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Multidecadal changes in moisture condition during climatic growing period of crops in Northeast China

机译:东北农作物气候生长期水分状况的数十年变化

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Investigating the spatiotemporal dynamics of agricultural water status during crop growth season can provide scientific evidences for more efficient use of water resources and sustainable development of agricultural production under climate change. In this study, the following were used to evaluate the multidecadal changes in moisture condition during climatic growth period of crops in Northeast China from 1961 to 2010: (1) the daily climate variables gathered from 101 meteorological stations in Northeast China for 1961-2010; (2) FAO (Food and Agriculture Organization) Penman-Monteith equation; (3) 80% guaranteed probability for agro-climatic indicators; and (4) the daily average temperature stably passing 0 degrees C, which is the threshold temperature of climatic growth period for crops. Reference crop evapotranspiration (ET0) and relative moisture index were further calculated. The results showed that Northeast China's climate in the main agricultural areas over the past 50 years was warmer and drier in general, with a growing range and intensity of drought. From 1961 to 2010, when the daily average temperature stably passed 0 degrees C, the average annual total precipitation (P) and ET with 80% guaranteed probability in Northeast China both emerged as decreasing trends with averages of 555.0 mm and 993.7 mm, respectively. However, the decline in P was greater than that of annual total ET0. As a result, the annual relative moisture indices sharply decreased with an average of -0.44, mostly fluctuating from -0.59 to -0.25. As far as spatial distributions were concerned, the inter-regional reductions in P and relative moisture index over the past 50 years were conspicuous, especially in some agricultural areas of central Heilong,jiang Province, northeastern Jilin Province and northeastern Liaoning Province. On the contrary, ET obviously increased in some agricultural areas of central and northwestern Heilongjiang Province (eg. Qiqiha'er, Shuangyashan, Hegang, Suihua, etc.), and northeastern Jilin Province (eg. Baicheng). This indicated that drought existed and was unfavorable for crop growth and development, especially during the period of 2001-2010. This finding revealed that drought was still one of the most important agricultural meteorological disasters in Northeast China. Some countermeasures should be formulated to adapt to climate change. Our findings have important implications for improving climate change impact studies, for breeding scientists to breed higher yielding cultivars, and for agricultural production to cope with ongoing climate change. (C) 2015 Elsevier Ltd. All rights reserved.
机译:调查农作物生长季节农业用水状况的时空动态可以为更有效利用水资源和气候变化下农业生产的可持续发展提供科学依据。本研究利用以下方法评估了1961年至2010年东北农作物气候生长期间水分状况的多年代变化:(1)东北地区101个气象站在1961-2010年期间的每日气候变量; (2)FAO(粮食及农业组织)Penman-Monteith方程; (3)80%的农业气候指标保证概率; (4)日平均温度稳定超过0℃,这是农作物气候生长期的临界温度。进一步计算了参考作物的蒸散量(ET0)和相对湿度指数。结果表明,近50年来,东北地区主要农业地区的气候总体上较为干燥和干旱,干旱的范围和强度也在不断增加。从1961年到2010年,当日平均温度稳定地超过0摄氏度时,东北地区的年平均总降水量(P)和ET有80%的保证概率均呈下降趋势,分别为555.0 mm和993.7 mm。但是,P的下降大于年度总ET0的下降。结果,年度相对湿度指数急剧下降,平均为-0.44,大部分在-0.59到-0.25之间波动。就空间分布而言,过去50年间磷和相对水分指数的区域间下降明显,尤其是在黑龙江中部,江西省,吉林省东北部和辽宁省东北部的一些农业地区。相反,在黑龙江省中部和西北部的一些农业地区(例如齐齐哈尔,双鸭山,鹤岗,Su化等)和吉林省东北部(例如白城),ET明显增加。这表明存在干旱,不利于作物的生长和发育,特别是在2001-2010年期间。这一发现表明,干旱仍然是中国东北地区最重要的农业气象灾害之一。应该制定一些应对气候变化的对策。我们的发现对改善气候变化影响研究,育种科学家培育高产品种以及农业生产以应对持续的气候变化具有重要意义。 (C)2015 Elsevier Ltd.保留所有权利。

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