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Hydrothermal change in winter wheat-producing area in Northern Anhui of China and its impact on winter wheat production

机译:皖北冬小麦产区热液变化及其对冬小麦产量的影响

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Generally speaking, in the context of global climate change, the water shortage in northern Anhui winter wheat-producing area will become increasingly serious. The current winter wheat high-yield heavily depended on groundwater irrigation which is not sustainable. Therefore, water interception and storage of the flood season precipitation should be considered from strategic perspectives to solve the water supply problem for winter wheat irrigation. In this article we evaluated the temperature, evaporation, precipitation and other data in various historical periods from major weather stations of main winter wheat –producing area in northern Anhui to study the variation trends of precipitation, evaporation and dryness in winter wheat growing season. We also analyzed their impact on winter wheat production. Our results showed that the northern Anhui area is sensitive to the global weather change and the temperature variation in synchronization with the general trend of global warming. The temperature has raised about 1.8 oC since the 1950s of last century, which is higher than the global average increase. In accordance to the temperature rise, evaporation was increased 3 to 5%, with a maximum in February and May. There was no significant change in precipitation in the area, but the non-uniformity of precipitation was enhanced and the proportion of short-term heavy rains tended to increase in the annual precipitation. 24 h maximum rainfall usually accounted for 10 to 30% and the process (storm) precipitation for more than 50% of annual precipitation, with hourly rainfall reaching up to 80 mm or over. The rainfalls per unit time during heavy precipitation are far more than most soil absorption rates. Most precipitations are lost in the form of runoffs and can not effectively replenish soil water and large runoff formations result in a large number of local floods. In total, the uneven rainfall and increased evaporation led to water shortage in this agricultural area which was detrimental to winter wheat production.
机译:总体而言,在全球气候变化的背景下,皖北冬小麦产区的缺水将越来越严重。当前的冬小麦高产严重依赖于地下水灌溉,这是不可持续的。因此,应从战略角度考虑拦截和存储汛期降水,以解决冬小麦灌溉的供水问题。本文评估了皖北主要冬小麦产区主要气象站不同历史时期的温度,蒸发,降水和其他数据,以研究冬小麦生长季节降水,蒸发和干燥的变化趋势。我们还分析了它们对冬小麦产量的影响。我们的研究结果表明,安徽北部地区对全球天气变化和温度变化敏感,并且与全球变暖的总体趋势同步。自上世纪1950年代以来,温度已升高约1.8 oC,高于全球平均水平。随着温度的升高,蒸发量增加了3%至5%,2月和5月最高。该地区的降水没有显着变化,但降水的不均匀性得到增强,年降水量中短期暴雨的比例有增加的趋势。 24小时的最大降雨量通常占10%至30%,过程(暴风)降水占年降水量的50%以上,每小时降雨量可达80毫米或以上。暴雨期间每单位时间的降雨量远远超过大多数土壤吸收率。大多数降水以径流的形式流失,无法有效补充土壤水,大量径流形成导致大量局部洪水。总体而言,降雨不均和蒸发增加导致该农业区缺水,这不利于冬小麦的生产。

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