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

[Текст] / С. Т. Им // Лесные биогеоценозы бореальной зоны: география, структура, функции, динамика. Материалы Всероссийской научной конференции с международным участием, посвященной 70-летию создания Института леса им. В.Н. Сукачева СО РАН 16-19 сентября 2014 г., Красноярск. - Новосибирск : Изд-во СО РАН, 2014. - С. 133-135. - Библиогр. в конце ст.
Аннотация: Проведено исследование изменений водной массы в зоне вечной мерзлоты Центральной Сибири по данным дистанционного зондирования GRACE за период 2003—2013 годов. Выделено одиннадцать зон с однородными временными сериями водного эквивалента массы. В период 2003—2009 гг. для восьми зон выделены значимые положительные тренды водной массы (4—21 мм в год, a 0,05). На участках, расположенных в тундре в зоне сплошной мерзлоты, наблюдается достоверный рост дисперсии водной массы в период 2010—2013 гг. по сравнению с 2003—2009 гг. Указанные аномалии водной массы связаны с климатическими изменениями.

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Институт леса им. В.Н. Сукачева СО РАН : 660036, Красноярск, Академгородок, 50, стр. 28

Доп.точки доступа:
Im, Sergey Tkhekdyeyevich

[Text] / S. T. Im [et al.] // Contemp. Probl. Ecol. - 2015. - Vol. 8, Is. 6. - P680-686, DOI 10.1134/S1995425515060074. - Cited References:23. - This study was supported by the Russian Scientific Foundation, project no. 14-24-00112. Analysis of the data of GRACE gravimetric survey was supported by the government of the Russian Federation, project no. 14.B.25.31.0031. . - ISSN 1995-4255. - ISSN 1995-4263РУБ Ecology

Аннотация: Quantitative dynamics, water surface area, and water level of lakes in the Trans-Baikal forest-steppe zone have been studied by spectroradiometry (Landsat satellite), gravimetry (GRACE satellite), and altimetry (Envisat satellite). The number of lakes and their water surface area correlated with precipitation (r = 0.84-0.85), summer and annual temperature (r =-0.77 to-0.9), and drought index (r = 0.95-0.97). During extremely dry periods (2006-2010), the number of lakes decreased by four (compared to 1989) and their water surface area decreased by three (compared to 2000). The rate of change in the water level of the lakes (periods of similar to 29 years) was determined.

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Держатели документа:
Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Krasnoyarsk 660036, Russia.
Siberian Fed Univ, Krasnoyarsk 660041, Russia.
Reshetnev Siberian State Aerosp Univ, Krasnoyarsk 660014, Russia.

Доп.точки доступа:
Im, S. T.; Kharuk, V. I.; Rakityanskaya, N. M.; Golyukov, A. S.; Russian Scientific Foundation [14-24-00112]; government of the Russian Federation [14.B.25.31.0031]

/ S. T. Im, V. I. Kharuk // Izv. Atmos. Ocean Phys. - 2015. - Vol. 51, Is. 8. - P806-818, DOI 10.1134/S0001433815080046 . - ISSN 0001-4338
Аннотация: The GRACE gravimetric survey is applied to analyze the equivalent water mass anomalies (EWMAs) in the permafrost zone of Central Siberia. Variations in EWMAs are related to precipitation, air temperature, potential evapotranspiration, and soil composition (drainage conditions). The EWMA dynamics demonstrates two periods. The period of 2003–2008 is characterized by a positive trend. The one of 2008–2012 shows a decrease in the trend with a simultaneous increase by 30–70% of EWMA dispersion in the background of growth (up to 40%) of precipitation variability. The rate of water mass increment demonstrates a positive correlation with the sand and gravel contents in soil (r = 0.72) and a negative one with clay content (r =–0.69 to–0.77). For Taimyr Peninsula, there is a deficit of residual water mass (~250 mm for the period of 2012–2013) indicating the deeper thawing of permafrost soils. In the Central Siberian Plateau, the indicator of more intensive permafrost thawing (and that of an increase in active layer thickness) is a considerable trend of water mass increase (2003–2008). The increasing trend of the largest Siberian rivers (Yenisei and Lena) is revealed in the period of 2003–2012. © 2015, Pleiades Publishing, Ltd.

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Держатели документа:
Sukachev Institute of Forest, Siberian Branch, Russian Academy of Sciences, Akademgorodok 50, buiding 28, Krasnoyarsk, Russian Federation
Institute of Economy, Management, and Nature Use, Siberian Federal University, ul. Kirenskogo 266, Krasnoyarsk, Russian Federation
Reshetnev Siberian State Aerospace University, pr. imeni gazety “Krasnoyarskii rabochii” 31, building A, Krasnoyarsk, Russian Federation
Institute of Space and Information Technologies, Siberian Federal University, pr. Svobodnyi 79, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Im, S. T.; Kharuk, V. I.

/ V. I. Kharuk [et al.] // Environ.Res.Lett. - 2015. - Vol. 10, Is. 12, DOI 10.1088/1748-9326/10/12/125009 . - ISSN 1748-9318
Аннотация: Aim: estimation of larch (Larix gmelinii) growth response to current climate changes. Location: permafrost area within the northern part of Central Siberia (∼65.8°N, 98.5°E). Method: analysis of dendrochronological data, climate variables, drought index SPEI, GPP (gross primary production) and EVI vegetation index (both Aqua/MODIS satellite derived), and soil water content anomalies (GRACE satellite measurements of equivalent water thickness anomalies, EWTA). Results: larch tree ring width (TRW) correlated with previous year August precipitation (r = 0.63), snow accumulation (r = 0.61), soil water anomalies (r = 0.79), early summer temperatures and water vapor pressure (r = 0.73 and r = 0.69, respectively), May and June drought index (r = 0.68-0.82). There are significant positive trends of TRW since late 1980 s and GPP since the year 2000. Mean TRW increased by about 50%, which is similar to post-Little Ice Age warming. TRW correlated with GPP and EVI of larch stands (r = 0.68-0.69). Main conclusions: within the permafrost zone of central Siberia larch TRW growth is limited by early summer temperatures, available water from snowmelt, water accumulated within soil in the previous year, and permafrost thaw water. Water stress is one of the limiting factors of larch growth. Larch TRW growth and GPP increased during recent decades. © 2015 IOP Publishing Ltd.

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Держатели документа:
Sukachev Institute of Forest, Krasnoyarsk, Russian Federation
Siberian Federal University, Krasnoyarsk, Russian Federation
Siberian State Aerospace University, Krasnoyarsk, Russian Federation
NASA's GSFC, Greenbelt, MD, United States

Доп.точки доступа:
Kharuk, V. I.; Ranson, K. J.; Im, S. T.; Petrov, I. A.

