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12. The concept of vegetation classification of Russia as an image of contemporary tasks of phytocoenology

Author

Plugatar, Yu. V., primary, Ermakov, N. B., additional, Krestov, P.V., additional, Matveyeva, N. V., additional, Martynenko, V. B., additional, Golub, V. B., additional, Neshataeva, V. Yu., additional, Neshataev, V. Yu., additional, Anenkhonov, O. A., additional, Lavrinenko, I. A., additional, Lavrinenko, O. V., additional, Chepinoga, V. V., additional, Sinelnikova, N. V., additional, Morozova, O. V., additional, Belonovskaya, E. A., additional, Tishkov, A. A., additional, Chernenkova, T. V., additional, Krivobokov, L. V., additional, Telyatnikov, M. Yu., additional, Lapshina, E. D., additional, Koroleva, N. E., additional, Cherosov, M. M., additional, Semenishchenkov, Yu. A., additional, Abramova, L. M., additional, Lysenko, T. M., additional, and Polyakova, M. A., additional

Published
2020
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16. Circumpolar Arctic Vegetation Classification

Author

Walker, D. A., Daniëls, F. J. A., Matveyeva, N. V., Šibík, J., Walker, M. D., Breen, A. L., Druckenmiller, L. A., Raynolds, M. K., Bültmann, H., Hennekens, S., Buchhorn, M., Epstein, H. E., Ermokhina, K., Fosaa, A. M., Heidmarsson, S., Heim, B., Jónsdóttir, I. S., Koroleva, N., Lévesque, E., MacKenzie, W. H., Henry, G. H. R., Nilsen, L., Peet, R., Razzhivin, V., Talbot, S. S., Telyatnikov, M., Thannheiser, D., Webber, P. J., Wirth, L. M., Walker, D. A., Daniëls, F. J. A., Matveyeva, N. V., Šibík, J., Walker, M. D., Breen, A. L., Druckenmiller, L. A., Raynolds, M. K., Bültmann, H., Hennekens, S., Buchhorn, M., Epstein, H. E., Ermokhina, K., Fosaa, A. M., Heidmarsson, S., Heim, B., Jónsdóttir, I. S., Koroleva, N., Lévesque, E., MacKenzie, W. H., Henry, G. H. R., Nilsen, L., Peet, R., Razzhivin, V., Talbot, S. S., Telyatnikov, M., Thannheiser, D., Webber, P. J., and Wirth, L. M.

Abstract

Aims: An Arctic Vegetation Classification (AVC) is needed to address issues related to rapid Arctic-wide changes to climate, land-use, and biodiversity. Location: The 7.1 million km2 Arctic tundra biome. Approach and conclusions: The purpose, scope and conceptual framework for an Arctic Vegetation Archive (AVA) and Classification (AVC) were developed during numerous workshops starting in 1992. The AVA and AVC are modeled after the European vegetation archive (EVA) and classification (EVC). The AVA will use Turboveg for data management. The AVC will use a Braun-Blanquet (Br.-Bl.) classification approach. There are approximately 31,000 Arctic plots that could be included in the AVA. An Alaska AVA (AVA-AK, 24 datasets, 3026 plots) is a prototype for archives in other parts of the Arctic. The plan is to eventually merge data from other regions of the Arctic into a single Turboveg v3 database. We present the pros and cons of using the Br.-Bl. classification approach compared to the EcoVeg (US) and Biogeoclimatic Ecological Classification (Canada) approaches. The main advantages are that the Br.-Bl. approach already has been widely used in all regions of the Arctic, and many described, well-accepted vegetation classes have a pan-Arctic distribution. A crosswalk comparison of Dryas octopetala communities described according to the EcoVeg and the Braun-Blanquet approaches indicates that the non-parallel hierarchies of the two approaches make crosswalks difficult above the plantcommunity level. A preliminary Arctic prodromus contains a list of typical Arctic habitat types with associated described syntaxa from Europe, Greenland, western North America, and Alaska. Numerical clustering methods are used to provide an overview of the variability of habitat types across the range of datasets and to determine their relationship to previously described Braun-Blanquet syntaxa. We emphasize the need for continued maintenance of the Pan-Arctic Species List, and additional plot data to

Published
2018

17. Forming of the professional competence of the future teacher in the process of preparation of the master: theoretical analysis of the problem

Author

Matveyeva, N. and Matishak, M.

