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

[Text] / Y. . Nakai [et al.] // Theor. Appl. Climatol. - 2008. - Vol. 93, Is. 03.04.2013. - P133-147, DOI 10.1007/s00704-007-0337-x. - Cited References: 47. - We gratefully thank V. Borovikov and other colleagues of the Sukachev Institute of Forest and the Evenki Forest Management Agency in Tura for their support with logistics and instrumentation. We also thank T. Yorisaki, H. Tanaka, and the staff of "Climatec Inc.'' for system integration and instrumentation. We acknowledge Y. Ohtani, Y. Yasuda, and T. Watanabe for providing software resources. N. Saigusa encouraged us greatly. This research was supported by the "Global environment research fund S-1'', as "Integrated Study for Terrestrial Carbon Management of Asia in the 21th Century based on Scientific Advancements (FY2002-2006)''. . - 15. - ISSN 0177-798XРУБ Meteorology & Atmospheric Sciences

Аннотация: Gmelin larch ( Larix gmelinii) forests are representative vegetation in the continuous permafrost region of Central Siberia. Information on the carbon budget is still limited for this Siberian larch taiga in comparison to boreal forests in other regions, while the larch forests are expected to play a key role in the global carbon balance due to their wide distribution over North-East Eurasia. The authors reported results of eddy covariance CO2 flux measurements at a mature Gmelin larch stand in Central Siberia, Russia (64 degrees 16'N, 100 degrees 12'E, 250m a.s.l.). The measurements were conducted during one growing season (June-early September in 2004). CO2 uptake was initiated in early June and increased sharply until late June, which was closely related to the phenology of the larch trees (i.e., bud-break and needle flush). Maximum half-hourly net CO2 uptake was similar to 6 mu mol m(-2) s(-1). Maximum daily net uptake of similar to 2 g C m(-2) day(-1) occurred at the end of June and in mid-July. Cumulative net uptake was 76-78 g C m(-2), indicating that the mature larch forest acted as a net sink for CO2 during the growing season (91 days). In comparison with other boreal forests, however, the magnitude of net CO2 uptake and night-time release of the forest, and cumulative net CO2 uptake were lower. We suggest that lower net ecosystem CO2 uptake of the study stand was primarily associated with low leaf area index.

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Держатели документа:
[Nakai, Y.] Forestry & Forest Prod Res Inst, Dept Meteorol Environm, Tsukuba, Ibaraki 3058687, Japan
[Kajimoto, T.] Forestry & Forest Prod Res Inst, Kyushu Res Ctr, Kumamoto, Japan
[Abaimov, A. P.
Zyryanova, O. A.] Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk, Russia
[Yamamoto, S.] Okayama Univ, Okayama, Japan

Доп.точки доступа:
Nakai, Y...; Matsuura, Y...; Kajimoto, T...; Abaimov, A.P.; Абаимов Анатолий Платонович; Yamamoto, S...; Zyryanova, O.A.

[Text] / K. J. Ranson [et al.] // Can. J. Remote Sens. - 2003. - Vol. 29, Is. 2. - P271-285. - Cited References: 32 . - 15. - ISSN 0703-8992РУБ Remote Sensing

Аннотация: As part of a Siberian mapping project supported by the National Aeronautics and Space Administration (NASA), this study evaluated the capabilities of radars flown on the European Remote Sensing Satellite (ERS), Japanese Earth Resources Satellite (JERS), and Radarsat spacecraft and an optical sensor enhanced thematic mapper plus (ETM+) on-board Landsat-7 to detect fire scars, logging, and insect damage in the boreal forest. Using images from each sensor individually and combined, an assessment of the utility of using these sensors was developed. Transformed divergence analysis revealed that Landsat ETM+ images were the single best data type for this purpose. However, the combined use of the three radar and optical sensors did improve the results of discriminating these disturbances.

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Держатели документа:
NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
Sci Syst & Applicat Inc, Lanham, MD 20706 USA
Univ Maryland, Dept Geog, College Pk, MD 20742 USA
VN Sukachev Inst Forest, Krasnoyarsk, Russia

Доп.точки доступа:
Ranson, K.J.; Kovacs, K...; Sun, G...; Kharuk, V.I.

[Text] / N. M. Tchebakova, T. A. Blyakharchuk, E. I. Parfenova // Environ. Res. Lett. - 2009. - Vol. 4, Is. 4. - Ст. 45025, DOI 10.1088/1748-9326/4/4/045025. - Cited References: 72. - This study was supported by the Russian Foundation for Basic Research (Grant 06-05-65127). The authors are grateful to Jane Bradford, Gerald Rehfeldt and Robert Monserud for helpful review comments. The authors greatly appreciate the comments of two reviewers which significantly improved the manuscript. . - 11. - ISSN 1748-9326РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: Two quantitative methods were used to reconstruct paleoenvironments and vegetation in the Altai-Sayan mountains, Central Asia, during the Holocene. The 'biomization' method of Prentice et al (1996 Clim. Dyn. 12 185-96), applied to the surface pollen record, worked fairly well in the reconstructions of current vegetation. Applying this method to fossil pollen data, we reconstructed site paleovegetation. Our montane bioclimatic model, MontBioCliM, was used inversely to convert site paleovegetation into site paleoclimates. The differences between site paleo and current climates served as past climate change scenarios. The climatic anomalies for 2020, 2050, and 2080 derived from HadCM3 A1FI and B1 of the Hadley Centre, UK, served as climate change scenarios in the 21st century. MontBioCliM was applied directly to all climate scenarios through the Holocene to map past and future mountain vegetation over the Altai-Sayan mountains. Our results suggest that the early Holocene ca 10 000 BP was cold and dry; the period between 8000 and 5300 BP was warm and moist; and the time slice ca 3200 BP was cooler and drier than the present. Using kappa statistics, we showed that the vegetation at 8000 BP and 5300 BP was similar, as was the vegetation at 10 000 BP and 3200 BP, while future vegetation was predicted to be dissimilar to any of the paleovegetation reconstructions. The mid-Holocene is frequently hypothesized to be an analog of future climate warming; however, being known as warm and moist in Siberia, the mid-Holocene climate would likely impact terrestrial ecosystems differently from the projected warm and dry mid-century climate.