[Text] / V. I. Kharuk [et al.] // Environ. Res. Lett. - 2015. - Vol. 12, Is. 12. - Ст. 125006, DOI 10.1088/1748-9326/10/12/125006. - Cited References:54. - The Russian Science Foundation (grant #14-24-00112) primarily supported this research. Additional support for K J Ranson by NASA's Terrestrial Ecology program is acknowledged. . - ISSN 1748-9326РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: The aim of this work is an analysis of the causes of spruce (Picea abies L.) decline and mortality in Belarus. The analysis was based on forest inventory and Landsat satellite (land cover classification, climate variables (air temperature, precipitation, evaporation, vapor pressure deficit, SPEI drought index)), and GRACE-derived soil moisture estimation (equivalent of water thickness anomalies, EWTA). We found a difference in spatial patterns between dead stands and all stands (i.e., before mortality). Dead stands were located preferentially on relief features with higher water stress risk (i.e., higher elevations, steeper slopes, south and southwestern exposure). Spruce mortality followed a series of repeated droughts between 1990 and 2010. Mortality was negatively correlated with air humidity (r = -0.52), and precipitation (r = -0.57), and positively correlated with the prior year vapor pressure deficit (r = 0.47), and drought increase (r = 0.57). Mortality increased with the increase in occurrence of spring frosts (r = 0.5), and decreased with an increase in winter cloud cover (r = -0.37). Spruce mortality was negatively correlated with snow water accumulation (r = -0.81) and previous year anomalies in water soil content (r = -0.8). Weakened by water stress, spruce stands were attacked by pests and phytopathogens. Overall, spruce mortality in Belarussian forests was caused by drought episodes and drought increase in synergy with pest and phytopathogen attacks. Vast Picea abies mortality in Belarus and adjacent areas of Russia and Eastern Europe is a result of low adaptation of that species to increased drought. This indicates the necessity of spruce replacement by drought-tolerant indigenous (e.g., Pinus sylvestris, Querqus robur) or introduced (e.g., Larix sp. or Pseudotsuga menzieslii) species to obtain sustainable forest growth management.

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Держатели документа:
VN Sukachev Inst Forest SB RAS, Krasnoyarsk, Russia.
Siberian Fed Univ, Krasnoyarsk, Russia.
Siberian State Aerosp Univ, Krasnoyarsk, Russia.
NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.

Доп.точки доступа:
Kharuk, Viacheslav I.; Im, Sergei T.; Dvinskaya, Maria L.; Golukov, Alexei S.; Ranson, Kenneth J.; Russian Science Foundation [14-24-00112]; NASA's Terrestrial Ecology program

[Текст] / С. Т. Им // Сибирский экологический журнал. - 2015. - т. 22. № 6. - С. 832-831. - Библиогр. в конце ст.
Аннотация: На основе спектрорадиометрии (спутник Landsat), гравиметрии (спутник GRACE) и альтиметрии (спутник Envisat) исследована динамика количества, площади и уровня водной поверхности озер лесостепной зоны Забайкалья. Количество и площадь поверхности озер коррелируют с количеством осадков (r = 0,84…0,85), летними и годовыми температурами (r = −0,77… −0,9) и индексом сухости (r = 0,95…0,97). В экстремально засушливые периоды (2006–2010 гг.) наблюдалось четырехкратное уменьшение количества озер (по сравнению с 1989 г.) и трехкратное — их площади (по сравнению с 2000 г.). Установлена периодичность (~ 29 лет) изменения уровня водной поверхности озер Забайкалья.

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Доп.точки доступа:
Харук, Вячеслав Иванович; Ракитянская, Н.М.; Голюков, А.С.; Im, Sergey Tkhekdyeyevich

/ V. I. Kharuk [et al.] // Environ.Res.Lett. - 2016. - Vol. 11, Is. 4, DOI 10.1088/1748-9326/11/4/045004 . - ISSN 1748-9318
Аннотация: Climate impact on landslide occurrence and spatial patterns were analyzed within the larch-dominant communities associated with continuous permafrost areas of central Siberia. We used high resolution satellite imagery (i.e. QuickBird, WorldView) to identify landslide scars over an area of 62 000 km2. Landslide occurrence was analyzed with respect to climate variables (air temperature, precipitation, drought index SPEI), and Gravity Recovery and Climate Experiment satellite derived equivalent of water thickness anomalies (EWTA). Landslides were found only on southward facing slopes, and the occurrence of landslides increased exponentially with increasing slope steepness. Lengths of landslides correlated positively with slope steepness. The observed upper elevation limit of landslides tended to coincide with the tree line. Observations revealed landslides occurrence was also found to be strongly correlated with August precipitation (r = 0.81) and drought index (r = 0.7), with June-July-August soil water anomalies (i.e., EWTA, r = 0.68-0.7), and number of thawing days (i.e., a number of days with t max > 0 °C; r = 0.67). A significant increase in the variance of soil water anomalies was observed, indicating that occurrence of landslides may increase even with a stable mean precipitation level. The key-findings of this study are (1) landslides occurrence increased within the permafrost zone of central Siberia in the beginning of the 21st century; (2) the main cause of increased landslides occurrence are extremes in precipitation and soil water anomalies; and (3) landslides occurrence are strongly dependent on relief features such as southward facing steep slopes. © 2016 IOP Publishing Ltd.

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Держатели документа:
Sukachev Forest Institute, Krasnoyarsk, Russian Federation
Siberian Federal University, Krasnoyarsk, Russian Federation
Siberian State Aerospace University, Krasnoyarsk, Russian Federation
NASA's Goddard Space Flight Center, Greenbelt, MD, United States

Доп.точки доступа:
Kharuk, V. I.; Shushpanov, A. S.; Im, S. T.; Ranson, K. J.

/ S. Im // WATER, RESOURCES, FOREST, MARINE AND OCEAN ECOSYSTEMS CONFERENCE : STEF92 TECHNOLOGY LTD, 2016. - 16th International Multidisciplinary Scientific Geoconference (SGEM (JUN 30-JUL 06, 2016, Albena, BULGARIA). - P835-842. - (International Multidisciplinary Scientific GeoConference-SGEM). - Cited References:15 . - РУБ Water Resources

Аннотация: The permafrost region represents about 25% of the northern hemisphere (23x10(6) km(2)) and covers about 63% of the area of the Russian Federation (10x10(6) km(2)). Arctic and sub-arctic territories are particularly sensitive to temperature variations. Permafrost ground temperature has increased by 0.3-2.0 degrees C in northern Russia during the last four decades. This will result in permafrost thawing and changes in water balance. Until 2050, the thaw depth in the northern part of Siberia could increase by more than 50%. The remote sensing technique is useful in the studies of permafrost area. Remotely sensed gravity measurements from the GRACE (Gravity Recovery and Climate Experiment) mission allowed identifying of significant decrease of water mass in ice regions. The aim of this investigation was to reveal relationships between active layer changes and water mass anomalies extracted from GRACE data in the cryolithozone of Central Siberia. Six test sites with available active layer data were investigated. Correlation analysis was carried out to determine relationships of the thaw depth with equivalent water thickness anomalies (EWTA). June EWTA significantly correlates with the thaw depth in July on the Samoilov Island (r = 0.82, p < 0.03). This means that an increasing amount of water in soil results in a better transfer of heat to the frozen soils, thus can result in thawing at greater depth. Depending on site mean thaw depth values positively correlates with April, May, June and August EWTA (r = 0.72-0.98, p < 0.05). For Igarka site, the negative correlation of thaw depth in September with August EWTA was revealed (r = -0.99, p < 0.1). This is opposed to the observed on Samoilov Island, and probably, explained by differences in hydrological regimes.

