Table of Contents Author Guidelines Submit a Manuscript
The Scientific World Journal
Volume 2014 (2014), Article ID 931515, 10 pages
http://dx.doi.org/10.1155/2014/931515
Research Article

Spatiotemporal Variations of Reference Crop Evapotranspiration in Northern Xinjiang, China

1Agriculture College, Shihezi University, 221 North four Road, Shihezi, Xinjiang 832003, China
2The Key Laboratory of Oasis Ecological Agriculture of Xinjiang Production and Construction Group, Shihezi, Xinjiang 832003, China

Received 1 March 2014; Accepted 14 August 2014; Published 31 August 2014

Academic Editor: Jose Marengo

Copyright © 2014 Jian Wang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract

To set up a reasonable crop irrigation system in the context of global climate change in Northern Xinjiang, China, reference crop evapotranspiration (ET0) was analyzed by means of spatiotemporal variations. The ET0 values from 1962 to 2010 were calculated by Penman-Monteith formula, based on meteorological data of 22 meteorological observation stations in the study area. The spatiotemporal variations of ET0 were analyzed by Mann-Kendall test, Morlet wavelet analysis, and ArcGIS spatial analysis. The results showed that regional average ET0 had a decreasing trend and there was an abrupt change around 1983. The trend of regional average ET0 had a primary period about 28 years, in which there were five alternating stages (high-low-high-low-high). From the standpoint of spatial scale, ET0 gradually increased from the northeast and southwest toward the middle; the southeast and west had slightly greater variation, with significant regional differences. From April to October, the ET0 distribution significantly influenced the distribution characteristic of annual ET0. Among them sunshine hours and wind speed were two of principal climate factors affecting ET0.

1. Introduction

Climate warming is an obvious feature of global climate change [1]. Changes in the distribution of water resource with climate change have a profound impact on human life, production, and ecological environment, which have attracted academic and local government’s attention [2, 3].

Reference crop evapotranspiration () is an important indicator which is used to characterize atmospheric evaporation capacity and evaluate drought degree, vegetation water consumption, production potential, water supply, and demand balance [4, 5]. The Food and Agriculture Organization (FAO) of the United Nations defined the reference crop water consumption as the upper evapotranspiration rate of a hypothetical reference crop, supposing that the plant’s height was at 0.12 m, resistance of plant leaves was fixed at 70 s/m, and emission rate was 0.23, similar to the evaporation capacity of green grassland with wide surface, that is, consistent height, vigorous growth, complete cover ground, and sufficient moisture [68].

Tianshan Mountains, across the center of Xinjiang, divide Xinjiang Uygur autonomous region into south and north parts, while the Northern part is called Northern Xinjiang, characterized by scarce rainfall and dry climate. Shortage of water resource limits sustainable agriculture, animal husbandry, and stable economic development and also changes the local ecological environment. In recent years some studies on spatiotemporal change of in Xinjiang showed up. However, in these papers the emphasis was mostly put on climate and meteorological rate, cumulative departure, Mann-Kendall detection, and geographic information system (GIS) interpolation in a wide range of Xinjiang. And the meticulous research in a limited scope has been very rare [911]. In this paper, we calculated 49 years of in Northern Xinjiang through the Penman-Monteith equation, using 1962–2010 daily meteorological data from 22 meteorological stations in the Northern region. Then we used Mann-Kendall test, Morlet wavelet analysis, and ArcGIS spatial analysis function to study the spatiotemporal variation of in Northern Xinjiang. It would provide a foundation for calculating crop water demand and optimizing water-resource allocation, so as to get a reasonable irrigation system in this region.