Subjects
професійна компетентність, професійна підготовка, professional formation, професійне становлення, skills, professional competence, self-development, саморозвиток, professional training, професійна мобільність, professional mobility, майстерність
Abstract

У статті автори виокремлюють основні завдання освітньої галузі на сучасному етапі, наголошуючи на потребі підготовки висококваліфікованих педагогічних кадрів. Під час навчання в магістратурі формуються професійні риси, якості та вміння, удосконалюється майстерність майбутнього педагога. Метою статті є теоретичне обґрунтування та вивчення ефективності науково-педагогічних умов формування професійної компетентності майбутніх педагогів у процесі магістерської підготовки. Для підвищення якості навчання необхідно реформувати освітній процес вищого навчального закладу, підвищити якість навчання, створити науково-педагогічні умови, які б забезпечили високу ефективність професійної підготовки майбутніх магістрів. Автори стверджують, що особливе місце у навчально-виховному процесі набуває компетентнісний підхід, що дозволяє формувати професійно мобільного фахівця з високим загальним, культурним та професійним рівнем, готового до змін, систематичного самовдосконалення та самореалізації. In the article, the authors singled out the main tasks of the educational branch at the present stage, stressing the need for the training of highly skilled pedagogical staff. It is emphasized that formation of professional competence is one of the priorities of the national education system. The purpose of the article is to substantiate theoretically and to explore the effectiveness of scientific and pedagogical conditions of formation of future teachers’ professional competence. The essence of such concepts as «professional mobility», «professional competence» and «self-development» has been grounded in the article. The authors analyzed scientific psychological, pedagogical and methodological literature concerning the disclosure of these concepts. The article is a consideration of various points of view and scientific positions on the problem of professional competence formation in students at higher educational institutions from the vantage point of the competency-based approach. It presents and generalizes the content of the main notions in the terminological apparatus of the competency-based approach and ways of professional competence formation in students as a result of their professional preparation. The authors argue that a special place in the educational process acquires a competent approach that allows the formation of a professionally mobile specialist with a high general, cultural and professional level, ready for change, systematic self-improvement and self-realization.

Published
2017

20. Recent circum-Arctic ice-wedge degradation and its hydrological impacts

Author

Liljedahl, A. K., Boike, Julia, Daanen, R. P., Fedorov, A.N., Frost, G.V., Grosse, Guido, Hinzman, L.D., Iijima, Y., Jorgenson, J.C., Matveyeva, N., Necsoiu, M., Raynolds, M., Romanovsky, V., Schulla, J., Tape, K.D., Walker, D.A., Wilson, C. J., Yabuki, H., Liljedahl, A. K., Boike, Julia, Daanen, R. P., Fedorov, A.N., Frost, G.V., Grosse, Guido, Hinzman, L.D., Iijima, Y., Jorgenson, J.C., Matveyeva, N., Necsoiu, M., Raynolds, M., Romanovsky, V., Schulla, J., Tape, K.D., Walker, D.A., Wilson, C. J., and Yabuki, H.

Abstract

Ice-wedges are common permafrost features formed over hundreds to thousands of years of repeated frost cracking and ice vein growth. We used field and remote sensing observations to assess changes in areas dominated by ice-wedges, and we simulated the effects of those changes on snow accumulation and runoff. We show that top melting of ice-wedges and subsequent ground subsidence has occurred at multiple sites in the North American and Russian Arctic. At most sites, melting ice-wedges have initially resulted in increased wetness contrast across the landscape, evident as increased surface water in the ice-wedge polygon troughs and somewhat drier polygon centers. Most areas are becoming more heterogeneous with wetter troughs, more small ponds (themokarst pits forming initially at ice-wedge intersections and then spreading along the troughs) and drier polygon centers. Some areas with initial good drainage, such as near creeks, lake margins, and in hilly terrain, highcentered polygons form an overall landscape drying due to a drying of both polygon centers and troughs. Unlike the multi-decadal warming observed in permafrost temperatures, the ice-wedge melting that we observed appeared as a sub-decadal response, even at locations with low mean annual permafrost temperatures (down to -14 °C). Gradual long-term air and permafrost warming combined with anomalously warm summers or deep snow winters preceded the onset of the ice-wedge melting. To assess hydrological impacts of ice-wedge melting, we simulated tundra water balance before and after melting. Our coupled hydrological and thermal model experiments applied over hypothetical polygon surfaces suggest that 1. ice-wedge melting that produces a connected trough-network reduces inundation and increases runoff, and that 2. changing patterns of snow distribution due to differential ground subsidence has a major control on ice-wedge polygon tundra water balance despite an identical snow water equivalent at the landscape-scale