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Держатели документа:
RAS, VN Sukachev Inst Forest SB, Krasnoyarsk, Russia.
Siberian Fed Univ, Krasnoyarsk, Russia.
MF Reshetnev Siberian State Aerosp Univ, Krasnoyarsk, Russia.

Доп.точки доступа:
Im, Sergei

/ I. V. Danilova, A. A. Onuchin // Russ. Meteorol. Hydrol. - 2019. - Vol. 44, Is. 1. - P71-77, DOI 10.3103/S1068373919010084. - Cited References:17. - The research was supported by the Russian Foundation for Basic Research (grant 18-05-00781). . - ISSN 1068-3739. - ISSN 1934-8096РУБ Meteorology & Atmospheric Sciences

Аннотация: A methodology is presented for the estimation of the annual spatial distribution of solid precipitation using GRACE (Gravity Recovery and Climate Experiment) satellite data. The data are provided in the grid cells of 1 degrees (latitude and longitude) and allow calculating the water thickness changes near the Earth's surface including the snow cover water. The GRACE-based difference in water equivalent between the beginning and end of winter was found to be caused by both snow water and land surface characteristics which control the groundwater movement. The regularities revealed for the analyzed region and spatial detailing enable the construction of annual raster low- and mediumresolution (1 degrees and 90 m, respectively) images of solid precipitation.

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Держатели документа:
Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Akademgorodok 50,Str 28, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Danilova, I. V.; Onuchin, A. A.; Russian Foundation for Basic Research [18-05-00781]

/ R. Poyatos, V. Granda, V. Flo [et al.] // Earth Sys. Sci. Data. - 2021. - Vol. 13, Is. 6. - P2607-2649, DOI 10.5194/essd-13-2607-2021 . - ISSN 1866-3508
Аннотация: Plant transpiration links physiological responses of vegetation to water supply and demand with hydrological, energy, and carbon budgets at the land-atmosphere interface. However, despite being the main land evaporative flux at the global scale, transpiration and its response to environmental drivers are currently not well constrained by observations. Here we introduce the first global compilation of whole-plant transpiration data from sap flow measurements (SAPFLUXNET, https://sapfluxnet.creaf.cat/, last access: 8 June 2021). We harmonized and quality-controlled individual datasets supplied by contributors worldwide in a semi-automatic data workflow implemented in the R programming language. Datasets include sub-daily time series of sap flow and hydrometeorological drivers for one or more growing seasons, as well as metadata on the stand characteristics, plant attributes, and technical details of the measurements. SAPFLUXNET contains 202 globally distributed datasets with sap flow time series for 2714 plants, mostly trees, of 174 species. SAPFLUXNET has a broad bioclimatic coverage, with woodland/shrubland and temperate forest biomes especially well represented (80% of the datasets). The measurements cover a wide variety of stand structural characteristics and plant sizes. The datasets encompass the period between 1995 and 2018, with 50% of the datasets being at least 3 years long. Accompanying radiation and vapour pressure deficit data are available for most of the datasets, while on-site soil water content is available for 56% of the datasets. Many datasets contain data for species that make up 90% or more of the total stand basal area, allowing the estimation of stand transpiration in diverse ecological settings. SAPFLUXNET adds to existing plant trait datasets, ecosystem flux networks, and remote sensing products to help increase our understanding of plant water use, plant responses to drought, and ecohydrological processes. SAPFLUXNET version 0.1.5 is freely available from the Zenodo repository (10.5281/zenodo.3971689; Poyatos et al., 2020a). The "sapfluxnetr"R package-designed to access, visualize, and process SAPFLUXNET data-is available from CRAN. © 2021 Rafael Poyatos et al.

