Please use this identifier to cite or link to this item: http://openlibrary.ge/handle/123456789/4985
Title: Assessment the role of snow in hydrological cycle of the Borjomula-Gudjareti Tskali rivers basin
Исследование роли снега в гидрогеологическом цикле в басейнах рек Боржомула – Гуджаретис Цкали
თოვლის როლის განსაზღვრა წყალბრუნვის ციკლში ბორჯომულა გუჯარეთის წყლის მდინარეთა აუზებში
Authors: Melikadze, G.
Kapanadze, N.
Todadze, M.
მელიქაძე, გ.
კაპანაძე, ნ.
თოდაძე, მ.
Меликадзе, Г.
Капанадзе, Н.
Тодадзе, М.
Keywords: გეოფიზიკა;შრომები;ჰიდროგეოფიზიკა
Issue Date: 2013
Citation: Journal Of The Georgian Geophysical Society Issue (A), Physics of Solid Earth. vol.16A 2013, pp.19-24.
საქართველოს გეოფიზიკური საზოგადოების ჟურნალი სერია ა. დედამიწის ფიზიკა. ტომი 16ა 2013, გვ.19-24.
Description: During 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.
URI: http://hdl.handle.net/123456789/4985
Appears in Collections:Journal Of The Georgian Geophysical Society (2013)

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