Published
2016

24. In memory of Rudolf Vladimirovich Kamelin (1938–2016)

Author

Galanina, O. V., primary, Gannibal, B. K., additional, Zanokha, L. L., additional, Matveyeva, N. V., additional, Neshatayeva, V. Yu., additional, Sekretareva, N. A., additional, Sumerina, I. Yu., additional, Khramtsov, V. N., additional, and Shchukina, K. V., additional

Published
2016
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25. Ice wedge degradation: Why Arctic lowlands are becoming wetter and drier

Author

Liljedahl, Anna K., Boike, Julia, Daanen, R. P., Fedorov, A., Frost, Gerald, Grosse, Guido, Hinzman, L., Iijima, Yoshihiro, Jorgenson, Janet, Matveyeva, N. V., Necsoiu, M., Raynolds, Martha K., Romanovsky, V. E., Schulla, J., Tape, Ken, Walker, Donald A., Wilson, Cathy, Yabuki, H, Liljedahl, Anna K., Boike, Julia, Daanen, R. P., Fedorov, A., Frost, Gerald, Grosse, Guido, Hinzman, L., Iijima, Yoshihiro, Jorgenson, Janet, Matveyeva, N. V., Necsoiu, M., Raynolds, Martha K., Romanovsky, V. E., Schulla, J., Tape, Ken, Walker, Donald A., Wilson, Cathy, and Yabuki, H

Abstract

Top melting of ice-wedges and subsequent ground subsidence is now a widespread phenomenon across the Arctic domain. We show field and remote sensing observations that document extensive ice-wedge degradation, which initially has resulted in increased wetness contrast across the landscape (i.e. both a drying and a wetting), a shift in pond type and an overall drying in later stages. The differential ground subsidence at cold continuous permafrost regions appear to be linked to press and pulse climate forcing. Here, the process of crossing the local threshold for ice-wedge stability may be favored by a press occurrence such as long-term, gradual increases in summer air temperature, mean annual air temperature and/or possibly winter precipitation, but our observations suggest it is most likely initiated by pulse atmospheric forcing such as extreme summer warmth and/or winter precipitation. Field measurements of water levels, frost tables and snow accumulation across the main ice-wedge polygon types and their respective features support dramatic shifts in the hydrologic regime with altered topography and a complexity that ultimately affect the larger-scale hydrologic system. For example, our numerical model experiments show that a connected trough-network reduces inundation and increases runoff and that changing patterns of snow distribution due to the differential ground subsidence play a crucial role in altering lowland tundra water balance. These fine-scale (10’s cm) geomorphic changes are expected to further expand and amplify in rapidly warming permafrost regions and likely will dramatically modify land-atmosphere and land-ocean fluxes and exchange of carbon, water, and energy.

Published
2015

26. Arctic Terrestrial Ecosystems

Author

Callaghan, T.V., Matveyeva, N., Chernov, Y., Schmidt, Niels Martin, Brooker, R., Johansson, M., and Levin, S.A.

Published
2013

31. Climate change and Arctic ecosystems: I. Vegetation changes north of 55 degrees N between the last glacial maximum, mid-Holocene, and present

Author

Bigelow, N., Brubaker, L., Edwards, M., Harrison, S., Prentice, I., Anderson, P., Andreev, A., Bartlein, P., Christensen, T., Cramer, W., Kaplan, J., Lozhkin, A., Matveyeva, N., Murray, D., Mcguire, A., Razzhivin, V., Ritchie, J., Smith, B., Walker, D., Gajewski, K., Wolf, V., Holmqvist, B., Igarashi, Y., Kremenetskii, K., Paus, A., Pisaric, M., and Volkova, V.