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Creaf, E08193 Bellaterra (Cerdanyola Del Valles), Catalonia, Spain
Universitat Autonoma de Barcelona, Bellaterra, (Cerdanyola del Valles), Catalonia, E08193, Spain
Joint Research Unit CREAF-CTFC, Bellaterra, Catalonia, Spain
Faculty of Science Engineering and Technology, Swinburne University of Technology, Hawthorn, VIC 3122, Australia
School of Life and Environmental Sciences, University of Sydney, Camperdown, NSW, Australia
Department of Botany, University of Debrecen, Faculty of Science and Technology, Egyetem ter 1, Debrecen, 4032, Hungary
Plant Physiology and Biochemistry, Institute of Botany, Sao Paulo, Brazil
Department of Natural Resources and Environmental Science, University of Nevada, Reno, NV, United States
Red Ecologia Funcional, Instituto de Ecologia A.C., Xalapa, Mexico
Center for Tropical Forest Science-Forest Global Earth Observatory, Smithsonian Tropical Research Institute, Panama, Panama
Conservation Ecology Center, Smithsonian Conservation Biology Institute, Front Royal, VA, United States
Department of Ecosystem Science and Management, Texas AandM University, College Station, TX, United States
School of Earth and Space Exploration, Arizona State University, Tempe, AZ, United States
School of Earth Environment and Society, McMaster Centre for Climate Change, McMaster University, Hamilton, ON, Canada
National Institute for Agricultural and Food Research and Technology (INIA), Forest Research Centre (CIFOR), Department of Forest Ecology and Genetics, Avda. A Coruna km 7.5, Madrid, 28040, Spain
Department of Natural Resources and the Environment, University of New Hampshire, Durham, NH, United States
Department of Biosciences, University of Durham, Durham, United Kingdom
School of Geography and Earth Sciences, McMaster Centre for Climate Change, McMaster University, Hamilton, ON, Canada
School of Informatics Computing and Cyber Systems, Northern Arizona University, Flagstaff, AZ, United States
Schmid College of Science and Technology, Chapman University, Orange, CA 92866, United States
Universite Paris-Saclay, Cnrs, AgroParisTech, Ecologie Systematique et Evolution, Orsay, 91405, France
University of Illinois at Urbana-Champaign, Urbana-Champaign, IL, United States
Eastern Forest Environmental Threat Assessment Center, Southern Research Station, Usda Forest Service, Research Triangle Park, NC 27709, United States
Department of Civil Environmental and Geodetic Engineering, Ohio State University, 405 Hitchcock Hall, 2070 Neil Avenue, Columbus, OH 43210, United States
Department of Forest Resources, University of Minnesota, Saint Paul, MN, United States
Universite de Lorraine, Inrae, AgroParisTech, Nancy, 54000, France
School of Forest Resources and Conservation, University of Florida, Gainesville, FL 32611, United States
Department of Botany Ecology and Plant Physiology, University of la Laguna (ULL), La Laguna, Tenerife, 38200, Spain
McMaster University Library, McMaster University, Hamilton, ON, Canada
CATIE-Centro Agronomico Tropical de Investigacion y Ensenanza, Costa Rica, Costa Rica
Laboratoire Evolution and Diversite Biologique, Cnrs, Ups, Ird, Batiment 4R1 Universite Paul Sabatier, 118 route de Narbonne, Toulouse CEDEX, 31062-4, France
Key Laboratory of the Ministry of Education for Coastal and Wetland Ecosystems, School of Life Sciences, Xiamen University, Xiamen, Fujian, 361005, China
Carrera de Ingenieria Ambiental, Facultad de Ingenieria, Universidad Nacional de Chimborazo, Riobamba, EC060108, Ecuador
Faculty of Geo-information and Earth Observation (ITC), University of Twente Enschede, Hengelosestraat 99, Enschede, 7514 AE, Netherlands
Usda Forest Service, Northern Research Station, Silas Little Experimental Forest, New Lisbon, NJ 08064, United States
Climate Change Unit, Environmental Protection Agency of Aosta Valley, Saint Christophe11020, Italy
Institute of Desertification Studies, Chinese Academy of Forestry, Beijing, 100091, China
Centro de Estudos Florestais, Instituto Superior de Agronomia, Universidade de Lisboa, Tapada da Ajuda, Lisbon, 1349-017, Portugal
Instituto Nacional de Investigacao Agraria e Veterinaria I.P., Quinta Do Marques, Av. da Republica, Oeiras, 2780-159, Portugal
Institut Universitaire de France (IUF), Paris, 75231, France
Universite Paris-Saclay, Cnrs, AgroParisTech, Ecologie Systematique et Evolution, Orsay, 91405, France
Dept of Atmospheric and Oceanic Sciences, University of Wisconsin-Madison, 1225 W Dayton St, Madison, WI 53706, United States
EcoandSols, Univ Montpellier, Cirad, Inrae, Institut Agro, Ird, Montpellier, 34060, France
Czech Technical University in Prague, Faculty of Civil Engineering, Thakurova 7, Prague, 16629, Czech Republic
Bordeaux Sciences Agro, Umr 1391 INRA-BSA, Bordeaux, France
Nicholas School of the Environment, Duke University, Durham, NC, United States
Department of Horticultural Science, University of Stellenbosch, Stellenbosch, South Africa
University of Alaska Fairbanks, Institute of Arctic Biology, Fairbanks, AK 99775, United States
Faculty of Regional and Environmental Sciences-Geobotany, University of Trier, Behringstra?e 21, Trier, 54296, Germany
Max Planck Institute for Biogeochemistry, Hans-Knoll-Str. 10, Jena, Germany
Wageningen University and Research, Water Systems and Global Change Group, P.O. Box 47, Wageningen, 6700AA, Netherlands
Department of Plant Biology, University of Campinas, Campinas, 13083-862, Brazil
Department of Botany, University of Wyoming, Laramie, WY, United States
Swiss Federal Institute for Forest, Snow and Landscape Research Wsl, Zuercherstrasse 111, Birmensdorf, 8903, Switzerland
Departamento de Ecologia Vegetal, Centro de Investigaciones Sobre Desertificacion (CSIC-UVEG-GV), Carretera Moncada-Naquera, km 4.5, Moncada, Valencia, 46113, Spain
Laboratorio Internacional de Cambio Global (LINCGlobal), Departamento de Biogeografia y Cambio Global, Museo Nacional de Ciencias Naturales, MNCN, Csic, C/Serrano 115 dpdo, Madrid, 28006, Spain
Sao Paulo State University (Unesp), School of Sciences, Bauru, Brazil
University of Sao Paulo, Institute of Astronomy Geophysics and Atmospheric Sciences, Sao Paulo, Brazil
Efficient Use of Water Program, Institut de Recerca i Tecnologia Agroalimentaries (IRTA), Parc de Gardeny, Edifici Fruitcentre, Lleida, 25003, Spain
AgResearch, Lincoln Research Centre, Private bag 4749, Christchurch, 8140, New Zealand
Basque Centre for Climate Change (BC3), Leioa, 48940, Spain
Basque Foundation for Science, Bilbao, 48008, Spain
School of Geosciences, University of Edinburgh, Edinburgh, United Kingdom
Nrae, Umr Silva 1434, Champenoux, 54280, France
Hawkesbury Institute for the Environment, Western Sydney University, Sydney, NSW, Australia
School of Ecosystem and Forest Sciences, The University of Melbourne, 500 Yarra Boulevard, Richmond, VIC 3121, Australia
Science and Collections Division, Royal Horticultural Society, Wisley, Woking, Surrey, GU23 6QB, United Kingdom
Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, United States
Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umea, Sweden
Section Climate Dynamics and Landscape Evolution, Helmholtz Centre Potsdam, Gfz German Research Centre for Geosciences, Potsdam, 14473, Germany
Irrigation and Crop Ecophysiology Group, Instituto de Recursos Naturales y Agrobiologia de Sevilla (IRNAS, CSIC), Avenida Reina Mercedes, no. 10, Seville, 41012, Spain
Conservation Ecology Center, Smithsonian Conservation Biology Institute, Front Royal, VA, United States
Institute for Atmospheric and Earth System Research/Forest Sciences, Faculty of Agriculture and Forestry, University of Helsinki, Helsinki, Finland
Centro de Ciencias de la Atmosfera, Universidad Nacional Autonoma de Mexico, Mexico City, Mexico
Department of Horticulture, Faculty of Agriculture, Khon Kaen University, Khon Kaen, Thailand
Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Str. 84, Muncheberg, 15374, Germany
Brazilian Platform of Biodiversity and Ecosystem Services/BPBES, Campinas, Brazil
Departamento de Biologia Vegetal, Instituto de Biologia, Universidade Estadual de Campinas, Campinas, Sao Paulo, Brazil
Head Office of Forest Protection, Brandenburg State Forestry Center of Excellence, Eberswalde, 16225, Germany
School of Biological Sciences, University of Auckland, Auckland, New Zealand
Department of Forest Sciences, Seoul National University, Seoul, South Korea
National Center for Agro Meteorology, Seoul, South Korea