2. Data Source and Analytical Methods

Northern Xinjiang includes Urumqi, Altay, Tacheng, Changji, Shihezi, Bole, Yili, and other regions, where Junggar Basin locates between Altai, the most Northern part of Xinjiang, and central Tianshan. Average elevation is 770 meters or so. The climate is temperate continental arid or semiarid. There are four distinct seasons, with average annual temperature −4 to 9°C, 150–200 mm annual precipitation, and annual frost-free period 140–185 days. In this area agricultural production is a major industry. This paper analyzed the meteorological data from 22 weather stations in Northern Xinjiang (the locations are shown in Figure 1) from 1960 to 2010, including average daily maximum temperature, average daily minimum temperature, average daily temperature, daily relative humidity, average wind speed, sunshine hours, and station altitude, latitude, and longitude. The Penman-Monteith formula recommended by the Food and Agriculture Organization of the United Nations was used to calculate reference crop evapotranspiration for Northern Xinjiang: where is reference crop evapotranspiration (mm day−1); is slope vapor pressure curve (kPa °C−1); is net radiation at the crop surface (MJ m−2 day−1); is soil heat flux density (MJ m−2 day−1); is the psychrometric constant (kPa °C−1); is mean daily air temperature at 2 m height (°C); is wind speed at 2 m height (m s−1); is saturation vapor pressure (kPa); and is actual vapor pressure (kPa).

931515.fig.001
Figure 1: Distribution of meteorological observation stations in Northern Xinjiang.

Mann-Kendall [12] test is a nonparametric test method, in which samples do not need to follow a certain distribution patter and will not be affected by the interference of a few of outliers. So it is very suitable for analyzing the nonnormal distribution. It has been wildly used for its wide detection range and high degree of quantitative and convenient calculation meanwhile it can identify when and where the mutation appears while the mutation analysis is carried out. Statistics of UFm algorithm was shown in the reference crop evapotranspiration (ET0). In this paper, given significance level equal to 0.05, after checking the table of normal distribution we could find that the distribution range of value U0.05 was equal to 1.96. If the absolute value of UFm was bigger than U0.05, it indicated that there was a clear trend change sequence. All UFm values were shown in a curve UF. This test sets up two series, a progressive one (UB) and a backward one (UF). The statistic curve, UF, UB, and two straight lines, plus or minus 1.96, were drawn in the same graph. When they exceeded the critical lines, it meant there was a significant upward or downward trend happening. For UF, if the value was greater than 0 it indicated that UF series were rising, conversely downward trend. If the two curves of UF and UB intersected between the critical lines, then the moment of the intersection might be the mutation start time. In this paper Mann-Kendall test was used to analyze mutation and trend of sequence.

Wavelet analysis [13] was developed over nearly 28 years and is a type of signal frequency with localization analysis, used to ascertain local characteristics of periodic change. One can clearly discern a cycle of temporal change by it. So wavelet analysis is very suitable for analyzing multiple time scales. Complex wavelet coefficients more realistically reflect the scale distribution of periodic size and cycles in the time domain, and the Morlet wavelet transform has seen years of development, so they have become turn into mature analysis tools. In this paper the Morlet wavelet was used to study the characteristics of sequence scale and periodicity, with wavelet generating function . Here, is a constant, is the imaginary part units, and is time.

Kriging space interpolation (kriging) is an ArcGIS software geostatistical interpolation method, which has unique advantages in statistics ideological space over the local interpolation method and spatial analysis randomness and structural variables [14]. The essence of the original data and structural characteristics of the variogram is regionalized variables, not the value of sampling-point regionalized variables from linear unbiased optimal estimation [15]. Given the estimated value of any one space variable point and within its sphere of influence, the effective observation values are determined by their respective weights: where is the meteorological observation and is the weight coefficient. The weight coefficients are obtained by ordinary or simple kriging equations. The weight coefficient is determined by the spatial structure of variables. And the spatial structure of variables is expressed in half variant function , that is, where is a distance vector and is the number of data points separated by distance .

