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

: материалы временных коллективов / V. I. Kharuk, K. Ranson, M. Dvinskaya // Eurasian Journal of Forest Research. - 2007. - Vol. 10-2. - С. 163-171. - Библиогр. в конце ст.
Аннотация: Models of climate warming predict the migration of "warm-adapted' species to habitates of "cold-adapted" species. Here we show evidence of expansion of "dark-needle" conifers (DNC: Siberian pine, spruce and fir) into the habitat of larch, the leader in adaptation to harsh climatic conditions in Asia. The studies were made along two transects oriented from the western and southern borders of a larch dominated forest to its center. The invasion of DNC into the historical larch habitat was quantified as an increase of the proportion of those species both in the overstory and in regeneration. The age structure of regeneration showed that regeneration occurred mainly during the last 2-3 decades. In particular warm winter temperatures promote the survival regenerated Siberian pine. The results obtained indicate the climate-driven migration of Siberian pine, spruce and fir into traditional zone of larch dominance. Substitution of a deciduous conifer (larch) by evergreen conifers decreases the albedo and may provide positive feedback for temperature increases.

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Институт леса им. В.Н. Сукачева Сибирского отделения Российской академии наук : 660036, Красноярск, Академгородок, 50, стр., 28

Доп.точки доступа:
Ranson, K.J.; Рэнсон К.Дж.; Dvinskaya, Mariya Leonidovna; Двинская, Мария Леонидовна; Харук, Вячеслав Иванович
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[Text] / H. . Flessa [et al.] // Glob. Change Biol. - 2008. - Vol. 14, Is. 9. - P2040-2056, DOI 10.1111/j.1365-2486.2008.01633.x. - Cited References: 68 . - 17. - ISSN 1354-1013РУБ Biodiversity Conservation + Ecology + Environmental Sciences

Аннотация: Terrestrial ecosystems in northern high latitudes exchange large amounts of methane (CH4) with the atmosphere. Climate warming could have a great impact on CH4 exchange, in particular in regions where degradation of permafrost is induced. In order to improve the understanding of the present and future methane dynamics in permafrost regions, we studied CH4 fluxes of typical landscape structures in a small catchment in the forest tundra ecotone in northern Siberia. Gas fluxes were measured using a closed-chamber technique from August to November 2003 and from August 2006 to July 2007 on tree-covered mineral soils with and without permafrost, on a frozen bog plateau, and on a thermokarst pond. For areal integration of the CH4 fluxes, we combined field observations and classification of functional landscape structures based on a high-resolution Quickbird satellite image. All mineral soils were net sinks of atmospheric CH4. The magnitude of annual CH4 uptake was higher for soils without permafrost (1.19 kg CH4 ha(-1) yr(-1)) than for soils with permafrost (0.37 kg CH4 ha(-1) yr(-1)). In well-drained soils, significant CH4 uptake occurred even after the onset of ground frost. Bog plateaux, which stored large amounts of frozen organic carbon, were also a net sink of atmospheric CH4 (0.38 kg CH4 ha(-1) yr(-1)). Thermokarst ponds, which developed from permafrost collapse in bog plateaux, were hot spots of CH4 emission (approximately 200 kg CH4 ha(-1) yr(-1)). Despite the low area coverage of thermokarst ponds (only 2.1% of the total catchment area), emissions from these sites resulted in a mean catchment CH4 emission of 3.8 kg CH4 ha(-1) yr(-1). Export of dissolved CH4 with stream water was insignificant. The results suggest that mineral soils and bog plateaux in this region will respond differently to increasing temperatures and associated permafrost degradation. Net uptake of atmospheric CH4 in mineral soils is expected to gradually increase with increasing active layer depth and soil drainage. Changes in bog plateaux will probably be much more rapid and drastic. Permafrost collapse in frozen bog plateaux would result in high CH4 emissions that act as positive feedback to climate warming.

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[Flessa, Heiner] Univ Gottingen, Buesgen Inst, D-37077 Gottingen, Germany
[Rodionov, Andrej] Univ Cottbus, Chair Soil Protect & Recultivat, D-03046 Cottbus, Germany
[Rodionov, Andrej
Guggenberger, Georg] Univ Halle Wittenberg, Inst Agr & Nutr Sci, D-06108 Halle, Germany
[Fuchs, Hans
Magdon, Paul] Univ Gottingen, Inst Forest Management, D-37077 Gottingen, Germany
[Shibistova, Olga
Zrazhevskaya, Galina
Mikheyeva, Natalia] SB RAS, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia
[Kasansky, Oleg A.] SB RAS, Permafrost Inst Yakutsk, Field Stn Igarka, Igarka 663200, Russia
[Blodau, Christian] Univ Bayreuth, Dept Hydrol, D-95440 Bayreuth, Germany

Доп.точки доступа:
Flessa, H...; Rodionov, A...; Guggenberger, G...; Fuchs, H...; Magdon, P...; Shibistova, O...; Zrazhevskaya, G...; Mikheyeva, N...; Kasansky, O.A.; Blodau, C...

[Текст] / A. S. Isaev, V. G. Soukhovolsky, T. M. Ovchinnikova // Zhurnal Obshchei Biol. - 2008. - Vol. 69, Is. 1. - С. 3-9. - Cited References: 22 . - 7. - ISSN 0044-4596РУБ Biology

Аннотация: Phenomenological models of the forest plantations growth are analyzed. Those derived from the Verhulst's model are shown to fail describing qualitative effects reflecting tree growth, phytomass withdrawals, and plantation restoration. The method of phase portraits is used for exploration of the forest ecosystem dynamics, which allows to describe regulatory mechanisms of the growth processes, regulation delay, and feedback types. A bistable phenomenological model is suggested herewith to characterize dynamic processes in the forest ecosystems. Principal patterns of formation of the forest plantations at different stages of the forest generation processes are considered on the basis of that model, and ecological effects responsible for the plantation dynamics are revealed.

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Держатели документа:
[Isaev, A. S.] RAS, Ctr Forest Ecol & Prod, Moscow 119997, Russia
[Soukhovolsky, V. G.
Ovchinnikova, T. M.] SB RAS, Sukachevs Forest Inst, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Isaev, A.S.; Soukhovolsky, V.G.; Ovchinnikova, T.M.

/ N. M. Tchebakova [et al.] // Biol. Bull. - 2015. - Vol. 42, Is. 6. - P579-588, DOI 10.1134/S1062359015660024 . - ISSN 1062-3590
Аннотация: Direct measurements of CO2 fluxes by the eddy covariance method have demonstrated that the examined middle-taiga pine forest, raised bog, true steppe, and southern tundra along the Yenisei meridian (~90° E) are carbon sinks of different capacities according to annual output. The tundra acts as a carbon sink starting from June; forest and bog, from May; and steppe, from the end of April. In transitional seasons and winter, the ecosystems are a weak source of carbon; this commences from September in the tundra, from October in the forest and bog, and from November in the steppe. The photosynthetic productivity of forest and steppe ecosystems, amounting to 480–530 g C/(m2 year), exceeds by 2–2.5 times that of bogs and tundras, 200–220 g C/(m2 year). The relationships between the heat balance structure and CO2 exchange are shown. Possible feedback of carbon exchange between the ecosystems and atmosphere as a result of climate warming in the region are assessed. © 2015, Pleiades Publishing, Inc.

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Держатели документа:
Sukachev Institute of Forestry, Siberian Branch, Russian Academy of Sciences, Akademgorodok 50/28, Krasnoyarsk, Russian Federation
Siberian Federal University, Svobodnyi pr. 79, Krasnoyarsk, Russian Federation
Sventokshistkaya Academy, Institute of Geography, Jan Kochanowski University, ul. Sweintokrzyska 15, Kielce, Poland
Department of Earth and Ecosystem Science, Lund University, Solvegatan 12, Lund, Sweden
Department of Forest Resources and Environment, Tuscia University, Via del San Camillo de Lellis, Viterbo, Italy
Max Planck Institute for Biogeochemistry, Hans Knoll str. 10, Jena, Germany
Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Leninskii pr. 33, Moscow, Russian Federation

Доп.точки доступа:
Tchebakova, N. M.; Vygodskaya, N. N.; Arneth, A.; Marchesini, L. B.; Kurbatova, Y. A.; Parfenova, E. I.; Valentini, R.; Verkhovets, S. V.; Vaganov, E. A.; Schulze, E.-D.

/ M. Saurer [et al.] // New Phytol. - 2016. - Vol. 209, Is. 3. - P955-964, DOI 10.1111/nph.13759 . - ISSN 0028-646X
Аннотация: Stable oxygen isotope ratios (δ18O) in trees from high latitude ecosystems are valuable sources of information for recent and past environmental changes, but the interpretation is hampered by the complex hydrology of forests growing under permafrost conditions, where only a shallow layer of soil thaws in summer. We investigated larch trees (Larix gmelinii) at two sites with contrasting soil conditions in Siberia and determined δ18O of water from different soil depths, roots, twigs, and needles as well as δ18O of soluble carbohydrates regularly over two growing seasons. A comparison of results from the 2 yrs revealed an unexpected 'inverse' climate-isotope relationship, as dry and warm summer conditions resulted in lower soil and root δ18O values. This was due to a stronger uptake of isotopically depleted water pools originating from melted permafrost or previous winter snow. We developed a conceptual framework that considers the dependence of soil water profiles on climatic conditions for explaining δ18O in needle water, needle soluble carbohydrates and stem cellulose. The negative feedback of drought conditions on the source isotope value could explain decreasing tree-ring δ18O trends in a warming climate and is likely relevant in many ecosystems, where a soil isotope gradient with depth is observed. © 2016 New Phytologist Trust.

