Agriculture, Forestry and Fisheries
Volume 4, Issue 6, December 2015, Pages: 252-256

Variations in Climate Change Indicators and Implications on Forest Resources Management in Taraba State, Nigeria

Agbidye Francis Sarwuan1, *, Emmanuel Zando Angyu1, Egbuche Christian. Toochi2

1Department of Forest Production and Products, University of Agriculture, Makurdi, Nigeria

2Department of Forest and Wildlife Technology, Federal University of Technology Owerri, Imo State, Nigeria

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(A. F. Sarwuan)

To cite this article:

Agbidye Francis Sarwuan, Emmanuel Zando Angyu, Egbuche Christian. Toochi. Variations in Climate Change Indicators and Implications on Forest Resources Management in Taraba State, Nigeria.Agriculture, Forestry and Fisheries.Vol.4, No. 6, 2015, pp. 252-256. doi: 10.11648/j.aff.20150406.13


Abstract: This study was carried out to investigate the variation in climate change indicators of specific interest of rainfall and temperature) in Taraba State from 1991 to 2011. Secondary data were obtained on these climate change indicators from the Nigerian Meteorological Agency (NIMET), Jalingo, Taraba State, Nigeria. Data obtained on amount of rainfall, maximum and minimum temperature and temperature range were subjected to Analysis of Variance (ANOVA). The results showed no significant differences in all the variables considered (p ≤ 0.05). This shows that the much talked about climate change in Taraba State is speculative and not based on empirical data. However, to forestall the possible menace of climate change in the study area, it was recommended that policies and programmes supporting afforestation and proper environmental management should be put in place. Also, there is need for a widespread enlightenment of the citizens on climate change to enable them to change some of the human behaviours contributing to climate change.

Keywords: Climate Change, Indicators, Temperature, Rainfall, Implications, Forest Resources


1. Introduction

Climate is the composite of the day-to-day weather condition and of atmospheric elements of a place or region, over a long period of time, at least about 30-35 years [1]. It is further accepted that climate change has been defined as a change in the state of the climate that can be identified (. by using statistical tests) by changes in the mean and/or the variability of its properties, and that persists for an extended period typically decades or longer [2]. Global climate change and warming however, is supported as the rising earth’s surface temperature caused by the increase in the concentration and accumulation of green house gases in the atmosphere. Today, climate change is among the major global environmental problems threatening the survival of the entire race. It is seen as a key phenomenon of our times, as a set of events which affects forestry and may alter the lives of human kind in general [2].

Climate change is controlled by factors such as temperature, precipitation (rainfall), solar energy, humidity, wind, air pressure, altitude, latitude, distribution of land and water, mountain barriers and ocean currents [3]. Temperature and rainfall are among the major factors that influence weather conditions of a place and has been documented that major indicators of climate change are the increase in the mean surface temperature [4] and increase in mean annual rainfall [5]. Global records of earth’s surface temperature have indicated a rise of about 0.3-7°C in temperature in the last century [6]; [7]. Precipitation has increased by about 1% across the world in the last century, while high latitudes tend to see more rainfall. Temperature changes affect plants in the following ways: Increase in temperature may prevent some plants from growing in their natural areas; abnormal increases in temperature have adverse effects on productivity of forest crops and plants; thereby alters flowering pattern of crops and forest plants species, resultant starvation leads to death and migration of wild species; low temperature could lead to formation of ice which hinders the germination of plants and operation of some important soil microbes that act as decomposers among others. Apart from this, some authors have suggested that climate change could lead to dieback in existing or future forests due to water stress, insect infestations, or fires [8]; [9]; [10].

The association between climate and forestry has widely been discussed in the literature [11]; [12]. There is great concern over the implications of a changing climate to the forest industry, particularly since the species and provenances planted at present and in the recent past reflect the current climate. It is now widely recognized that climate change is likely to have strong influences on the structure and function of the forests [13]; [2]. These impacts can be categorized into three general areas that include forest productivity changes, ecosystem disturbances and changes in forest species distributions. Productivity changes are adjustments in the productivity of the forest which alter the growth rates of forest species (in either a positive or negative way), while changes in disturbance influence the standing stock of timber and non-timber species through pest infestation, forest fires, wind-throw, and ice damage. Changes in species distribution results from shift in climate, which ultimately alters the optimal geographic location of different species [14].

