A study on the intra-annual variation and the spatial distribution of precipitation amount and duration over Greece on a 10 day basis

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Μικρογραφία εικόνας

Ημερομηνία

Συγγραφείς

Bartzokas, A.
Lolis, C. J.
Metaxas, D. A.

Τίτλος Εφημερίδας

Περιοδικό ISSN

Τίτλος τόμου

Εκδότης

Περίληψη

Τύπος

Είδος δημοσίευσης σε συνέδριο

Είδος περιοδικού

peer reviewed

Είδος εκπαιδευτικού υλικού

Όνομα συνεδρίου

Όνομα περιοδικού

International Journal of Climatology

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Έκδοση βιβλίου

Συμπληρωματικός/δευτερεύων τίτλος

Περιγραφή

The intra-annual variation of precipitation amount and duration and their spatial distribution during the year are studied on a 10 day basis for the Greek region, using S-mode and T-mode factor analysis. (i) For the intra-annual variation of precipitation amount, two modes were revealed: the first shows one broad maximum during the conventional winter in stations affected by the sea; the second presents two maxima, the first during late autumn-early winter and the second during late spring, corresponding to the northern mainland stations. (ii) For the spatial distribution of precipitation, three main patterns were revealed: the first one is the 'winter' pattern, with the maximum over the west windward area; the second is the 'summer' pattern, with a maximum over the north inland region; and the third is the 'autumn' pattern, with the maximum over northwestern Greece. (iii) For precipitation duration, two types of intra-annual variation were revealed. The first one is similar to the first of the analysis for precipitation amount; the second presents two maxima, the first during the beginning of December and the second during the middle of February, corresponding to the areas of northwestern and northeastern Greece. (iv) For the spatial distribution of precipitation duration, three main patterns were revealed: the first is the 'summer' pattern, which is similar to the second of the analysis for precipitation amount; the second is the 'winter' pattern, with the spatial maximum located over the eastern mainland and western Crete; finally, the third one is the 'autumn' pattern, with the maximum in northwestern Greece. During the third 10 day period of October and the second 10 day period of February, precipitation seems to present singularities, possibly due to fluctuations in atmospheric circulation, The above intra-annual variations and spatial distribution patterns are connected to the seasonal variations of the depression trajectories, the atmospheric instability, the influence of sea-surface temperature as a cyclogenesis factor, and the windward or leeward character of the various areas (orographic effect). Copyright (C) 2003 Royal Meteorological Society.

Περιγραφή

Λέξεις-κλειδιά

greece, factor analysis, precipitation amount, precipitation duration, 10-day periods, variability

Θεματική κατηγορία

Παραπομπή

Σύνδεσμος

<Go to ISI>://000181074000006
http://onlinelibrary.wiley.com/store/10.1002/joc.874/asset/874_ftp.pdf?v=1&t=hfwdwam7&s=008a94a3e9e15e0d95884897b5285683a0fbb944
http://onlinelibrary.wiley.com/store/10.1002/joc.874/asset/874_ftp.pdf?v=1&t=hfwdwguh&s=1d98b633c9c9bb3de11b1ae5dc976310196bc852

Γλώσσα

en

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Όνομα επιβλέποντος

Εξεταστική επιτροπή

Γενική Περιγραφή / Σχόλια

Ίδρυμα και Σχολή/Τμήμα του υποβάλλοντος

Πανεπιστήμιο Ιωαννίνων. Σχολή Επιστημών και Τεχνολογιών. Τμήμα Βιολογικών Εφαρμογών και Τεχνολογιών

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