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Climatic factors are the most important of all the factors that influence the hydrograph shape of a river; this is because they are dynamic in space and time. The presence of hydrographs with a similar shape in long-term observation series of water runoff indicates that from time to time in the catchment of a river the same conditions of water runoff formation repeat. This is due to the cyclicity of climatic and – as a consequence – hydrological processes. The classification of hydrographs based on the similarity of their shapes on the Desna River (observation period 18852010) was carried out using the geometrical similarity criterion (ρ) and the average Euclidean distance between values of hydrograph pairs (η). 41 classes of hydrographs, which included from 1 to 6 hydrographs, were obtained. Among them were determined 12 classes with low probability, 9 classes with medium probability and 20 classes with high probability. An analysis of the conditions of hydrograph formation for each of the identified classes was performed for the following factors: the sums of daily air temperatures and precipitation during the period of positive air temperature (from July) and the period of negative air temperatures, and also during the period of temperature transition through 0ºC up to the peak discharges, index of depth of soil freezing, index of snow water equivalent, index of soil moisture content, and index of snowmelt. In general, hydrographs which are included in one class have similar climatic conditions to those of water runoff formation. However, in some cases, a combination of different values and dynamic factors can lead to the formation of similar hydrograph shapes.
Słowa kluczowe
Rocznik
Tom
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63--70
Opis fizyczny
Bibliogr. 19 poz., rys., tab., wykr.
Twórcy
autor
- Ukrainian Hydrometeorological Institute, Prospekt Nauki 37, 03028 Kyiv, Ukraine
autor
- Ukrainian Hydrometeorological Institute, Prospekt Nauki 37, 03028 Kyiv, Ukraine
autor
- Ukrainian Hydrometeorological Institute, Prospekt Nauki 37, 03028 Kyiv, Ukraine
Bibliografia
- 1. Bagrov N.A., 1969, Classification of synoptic situations, (in Ukrainian), Meteorology and Hydrology, 5, 3-12
- 2. de Laat P.J.M., Savenije H.H.G., 1992, Factors affecting hydrograph shape, Hydrology, Delft, 89-91
- 3. Gorbachova L.O., 2014a, Methodical approaches to the assessment of the homogeneity and stationarity of hydrological observation series, (in Ukrainian), Hydrology, Hydrochemistry and Hydroecology, 1 (32), 22-31
- 4. Gorbachova L.O., 2014b, Spatial distribution of links between the elements of the water balance catchments of Ukraine, (in Ukrainian), Ukrainian Geographical Journal, 2, 17-21
- 5. Gorbachova L., Bauzha T., 2013, Complex analysis of stationarity and homogeneity of flash flood maximum discharges in the Rika River basin, Energetika, 59 (3), 167-174
- 6. Gorbachova L.O., Kolianchuk O.V., 2012, Long-term dynamics of the main hydrometeorological characteristics of spring flood in the Desna River basin, [in:] Water Resource and Wetlands Conference proceedings, Tulcea, Romania, 174-179
- 7. Hannah D.M., Gurnell A.M., McGregor G.R, 1999, A methodology for investigation of the seasonal evolution in proglacial hydrograph form, Hydrological Processes, 13 (16), 2603-2621
- 8. Koshkina O.V., Gorbachova L.O., 2013, Hydro-genetic research method of the main factors of the spring flood in the Desna River Basin, 11th annual International Conference of Young Scientists on Energy Issues, Cyseni, Kaunas, Lithuanian Energy Institute, IX618-IX631
- 9. Koshkina O.V., Hlotka D.V., 2013, Spatial distribution of spring flood hydrometeorological characteristics in the Desna River basin using GIS, (in Ukrainian), Proceedings of Ukrainian Hydrometeorological Institute, 264, 34-43
- 10. Khrystyuk B.F., 2013, The technique of the classification of river hydrographs by criteria of analogy, (in Ukrainian), Hydrology, Hydrochemistry and Hydroecology, 3 (30), 15-20
- 11. Martazinova V.F., 2005, The classification of synoptic patterns by method of analogs, Journal of Environmental Science and Engineering, 7, 61-65
- 12. Perkins, R.M., Jones J.A., 2008, Climate variability, snow, and physiographic controls on storm hydrographs in small forested basins, western Cascades, Oregon, Hydrological Processes, 22, 4949-4964, DOI: 10.1002/hyp.7117
- 13. Ramirez J.A., 2000, Prediction and modeling of flood hydrology and hydraulics, [in:] Inland flood hazards: human, riparian and aquatic communities, E. Wohl (ed.), Cambridge University Press, 293-333
- 14. Szalińska W., Otop I., Tokarczyk T., 2014, Precipitation extremes during flooding in the Odra River Basin in May-June 2010, Meteorology Hydrology and Water Management, 2, 13-20
- 15. Tennant C.J., 2011, The influence of precipitation phase on hydrograph form: an investigation of twelve tributaries to the Salmon River, Idaho, M.S. thesis, Idaho State University, 89 pp.
- 16. Vishnevskiy V.I., 2000, Rivers and reservoirs of Ukraine. Condition and use, (in Ukrainian), Monograph, Vipol, 376 pp.
- 17. Vladimirov A.М., 2009, The factors determining occurrence of the high flow and highest water level during a flood, (in Russian), Proceedings of the Russian State Hydrometeorological University. A theoretical research journal, 9, 22-39
- 18. Wirosoedarmo R., Haji A., Tunggul Sutan, Pramesti E.M., 2010, Study on form, drainage network, and watershed hydrograph by using SIMODAS (case study on Sabu Island – Nusa Tenggara Timur), Jurnal Teknologi Pertanian, 11 (2), 123-130
- 19. WMO, 2009, Guide to hydrological practices. Volume II: Management of water resources and application of hydrological practices, WMO No 168, Geneva, available at: http:// www.whycos.org/chy/guide/168_Vol_II_en.pdf (data access 06.05.2016
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-30d84c62-9125-44f4-8647-0c6bfc83a427