{"id":{"repo_id":"greece","oai_identifier":"oai:10442/0236"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/0236","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"Ο ΥΕΤΟΣ ΣΤΗ ΘΕΣΣΑΛΙΑ","abstract":"THE PRESENT THESIS BASED ON THE METEOROLOGICAL MEASUREMENTS OF PRECIPITATION AT 60 STATIONS DURING THE 20-YEAR PERIOD 1961 THROUGH 1980. 45 OF THE ABOVE 60 STATIONS ARE LYING IN THE AREA OF THESSALY AND THE REST 15 STATIONS ARE OUTSIDE, NEAR THE PERIFERY OF THESSALY, BUT THEY HAVE BEEN EXAMINED FOR THE HARMONIZATION AND COUNTINUATION OF THE PRECIPITATION REGIME TO THE GENERAL PRECIPITATION REGIME OF GREECE. THE PRECIPITATION, IN THE PRESENT THESIS, IS STUDYING ANALYTICALLY BY A MODERN AND PRACTICAL METHODOLOGY FOR EVERY MONTH, SEASON AND YEAR. BESIDES STATISTICAL TESTS OF SIGNIFICANCE AND CONFIDENCE ARE APPLIED. THEELEMENTARY AND THE UPPER STATISTICAL CHARACTERISTICS OF THE MEAN ANNUAL SERIES OF PRECIPITATION AMOUNT, AS WELL AS THE NUMBER OF DAYS OF PRECIPITATION HAVEBEEN ALSO STUDIED. THE PRECIPITATION REGIME IS OF THE MEDITERRANEAN TYPE WITHRAINY WINTERS AND DRY SUMMERS. THE HEIGHT OF PRECIPITATION AND THE GEOGRAPHICAL DISTRIBUTION, THE TOTAL PRECIPITATION, THE NUMBER OF PRECIPITATION, SNOW, HAILSTORM AND THUNDERSTORM DAYS AND THE 24-HOUR HEIGHT OF PRECIPITATION HAVE BEEN ALSO STUDIED.","abstract_html":"THE PRESENT THESIS BASED ON THE METEOROLOGICAL MEASUREMENTS OF PRECIPITATION AT 60 STATIONS DURING THE 20-YEAR PERIOD 1961 THROUGH 1980. 45 OF THE ABOVE 60 STATIONS ARE LYING IN THE AREA OF THESSALY AND THE REST 15 STATIONS ARE OUTSIDE, NEAR THE PERIFERY OF THESSALY, BUT THEY HAVE BEEN EXAMINED FOR THE HARMONIZATION AND COUNTINUATION OF THE PRECIPITATION REGIME TO THE GENERAL PRECIPITATION REGIME