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应用ＡＲＩＤＣＲＯＰ模型对黄淮海地区冬小麦气候生产力进行了数值模拟研究，给出了该地区冬小麦气候生产力Ｙｑ分布图，继而研究了水分保持最适状况时的光温生产力Ｙｗ分布状况，在此基础上给出了水分增产力Ｑ（Ｑ＝（Ｙｗ－Ｙｑ）／Ｙｑ）分布图。研究表明，黄淮海地区冬小麦气候生产力变幅在３７５０～９７５０ｋｇ／ｈｍ２之间，总的趋势北低南高，黑龙港地区出现了一个３７５０ｋｇ／ｈｍ２的低值区。水分是黄淮海北部地区冬小麦气候生产力的一个重要限制因子，当水分完全适宜时，南部淮河流域冬小麦气候生产力仅可提高５％～１０％，而黄淮海北部地区气候生产力则可提高７５％～１００％。用黄淮海地区冬小麦高产记录与生产力模拟值进行了对比分析，表明用ＡＲＩＤＣＲＯＰ模型对该地区冬小麦气候生产力进行研究是可行的，该研究为引黄灌溉提供了一定的理论依据。
Using ARIDCROP model to simulate the winter wheat climate productivity in Huang-Huai-Hai region, the Yq distribution of winter wheat productivity in the region was given, and then the distribution of light-temperature productivity Yw in the optimum condition of moisture was studied. On this basis, Out of the water yield Q (Q = (Yw-Yq) / Yq) distribution. The results show that the climate productivity of winter wheat in Huang-Huai-Hai region fluctuates between 3750-9750kg / hm2. The general trend is north and south high. There is a low value area of 3750kg / hm2 in Heilongjiang. Moisture is an important limiting factor for winter wheat climate productivity in the north of the Huang-Huai-Hai region. When the water is suitable, the climate productivity in the southern Huaihe River can only increase by 5% ~ 10%, while the climate productivity in the north of Huang-Huai-Hai can increase by 75% ~ 100 %. Comparison of high-yield winter wheat records and simulated productivity values in Huang-Huai-Hai region shows that it is feasible to use ARIDCROP model to study the climatic productivity of winter wheat in this area. This study provides a theoretical basis for irrigating.