There have been widespread speculations about climate change all over the world which in most cases not backed by relevant data that has resulted in such questions as Is climate change real or speculative? This research sought to provide the answer to this question particularly as it relates to Taraba State. This study was therefore carried out to determine whether there is a significant change or variation in the amount and pattern of rainfall and temperature in Taraba State from the inception of the State in 1991 to 2011. The analyses of climate change indicators (particularly rainfall and temperature) in the study area are is of paramount importance to the people of the State. As an agrarian State, climate change will have negative impacts on the overall economy of the State. Therefore, this study was to throw more light on whether there is significant variation in the climate of the State judging from the analyses of rainfall and temperature figures. This will enable the people to take precautions against the possible effects of climate change in the area.

2. Methodology

2.1. The Study Area

Taraba State is located in the North-East geographical zone of the country, with its head-quarters in Jalingo. It has sixteen (16) Local Government Areas (LGAs). The State has a total land mass of 51,000 kilometer square. It lies roughly between latitude 60301 and 9o361N and longitude 90101and 11051E. It is bounded on the North-East by Adamawa State and the West and South-East by Plateau and Benue States respectively. On its east border is the Republic of Cameroun. According to the 2006 Census figures released by the National Population Commission (NPC), Taraba State has a population of 2, 294, 800 people [16].

The temperature of Taraba State ranges between 33°C and 37°C; however, in the driest month (March), it could rise to 40°C. The amount of rainfall in the State ranges between 1350mm in the North and 1650mm in the South. The rainy season starts in April and ends in October, while the dry season begins in November and terminates in March. The dry season reaches its peak in January and February when the dusty North-East trade wind blows across the State. The climate, soil and hydrology of the State provide a conducive atmosphere for the cultivation of most staple food crops, grazing lands for animals and fresh water for fishing and forestry. As a result of its agrarian nature, the predominant population of the State engages in farming as an occupation. About three quarters (75%) of the people are farmers while an estimated one quarter (25%) are engaged in other economic activities [15].

The vegetation of Taraba state comprises of three types of vegetation zones namely: the guinea savannah, which is marked mainly by forest and tall grass is found in the Southern part of the state like Wukari, Takum and Dunga, the sub-sudan type characterized by short grasses is found in Jalingo, Lau, and Ardo-kola, interspersed with short trees, while the semi-temperate zone is found in the central part of the State [15].

2.2. Data Collection and Analyses

The data used for this research was secondary data of monthly rainfall and temperature from 1991 to 2011 which were obtained from the Nigerian Meteorological Agency, Jalingo, Taraba State. The data obtained were analyzed using both one way and two way analysis of variance (ANOVA) with mean separation by Fischer’s Least Significance Difference (LSD). All probability levels were at 5% level of significance. The statistical package used was Genstat Discovery Edition 4.

3. Results

3.1. Mean Annual Maximum Temperature (°C)

The results on maximum temperature are presented in Table 1 and Figure 1. There were no significant differences noticed and the temperature trend remained somewhat stable since 1991 to 2011. However, a gradual increase was noticed in the years 1998 (Tmax(°C) = 34.02±3.14), 2003 (Tmax (°C) = 34.60±3.21), 2006 (Tmax(°C) = 34.23±3.33), 2009 (Tmax(°C) =34.04 ±3.10) and 2010 (Tmax(°C) = 34.42±3.44). A slight drop was also experienced in the maximum temperature of 1992 (Tmax(°C) = 32.99±2.11) and 1994 (Tmax(°C) = 32.85±2.66).

3.2. Mean Annual Minimum Temperature (°C)

As indicated in Table 1, the results on minimum temperature showed no significant differences. There was a slight increase in the minimum temperature in 1998 (Tmin (°C) = 23.08±2.39) and2005 (Tmin (°C) = 23.38±2.59).

3.3. Temperature Range (°C)

Results on temperature range within the period of study (1991 - 2011) also recorded no significant differences at 5% level of probability even though the results were fluctuating (Table 1, Figure 1). There was a slight rise in the temperature range in 2003 (Trange (°C) = 12.01± 3.84).

3.4. Rainfall (mm)

The results on rainfall as indicated on Table 1 and Figure 2 revealed that there were no significant differences in the rainfall distribution for the periods under study (1991-2011). Although a slight increase in rainfall distribution was recorded in 1993 (113.30 ± 109.70mm) and 2009 (129.00 ± 128.60mm), statistically, the differences were not significant.

Table 1. Mean Annual Temperature and Rainfall Values in Taraba State from 1991-2011.