OF GREECE. THE PRECIPITATION, IN THE PRESENT THESIS, IS STUDYING ANALYTICALLY BY A MODERN AND PRACTICAL METHODOLOGY FOR EVERY MONTH, SEASON AND YEAR. BESIDES STATISTICAL TESTS OF SIGNIFICANCE AND CONFIDENCE ARE APPLIED. THEELEMENTARY AND THE UPPER STATISTICAL CHARACTERISTICS OF THE MEAN ANNUAL SERIES OF PRECIPITATION AMOUNT, AS WELL AS THE NUMBER OF DAYS OF PRECIPITATION HAVEBEEN ALSO STUDIED. THE PRECIPITATION REGIME IS OF THE MEDITERRANEAN TYPE WITHRAINY WINTERS AND DRY SUMMERS. THE HEIGHT OF PRECIPITATION AND THE GEOGRAPHICAL DISTRIBUTION, THE TOTAL PRECIPITATION, THE NUMBER OF PRECIPITATION, SNOW, HAILSTORM AND THUNDERSTORM DAYS AND THE 24-HOUR HEIGHT OF PRECIPITATION HAVE BEEN ALSO STUDIED.","abstract_has_math":false,"creators":["Νικολάκης, Δημήτριος","Nikolakis, Dimitrios"],"institution":"National and Kapodistrian University of Athens","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1985,"date_issued":"1985","date_published":"1985","updated_at":"2026-07-24T02:25:08Z","subjects":["ΒΡΟΧΟΜΕΤΡΙΚΟ ΣΥΣΤΗΜΑ","ΒΡΟΧΟΜΕΤΡΙΚΟΙ ΣΤΑΘΜΟΙ","ΘΕΡΜΗ ΕΠΟΧΗ","ΚΛΙΜΑΤΙΚΑ ΣΤΟΙΧΕΙΑ","Κλιματολογία","ΟΛΙΚΟΣ ΟΓΚΟΣΥΕΤΟΥ","ΣΕΙΡΕΣ ΚΛΙΜΑΤΙΚΩΝ ΣΤΟΙΧΕΙΩΝ","Υετός ή ατμοσφαιρικά κατακρημήσματα","ΥΨΟΣ ΥΕΤΟΥ","ΨΥΧΡΗ ΕΠΟΧΗ","CLIMATIC SERIES","CLIMATOLOGICAL ELEMENTS","COLD SEASON","HEIGHT OF PRECIPITATION","ISOPLETHS OF PRECIPITATION","METEOROLOGICAL STATIONS","NUMBER OF PRECIPITATION DAYS","Precipitation","STATISTICAL CHARACTERISTICS","Warm season"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/0236"],"render_values":[{"text":"10.12681/eadd/0236","href":"https://doi.org/10.12681/eadd/0236","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/0236","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Νικολάκης, Δημήτριος","Nikolakis, Dimitrios"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1985"]},{"key":"dc:publisher","label":"Institution","values":["National