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

[Text] / Y. L. Liu [et al.] // Clim. Change. - 2014. - Vol. 126, Is. 03.04.2014. - P413-427, DOI 10.1007/s10584-014-1234-9. - Cited References: 53. - This research is supported by the NASA Land Use and Land Cover Change program (NASA-NNX09AI26G, NN-H-04-Z-YS-005-N, and NNX09AM55G), the Department of Energy (DE-FG02-08ER64599), the National Science Foundation (NSF-1028291 and NSF- 0919331), the NSF Carbon and Water in the Earth Program (NSF-0630319), and the Dynamics of Coupled Natural and Human Systems (CNH) Program of the NSF (#1313761). We also acknowledge the Global Runoff Data Centre for provision of the gauge station data. Runoff data in Peterson et al. (2002) were obtained from the R-ArcticNet database. A special acknowledgment is made here to Prof. Eric Wood for his generous provision of the ET datasets of Vinukollu et al. (2011), and to Dr. Brigitte Mueller and Dr. Martin Hirsci for the provision of the LandFlux-EVAL dataset of Mueller et al. (2013). Diego Miralles acknowledges the support by the European Space Agency WACMOS-ET project (4000106711/12/I-NB). . - ISSN 0165-0009. - ISSN 1573-1480РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: Northern Eurasian ecosystems play an important role in the global climate system. Northern Eurasia (NE) has experienced dramatic climate changes during the last half of the 20th century and to present. To date, how evapotranspiration (ET) and water availability (P-ET, P: precipitation) had changed in response to the climatic change in this region has not been well evaluated. This study uses an improved version of the Terrestrial Ecosystem Model (TEM) that explicitly considers ET from uplands, wetlands, water bodies and snow cover to examine temporal and spatial variations in ET, water availability and river discharge in NE for the period 1948-2009. The average ET over NE increased during the study period at a rate of 0.13 mm year(-1) year(-1). Over this time, water availability augmented in the western part of the region, but decreased in the eastern part. The consideration of snow sublimation substantially improved the ET estimates and highlighted the importance of snow in the hydrometeorology of NE. We also find that the modified TEM estimates of water availability in NE watersheds are in good agreement with corresponding measurements of historical river discharge before 1970. However, a systematic underestimation of river discharge occurs after 1970 indicates that other water sources or dynamics not considered by the model (e.g., melting glaciers, permafrost thawing and fires) may also be important for the hydrology of the region.

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Держатели документа:
[Liu, Yaling
Zhuang, Qianlai
He, Yujie] Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA
[Zhuang, Qianlai] Purdue Univ, Dept Agron, W Lafayette, IN 47907 USA
[Pan, Zhihua] China Agr Univ, Coll Resources & Environm Sci, Beijing 100094, Peoples R China
[Miralles, Diego] Univ Ghent, Lab Hydrol & Water Management, B-9000 Ghent, Belgium
[Miralles, Diego] Univ Bristol, Sch Geog Sci, Bristol, Avon, England
[Tchebakova, Nadja] Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk, Russia
[Kicklighter, David
Melillo, Jerry] Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA
[Chen, Jiquan] Michigan State Univ, CGCEO Geog, E Lansing, MI 48824 USA
[Sirin, Andrey] Acad Sci, Lab Peatland Forestry & Ameliorat, Inst Forest Sci, Uspenskoye, Moscow Oblast, Russia
[Zhou, Guangsheng] Chinese Acad Sci, Inst Bot, Beijing, Peoples R China
ИЛ СО РАН

Доп.точки доступа:
Liu, Y.L.; Zhuang, Q.L.; Pan, Z.H.; Miralles, D...; Tchebakova, N...; Kicklighter, D...; Chen, J.Q.; Sirin, A...; He, Y.J.; Zhou, G.S.; Melillo, J...; NASA Land Use and Land Cover Change program [NASA-NNX09AI26G, NN-H-04-Z-YS-005-N, NNX09AM55G]; Department of Energy [DE-FG02-08ER64599]; National Science Foundation [NSF-1028291, NSF- 0919331]; NSF Carbon and Water in the Earth Program [NSF-0630319]; Dynamics of Coupled Natural and Human Systems (CNH) Program of the NSF [1313761]; European Space Agency WACMOS-ET project [4000106711/12/I-NB]

