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Historical drought patterns over Canada and their teleconnections with large-scale climate signals

机译:加拿大的历史干旱模式及其具有大规模气候信号的电信连接

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Drought is a recurring extreme climate event and among the most costly natural disasters in the world. This is particularly true over Canada, where drought is both a frequent and damaging phenomenon with impacts on regional water resources, agriculture, industry, aquatic ecosystems, and health. However, nationwide drought assessments are currently lacking and impacted by limited ground-based observations. This study provides a comprehensive analysis of historical droughts over the whole of Canada, including the role of large-scale teleconnections. Drought events are characterized by the Standardized Precipitation Evapotranspiration Index (SPEI) over various temporal scales (1, 3, 6, and 12 consecutive months, 6 months from April to September, and 12 months from October to September) applied to different gridded monthly data sets for the period 1950-2013. The Mann-Kendall test, rotated empirical orthogonal function, continuous wavelet transform, and wavelet coherence analyses are used, respectively, to investigate the trend, spatio-temporal patterns, periodicity, and teleconnectivity of drought events. Results indicate that southern (northern) parts of the country experienced significant trends towards drier (wetter) conditions although substantial variability exists. Two spatially well-defined regions with different temporal evolution of droughts were identified - the Canadian Prairies and northern central Canada. The analyses also revealed the presence of a dominant periodicity of between 8 and 32 months in the Prairie region and between 8 and 40 months in the northern central region. These cycles of low-frequency variability are found to be associated principally with the Pacific-North American (PNA) and Multivariate El Nino/Southern Oscillation Index (MEI) relative to other considered large-scale climate indices. This study is the first of its kind to identify dominant periodicities in drought variability over the whole of Canada in terms of when the drought even
机译:干旱是一种反复性的极端气候活动,以及世界上最昂贵的自然灾害。这尤其如此,在加拿大尤其如此,干旱既是对区域水资源,农业,工业,水生生态系统和健康影响的频繁和损害现象。但是,目前受到基于地面的有限意见缺乏和影响的全国性干旱评估。本研究规定了对整个加拿大的历史干旱综合分析,包括大型电信连接的作用。干旱事件的特点是,在各个时间尺度上的标准化降水蒸散指数(SPEI)(连续6个月,6个月从4月至9月,10月至9月的12个月)应用于不同的网格月度数据套装1950 - 2013年期间。使用Mann-Kendall测试,旋转经验正交函数,连续小波变换和小波相干分析,研究干旱事件的趋势,时空模式,周期性和替换性。结果表明,该国南部(北部)部分虽然存在大量可变性,但该国的南部(北部)部分朝向干旱频率(湿润)条件的趋势。鉴定了两个具有不同时间进化的空间明确的区域 - 加拿大大草原和加拿大北部。分析还揭示了大草原地区8至32个月的主要周期性,中部地区8至40个月。发现这些低频变异性的周期主要与太平洋 - 北美(PNA)和多元el Nino / Southern振荡指数(MEI)相对于其他考虑的大规模气候指数。本研究首先,在干旱的情况下,识别在整个加拿大的干旱变异性中的主导周期

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