and Kapodistrian University of Athens","Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["ΒΡΟΧΟΜΕΤΡΙΚΟ ΣΥΣΤΗΜΑ","ΒΡΟΧΟΜΕΤΡΙΚΟΙ ΣΤΑΘΜΟΙ","ΘΕΡΜΗ ΕΠΟΧΗ","ΚΛΙΜΑΤΙΚΑ ΣΤΟΙΧΕΙΑ","Κλιματολογία","ΟΛΙΚΟΣ ΟΓΚΟΣΥΕΤΟΥ","ΣΕΙΡΕΣ ΚΛΙΜΑΤΙΚΩΝ ΣΤΟΙΧΕΙΩΝ","Υετός ή ατμοσφαιρικά κατακρημήσματα","ΥΨΟΣ ΥΕΤΟΥ","ΨΥΧΡΗ ΕΠΟΧΗ","CLIMATIC SERIES","CLIMATOLOGICAL ELEMENTS","COLD SEASON","HEIGHT OF PRECIPITATION","ISOPLETHS OF PRECIPITATION","METEOROLOGICAL STATIONS","NUMBER OF PRECIPITATION DAYS","Precipitation","STATISTICAL CHARACTERISTICS","Warm season"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["gre"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/0236","http://hdl.handle.net/10442/hedi/0236"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE PRESENT THESIS BASED ON THE METEOROLOGICAL MEASUREMENTS OF PRECIPITATION AT 60 STATIONS DURING THE 20-YEAR PERIOD 1961 THROUGH 1980. 45 OF THE ABOVE 60 STATIONS ARE LYING IN THE AREA OF THESSALY AND THE REST 15 STATIONS ARE OUTSIDE, NEAR THE PERIFERY OF THESSALY, BUT THEY HAVE BEEN EXAMINED FOR THE HARMONIZATION AND COUNTINUATION OF THE PRECIPITATION REGIME TO THE GENERAL PRECIPITATION REGIME OF GREECE. THE PRECIPITATION, IN THE PRESENT THESIS, IS STUDYING ANALYTICALLY BY A MODERN AND PRACTICAL METHODOLOGY FOR EVERY MONTH, SEASON AND YEAR. BESIDES STATISTICAL TESTS OF SIGNIFICANCE AND CONFIDENCE ARE APPLIED. THEELEMENTARY AND THE UPPER STATISTICAL CHARACTERISTICS OF THE MEAN ANNUAL SERIES OF PRECIPITATION AMOUNT, AS WELL AS THE NUMBER OF DAYS OF PRECIPITATION HAVEBEEN ALSO STUDIED. THE PRECIPITATION REGIME IS OF