximum) was 23.2, 21.9, and 24.2 (oC). However, other important weather parameters are shown in( Table 1) including area planted (ha). Table 1. Results for descriptive statistics of all variables Variable Obs Mean Std. Dev. Minimum Maximum Rice production (“000”kg/ha) 35 2528.2 1449.1 200.0 8452.0 Area “ha” 35 43.1 18.7 12.2 81.3 Average rainfall (mm) 37 123.3 30.3 66.8 181.7 Average maximum Temperature (o C) 37 23.2 0.5 21.9 24.2 Average Temperature minimum (o C) 37 11.1 0.5 9.9 12.3 Average Sunshine 37 7.8 0.5 6.8 8.7 V. Estimating model for weather variables impact on rice production Rice productions involve interactions of various variables including both the natural and non-natural parameters. The natural parameters include weather variables such as rainfall, temperatures, and sunshine to mention a few while non-natural variables are like technology, capital, labor and many others. More so, the relationship between variables influences rice production as well as productivity in a particular environment. In order to estimate the impacts of weather on rice production, an econometric model was designed using OLS regression equation. The relationship between rice productions as dependent variable is established with average rainfall, average maximum and minimum temperature, sunshine, time, and also the size of planting area equation (1). Using a stepwise regression both rainfall and planting area confirm to show positive impacts on rice production in the study areas. 𝑦𝑟 = 𝛼0 + 𝛼1 𝐴𝑟𝑓 + 𝛼2 𝐴𝑡𝑚𝑎𝑥 + 𝛼3 𝐴𝑡𝑚𝑖𝑛 + 𝛼4 𝐴𝑠𝑠 + 𝛼5 𝐴𝑎𝑟𝑒𝑎 + 𝛼6 𝑡𝑖𝑚𝑒 + 𝜀𝑡 (1) Where, yris the rice production, 𝛼0 is a constant term, 𝛼1is a coefficient for rainfall variable denoted as Arf, 𝛼2 is a coefficient for maximum temperature variable denoted as Atmax, 𝛼3 is coefficient for temperature minimum denoted as Atmin,𝛼4 is coefficient of sunshine denoted as Ass, 𝛼5is coefficient of planting area denoted as Area, 𝛼6 is a coefficient of time trend variabledenoted as time in years, and 𝜀𝑡 is an error term. Henceforth, after we performed a stepwise regression we obtained equation (2). 𝑦𝑟 = 𝛼0 + 𝛼1 𝐴𝑟𝑓 + 𝛼2 𝐴𝑎𝑟𝑒𝑎 + 𝜀𝑡 (2) Whereas, 𝛼0 constant, 𝛼1is a coefficient for rainfall denoted as Arf, 𝛼2is coefficient of planting area denoted as Area, and 𝜀𝑡 is an error term. VI. Stationarity checking for both rainfall and area variables
  • 4. Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of International Journal of Business Marketing and Management (IJBMM) Page 39 Before we used the equation described in the model (2) for the analysis the authors performed the stationarity test by using the Dickey & Fuller, (1979) method. Our intention was to eliminate the unit root if exist in the respective time series data which could end up with spurious equations. The underlined hypotheses for the test are H0: 𝜌 = 0“there is unit root”, and 𝜌 => 0“no unit root”. Therefore, the true models are described in following equations 3-5. 𝑦𝑡𝑦 = 𝑦𝑡𝑦−1 + 𝑢𝑡 (3) Where, 𝑦𝑡𝑦 is the rice for Mbeya region at time t, 𝑦𝑡𝑦−1 is the rice production at time t-1, and 𝑢𝑡is an error term at time t. 𝑦𝑡𝑟 = 𝑦𝑡𝑟−1 + 𝑢𝑡𝑟 (4) Whereby;𝑦𝑡𝑟 is rainfall variable for Mbeya at time t, 𝑦𝑡𝑟−1 is rainfall for Mbeya at time𝑡𝑟 − 1, and 𝑢𝑡 is an error term at time t. 𝑦𝑡𝑎 = 𝑦𝑡𝑎−1 + 𝑢𝑡𝑟 (5) Whereby;𝑦𝑡𝑎 is area planted rice in Mbeya at time t, 𝑦𝑡𝑎−1 is an area planted rice for Mbeya region at time 𝑡𝑟𝑎 − 1, and 𝑢𝑡 is an independent error term at time t. VII. Augmented Dickey and Fuller Stationarity test for rice production Mbeya region Table 2.dfuller production, reg Dickey-Fuller test for unit root Number of obs = 34 ---------- Interpolated Dickey-Fuller --------- Test 1% Critical 5% Critical 10% Critical StatisticValue Value Value Z(t) -4.821 -3.689 -2.975 -2.619 MacKinnon approximate p-value for Z(t) = 0.0000 D.production Coef. Std. Err. tP>|t| [95% Conf. Interval] production L1. -.8593911 .1782449 -4.82 0.000 -1.222464-.4963182 _cons 2205.635 508.3602 4.34 0.000 1170.139 3241.131 The results dictate that Dfuller t-statistics was -4.821 (in absolute value), which is greater than the critical values at 1%, 5%, and 10%. Also from the result P-value = 0.000 which means we have enough reasons to reject null hypothesis at .05 significance level. Hence the rice productiondata are stationary series. VIII. Augmented Dickey and Fuller Stationarity test for planted area in Mbeya region Table 3. dfuller area, reg Dickey-Fuller test for unit root Number of obs = 34 ---------- Interpolated Dickey-Fuller --------- Test 1% Critical 5% Critical 10% Critical Statistic Value Value Value ------------------------------------------------------------------------------ Z(t) -2.661 -3.689 -2.975 -2.619 MacKinnon approximate p-value for Z(t) = 0.0810 D. Area Coef. Std. Err. tP>|t| [95% Conf. Interval] L1. -.3735319 .1403539 -2.66 0.012 -.6594234 -.0876403 _cons 17.26563 6.453911 2.68 0.012 4.119445 30.41182 The results show that Dfuller T-statistics is 2.661 (in absolute value), which is greater than the critical value at 10% (Significant) but less than critical values at 1% and 5% in absolute values. Therefore, we have failed to
  • 5. Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of International Journal of Business Marketing and Management (IJBMM) Page 40 reject the null hypothesis that the series data are not stationary at 0.05 significant levels. So, we had to perform a second difference of the series data. Table 4.dfuller darea, reg Dickey-Fuller test for unit root Number of obs = 34 ---------- Interpolated Dickey-Fuller --------- Test 1% Critical 5% Critical 10% Critical Statistic Value Value Value Z(t) -6.135 -3.689 -2.975 -2.619 MacKinnon approximate p-value for Z(t) = 0.0000 D.darea Coef. Std. Err. t P>|t| [95% Conf. Interval] darea L1. -1.321712 .2154422 -6.13 0.000 -1.760553 -.8828703 _cons .1252123 3.438219 0.04 0.971 -6.87821 7.128635 Therefore, thedfuller T-statistics = -6.135 (in absolute value), which is greater than the critical values at 1%, 5%, and 10% in absolute values. Then, we have enough reasons to reject the null hypothesis the series are not stationary at 0.05 significant levels. Hence, we conclude by accepting the alternative hypothesis that the series is stationary after second difference at 0.05 significant levels. IX. Results and Discussion The results revealed that out of six independent variables regressed by average rice production only rainfall and the area was significant for the model as shown in equation (2).Therefore, it was revealed that rice production in the study area is affected by the average rainfall (mm) and average planting area (ha) for the whole farming seasons.According to our results, it illustrates that increase in unit rainfall above the average amount required was likely to decrease rice production by 13%(Table 5).The study demonstrated thatrice requires an optimal amount of rainfall during the growth period but any deviations from the optimal plant requirement lead to poor yields. Similar findings wereobserved by Horie(2006)as he studiedthe effect of rainfall and cropping intensity on rice. Asada and Matsumoto ( 2015) also revealed that an increase of rainfall above the required amount could reduce rice yield and rice in the Ganges-Brahmaputra Basin. Among the two important rice producer districts, Mbarali district is reported to receive less rainfall thanthe Kyela district, however, the former was superior in terms of rice production due to the existence of small irrigation schemes which are less developed (Ngailo et al, 2016). Therefore, availability of irrigation technology in the locality could help farmers to have a decent water plan according to plant requirement than rain-water which is beyond famers‟ control. More specific the result draws attention on the overall effect of rainfall