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Trend analysis of effective precipitation in different growth stages of winter wheat in Huaihe River Plain

机译:淮河平原冬小麦不同增长阶段有效降水的趋势分析

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摘要

The Huaihe River Plain (HRP) is one of the main planting areas of winter wheat in China. Uncertain and erratic distribution of precipitation and the shortage of water resources are the major limitations to crop growth in this region. In this study, the spatial and temporal distributions of effective precipitation during the different growth stages of winter wheat in the HRP were examined using a daily precipitation time series of 53 years (1961/1962 similar to 2013/2014) from 42 meteorological stations. The effective accumulative temperature index method was used to interpolate the winter wheat growth period data (recorded by 4 representative agro-meteorological stations). The Mann-Kendall method was used to check the statistical significance of the trends. The following conclusions are based on these results. (1) The effective accumulative temperature index method can be used to interpolate the observed data. (2) The effective precipitation results show downward trends with magnitudes of 0 similar to- 6 mm/decade for the majority of the stations during certain stages (the tillering date to the jointing date, the jointing date to the heading date, and the entire growth period). (3) Most of the stations show strong downward trends during the growth stages corresponding to the tillering date to the jointing date and the jointing date to the heading date but show insignificant trends during other stages. (4) The spatially averaged effective precipitation data show very strong downward trends during the tillering to heading stage and weak downward trends over the entire growth period.
机译:淮河平原(HRP)是中国冬小麦的主要种植区之一。降水不确定和不稳定分布和水资源短缺是该地区作物增长的主要限制。在这项研究中,使用来自42个气象站的每日降水时间序列(1961/1962),检查了HRP中冬小麦不同生长阶段的有效降水的空间和时间分布。有效的累积温度指数方法用于插入冬小麦生长期数据(由4个代表农业气象站记录)。 Mann-Kendall方法用于检查趋势的统计显着性。以下结论是基于这些结果。 (1)有效的累积温度指数方法可用于插值观察到的数据。 (2)有效降水结果表明,在某些阶段的大多数车站(在拟订日期,向标题日期的分蘖日期和整个阶段的分蘖日期以及标题日期的分蘖日和整个日期,以及整个阶段)的下降趋势下降趋势生长期)。 (3)大多数车站在对应于联合日期的分蘖日和向前日期的分蘖日与分蘖日相对应的增长阶段的强劲下降趋势,但在其他阶段展示了微不足道的趋势。 (4)空间平均的有效降水数据显示在分蘖过程中出现非常强大的下降趋势,并在整个增长期间疲弱的下行趋势。

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  • 来源
    《Theoretical and applied climatology》 |2019年第4期|2043-2056|共14页
  • 作者单位

    China Inst Water Resources & Hydropower Res State Key Lab Simulat & Regulat Water Cycle River 1 Fuzing Rd Beijing 100038 Peoples R China|Tsinghua Univ Dept Hydraul Engn 30 Shuangqing Rd Beijing 100084 Peoples R China;

    China Inst Water Resources & Hydropower Res State Key Lab Simulat & Regulat Water Cycle River 1 Fuzing Rd Beijing 100038 Peoples R China;

    China Inst Water Resources & Hydropower Res State Key Lab Simulat & Regulat Water Cycle River 1 Fuzing Rd Beijing 100038 Peoples R China;

    Tianjin Univ State Key Lab Hydraul Engn Simulat & Safety 92 Weijin Rd Tianjin 300072 Peoples R China;

    China Inst Water Resources & Hydropower Res State Key Lab Simulat & Regulat Water Cycle River 1 Fuzing Rd Beijing 100038 Peoples R China;

    China Inst Water Resources & Hydropower Res State Key Lab Simulat & Regulat Water Cycle River 1 Fuzing Rd Beijing 100038 Peoples R China;

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