首页> 外文期刊>Climatic Change >Assessing the site-specific impacts of climate change on hydrology, soil erosion and crop yields in the Loess Plateau of China
【24h】

Assessing the site-specific impacts of climate change on hydrology, soil erosion and crop yields in the Loess Plateau of China

机译:评估中国黄土高原气候变化对水文,土壤侵蚀和农作物产量的特定地点影响

获取原文
获取原文并翻译 | 示例
       

摘要

Climate changes may have great impacts on the fragile agro-ecosystems of the Loess Plateau of China, which is one of the most severely eroded regions in the world. We assessed the site-specific impacts of climate change during 2010–2039 on hydrology, soil loss and crop yields in Changwu tableland region in the Loess Plateau of China. Projections of four climate models (CCSR/NIES, CGCM2, CSIRO-Mk2 and HadCM3) under three emission scenarios (A2, B2 and GGa) were used. A simple spatiotemporal statistical method was used to downscale GCMs monthly grid outputs to station daily weather series. The WEPP (Water and Erosion Prediction Project) model was employed to simulate the responses of agro-ecosystems. Compared with the present climate, GCMs projected a −2.6 to 17.4% change for precipitation, 0.6 to 2.6°C and 0.6 to 1.7°C rises for maximum and minimum temperature, respectively. Under conventional tillage, WEPP predicted a change of 10 to 130% for runoff, −5 to 195% for soil loss, −17 to 25% for wheat yield, −2 to 39% for maize yield, −14 to 18% for plant transpiration, −8 to 13% for soil evaporation, and −6 to 9% for soil water reserve at two slopes during 2010–2039. However, compared with conventional tillage under the present climate, conservation tillage would change runoff by −34 to 71%, and decrease soil loss by 26 to 77% during 2010–2039, with other output variables being affected slightly. Overall, climate change would have significant impacts on agro-ecosystems, and adoption of conservation tillage has great potential to reduce the adverse effects of future climate changes on runoff and soil loss in this region.
机译:气候变化可能会对中国黄土高原脆弱的农业生态系统产生巨大影响,而黄土高原是世界上受侵蚀最严重的地区之一。我们评估了2010-2039年气候变化对中国黄土高原长武高原地区水文,土壤流失和农作物产量的特定地点影响。在三个排放情景(A2,B2和GGa)下,使用了四个气候模型(CCSR / NIES,CGCM2,CSIRO-Mk2和HadCM3)的投影。使用一种简单的时空统计方法将GCM的每月网格输出缩减为站点的每日天气序列。 WEPP(水和侵蚀预测项目)模型用于模拟农业生态系统的响应。与目前的气候相比,GCM预测降水变化为-2.6至17.4%,最高和最低温度分别升高0.6至2.6°C和0.6至1.7°C。在常规耕作下,WEPP预测径流变化为10%到130%,土壤流失-5%到195%,小麦单产-17%到25%,玉米单产-2%到39%,植物-14%到18%。蒸腾作用,2010-2039年两个坡度的土壤蒸发量为−8至13%,土壤水储备的−6至9%。但是,与当前气候下的传统耕作相比,保护性耕作在2010-2039年间会将径流量降低-34%至71%,将土壤流失减少26%至77%,其他产出变量也会受到轻微影响。总体而言,气候变化将对农业生态系统产生重大影响,采用保护性耕作法有很大的潜力来减少未来气候变化对该地区径流和土壤流失的不利影响。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号