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Держатели документа:
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
V.N. Sukachev Institute of Forest, Siberian Branch of the Russian Academy of Sciences, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Saurer, M.; Kirdyanov, A. V.; Prokushkin, A. S.; Rinne, K. T.; Siegwolf, R. T.W.

[Text] / J. Boy [et al.] // Rev. Chil. Hist. Nat. - 2016. - Vol. 89. - Ст. 6, DOI 10.1186/s40693-016-0056-8. - Cited References:53. - We cordially thank the Instituto Antarctico Chileno (INACH-T 28-11) and the Deutsche Forschungsgemeinschaft (DFG, BO 3741-2-1, in the framework of the priority programme SPP 1158 Antarctic Research with comparative investigations in Arctic ice areas) for supporting this research and acknowledge the assistance of the staff at the Prof. Julio Escudero Station at Fildes. We are also grateful to Roger Michael Klatt, Pieter Wiese, Leopold Sauheitl, Joanna Weiss, Norman Gentsch and Christian Weiss for their support with this work. Special Acknwoledgements to Y. Villagra and F. Osorio for the identification of Lichens and Bryophytes species, respectively. We especially thank the reviewers for their appreciated input to the manuscript. . - ISSN 0716-078X. - ISSN 0717-6317РУБ Biodiversity Conservation + Ecology

Аннотация: Background: Maritime Antarctica is severely affected by climate change and accelerating glacier retreat forming temporal gradients of soil development. Successional patterns of soil development and plant succession in the region are largely unknown, as are the feedback mechanisms between both processes. Here we identify three temporal gradients representing horizontal and vertical glacier retreat, as well as formation of raised beaches due to isostatic uplift, and describe soil formation and plant succession along them. Our hypotheses are (i) plants in Antarctica are able to modulate the two base parameters in soil development, organic C content and pH, along the temporal gradients, leading to an increase in organic carbon and soil acidity at relatively short time scales, (ii) the soil development induces succession along these gradients, and (iii) with increasing soil development, bryophytes and Deschampsia antarctica develop mycorrhiza in maritime Antarctica in order to foster interaction with soil. Results: All temporal gradients showed soil development leading to differentiation of soil horizons, carbon accumulation and increasing pH with age. Photoautptroph succession occurred rapidly after glacier retreat, but occurrences of mosses and lichens interacting with soils by rhizoids or rhizines were only observed in the later stages. The community of ground dwelling mosses and lichens is the climax community of soil succession, as the Antarctic hairgrass D. antarctica was restricted to ornithic soils. Neither D. antarctica nor mosses at the best developed soils showed any sign of mycorrhization. Conclusion: Temporal gradients formed by glacier retreat can be identified in maritime Antarctic, where soil development and plant succession of a remarkable pace can be observed, although pseudo-succession occurs by fertilization gradients caused by bird feces. Thus, the majority of ice-free surface in Antarctica is colonized by plant communities which interact with soil by litter input rather than by direct transfer of photoassimilates to soil.

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Leibniz Univ Hannover, Inst Soil Sci, Herrenhauser Str 2, D-30419 Hannover, Germany.
Univ Austral Chile, Inst Ciencias Ambientales & Evolut, Valdivia, Chile.
Univ Stirling, Biol & Environm Sci, Stirling FK9 4LA, Scotland.
Univ Halle Wittenberg, Inst Soil Sci, D-06108 Halle, Germany.
VN Sukachev Inst Forest, Krasnoyarsk, Russia.

Доп.точки доступа:
Boy, Jens; Godoy, Roberto; Shibistova, Olga; Boy, Diana; McCulloch, Robert; de la Fuente, Alberto Andrino; Morales, Mauricio Aguirre; Mikutta, Robert; Guggenberger, Georg; Instituto Antarctico Chileno [INACH-T 28-11]; Deutsche Forschungsgemeinschaft (DFG) [BO 3741-2-1]; [SPP 1158]

[Text] / B. Wild [et al.] // Sci Rep. - 2016. - Vol. 6. - Ст. 25607, DOI 10.1038/srep25607. - Cited References:52. - This study is part of the CryoCARB project (Long-term Carbon Storage in Cryoturbated Arctic Soils), and co-funded by the Austrian Science Fund (FWF): I370-B17, the German Federal Ministry of Education and Research (03F0616A), the Czech Ministry of Education, Youth and Sports (MSM 7E10073 - CryoCARB), the Russian Ministry of Education and Science (No. 14.25.31.0031), the Swedish Research Council (824-2009-77357), and the Norwegian Research Fund (NFR): NFR-200411. . - ISSN 2045-2322РУБ Multidisciplinary Sciences

Аннотация: Arctic ecosystems are warming rapidly, which is expected to promote soil organic matter (SOM) decomposition. In addition to the direct warming effect, decomposition can also be indirectly stimulated via increased plant productivity and plant-soil C allocation, and this so called "priming effect" might significantly alter the ecosystem C balance. In this study, we provide first mechanistic insights into the susceptibility of SOM decomposition in arctic permafrost soils to priming. By comparing 119 soils from four locations across the Siberian Arctic that cover all horizons of active layer and upper permafrost, we found that an increased availability of plant-derived organic C particularly stimulated decomposition in subsoil horizons where most of the arctic soil carbon is located. Considering the 1,035 Pg of arctic soil carbon, such an additional stimulation of decomposition beyond the direct temperature effect can accelerate net ecosystem C losses, and amplify the positive feedback to global warming.

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Univ Vienna, Dept Microbiol & Ecosyst Sci, Vienna, Austria.
Austrian Polar Res Inst, Vienna, Austria.
Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden.
Leibniz Univ Hannover, Inst Soil Sci, D-30167 Hannover, Germany.
Univ South Bohemia, Dept Ecosyst Biol, Ceske Budejovice, Czech Republic.
Univ Vienna, Dept Ecogen & Syst Biol, Vienna, Austria.
Univ Bergen, Dept Biol, Ctr Geobiol, Bergen, Norway.
Ctr Geomicrobiol, Dept Biosci, Aarhus, Denmark.
Stockholm Univ, Dept Phys Geog, S-10691 Stockholm, Sweden.
Russian Acad Sci, Siberian Branch, Cent Siberian Bot Garden, Novosibirsk, Russia.
Univ Halle Wittenberg, Soil Sci & Soil Protect, D-06108 Halle, Saale, Germany.
Univ New Hampshire, Dept Nat Resources & Environm, Durham, NH 03824 USA.
Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk, Russia.
Univ Lancaster, Lancaster Environm Ctr, Lancaster, England.
Ernst Moritz Arndt Univ Greifswald, Inst Microbiol, Greifswald, Germany.

Доп.точки доступа:
Wild, Birgit; Gentsch, Norman; Capek, Petr; Diakova, Katerina; Alves, Ricardo J. Eloy; Barta, Jiri; Gittel, Antje; Hugelius, Gustaf; Knoltsch, Anna; Kuhry, Peter; Lashchinskiy, Nikolay; Mikutta, Robert; Palmtag, Juri; Schleper, Christa; Schnecker, Joerg; Shibistova, Olga; Takriti, Mounir; Torsvik, Vigdis L.; Urich, Tim; Watzka, Margarete; Santruckova, Hana; Guggenberger, Georg; Richter, Andreas; CryoCARB project (Long-term Carbon Storage in Cryoturbated Arctic Soils); Austrian Science Fund (FWF) [I370-B17]; German Federal Ministry of Education and Research [03F0616A]; Czech Ministry of Education, Youth and Sports (MSM) [7E10073]; Russian Ministry of Education and Science [14.25.31.0031]; Swedish Research Council [824-2009-77357]; Norwegian Research Fund (NFR) [NFR-200411]

[Text] / S. Tautenhahn [et al.] // Glob. Change Biol. - 2016. - Vol. 22, Is. 6. - P2178-2197, DOI 10.1111/gcb.13181. - Cited References:94. - We thank Danilo Mollicone, Marina Bryukhanova, Alexey Panov, and Sergey Verkhovets for their help preparing the expeditions. This work would not have been possible without the hard work in the field of Jan Hertwig, Waldemar Ziegler, Ulrich Pruschitzki, Norman Gentsch, Luisa Hiese, Surgery Titov, Vladimir Kislitsyn, Kolya Savaronsky, and Roman Bachman. Henrik Hartmann, Angela Gunther, and Corinna Hohl assisted with dendrochronological analysis. Miguel Mahecha, Jannis van Buttlar, and Ulrich Weber helped with R and the artwork. Corinna Buendia gave helpful comments on a early stage of the manuscript. We thank three anonymous reviewers for their valuable input. The project was funded by the Max Planck Society. Anatoly Prokushkin was supported by the RSF grant 14-24-00113. . - ISSN 1354-1013. - ISSN 1365-2486РУБ Biodiversity Conservation + Ecology + Environmental Sciences

Аннотация: Fire is a primary driver of boreal forest dynamics. Intensifying fire regimes due to climate change may cause a shift in boreal forest composition toward reduced dominance of conifers and greater abundance of deciduous hardwoods, with potential biogeochemical and biophysical feedbacks to regional and global climate. This shift has already been observed in some North American boreal forests and has been attributed to changes in site conditions. However, it is unknown if the mechanisms controlling fire-induced changes in deciduous hardwood cover are similar among different boreal forests, which differ in the ecological traits of the dominant tree species. To better understand the consequences of intensifying fire regimes in boreal forests, we studied postfire regeneration in five burns in the Central Siberian dark taiga, a vast but poorly studied boreal region. We combined field measurements, dendrochronological analysis, and seed-source maps derived from high-resolution satellite images to quantify the importance of site conditions (e.g., organic layer depth) vs. seed availability in shaping postfire regeneration. We show that dispersal limitation of evergreen conifers was the main factor determining postfire regeneration composition and density. Site conditions had significant but weaker effects. We used information on postfire regeneration to develop a classification scheme for successional pathways, representing the dominance of deciduous hardwoods vs. evergreen conifers at different successional stages. We estimated the spatial distribution of different successional pathways under alternative fire regime scenarios. Under intensified fire regimes, dispersal limitation of evergreen conifers is predicted to become more severe, primarily due to reduced abundance of surviving seed sources within burned areas. Increased dispersal limitation of evergreen conifers, in turn, is predicted to increase the prevalence of successional pathways dominated by deciduous hardwoods. The likely fire-induced shift toward greater deciduous hardwood cover may affect climate-vegetation feedbacks via surface albedo, Bowen ratio, and carbon cycling.