/ V. Margaryan, E. Fedotova // E3S Web of Conferences : EDP Sciences, 2020. - Vol. 149: 2019 Regional Problems of Earth Remote Sensing, RPERS 2019 (10 September 2019 through 13 September 2019, ) Conference code: 157574. - Ст. 03010, DOI 10.1051/e3sconf/202014903010 . -
Аннотация: The paper analyzes the peculiarities of formation of the absolute maximum runoff of the Marmarik river evaluates the patterns of multi-year fluctuations of maximum runoff rates in different river sites and gives a forecast of the maximum runoff in the context of global climate change. Absolute values of the maximum river runoff for different scenarios of climate change are estimated. The actual observational data of Armhydromet for maximum runoff rate, the air temperature and precipitation were used as the source material. As a result of the study, it turned out that there is only a tendency to decrease in the values of maximum runoff. It turned out that for all scenarios and cases in the Marmarik river basin, a different degree of changes in the maximum flow is observed. Moreover, the largest decrease in the maximum runoff of the Marmarik river basin is expected under the conditions of an increase in the average air temperature of the spring season by 2,7 - 3,9 degrees Celsius and a decrease in the amount of spring atmospheric precipitation by 2,4 - 2,6 %. © The Authors, published by EDP Sciences 2020.

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Держатели документа:
Yerevan State University, Department of Physical Geography and Hydrometeorology, Faculty of Geography and Geology, Yerevan, Armenia
Sukachev Institute of Forest Sb Ras, Frc Ksc Sb Ras, Krasnoyarsk, Russian Federation
Sfu, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Margaryan, V.; Fedotova, E.

/ V. Margaryan, G. Tsibulskii, E. Fedotova // E3S Web of Conferences : EDP Sciences, 2020. - Vol. 223: 2020 Regional Problems of Earth Remote Sensing, RPERS 2020 (29 September 2020 through 2 October 2020, ) Conference code: 166122. - Ст. 03019, DOI 10.1051/e3sconf/202022303019 . -
Аннотация: The article assesses the change in air temperature and precipitation, and also examines the impact of climate change on crop yields in the Republic of Armenia. As a source of information, the actual data of agrometeorological observations of the GEO "Center for Hydrometeorology and Monitoring"of the Ministry of Environment of the Republic of Armenia and the National Statistical Service are used. As a result of the study, it turned out that there are trends towards an increase in the average annual values of air temperature and heat provision of crops (in total temperatures above 10.0 ° C). In the studied area, there are no regular changes in the amount of atmospheric precipitation over the year. The impact of climate change will only worsen and lead to various problems in water industry, agriculture, energy, health and other sectors. In the republic in 2000-2018 are observed of both the gross harvest and agricultural crops yield increase, with the exception of the tobacco crop. However, this does not mean that agricultural crops are not affected by climate change. © The Authors, published by EDP Sciences, 2020.

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Держатели документа:
Yerevan State University, Department of Physical Geography and Hydrometeorology, Faculty of Geography and Geology, Yerevan, Armenia
Siberian Federal University, Institute of Space and Information Technologies, Chair of Systems of Artificial Intelligence, 660074 Kirenskogo St. 26, Krasnoyarsk, Russian Federation
Sukachev Institute of Forest SB RAS, FRC KSC SB RAS, Academgorodok 50, Krasnoyarsk, 660036, Russian Federation

Доп.точки доступа:
Margaryan, V.; Tsibulskii, G.; Fedotova, E.

/ V. Margaryan, G. Tsibulskii, E. Fedotova ; ed.: GMT Gennady [et al.] // REGIONAL PROBLEMS OF EARTH REMOTE SENSING (RPERS 2020) : E D P SCIENCES, 2020. - Vol. 223: Conference on Regional Problems of Earth Remote Sensing (RPERS) (SEP 29-OCT 02, 2020, Krasnoyarsk, RUSSIA). - Ст. 03019. - (E3S Web of Conferences), DOI 10.1051/e3sconf/202022303019. - Cited References:7 . - РУБ Environmental Sciences + Geosciences, Multidisciplinary + Remote Sensing