Abstract

[1] A unified scheme to assign pollen samples to vegetation types was used to reconstruct vegetation patterns north of 55degreesN at the last glacial maximum (LGM) and mid-Holocene (6000 years B. P.). The pollen data set assembled for this purpose represents a comprehensive compilation based on the work of many projects and research groups. Five tundra types (cushion forb tundra, graminoid and forb tundra, prostrate dwarf-shrub tundra, erect dwarf-shrub tundra, and low- and high-shrub tundra) were distinguished and mapped on the basis of modern pollen surface samples. The tundra-forest boundary and the distributions of boreal and temperate forest types today were realistically reconstructed. During the mid-Holocene the tundra-forest boundary was north of its present position in some regions, but the pattern of this shift was strongly asymmetrical around the pole, with the largest northward shift in central Siberia (similar tO200 km), little change in Beringia, and a southward shift in Keewatin and Labrador (similar tO200 km). Low- and high-shrub tundra extended farther north than today. At the LGM, forests were absent from high latitudes. Graminoid and forb tundra abutted on temperate steppe in northwestern Eurasia while prostrate dwarf-shrub, erect dwarf-shrub, and graminoid and forb tundra formed a mosaic in Beringia. Graminoid and forb tundra is restricted today and does not form a large continuous biome, but the pollen data show that it was far more extensive at the LGM, while low- and high-shrub tundra were greatly reduced, illustrating the potential for climate change to dramatically alter the relative areas occupied by different vegetation types.

Published
2003

32. Multi-decadal changes in tundra environments and ecosystems: Synthesis of the International Polar Year-Back to the Future Project (IPY-BTF).

Author

Callaghan, T.V., Tweedie, G.E., Kerman, J.A., Andrews, C., Bergstedt, J., Butler, M.G., Christensen, T.R., Cooley, D., Dahlberg, U., Danby, R.K., Daniels, F.J.A., de Molenaar, J.G.., Dick, J., Mortensen, C.E., Ebert-May, D., Emanuelsson, U., Hedena, E.H., Henry, G.H.R., Hik, D.S., Hobbie, J.E., Jantze, E.J., Jaspers, C., Johansson, M., Johnson, D.R., Johnstone, J.F., Jonasson, C., Kennedy, C., Kenney, A.J., Keuper, F., Koh S. Krebs, C.J., Lantuit, H., Lara, M.J., Lin, D., Lougheed, V.L., Madsen, J., Matveyeva, N., McEwen, D.C., Myers-Smith, I.H., Narozhniy, Y.K., Olsson, H., Pohjola, V.A., Price, L.W., Riget, F., Rundqvist, S., Sandstrom, A., Tamstorf, M., van Bogaert, R., Villarreal, S., Webber, P.J., Zemtsov, V.A., Callaghan, T.V., Tweedie, G.E., Kerman, J.A., Andrews, C., Bergstedt, J., Butler, M.G., Christensen, T.R., Cooley, D., Dahlberg, U., Danby, R.K., Daniels, F.J.A., de Molenaar, J.G.., Dick, J., Mortensen, C.E., Ebert-May, D., Emanuelsson, U., Hedena, E.H., Henry, G.H.R., Hik, D.S., Hobbie, J.E., Jantze, E.J., Jaspers, C., Johansson, M., Johnson, D.R., Johnstone, J.F., Jonasson, C., Kennedy, C., Kenney, A.J., Keuper, F., Koh S. Krebs, C.J., Lantuit, H., Lara, M.J., Lin, D., Lougheed, V.L., Madsen, J., Matveyeva, N., McEwen, D.C., Myers-Smith, I.H., Narozhniy, Y.K., Olsson, H., Pohjola, V.A., Price, L.W., Riget, F., Rundqvist, S., Sandstrom, A., Tamstorf, M., van Bogaert, R., Villarreal, S., Webber, P.J., and Zemtsov, V.A.

