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S. del Río A. Cano-Ortiz L. Herrero A. Penas 《Theoretical and Applied Climatology》2012,109(3-4):605-626
This study analyzes the mean maximum and minimum temperature trends on a monthly, seasonal, and annual timescale by applying various statistical tools to data from 476 Spanish weather stations during the period between 1961 and 2006. The magnitude of the trends was derived from the slopes of the regression lines using the least squares method, and the nonparametric Mann–Kendall test was used to determine the statistical significance of the trends. Temperature significantly increased in over 60% of the country in March, June, spring, and summer in the case of maximum temperatures and in March, May, June, August, spring, and summer for minimum temperatures. At the annual resolution, temperatures significantly increased in over 90% of Spain with a rise of around 0.3°C/decade. The maximum temperature increased at a higher rate than the minimum temperature from midsummer to early winter as well as in winter, spring, and summer and also on an annual basis. 相似文献
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Summary The present paper is an analysis of mean maximum and minimum temperatures carried out on monthly, seasonal and annual time-scales
examining the data collected at 171 meteorological stations over a region in the North West of Spain (Castilla y León) for
the period 1961–1997. Various statistical tools were used to detect and describe significant trends in these data. The magnitude
of the trends was derived from the slopes of the regression lines using the least squares method, and the statistical significance
was determined by means of the non-parametric Mann-Kendall test. The pattern obtained is quite similar for mean maximum and
minimum temperatures with increases in all months of the year, and in the annual series. The seasonal series corresponding
to winter and summer also followed this same pattern. Spring and autumn were found to be more irregular. Because maximum temperature
increased at a higher rate than minimum temperature in this period, an increase in the annual diurnal temperature range (DTR)
was observed. The correlation between the North Atlantic Oscillation (NAO) and the regional maximum and minimum temperatures
and DTR series for the period 1961–1997 have also be studied in this paper. 相似文献
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