THE MEDITERRANEAN TYPE WITHRAINY WINTERS AND DRY SUMMERS. THE HEIGHT OF PRECIPITATION AND THE GEOGRAPHICAL DISTRIBUTION, THE TOTAL PRECIPITATION, THE NUMBER OF PRECIPITATION, SNOW, HAILSTORM AND THUNDERSTORM DAYS AND THE 24-HOUR HEIGHT OF PRECIPITATION HAVE BEEN ALSO STUDIED.","Η ΠΑΡΟΥΣΑ ΔΙΑΤΡΙΒΗ ΣΤΗΡΙΧΘΗΚΕ ΣΤΑ ΣΤΟΙΧΕΙΑ 60 ΣΤΑΘΜΩΝ ΠΑΡΑΤΗΡΗΣΕΩΝ ΤΗΣ ΠΕΡΙΟΧΗΣ ΤΗΣ ΘΕΣΣΑΛΙΑΣ ΚΑΙ ΓΙΑ ΤΗΝ ΧΡΟΝΙΚΗ ΠΕΡΙΟΔΟ 1961-80. ΑΠΟ ΤΟΥΣ 60 ΣΤΑΘΜΟΥΣ 45 ΑΝΗΚΑΝ ΜΕΣΑ ΣΤΗ ΘΕΣΣΑΛΙΑ ΚΑΙ 15 ΣΤΟΥΣ ΠΕΡΙΦΕΡΕΙΑΚΟΥΣ ΝΟΜΟΥΣ ΚΟΝΤΑ ΣΤΑ ΟΡΙΑ ΑΛΛΑΛΗΦΘΗΚΑΝ ΥΠ'ΟΨΗ ΓΙΑ ΤΗΝ ΚΑΛΥΤΕΡΗ ΜΕΛΕΤΗ ΣΤΑ ΟΡΙΑ ΚΑΙ ΓΙΑ ΤΗ ΣΥΝΕΧΕΙΑ ΤΟΥ ΚΛΙΜΑΤΟΣ ΜΕΣΑ ΣΤΟ ΓΕΝΙΚΟ ΕΛΛΗΝΙΚΟ ΠΛΑΙΣΙΟ. ΕΠΙ ΤΩΝ ΕΤΗΣΙΩΝ ΣΕΙΡΩΝ ΤΩΝ ΚΛΙΜΑΤΙΚΩΝ ΣΤΟΙΧΕΙΩΝ ΕΓΙΝΑΝ ΟΙ ΑΠΑΙΤΟΥΜΕΝΟΙ ΣΤΑΤΙΣΤΙΚΟΙ ΕΛΕΓΧΟΙ ΟΜΟΙΟΓΕΝΕΙΑΣ ΚΑΙ ΑΞΙΟΠΙΣΤΙΑΣ ΓΙΑ ΤΗΝ ΟΡΘΟΤΗΤΑ ΤΩΝ ΑΠΟΤΕΛΕΣΜΑΤΩΝ. ΚΑΤΑΣΚΕΥΑΣΤΗΚΑΝ ΟΙ ΧΑΡΤΕΣ ΙΣΑΥΕΤΩΝ ΚΑΜΠΥΛΩΝ ΠΟΥ ΑΠΕΙΚΟΝΙΖΟΥΝ ΤΗΝ ΓΕΩΓΡΑΦΙΚΗ ΔΙΑΝΟΜΗ ΤΟΥ ΥΕΤΟΥ ΜΕ ΤΗΝ ΣΥΓΧΡΟΝΗ ΚΑΙ ΠΡΑΚΤΙΚΗ ΜΕΘΟΔΟΛΟΓΙΑ ΓΙΑ ΚΑΘΕ ΜΗΝΑ, ΕΠΟΧΗ ΚΑΙ ΤΟ ΕΤΟΣ ΚΑΙ ΥΠΟΛΟΓΙΣΤΗΚΕ Ο ΟΛΙΚΟΣ ΟΓΚΟΣ ΝΕΡΟΥ ΠΟΥ ΔΕΧΕΤΑΙ ΚΑΤΑ ΜΕΣΟ ΟΡΟ ΣΤΟ ΕΤΟΣ Η ΠΕΡΙΟΧΗ ΤΗΣ ΘΕΣΣΑΛΙΑΣ. ΔΙΑΧΩΡΙΣΤΗΚΑΝ ΖΩΝΕΣ ΜΕ ΔΙΑΦΟΡΑ ΥΨΗ ΥΕΤΟΥ ΚΑΙ ΕΝΤΟΠΙΣΘΗΚΕ Η ΖΩΝΗ ΕΛΑΧΙΣΤΗΣ ΥΕΤΟΠΤΩΣΗΣ. ΜΕΛΕΤΗΘΗΚΕ ΚΑΤΑ ΜΗΝΑ ΕΠΟΧΗ ΚΑΙ ΕΤΟΣ Ο ΑΡΙΘΜΟΣ ΗΜΕΡΩΝ ΥΕΤΟΥ, ΧΙΟΝΙΟΥ, ΧΑΛΑΖΙΟΥ ΚΑΙ ΗΜΕΡΩΝ ΚΑΤΑΙΓΙΔΑΣ. ΕΞΕΤΑΣΘΗΚΕ Η ΜΕΤΑΒΟΛΗ ΤΟΥ ΜΕΣΟΥ ΕΤΗΣΙΟΥ ΥΨΟΥΣ ΥΕΤΟΥ ΜΕ ΤΟ ΥΨΟΜΕΤΡΟ ΤΟ ΑΝΑΓΛΥΦΟ ΚΑΙ ΤΙΣ ΓΕΩΓΡΑΦΙΚΕΣ ΣΥΝΤΕΤΑΓΜΕΝΕΣ. ΜΕΛΕΤΗΘΗΚΑΝ ΤΑ ΜΕΓΙΣΤΑ ΥΨΗ ΥΕΤΟΥ 24 ΩΡΩΝ ΜΕ ΤΗΝ ΧΡΗΣΗ ΤΗΣ ΚΑΤΑΝΟΜΗΣ GUMBEL, ΕΓΙΝΑΝ ΣΥΣΧΕΤΙΣΕΙΣΚΑΙ ΚΑΤΑΣΚΕΥΑΣΤΗΚΑΝ ΠΛΗΘΟΣ ΙΣΤΟΓΡΑΜΜΑΤΑ, ΔΙΑΓΡΑΜΜΑΤΑ, ΕΥΘΕΙΕΣ ΠΑΛΙΝΔΡΟΜΗΣΗΣ ΚΑΙ ΓΕΝΙΚΑ ΟΤΙΔΗΠΟΤΕ ΕΙΝΑΙ ΔΥΝΑΤΟ ΝΑ ΑΠΟΒΕΙ ΧΡΗΣΙΜΟ ΜΕ ΟΤΙ ΕΧΕΙ ΣΧΕΣΗ ΜΕ ΤΗΝ ΠΟΣΟΤΗΤΑ ΚΑΙ ΤΗΝ ΔΙΑΝΟΜΗ ΤΟΥ ΥΕΤΟΥ ΣΤΗ ΘΕΣΣΑΛΙΑ."]