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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Inter-annual and inter-decadal variability modes of the Athens total cloud cover
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Inter-annual and inter-decadal variability modes of the Athens total cloud cover

机译:雅典的年间和间间际变异变化模式总云覆盖

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The historical observations of the total cloud cover (TCC) index since 1900 from the National Observatory of Athens archives were used here, in order to investigate the inter-annual variability of TCC. Multi-spectral decomposition analysis was applied in order to resolve statistically significant modes of TCC variability out of the estimated stochastic variations. An increase of the Athens TCC (A-TCC) was ascertained during the observational period (1900-2012). The observed A-TCC variability was found to be composed by a dominant nonlinear trend that represents the centennial increment of the cloud cover, and a small number of sub-decadal oscillatory modes, particularly in the winter series. Additionally, the evolutionary history of the A-TCC variability involves a significant regime shift in about 1960 that was followed by an increase on the mean TCC level and an enhancement of the positive TCC trends apart from winter, in which the trend was faded out. The influence of global and hemispheric climatic variability patterns on the observed A-TCC changes was explored in the timescale domain along with the impacts of the Mediterranean evaporation field. Results showed that the A-TCC inter-decadal variability is strongly coupled with the Atlantic Multidecadal Oscillation (AMO) and the Mediterranean evaporation during all seasons, except winter, in which the atmospheric dynamic drives decadal and sub-decadal TCC variations, primarily modulated by the North Atlantic Oscillation (NAO). During the hot season, the AMO and the Mediterranean Sea thermodynamic processes become major regulators of the A-TCC variability, particularly on the inter-decadal scales, but the tropospheric North Atlantic activity still affects the A-TCC through the summer NAO (SNAO) pattern. In this framework, different epochs were discerned in the relation of the A-TCC with the Mediterranean evaporation field, which seem to be associated with the prevalence either of sea thermodynamic processes or of t
机译:自1900年从1900年从雅典档案馆的国家天文台使用自1900年以来的历史观察,以调查TCC的年间变异性。应用多光谱分解分析,以便在估计随机变化中解析TCC变异性的统计上显着的模式。在观察期间确定了雅典TCC(A-TCC)的增加(1900-2012)。发现观察到的A-TCC变异性由主要的非线性趋势组成,该趋势代表云覆盖的百年增量,以及少数次数振荡模式,特别是在冬季系列中。此外,A-TCC变异的进化历史涉及大约1960年的重大政权转变,然后增加平均TCC水平,并在冬季增加阳性TCC趋势的增强,其中趋势被褪色。在时间尺度领域探讨了全局和半球气候变化模式对观察到的A-TCC变化的影响以及地中海蒸发领域的影响。结果表明,除冬季外,A-TCC间跨越式变异性强烈耦合,冬季,除了冬季,其中大气动态驱动DICADAL和亚截止地区TCC变异,主要被调制北大西洋振荡(NAO)。在炎热的季节期间,AMO和地中海热力学过程成为A-TCC变异性的主要监管机构,特别是在截止间鳞片上,但对流层北大西洋活动仍然会通过夏天(SNAO)影响A-TCC图案。在该框架中,在A-TCC与地中海蒸发场的关系中被辨别不同的时期,这似乎与海热力学过程或T的患病率相关联

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