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Spatiotemporal Changes in Precipitation and Temperature in the Huaibei Plain and the Relation between Local Precipitation and Global Teleconnection Patterns

机译:淮北平原降水和气温的时空变化及局部降水与全球遥相关型的关系

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摘要

The Huaibei Plain is one of the most severe water scarcity areas in China. Understanding of hydroclimatic variation in this area at different timescales and its relationship with global teleconnection patterns are important for assessment of water resources utilization. In this study, spatiotemporal changes of seasonal and annual precipitation and temperature, including trend, abrupt change, variability, and periodicity were examined to recognize the potential remarkable changes during the last 41 years. The relationship between precipitation in the Huaibei Plain and teleconnection patterns using climate indexes was revealed by applying singular value decomposition. Results showed a nonsignificant annual precipitation increase about 2.4 mm/year. The annual average temperature increased about 1.2 degrees C during 1970-2010. The abrupt change of annual precipitation mainly occurred during the 1970s and 1980s, while the primary mutation points for temperature were detected in 1990s, especially in 1997. The mean areal precipitation is characterized by a statistically significant 2- to 4-year periodicity at different phases, and the 2- to 5-year band is the major cycle for annual average temperature in this region. A statistically strong 5- to 8-year periodicity for precipitation could be detected from the middle of the 1980s to the end of the 1990s. Precipitation has positive correlation with the West Pacific Pattern and El Nino Southern Oscillation. The investigated results might have considerable implications for managing water resources in the Huaibei Plain.
机译:淮北平原是中国最严重的缺水地区之一。了解该地区不同时间尺度的水文气候变化及其与全球遥相关型的关系,对于评估水资源利用非常重要。在这项研究中,研究了季节性和年度降水量和温度的时空变化,包括趋势,突变,变异性和周期性,以确认过去41年中潜在的显着变化。通过奇异值分解揭示了淮北平原降水与遥相关型的气候指数关系。结果表明,年降水量增长不明显,约为2.4毫米/年。在1970-2010年期间,年平均温度升高了约1.2摄氏度。年降水量的突然变化主要发生在1970年代和1980年代,而温度的主要突变点是在1990年代,特别是1997年。温度的平均降水量在不同阶段具有2至4年的统计显着周期性,而2至5年的波段是该地区年平均气温的主要周期。从1980年代中期到1990年代末,可以发现5至8年的统计降水周期很强。降水与西太平洋格局和厄尔尼诺南方涛动呈正相关。研究结果可能对淮北平原水资源管理具有重要意义。

著录项

  • 来源
    《Journal of hydrologic engineering》 |2019年第8期|05019019.1-05019019.12|共12页
  • 作者单位

    Sun Yat Sen Univ, Sch Geog & Planning, 135 Xingang Xi Rd, Guangzhou 510275, Guangdong, Peoples R China|Guangdong Res Inst Water Resources & Hydropower, 116 Tianshou Rd, Guangzhou 510000, Guangdong, Peoples R China;

    Guangdong Res Inst Water Resources & Hydropower, State & Local Joint Engn Lab Estuarine Hydraul Te, 116 Tianshou Rd, Guangzhou 510000, Guangdong, Peoples R China;

    Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, 1 Xikang Rd, Nanjing 210098, Jiangsu, Peoples R China;

    Lund Univ, Dept Water Resources Engn, POB 118, SE-22100 Lund, Sweden|Lund Univ, Ctr Middle Eastern Studies, POB 118, SE-22100 Lund, Sweden;

    Guangdong Res Inst Water Resources & Hydropower, State & Local Joint Engn Lab Estuarine Hydraul Te, 116 Tianshou Rd, Guangzhou 510000, Guangdong, Peoples R China;

    Sun Yat Sen Univ, Sch Geog & Planning, 135 Xingang Xi Rd, Guangzhou 510275, Guangdong, Peoples R China;

    Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, 1 Xikang Rd, Nanjing 210098, Jiangsu, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Climate change; The Huaibei Plain; Precipitation; Temperature; Teleconnection patterns;

    机译:气候变化淮北平原降水温度遥相关型;
  • 入库时间 2022-08-18 04:23:00

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