Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН

[Text] / A. . Onuchin, T. . Burenina ; ed.: J Krope, Krope, J // ADVANCED TOPICS ON WATER RESOURCES, HYDRAULICS AND HYDROLOGY: PROCEEDINGS OF THE 3RD IASME/WSEAS INTERNATIONAL CONFERENCE ON WATER RESOURCES, HYDRAULICS AND HYDROLOGY (WHH '08). Ser. Mathematics and Computers in Science and Engineering : WORLD SCIENTIFIC AND ENGINEERING ACAD AND SOC, 2008. - 3rd IASME/WSEAS International Conference on Water Resources, Hydraulics and Hydrology (FEB 23-25, 2008, Cambridge, ENGLAND). - P131-133. - Cited References: 6 . - 3. - ISBN 978-960-6766-37-4РУБ Engineering, Civil + Water Resources

Аннотация: Siberian Rivers account for a great part of water discharge into the Arctic Ocean. Along with the regional climate and the presence permafrost, hydrological processes occurring in catchments of the boreal taiga rivers are controlled by forest harvesting levels. Forests of the Lower Angara region have been harvested extensively over the past fifty years. As a result, forest area has been reduced and forest age structure and composition have changed. These changes are reflected in the natural water budget structure and hydrological regimes of areas. The study revealed that hydrological effects of forest logging conducted in Siberia characterized by a highly continental climate and, hence, severe forest growing conditions differ from those observed for the European Russia.

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Держатели документа:
[Onuchin, Alexander
Burenina, Tamara] Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Onuchin, A...; Burenina, T...; Krope, J \ed.\

[Text] / A. S. Prokushkin [et al.] // Glob. Biogeochem. Cycle. - 2007. - Vol. 21, Is. 4. - Ст. GB4003, DOI 10.1029/2007GB002938. - Cited References: 39 . - 12. - ISSN 0886-6236РУБ Environmental Sciences + Geosciences, Multidisciplinary + Meteorology & Atmospheric Sciences

Аннотация: Terrestrial and aquatic dissolved organic matter (DOM) was characterized to trace the likely processes of DOM formation and stream export in a permafrost-dominated watershed in central Siberia. Stream samples were collected in spring (May-June 2003) and summer (July-August 2003) at both low flow and stormflow. Dissolved organic matter was analyzed by pyrolysis/gas chromatography/mass spectrometry, and identified pyrolysis products were simultaneously analyzed for compound-specific isotope ratios by isotope ratio mass spectrometry. Pyrograms of terrestrial and stream DOM contained a similar series of pyrolysis products, suggesting a terrestrial origin for DOM in the small stream draining our study catchment. However, despite the overall similarity of chemical composition of stream DOM at different seasons, we also observed distinct differences in isotopic fingerprint between seasons and hydrologic phases ( stormflow versus low flow). This variation appears to be due to the changing origin of stream DOM from different soil layers and the catchment sources following permafrost thawing during the frost-free period. In general, chemical and isotopic composition of stream DOM was similar to DOM produced in soils of colder north facing slopes ( P 0.01) with a shallow active layer. South facing slopes with deeper active layers produce little DOM that enters the stream, suggesting that DOM produced in the active layer is retained and stabilized in underlying, unfrozen mineral soils. Climate change that results in additional seasonal thawing of permafrost-dominated landscapes will decrease the amount of DOM exported to riverine systems and change its chemical composition.

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Держатели документа:
Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia
Max Planck Inst Biogeochem, D-07745 Jena, Germany
Univ New Hampshire, Durham, NH 03824 USA

Доп.точки доступа:
Prokushkin, A.S.; Gleixner, G...; McDowell, W.H.; Ruehlow, S...; Schulze, E.D.

