The Analysis of Spring Precipitation in Semi-Arid Regions: Case Study in Iran ()

Hossein Ali HASANIHA, Majid MEGHDADI

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**DOI: **10.4236/iwarp.2010.21008
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In this study, Zanjan from Iran has been chosen from among all the semi-arid regions of world, which has Synoptic station and statistical data since 1955. Spring and monthly precipitations are also provided in the period of 1956-2005. First, all data has been controlled by double mass method with the help of adjacent stations, and then it was normalized by the box-cox transformations method. The global SPI index was calculated for all months and spring, also drought and wet periods were determined and finally compared. In the drought category view, spring months have represented the great similarities. The moving averages are represented all months and spring’s precipitations such as three years, five years, seven years and nine years are shown. Statistical period was observed and analyzed based on five periods of ten years, and results precipitation with more than 5mm and 10mm has gradually decreased on April. However the number of days with precipitation has increased. The calculated spring precipitations and all of the atmospheric factors represented the dependence of this model to maximum average of spring temperature and relative humidity of spring and winter by the use of multi variable regression method. The predicted precipitation of spring also showed the gradual decline of precipitation in the next 30 years by the arima model.

Keywords

Iran, Semi-Arid Regions, Precipitation, Drought, Box-Cox Transformations Method, Arima Model

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Ali HASANIHA, H. and MEGHDADI, M. (2010) The Analysis of Spring Precipitation in Semi-Arid Regions: Case Study in Iran. *Journal of Water Resource and Protection*, **2**, 69-76. doi: 10.4236/iwarp.2010.21008.

1. Introduction

The semi-arid regions involve the great part of the earth’s all arid regions. Nowadays, the study of these regions is one on the most important studies; especially in the last two decades, where there is repetitive drought as a result of shortage of precipitations [1]. These shortages have caused some changes that tend to have influence on these regions. The lack of precipitation’s time distribution is one of the features of the regions, so that there is a great degree of precipitations in the seasons other than the required seasons and can not be controlled. The shortage precipitations and repetitive drought in the last two decades made the rural people to immigrate from villages to cities. Also, the cultivating and animal husbandry has been under losses. These immigrations tend to great problems in the cities’ management. The shortage of the precipitations causes some problems in providing beverage water of cities and industries’ water. As a result of this issue stores and dams become dry and the surface of underground canals began to decline in terms of excessive use. Consequently, the study of precipitations trend and acquaintance of their condition in this period is more useful. In this study, our focus is on the spring precipitations in the semi-arid regions of the world.

Semi-arid regions’ importance is because of their capacity of dry farming. Also, the great amount of these regions’ precipitations in the spring become in the form of rainstorm which is out of control. Therefore acquaintance with the precipitations trend of these regions, in terms of number of factors such as amount, rate, continuousness, recurrence, maximum, minimum degree and day of precipitations, can lead to the correct and proper planning [2]. In this respect we can have proper planning of watering and dry farming, filling of dam, saving superficial water sources, distributing of the flood waters, feeding groundwater tables, preventing floods, and overflows, soil protection and watershed.

2. Materials and Methods

2.1. The Study Site

A semi-arid climate or steppe climate generally described

Figure 1. Arid and semi-arid regions of the world.

Figure 2. Iran and the location of Zanjan.

climatic regions that received low annual precipitation (250-500 mm or 10-20 in). A more precise definition was given by the Köppen climate classification that treated steppe climates (BS) as intermediates between the desert climates (BW) and humid climates in ecological characteristics and agricultural potential [3]. The Köppen climate classification allows adjustments for temperature and for seasonality of precipitation, effectively excluding forested regions. (In the tables and figures hereafter, the statistics and information belongs to Zanjan).

In this study, we have chosen Zanjan synoptic station where is one of the semi-arid regions of the world in order to observe spring precipitations’ trend in these kinds of areas. Figure 1 represents the semi-arid regions of the world and Figure 2 shows Iran’s geographical map in which Zanjan is specified. Zanjan is located in the North-West of Iran which has 29, 48º longitude and 36, 47º latitude and 1663.6 ^{m}^{ }height of see surface [4].

The average precipitation in a year reached to 313.1 ^{mm} in Zanjan and its average temperature was 10º C in a year, it is necessary to say that the number of glacial days is 117 and the average of evapotranspiration reached to 1025 ^{mm} during a year.

Near to 238 million cube meter of the whole amount of Zanjan precipitation that equaled to 1157 million cube meter, was the same as 21 percent of the whole amount of precipitation of this area, in which there was no uses and even in some cases it caused to some material and financial damages such as demolition of agricultural lands and gardens, institutions, buildings, and communication means [1].

2.2. Used Method

2.2.1. Double Mass Method

One of the common graphic methods which are used for making sure of the homogeneity of data is double mass method. This method is usually used for homogenizing of data related to the precipitation and flowing waters [5].

If we had hydrologic time series data in the condition that they had any periodic and non-periodic changes, we could call those data as stationary data. There was always the stationary (fixed) amount of mean and variance if some other identical data was added to them. However, in some cases where the data are not similar we should homogenize them first or make sure they are homogeneous.

