Long-time temperature variations in Portugal over the last 140 years and the effect of the solar activity

Details Long-time temperature variations in Portugal over the last 140 years and the effect of the solar activity Long-time temperature variations in Portugal over the last 140 years and the effect of the solar activity

2010-09-03

arxiv.org/abs/1009.0768v1

Physics

Atmospheric and Oceanic Physics

27 pages, 8 figures, 4 tables. submitted to JASTP

Scientific paper

We present the analysis of temperature variations in Portugal for 140 years (from 1865 to 2005). The two stations with the longest time series of temperature measurements (Lisbon and Coimbra) have been used to study the dependence of the portuguese climate variations on the changes of both global circulation and solar activity. Monthly averaged temperature series have been analyzed together with monthly North-Atlantic Oscillation index data, sunspot numbers and cosmic ray flux intensity. Different statistical methods (the correlation analysis and the multiple regression analysis) were used. Our results show that the temperature in Portugal depends not only on the atmospheric variations in the studied region but also on the variations of the solar parameters such as sunspot numbers and the cosmic rays flux intensity. Also, the dependence of temperature on solar parameters is strong during the cold season (November to February), while much weaker during the warm season. For some months, strong correlations between the temperature variations of the current month and the North-Atlantic Oscillation index values of the previous month have been found. The correlation between climatic and solar parameters shows up best on the decadal and decadal-to-centennial timescale. It is found that the temperature correlates positively with the sunspot numbers and negatively with the CR flux intensity throughout the year. Besides, the absolute values of the correlation coefficients between the temperature and the CR are higher than those between the temperature and the sunspot numbers. Our results are consistent with some of the proposed mechanisms that relate solar activity to Earth climate and could be explained through the effect of the solar UV radiation and stratosphere-troposphere coupling or/and through the effect of the CR particles on clouds and stratospheric and tropospheric conditions.

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