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Trends and periodicity of daily temperature and precipitation extremes during 1960-2013 in Hunan Province, central south China

机译:中国中南部湖南省1960-2013年每日气温和极端降水的趋势和周期性

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In this study, the trends and periodicity in climate extremes are examined in Hunan Province over the period 1960-2013 on the basis of 27 extreme climate indices calculated from daily temperature and precipitation records at 89 meteorological stations. The results show that in the whole province, temperature extremes exhibit a warming trend with more than 50% stations being statistically significant for 7 out of 16 temperature indices, and the nighttime temperature increases faster than the daytime temperature at the annual scale. The changes in most extreme temperature indices show strongly coherent spatial patterns. Moreover, the change rates of almost all temperature indices in north Hunan are greater than those of other regions. However, the statistically significant changes in indices of extreme precipitation are observed at fewer stations than in extreme temperature indices, forming less spatially coherent patterns. Positive trends in indices of extreme precipitation show that the amount and intensity of extreme precipitation events are generally increasing in both annual and seasonal scales, whereas the significant downward trend in consecutive wet days indicates that the precipitation becomes more even over the study period. Analysis of changes in probability distributions of extreme indices for 1960-1986 and 1987-2013 also demonstrates a remarkable shift toward warmer condition and increasing tendency in the amount and intensity of extreme precipitation during the past decades. The variations in extreme climate indices exhibit inconstant frequencies in the wavelet power spectrum. Among the 16 temperature indices, 2 of them show significant 1-year periodic oscillation and 7 of them exhibit significant 4-year cycle during some certain periods. However, significant periodic oscillations can be found in all of the precipitation indices. Wet-day precipitation and three absolute precipitation indices show significant 1-year cycle and other seven provide significant power at the 4-year period, which are mainly found during 1970-1980 and after 1992.
机译:在这项研究中,根据从89个气象站的每日温度和降水记录中得出的27个极端气候指数,研究了1960-2013年湖南省极端气候的趋势和周期性。结果表明,在全省,极端温度呈现出变暖的趋势,在16个温度指数中有7个超过50%的气象站具有统计学意义,而在年尺度上,夜间温度的升高速度要快于白天的温度。大多数极端温度指数的变化都显示出高度连贯的空间格局。而且,湘北几乎所有温度指数的变化率都比其他地区大。但是,与极端温度指数相比,在更少的观测站观测到极端降水指数的统计显着变化,从而形成了空间上不连贯的模式。极端降水指数的正趋势表明,极端降水事件的数量和强度在年度和季节尺度上总体上都在增加,而连续湿日的显着下降趋势表明,在研究期内降水变得更加均匀。对1960-1986年和1987-2013年极端指数概率分布变化的分析还表明,在过去的几十年中,极端气候向暖化方向转变,极端降水的数量和强度呈增加趋势。极端气候指数的变化在小波功率谱中显示出不固定的频率。在这16个温度指数中,其中2个显示出明显的1年周期振荡,其中7个显示出在某些时期内的4年周期。但是,在所有降水指数中都可以发现明显的周期性振荡。湿日降水和三个绝对降水指数显示了显着的1年周期,而其他7个在4年期间提供了显着的功率,这些功率主要出现在1970-1980年以及1992年之后。

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