Please use this identifier to cite or link to this item: http://openlibrary.ge/handle/123456789/10417
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dc.contributor.authorAmiranashvili, A.en
dc.contributor.authorKartvelishvili, L.en
dc.contributor.authorKutaladze, N.en
dc.contributor.authorMegrelidze, L.en
dc.contributor.authorTatishvili, M.en
dc.date.accessioned2023-11-21T13:13:05Z-
dc.date.available2023-11-21T13:13:05Z-
dc.date.issued2023-
dc.identifier.citationსაერთაშორისო სამეცნიერო კონფერენცია „დედამიწასა და მის გარსებში მიმდინარე გეოფიზიკური პროცესები“. შრომები, ISBN 978-9941-36-147-0, ივ. ჯავახიშვილის სახ. თბილისის სახელმწიფო უნივერსიტეტის გამომცემლობა, თბილისი, საქართველო, 16–17 ნოემბერი, 2023 წ., გვ. 122-126.ka_GE
dc.identifier.citationInternational Scientific Conference "Geophysical Processes in the Earth and its Envelopes". Proceedings, ISBN 978-9941-36-147-0, Publish House of Iv. Javakhishvili Tbilisi State University, November 16-17, 2023, pp. 122-126.en
dc.identifier.urihttp://openlibrary.ge/handle/123456789/10417-
dc.description.abstractThe research results of the variability of the mean max annual air temperature at 39 locations in Georgia against the background of global climate change in 1956-2015 are presented. The statistical characteristics of the mean max annual air temperature in the period 1956-2015 (T), 1956-1985 (T₁) and 1986-2015 (T₂) for each point were studied. It has been established that in the second period compared to the first, there is a significant increase in the average max air temperature at the 29 stations from 0.3˚С (Stepantsminda) to 1.2˚С (Bakuriani); for Shovi this difference is 1.1˚С. It is shown that between the T₁, T₂ values and the terrain height there has been observed the high inverse linear correlation and regression relationship there. At the same time, the lines of the regression equations are parallel with the increasing in the second period compared to the first by 0.6 ˚С. It is shown, that a significant value of (T₂- T₁)/T changes from 2.0 % (Chokhatauri) to 11.0% (Bakuriani); for Shovi this indicator is 8.4 %. The significant value (T₂- T₁)/T increases with terrain height in accordance with a second power polynomial.en
dc.language.isoenen
dc.subjectდედამიწა და მის გარსებიka_GE
dc.subjectგეოფიზიკური პროცესებიka_GE
dc.subjectEarth and its Envelopesen
dc.subjectGeophysical Processesen
dc.subjectmean max annual air temperatureen
dc.subjectclimate changeen
dc.subjectsignificant valueen
dc.subjectsecond power polynomialen
dc.titleVariability of the Mean Max Annual Air Temperature in 39 Locations of Georgia in 1956-2015en
dc.typeArticleen
dc.typeსტატიაka_GE
Appears in Collections:საერთაშორისო სამეცნიერო კონფერენცია „დედამიწასა და მის გარსებში მიმდინარე გეოფიზიკური პროცესები“ - International Scientific Conference "Geophysical Processes in the Earth and its Envelopes" - (2023)

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