in whole growing season from sowing to mature, however, it may be reported otherwise when is to be considered at different stages of plant growth. A similar result is reported by (Ali, Paliwal, Kumar, & Kumar, 2017) on the effect of rainfall on different growth stages of rice in India. For example, during transplanting more rainfall is required to facilitate plant development but similar quantitycould bedetrimental to rice during pollination, grain filling, maturity,and also duringthe harvesting process. Table 5. Rice production estimates from OLS regression Production Coef. Std. Err t P>|t| [95% Conf. Interval] area 41.42415 12.26956 3.38 0.002 16.43187 66.41643 avrf -12.87381 7.839164 -1.64 0.110 -28.84166 3.094049 _cons 2304.758 960.7709 2.40 0.022 347.7313 4261.784 F=0.0066 R-squared =0.2696Adj R-squared = 0.2240DW (3, 35)= 2.150584 Meanwhile, the result from (Table 5) shows that an increase in unit farm area (ha) increases rice production by 41%and wassignificant at 0.05% level. The findings indicate that farmers could reap more rice outputs if increase in planting area was his best choice. This implies that there is a need for farmers to increase their farm
  • 6. Estimating Impact of Weather Variables on Rice Production in Tanzania: What is the contribution of International Journal of Business Marketing and Management (IJBMM) Page 41 size in order to attain optimal rice productions in the study area. A Similar result was reported by (van Ittersum et al, 2016),as they commented thatupsurge in cropping area remains the main option for small scale farmers to increase their crop production in Sub-Sahara Africa Tanzania inclusive.In addition, the rice production model reveals that apart from roles played by rainfall, and the variations of an area,rice productionwas also facilitated by other variables such as technology advancement such as seeds, machinery, insecticides and herbicides, soil characteristics, and other management practices which in combination contribute to rice production. X. Conclusion The study used an econometric approach basically the OLSregression to determine the estimates for rice production in the Mbeya region of Tanzania. The results revealed that rice production is highly affected by variations in both rainfall and planting area. To be more specific, an increase in unit mean rainfall above normal plants requirement in the farming season decrease rice production by 13%. In addition, increases in planting area by one unit revealed to an increase rice production by 41%. However, the results create an alert that increases in population will demand more land for both agricultural and other human activities,therefore, there is a high possibility ofincreasing land pressure in the study area. It is suggested that more studies be undertaken especially on land management with relationship to crops production. In addition, the government should also have an eye look on land tenure systems that will have a harmonious relationship among land usersespecially farmers and animal keepers, since, farmers best desires are to maximize rice production by increasing their farm size. References [1]. Ali, A., Paliwal, H. B., Kumar, H., & Kumar, S. (2017). Effect of temperature and rainfall different growth stages and production of rice ( Oryzae sativa L .), 6(1), 331–332. [2]. Asada, H., & Matsumoto, J. (2015). Effects of rainfall variation on rice production in the Ganges- Brahmaputra Basin, (April 2009). https://doi.org/10.3354/cr00785 [3]. Call, A. (2017). Climate-smart agriculture. CSA News, 62(2), 4. https://doi.org/10/gdpc5n [4]. Dickey, D. A., & Fuller, W. A. (1979). Distribution of the Estimators for Autoregressive Time Series With a Unit Root. Journal of the American Statistical Association, 74(366), 427. https://doi.org/10.2307/2286348 [5]. FAO. (2014). 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