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Impacts of climate change on water requirements of winter wheat over 59 years in the Huang-Huai-Hai Plain

机译:黄淮海平原59年以来气候变化对冬小麦需水量的影响

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Daily data from 40 meteorological stations in the Huang-Huai-Hai Plain from 1955 to 2013 were analyzed using the Mann-Kendall test and partial correlation to determine the temporal trends of meteorological factors and their impacts on water requirements of winter wheat in different growing periods. Results showed that water requirements during the whole growing period in the Huang-Huai-Hai Plain were between 374 and 485.2 mm with an average of 412 mm in the past 59 years. In general, the value declined by 4 mm per decade. The distribution was ribbon-like, decreasing from the N to the S. Average wind speed, humidity, and sunshine hours declined significantly (α = 0.01, 0.05, and 0.01, respectively). Average vapour pressure and temperature increased significantly (α = 0.01). Only rainfall in Dongtai, Gaoyou, and Zhumadian could meet the water requirement of winter wheat over the whole growing period. Response of crop water requirement (ETc) to meteorological factors change was linear and the order of impact on ETc was vapour pressure, temperature, wind speed, and sunshine hours, while humidity had little impact on ETc. Among the impacting factors, vapour pressure was in positive relation with ETc.
机译:利用Mann-Kendall检验和偏相关分析了黄淮海平原40个气象站1955年至2013年的每日数据,并确定了气象因子在不同生育时期的时间趋势及其对冬小麦需水量的影响。 。结果表明,黄淮海平原整个生长期的需水量在374至485.2 mm之间,在过去59年中平均为412 mm。通常,每十年该值下降4毫米。分布呈带状,从N到S减小。平均风速,湿度和日照小时显着下降(分别为α= 0.01、0.05和0.01)。平均蒸气压和温度显着升高(α= 0.01)。在整个生育期内,只有东台,高邮和驻马店的降雨才能满足冬小麦的需水量。作物需水量(ET c )对气象因子变化的响应呈线性关系,对ET c 的影响顺序为蒸气压,温度,风速和日照时数,而湿度对ET c 的影响很小。影响因素中,蒸气压与ET c 呈正相关。

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