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Spatiotemporal patterns of drought at various time scales in Shandong Province of Eastern China

机译:中国东部山东省不同时间尺度上干旱的时空格局

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摘要

The temporal variations and spatial patterns of drought in Shandong Province of Eastern China were investigated by calculating the standardized precipitation evapotranspiration index (SPEI) at 1-, 3-, 6-, 12-, and 24-month time scales. Monthly precipitation and air temperature time series during the period 1960-2012 were collected at 23 meteorological stations uniformly distributed over the region. The non-parametric Mann-Kendall test was used to explore the temporal trends of precipitation, air temperature, and the SPEI drought index. S-mode principal component analysis (PCA) was applied to identify the spatial patterns of drought. The results showed that an insignificant decreasing trend in annual total precipitation was detected at most stations, a significant increase of annual average air temperature occurred at all the 23 stations, and a significant decreasing trend in the SPEI was mainly detected at the coastal stations for all the time scales. The frequency of occurrence of extreme and severe drought at different time scales generally increased with decades; higher frequency and larger affected area of extreme and severe droughts occurred as the time scale increased, especially for the northwest of Shandong Province and Jiaodong peninsular. The spatial pattern of drought for SPEI-1 contains three regions: eastern Jiaodong Peninsular and northwestern and southern Shandong. As the time scale increased to 3, 6, and 12 months, the order of the three regions was transformed into another as northwestern Shandong, eastern Jiaodong Peninsular, and southern Shandong. For SPEI-24, the location identified by REOF1 was slightly shifted from northwestern Shandong to western Shandong, and REOF2 and REOF3 identified another two weak patterns in the south edge and north edge of Jiaodong Peninsular, respectively. The potential causes of drought and the impact of drought on agriculture in the study area have also been discussed. The temporal variations and spatial patterns of drought obtained in this study provide valuable information for water resources planning and drought disaster prevention and mitigation in Eastern China.
机译:通过计算1、3、6、12和24个月时间尺度上的标准降水蒸发蒸腾指数(SPEI),研究了中国东部山东省干旱的时空变化和空间格局。在均匀分布于该地区的23个气象站收集了1960-2012年期间的月降水量和气温时间序列。使用非参数Mann-Kendall检验来探索降水,气温和SPEI干旱指数的时间趋势。 S模式主成分分析(PCA)用于识别干旱的空间格局。结果表明,大多数站台的年总降水量没有明显下降的趋势,所有23个站台的年平均气温都出现了显着上升,而SPEI的显着下降趋势主要出现在沿海站台。时间尺度。在不同的时间尺度上,极端干旱和严重干旱的发生频率通常随着几十年而增加;随着时间尺度的增加,极端和严重干旱的发生频率更高,受影响区域更大,特别是在山东省西北部和胶东半岛。 SPEI-1的干旱空间格局包括三个区域:胶东半岛东部和山东西北部和南部。随着时间尺度增加到3、6和12个月,这三个区域的顺序也转变为另一个区域,即山东西北部,胶东半岛东部和山东南部。对于SPEI-24,由REOF1识别的位置从山东西北部稍微移至山东西部,而REOF2和REOF3分别在胶东半岛的南边缘和北边缘识别了另外两个弱模式。研究区域还讨论了干旱的潜在原因以及干旱对农业的影响。这项研究获得的干旱的时空变化和空间格局为中国东部的水资源规划和干旱减灾减灾提供了有价值的信息。

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  • 来源
    《Theoretical and applied climatology》 |2018年第2期|271-284|共14页
  • 作者单位

    Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China|Joint Ctr Global Change Studies, Beijing 100875, Peoples R China;

    Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China;

    Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China|Joint Ctr Global Change Studies, Beijing 100875, Peoples R China;

    Water Conservancy Res Inst Shandong Prov, Jinan 250013, Shandong, Peoples R China;

    Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China|Joint Ctr Global Change Studies, Beijing 100875, Peoples R China;

    Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China;

    Minist Water Resources, China Inst Water Resources & Hydropower Res, Res Ctr Flood & Drought Disaster Reduct, Beijing 100038, Peoples R China;

    Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China;

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  • 正文语种 eng
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  • 入库时间 2022-08-18 03:33:31

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