3. Results

3.1. Interannual Variability

We obtained annual average of all studied weather stations over 49 years (1962–2010). Figure 2 shows interannual variation curve and linear trend of average in the study area. The annual average was 1407.4 mm with fluctuation range from 1228.4 to 1628.7 mm. The minimum was about 1228.4 mm turning up in 1992 while the maximum was about 1628.7 mm in 1974. The ratio of maximum to minimum was 1.33. The linear trend line indicated that went downward over time with a decrease extent about 1.3 mm/a. The Mann-Kendall test was performed on the sequence. The result showed that statistic was equal to −4.32 and less than −1.96, indicating a significant downward trend (confidence level 95%). Table 1 showed the Mann-Kendall test result of sequence in a confidence level of 95%. values of stations in Fuyun, Beitashan, and Tacheng showed a significant increasing trend while in other sites showed a decreasing trend. According to the above the study area was divided into two regions, that is, decreasing area and increasing area.

tab1
Table 1: Mann-Kendall test of at each meteorological observation station.
931515.fig.002
Figure 2: Annual variation of average in Northern Xinjiang.
3.2. Characterization of Mutations

In order to estimate the significant downtrend of reference crop evapotranspiration in the study area and the relationship between decrease or increase and mutation, mutation analysis of sequence was carried out by means of the Mann-Kendall test (Figure 3). Figure 3(a) showed that the average in the study area began to decline in 1979, and it dropped significantly in 1987. The two curves of UF and UB intersected at about 1983. The average mutation of the study area showed up in this year, indicating a sudden decline in the early 1980s. The sudden decrease was about 128.6 mm. Figure 3(b) showed that the regional-average began to decline in 1979, with a significant reduction beginning in 1987. The mutation point appeared around 1984, with a decrease approximately 160.7 mm. Figure 3(c) showed that the mutation time of average showed up in 2004 in the increasing area and began to rise from 1981 with a sharp rise in 2008 and the increase was about 153.4 mm.

fig3
Figure 3: Mann-Kendall test of average .

Comprehensive analysis of Figures 3(a), 3(b), and 3(c) showed that the mutation time of the reference crop evapotranspiration in reduced area was relatively similar to the whole study area, while that in increased area was totally different from the whole study area.

3.3. Cycle Characteristics

Figures 4(a), 4(b), and 4(c), respectively, represented an average Morlet wavelet transform coefficient (real part) contour map of the study area, decrease area, and increase area. The real part of the wavelet reflected the time-scale signal characteristic at varying times for the strength and phase information. The positive phase represented the period with more than normal, the negative phase represented the period with less than normal, and zero wavelet coefficients corresponded to the mutation point. Figure 4(a) showed that at different time scales, sequence change had different characteristics and the phase structure had a strong cycle around 28 years. On this time scale, there were some increases during 1962–1966, 1977–1997, and 2008–2010. There were decreases during 1967–1976 and 1967–2007, that is, the negative phase. So there was a high-low-high-low-high cycle in the process. Mutation points turned up in 1965 and 2002. Figures 4(b) and 4(c) showed that at different time scales the change characteristics of average in the increase area and decrease area were similar to those in the study area. The results of primary period analysis of in the study area, increase area, and decrease area during 1962–2010 were shown in Table 2. The results showed that both primary period and secondary period of in the reduction area were the same as those in the study area, while only primary period of in the increase area was the same as the study area and secondary period was very close to the study area.

tab2
Table 2: Period statistics.
fig4
Figure 4: Morlet wavelet transform of average ET0.
3.4. Spatial Variation

Using the spatial kriging interpolation method of ArcGIS 9.3 based on spatial rasterization, we obtained values on each grid and also continuous spatial distribution. It provided detailed data for the spatial variation analysis in the Northern agricultural area of Tianshan Mountains, Xinjiang. To analyze the spatial distribution characteristics of mean in many years before and after mutations in the study area, we used Arc GIS 9.3 to map the characteristics by using spatial interpolation (Figure 5). Figure 5(a) showed that before the mutation (1962–1983) spatial distribution characteristics of were that the value of was low in the northeast and southwest, but it was high in the southeast and west. Meanwhile, from the northeast and southwest to the middle slowly increased and the average variation ranges of over many years were 1008.6–2514.6 mm; the high value area in the southeast and west was within 1596.1–2514.6 mm; and the low value area in the northeast and southwest was within 1008.6–1405.3 mm. We could see that there were significant regional differences in the study area. Figure 5(b) showed that after mutation (1984–2010) spatial distribution characteristics were that the in the northeast and southwest was low and the significantly declined compared to it before mutation. The average for many years was in the range of 913.9–2355 mm, with the low value area of the southwest and northeast from 913.9–1191.3 mm and the high value area within 1317.5–1621.8 mm. Therefore, there was a significant difference.

fig5
Figure 5: Spatial distribution of average annual between 1962 and 1983 and 1984 and 2010 in Northern Xinjiang.

