[ 45 ] found a positive trend in total cloud cover (TCC) in Spain from 1886 to the 1960s, followed by a reversal.
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Millennium-Scale Atlantic Multidecadal Oscillation and Soil Moisture Influence on Western Mediterranean Cloudiness.
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The sentences
[ 45 , 52 ] reported a declining trend in the TCC that has persisted beyond the 1960s, despite an increasing trend in autumn.