Research Institute for Agriculture and Life Sciences, Seoul National University, Seoul, South Korea
Department of Earth Sciences, Gothenburg Univ., Guldhedsgatan 5A, Gothenburg, 405 30, Sweden
Environmental Studies, Hamilton College, Clinton, NY, United States
Geography Department, Colgate University, Hamilton, NY, United States
Department of Physical Geography and Ecosystem Science, Lund University, Lund, Sweden
School of Ecosystem and Forest Sciences, The University of Melbourne, Parkville, VIC 3010, Australia
Landeshauptstadt Munchen, Referat fur Gesundheit und Umwelt, Nachhaltige Entwicklung Umweltplanung, SG Ressourcenschutz, Munich, 80335, Germany
Department of Geography and Planning, University at Albany, Albany, NY, United States
Department of Animal Biology Vegetal Biology and Ecology, University of Jaen, Jaen, Spain
Plant Ecology, University of Goettingen, Gottingen, 37073, Germany
Cefe, Univ Montpellier, Cnrs, Ephe, Ird, Univ Paul Valery Montpellier 3, Montpellier, France
Department of Physical Chemical and Natural Systems, University Pablo de Olavide, Seville, 41013, Spain
Surface Hydrology and Erosion Group, Institute of Environmental Assessment and Water Research, Csic, Barcelona, Spain
Departamento de Agronomia, Universidad de Cordoba, Cordoba, 14071, Spain
Department of Geography, Colgate University, Hamilton, NY, United States
Amap, Univ Montpellier, Cirad, Cnrs, Inrae, Ird, Montpellier, 34000, France
University of Florida, School of Forest Resources and Conservation, 136 Newins-Ziegler Hall, Gainesville, FL 32611, United States
Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, United States
Pacific Northwest National Laboratory, Richland, WA, United States
Center for Tropical Forest Science-Forest Global Earth Observatory, Smithsonian Environmental Research Center, Edgewater, MD 21307, United States
Research School of Biology, Australian National UniversityACT 2601, Australia
Csiro Agriculture and Food, Sandy Bay, TAS 7005, Australia
Dept. of Physical Geography and Ecosystem Science, University of Lund, Lund, Sweden
Faculty of Science and Technology, Free University of Bolzano, Piazza Universita 5, Bolzano, Italy
Forest Services, Autonomous Province of Bolzano, Bolzano, Italy
Department of Ecology and Conservation Biology, Texas AandM University, College Station, TX, United States
Hokkaido Regional Breeding Office, Forest Tree Breeding Center, Forestry and Forest Products Research Institute, Ebetsu, Hokkaido, Japan
School of Natural Resources and the Environment, University of Arizona, Tucson, AZ 85721, United States
Tropical Silviculture and Forest Ecology, University of Goettingen, Busgenweg 1, Gottingen, 37077, Germany
Department of Ecology and Evolutionary Biology, University of Tennessee, Knoxville, TN, United States
O'Neill School of Public and Environmental Affairs, Indiana University-Bloomington, Bloomington, IN, United States
University of Innsbruck, Department of Botany, Sternwartestrasse 15, Innsbruck, 6020, Austria
Eurac Research, Institute for Alpine Environment, Viale Druso 1, Bolzano, Italy
Usda Forest Service, Southern Research Station, Coweeta Hydrologic Laboratory, Otto, NC, United States
Department of Forest Sciences, University of Helsinki, P.O. Box 27, Helsinki, 00014, Finland
Division of Environmental Science and Policy, Nicholas School of the Environment, Department of Civil and Environmental Engineering, Pratt School of Engineering, Duke University, Durham, NC, United States
Institute for Atmospheric and Earth System Research (INAR)/Forest, University of Helsinki, Helsinki, 00014, Finland
Biological Sciences Department, Macquarie University, Sydney, NSW, Australia
National Institute of Agricultural Technology (INTA), Cc 332, Rio Gallegos, Santa Cruz, CP 9400, Argentina
National Scientific and Technical Research Council of Argentina (CONICET), Rio Gallegos, Santa Cruz, Argentina
National University of Southern Patagonia (UNPA), Rio Gallegos, Santa Cruz, Argentina
Laboratory of Plant Ecology, Faculty of Bioscience Engineering, Ghent University, Coupure links 653, Ghent, 9000, Belgium
Urban Studies, School of Social Sciences, Western Sydney University, Locked Bag 1797, Penrith, NSW 2751, Australia
Department of Biology, University of New Mexico, Albuquerque, NM, United States
The Earth and Planetary Science Department, Weizmann Institute of Science, Rehovot, Israel
University of Cologne, Faculty of Medicine, University Hospital Cologne, Cologne, Germany
Department of Biological Science, University at Albany, Albany, NY, United States
Laboratorio de Clima e Biosfera, Instituto de Astronomia Geofisica e Ciencias Atmosfericas, Universidade de Sao Paulo, Sao Paulo, Brazil
Department of Ecology, Ibrag, Universidade Do Estado Do Rio de Janeiro (UERJ), R. Sao Francisco Xavier, 524, PHLC, Sala 220, Maracana, Rio de Janeiro, RJ, CEP 20550900, Brazil
College of Life and Environmental Sciences, University of Exeter, Laver Building, North Park Road, Exeter, EX4 4QE, United Kingdom
Laboratory for Complex Studies of Forest Dynamics in Eurasia, Siberian Federal University, Akademgorodok 50A-K2, Krasnoyarsk, Russian Federation
Department of Evolutionary Biology Ecology, and Environmental Sciences, University of Barcelona (UB), Barcelona, 08028, Spain
Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, Helsinki, 00014, Finland
Forest Genetics and Ecophysiology Research Group, Universidad Politecnica de Madrid, Ciudad Universitaria s/n, Madrid, 28040, Spain
Laboratory of Plant Ecology, Faculty of Bioscience Engineering, Ghent University, Ghent, 9000, Belgium
Irta, Institute of Agrifood Research and Technology, Torre Marimon, Caldes de Montbui, Barcelona, 08140, Spain
Earth and Environmental Science Department, Rutgers University Newark, 195 University Av, Newark, NJ 07102, United States
University of Wurzburg, Julius-von-Sachs-Institute for Biological Sciences, Chair of Ecophysiology and Vegetation Ecology, Julius-von-Sachs-Platz 3, Wurzburg, 97082, Germany
Sukachev Institute of Forest of the Siberian Branch of the Ras, Krasnoyarsk, Russian Federation
Umr EcoFoG, Cnrs, Cirad, Inrae, AgroParisTech, Universite des Antilles, Universite de Guyane, Kourou97310, France
Global Change Research Institute of the Czech Academy of Sciences, Blidla 4a, Brno, 60300, Czech Republic
Centro de Investigaciones Amazonicas Cimaz Macagual Cesar Augusto Estrada Gonzalez, Grupo de Investigaciones Agroecosistemas y Conservacion en Bosques Amazonicos-GAIA, Florencia, Caqueta, Colombia
Universidad de la Amazonia, Programa de Ingenieria Agroecologica, Facultad de Ingenieria, Florencia, Caqueta, Colombia
Institute of Hydrodynamics, Czech Academy of Sciences, Prague, Czech Republic
Trier University, Faculty of Regional and Environmental Sciences, Geobotany, Behringstr. 21, Trier, 54296, Germany
Department of Environmental Science, Faculty of Science, Chulalongkorn University, Bangkok, 10330, Thailand
Environment Health and Social Data Analytics Research Group, Chulalongkorn University, Bangkok, 10330, Thailand
Water Science and Technology for Sustainable Environment Research Group, Chulalongkorn University, Bangkok, 10330, Thailand
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Departamento de Biologia y Geologia, Escuela Superior de Ciencias Experimentales y Tecnolo Gicas, Universidad Rey Juan Carlos, C/Tulipan s/n, Mostoles, 28933, Spain
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Department of Geography Hydrology and Climate, University of Zurich, Winterthurerstrasse 190, Zurich, 8057, Switzerland
A.N. Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Leninsky pr.33, Moscow, 119071, Russian Federation
Zef Center for Development Research, University of Bonn, Genscherallee 3, Bonn, 53113, Germany
Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, United States
Ecosystem Physiology, University of Freiburg, Freiburg, 79098, Germany
Geobotany Department, University of Trier, Trier, 54286, Germany
Division of Alpine Timberline Ecophysiology, Federal Research and Training Centre for Forests, Natural Hazards and Landscape (BFW), Rennerg 1, Innsbruck, 6020, Austria
Inrae, Umr Ispa 1391, Villenave D'Ornon, 33140, France
Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, United States
Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, United States
O'Neill School of Public and Environmental Affairs, Indiana University Bloomington, Bloomington, IN 47405, United States
Swiss Federal Institute for Forest, Snow and Landscape Research Wsl, Birmensdorf, Switzerland
Icrea, Barcelona, Catalonia, Spain

