Simulation of agricultural water supply and demand at irrigation district under climate change using STELLA.

Climate change has significant influences on irrigation water demand (IWD) and available irrigation water supply (IWS), which poses grave challenges to farmers and administrators of agriculture and water resources. Due to the complexity and uncertainties from climate, agriculture and water systems, only a few studies have combined these systems together, especially at irrigation district scale. Furthermore, most climate change scenarios (CCS) are continuous time series with uncertainties, meanwhile the corresponding CCS of the typical hydrological years are deficient. Thus it is difficult for the administrators from water sectors and agriculture to make positive responses to climate change. The object of the study was to provide an approach to estimate and assess the influences of climate change on IWS and IWD systems in irrigation district. The study area was a typical northern irrigation district of China, the Baojixia Irrigation District. The model considering IWD, IWS and CCS was developed using system dynamics software i.e. structure thinking experimental learning laboratory with animation (STELLA). There were four function modules: IWDM, IWSM, CCSM and WSDBI. CCSM included the reference crop evapotranspiration (ET₀) and the climate factors of future typical hydrological years. Climate factors (i.e. precipitation, air temperature, wind speed, relative humidity and sunshine duration) were predicted using historical data and hydrological frequency calculation principle of inconsistent series. ET₀ was calculated by Penman-Monteith equation from the Food and Agriculture Organization of the United Nations (FAO) based on the predicted climate factors. IWDM calculated the irrigation water demands of main crops (wheat, maize, cotton, cole and apple). Crop water requirement was calculated by a simple soil water balance model including effective precipitation, crop coefficient (Kc) and ET₀. Net irrigation water demand (NIWD) was the sum of crop water requirements multiplied by their planting areas. IWD was NIWD divided by coefficient of irrigation water effective utilization. IWS was the available irrigation water supply which consisted of ground water and surface water (runoff of Weihe River and reservoirs). The runoff was estimated by historical data and hydrological frequency calculation principle of inconsistent series. The outputs were IWD, IWS and a water supply-demand balance index (WSDBI, i.e. the ratio of IWD and IWS), which were used to evaluate the effects of climate change. The model was verified by historical hydro-meteorological and agriculture data from 2000 to 2010. After validation the predicted CCS and IWS were used as inputs for the simulation of the future irrigation water balance conditions. The conclusions of this research are: 1) The water supply and demand model based on STELLA has a good performance and can be a steady approach for agriculture and water resource simulation. The mean relative errors for IWD and WSDBI are both 3.13%. The mean absolute errors for IWD and WSDBI are 3.9×10^-7 m³ and 0.06, respectively. 2) The runoff of Weihe River at Linjiacun station had a significant downward trend at the 0.05 level from 1954 to 2010. It was a jump type of change with its jump range of about -1.43×10^-9 m³ occurred in 1989. Compared with the runoff values of different typical hydrological years from 1954 to 2010, the predicted values from 1989 to 2030 were declined by 40%-55% which caused a large reduction of agricultural water supply. The mean temperature and maximum temperature significantly increased meanwhile relative humidity and wind speed significantly decreased at the 0.05 level during 1981-2010. 3) Compared with 2010, the simulation values of IWD in 2030 for wet year (P=25%), normal year (P=50%) and dry year (P=75%) increased by 1.08×10^-8, 1.29×10^-8 and 1. 21×10^-8 m³ respectively, meanwhile the corresponding values of WSDBI increased by 14.46%, 11.70% and 9.06% respectively. The simulation indicated that the IWD and WSDBI increased dramatically under the synthetic action of meteorological factors in future. The supply could not meet the demands except wet years and the situation could be worse over the time, so effective measures should be taken in water resource and agriculture planning and management. This research can provide the reference for assessing the effect of climate change on agricultural water supply and demand in the irrigation district. [ABSTRACT FROM AUTHOR]