Overall, spatial distribution of had a significant change before and after mutation. Reduction areas were as follows. Ili Valley in southwest declined by 92.8–124.8 mm. Altay region in the northeastern Xinjiang declined by 20.8–261.4 mm. Along the north slope area of Tianshan Mountains declined by 86.6–379.5 mm. And the Western declined by 156.6–24.15 mm.

The from April to October accounted for more than 80% of the annual of the main seasonal crop in Northern Xinjiang. Thus, the analysis of the spatial distribution in these months was of great significance. Using Penman-Monteith equation and meteorological data in combination with the monthly-average and the sum from April to October of the study area, the spatial distribution for April to October was produced with ArcGIS 9.3 (Figure 6). Figure 6 showed that the spatial distribution characteristics of : in Midwest and southeast flanks were high, in southwest and northeast were low, and in Midwest and East to the middle were decreasing. changed in the range of 856.5–2207.3 mm, while Midwest and southeast flanks, the high value area, changed in the range of 1201.7–2207.3 mm, northeast and southwest, the low value area, changed in the range of 856.5–1095 mm. It showed distinct regional differences.

931515.fig.006
Figure 6: Spatial distribution of average monthly from April to October of 1962–2010 in Northern Xinjiang.
3.5. Spatiotemporal Variation Causes

spatiotemporal change was affected by a variety of factors. Six important meteorological and topographical factors (altitude) of them were selected in this paper. Factor analysis results were shown in Tables 3 and 4 and Figure 7. Table 3 showed that wind speed and sunshine hours had significant positive correlation with in the study area. Relative humidity and rainfall had highly significant negative correlations with . And wind speed and in the reduction area showed a significant positive correlation, while relative humidity and rainfall had highly significant negative correlations with ET0. In other words, increase, wind speed, sunshine hours, and had highly significant positive correlations, but there was a negative correlation between relative humidity and . According to Table 3, the partial correlation between meteorological factors and , and Table 4, the main meteorological factor trend with time, results showed that decreased mainly because of a significant decline of wind speed. Within the context of the overall decline, ET0 values of Tacheng, Fuyun, and Beitashan with special upward trends were due to wind speed and there was no significant decrease of sunshine hours.

tab3
Table 3: Partial correlation coefficient between and meteorological factors.
tab4
Table 4: Mann-Kendall test of meteorological factors significantly associated with .
931515.fig.007
Figure 7: Tendency of with altitude.

From Figure 7, ET0 decreased with altitude but changed little in space. The linear trend line equation was , with nonsignificant correlation coefficient −0.229. In Northern Xinjiang, elevation was not the main cause of significant regional differences of .

4. Discussion

Many studies on in the northwest of China showed that of Northern Xinjiang was usually around 1800 mm [16, 17]. In this study, the maximum value of in Dabancheng and Alashankou reached 1935.8 mm and 2426.9 mm differently. As far as the reasons were concerned, firstly, previous studies had generally limited number meteorological of stations selected (roughly 13–17 sites) and limited coverage [16, 17]; secondly, “Xinjiang Meteorological Handbook” compiled by Zhang showed that annual average wind speed of Dabancheng was 4-5 m/s, annual average wind speed of Alashankou was up to 6 m/s, and “Baili wind zone” in Eastern of Xinjiang had an average annual wind speed at 5–8 m/s [18]. The wind speed was one of the main meteorological factors affecting and there was a significant positive correlation between them. Therefore, values of those areas were high. Zhang and Pu had found that the of wind line, outlet and the Gobi desert zone in “Baili wind zone” of Eastern Xinjiang was up to 1800–2600 mm, where the was the largest in Xinjiang. It was similar to the conclusions of this study [11].