/ A. Onuchin [et al.] // IAHS-AISH Publication. - 2009. - Vol. 331: Symposium JS.4 at the Joint Convention of the International Association of Hydrological Sciences, IAHS and the International Association of Hydrogeologists, IAH (6 September 2009 through 12 September 2009, Hyderabad) Conference code: 83573. - P163-170 . -
Аннотация: River flow is vitally important to many human activities. River flow is influenced by climatic and land-cover changes. Land-use practices have a significant effect on water flow and quality. Land use can change surface runoff, which in turn can be used as an environmental indicator of a land use level of sustamability. Along with the regional climate, hydrological processes occurring in river basins in Siberia and mountainous Kyrgyzia are controlled by forest logging and afforestation. The method used to analyse annual river flow genesis to date allowed the onset of, and assessment of, the level of human activities in the watersheds. Moreover, river flow genesis can be used in land use decision-making. River flow reflects all watershed changes, which can have opposite effects, thus compensating for each other. This study confirmed that river flow changes in time, thus reflecting land cover changes in watersheds. Copyright В© 2009 IAHS Press.

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Держатели документа:
V. N. Sukachev Institute of Forest Siberian Branch, Russian Academy of Sciences, 660036, Academgorodok, Krasnoyarsk, Russian Federation
P. A. Gan Institute of Forest and Nut Plantation, Kyrgyzian Academy of Sciences, Kargachevaya rosha, 15, 720015, Bishkek, Kyrgyzstan

Доп.точки доступа:
Onuchin, A.; Burenina, T.; Gaparov, K.; Ziryukina, N.

/ A. A. Onuchin, T. A. Burenina // Trends in Water Resour. Res. - 2008. - P67-92 . - ISBN 9781604560381 (ISBN)
Аннотация: There are many aspects of the hydrological role of forest ecosystems. It includes the forest effect on transformation and spatial distribution of precipitation and snow-cover, regulating of runoff, soil evaporation and evapotranspiration. Scientific research in boreal forests of Siberia (Sayn, Prybaikalje, Enisey chain of hills, plateau Putorana) showed that 1-5% of snow is caught by crown of deciduous stands and 10-45% - by crowns of coniferous. As for summer precipitation it was obtained that 8-27% of precipitation is caught by crown of deciduous stands and 15-40% - by crowns of coniferous. Siberian rivers are of global importance as they impact on the fresh water budget of the Arctic Ocean. Formation of Siberian rivers runoff and its season dynamics depends on forest vegetation to a considerable extent. Many rivers of Southern taiga and mountain regions drain areas of land that experienced a dramatic land-cover change, with a decrease in overall forest area and a relative increase in deciduous trees. Land cover change in forest catchments (cutting down, wild fires) impact on water balance and water-protective functions of forest. Scientific research in Prybaikalje showed that restoration of water protective and, in particular, erosion- protective functions of forest after cuttings on separate slopes and in large catchments occur differently. The idea of ranging catchments according to hierarchical levels was used to make a deep analysis of erosion- protective and water- protective forest functions for the territorial units of different ranks. Date obtained by different methods was generalized and the elements of the system analysis and mathematical modeling of water- protective, water- regulating and soil- protective forest functions were used. В© 2008 by Nova Science Publishers, Inc. All rights reserved.

Scopus

Держатели документа:
V.N. Sukachev Institute of Forest, Siberian Br., Russian Academy of Sciences, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Onuchin, A.A.; Burenina, T.A.

/ T. A. Burenina, A. A. Onuchin, E. V. Fedotova // Forest Ecosystems: Biodiversity, Management and Conservation . - 2014. - P117-148 . - ISBN 9781631178160 (ISBN); 9781631178153 (ISBN)
Аннотация: Siberian rivers account for a great part of water discharge into the Arctic Ocean. Along with the regional climate and the presence permafrost, hydrological processes occurring in catchments of the boreal taiga rivers are controlled by forest harvesting levels. Forests of the Angara region and West Sayan have been harvested extensively over the past fifty years. As a result, forest area has been reduced and forest age structure and composition have changed. These changes are reflected in the natural water budget structure and hydrological regimes of areas. The study revealed that hydrological effects of forest logging conducted in North Angara region characterized by a highly continental climate and, hence, severe forest growing conditions differ from those in West Sayan. © 2014 by Nova Science Publishers, Inc. All rights reserved.