Year Tmin (°C) Tmax(°C) Trange (°C) Rainfall (mm)
1991 22.58±2.34 33.27±2.70 10.69±3.59 88.47±88.46
1992 22.06±2.33 32.99±2.11 11.00±3.37 78.78±75.56
1993 22.66±2.08 33.03±2.02 10.37±2.49 113.30±109.70
1994 22.48±2.41 32.85±2.66 10.82±2.94 84.02±93.91
1995 22.46±2.59 33.70±2.70 11.24±3.40 102.70±108.50
1996 22.04±3.18 33.38±3.12 11.34±4.52 112.20±115.50
1997 22.34±2.04 33.15±2.01 10.81±2.88 72.58±78.15
1998 23.08±2.39 34.02±3.14 10.20±4.36 75.10±83.66
1999 22.83±2.40 33.73±2.56 10.91±3.04 90.92±94.83
2000 22.47±2.04 33.53±2.65 11.07±3.12 76.93±83.23
2001 22.27±2.81 33.89±2.94 11.62±3.88 85.15±110.40
2002 22.66±2.68 33.52±2.83 10.86±3.65 103.70±109.10
2003 22.51±2.32 34.60±3.21 12.01±3.84 59.88±66.83
2004 22.30±2.13 33.97±2.95 11.68±3.98 69.50±84.54
2005 23.38±2.59 33.87±3.16 10.49±3.42 71.03±78.54
2006 22.89±2.90 34.23±3.33 11.34±3.86 76.97±91.23
2007 22.54±2.33 33.82±3.04 11.28±3.82 79.32±71.87
2008 22.74±1.92 33.73±2.66 10.99±3.02 102.80±109.00
2009 22.49±2.36 34.04±3.10 11.55±3.85 129.00±128.60
2010 22.34±2.87 34.42±3.44 10.71±4.27 82.60±111.60
2011 22.63±2.33 33.85±3.08 11.37±3.28 76.85±87.44

Figure 1. Mean Annual Temperature (°C).

Figure 2. Mean Annual Rainfall (mm).

4. Discussion

This study has revealed a steady rise in temperature in Taraba State during the period under review even though significant differences were not observed. This is observed is in agreement with the global trend [2]. Similarly, [17] also recorded a slight difference in temperature within the late 1940s and early 1960s in Nigeria. The rise in the minimum temperature also agreed with [18] that the earth has warmed by 0.6±0.2°C on the average since 1900. The findings also conform to those of [19] who reported that the climatic records and the statistical manipulation of daily records of temperature, rainfall and other parameters have shown considerable variations over the years.

The rise in temperature range recorded in the study was in conformity with [20], that in Africa, it has been predicted that by 2100, temperatures could rise between 2°C to 6°C relative to what is obtained at present. Despite the fact that that there were no significant differences in the trends, the area under study (Taraba State) still experienced some level of warmth within the years of study (1991-2011). It is worth mentioning that if the temperature trends continue to increase, there is the possibility of Taraba State experiencing a warmer climate in the near future?

The increase in the amount of rainfall recorded in Taraba State within the period under study agrees with [20] who predicted that there would be corresponding increases in mean global precipitation (from 2.5 – 5.1%) with regional differences that include significant localized reductions in annual precipitation. Also, the distribution of rainfall across the months showed higher concentrations mostly around July, August and September in most of the years. Some of the years may not have much rainfall, but because of such concentration of rainfall intensity, the soil may not be able to accommodate moisture any longer, and this could lead to high runoff that makes the volume of water in the rivers rise and consequently overflow as flood, causing all sorts of destruction; as has been experienced severally in the study area (Taraba State). This indicates that the effects of climate change could be enormous all over the world. For example, [21] wrote that United States will suffer a wide range of increasingly extreme weather events in the coming decades as a result of global warming from drought and excessive heat to wildly destructive hurricanes and record floods triggered by intense rains. Furthermore, [22] noted that impacts of climate change include increasing water scarcity and flood risk, along with decline in water quality.

5. Conclusion

Slight variations were noticed in the temperature trends (maximum, minimum and temperature range) and also in the rainfall distribution within the period under investigation (1991 and 2011). The variations in temperatures (maximum, minimum and range) and the rainfall distribution in the study area (Taraba State) showed that climate change is unequivocal and climate change indicators are becoming stronger; and therefore, the effects of climate change on forest resources and the environment as a whole are generally becoming threatening in the study area (Taraba State).

Recommendations

To forestall the possible menace of climate change in the study area, the following are hereby recommended:

Policies and subsidy programmes supporting private forestry management and reforestation should be put in place.

Ministry of environment should enforce various laws on conservation and proper management of the environment.

There should be the integration of climate change impacts information into the general planning process; and

There is need for a widespread enlightenment of the citizens on climate change to enable them to change some of the human behaviours contributing to climate change.


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