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Держатели документа:
[Tchebakova, N. M.
Parfenova, E. I.] Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forests, Krasnoyarsk 660036, Russia
[Blyakharchuk, T. A.] Russian Acad Sci, Siberian Branch, Inst Monitoring Climat & Ecol Syst, Tomsk 643055, Russia

Доп.точки доступа:
Tchebakova, N.M.; Blyakharchuk, T.A.; Parfenova, E.I.; Russian Foundation for Basic Research [06-05-65127]

/ L. Mukhortova, D. Schepaschenko, E. Moltchanova [et al.] // Sci. Total Environ. - 2021. - Vol. 785. - Ст. 147314, DOI 10.1016/j.scitotenv.2021.147314. - Cited References:117. - The authors gratefully acknowledge financial support from the Scholarship Council of the Scholarship Foundation of the Republic of Austria and the Austrian Agency for International Cooperation in Education and Research (OeAD-GmbH), Centre for International Cooperation & Mobility (ICM), whichwas granted to LiudmilaMukhortova (ZI: ICM2010-00915). This research was partially supported by State Assignment of Sukachev Institute of Forest SB RAS "Natural and anthropogenic dynamics of boreal forests in Central Siberia under the changing climate" (. 0287-2021-0008) and by the project "Delivering Incentives to End Deforestation: Global Ambition, Private/Public Finance and ZeroDeforestation Supply Chains" funded by the Norwegian Agency for Development Cooperation under agreement number QZA-0464, QZA-16/0218. The Russian Science Foundation supported processing of the plot data (project no. 19-77-30015). Training data collection for European Russia were supported by state assignment No.:..-.18118052590019-7. . - ISSN 0048-9697. - ISSN 1879-1026РУБ Environmental Sciences

Аннотация: Soil respiration is one of the major ecosystem carbon fluxes and has a strong relationship with climate. We quantified this dependence for the Russian territory based on coupling climate data and in-situ soil respiration (Rs) measurements compiled into a database from the literature using regression and random forest models. The analysis showed that soil properties are a strong factor that mediates the climate effect on Rs. The vegetation class determines the contribution of the autotrophic respiration to the total Rs flux. The heterotrophic soil respiration efflux of Russia was estimated to be 3.2 Pg C yr(-1) or 190 g C m(-2) yr(-1), which is 9-20% higher than most previously reported estimates. According to our modeling, heterotrophic soil respiration is expected to rise by 12% on average by 2050 according to the RCP2.6 climate scenario and at 10% based on RCP6. The total for Russia may reach 3.5 Pg C yr(-1) by 2050. By the end of the century heterotrophic respiration may reach 3.6 Pg C yr(-1) (+13%) and 4.3 Pg C yr(-1) (+34%) based on RCP2.6 and RCP6, respectively. In order to understand to what extent the lack of information on disturbances impact contributes to uncertainty of our model, we analyzed a few available publications and expert estimates. Taking into account the specifics of Russian forest management and regional disturbance regimes, we have found that for the entire territory of Russia, the disturbances are responsible for an increase in heterotrophic soil respiration by less than 2%. (C) 2021 The Authors. Published by Elsevier B.V.

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Держатели документа:
Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Akademgorodok 50,28, Krasnoyarsk 660036, Russia.
Int Inst Appl Syst Anal, A-2361 Laxenburg, Austria.
Russian Acad Sci, Ctr Forest Ecol & Prod, Profsoyuznaya 84-32-14, Moscow 117997, Russia.
Univ Canterbury, Christchurch 8041, New Zealand.

Доп.точки доступа:
Mukhortova, Liudmila; Schepaschenko, Dmitry; Moltchanova, Elena; Shvidenko, Anatoly; Khabarov, Nikolay; See, Linda; Scholarship Council of the Scholarship Foundation of the Republic of Austria; Austrian Agency for International Cooperation in Education and Research (OeAD-GmbH), Centre for International Cooperation Mobility (ICM) [ZI: ICM2010-00915]; State Assignment of Sukachev Institute of Forest SB RAS "Natural and anthropogenic dynamics of boreal forests in Central Siberia under the changing climate" [0287-2021-0008]; project "Delivering Incentives to End Deforestation: Global Ambition, Private/Public Finance and ZeroDeforestation Supply Chains" - Norwegian Agency for Development Cooperation [QZA-0464, QZA-16/0218]; Russian Science FoundationRussian Science Foundation (RSF) [19-77-30015]; [AAAA-A18-18118052590019-7]