The multitemporal and spatial variation analysis of revealed that wind speed and sunshine hours were the main influences on in Northern Xinjiang [1922]. Maximum and minimum temperature effects were relatively weak and consistent with earlier studies [2325]. Relative humidity and rainfall had a negative correlation with . This might attribute to that precipitation had increased, relative humidity had gotten high, and climate was becoming warmer and wetter during recent years in Northern Xinjiang [26]. Maximum temperature affected somewhat, but not significantly in Northern Xinjiang in contrast to the traditional perception [13, 27, 28]. This is the “evaporation paradox” phenomenon [29]. Wind had a significant impact on in windy areas. Therefore, farmland shelterbelts and other measures were important to agricultural production in such areas.

Some scholars hold that elevation had a significant influence [20], but this was not significant in the study area. This finding might be due to the complex terrain of Northern Tianshan Mountains, Yili Valley and Junggar basin, Gurbantünggüt Desert, and Altai. Additional research needs to be done to confirm this idea.

Several studies have shown that the development of irrigation in arid zone oasis agriculture has resulted in a reduction in wind speed and an increase in relative humidity. As a consequence of these changes, reference crop evapotranspiration in this region has decreased [30]. While different irrigation systems had different operating modes, irrigation and drainage system could have an influence on the soil moisture in field, farmland microclimate, and crops’ demand for water. In the conventional broad irrigation evapotranspiration was more than spray irrigation, drip irrigation, and other water-saving irrigation modes. Therefore, irrigation modes would have some impacts on the reference crop evapotranspiration [31].

The agriculture in Northern Xinjiang belongs to irrigated agriculture. In the early 1950s the irrigation area of Xinjiang was only 0.6 million hm2 [32]. From the beginning of the 1980s, with the growing investment in water conservancy facilities and construction, irrigation area gradually expanded. In the beginning of 1990s drip irrigation technology was introduced in Northern Xinjiang; the drip irrigation was proven to be the best water-saving irrigation technique in Northern Xinjiang, which has been successfully applied to a variety of crops, such as cotton, corn, tomato, and wheat at present [33]. According to statistics, the amount of water diversion in Northern Xinjiang reached 11.71 billion m3 and the irrigation area peaked up to 1.53 million hm2 in 2009 [34], but it only accounts for about 40% of the irrigated area [34].

In order to further improve the accumulated temperature and reduce evaporation in production, spring sowing of thermophilic crops (cotton, corn, processed tomatoes, etc.) used drip irrigation under film. Compared to the irrigation mode with ditches in the past, this irrigation mode not only reduced the water loss in conveying and water surface evaporation during flood irrigation. Moreover in this mode high irrigation frequency and small amount of irrigation every time made relatively less change in soil moisture before and after irrigation, that is, soil evaporation was almost unchanged; so the dominant factor affecting the crop evapotranspiration was just crop transpiration [35]. Meanwhile, covering film also reduced the surface evaporation in field. Because it formed a different field microclimate, which could have an influence on reference crop evapotranspiration in some extent.

As the drip irrigation mode has great popularization potential, whether it will contribute to the reference crop evapotranspiration change and to what extent in the future is still unknown and needs further exploration and deeper research.

In the recent 49 years in Northern Xinjiang overall showed a downward trend, and annual changes of in the world and most parts of China were consistent [911, 23, 3639]. Thus, if the crop coefficient is unchanged, it will make the annual water need of main crops, such as cotton, wheat, corn, and oil sunflower, decrease. Although this can ease the pressure on agricultural water use in certain extent, but the agriculture in the study area belongs to irrigated agriculture. So Northern Xinjiang should set up a relative optimizing irrigation system based on the different local situation under the context of global climate change.

According to Mann-kendall test results there would be two kinds of change trends with time in Northern Xinjiang. One was increase where three sites were far away from each other, and the other was reducing surrounding the increase area. This phenomenon needs to be further investigated in the future.