Аннотация: The article assesses the change in air temperature and precipitation, and also examines the impact of climate change on crop yields in the Republic of Armenia. As a source of information, the actual data of agrometeorological observations of the GEO "Center for Hydrometeorology and Monitoring" of the Ministry of Environment of the Republic of Armenia and the National Statistical Service are used. As a result of the study, it turned out that there are trends towards an increase in the average annual values of air temperature and heat provision of crops (in total temperatures above 10.0 degrees C). In the studied area, there are no regular changes in the amount of atmospheric precipitation over the year. The impact of climate change will only worsen and lead to various problems in water industry, agriculture, energy, health and other sectors. In the republic in 2000-2018 are observed of both the gross harvest and agricultural crops yield increase, with the exception of the tobacco crop. However, this does not mean that agricultural crops are not affected by climate change.

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Держатели документа:
Yerevan State Univ, Fac Geog & Geol, Dept Phys Geog & Hydrometeorol, Yerevan, Armenia.
Siberian Fed Univ, Inst Space & Informat Technol, Chair Syst Artificial Intelligence, Kirenskogo St 26, Krasnoyarsk 660074, Russia.
Sukachev Inst Forest SB RAS, FRC KSC SB RAS, Academgorodok 50, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Margaryan, Varduhi; Tsibulskii, Gennady; Fedotova, Elena; Gennady, GMT \ed.\; Noskov, M.V. \ed.\; Maglinets, Y.A. \ed.\

/ S. N. Kirpotin, T. V. Callaghan, A. M. Peregon [et al.] // Ambio. - 2021, DOI 10.1007/s13280-021-01570-6 . - Article in press. - ISSN 0044-7447
Аннотация: Biological diversity is the basis for, and an indicator of biosphere integrity. Together with climate change, its loss is one of the two most important planetary boundaries. A halt in biodiversity loss is one of the UN Sustainable Development Goals. Current changes in biodiversity in the vast landmass of Siberia are at an initial stage of inventory, even though the Siberian environment is experiencing rapid climate change, weather extremes and transformation of land use and management. Biodiversity changes affect traditional land use by Indigenous People and multiple ecosystem services with implications for local and national economies. Here we review and analyse a large number of scientific publications, which are little known outside Russia, and we provide insights into Siberian biodiversity issues for the wider international research community. Case studies are presented on biodiversity changes for insect pests, fish, amphibians and reptiles, birds, mammals and steppe vegetation, and we discuss their causes and consequences. © 2021, Royal Swedish Academy of Sciences.

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Держатели документа:
Tuvan State University, 36 Lenina St., Kyzyl, Republic of Tuva 667000, Russian Federation
Tomsk State University, 36 Lenina Pr., Tomsk, 634050, Russian Federation
University of Sheffield, Alfred Denny Building, Western Bank, Sheffield, S10 2TN, United Kingdom
Institute of Soil Science and Agrochemistry, Siberian Branch of the Russian Academy of Sciences (ISSA SB RAS), Prospect Akademika Lavrentyeva, 8/2, Novosibirsk, 630090, Russian Federation
Institute of the Biological Problem of the North of the Far Eastern Branch of the RAS, 18 Portovaya St, Magadan, 685000, Russian Federation
Siberian Center of State Research Center for Space Hydrometeorology « Planeta», 30, Sovetskaya St, Novosibirsk, 630099, Russian Federation
Novosibirsk Branch of the Russian Federal Research Institute of Fisheries and Oceanography, 1 Pisareva, Novosibirsk, 630091, Russian Federation
Institute of Monitoring of Climatic and Ecological Systems SB RAS, 10/3 Academichesky Pr, Tomsk, 634055, Russian Federation
Sukachev Institute of Forests, Siberian Branch of the Russian Academy of Sciences, 50-28, Academgorodok, Krasnoyarsk, 660036, Russian Federation
Siberian Federal University, Svobodny Pr., 82A, Krasnoyarsk, 660041, Russian Federation
Joint Directorate of Taimyr Nature Reserves, 22 Talnakhskaya St, Norilsk, 663305, Russian Federation
Tomsk State Pedagogical University, 60 Kievskaya St, Tomsk, 634061, Russian Federation