2.2.2. The Box-Cox Transformations Method

The most commonly used symmetry-producing transformations are the two closely related functions;

(1)

(2)

Here “Spread” is some resistant measure of dispersion, such as the “Inter-Quantile range” or “Median absolute deviation”. The Hinkley is used to decide among power transformations essentially by trial and error, by computing its value for each of a number of different choices for [6].

(3)

(4)

(5)

In the aforementioned method, data are normalized. In other words, data are not normal in %99 of cases and all of the time series of data, and central norms such as mean, median and mode have some differences however they cover one another in the vertex. To analyze data, first we should normalize them.

Normal or Gaussian distribution Law is:

(6)

where:

π = 3.14, e = 2.72, µ = mean and σ = variance.

All normal averages are similar and bell shaped and their difference is just in the amount of µ and σ. We assign λ to different numbers in box-cox transformations method formula and then calculate d_{X}. The value of d_{X} is calculated by trial and error. The value of d_{X}_{ }is usually acceptable up to 0.01. In order to normalize the data, we do analyzing it near to 0.00 and make sure that all data are normalized %100.

2.2.3. The Standardized Precipitation Index (SPI)

To calculate the SPI, a long-term precipitation record at the desired station was first fitted to the probability of distribution (e.g. gamma distribution), which was transformed into a normal distribution later so that the mean SPI is zero. The SPI might be computed with different time steps (e.g. 1 month, 3 months, and 24 months). Positive SPI values indicated greater than mean precipitation and negative values indicated less than mean precipitation [7] (See table 1).

In this research, we used global SPI Index in order to study the drought, and we calculated the SPI precipitations of the months of spring. The above table represented the SPI Index for categorizing of wet and drought periods.

2.2.4. Stepwise Linear Regression

Linear Regression estimated the coefficients of the linear equation, involving one or more independent variables that best predict the value of the dependent variable. Method selection allowed us to specify how independent variables were entered into the analysis. Using different methods, we could construct a variety of regression models from the same set of variables. In Stepwise Linear Regression, the independent variable not in the equation which had the smallest probability of Analysis of Variance (F), was entered at each step, if that probability was sufficiently small. Variables already in the regression equation were removed if their probability of F became sufficiently large. The method terminated when no more variables were eligible for inclusion or removal [8].

This research used multi variable regression-stepwisemethod that existed in SPSS software in order to reach spring precipitations’ model in terms of all the atmosph eric characteristics.

2.2.5. Arima Forcast Model

Arima fitted a box-jenkins arima model to generate forecosts. Arima stands for autoregressive integrated moving

Table 1. The standardized precipitation index values.

average with each term representing steps taken in the model construction until only random noise remained [9].

In this study we used time series and arima model that is a linear model. Ochoa [10] used time series and he divided the method into two groups linear and non-linear models. He mentioned that results of linear models-like arima model – are very better than non-linear models [10].

Table 2. Drought category in different periods.

Figure 3. Drought frequency at different periods.

Figure 4. Spring precipitation SPI values in different periods.

This study was done in Zanjan synoptic station using arima model which exists in Minitab software in order to predict the spring 30 years’ precipitations. By using the past fifty year data, we predicted the coming thirty years precipitations of station.

3. Results and Discussion

The opposite situations of drought categories during 1956–2005 are represented. In four periods, light drought category is replicated more than others (Table 2 and Figure 3). On June there were no intensive categories of drought and all ones were in the mean and slight categories. It is necessary to mention that on May there was lack of most intensive categories; however, all of the categories existed on April.

We have drawn the SPI Index’s value on the different time periods in Figure 4. In this figure, the intense of droughts was the most one on April and the last on June. The accumulation of recurrent drought is well cleared in recent years. In [11] the authors used SPI index to investigate meteorological and hydrological drought to see the surface of groundwater tables and to forecast drought. SPI index was not estimated in different time periods. This index has shown a good correlation with GRI index in which it inspects and forecast the conditions of groundwater tables.

The moving averages of precipitations for the periods of 3, 5, 7 and 9 years of April were represented (Figure 5). In the figures you could find the wet and drought periods more clearly and also the gradual decrease of precipitation during fifty years statistical period. As the nine years moving average represented, the amount of accumulated precipitation of April in Zanjan decreased from 60 ^{mm} to 40^{ mm}.

The moving average of precipitation of 3, 5, 7 and 9 years during the statistical period has been shown in Figure 6. As the average represents, the amount of accumulative precipitation during spring decreased from 110^{mm} to 80 ^{mm}^{ }.

The graph of wet and drought periods during 50 statistical years for all months of spring and also for spring itself is shown in Figure 7. Among four trends of drought period’s representations, we confronted with some similarities between May and spring as a whole.

We analyzed the fifty years precipitation of statistical periods (1956–2005) in terms of ten years periods. Figure 8 represented the change of ten years precipitation for different periods. Although all periods showed gradual decrease during the statistical periods, this trend became clearer on April.

Figure 9 represented the accumulative precipitation of different months of spring in terms of percent. As this figure shows, the amount of spring precipitation on April, May and June are respectively %52.90, %37.85 and % 9.25.

Conflicts of Interest

The authors declare no conflicts of interest.

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