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Max Planck Inst Biogeochem, Hans Knoll Str 10, D-07745 Jena, Germany.
Tech Univ Bergakad Freiberg, Dept Biosci, Leipziger Str 29, D-09596 Freiberg, Germany.
Univ Florida, Dept Biol, Gainesville, FL 32611 USA.
German Ctr Integrat Biodivers Res iDiv, Deutsch Pl 5e, D-04103 Leipzig, Germany.
Univ Florida, Sch Forest Resources & Conservat, Gainesville, FL 32611 USA.
Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Akademgorodok 50-28, Krasnoyarsk 660036, Russia.
Univ Leipzig, Johannisallee 21-23, D-04103 Leipzig, Germany.

Доп.точки доступа:
Tautenhahn, Susanne; Lichstein, Jeremy W.; Jung, Martin; Kattge, Jens; Bohlman, Stephanie A.; Heilmeier, Hermann; Prokushkin, Anatoly; Kahl, Anja; Wirth, Christian; Max Planck Society; RSF [14-24-00113]

/ A. A. Knorre [et al.] // Sci. Total Environ. - 2019. - Vol. 652. - P314-319, DOI 10.1016/j.scitotenv.2018.10.124 . - ISSN 0048-9697
Аннотация: Although it has been recognized that rising temperatures and shifts in the hydrological cycle affect the depth of the seasonally thawing upper permafrost stratum, it remains unclear to what extent the frequency and intensity of wildfires, and subsequent changes in vegetation cover, influence the soil active layer on different spatiotemporal scales. Here, we use ring width measurements of the subterranean stem part of 15 larch trees from a Sphagnum bog site in Central Siberia to reconstruct long-term changes in the thickness of the active layer since the last wildfire occurred in 1899. Our approach reveals a three-step feedback loop between above- and belowground ecosystem components. After all vegetation is burned, direct atmospheric heat penetration over the first ~20 years caused thawing of the upper permafrost stratum. The slow recovery of the insulating ground vegetation reverses the process and initiates a gradual decrease of the active layer thickness. Due to the continuous spreading and thickening of the peat layer during the last decades, the upper permafrost horizon has increased by 0.52 cm/year. This study demonstrates the strength of annually resolved and absolutely dated tree-ring series to reconstruct the effects of historical wildfires on the functioning and productivity of boreal forest ecosystems at multi-decadal to centennial time-scale. In so doing, we show how complex interactions of above- and belowground components translate into successive changes in the active permafrost stratum. Our results are particularly relevant for improving long-term estimates of the global carbon cycle that strongly depends on the source and sink behavior of the boreal forest zone. © 2018

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Institute of Ecology and Geography, Siberian Federal University, Krasnoyarsk, 660041, Russian Federation
State Natural Reserve ‘Stolby’, Kar'ernaya 26A, Krasnoyarsk, 660006, Russian Federation
Department of Geography, University of CambridgeCB2 3EN, United Kingdom
Sukachev Institute of Forest SB RAS, Akademgorodok, Krasnoyarsk, 660036, Russian Federation
Global Change Research Institute CAS, Brno, 603 00, Czech Republic
Swiss Federal Research Institute WSL, Birmensdorf, CH-8903, Switzerland
Department of Geography, Masaryk University, Kotlarska 261137, Czech Republic

Доп.точки доступа:
Knorre, A. A.; Kirdyanov, A. V.; Prokushkin, A. S.; Krusic, P. J.; Buntgen, U.

/ P. Groisman [et al.] // Environ. Res. Lett. - 2018. - Vol. 13, Is. 11. - Ст. 115008, DOI 10.1088/1748-9326/aae43c. - Cited References:92. - PG and GH were supported in part by NASA grant NNX15AP81G. NT acknowledges the Russian Foundation for Basic Research grant 16-05-00496. OZ, AD, and PG were partially supported through 'ARCTIC-ERA: ARCTIC climate change and its impact on environment, infrastructures, and resource availability' sponsored by ANR (France), RFBR (Russia), and US NSF (grants 1717770 and 1558389). YC was supported by National Youth Science Fund of China grant 41701227 and by the Priority Academic Program Development of Jiangsu Higher Education Institutions in China. The work of AS was partially supported by US NSF grant 1602879 and Russian RFFI grant 18-05-60240. Grant 14.B25.31.0026 of the Ministry of Education and Science of the Russian Federation provided support to PG, NT, AS, OB, and OZ for their work conducted at the P P Shirshov Institute of Oceanology. Support for the work of IY and IK was provided by grant AP05135848 of the Ministry of Education and Sciences of the Republic of Kazakhstan. JC and RJ were supported by the Dynamics of Coupled Natural and Human Systems (CNH) Program of the NSF (grant 1313761) and the LCLUC program of NASA (grant NNX14AD85G). Grant 1717770 by the US National Science Foundation to George Washington University provided support to PG for his work at the Hydrology Science and Services Corporation via Sub-Recipient Agreement Number 17-S03R. The synthesis workshop (Ulaanbaatar, 2-5 June 2017) was partially sponsored by the 'Dynamics of Coupled Natural and Human Systems' program of the NSF (grant 1313761) and the LCLUC program of NASA (grant NNX15AD10G). . - ISSN 1748-9326РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: The dryland belt (DLB) in Northern Eurasia is the largest contiguous dryland on Earth. During the last century, changes here have included land use change (e.g. expansion of croplands and cities), resource extraction (e.g. coal, ores, oil, and gas), rapid institutional shifts (e.g. collapse of the Soviet Union), climatic changes, and natural disturbances (e.g. wildfires, floods, and dust storms). These factors intertwine, overlap, and sometimes mitigate, but can sometimes feedback upon each other to exacerbate their synergistic and cumulative effects. Thus, it is important to properly document each of these external and internal factors and to characterize the structural relationships among them in order to develop better approaches to alleviating negative consequences of these regional environmental changes. This paper addresses the climatic changes observed over the DLB in recent decades and outlines possible links of these changes (both impacts and feedback) with other external and internal factors of contemporary regional environmental changes and human activities within the DLB.

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North Carolina State Univ, NOAA, Ctr Environm Informat, Asheville, NC 28804 USA.
RAS, PP Shirshov Inst Oceanol, Moscow, Russia.
Hydrol Sci & Serv Corp, Asheville, NC 28801 USA.
Russian Inst Hydrometeorol Informat, Obninsk, Kaluga Area, Russia.
Michigan State Univ, E Lansing, MI 48824 USA.
State Hydrol Inst, St Petersburg, Russia.
Univ New Hampshire, Earth Syst Res Ctr, Durham, NH 03824 USA.
Nanjing Forestry Univ, Coll Biol & Environm, Joint Innovat Ctr Modern Forestry Studies, Nanjing, Jiangsu, Peoples R China.
SB RAS, Krasnoyarsk Fed Res Ctr, Sukachev Inst Forest, Krasnoyarsk, Russia.
Joseph Fourier Univ, Lab Glaciol & Geophys Environm, Grenoble, France.
Oklahoma State Univ, Stillwater, OK 74078 USA.
Univ Sopron, Sopron, Hungary.
Minist Energy Republ Kazakhstan, Joint Stock Co Zhasyl Damu, Alma Ata, Kazakhstan.
Natl Ctr Space Res & Technol, Alma Ata, Kazakhstan.

