Abstract

Time series of mean monthly temperature and total monthly precipitation are two of the climatic variables most easily obtained from weather station records. There are many studies analyzing historical series of these variables, particularly in the Spanish territory. In this study, the series of these two variables in 47 stations of the provincial capitals of mainland Spain were analyzed. The series cover time periods from the 1940s to 2013; the studies reviewed in mainland Spain go up to 2008. ARIMA models were used to represent their variation. In the preliminary phase of description and identification of the model, a study to detect possible trends in the series was carried out in an isolated manner. Significant trends were found in 15 of the temperature series, and there were trends in precipitation in only five of them. The results obtained for the trends are discussed with reference to those of other, more detailed studies in the different regions, confirming whether the same trend was maintained over time. With the ARIMA models obtained, 12-month predictions were made by measuring errors with the observed data. More than 50% of the series of both were modeled. Predictions with these models could be useful in different aspects of seasonal job planning, such as wildfires, pests and diseases, and agricultural crops.

Highlights

  • Among the most influential climatic elements in the biosphere and human activities are surface air temperature and precipitation

  • To obtain an ARIMA model, in the first stage, the graph of the data is observed as a function of time with the option of making a linear adjustment of the trend

  • The study revealed the existence of a significant, positive trend in the temperature series of Oviedo, Santander, A Coruña, and Ourense with the magnitude from 0.002 to 0.003 belonging to study zone I

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Summary

Introduction

Among the most influential climatic elements in the biosphere and human activities are surface air temperature and precipitation. For this reason, much attention has been focused on their measurement. The first attempt to obtain the mean global surface air temperature time series was made at the end of the 19th century by Köppen in 1883 [1]. His series covered a long period of time, 1731–1871 [1]. Harvey and Mills [7] analyzed annual temperatures of the northern and southern hemisphere from 1856 to 1998 based on the study of linear trends

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