首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Spatial and temporal distributions of trends in climate extremes of the Feilaixia catchment in the upstream area of the Beijiang River Basin, South China
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Spatial and temporal distributions of trends in climate extremes of the Feilaixia catchment in the upstream area of the Beijiang River Basin, South China

机译:华南北江流域上游飞来峡流域气候极端变化趋势的时空分布

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摘要

To evaluate the changes in extreme climatic events in the Feilaixia catchment in South China, the spatial and temporal distributions of extreme climate indices trends during 1969-2011 were investigated. With quality control and homogeneity assessment, daily maximum and minimum surface air temperature from 11 meteorological stations and daily precipitation from 24 rainfall stations were used. Eight indices of extreme temperature and six indices of extreme precipitation were chosen. Trends were calculated using Sen's slope estimator. Statistical significance of trends was checked with the Mann-Kendall method. High correlations were found between the mean annual temperature and temperature extremes, as well as between the annual total precipitation and precipitation extremes in most cases. The analyses of extreme temperature indices detected significant and stable trends in the majority of the stations. The strongly stable downward trends in cold extremes and the strongly stable upward trends in hot extremes were recorded in the whole region, except for in some small areas primarily located in the central part of the region. In contrast, significant and stable positive trends were sporadically recorded for precipitation extremes in the study area during 1969-2011, which predominantly occurred in the northern part of the region. Furthermore, the positive trends were much more frequent than the negative trends in most extreme precipitation indices. There were significant and stable trends recorded in most of the average temperature extremes, whereas insignificant and unstable trends were found for most of the average precipitation extremes.
机译:为了评估华南飞来峡流域极端气候事件的变化,研究了1969-2011年极端气候指数趋势的时空分布。通过质量控制和均质性评估,使用了11个气象站的每日最高和最低地表温度以及24个降雨站的每日降水。选择了八个极端温度指标和六个极端降水指标。使用Sen的斜率估计器计算趋势。使用Mann-Kendall方法检查趋势的统计显着性。在大多数情况下,发现年平均温度与极端温度之间以及年总降水量与极端降水之间存在高度相关性。极端温度指数的分析在大多数台站中发现了显着且稳定的趋势。除了主要位于该区域中部的一些小区域外,整个区域都记录到了寒冷极端的强烈稳定下降趋势和高温极端的强烈稳定上升趋势。相反,在1969年至2011年期间,研究区域的极端降水偶发地记录了显着且稳定的正趋势,这主要发生在该区域的北部。此外,在大多数极端降水指数中,正趋势比负趋势要频繁得多。在大多数平均气温极端值中都记录有明显和稳定的趋势,而在大多数平均降水极端值中却发现了微不足道和不稳定的趋势。

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