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Groisman, Pavel; Bulygina, Olga; Henebry, Geoffrey; Speranskaya, Nina; Shiklomanov, Alexander; Chen, Yizhao; Tchebakova, Nadezhda; Parfenova, Elena; Tilinina, Natalia; Zolina, Olga; Dufour, Ambroise; Chen, Jiquan; John, Ranjeet; Fan, Peilei; Mayas, Csaba; Yesserkepova, Irina; Kaipov, Ildan; NASA [NNX15AP81G]; Russian Foundation for Basic Research grant [16-05-00496]; 'ARCTIC-ERA: ARCTIC climate change and its impact on environment, infrastructures, and resource availability' - ANR (France); RFBR (Russia); US NSF [1602879, 1717770, 1558389]; National Youth Science Fund of China [41701227]; Priority Academic Program Development of Jiangsu Higher Education Institutions in China; Russian RFFI [18-05-60240]; Ministry of Education and Science of the Russian Federation [14.B25.31.0026]; Ministry of Education and Sciences of the Republic of Kazakhstan [AP05135848]; Dynamics of Coupled Natural and Human Systems (CNH) Program of the NSF [1313761]; LCLUC program of NASA [NNX15AD10G, NNX14AD85G]; US National Science Foundation [1717770, 17-S03R]; 'Dynamics of Coupled Natural and Human Systems' program of the NSF [1313761]

/ B. S. Steidinger [et al.] // Nature. - 2019. - Vol. 569, Is. 7756. - P404-+, DOI 10.1038/s41586-019-1128-0. - Cited References:45 . - ISSN 0028-0836. - ISSN 1476-4687РУБ Multidisciplinary Sciences

Аннотация: The identity of the dominant root-associated microbial symbionts in a forest determines the ability of trees to access limiting nutrients from atmospheric or soil pools(1,2), sequester carbon(3,4) and withstand the effects of climate change(5,6). Characterizing the global distribution of these symbioses and identifying the factors that control this distribution are thus integral to understanding the present and future functioning of forest ecosystems. Here we generate a spatially explicit global map of the symbiotic status of forests, using a database of over 1.1 million forest inventory plots that collectively contain over 28,000 tree species. Our analyses indicate that climate variables-in particular, climatically controlled variation in the rate of decomposition-are the primary drivers of the global distribution of major symbioses. We estimate that ectomycorrhizal trees, which represent only 2% of all plant species(7), constitute approximately 60% of tree stems on Earth. Ectomycorrhizal symbiosis dominates forests in which seasonally cold and dry climates inhibit decomposition, and is the predominant form of symbiosis at high latitudes and elevation. By contrast, arbuscular mycorrhizal trees dominate in aseasonal, warm tropical forests, and occur with ectomycorrhizal trees in temperate biomes in which seasonally warm-and-wet climates enhance decomposition. Continental transitions between forests dominated by ectomycorrhizal or arbuscular mycorrhizal trees occur relatively abruptly along climate-driven decomposition gradients; these transitions are probably caused by positive feedback effects between plants and microorganisms. Symbiotic nitrogen fixers-which are insensitive to climatic controls on decomposition (compared with mycorrhizal fungi)-are most abundant in arid biomes with alkaline soils and high maximum temperatures. The climatically driven global symbiosis gradient that we document provides a spatially explicit quantitative understanding of microbial symbioses at the global scale, and demonstrates the critical role of microbial mutualisms in shaping the distribution of plant species.