Scopus

Держатели документа:
V.N. Sukachev Institute of Forest Siberian Branch, Russian Academy of Sciences, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Burenina, T. A.; Onuchin, A. A.; Fedotova, E. V.
Свободных экз. нет

/ L. Hellmann [et al.] // Dendrochronologia. - 2016. - Vol. 39: Workshop on Current Status and the Potential of Tree-Ring Research in (JAN 20-21, 2015, Krasnoyarsk, RUSSIA). - P3-9, DOI 10.1016/j.dendro.2015.12.010. - Cited References:53 . - ISSN 1125-7865. - ISSN 1612-0051РУБ Plant Sciences + Forestry + Geography, Physical

Аннотация: Arctic driftwood represents a unique proxy archive at the interface of marine and terrestrial environments. Combined wood anatomical and dendrochronological analyses have been used to detect the origin of driftwood and may allow past timber floating activities, as well as past sea ice and ocean current dynamics to be reconstructed. However, the success of driftwood provenancing studies depends on the length, number, and quality of circumpolar boreal reference chronologies. Here, we introduce a Eurasian-wide high-latitude network of 286 ring width chronologies from the International Tree Ring Data Bank (ITRDB) and 160 additional sites comprising the three main boreal conifers Pinus, Larix, and Picea. We assess the correlation structure within the network to identify growth patterns in the catchment areas of large Eurasian rivers, the main driftwood deliverers. The occurrence of common growth patterns between and differing patterns within catchments indicates the importance of biogeographic zones for ring width formation and emphasizes the degree of spatial precision when provenancing. Reference chronologies covering millennial timescales are so far restricted to a few larch sites in Central and Eastern Siberia (eastern Taimyr, Yamal Peninsula and north-eastern Yakutia), as well as several pine sites in Scandinavia, where large rivers are missing though. The general good spatial coverage of tree-ring sites across northern Eurasia indicates the need for updating and extending existing chronologies rather than developing new sites. (C) 2016 Elsevier GmbH. All rights reserved.

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Держатели документа:
WSL, Swiss Fed Res Inst, Birmensdorf, Switzerland.
Oeschger Ctr Climate Change Res, Bern, Switzerland.
Inst Plant & Anim Ecol UD RAS, Ekaterinburg, Russia.
Swiss Fed Inst Technol, Inst Terr Ecosyst, Zurich, Switzerland.
Univ Bern, Dendrolab Ch, Bern, Switzerland.
Johannes Gutenberg Univ Mainz, Mainz, Germany.
Iceland Forest Serv, Reykjavik, Iceland.
VN Sukachev Inst Forest SB RAS, Krasnoyarsk, Russia.
Stolby Natl Wildlife Nat Reserve, Krasnoyarsk, Russia.
Siberian Fed Univ, Krasnoyarsk, Russia.
North Eastern Fed Univ, Yakutsk, Russia.
Melnikov Permafrost Inst, Yakutsk, Russia.
RAS, Inst Geog, Moscow, Russia.
Univ Freiburg, Inst Forest Sci IWW, Freiburg, Germany.
Global Change Res Ctr AS CR, Brno, Czech Republic.

Доп.точки доступа:
Hellmann, Lena; Agafonov, Leonid; Churakova, O.; Duthorn, Elisabeth; Eggertsson, Olafur; Esper, Jan; Kirdyanov, Alexander V.; Knorre, Anastasia A.; Moiseev, Pavel; Myglan, Vladimir S.; Nikolaev, Anatoly N.; Reinig, Frederick; Schweingruber, Fritz; Solomina, Olga; Tegel, Willy; Buntgen, Ulf; buentgen, ulf