5. Conclusions

(1)Time-varying characteristics: The multiyear average was 1407.4 mm in the study area, with a range of 1228.4–1628.7 mm. The results of Mann-Kendall test showed values of 19 weather stations that had a significant downward trend with time while the other three stations had an upward trend. The mutations of average in the study area, reduction area, and increase area appeared, respectively, in 1983, 1984, and 2004. Morlet wavelet analysis showed a corresponding phase structure, with a strong cycle around 28 years. On this time scale, there were increases between 1962 and 1966, 1977and 1997, and 2008 and 2010. Meanwhile there was a decline between 1967 and1976 and 1967 and 2007, that is, the negative phase. There were high-low-high-low-high cycles in the process. The principal cycle was 28a, and the minor cycle was around 15a. The of the reduction area had the same main period and hypoperiod as the study area, and the increase area only had a similar hypoperiod to the study area.(2)The results of spatial variation characteristics showed that compared to the spatial distribution of average before and after mutation, the average values in northeast and southwest of Northern Xinjiang were low while the average of southeast part was high. Before mutations the average ET0 in the northeast and southwest of Xinjiang north to the middle gradually increased. The average spatial distribution from April to October was consistent with the distribution of annual .(3)In general, the main meteorological factors impacting were sunshine duration and wind speed. The values of Tacheng, Fuyun, and Beitashan stations showed significant increasing trend because of nonsignificant declines in sunshine hours and wind speed. Wind speed significantly affected ; so the shelterbelts and other measures to reduce wind speed are very important for agricultural production in Northern Xinjiang and Tianshan regional farmland. With the continuous development of 3S (GIS, RS, and GPS) technologies, their application in the agriculture will become more common and sophisticated. This would give increasingly accurate spatiotemporal variation results of , including those places with complex terrain.

Conflict of Interests

The authors declare that there is no conflict of interests regarding the publication of this paper.

Acknowledgments

The authors appreciate the China Meteorological Bureau for providing meteorological data of Xinjiang. The authors are indebted to a key project of the China National “Twelfth Five-Year” Science and Technology Support Program (2011BAD29B06-1) and the Xinjiang Production and Construction Corps special focus on teaching and scientific research (2060402).