},{"key":"dc:title","label":"Title","values":["Ο ΥΕΤΟΣ ΣΤΗ ΘΕΣΣΑΛΙΑ","PRECIPITATION IN THE AREA OF THESSALY GREECE"]}]}],"canonical_facts":{"dc:creator":["Νικολάκης, Δημήτριος","Nikolakis, Dimitrios"],"dc:date":["1985"],"dc:description":["THE PRESENT THESIS BASED ON THE METEOROLOGICAL MEASUREMENTS OF PRECIPITATION AT 60 STATIONS DURING THE 20-YEAR PERIOD 1961 THROUGH 1980. 45 OF THE ABOVE 60 STATIONS ARE LYING IN THE AREA OF THESSALY AND THE REST 15 STATIONS ARE OUTSIDE, NEAR THE PERIFERY OF THESSALY, BUT THEY HAVE BEEN EXAMINED FOR THE HARMONIZATION AND COUNTINUATION OF THE PRECIPITATION REGIME TO THE GENERAL PRECIPITATION REGIME OF GREECE. THE PRECIPITATION, IN THE PRESENT THESIS, IS STUDYING ANALYTICALLY BY A MODERN AND PRACTICAL METHODOLOGY FOR EVERY MONTH, SEASON AND YEAR. BESIDES STATISTICAL TESTS OF SIGNIFICANCE AND CONFIDENCE ARE APPLIED. THEELEMENTARY AND THE UPPER STATISTICAL CHARACTERISTICS OF THE MEAN ANNUAL SERIES OF PRECIPITATION AMOUNT, AS WELL AS THE NUMBER OF DAYS OF PRECIPITATION HAVEBEEN ALSO STUDIED. THE PRECIPITATION REGIME IS OF THE MEDITERRANEAN TYPE WITHRAINY WINTERS AND DRY SUMMERS. THE HEIGHT OF PRECIPITATION AND THE GEOGRAPHICAL DISTRIBUTION, THE TOTAL PRECIPITATION, THE NUMBER OF PRECIPITATION, SNOW, HAILSTORM AND THUNDERSTORM DAYS AND THE 24-HOUR HEIGHT OF PRECIPITATION HAVE BEEN ALSO STUDIED.","Η ΠΑΡΟΥΣΑ ΔΙΑΤΡΙΒΗ ΣΤΗΡΙΧΘΗΚΕ ΣΤΑ ΣΤΟΙΧΕΙΑ 60 ΣΤΑΘΜΩΝ ΠΑΡΑΤΗΡΗΣΕΩΝ ΤΗΣ ΠΕΡΙΟΧΗΣ ΤΗΣ ΘΕΣΣΑΛΙΑΣ ΚΑΙ ΓΙΑ ΤΗΝ ΧΡΟΝΙΚΗ ΠΕΡΙΟΔΟ 1961-80. ΑΠΟ ΤΟΥΣ 60 ΣΤΑΘΜΟΥΣ 45 ΑΝΗΚΑΝ ΜΕΣΑ ΣΤΗ ΘΕΣΣΑΛΙΑ ΚΑΙ 15 ΣΤΟΥΣ ΠΕΡΙΦΕΡΕΙΑΚΟΥΣ ΝΟΜΟΥΣ ΚΟΝΤΑ ΣΤΑ ΟΡΙΑ ΑΛΛΑΛΗΦΘΗΚΑΝ ΥΠ'ΟΨΗ ΓΙΑ ΤΗΝ ΚΑΛΥΤΕΡΗ ΜΕΛΕΤΗ ΣΤΑ ΟΡΙΑ ΚΑΙ ΓΙΑ ΤΗ ΣΥΝΕΧΕΙΑ ΤΟΥ ΚΛΙΜΑΤΟΣ ΜΕΣΑ ΣΤΟ ΓΕΝΙΚΟ ΕΛΛΗΝΙΚΟ ΠΛΑΙΣΙΟ. ΕΠΙ ΤΩΝ ΕΤΗΣΙΩΝ ΣΕΙΡΩΝ ΤΩΝ ΚΛΙΜΑΤΙΚΩΝ ΣΤΟΙΧΕΙΩΝ ΕΓΙΝΑΝ ΟΙ ΑΠΑΙΤΟΥΜΕΝΟΙ ΣΤΑΤΙΣΤΙΚΟΙ ΕΛΕΓΧΟΙ ΟΜΟΙΟΓΕΝΕΙΑΣ ΚΑΙ ΑΞΙΟΠΙΣΤΙΑΣ ΓΙΑ ΤΗΝ ΟΡΘΟΤΗΤΑ ΤΩΝ ΑΠΟΤΕΛΕΣΜΑΤΩΝ. ΚΑΤΑΣΚΕΥΑΣΤΗΚΑΝ ΟΙ ΧΑΡΤΕΣ ΙΣΑΥΕΤΩΝ ΚΑΜΠΥΛΩΝ ΠΟΥ ΑΠΕΙΚΟΝΙΖΟΥΝ ΤΗΝ ΓΕΩΓΡΑΦΙΚΗ ΔΙΑΝΟΜΗ ΤΟΥ ΥΕΤΟΥ ΜΕ ΤΗΝ ΣΥΓΧΡΟΝΗ ΚΑΙ ΠΡΑΚΤΙΚΗ ΜΕΘΟΔΟΛΟΓΙΑ ΓΙΑ ΚΑΘΕ ΜΗΝΑ, ΕΠΟΧΗ ΚΑΙ ΤΟ ΕΤΟΣ ΚΑΙ ΥΠΟΛΟΓΙΣΤΗΚΕ Ο ΟΛΙΚΟΣ ΟΓΚΟΣ ΝΕΡΟΥ ΠΟΥ ΔΕΧΕΤΑΙ ΚΑΤΑ ΜΕΣΟ ΟΡΟ ΣΤΟ ΕΤΟΣ Η ΠΕΡΙΟΧΗ ΤΗΣ ΘΕΣΣΑΛΙΑΣ. ΔΙΑΧΩΡΙΣΤΗΚΑΝ ΖΩΝΕΣ ΜΕ ΔΙΑΦΟΡΑ ΥΨΗ ΥΕΤΟΥ ΚΑΙ ΕΝΤΟΠΙΣΘΗΚΕ Η ΖΩΝΗ ΕΛΑΧΙΣΤΗΣ ΥΕΤΟΠΤΩΣΗΣ. ΜΕΛΕΤΗΘΗΚΕ ΚΑΤΑ ΜΗΝΑ ΕΠΟΧΗ ΚΑΙ ΕΤΟΣ Ο ΑΡΙΘΜΟΣ ΗΜΕΡΩΝ ΥΕΤΟΥ, ΧΙΟΝΙΟΥ, ΧΑΛΑΖΙΟΥ ΚΑΙ ΗΜΕΡΩΝ ΚΑΤΑΙΓΙΔΑΣ. ΕΞΕΤΑΣΘΗΚΕ Η ΜΕΤΑΒΟΛΗ ΤΟΥ ΜΕΣΟΥ ΕΤΗΣΙΟΥ ΥΨΟΥΣ ΥΕΤΟΥ ΜΕ ΤΟ ΥΨΟΜΕΤΡΟ ΤΟ ΑΝΑΓΛΥΦΟ ΚΑΙ ΤΙΣ ΓΕΩΓΡΑΦΙΚΕΣ ΣΥΝΤΕΤΑΓΜΕΝΕΣ. ΜΕΛΕΤΗΘΗΚΑΝ ΤΑ ΜΕΓΙΣΤΑ ΥΨΗ ΥΕΤΟΥ 24 ΩΡΩΝ ΜΕ ΤΗΝ ΧΡΗΣΗ ΤΗΣ ΚΑΤΑΝΟΜΗΣ GUMBEL, ΕΓΙΝΑΝ ΣΥΣΧΕΤΙΣΕΙΣΚΑΙ ΚΑΤΑΣΚΕΥΑΣΤΗΚΑΝ ΠΛΗΘΟΣ ΙΣΤΟΓΡΑΜΜΑΤΑ, ΔΙΑΓΡΑΜΜΑΤΑ, ΕΥΘΕΙΕΣ ΠΑΛΙΝΔΡΟΜΗΣΗΣ ΚΑΙ ΓΕΝΙΚΑ ΟΤΙΔΗΠΟΤΕ ΕΙΝΑΙ ΔΥΝΑΤΟ ΝΑ ΑΠΟΒΕΙ ΧΡΗΣΙΜΟ ΜΕ ΟΤΙ ΕΧΕΙ ΣΧΕΣΗ ΜΕ ΤΗΝ ΠΟΣΟΤΗΤΑ ΚΑΙ ΤΗΝ ΔΙΑΝΟΜΗ ΤΟΥ ΥΕΤΟΥ ΣΤΗ ΘΕΣΣΑΛΙΑ."],"dc:identifier":["10.12681/eadd/0236","http://hdl.handle.net/10442/hedi/0236"],"dc:language":["gre"],"dc:publisher":["National and Kapodistrian University of Athens","Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)"],"dc:subject":["ΒΡΟΧΟΜΕΤΡΙΚΟ ΣΥΣΤΗΜΑ","ΒΡΟΧΟΜΕΤΡΙΚΟΙ ΣΤΑΘΜΟΙ","ΘΕΡΜΗ ΕΠΟΧΗ","ΚΛΙΜΑΤΙΚΑ ΣΤΟΙΧΕΙΑ","Κλιματολογία","ΟΛΙΚΟΣ ΟΓΚΟΣΥΕΤΟΥ","ΣΕΙΡΕΣ ΚΛΙΜΑΤΙΚΩΝ ΣΤΟΙΧΕΙΩΝ","Υετός ή ατμοσφαιρικά κατακρημήσματα","ΥΨΟΣ ΥΕΤΟΥ","ΨΥΧΡΗ ΕΠΟΧΗ","CLIMATIC SERIES","CLIMATOLOGICAL ELEMENTS","COLD SEASON","HEIGHT OF PRECIPITATION","ISOPLETHS OF PRECIPITATION","METEOROLOGICAL STATIONS","NUMBER OF PRECIPITATION DAYS","Precipitation","STATISTICAL CHARACTERISTICS","Warm season"],"dc:title":["Ο ΥΕΤΟΣ ΣΤΗ ΘΕΣΣΑΛΙΑ","PRECIPITATION IN THE AREA OF THESSALY GREECE"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:08Z"}