Analysis of hot spell characteristics in the Greek region
2005; Inter-Research Science Center; Volume: 28; Linguagem: Inglês
10.3354/cr028229
ISSN1616-1572
AutoresBD Katsoulis, N. Hatzianastassiou,
Tópico(s)Cryospheric studies and observations
ResumoCR Climate Research Contact the journal Facebook (Twitter) RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials CR 28:229-241 (2005) - doi:10.3354/cr028229 Analysis of hot spell characteristics in the Greek region B. D. Katsoulis, N. Hatzianastassiou* Laboratory of Meteorology, Department of Physics, University of Ioannina, 45110 Ioannina, Greece *Corresponding author. Email: nhatzian@cc.uoi.gr ABSTRACT: In the present study, hot spell conditions over the Greek region during the warm period (June to September) were examined by using daily maximum temperature data from 16 meteorological stations of the Hellenic National Meteorological Service (HNMS) and a combined deterministic-stochastic model. The results show that daily maximum temperatures can be studied as a mixture of deterministic and stochastic components, whereas the properties of hot spells can be adequately described with statistical distributions. Trends and the geographical and temporal distribution of hot spells at the surface were investigated by linear regression, Fourier analysis and statistical distributions. Partial duration series of hot spells, fitted with Poisson, Gauss and exponential distributions, provide information on their frequency, timing, magnitude and geographical distribution. The most frequent hot spells are found over southern parts of inland Greece, as well as over the northern mainland, while less frequent events occur along the coastal belt of the Greek Peninsula and in the Aegean islands. Hot spells are more frequent at inland than in marine areas, and occur from June to September. Statistical analysis of synoptic weather conditions that favour the development of hot spells shows that such events are most probable over Greece when (1) a persistent Azores anticyclone appears over North Africa and extends ridges of high pressure towards the NE Mediterranean, and (2) when western and central European anticyclones extend towards the region. KEY WORDS: synoptic weather conditions · hot spell · frequency · timing · magnitude · statistical distributions Full text in pdf format PreviousNextExport citation RSS - Facebook - Tweet - linkedIn Cited by Published in CR Vol. 28, No. 3. Online publication date: May 24, 2005 Print ISSN: 0936-577X; Online ISSN: 1616-1572 Copyright © 2005 Inter-Research.
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