References

  1. IPCC, “Summary for policymakers,” in Climate Change 2007—The Physical Science Basis: Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press, Cambridge, UK, 2007. View at Google Scholar
  2. B. Zhang, H. W. Chen, W. Y. Mao et al., “The elementary assessment of climate change and environment in Xinjiang,” Desert and Oasis Meteorology, vol. 2, no. 4, pp. 1–11, 2008. View at Google Scholar
  3. S. Q. Zhang, Z. C. Pu, X. H. Fu et al., “Effect of climate change on NPP of natural vegetation in Xinjiang,” Arid Zone Research, vol. 27, no. 6, pp. 905–914, 2010. View at Google Scholar
  4. R. G. Allen, L. S. Pereira, D. Raes, and M. Smith, “Crop Evapotranspiration Guidelines for Computing Crop Water Requirements,” FAO Irrigation and Drainage, 56., 1998.
  5. F. Mao, G. Z. Zhang, and X. D. Xu, “Computational method and result comparison about reference crops evapotranspiration quantity,” Using Meteorological Journal, vol. 11, pp. 128–136, 2000. View at Google Scholar
  6. Y. Liu, L. S. Pereira, J. L. Teixeira et al., “The new definition and computational method contrast about reference evapotranspiration,” Water Conservation Journal, no. 6, pp. 27–33, 1997. View at Google Scholar
  7. W. Brutsaert and M. B. Parlange, “Hydrologic cycle explains the evaporation paradox,” Nature, vol. 396, p. 30, 1998. View at Publisher · View at Google Scholar · View at Scopus
  8. A. Thomas, “Spatial and temporal characteristics of potential evapotranspiration trends over China,” International Journal of Climatology, vol. 20, no. 4, pp. 381–396, 2000. View at Google Scholar
  9. Z. C. Pu, S. Q. Zhang, S. L. Wang et al., “Study on the change of annual potential evapotranspiration in the Tianshan Mountainous in recent 36 years and its comparison with that in south Xinjiang and north Xinjiang,” Arid Zone Research, vol. 26, no. 3, pp. 424–432, 2009. View at Google Scholar
  10. Z. C. Pu and S. Q. Zhang, “Study on spatial-temporal variation characteristic of summer half year ET0 in recent 48 years in Xinjiang,” Chinese Journal of Agrometeorology, vol. 32, no. 1, pp. 67–72, 2011. View at Google Scholar
  11. S. Q. Zhang and Z. C. Pu, “Temporal and spatial variation characteristics of reference evapotranspiration in Xinjiang,” Transactions of the Chinese Society of Agricultural Engineering, vol. 27, no. 5, pp. 73–79, 2011. View at Publisher · View at Google Scholar · View at Scopus
  12. Y. Y. Zhao, C. Y. He, H. Yao, Q. Huang, and Y. Yang, “Effect of drought process on natural production function of cultivated land,” Transactions of the Chinese Society of Agricultural Engineering, vol. 25, no. 12, pp. 278–284, 2009. View at Publisher · View at Google Scholar · View at Scopus
  13. X. Chen and T. Jiang, “Suitability analysis of the calculation formulas for monthly potential evapotranspiration in different climatic zones,” Hydrology, vol. 4, no. 5, pp. 1–4, 2004. View at Google Scholar
  14. W. Wu, X. Ma, X. Chen, T. Yang, and A. Zhang, “Temporal-spatial variations of reference crop evapotranspiration in Anhui Province in recent 35 years supported by GIS,” Transactions of the Chinese Society of Agricultural Engineering, vol. 26, no. 2, pp. 251–256, 2010. View at Publisher · View at Google Scholar · View at Scopus
  15. J. G. Shi, C. R. Yan, W. Q. He et al., “Study on spatiotemporal change of evapotranspiration in the yellow river basin,” Arid Zone Research, vol. 24, no. 6, pp. 773–778, 2007. View at Google Scholar
  16. F. M. Zhang and S. H. Shen, “Spatial distribution and temporal trend of reference crop evapotranspiration in China,” Journal of Nanjing Institute of Meteorology, vol. 30, no. 5, pp. 705–709, 2007. View at Google Scholar
  17. Z. C. Pu, S. Q. Zhang, S. L. Wang et al., “Study on the change of annual potential evapotranspiration in the Tian shan mountainous in resent 36 years and its comparison with that in south Xinjiang and north Xinjiang,” Arid Zone Research, vol. 26, no. 3, pp. 424–432, 2009. View at Google Scholar
  18. X. W. Zhang, Xinjiang Meteorological Handbook, China Meteorological Press, Beijing, China, 2006.
  19. J. Li and A. Luo, “Reference crops evapotranspiration quantity from 1961 to 2000 in Xinjiang time change research,” in Proceedings of the 2007 Annual Meeting at the Venue on Climate Change, pp. 1050–1056, Chinese Meteorological Society, EAAP Publication, Beijing, China, 2007.
  20. D. P. Yu, X. Zhang, Y. He, and X. Shi, “Temporal-spatial variations of reference crop evapotranspiration in eastern plateau agricultural region of Qinghai province,” Transactions of the Chinese Society of Agricultural Engineering, vol. 28, no. 2, pp. 66–71, 2012. View at Publisher · View at Google Scholar · View at Scopus
  21. C. Q. Li, K. Q. Hong, and B. G. Li, “Analysis of temporal-spatial variations of reference evapotranspiration during 1965 and 1999 in Hebei Province,” Chinese Journal of Agrometeorology, vol. 29, no. 4, pp. 414–419, 1965. View at Google Scholar
  22. C. Y. Li, J. S. Zhang, P. Meng et al., “Study on temporal variation and fractal characteristics of reference crop evapotranspiration in the Heilonggang Basin,” Chinese Journal of Agrometeorology, vol. 32, no. 1, pp. 81–88, 2011. View at Google Scholar
  23. M. L. Roderick and G. D. Farquhar, “Changes in Australian pan evaporation from 1970 to 2002,” International Journal of Climatology, vol. 24, no. 9, pp. 1077–1090, 2004. View at Publisher · View at Google Scholar · View at Scopus
  24. B. Liu, Z. G. Ma, and Y. G. Ding, “Characteristics of the changes in pan evaporation over Northern China during the past 45 years and the relations to environment factors,” Plateau Meteorology, vol. 25, no. 5, pp. 840–848, 2006. View at Google Scholar
  25. G. Gao, D. L. Chen, G. Y. Ren et al., “Trend of potential evapotranspiration over China during 1956 to 2000,” Geography Research, vol. 25, no. 3, pp. 378–387, 1956. View at Google Scholar
  26. Y. F. Shi, Y. P. Shen, and R. J. Hu, “Preliminary study on signal impact and foreground of climatic shift from warm dry to warm humid in Northwest China,” Journal of Glaciology and Geocryology, vol. 24, no. 3, pp. 219–226, 2002. View at Google Scholar
  27. R. G. Allen, M. Smith, A. Perrier et al., “An update for the definition of reference evapotranspiration,” ICID Bulletin, vol. 43, no. 2, pp. 64–92, 1994. View at Google Scholar
  28. R. K. Goyal, “Sensitivity of evapotranspiration to global warming: a case study of arid zone of Rajasthan (India),” Agricultural Water Management, vol. 69, no. 1, pp. 1–11, 2004. View at Publisher · View at Google Scholar · View at Scopus
  29. Z.-T. Cong, G.-H. Ni, D.-W. Yang, and Z.-D. Lei, “Evaporation paradox in China,” Advances in Water Science, vol. 19, no. 2, pp. 147–152, 2008. View at Google Scholar · View at Scopus
  30. S. J. Han, Q. C. Liu, H. P. Hu, and D. W. Yang, “Impacts of irrigation on annual potential evapotranspiration in Jingtai irrigation district,” Advances in Water Science, vol. 21, no. 3, pp. 364–369, 2010. View at Google Scholar · View at Scopus
  31. X. C. Wu, H. P. Zhou, and J. Q. Zhang, “Study on the irrigated agriculture development and water-saving potential in Xinjiang,” China's Rural Water Conservancy Water Electricity, no. 2, pp. 24–27, 2006. View at Google Scholar
  32. D. I. Cheng, X. C. Lin, and H. J. Ca, “Effects of drip irrigation underneath mulching film on sustainable oasis agriculture in Xinjiang,” Agricultural Research in the Arid Areas, vol. 23, no. 2, pp. 59–62, 2009. View at Google Scholar
  33. Z. X. Zhang, Drip Irrigation Technology and Application of Membrane in the Field, China Water Power Press, Beijing, China, 2012.
  34. Z. Wang, H. P. Zhou, and J. H. Zhang, Xinjiang Agricultural Water Quota Application Technology Research, China's Agricultural Science and Technology Press, Beijing, China, 2012.
  35. B. Cao, “Evapotranspiration rules of cotton in plastic film using drip Irrigation and comparative analysis on five calculation methods of crop evapotranspiration,” Northwest University of Science and Technology, 2003.
  36. C. Chen, Y. M. Pang, X. B. Pan et al., “Analysis on change of reference crop evapotranspiration and climatic influence factors in Sichuan,” Chinese Journal of Agrometeorology, vol. 32, no. 1, pp. 35–40, 2011. View at Google Scholar
  37. X. J. Ji, Y. Y. Zhu, and W. L. Gu, “Analysis on trends in annual reference crop evapotranspiration and its impact climatic factors,” Chinese Journal of Agrometeorology, vol. 34, no. 1, pp. 14–22, 1971. View at Google Scholar
  38. A. Bandyopadhyay, A. Bhadra, N. S. Raghuwanshi, and R. Singh, “Temporal trends in estimates of reference evapotranspiration over India,” Journal of Hydrologic Engineering, vol. 14, no. 5, pp. 508–515, 2009. View at Publisher · View at Google Scholar · View at Scopus
  39. T. Tebakari, J. Yoshitani, and C. Suvanpimol, “Time-space trend analysis in pan evaporation over Kingdom of Thailand,” Journal of Hydrologic Engineering, vol. 10, no. 3, pp. 205–215, 2005. View at Publisher · View at Google Scholar · View at Scopus