Доп.точки доступа:
Poyatos, R.; Granda, V.; Flo, V.; Adams, M. A.; Adorjan, B.; Aguade, D.; Aidar, M. P.M.; Allen, S.; Alvarado-Barrientos, M. S.; Anderson-Teixeira, K. J.; Aparecido, L. M.; Altaf Arain, M.; Aranda, I.; Asbjornsen, H.; Baxter, R.; Beamesderfer, E.; Berry, Z. C.; Berveiller, D.; Blakely, B.; Boggs, J.; Bohrer, G.; Bolstad, P. V.; Bonal, D.; Bracho, R.; Brito, P.; Brodeur, J.; Casanoves, F.; Chave, J.; Chen, H.; Cisneros, C.; Clark, K.; Cremonese, E.; Dang, H.; David, J. S.; David, T. S.; Delpierre, N.; Desai, A. R.; Do, F. C.; Dohnal, M.; Domec, J. -C.; Dzikiti, S.; Edgar, C.; Eichstaedt, R.; El-Madany, T. S.; Elbers, J.; Eller, C. B.; Euskirchen, E. S.; Ewers, B.; Fonti, P.; Forner, A.; Forrester, D. I.; Freitas, H. C.; Galvagno, M.; Garcia-Tejera, O.; Ghimire, C. P.; Gimeno, T. E.; Grace, J.; Granier, A.; Griebel, A.; Guangyu, Y.; Gush, M. B.; Hanson, P. J.; Hasselquist, N. J.; Heinrich, I.; Hernandez-Santana, V.; Herrmann, V.; Holtta, T.; Holwerda, F.; Irvine, J.; Na Ayutthaya, S. I.; Jarvis, P. G.; Jochheim, H.; Joly, C. A.; Kaplick, J.; Kim, H. S.; Klemedtsson, L.; Kropp, H.; Lagergren, F.; Lane, P.; Lang, P.; Lapenas, A.; Lechuga, V.; Lee, M.; Leuschner, C.; Limousin, J. -M.; Linares, J. C.; Linderson, M. -L.; Lindroth, A.; Llorens, P.; Lopez-Bernal, A.; Loranty, M. M.; Luttschwager, D.; MacInnis-Ng, C.; Marechaux, I.; Martin, T. A.; Matheny, A.; McDowell, N.; McMahon, S.; Meir, P.; Meszaros, I.; Migliavacca, M.; Mitchell, P.; Molder, M.; Montagnani, L.; Moore, G. W.; Nakada, R.; Niu, F.; Nolan, R. H.; Norby, R.; Novick, K.; Oberhuber, W.; Obojes, N.; Oishi, A. C.; Oliveira, R. S.; Oren, R.; Ourcival, J. -M.; Paljakka, T.; Perez-Priego, O.; Peri, P. L.; Peters, R. L.; Pfautsch, S.; Pockman, W. T.; Preisler, Y.; Rascher, K.; Robinson, G.; Rocha, H.; Rocheteau, A.; Roll, A.; Rosado, B. H.P.; Rowland, L.; Rubtsov, A. V.; Sabate, S.; Salmon, Y.; Salomon, R. L.; Sanchez-Costa, E.; Schafer, K. V.R.; Schuldt, B.; Shashkin, A.; Stahl, C.; Stojanovic, M.; Suarez, J. C.; Sun, G.; Szatniewska, J.; Tatarinov, F.; TesaA™, M.; Thomas, F. M.; Tor-Ngern, P.; Urban, J.; Valladares, F.; Van Der Tol, C.; Van Meerveld, I.; Varlagin, A.; Voigt, H.; Warren, J.; Werner, C.; Werner, W.; Wieser, G.; Wingate, L.; Wullschleger, S.; Yi, K.; Zweifel, R.; Steppe, K.; Mencuccini, M.; Martinez-Vilalta, J.

