Water runoff vs modern climatic warming in mountainous cryolithic zone in North-East Russia

3rd International Conference Environment and Sustainable Development of Territories: Ecological Challenges of the 21st Century

生态环境科学;地球科学;经济学

Glotov, V.E.^1,2 ; Glotova, L.P.^1,2

North-East Interdisciplinary Science Research Institute, Port str., 16, Magadan

685000, Russia^1

Russian Academy of Sciences Far East Branch, Svetlanskaya str., 50, Vladivostok

690990, Russia^2

关键词: Biological productivity;    Climatic conditions;    Climatic warming;    Continental slope;    Ground water recharge;    Recharge process;    Subsurface waters;    Vegetation cover;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/107/1/012028/pdf
DOI  :  10.1088/1755-1315/107/1/012028

学科分类：环境科学（综合）

来源: IOP

【 摘 要 】

The article presents the results of studying the effects of current climatic warming for both surface and subsurface water runoffs in North-East Russia, where the Main Watershed of the Earth separates it into the Arctic and Pacific continental slopes. The process of climatic warming is testified by continuous weather records during 80-100 years and longer periods. Over the Arctic slope and in the northern areas of the Pacific slope, climatic warming results in a decline in a total runoff of rivers whereas the ground-water recharge becomes greater in winter low-level conditions. In the southern Pacific slope and in the Sea of Okhotsk basin, the effect of climatic warming is an overall increase in total runoff including its subsurface constituents. We believe these peculiar characters of river runoff there to be related to the cryolithic zone environments. Over the Arctic slope and the northern Pacific slope, where cryolithic zone is continuous, the total runoff has its subsurface constituent as basically resulting from discharge of ground waters hosted in seasonally thawing rocks. Warmer climatic conditions favor growth of vegetation that needs more water for the processes of evapotranspiration and evaporation from rocky surfaces in summer seasons. In the Sea of Okhotsk basin, where the cryolithic zone is discontinuous, not only ground waters in seasonally thawing layers, but also continuous taliks and subpermafrost waters participate in processes of river recharges. As a result, a greater biological productivity of vegetation cover does not have any effect on ground-water supply and river recharge processes. If a steady climate warming is provided, a continuous cryolithic zone can presumably degrade into a discontinuous and then into an island-type permafrost layer. Under such a scenario, there will be a general increase in the total runoff and its subsurface constituent. From geoecological viewpoints, a greater runoff will have quite positive effects, whereas some minor negative consequences of it can be successfully prevented.