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Stanford Univ, Dept Biol, Stanford, CA 94305 USA.
Swiss Fed Inst Technol, Dept Environm Syst Sci, Zurich, Switzerland.
Purdue Univ, Dept Forestry & Nat Resources, W Lafayette, IN 47907 USA.
Beijing Forestry Univ, Res Ctr Forest Management Engn, State Forestry & Grassland Adm, Beijing, Peoples R China.
Univ Oxford, Dept Zool, Oxford, England.
Univ Minnesota, Dept Forest Resources, St Paul, MN USA.
Western Sydney Univ, Hawkesbury Inst Environm, Penrith, NSW, Australia.
Wageningen Univ & Res, Wageningen, Netherlands.
Univ Lleida, Dept Crop & Forest Sci, Agrotecnio Ctr UdL Agrotecnio, Lleida, Spain.
Forest Sci & Technol Ctr Catalonia CTFC, Solsona, Spain.
UN, Food & Agr Org, Rome, Italy.
Univ Montpellier, Cirad, UPR Forets & Soc, Montpellier, France.
Natl Polytech Inst INP HB, Dept Forestry & Environm, Yamoussoukro, Cote Ivoire.
Swiss Fed Inst Forest Snow & Landscape Res, WSL, Birmensdorf, Switzerland.
Univ Felix Houphouet Boigny, UFR Biosci, Abidjan, Cote Ivoire.
Univ Udine, Dept Agr Food Environm & Anim Sci, Udine, Italy.
Natl Res Council CNR IBIMET, Inst Biometeorol, Florence, Italy.
Univ Florida, Dept Tourism Recreat & Sport Management, Spatial Ecol & Conservat Lab, Gainesville, FL USA.
UNAD, Fdn ConVida, Medellin, Colombia.
Field Museum Nat Hist, Chicago, IL 60605 USA.
Univ Calif Los Angeles, Ctr Trop Res, Inst Environm & Sustainabil, Los Angeles, CA USA.
Univ Gottingen, Silviculture & Forest Ecol Temperate Zones, Gottingen, Germany.
Norwegian Inst Bioecon Res NIBIO, Div Forest & Forest Resources, As, Norway.
Univ Autonoma Gabriel Rene Moreno, Museo Hist Nat Noel Kempff Mercado, Santa Cruz, Bolivia.
European Commiss, Joint Res Ctr, Ispra, Italy.
Herbario Univ PORT, UNELLEZ Guanare, Programa Ciencias Agro & Mar, Portuguesa, Venezuela.
Univ Leeds, Sch Geog, Leeds, W Yorkshire, England.
Forest Res Inst, Dept Geomat, Raszyn, Poland.
Nat Biodivers Ctr, Leiden, Netherlands.
Univ Fed Acre, Ctr Multidisciplinar, Rio Branco, Brazil.
Smithsonians Natl Zoo & Conservat Biol Inst, Washington, DC USA.
Mbarara Univ Sci & Technol, Inst Trop Forest Conservat, Mbarara, Uganda.
Univ Ghent, Isotope Biosci Lab ISOFYS, Ghent, Belgium.
Stefan Cel Mare Univ Suceava, Integrated Ctr Res Dev & Innovat Adv Mat Nanotech, Suceava, Romania.
Univ Sao Paulo, Luiz de Queiroz Coll Agr, Dept Forest Sci, Piracicaba, Brazil.
Bavarian State Inst Forestry, Freising Weihenstephan, Germany.
Manchester Metropolitan Univ, Manchester, Lancs, England.
Martin Luther Univ Halle Wittenberg, Inst Biol Geobot & Bot Garden, Halle, Germany.
German Ctr Integrat Biodivers Res iDiv, Leipzig, Germany.
Univ Firenze, Dept Agr Food Environm & Forest DAGRI, Florence, Italy.
Tomsk State Univ, Inst Biol, Tomsk, Russia.
Inst Forestry, Dept Spatial Regulat GIS & Forest Policy, Belgrade, Serbia.
Univ Connecticut, Dept Ecol & Evolutionary Biol, Storrs, CT USA.
Univ Sunshine Coast, Trop Forests & People Res Ctr, Maroochydore, Qld, Australia.
Lakehead Univ, Fac Nat Resources Management, Thunder Bay, ON, Canada.
Fujian Normal Univ, Minist Educ, Key Lab Humid Subtrop Ecogeog Proc, Fuzhou, Fujian, Peoples R China.
Swiss Fed Inst Technol, Inst Integrat Biol, Zurich, Switzerland.
IFER, Jilove, Czech Republic.
Global Change Res Inst CAS, Brno, Czech Republic.
Duke Univ, Nicholas Sch Environm, Durham, NC 27708 USA.
Univ Missouri, Dept Biol, 8001 Nat Bridge Rd, St Louis, MO 63121 USA.
Univ Estadual Campinas, Inst Biol, Dept Plant Biol, Campinas, SP, Brazil.
Smithsonian Trop Res Inst, Balboa, Panama.
Univ Cambridge, Dept Plant Sci, Cambridge, England.
Andes Amazon Biodivers Program, Madre De Dios, Peru.
Univ Juarez Estado Durango, Fac Ciencias Forestales, Durango, Mexico.
Coll St Rose, Dept Phys & Biol Sci, Albany, NY USA.
West Virginia Univ, Dept Biol, Morgantown, WV 26506 USA.
Concordia Univ, Dept Biol, Montreal, PQ, Canada.
Univ Reg Blumenau, Dept Nat Sci, Blumenau, Brazil.
Cirad, UMR EcoFoG, Kourou, French Guiana.
Univ Maryland, Dept Geol Sci, College Pk, MD 20742 USA.
Inst Forestry, Belgrade, Serbia.
Natl Inst Amazonian Res, Manaus, Amazonas, Brazil.
Herbier Natl Gabon CENAREST, IRET, Libreville, Gabon.
Univ Arizona, Dept Ecol & Evolutionary Biol, Tucson, AZ USA.
Santa Fe Inst, Santa Fe, NM 87501 USA.
Queensland Herbarium, Dept Environm & Sci, Toowong, Qld, Australia.
Univ Natl Agr, Ecole Foresterie & Ingn Bois, Ketou, Benin.
Czech Acad Sci, Inst Entomol, Biol Ctr, Ceske Budejovice, Czech Republic.
Univ Exeter, Coll Life & Environm Sci, Geog, Exeter, Devon, England.
Nat Resources Inst Finland Luke, Joensuu, Finland.
Univ Bern, Inst Plant Sci, Bern, Switzerland.
Forest Res Inst Malaysia, Kuala Lumpur, Malaysia.
Swedish Univ Agr Sci SLU, Dept Forest Resource Management, Umea, Sweden.
Fdn Edmund Mach, Dept Sustainable Agroecosyst & Bioresources, San Michele All Adige, Italy.
Yale Univ, Sch Forestry & Environm Studies, New Haven, CT 06511 USA.
Royal Bot Garden Edinburgh, Edinburgh, Midlothian, Scotland.
Univ Oxford, Dept Plant Sci, Oxford, England.
Univ Bayreuth, Dept Plant Systemat, Bayreuth, Germany.
Royal Soc Protect Birds, Ctr Conservat Sci, Sandy, Beds, England.
Inst Invest Amazonia Peruana, Iquitos, Peru.
Stellenbosch Univ, Dept Math Sci, Ctr Invas Biol, Stellenbosch, South Africa.
African Inst Math Sci, Theoret Ecol Unit, Cape Town, South Africa.
Korea Forest Promot Inst, Div Forest Resources Informat, Seoul, South Korea.
Inst Agron Neocaledonien IAC, Equipe Sol & Vegetat SolVeg, Noumea, New Caledonia.
Tokyo Univ Agr, Dept Forest Sci, Tokyo, Japan.
Polish Acad Sci, Inst Dendrol, Kornik, Poland.
Poznan Univ Life Sci, Dept Game Management & Forest Protect, Poznan, Poland.
Univ Warsaw, Bialowieza Geobot Stn, Fac Biol, Bialowieza, Poland.
Univ Copenhagen, Dept Geosci & Nat Resource Management, Copenhagen, Denmark.
CSIRO Land & Water, Ctr Environm & Life Sci, Floreat, WA, Australia.
Bauman Moscow State Tech Univ, Fac Forestry, Mytishchi, Russia.
Univ Ghent, Dept Environm, CAVElab Computat & Appl Vegetat Ecol, Ghent, Belgium.
Smithsonian Trop Res Inst, CTFS ForestGEO, Balboa, Panama.
Colorado Mesa Univ, Dept Phys & Environm Sci, Grand Junction, CO USA.
Univ South Australia, Sch Nat & Built Environm, Adelaide, SA, Australia.
Univ South Australia, Future Ind Inst, Adelaide, SA, Australia.
Dr Harisingh Gour Cent Univ, Dept Bot, Sagar, India.
Seoul Natl Univ, Dept Forest Sci, Seoul, South Korea.
Seoul Natl Univ, Interdisciplinary Program Agr & Forest Meteorol, Seoul, South Korea.
Natl Ctr Agro Meteorol, Seoul, South Korea.
Seoul Natl Univ, Res Inst Agr & Life Sci, Seoul, South Korea.
Kyoto Univ, Grad Sch Agr, Kyoto, Japan.
Univ Hamburg, Inst World Forestry, Hamburg, Germany.
Estonian Univ Life Sci, Inst Forestry & Rural Engn, Tartu, Estonia.
Int Inst Appl Syst Anal, Ecosyst Serv & Management, Laxenburg, Austria.
UCL, Dept Geog, London, England.
Qingdao Agr Univ, Fac Forestry, Qingdao, Shandong, Peoples R China.
Russian Acad Sci, Ctr Forest Ecol & Prod, Moscow, Russia.
Univ Oxford, Sch Geog, Oxford, England.
AgroParisTech, UMR EcoFoG, Kourou, France.
Univ Estado Mato Grosso, Dept Ciencias Biol, Nova Xavantina, Brazil.
Univ York, Dept Environm & Geog, York, N Yorkshire, England.
Coll African Wildlife Management, Dept Wildlife Management, Mweka, Tanzania.
Univ Nacl Autonoma Mexico, Fac Ciencias, Dept Ecol & Recursos Nat, Mexico City, DF, Mexico.
Univ Tolima, Ibague, Colombia.
Colegio Profes Forestales Cochabamba, Cochabamba, Bolivia.
Jardin Bot Missouri, Oxapampa, Peru.
Univ Nacl San Antonio Abad Cusco, Cuzco, Peru.
Independent Univ Bangladesh, Sch Environm Sci & Management, Dept Environm Management, Dhaka, Bangladesh.
Univ Juarez Estado Durango, Inst Silvicultura Ind Madera, Durango, Mexico.
Univ Estatal Amazon, Puyo, Pastaza, Ecuador.
Univ Zurich, Dept Evolutionary Biol & Environm Studies, Zurich, Switzerland.
Tecnol Costa Rica TEC, Sch Forestry, Cartago, Costa Rica.
US Forest Serv, Climate Fire & Carbon Cycle Sci, USDA, Durham, NC USA.
Univ Quebec Montreal, Ctr Forest Res, Montreal, PQ, Canada.
Russian Acad Sci, Siberian Branch, FRC KSC, VN Sukachev Inst Forest, Krasnoyarsk, Russia.
World Res Inst, Dept Forestry, Washington, DC USA.
Pondicherry Univ, Dept Ecol & Environm Sci, Pondicherry, India.
UNPA, INTA, CONICET, Rio Gallegos, Argentina.
Western Sydney Univ, Sch Social Sci & Psychol Urban Studies, Penrith, NSW, Australia.
Inst Nacl de Pesquisas da Amazonia, Manaus, Amazonas, Brazil.
Univ Fed Sul Bahia, Ctr Formacao Ciencias Agroflorestais, Lab Dendrol & Silvicultura Trop, Itabuna, Brazil.
Jardin Bot Medellin, Medellin, Colombia.
Tech Univ Munich, TUM Sch Life Sci, Chair Forest Growth & Yield Sci, Munich, Germany.
Univ Nacl Amazonia Peruana, Iquitos, Peru.
Fdn Con Vida & Corp COL TREE, SECC, Medellin, Colombia.
Boise State Univ, Dept Biol Sci, Boise, ID 83725 USA.
MUSE Museo Sci, Trop Biodivers Sect, Trento, Italy.
Univ Florence, Dept Biol, Florence, Italy.
Cent Univ Jharkhand, Dept Environm Sci, Ranchi, Bihar, India.
Univ Freiburg, Geobot, Fac Biol, Freiburg, Germany.
Forest Res Inst Zvolen, Natl Forest Ctr, Zvolen, Slovakia.
Univ Lorraine, AgroParisTech, INRA, Silva, Nancy, France.
Aarhus Univ, Dept Biosci, Ctr Biodivers Dynam Changing World BIOCHANGE, Aarhus, Denmark.
Univ La Serena, Dept Biol, La Serena, Chile.
Univ Fed Acre, Ctr Ciencias Biol & Nat, Acre, Brazil.
Guyana Forestry Commiss, Georgetown, French Guiana.
Univ Brunei Darussalam, Fac Sci, Bandar Seri Begawan, Brunei.
Univ Yaounde, Dept Biol, Higher Teachers Training Coll, Plant Systemat & Ecol Lab, Yaounde, Cameroon.
Univ Fed Rio Grande do Norte, Dept Ecol, Natal, RN, Brazil.
Aarhus Univ, Dept Biosci, Sect Ecoinformat & Biodivers, Aarhus, Denmark.
Czech Univ Life Sci, Fac Forestry & Wood Sci, Prague, Czech Republic.
Free Univ Amsterdam, Syst Ecol, Amsterdam, Netherlands.
Iwokrama Int Ctr Rainforest Conservat & Dev IIC, Georgetown, French Guiana.
Ural State Forest Engn Univ, Russian Acad Sci, Ural Branch, Bot Garden, Ekaterinburg, Russia.
CSIC, Museo Nacl Ciencias Nat, LINCGlobal, Madrid, Spain.
Univ Leipzig, Inst Biol, Systemat Bot & Funct Biodivers, Leipzig, Germany.
Vietnamese Acad Forest Sci, Silviculture Res Inst, Hanoi, Vietnam.
Univ Montpellier, CNRS, Cirad, INRA,IRD,UMR AMAP, Montpellier, France.
Univ Tras Os Montes & Alto Douro, Ctr Res & Technol Agroenvironm & Biol Sci, CITAB, UTAD, Vila Real, Portugal.
Polytech Inst Viseu, Agr High Sch, Viseu, Portugal.
Univ Estadual Campinas, Environm Studies & Res Ctr, Campinas, SP, Brazil.
Univ Stellenbosch, Dept Forest & Wood Sci, Stellenbosch, South Africa.
Hainan Univ, Sch Life & Pharmaceut Sci, Key Lab Trop Biol Resources, Minist Educ, Haikou, Hainan, Peoples R China.
West Virginia Univ, Div Forestry & Nat Resources, Morgantown, WV 26506 USA.
Manaaki Whenua Landcare Res, Lincoln, New Zealand.
Karlsruhe Inst Technol, Inst Geog & Geoecol, Dept Wetland Ecol, Karlsruhe, Germany.
Ctr Agr Res Suriname CELOS, Paramaribo, Surinam.
Tropenbios Int, Wageningen, Netherlands.
Polish State Forests, Coordinat Ctr Environm Projects, Warsaw, Poland.
Univ Estadual Campinas, Inst Biol, Programa Posgrad Biol Vegetal, Campinas, SP, Brazil.
Univ Florida, Sch Forest Resources & Conservat, Spatial Ecol & Conservat Lab, Gainesville, FL 32611 USA.
Flamingo Land Ltd, Kirby Misperton, England.
Univ Trento, Ctr Agr, Alimenti, Ambiente, San Michele All Adige, Italy.
Wild Chimpanzee Fdn, Liberia Off, Monrovia, Liberia.
Univ Mayor, Ctr Modelac & Monitoreo Ecosistemas, Santiago, Chile.
Univ La Frontera, Lab Biometria, Temuco, Chile.
Norwegian Univ Life Sci, Fac Environm Sci & Nat Resource Management, As, Norway.

