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The impacts of climate change on agricultural production systems in China

机译:气候变化对中国农业生产系统的影响

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Climate change can bring positive and negative effects on Chinese agriculture, but negative impacts tend to dominate. The annual mean surface temperature has risen about 0.5-0.8 A degrees C. The precipitation trends have not been identified during the past 100 years in China, although the frequency and intensity of extreme weather/climate events have increased, especially of drought. Water scarcity, more frequent and serious outbreaks of insects and diseases, and soil degradation caused by climate change have impacted agro-environmental conditions. However, temperature rise prolonged the crop growth seasons and cold damages have reduced in Northeast China. The projection of climate change indicates that the surface temperature will continue to increase with about 3.9 to 6.0 A degrees C and precipitation is expected to increase by 9 to 11 % at the end of 21st century in China. Climate warming will provide more heat and as a consequence, the boundary of the triple-cropping system (TCS) will extend northwards by as much as 200 to 300 km, from the Yangtze River Valley to the Yellow River Basin, and the current double-cropping system (DCS) will move to the central part of China, into the current single cropping system (SCS) area which will decrease in SCS surface area of 23.1 % by 2050. Climate warming will also affect the optimum location for the cultivation of China's main crop varieties. If no measures are taken to adapt to climate changes, compared with the potential yield in 1961-1990, yields of irrigated wheat, corn and rice are projected to decrease by 2.2-6.7 %, 0.4 %-11.9 % and 4.3-12.4 % respectively in the 2050s. Climate warming will enhance potential evaporation and reduce the availability of soil moisture, thus causing a greater need for agricultural irrigation, intensifying the conflict between water supply and demand, especially in arid and semi-arid areas of China. With adequate irrigation, the extent of the reduction in yield of China's corn and wheat can be improved by 5 % to 15 %, and rice by 5 % or so than the potential yield in 1961-1990. Adaptive measures can reduce the agricultural loss under climate change. If effective measures are taken in a timely way, then climate change in the next 30-50 years will not have a significant influence on China's food security.
机译:气候变化可以给中国农业带来正面和负面影响,但负面影响往往占主导地位。年平均地表温度上升了约0.5-0.8 A摄氏度。尽管极端天气/气候事件的频率和强度有所增加,尤其是干旱,但过去100年来中国没有发现降水趋势。缺水,更频繁,更严重的昆虫和疾病暴发以及气候变化导致的土壤退化已经影响了农业环境条件。但是,温度升高延长了农作物的生长季节,而东北地区的冷害有所减少。气候变化的预测表明,到21世纪末,中国的地表温度将继续升高,达到3.9至6.0 A摄氏度,而降水量预计将增长9至11%。气候变暖将提供更多的热量,因此,三作系统的边界将从长江流域到黄河流域向北延伸200至300公里,目前,种植系统(DCS)将移至中国中部,进入目前的单一种植系统(SCS)区域,到2050年,该区域的SCS表面积将减少23.1%。气候变暖还将影响中国种植的最佳地点主要农作物品种。如果不采取任何措施来适应气候变化,则与1961-1990年的潜在单产相比,预计灌溉的小麦,玉米和大米的单产将分别下降2.2-6.7%,0.4%-11.9%和4.3-12.4%在2050年代。气候变暖将增加潜在的蒸发并减少土壤水分的供应,从而引起对农业灌溉的更大需求,加剧了供需之间的矛盾,特别是在中国的干旱和半干旱地区。通过适当的灌溉,与1961-1990年的潜在产量相比,中国的玉米和小麦的减产幅度可以提高5%至15%,水稻的减幅约为5%。适应性措施可以减少气候变化下的农业损失。如果及时采取有效措施,那么未来30至50年的气候变化将不会对中国的粮食安全产生重大影响。

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