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dc.contributor.authorMelikadze, G.en_US
dc.contributor.authorKapanadze, N.en_US
dc.contributor.authorTodadze, M.en_US
dc.contributor.authorმელიქაძე, გ.ka_Ge
dc.contributor.authorკაპანაძე, ნ.ka_Ge
dc.contributor.authorთოდაძე, მ.ka_Ge
dc.contributor.authorМеликадзе, Г.ru
dc.contributor.authorКапанадзе, Н.ru
dc.contributor.authorТодадзе, М.ru
dc.identifier.citationJournal Of The Georgian Geophysical Society Issue (A), Physics of Solid Earth. vol.16A 2013, pp.19-24.en_US
dc.identifier.citationსაქართველოს გეოფიზიკური საზოგადოების ჟურნალი სერია ა. დედამიწის ფიზიკა. ტომი 16ა 2013, გვ.19-24.ka_Ge
dc.descriptionDuring study summarizing exiting meteorological, hydrological and snow data in the studied area, installation of the monitoring network, collection of water samples, snow expeditions and a more detailed sampling during snowmelt. Regular monitoring consists of precipitation, air temperature and humidity measurements at 3 sites, and water level measurements at 2 rivers. Monthly samples for isotopic analyses (stable water isotopes) are collected from 3 raingauges, 2 rivers, 1 borehole and 2 springs since. The network build in the project provided a lot of new data on snow hydrology in the studied area that was not available before. Measurements at different altitudes were useful. Although snowfall represents just about 30% of annual precipitation, snowmelt water is an important source of water for the rivers (maximum contribution about 50%). Snowmelt affects river runoff at least 2-3 months. Yet, stable water isotopes in the snowmelt water significantly differ among the sites and they are different from those in the snow cover.en_US
dc.titleAssessment the role of snow in hydrological cycle of the Borjomula-Gudjareti Tskali rivers basinen_US
dc.titleИсследование роли снега в гидрогеологическом цикле в басейнах рек Боржомула – Гуджаретис Цкалиru
dc.titleთოვლის როლის განსაზღვრა წყალბრუნვის ციკლში ბორჯომულა გუჯარეთის წყლის მდინარეთა აუზებშიka_Ge
Appears in Collections:Journal Of The Georgian Geophysical Society (2013)

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