Доп.точки доступа:
Steidinger, B. S.; Crowther, T. W.; Liang, J.; Van Nuland, M. E.; Werner, G. D. A.; Reich, P. B.; Nabuurs, S.; De-Miguel, M.; Zhou, N.; Picard, B.; Herault, X.; Zhao, C.; Zhang, D.; Routh, K. G.; Peay, K. G.; Abegg, Meinrad; Yao, C. Yves Adou; Alberti, Giorgio; Zambrano, Angelica Almeyda; Alvarez-Davila, Esteban; Alvarez-Loayza, Patricia; Alves, Luciana F.; Ammer, Christian; Anton-Fernandez, Clara; Araujo-Murakami, Alejandro; Arroyo, Luzmila; Avitabile, Valerio; Aymard, Gerardo; Baker, Timothy; Balazy, Radomir; Banki, Olaf; Barroso, Jorcely; Bastian, Meredith; Bastin, Jean-Francois; Birigazzi, Luca; Birnbaum, Philippe; Bitariho, Robert; Boeckx, Pascal; Bongers, Frans; Bouriaud, Olivier; Brancalion, Pedro H. S.; Brandl, Susanne; Brearley, Francis Q.; Brienen, Roel; Broadbent, Eben; Bruelheide, Helge; Bussotti, Filippo; Gatti, Roberto Cazzolla; Cesar, Ricardo; Cesljar, Goran; Chazdon, Robin; Chen, Han Y. H.; Chisholm, Chelsea; Cienciala, Emil; Clark, Connie J.; Clark, David; Colletta, Gabriel; Condit, Richard; Coomes, David; Valverde, S.; Corral-Rivas, Jose J.; Crim, Philip; Cumming, Jonathan; Dayanandan, Selvadurai; de Gasper, Andre L.; Decuyper, Mathieu; Derroire, Geraldine; DeVries, Ben; Djordjevic, Ilija; Ieda, Amaral; Dourdain, Aurelie; Obiang, Nestor Laurier Engone; Enquist, Brian; Eyre, Teresa; Fandohan, Adande Belarmain; Fayle, Tom M.; Feldpausch, Ted R.; Finer, Leena; Fischer, Markus; Fletcher, Christine; Fridman, Jonas; Frizzera, Lorenzo; Gamarra, Javier G. P.; Gianelle, Damiano; Glick, Henry B.; Harris, David; Hector, Andrew; Hemp, Andreas; Hengeveld, Geerten; Herbohn, John; Herold, Martin; Hillers, Annika; Coronado, A. M.; Huber, Markus; Hui, Cang; Cho, Hyunkook; Ibanez, Thomas; Jung, Ilbin; Imai, Nobuo; Jagodzinski, Andrzej M.; Jaroszewicz, Bogdan; Johannsen, Vivian; Joly, Carlos A.; Jucker, Tommaso; Karminov, Viktor; Kartawinata, Kuswata; Kearsley, Elizabeth; Kenfack, David; Kennard, Deborah; Kepfer-Rojas, Sebastian; Keppel, Gunnar; Khan, Mohammed Latif; Killeen, Timothy; Kim, Hyun Seok; Kitayama, Kanehiro; Kohl, Michael; Korjus, Henn; Kraxner, Florian; Laarmann, Diana; Lang, Mait; Lewis, Simon; Lu, Huicui; Lukina, Natalia; Maitner, Brian; Malhi, Yadvinder; Marcon, Eric; Marimon, Beatriz Schwantes; Marshall, Andrew Robert; Martin, Emanuel; Martynenko, Olga; Meave, Jorge A.; Melo-Cruz, Omar; Mendoza, Casimiro; Merow, Cory; Mendoza, Abel Monteagudo; Moreno, Vanessa; Mukul, Sharif A.; Mundhenk, Philip; Nava-Miranda, Maria G.; Neill, David; Neldner, Victor; Nevenic, Radovan; Ngugi, Michael; Niklaus, Pascal; Oleksyn, Jacek; Ontikov, Petr; Ortiz-Malavasi, Edgar; Pan, Yude; Paquette, Alain; Parada-Gutierrez, Alexander; Parfenova, Elena; Park, Minjee; Parren, Marc; Parthasarathy, Narayanaswamy; Peri, Pablo L.; Pfautsch, Sebastian; Phillips, Oliver; Piedade, Maria Teresa; Piotto, Daniel; Pitman, Nigel C. A.; Polo, Irina; Poorter, Lourens; Poulsen, Axel Dalberg; Poulsen, John R.; Pretzsch, Hans; Arevalo, Freddy Ramirez; Restrepo-Correa, Zorayda; Rodeghiero, Mirco; Rolim, Samir; Roopsind, Anand; Rovero, Francesco; Rutishauser, Ervan; Saikia, Purabi; Saner, Philippe; Schall, Peter; Schelhaas, Mart-Jan; Schepaschenko, Dmitry; Scherer-Lorenzen, Michael; Schmid, Bernhard; Schongart, Jochen; Searle, Eric; Seben, Vladimir; Serra-Diaz, Josep M.; Salas-Eljatib, Christian; Sheil, Douglas; Shvidenko, Anatoly; Silva-Espejo, Javier; Silveira, Marcos; Singh, James; Sist, Plinio; Slik, Ferry; Sonke, Bonaventure; Souza, Alexandre F.; Sterenczak, Krzysztof; Svenning, Jens-Christian; Svoboda, Miroslav; Targhetta, Natalia; Tchebakova, Nadja; ter Steege, Hans; Thomas, Raquel; Tikhonova, Elena; Umunay, Peter; Usoltsev, Vladimir; Valladares, Fernando; van der Plas, Fons; Do, B.; Martinez, S.; Verbeeck, Hans; Viana, Helder; Vieira, Simone; von Gadow, Klaus; Wang, Hua-Feng; Watson, James; Westerlund, Bertil; Wiser, Susan; Wittmann, Florian; Wortel, Verginia; Zagt, Roderick; Zawila-Niedzwiecki, Tomasz; Zhu, Zhi-Xin; Zo-Bi, Irie Casimir; Almeyda, Angelica; Herault, Bruno; ter, Hans

/ A. Panov [et al.] // International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM : International Multidisciplinary Scientific Geoconference, 2019. - Vol. 19: 19th International Multidisciplinary Scientific Geoconference, SGEM 2019 (30 June 2019 through 6 July 2019, ) Conference code: 150491, Is. 5.2. - P249-262, DOI 10.5593/sgem2019/5.2/S20.032 . -
Аннотация: Vast carbon reservoirs hosted in the Arctic realm may trigger a significant positive feedback loop in the global Earth climate system under existing global warming scenarios. Nevertheless, sparse coverage of the Arctic region with greenhouse gas (GHG) observation network limits our understanding of carbon cycling in this environment and making predictions about a fate of carbon conserved in currently frozen ground. Especially critical gaps exist in the vast Arctic territories of Siberia, where solely 3 continuous atmospheric carbon observation stations are currently operational and located entirely in Northeastern Siberia: Atmospheric carbon observation station Ambarchik (69.62° N, 162.30° E), the Tiksi hydrometeorological observatory (71.6°N, 128.9° E) and the Cape Baranova ice base observatory on the Bolshevik Island, Severnaya Zemlya (79.3° N, 101.8° E). In this paper we introduce a newly established coastal atmospheric carbon observation station Dikson (73.33° N, 80.34° E), jointly maintained by the V. N. Sukachev Institute of Forest SB RAS (Krasnoyarsk, Russia), Joint Directorate of Taimyr Nature Reserves (Norilsk, Russia) and the Max Planck Institute for Biogeochemistry (Jena, Germany), which is intended to fill the gap in the atmospheric GHG observations in the northcentral Siberian domain. The general west wind drift expected at the location of the site makes it more sensitive to the northern latitudes of Western Siberia, as compared to the other, more eastern, stations, which, due to the specific cyclonic activity that prevents air from the Icelandic low pressure minimum spreading towards the east of Severnaya Zemlya. The measurement site, which was launched in September 2018, is located on the Taimyr Peninsula near the gulf of the Yenisei River at the coast of the Kara Sea. Atmospheric mole fractions of CO2, CH4 and H2O at the station are continuously measured by an analyzer based on the cavity ring-down spectroscopy (CRDS) technique (G2301-f, Picarro Inc., USA). Data quality control of trace gas measurements is achieved by regular calibrations against WMO-traceable reference gases, an applied water vapor correction and meteorological records that permit data screening. A preliminary wind analysis and calculated backward trajectories from hot spots downwind of the measurement site reveal that during late spring and summer tundra landscapes of the upper part of the Taimyr Peninsula, the gulf of the Yenisei River and the adjacent shelf areas of the Arctic Ocean are the major contributors to the observed variability at the station. Conversely in winter (frost period) this site becomes receptive to air masses originated in the continental domain and containing the anthropogenic GHGs, e.g. the gas production on the Tazovskiy Peninsula. Here we summarize the scientific rationale of the new site, give technical details of the instrumental setup, analyze the local environments and present some exemplary results. © SGEM2019.

