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Spatiotemporal variation of drought frequency of winter wheat in Hebei Province

机译:河北省冬小麦干旱频率的时空变化

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Based on the daily meteorological data of 23 meteorological stations during 1960–2013 across the study area and its surroundings, the spatiotemporal variation of drought frequency of winter wheat is investigated by using the crop water deficit index (CWDI). The results show that during the entire growth period, the sequence of drought frequency is extreme drought > severe drought > moderate drought > light drought. The frequencies of moderate and severe droughts presented increasing trends after 1995, whereas light and extreme droughts showed decreasing trends during the same period. In addition, the drought frequency decreased from seeding to maturation, and the fluctuation of drought frequency tended to intense with an increase in the level of drought, especially during green-up to jointing. During that period, the frequency of extreme drought presented a decreasing trend after 1995, whereas an increasing trend was detected in severe drought conditions. Moreover, significant spatial differences in the trend of drought frequency were detected. For example, severe drought presented an increasing trend in the northwest parts of the study area and a decreasing trend in the east. Increasing and decreasing trends in extreme drought were detected in the northern and southern regions of the study area, respectively. Further, the drought frequency was characterized as a decreasing trend during seeding to overwinter. The frequencies of light, moderate, and severe droughts presented decreasing trends, whereas extreme drought showed an increasing trend during green-up to jointing. On the contrary, a reverse trend was detected during tasselling to maturation.
机译:根据研究区域及其周围地区1960-2013年间23个气象站的每日气象数据,利用作物水分亏缺指数(CWDI)研究了冬小麦干旱频率的时空变化。结果表明,在整个生育期内,干旱发生的顺序为:极端干旱>重度干旱>中度干旱>轻度干旱。 1995年以后,中度和重度干旱的频率呈上升趋势,而同期轻度和极度干旱的频率呈下降趋势。另外,从播种到成熟期的干旱频率降低,并且干旱频率的波动倾向于随着干旱水平的增加而加剧,特别是在绿化至拔节期间。在此期间,1995年以后极端干旱的频率呈下降趋势,而在严重干旱条件下则呈上升趋势。此外,在干旱频率趋势中发现了显着的空间差异。例如,严重干旱在研究区域的西北部呈上升趋势,而在东部则呈下降趋势。在研究区域的北部和南部分别发现了极端干旱的增加和减少趋势。此外,干旱频率被表征为播种至越冬期间的下降趋势。轻度,中度和重度干旱的频率呈下降趋势,而极端干旱在绿化至拔节期间呈上升趋势。相反,在流苏到成熟的过程中发现了相反的趋势。

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