Variability of tropical days over Greece within the second half of the twentieth century

Citation:

Nastos, P.T. & Matzarakis, A.P. Variability of tropical days over Greece within the second half of the twentieth century. Theoretical and Applied Climatology 93, 75 - 89 (2008). Copy at http://www.tinyurl.com/y6kbswzm

Abstract:

Tropical days (TD) are defined as the days with a maximum air temperature greater than 30.0°C. It is clear that the study of TD includes also the absolute maximum temperatures, which are of great interest for the description of a region's climate. These days are considered as very hot, and they particularly are of great importance not only for bioclimatology and applied sciences, but also for the individuals who are sensitive in the heat-stress. The regime of the TD in Greece is the focus of this study. The aim is to demonstrate their changes from decade to decade, for the time period 1960-2000. For this study, the Annual Number of Tropical Days (ANTD) recorded by each of the 26 meteorological stations of National Meteorological Service, which are uniformly distributed in the Hellenic peninsula, was calculated and analysed. In terms of quantifying the conditions in a human-biometeorological manner, the thermal index Physiological Equivalent Temperature (PET) and the consecutive days for Athens have been included in this study. The trends of the TD for each station were analysed through the Mann-Kendall technique, while the spatial distribution per decade reveals the regions with change (increase or decrease) in the ANTD during the examined period. Two characteristic periods of change for the ANTD appear in the majority of the meteorological stations in Greece. The first period (1955-1976) is determined by a negative trend, which is statistically significant (c.l. 95%), for adequate stations. In the period between 1976 and 2000, the increase in the ANTD and the maximum temperature exceed the corresponding maximum that appeared in the beginning of the 1950s for several of the examined meteorological stations. The human-biometeorological analysis shows that the consecutive days of PET >35°C have had a positive trend in the last two decades of the last century. © Springer-Verlag 2007.

Notes:

Cited By :22Export Date: 2 November 2015Correspondence Address: Nastos, P.T.; Laboratory of Climatology and Atmospheric Environment, Department of Geography and Climatology, University of Athens, Panepistimiopolis GR, 157 84 Athens, Greece; email: nastos@geol.uoa.grReferences: Alexandersson, H., A homogeneity test applied to precipitation data (1986) J Climatol, 6, pp. 661-675. , 10.1002/joc.3370060607;Arseni-Papadimitriou, A., Maheras, P., Some statistical characteristics of air temperature variations at four Mediterranean stations (1991) Theor Appl Climatol, 43, pp. 105-112. , 10.1007/BF00867467; Balafoutis, C., Arseni-Papadimitriou, A., Analyse en composantes principales des temperatures moyennes maximales et minimales en Greece (1992) Publications De L' Association De Climatologie, 5, pp. 213-219; Bartzokas, A., Metaxas, D.A., Factor analysis of some climatological elements in Athens, 1931-1992: Covariability and climatic change Theor (1995) Appl Climatol, 52, pp. 195-205. , 10.1007/BF00864043; Carapiperis, L., The distribution of the absolute extreme temperatures in Greek Peninsula (1954) Minutes of the Academy of Athens, 29, pp. 411-419; Carapiperis, P., Contribution to the study of tropical days in Athens (1959) Bulletin of Army Geographical Service, 2, pp. 61-68; Chu, P.S., Yu, Z.P., Hastenrath, S., Detecting climate change concurrent with deforestation in the Amazon basin: Which way has it gone? 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