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V. N. Sukachev Institute of Forest of the Siberian Branch of Russian Akademy of Sciences – separated department of the FRC KSC SB RAS, Akademgorodok 50/28, Krasnoyarsk, 660036, Russian Federation
Max Planck Institute for Biogeochemistry, Hans-Knoll-Str. 10, Jena, D07745, Germany
University of Helsinki, Faculty of Science, Institute for Atmospheric and Earth System Research (INAR) / Physics, Gustaf Hallstromin katu 2b, Helsinki, 00560, Finland

Доп.точки доступа:
Panov, A.; Prokushkin, A.; Korets, M.; Sidenko, N.; Heimann, M.

/ M. Mellat, H. Bailey, K. R. Mustonen [et al.] // Front. Earth Sci. - 2021. - Vol. 9. - Ст. 651731, DOI 10.3389/feart.2021.651731. - Cited References:64. - The Pan-Arctic Precipitation Isotope Network (PAPIN) received funding from the European Union's Horizon 2020 Project INTERACT, under Grant Agreement No.730938 (JW PI). An Academy of Finland Grant (316014-JW PI). Support was also provided by a University of the Arctic Research Chairship to JW that funded isotope analyses and provided postdoctoral support for HB and K-RM and postgraduate research support for MM. A Russian Science Foundation Grant (No. 18-11-00024) to KG funded isotope analyses. SK was thankful to Russian Science Foundation (No. 20-67-46018). Russian Foundation for Basic Research (BFBR) supported isotopic analyses conducted by AP (#18-05-60203-Arktika). . - ISSN 2296-6463РУБ Geosciences, Multidisciplinary

Аннотация: Arctic sea-ice loss is emblematic of an amplified Arctic water cycle and has critical feedback implications for global climate. Stable isotopes (delta O-18, delta H-2, d-excess) are valuable tracers for constraining water cycle and climate processes through space and time. Yet, the paucity of well-resolved Arctic isotope data preclude an empirically derived understanding of the hydrologic changes occurring today, in the deep (geologic) past, and in the future. To address this knowledge gap, the Pan-Arctic Precipitation Isotope Network (PAPIN) was established in 2018 to coordinate precipitation sampling at 19 stations across key tundra, subarctic, maritime, and continental climate zones. Here, we present a first assessment of rainfall samples collected in summer 2018 (n = 281) and combine new isotope and meteorological data with sea ice observations, reanalysis data, and model simulations. Data collectively establish a summer Arctic Meteoric Water Line where delta H-2 = 7.6.delta O-18-1.8 (r(2) = 0.96, p < 0.01). Mean amount-weighted delta O-18, delta H-2, and d-excess values were -12.3, -93.5, and 4.9 parts per thousand, respectively, with the lowest summer mean delta O-18 value observed in northwest Greenland (-19.9 parts per thousand) and the highest in Iceland (-7.3 parts per thousand). Southern Alaska recorded the lowest mean d-excess (-8.2%) and northern Russia the highest (9.9 parts per thousand). We identify a range of delta O-18-temperature coefficients from 0.31 parts per thousand/degrees C (Alaska) to 0.93 parts per thousand/degrees C (Russia). The steepest regression slopes (>0.75 parts per thousand/degrees C) were observed at continental sites, while statistically significant temperature relations were generally absent at coastal stations. Model outputs indicate that 68% of the summer precipitating air masses were transported into the Arctic from mid-latitudes and were characterized by relatively high delta O-18 values. Yet 32% of precipitation events, characterized by lower delta O-18 and high d-excess values, derived from northerly air masses transported from the Arctic Ocean and/or its marginal seas, highlighting key emergent oceanic moisture sources as sea ice cover declines. Resolving these processes across broader spatial-temporal scales is an ongoing research priority, and will be key to quantifying the past, present, and future feedbacks of an amplified Arctic water cycle on the global climate system.

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Держатели документа:
Univ Oulu, Ecol & Genet Res Unit, Oulu, Finland.
Univ Oulu, Water Energy & Environm Engn Res Unit, Oulu, Finland.
Univ Alaska Anchorage, Dept Geol Sci, Anchorage, AK USA.
Ural Fed Univ, Inst Nat Sci, Ekaterinburg, Russia.
Univ Alaska, Inst Arctic Biol, Fairbanks, AK 99701 USA.
UrB Russian Acad Sci, N Laverov Fed Ctr Integrated Arctic Res, Arkhangelsk, Russia.
Fram Ctr, Norwegian Polar Inst, Tromso, Norway.
Ny Alesund Res Stn, Tromso, Norway.
Univ Calgary, Dept Geog, Calgary, AB, Canada.
Yugra State Univ, UNESCO Chair Environm Dynam & Global Climate Chan, Environm Dinam & Global Climate Change Res Ctr, Khanty Mansiysk, Russia.
Finnish Forest Adm, Metsahallitus, Muonio, Finland.
Tomsk State Univ, BIO GEO CLIM Lab, Tomsk, Russia.
Tuvan State Univ, Kyzyl, Russia.
Univ Copenhagen, Arctic Stn, Greenland, Copenhagen, Greenland.
Greenland Inst Nat Resources, Dept Environm & Mineral Resources, Nuuk, Greenland.
Univ Oulu, Oulanka Res Stn, Oulu, Finland.
Univ Toulouse, CNRS, Geosci Environm Toulouse, Toulouse, France.
Siberian Fed Univ, Fac Biol, Krasnoyarsk, Russia.
SB RAS, VN Sukachev Inst Forest, Krasnoyarsk, Akademgorodok, Russia.
Univ Turku, Biodivers Unit, Kevo Subarct Res Inst, Turku, Finland.
Sudurnes Sci & Learning Ctr, Sandgerdi, Iceland.
Univ Alaska Anchorage, Dept Biol Sci, Anchorage, AK USA.
Univ Arctic UArctic, Rovaniemi, Finland.

Доп.точки доступа:
Mellat, Moein; Bailey, Hannah; Mustonen, Kaisa-Riikka; Marttila, Hannu; Klein, Eric S.; Gribanov, Konstantin; Bret-Harte, M. Syndonia; Chupakov, Artem V.; Divine, Dmitry V.; Else, Brent; Filippov, Ilya; Hyoky, Valtteri; Jones, Samantha; Kirpotin, Sergey N.; Kroon, Aart; Markussen, Helge Tore; Nielsen, Martin; Olsen, Maia; Paavola, Riku; Pokrovsky, Oleg S.; Prokushkin, Anatoly; Rasch, Morten; Raundrup, Katrine; Suominen, Otso; Syvanpera, Ilkka; Vignisson, Solvi Runar; Zarov, Evgeny; Welker, Jeffrey M.; European Union's Horizon 2020 Project INTERACT [730938]; Academy of FinlandAcademy of FinlandEuropean Commission [316014]; University of the Arctic Research Chairship; Russian Science FoundationRussian Science Foundation (RSF) [18-11-00024, 20-67-46018]; Russian Foundation for Basic Research (BFBR) [18-05-60203-Arktika]

/ S. Veraverbeke, C. J.F. Delcourt, E. Kukavskaya [et al.] // Curr. Opin. Environ. Sci. Health. - 2021. - Vol. 23. - Ст. 100277, DOI 10.1016/j.coesh.2021.100277 . - ISSN 2468-5844
Аннотация: Increases in arctic-boreal fires can switch these biomes from a long-term carbon (C) sink to a source of atmospheric C through direct fire emissions and longer-term emissions from soil respiration. We here review advances made by the arctic-boreal fire science community over the last three years. Landscapes of intermediate drainage tend to experience the highest C combustion, dominated by soil C emissions, because of relatively thick and periodically dry organic soils. These landscapes may also induce a climate warming feedback through combustion and postfire respiration of legacy C, including from permafrost thaw and degradation. Legacy C is soil C that had escaped burning in the previous fire. Data shortages from fires in tundra ecosystems and Eurasian boreal forests limit our understanding of C emissions from arctic-boreal fires. Interactions between fire, topography, vegetation, soil, and permafrost need to be considered when estimating climate feedbacks of arctic-boreal fires. © 2021 The Author(s)

Scopus

Держатели документа:
Faculty of Science, Vrije Universiteit Amsterdam, Amsterdam, Netherlands
V.N. Sukachev Institute of Forest, Siberian Branch of the Russian Academy of Sciences – Separate Subdivision of the FRC KSC SB RAS, Krasnoyarsk, Russian Federation
Center for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, United States
Woodwell Climate Research Center, Falmouth, MA, United States

Доп.точки доступа:
Veraverbeke, S.; Delcourt, C. J.F.; Kukavskaya, E.; Mack, M.; Walker, X.; Hessilt, T.; Rogers, B.; Scholten, R. C.

