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ÁNGEL L. LABAJO,MOISÉS EGIDO,QUINTÍN MARTÍN,JUAN LABAJO,JOSÉ LUIS LABAJO
The temporal behavior of the annual frequency of heat and cold waves observed between 1961 and 2010is established for the Spanish Central Plateau and for the two sub-areas in it. The series of daily maximumand minimum temperature anomalies for the workin...
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J. L. LABAJO,A. L. LABAJO,M. EGIDO,Q. MARTÍN,C. MORALES,M. T. ORTEGA
An analysis of the temporal behavior of the annual and seasonal frequencies of extreme maximum daily temperature values on the Spanish Central Plateau is performed. With the daily data on maximum temperatures measured at 14 weather stations, between 1961...
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A. L. Labajo,J. L. Labajo
A forecasting model for the mean monthly maximum temperatures (TMaxMean) using an artificial neuronal network (ANN) of the multilayer perceptron type (Multilayer Perceptron, MLP) has been developed. This model forecast the TMaxMean variable one month ahe...
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J. L. LABAJO SALAZAR,A. L. LABAJO,A. L. PIORNO,Q. MARTÍN,M. T. ORTEGA,C. MORALES
A study was undertaken to establish the spatio-temporal behavior of the extreme daily values of atmospheric pressure at ground level in a zone comprising the central part of the Iberian Peninsula (Spanish Central Plateau). The study involves the time ...
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C. G. MORALES,M. T. ORTEGA,J. L. LABAJO SALAZAR,A. PIORNO HERNÁNDEZ
The behavior of temperatures in the region of Castilla-León in Spain was explored in a study of trend analyzes of the regional thermal anomalies in the zone. The work was developed in two steps: in the first, the working data ...
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M. S. ALONSO,J. L. LABAJO SALAZAR,M. R. FIDALGO
In this paper the urban heat island (UHI) of the city of Salamanca, Spain is examined. The temporal evolution of the intensity of the UHI for the three-year period between 1996 and 1998 was studied by comparing the temperatures ...
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J. L. LABAJO SALAZAR,A. PIORNO HERNÁNDEZ,M. J. IZQUIERDO GALLEGO
In this work, a model for the short term prediction of the temperature of formation of radiation fogs is developed. the model is generated from a lineal relationship between the relative humidity and the air temperature, that in function of it the temper...
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J. L. LABAJO SALAZAR,F. DE PABLO,E. L. GARCÍA
This work is directed to establish how the linear relation h2 ? h1 = -0,03 - 3,586(T2 ? T1), which is suppose to be valid at any point on the Earth and time of the year, and whose coefficients are obtained using synchronous series of three hourly data...
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