Доп.точки доступа:
Kirpotin, S. N.; Callaghan, T. V.; Peregon, A. M.; Babenko, A. S.; Berman, D. I.; Bulakhova, N. A.; Byzaakay, A. A.; Chernykh, T. M.; Chursin, V.; Interesova, E. A.; Gureev, S. P.; Kerchev, I. A.; Kharuk, V. I.; Khovalyg, A. O.; Kolpashchikov, L. A.; Krivets, S. A.; Kvasnikova, Z. N.; Kuzhevskaia, I. V.; Merzlyakov, O. E.; Nekhoroshev, O. G.; Popkov, V. K.; Pyak, A. I.; Valevich, T. O.; Volkov, I. V.; Volkova, I. I.

/ Т. А. Буренина, Д. А. Прысов, А. В. Мусохранова // География и природные ресурсы. - 2021. - № 3. - P113-121, DOI 10.15372/GIPR20210312 . - ISSN 0206-1619
Аннотация: Для выявления региональных и локальных особенностей гидрологического режима рек криолитозоны на территории Красноярского края проанализирована в пространственном и временном аспектах динамика годового стока исследуемых водотоков региона и выполнен анализ трендов температуры воздуха и атмосферных осадков. В качестве тестовых полигонов выбраны девять речных бассейнов, расположенных в пределах трех ландшафтных зон: лесотундры, северной и средней тайги. Для формирования базы данных были привлечены фондовые материалы Среднесибирского управления по гидрометеорологии и мониторингу окружающей среды - данные многолетних наблюдений за стоком на гидрологических постах, температурой воздуха и осадками на метеостанциях исследуемого региона. Сформированная база данных была использована при построении моделей формирования годового стока рек в зависимости от климатических факторов и для анализа пространственно-временных особенностей формирования речного стока. Исследования показали, что ландшафтная дифференциация территории влияет на пространственное распределение климатических характеристик и, соответственно, на особенности гидрологического режима. Для всех исследуемых водосборов получены уравнения регрессии, отражающие связь речного стока с температурой воздуха и атмосферными осадками. Выявлено, что для среднего годового стока наиболее значимы зимние осадки и температура воздуха теплого периода, тогда как для зимней межени большую роль играют жидкие атмосферные осадки и температурный режим воздуха в зимние месяцы. Анализ линейных трендов среднегодовых температур воздуха и осадков показал, что с середины 1950-х гг. наблюдается устойчивая тенденция повышения температуры воздуха, тогда как тренды атмосферных осадков не только имеют значительные различия в абсолютных величинах, но различаются по знаку. Анализ динамики годового и минимального зимнего стока исследуемых рек за разные периоды наблюдений выявил, что для большей части рек отмечен положительный тренд годового стока от 0,57 до 4,76 мм/год. Зимний сток увеличился от 0,09 до 1,42 мм/год. Это указывает на общую тенденцию увеличения речного стока в исследуемом регионе. Установленная разнонаправленность трендов речного стока и атмосферных осадков показывает, что более значимым фактором в формировании стока рек криолитозоны становится оттаивание многолетнемерзлых грунтов, связанное с ростом температуры воздуха
The spatial and temporal aspects of the dynamics of the annual runoff and the trends in air temperature and precipitation were analyzed to identify regional and local features of the hydrological regime of rivers in the permafrost zone in the territory of Krasnoyarsk krai. Nine river basins located within three landscape zones: forest-tundra, and northern and middle taiga were selected as test sites. To make clear the influence of climatic factors on hydrological regime of the study area the database of long-term hydrological and meteorological observation data was created. Generation of the database used archival material of the Central-Siberian Administration for Hydrometeorology and Environmental Monitoring: long-term observational data on the runoff at hydrological stations, and air temperature and precipitation at weather stations in the study area. The database thus generated was used in constructing models of annual river runoff formation depending on climatic factors, and in analyzing spatial-temporal characteristics of river runoff formation. Investigations showed that the landscape differentiation of the territory influences the spatial distribution of climatic characteristics and, accordingly, the features in the hydrological regime. For all the watersheds under study, regression equations were obtained, which reflect the relationship between river runoff and air temperature and precipitation. For the average annual runoff, precipitation and air temperature during a warm period are most significant, whereas for the winter runoff low the liquid precipitation and air temperature in the winter months are more important. Analysis of linear trends in average annual air temperatures and precipitation showed that since the mid-1950s there has been a steady increase in air temperature, whereas the precipitation trends have not only significant differences in absolute values but differ in sign. Analysis of the dynamics of the annual and minimum winter runoff of the rivers studied in different observation periods showed that most of the rivers are characterized by a positive trend of the annual runoff varying from 0.57 to 4.76 mm/year. The winter runoff increased from 0.09 to 1.42 mm/year. This indicates a general trend for an increase in river discharge in the study area. The opposing trends observed in the river runoff and precipitation show that the thawing of permafrost caused by an increase in air temperature becomes a more significant formation factor for the river runoff in the permafrost zone.