/ A. Onuchin, T. Burenina, I. Pavlov // Environments. - 2017. - Vol. 4, Is. 3. - Ст. 51, DOI 10.3390/environments4030051. - Cited References:58. - Government of Krasnoyarsk Territory according to the research project NO 16-44-242145. . - ISSN 2076-3298РУБ Agricultural Engineering

Аннотация: Despite a large number of publications covering various aspects of the influence of climatic factors on runoff, this direction in hydrological research acquires a new meaning in connection with global climate change and the increase in anthropogenic press on river systems. The authors of this work focused on the impact of anthropogenic factors on river runoff. Many rivers of Siberian taiga drain areas have experienced a dramatic land-cover change, with a decrease in overall forest area and a relative increase in deciduous trees. Land cover change in forest catchments impact water balance and accordingly, river flow. The study areas, the West Sayan and Northern Angara regions located in Central Siberia, are now a mosaic of forest regeneration sites including both post-human and post-fire regeneration patterns. Data of our own hydrological experiments conducted on clear cuts of different ages and reference materials for regular hydrological observations were analyzed. Dynamics of river flow under influence of timber harvesting were studied for 11 river basins in different landscape zones of Siberia. The studies showed that, in Siberia, forest cover changes lead to either reduction of, or increase in water yield depending on forest structure and climate. Dynamics of river flow after forest logging differ for continental and humid climates. Where precipitation is excessive, water yield increases twice that of control plots during the first several post-cutting years, due to reduction of transpiring phytomass. It takes 30-40 years and sometimes even over 50 years, depending on forest succession trajectories, for water yield to recover to the pre-cutting level. In an extremely continental climate, extensive forest cutting results in decreasing water yield during the first post-clearcutting years, because wind activity increases and enhances snow evaporation on vast clear cuts. Water yield exhibited an average annual decrease of 0.5-1.0 mm during the first two decades after cutting, i.e., until when clear cuts began to regenerate. With further development of forest vegetation, water yield increased by 1.5-3 mm annually. Obtained results show that at the regional level in conditions of anthropogenic press on the forests at the catchments of medium and small rivers, the climatic trends are offset by the felling and subsequent reforestation dynamics at clear cuts.

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Держатели документа:
Russian Acad Sci, Forest Siberian Branch, VN Sukachev Inst, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Onuchin, Alexander; Burenina, Tamara; Pavlov, Igor; RFBR; Government of Krasnoyarsk Territory [16-44-242145]

/ A. Onuchin, Т. Burenina, А. Shvidenko [et al.] // For. Ecosyst. - 2021. - Vol. 8, Is. 1. - Ст. 45, DOI 10.1186/s40663-021-00316-w . - ISSN 2095-6355
Аннотация: Background: Assessment of the reasons for the ambiguous influence of forests on the structure of the water balance is the subject of heated debate among forest hydrologists. Influencing the components of total evaporation, forest vegetation makes a significant contribution to the process of runoff formation, but this process has specific features in different geographical zones. The issues of the influence of forest vegetation on river runoff in the zonal aspect have not been sufficiently studied. Results: Based on the analysis of the dependence of river runoff on forest cover, using the example of nine catchments located in the forest-tundra, northern and middle taiga of Northern Eurasia, it is shown that the share of forest cover in the total catchment area (percentage of forest cover, FCP) has different effects on runoff formation. Numerical experiments with the developed empirical models have shown that an increase in forest cover in the catchment area in northern latitudes contributes to an increase in runoff, while in the southern direction (in the middle taiga) extensive woody cover of catchments “works” to reduce runoff. The effectiveness of geographical zonality in regards to the influence of forests on runoff is more pronounced in the forest-tundra zone than in the zones of northern and middle taiga. Conclusion: The study of this problem allowed us to analyze various aspects of the hydrological role of forests, and to show that forest ecosystems, depending on environmental conditions and the spatial distribution of forest cover, can transform water regimes in different ways. Despite the fact that the process of river runoff formation is controlled by many factors, such as temperature conditions, precipitation regime, geomorphology and the presence of permafrost, the models obtained allow us to reveal general trends in the dependence of the annual river runoff on the percentage of forest cover, at the level of catchments. The results obtained are consistent with the concept of geographic determinism, which explains the contradictions that exist in assessing the hydrological role of forests in various geographical and climatic conditions. The results of the study may serve as the basis for regulation of the forest cover of northern Eurasian river basins in order to obtain the desired hydrological effect depending on environmental and economic conditions. © 2021, The Author(s).

