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Long‐term change of total cloud cover and its possible reason over South China during 1960–2012

机译:1960–2012年华南地区总云量的长期变化及其可能原因

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Long‐term trend of total cloud cover (TCC) had been studied based on 51 meteorological stations across South China during the period 1960–2012. TCC reduction mainly happened over the past 53?years, and the value of climatic trend rate (CTR) averaged in all stations was???0.625%·10a~(?1). The primary cause of the significant reduction of TCC was the temperature (LT) and relative humidity (LRH) in the low troposphere in the context of global warming. Correlation coefficients between TCC and LRH in annual and seasonal mean had all passed 99% significance test, and strong positive correlations indicate that LRH plays a much more important role in the change of TCC in South China. Spatial distribution of CTC (a) and temporal variation (b) of all stations averaged annual TCC in South China during1960 to 2012.
机译:基于1960-2012年期间华南地区的51个气象站,研究了总云量(TCC)的长期趋势。 TCC的减少主要发生在过去的53年中,所有站点的平均气候趋势率(CTR)的值为0.625%·10a〜(?1)。 TCC显着降低的主要原因是全球变暖背景下低对流层的温度(LT)和相对湿度(LRH)。 TCC与LRH在年均和季节均值之间的相关系数均通过了99%的显着性检验,并且强正相关表明LRH在华南地区TCC的变化中起着更为重要的作用。 1960年至2012年,华南地区所有台站的CTC空间分布(a)和时间变化(b)

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