Держатели документа:
Sukachev Institute of Forest SB RAS, Federal Research Center “Krasnoyarsk Science Center SB RAS, Krasnoyarsk, 660036, Russian Federation
ИЛ СО РАН : 660036, Красноярск, Академгородок, 50, стр. 28

Доп.точки доступа:
Буренина, Тамара Анисимовна; Burenina, Tamara Anisimovna; Прысов, Дмитрий Александрович; Prysov, Dmitry Alexandrovich; Мусохранова, Анастасия Викторовна; Musokhranova Anastasiya Viktorovna

/ T. A. Burenina, D. A. Prysov, A. V. Musokhranova // Geogr. Natural Resources. - 2021. - Vol. 42, Is. 3. - P282-289, DOI 10.1134/S1875372821030070. - Cited References:27. - The study was supported by the base project of the Sukachev Institute of Forest, Siberian Branch, Russian Academy of Sciences ("Theoretical Bases for the Preservation of the Environmental and Resource Potential of Siberian Forests amid the Increasing Anthropogenic Pressure and Cli-matic Anomalies"), project no. AAAA-A17-117101940014-9 (0356-2019-0027). . - ISSN 1875-3728. - ISSN 1875-371XРУБ Geography

Аннотация: The annual runoff dynamics of the studied regional watercourses, as well as the air temperature and precipitation trends, were analyzed in the spatial and temporal aspects to identify the regional and local characteristics of the hydrological regime of rivers in the cryolithozone of Krasnoyarsk krai. Nine river basins located in three landscape zones (forest-tundra, northern taiga, and middle taiga) were selected as test sites. A hydrological and meteorological database was produced using archive materials provided by the Central Siberian Administration for Hydrometeorology and Environmental Monitoring, including long-time river runoff data collected at hydrological stations and air temperature and precipitation data collected at meteorological stations in the studied region. The database was used to develop models that describe the annual river runoff formation in dependence to climatic factors and to analyze the spatiotemporal characteristics of the river runoff formation. It was found that the landscape differentiation of the area affects the spatial distribution of climatic parameters and, accordingly, hydrological regime characteristics. Regression equations describing relationships between river runoff on the one hand and air temperature and precipitation on the other hand were produced for all studied catchment basins. It is established that precipitation and air temperature during the warm period affect the average annual runoff most significantly, while liquid precipitation and air temperature in winter months largely determine the winter low-water runoff. Analysis of linear trends in average annual air temperatures and precipitations shows a steady increase in air temperature since the mid-1950s; while precipitation trends not only differ significantly in absolute values, but are of different signs. Analysis of the annual and minimum winter runoff dynamics in different observation periods performed for the studied rivers shows that most of them demonstrate upward annual runoff trends varying from 0.57 to 4.76 mm/yr. The winter runoff has increased from 0.09 to 1.42 mm/yr. This indicates an overall upward river runoff trend in the studied region. The established multidirectionality of the river runoff and precipitation trends indicates that thawing of perennially frozen grounds caused by the increase in air temperature is becoming an increasingly significant river runoff formation factor in the cryolithozone.

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

Доп.точки доступа:
Burenina, T. A.; Prysov, D. A.; Musokhranova, A., V; Sukachev Institute of Forest, Siberian Branch, Russian Academy of SciencesRussian Academy of Sciences [AAAA-A17-117101940014-9 (0356-2019-0027)]