/ R. Poyatos, V. Granda, V. Flo [et al.] // Earth Syst. Sci. Data. - 2021. - Vol. 13, Is. 6. - P2607-2649, DOI 10.5194/essd-13-2607-2021. - Cited References:169. - This research was supported by the Ministerio de Economia y Competitividad (grant no. CGL2014-55883-JIN), the Ministerio de Ciencia e Innovacion (grant no. RTI2018-095297-J-I00), the Ministerio de Ciencia e Innovacion (grant no. CAS16/00207), the Agencia de Gestio d'Ajuts Universitaris i de Recerca (grant no. SGR1001), the Alexander von Humboldt-Stiftung (Humboldt Research Fellowship for Experienced Researchers (RP)), and the Institucio Catalana de Recerca i Estudis Avancats (Academia Award (JMV)). Victor Flo was supported by the doctoral fellowship FPU15/03939 (MECD, Spain). . - ISSN 1866-3508. - ISSN 1866-3516РУБ Geosciences, Multidisciplinary + Meteorology & Atmospheric Sciences

Аннотация: Plant transpiration links physiological responses of vegetation to water supply and demand with hydrological, energy, and carbon budgets at the land-atmosphere interface. However, despite being the main land evaporative flux at the global scale, transpiration and its response to environmental drivers are currently not well constrained by observations. Here we introduce the first global compilation of whole-plant transpiration data from sap flow measurements (SAPFLUXNET, https://sapfluxnet.creaf.cat/, last access: 8 June 2021). We harmonized and quality-controlled individual datasets supplied by contributors worldwide in a semi-automatic data workflow implemented in the R programming language. Datasets include sub-daily time series of sap flow and hydrometeorological drivers for one or more growing seasons, as well as metadata on the stand characteristics, plant attributes, and technical details of the measurements. SAPFLUXNET contains 202 globally distributed datasets with sap flow time series for 2714 plants, mostly trees, of 174 species. SAPFLUXNET has a broad bioclimatic coverage, with woodland/shrubland and temperate forest biomes especially well represented (80 % of the datasets). The measurements cover a wide variety of stand structural characteristics and plant sizes. The datasets encompass the period between 1995 and 2018, with 50 % of the datasets being at least 3 years long. Accompanying radiation and vapour pressure deficit data are available for most of the datasets, while on-site soil water content is available for 56 % of the datasets. Many datasets contain data for species that make up 90 % or more of the total stand basal area, allowing the estimation of stand transpiration in diverse ecological settings. SAPFLUXNET adds to existing plant trait datasets, ecosystem flux networks, and remote sensing products to help increase our understanding of plant water use, plant responses to drought, and ecohydrological processes. SAPFLUXNET version 0.1.5 is freely available from the Zenodo repository (https://doi.org/10.5281/zenodo.3971689; Poyatos et al., 2020a). The "sapfluxnetr" R package - designed to access, visualize, and process SAPFLUXNET data - is available from CRAN.

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CREAF, E-08193 Catalonia, Cerdanyola Del, Spain.
Univ Autonoma Barcelona, E-08193 Catalonia, Cerdanyola Del, Spain.
Joint Res Unit CREAF CTFC, Bellaterra, Catalonia, Spain.
Swinburne Univ Technol, Fac Sci Engn & Technol, Hawthorn, Vic 3122, Australia.
Univ Sydney, Sch Life & Environm Sci, Camperdown, NSW, Australia.
Univ Debrecen, Fac Sci & Technol, Dept Bot, Egyet Ter 1, H-4032 Debrecen, Hungary.
Inst Bot, Plant Physiol & Biochem, Sao Paulo, Brazil.
Univ Nevada, Dept Nat Resources & Environm Sci, Reno, NV 89557 USA.
Inst Ecolog AC, Red Ecolog Func, Xalapa, Veracruz, Mexico.
Smithsonian Trop Res Inst, Ctr Trop Forest Sci Forest Global Earth Observ, Panama City, Panama.
Smithsonian Conservat Biol Inst, Conservat Ecol Ctr, Front Royal, VA USA.
Texas A&M Univ, Dept Ecosyst Sci & Management, College Stn, TX USA.
Arizona State Univ, Sch Earth & Space Explorat, Tempe, AZ USA.
McMaster Univ, Sch Earth Environm & Soc, Hamilton, ON, Canada.
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Natl Inst Agr & Food Res & Technol INIA, Forest Res Ctr CIFOR, Dept Forest Ecol & Genet, Avda A Coruna Km 7-5, Madrid 28040, Spain.
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McMaster Univ, Sch Geog & Earth Sci, Hamilton, ON, Canada.
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Univ Lorraine, AgroParisTech, INRAE, F-54000 Nancy, France.
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Max Planck Inst Biogeochem, Hans Knoll Str 10, Jena, Germany.
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Univ Trier, Geobot Dept, D-54286 Trier, Germany.
Fed Res & Training Ctr Forests Nat Hazards & Land, Div Alpine Timberline Ecophysiol, Rennerg 1, A-6020 Innsbruck, Austria.
INRAE, UMR ISPA 1391, F-33140 Villenave Dornon, France.
Univ Virginia, Dept Environm Sci, Charlottesville, VA 22904 USA.
ICREA, Barcelona, Catalonia, Spain.

Доп.точки доступа:
Poyatos, Rafael; Granda, Victor; Flo, Victor; Adams, Mark A.; Adorjan, Balazs; Aguade, David; Aidar, Marcos P. M.; Allen, Scott; Alvarado-Barrientos, K. J.; Anderson-Teixeira, Kristina J.; Aparecido, Luiza Maria; Arain, M. Altaf; Aranda, Ismael; Asbjornsen, Heidi; Baxter, Robert; Beamesderfer, Eric; Berry, Z. Carter; Berveiller, Daniel; Blakely, Bethany; Boggs, Johnny; Bohrer, Gil; Bolstad, Paul, V; Bonal, Damien; Bracho, Rosvel; Brito, Patricia; Brodeur, Jason; Casanoves, Fernando; Chave, Jerome; Chen, Hui; Cisneros, Cesar; Clark, Kenneth; Cremonese, Edoardo; Dang, Hongzhong; David, Jorge S.; David, Teresa S.; Delpierre, Nicolas; Desai, Ankur R.; Do, Frederic C.; Dohnal, Michal; Domec, Jean-Christophe; Dzikiti, Sebinasi; Edgar, Colin; Eichstaedt, Rebekka; El-Madany, Tarek S.; Elbers, Jan; Eller, Cleiton B.; Euskirchen, Eugenie S.; Ewers, Brent; Fonti, Patrick; Forner, Alicia; Forrester, David, I; Freitas, Helber C.; Galvagno, Marta; Garcia-Tejera, Omar; Ghimire, Chandra Prasad; Gimeno, Teresa E.; Grace, John; Granier, Andre; Griebel, Anne; Guangyu, Yan; Gush, Mark B.; Hanson, Paul J.; Hasselquist, Niles J.; Heinrich, Ingo; Hernandez-Santana, Virginia; Herrmann, Valentine; Holtta, Teemu; Holwerda, Friso; Irvine, James; Ayutthaya, Supat Isarangkool Na; Jarvis, Paul G.; Jochheim, Hubert; Joly, Carlos A.; Kaplick, Julia; Kim, Hyun Seok; Klemedtsson, Leif; Kropp, Heather; Lagergren, Fredrik; Lane, Patrick; Lang, Petra; Lapenas, Andrei; Lechuga, Victor; Lee, Minsu; Leuschner, Christoph; Limousin, Jean-Marc; Linares, Juan Carlos; Linderson, Maj-Lena; Lindroth, Anders; Llorens, Pilar; Lopez-Bernal, Alvaro; Loranty, Michael M.; Luttschwager, Dietmar; Macinnis-Ng, Cate; Marechaux, Isabelle; Martin, Timothy A.; Matheny, Ashley; McDowell, Nate; McMahon, Sean; Meir, Patrick; Meszaros, Ilona; Migliavacca, Mirco; Mitchell, Patrick; Molder, Meelis; Montagnani, Leonardo; Moore, Georgianne W.; Nakada, Ryogo; Niu, Furong; Nolan, Rachael H.; Norby, Richard; Novick, Kimberly; Oberhuber, Walter; Obojes, Nikolaus; Oishi, A. Christopher; Oliveira, Rafael S.; Oren, Ram; Ourcival, Jean-Marc; Paljakka, Teemu; Perez-Priego, Oscar; Peri, Pablo L.; Peters, Richard L.; Pfautsch, Sebastian; Pockman, William T.; Preisler, Yakir; Rascher, Katherine; Robinson, George; Rocha, Humberto; Rocheteau, Alain; Roll, Alexander; Rosado, Bruno H. P.; Rowland, Lucy; Rubtsov, Alexey, V; Sabate, Santiago; Salmon, Yann; Salomon, Roberto L.; Sanchez-Costa, Elisenda; Schafer, Karina V. R.; Schuldt, Bernhard; Shashkin, Alexandr; Stahl, Clement; Stojanovic, Marko; Suarez, Juan Carlos; Sun, G.e.; Szatniewska, Justyna; Tatarinov, Fyodor; Tesar, Miroslav; Thomas, Frank M.; Tor-ngern, Pantana; Urban, Josef; Valladares, Fernando; van der Tol, Christiaan; van Meerveld, Ilja; Varlagin, Andrej; Voigt, Holm; Warren, Jeffrey; Werner, Christiane; Werner, Willy; Wieser, Gerhard; Wingate, Lisa; Wullschleger, Stan; Yi, Koong; Zweifel, Roman; Steppe, Kathy; Mencuccini, Maurizio; Martinez-Vilalta, Jordi; David, Jorge; David, Teresa Soares; R., Ram; Ministerio de Economia y CompetitividadSpanish Government [CGL2014-55883-JIN]; Ministerio de Ciencia e InnovacionInstituto de Salud Carlos IIISpanish GovernmentEuropean Commission [CAS16/00207, RTI2018-095297-J-I00]; Agencia de Gestio d'Ajuts Universitaris i de RecercaAgencia de Gestio D'Ajuts Universitaris de Recerca Agaur (AGAUR) [SGR1001]; Alexander von Humboldt-StiftungAlexander von Humboldt Foundation; Institucio Catalana de Recerca i Estudis AvancatsICREA; MECD, Spain [FPU15/03939]

