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200 1 _aResources, regime and quality of surface waters in the Ob River basin: history, current state and problems of research
_fV. A. Zemtsov, O. G. Savichev
203 _aText
_celectronic
300 _aTitle screen
320 _a[References: p. 394-396 (48 tit.)]
330 _aThe paper presents the history and major results of research into resources, regime and quality of the surface water in the Ob basin, concentrated in such water bodies as glaciers, rivers, lakes, reservoirs and wetlands. Studies have long been carried out by such government agencies as the Hydrometeorological Service (Hydromet), the Ministry of Energy and others, engineering organizations, scientific research institutes of the academy of sciences and universities. The studies included large complex tasks aimed at economic development of the basin territory. By the 1980s, an expanded network of stationary hydrological observations existed, and basic information about the factors of resources formation, regime and surface water quality, as well as long-term dynamics of hydrological characteristics had been obtained. Today, a multidisciplinary and interdisciplinary approach to the hydrological cycle and geo-run-off at the global and regional scales is related to the changes in climate and the environment in general.
333 _aРежим доступа: по договору с организацией-держателем ресурса
461 _tInternational Journal of Environmental Studies
_d1970-
463 _tVol. 72, iss. 3 : The great Ob River basin
_v[P. 386-396]
_d2015
610 1 _aэлектронный ресурс
610 1 _aтруды учёных ТПУ
610 1 _aгидрология
610 1 _aгидрохимия
610 1 _aОбь
610 1 _aбассейны рек
610 1 _aгеосток
700 1 _aZemtsov
_bV. A.
_gValeriy A.
701 1 _aSavichev
_bO. G.
_cgeologist
_cProfessor of Tomsk Polytechnic University, doctor of geographical sciences
_f1967-
_gOleg Gennadievich
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712 0 2 _aНациональный исследовательский Томский политехнический университет (ТПУ)
_bИнститут природных ресурсов (ИПР)
_bКафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
_h100
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856 4 _uhttp://dx.doi.org/10.1080/00207233.2015.1019299
942 _cCF