Published
2011
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33. Holographic nanointerferometer with digital magnification

Author

Pulkin, S. A., primary, Venediktov, V. Yu., additional, Ivanov, V., additional, Korotkov, V. I., additional, Matveyeva, N. I., additional, Panova, A. V., additional, Pasechnik, I. M., additional, Sevrygin, A. A., additional, and Solov’ev, M. A., additional

Published
2013
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39. Arctic Tundra and Polar Desert Ecosystems

Author

Callaghan, T., Björn, L.O., Chapin, F.S., Chernov, Y., Christensen, T.R., Huntley, B., Ims, R., Johansson, M., Jolly, R.D, Jonasson, Sven Evert, Matveyeva, N., Oechel, W., Panikov, N., Shaver, G., Elster, J., Henttonen, H., Jónsdóttir, I.S., Laine, K., Schaphoff, S., Stich, S., Taulavuori, E., Taulavuori, K., Zöckler, C., Callaghan, T., Björn, L.O., Chapin, F.S., Chernov, Y., Christensen, T.R., Huntley, B., Ims, R., Johansson, M., Jolly, R.D, Jonasson, Sven Evert, Matveyeva, N., Oechel, W., Panikov, N., Shaver, G., Elster, J., Henttonen, H., Jónsdóttir, I.S., Laine, K., Schaphoff, S., Stich, S., Taulavuori, E., Taulavuori, K., and Zöckler, C.

Published
2005

40. Key findings and extended summaries

Author

Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Schaphoff, S., Sitch, S., Zöckler, C., Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Schaphoff, S., Sitch, S., and Zöckler, C.

Published
2004

41. Effects on the function of Arctic ecosystems in the short- and long-term perspectives

Author

Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., and Shaver, G.

Published
2004

42. Rationale, concepts and approach to the assessment

Author

Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., and Shaver, G.

Published
2004

43. Effects on the structure of Arctic ecosystems in the short- and long-term perspectives

Author

Callghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, R.A., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Henttonen, H., Callghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, R.A., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., and Henttonen, H.

Published
2004

44. Biodiversity, distributions and adaptations of Arctic species in the context of environmental change

Author

Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Elster, J., Henttonen, H., Laine, K., Taulavuori, K., Taulavuori, E., Zöckler, C., Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Elster, J., Henttonen, H., Laine, K., Taulavuori, K., Taulavuori, E., and Zöckler, C.

Published
2004

45. Synthesis of effects in four Arctic subregions

Author

Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Schaphoff, S., Sitch, S., Zöckler, C., Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Schaphoff, S., Sitch, S., and Zöckler, C.

Published
2004

46. Effects of changes in climate on landscape and regional processes, and feedbacks to the climate system

Author

Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Schaphoff, S., Sitch, S., Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Schaphoff, S., and Sitch, S.

Published
2004

47. Responses to projected changes in climate and UV-B at the species level

Author

Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Elster, J., Jónsdóttir, I.S., Laine, K., Taulavuori, K., Taulavuori, E., Zöckler, C., Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Elster, J., Jónsdóttir, I.S., Laine, K., Taulavuori, K., Taulavuori, E., and Zöckler, C.

Published
2004

48. Uncertainties and recommendations

Author

Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., Shaver, G., Callaghan, T.V., Björn, L.O., Chernov, Y., Chapin, T., Christensen, T.R., Huntley, B., Ims, R.A., Johansson, M., Jolly, D., Jonasson, Sven Evert, Matveyeva, N., Panikov, N., Oechel, W., and Shaver, G.

Published
2004

50. Climate change and Arctic ecosystems: 2. Modeling, paleodata‐model comparisons, and future projections

Author

Kaplan, J. O., Bigelow, N. H., Bartlein, P. J., Christiansen, T. R., Cramer, W., Harrison, S. M., Matveyeva, N. V., McGuire, A. D., Murray, D. F., Prentice, I. C., Razzhivin, V. Y., Smith, B., Walker, D. A., Andreson, P. M., Andreev, Andrei, Kaplan, J. O., Bigelow, N. H., Bartlein, P. J., Christiansen, T. R., Cramer, W., Harrison, S. M., Matveyeva, N. V., McGuire, A. D., Murray, D. F., Prentice, I. C., Razzhivin, V. Y., Smith, B., Walker, D. A., Andreson, P. M., and Andreev, Andrei

Published
2003

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