[Текст] / И. А. Петров, А. С. Шушпанов, А. С. Голюков, М. Л. Двинская, В. И. Харук // Сибирский экологический журнал. - 2023. - Т. 30, № 1. - С. 46-59, DOI 10.15372/SJFS20220401 . - ISSN 0869-8619

ГРНТИ

68

68.47.41

Аннотация: Изменения климата влекут возрастание горимости лесов во всей бореальной зоне. Исследована многолетняя динамика горимости в сосняках Средней Сибири, зависимость частоты возгораний и площади гарей от эколого-климатических переменных, а также послепожарная динамика продуктивности растительного покрова. Методически работа основана на сопряженном анализе результатов наземных обследований, материалов дистанционного зондирования (спектрорадио- и гравиметрическая съемки спутниками Terra/MODIS и GRACE) и дендроэкологических данных. В период с XVIII по XX в. выявлено снижение величины межпожарных интервалов с 33 лет до 20-25 лет. Хотя значимых трендов горимости в текущем столетии не выявлено, во втором его десятилетии наблюдались катастрофические (более 1 млн га) пожары, а также зафиксировано значительное возрастание числа возгораний и площади гарей (в 3,5 и 3,0 раза соответственно). Отмечено, что частота пожаров и площадь гарей тесно связаны с условиями увлажнения и температурным режимом в период, предшествующий возникновению пожара. Вместе с тем величины корреляций параметров горимости с условиями увлажнения (сумма осадков, влажность напочвенного покрова и почвогрунтов, индекс засушливости scPDSI) выше, чем с температурой воздуха. Показано, что определение влажности почвогрунтов методами гравиметрии применимо в оценке риска возникновения лесных пожаров. Установлен высокий уровень корреляции между индексом прироста деревьев сосны и индексами продуктивности растительного покрова (валовая (GPP) и чистая (NPP) продуктивность), генерируемыми по данным дистанционного зондирования. Полученный результат подтверждает применимость указанных индексов в исследованиях динамики продуктивности древостоев. Продуктивность растительного покрова на гарях, а также величина индекса радиального прироста деревьев сосны быстро (в течение примерно десятилетия) восстанавливается до предпожарных величин, что говорит о сохранении северными сосняками углерод-депонирующей функции в условиях меняющегося климата и возрастающей горимости лесов
Climate changes entails an increase in the forests burning throughout the whole boreal zone. We have studied the long-term dynamics of fire rate and post-fire recovery of vegetation cover productivity in the pine forests of Central Siberia, and analyzed the dependences of the fire frequency and the burnt areas on climatic variables. Methodically, the work is based on a combined analysis of data from ground surveys, remote sensing (spectroradiometric and gravimetric surveys by Terra / MODIS and GRACE satellites), and coupled analysis of dendroecological data and environmental and climatic variables. The main impact on the fire frequency and burnt areas is due to the moistening conditions (total precipitation, soil moisture, aridity index scPDSI) in the period preceding the fire. The correlations of combustibility parameters with air temperature are lower than with humidification conditions. It is shown that soil moisture gravimetry data can be used in assessing the risk of forest fires. A decrease of fire Return intervals from 33 years to 20-25 years in the period from the 18th to the 20th century was revealed. In the second decade of the 21st century, both catastrophic (more than 1 million ha) forest fires and a significant increase in flammability were observed: the number of fires and the area of burnt areas increased, respectively, by 3.5 and 3.0 times. A high level of correlation has been determined between the growth index of pine trees and the vegetation cover productivity indices (gross (GPP) and net (NPP) productivity) generated from remote sensing data. The result obtained indicates the applicability of the indices in the studies of the forest stands productivity. Significant trends in flammability in the 21st century, both in terms of the frequency of fires and the areas covered by fire, have not been identified. The productivity of the vegetative cover on burnt areas, as well as the value of the index of radial increment of pine trees, quickly (within ~ a decade) recovers to pre-fire values, which indicates that northern pine forests retain their carbon-storing function under conditions of climate change and increased fire rate.

РИНЦ

Держатели документа:
ИЛ СО РАН : 660036, Красноярск, Академгородок, 50, стр. 28

Доп.точки доступа:
Шушпанов, Александр Сергеевич; SHUSHPANOV A.S.; Голюков, А.С.; Двинская, Мария Леонидовна; Dvinskaya, Mariya Leonidovna; Харук, Вячеслав Иванович; Petrov I.A.