/ Q. Sun, A. Burrell, K. Barrett [et al.] // Remote Sens. - 2021. - Vol. 13, Is. 12. - Ст. 2247, DOI 10.3390/rs13122247 . - ISSN 2072-4292
Аннотация: Prolonged dry periods and increased temperatures that result from anthropogenic climate change have been shown to increase the frequency and severity of wildfires in the boreal region. There is growing evidence that such changes in fire regime can reduce forest resilience and drive shifts in post-fire plant successional trajectories. The response of post-fire vegetation communities to climate variability is under-studied, despite being a critical phase determining the ultimate successional conclusion. This study investigated the responses of post-fire recruited species to climate change and inter-annual variability at 16 study sites that experienced high-severity fire events, mostly in early 2000, within the Scots pine forest-steppe zone of southeastern Siberia, Russia. These sites were originally dominated by Scots pine, and by 2018, they were recruited by different successional species. Additionally, three mature Scots pine stands were included for comparison. A Bayesian Additive Regression Trees (BART) approach was used to model the relationship between Landsat-derived Normalized Difference Vegetation Index (NDVI) time series, temperature and precipitation in the 15 years after a stand-replacing fire. Using the resulting BART models, together with six projected climate scenarios with increased temperature and enhanced inner-annual precipitation variability, we simulated NDVI at 5-year intervals for 15 years post-fire. Our results show that the BART models performed well, with in-sample Pseudo-R2 varying from 0.49 to 0.95 for fire-disturbed sites. Increased temperature enhanced greenness across all sites and across all three time periods since fires, exhibiting a positive feedback in a warming environment. Repeatedly dry spring periods reduced NDVI at all the sites and wetter summer periods following such dry springs could not compensate for this, indicating that a prolonged dry spring has a strong impact consistently over the entire early developmental stages from the initial 5 years to 15 years post-fire. Further, young forests showed higher climate sensitivity compared to the mature forest, irrespective of species and projected climatic conditions. Our findings suggest that a dry spring not only increases fire risk, but also delays recovery of boreal forests in southern Siberia. It also highlights the importance of changing rainfall seasonality as well as total rainfall in a changing climate for post-fire recovery of forest. © 2021 by the authors. Licensee MDPI, Basel, Switzerland.

Scopus

Держатели документа:
College of Wildlife and Protected Area, Northeast Forestry University, 26 Hexing Road, Harbin, 150040, China
Department of Biosciences, University of Durham, South Road, Durham, DH1 3LE, United Kingdom
Woodwell Climate Research Centre, 149 Woods Hole Road, Falmouth, MA 02540, United States
Centre for Landscape and Climate Research, School of Geography, Geology and Environment, University of Leicester, University Road, Leicester, LE1 7RH, United Kingdom
Leicester Institute for Space and Earth Observation, University of Leicester, University Road, Leicester, LE1 7RH, United Kingdom
V.N. Sukachev Institute of Forest of the Siberian Branch of the Russian Academy of Sciences-Separate Subdivision of the FRC KSC SB RAS, 50/28 Akademgorodok, Krasnoyarsk, 660036, Russian Federation
The Branch of FBU VNIILM “Centre of Forest Pyrology”, 42 Krupskaya, Krasnoyarsk, 660062, Russian Federation
Reshetnev Siberian State University of Science and Technology, 31 Krasnoyarskiy Rabochiy Ave, Krasnoyarsk, 660037, Russian Federation

Доп.точки доступа:
Sun, Q.; Burrell, A.; Barrett, K.; Kukavskaya, E.; Buryak, L.; Kaduk, J.; Baxter, R.

/ Q. Q. Sun, A. Burrell, K. Barrett [et al.] // Remote Sens. - 2021. - Vol. 13, Is. 12. - Ст. 2247, DOI 10.3390/rs13122247. - Cited References:78. - This research was funded by the UK Natural Environment Research Council, grant number NE/N009495/1, awarded to K.B. and R.B. . - ISSN 2072-4292РУБ Environmental Sciences + Geosciences, Multidisciplinary + Remote Sensing

Аннотация: Prolonged dry periods and increased temperatures that result from anthropogenic climate change have been shown to increase the frequency and severity of wildfires in the boreal region. There is growing evidence that such changes in fire regime can reduce forest resilience and drive shifts in post-fire plant successional trajectories. The response of post-fire vegetation communities to climate variability is under-studied, despite being a critical phase determining the ultimate successional conclusion. This study investigated the responses of post-fire recruited species to climate change and inter-annual variability at 16 study sites that experienced high-severity fire events, mostly in early 2000, within the Scots pine forest-steppe zone of southeastern Siberia, Russia. These sites were originally dominated by Scots pine, and by 2018, they were recruited by different successional species. Additionally, three mature Scots pine stands were included for comparison. A Bayesian Additive Regression Trees (BART) approach was used to model the relationship between Landsat-derived Normalized Difference Vegetation Index (NDVI) time series, temperature and precipitation in the 15 years after a stand-replacing fire. Using the resulting BART models, together with six projected climate scenarios with increased temperature and enhanced inner-annual precipitation variability, we simulated NDVI at 5-year intervals for 15 years post-fire. Our results show that the BART models performed well, with in-sample Pseudo-R-2 varying from 0.49 to 0.95 for fire-disturbed sites. Increased temperature enhanced greenness across all sites and across all three time periods since fires, exhibiting a positive feedback in a warming environment. Repeatedly dry spring periods reduced NDVI at all the sites and wetter summer periods following such dry springs could not compensate for this, indicating that a prolonged dry spring has a strong impact consistently over the entire early developmental stages from the initial 5 years to 15 years post-fire. Further, young forests showed higher climate sensitivity compared to the mature forest, irrespective of species and projected climatic conditions. Our findings suggest that a dry spring not only increases fire risk, but also delays recovery of boreal forests in southern Siberia. It also highlights the importance of changing rainfall seasonality as well as total rainfall in a changing climate for post-fire recovery of forest.

WOS

Держатели документа:
Northeast Forestry Univ, Coll Wildlife & Protected Area, 26 Hexing Rd, Harbin 150040, Peoples R China.
Univ Durham, Dept Biosci, South Rd, Durham DH1 3LE, England.
Woodwell Climate Res Ctr, 149 Woods Hole Rd, Falmouth, MA 02540 USA.
Univ Leicester, Ctr Landscape & Climate Res, Sch Geog Geol & Environm, Univ Rd, Leicester LE1 7RH, Leics, England.
Univ Leicester, Leicester Inst Space & Earth Observat, Univ Rd, Leicester LE1 7RH, Leics, England.
Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Separate Subdiv FRC KSC SB RAS, 50-28 Akad Gorodok, Krasnoyarsk 660036, Russia.
FBU VNIILM Ctr Forest Pyrol, 42 Krupskaya, Krasnoyarsk 660062, Russia.
Reshetnev Siberian State Univ Sci & Technol, 31 Krasnoyarskiy Rabochiy Ave, Krasnoyarsk 660037, Russia.

Доп.точки доступа:
Sun, Qiaoqi; Burrell, Arden; Barrett, Kirsten; Kukavskaya, Elena; Buryak, Ludmila; Kaduk, Jorg; Baxter, Robert; UK Natural Environment Research CouncilUK Research & Innovation (UKRI)Natural Environment Research Council (NERC) [NE/N009495/1]

/ S. Veraverbeke, CJF Delcourt, E. Kukavskaya [et al.] // Curr. Opin. Environ. Sci. Health. - 2021. - Vol. 23. - Ст. 100277, DOI 10.1016/j.coesh.2021.100277. - Cited References:39. - The authors thank the reviewers for their suggestions on the manuscript. Sander Veraverbeke thanks funding support from the Netherlands Organisation for Scientific Research (NWO) through his Vidi grant `Fires pushing trees North' (016. Vidi.189.070). Brendan Rogers acknowledges support from the National Aeronautics and Space Administration (NASA) Arctic-Boreal Vulnerability Experiment (NNX15AU56A) and the Gordon and Betty Moore Foundation (Grant #8414). Elena Kukavskaya thanks funding support from the RFBR, Government of the Krasnoyarsk krai and the Krasnoyarsk regional foundation of scientific and scientific-technical support (Grant #20-44-242004). . - ISSN 2468-5844
Аннотация: Increases in arctic-boreal fires can switch these biomes from a long-term carbon (C) sink to a source of atmospheric C through direct fire emissions and longer-term emissions from soil respiration. We here review advances made by the arcticboreal fire science community over the last three years. Landscapes of intermediate drainage tend to experience the highest C combustion, dominated by soil C emissions, because of relatively thick and periodically dry organic soils. These landscapes may also induce a climate warming feedback through combustion and postfire respiration of legacy C, including from permafrost thaw and degradation. Legacy C is soil C that had escaped burning in the previous fire. Data shortages from fires in tundra ecosystems and Eurasian boreal forests limit our understanding of C emissions from arcticboreal fires. Interactions between fire, topography, vegetation, soil, and permafrost need to be considered when estimating climate feedbacks of arctic-boreal fires. (C) 2021 The Author(s). Published by Elsevier B.V.

WOS

Держатели документа:
Vrije Univ Amsterdam, Fac Sci, Amsterdam, Netherlands.
Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, FRC KSC SB RAS,Separate Subdiv, Krasnoyarsk, Russia.
No Arizona Univ, Ctr Ecosyst Sci & Soc, Flagstaff, AZ 86011 USA.
Woodwell Climate Res Ctr, Falmouth, MA USA.

Доп.точки доступа:
Veraverbeke, Sander; Delcourt, Clement J. F.; Kukavskaya, Elena; Mack, Michelle; Walker, Xanthe; Hessilt, Thomas; Rogers, Brendan; Scholten, Rebecca C.; Netherlands Organisation for Scientific Research (NWO)Netherlands Organization for Scientific Research (NWO) [016. Vidi.189.070]; National Aeronautics and Space Administration (NASA) Arctic-Boreal Vulnerability Experiment [NNX15AU56A]; Gordon and Betty Moore FoundationGordon and Betty Moore Foundation [8414]; RFBR, Government of the Krasnoyarsk krai; Krasnoyarsk regional foundation of scientific and scientific-technical support [20-44-242004]