Scopus

Держатели документа:
V.N. Sukachev Institute of Forest, Siberian Branch of the Russian Academy of Sciences 660036, Academgorodok, 50/28, Russia 31, Krasnoyarsk, Russian Federation
International Institute for Applied Systems Analysis, Laxenburg, A-2361, Austria

Доп.точки доступа:
Onuchin, A.; Burenina, Т.; Shvidenko, А.; Prysov, D.; Musokhranova, A.

/ A. Onuchin, T. Burenina, A. Shvidenko [et al.] // For. Ecosyst. - 2021. - Vol. 8, Is. 1. - Ст. 45, DOI 10.1186/s40663-021-00316-w. - Cited References:44. - This work was supported by the basic project of the IF SB RAS "Theoretical Foundations of Preserving the Ecological and Resource Potential of Siberian Forests under the Conditions of Increasing Anthropogenic Press and Climate Anomalies", No. AAAA-A17-117101940014-9 (0356-2019-0027). The reported study was funded by RFBR (project number 20-05-00095). . - ISSN 2095-6355. - ISSN 2197-5620РУБ Forestry

Аннотация: Background Assessment of the reasons for the ambiguous influence of forests on the structure of the water balance is the subject of heated debate among forest hydrologists. Influencing the components of total evaporation, forest vegetation makes a significant contribution to the process of runoff formation, but this process has specific features in different geographical zones. The issues of the influence of forest vegetation on river runoff in the zonal aspect have not been sufficiently studied. Results Based on the analysis of the dependence of river runoff on forest cover, using the example of nine catchments located in the forest-tundra, northern and middle taiga of Northern Eurasia, it is shown that the share of forest cover in the total catchment area (percentage of forest cover, FCP) has different effects on runoff formation. Numerical experiments with the developed empirical models have shown that an increase in forest cover in the catchment area in northern latitudes contributes to an increase in runoff, while in the southern direction (in the middle taiga) extensive woody cover of catchments "works" to reduce runoff. The effectiveness of geographical zonality in regards to the influence of forests on runoff is more pronounced in the forest-tundra zone than in the zones of northern and middle taiga. Conclusion The study of this problem allowed us to analyze various aspects of the hydrological role of forests, and to show that forest ecosystems, depending on environmental conditions and the spatial distribution of forest cover, can transform water regimes in different ways. Despite the fact that the process of river runoff formation is controlled by many factors, such as temperature conditions, precipitation regime, geomorphology and the presence of permafrost, the models obtained allow us to reveal general trends in the dependence of the annual river runoff on the percentage of forest cover, at the level of catchments. The results obtained are consistent with the concept of geographic determinism, which explains the contradictions that exist in assessing the hydrological role of forests in various geographical and climatic conditions. The results of the study may serve as the basis for regulation of the forest cover of northern Eurasian river basins in order to obtain the desired hydrological effect depending on environmental and economic conditions.

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Держатели документа:
Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Academgorodok 50-28,Russia 31, Krasnoyarsk 660036, Russia.
Int Inst Appl Syst Anal, A-2361 Laxenburg, Austria.

Доп.точки доступа:
Onuchin, A.; Burenina, T.; Shvidenko, A.; Prysov, D.; Musokhranova, A.; basic project of the IF SB RAS "Theoretical Foundations of Preserving the Ecological and Resource Potential of Siberian Forests under the Conditions of Increasing Anthropogenic Press and Climate Anomalies" [AAAA-A17-117101940014-9 (0356-2019-0027)]; RFBRRussian Foundation for Basic Research (RFBR) [20-05-00095]