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Страница 8 из 2112

Современная динамика высокогорных лесов на Северном Урале: основные тенденции

Дэви, Н.М., Кукарских, В.В., Галимова, А.А., Бубнов, М.О., Зыков, C.В., Devi, Nadezhda M., Kukarskih, Vladimir V., Galimova, Arina A., Bubnov, Maksim O., Zykov, Sergey V.

and increasing winter precipitation. Climatic response analysis, contained in 4 generalized tree

Структура лесов и климатический отклик деревьев в зоне контакта «лес-степь» (Горный Алтай)

Бочаров, А.Ю., Савчук, Д.А., Bocharov, Anatoly Yu., Savchuk, Dmitry A.

belt –> forest-steppe boundary –> forest-steppe ecotone. Percentage of larch trees increases from

Earlywood and Latewood Features of Pinus sylvestris in Semiarid Natural Zones of South Siberia

Babushkina, E. A., Belokopytova, L. V., Kostyakova, T. V., Kokova, V. I.

moisture conditions. Patterns of statistical characteristics and climatic responses of the chronologies

Climatic controls of decomposition drive the global biogeography of forest-tree symbioses

Crowther, T. W., Liang, J., Van Nuland, M. E., Werner, G. D. A., Reich, P. B., Nabuurs, G., de-Miguel, S., Zhou, M., Picard, N., Herault, B., Zhao, X., Zhang, C., Routh, D., Peay, K. G., Cazzolla Gatti, Roberto, Steidinger, B. S.

and elevation. By contrast, arbuscular mycorrhizal trees dominate in aseasonal, warm tropical forests, and occur

Palaeoclimate constraints on a world with post-industrial warming of 2 degrees and beyond warmer than during the preindustrial Holocene. Although past intervals of warming were forced differently

Notes towards an optimal sampling strategy in dendroclimatology

Kirdyanov, A. V., Piermattei, A., Kolar, T., Rybnicek, M., Krusic, P. J., Nikolaev, A. N., Reinig, F., Buntgen, U

Though the extraction of increment cores is common practice in tree-ring research

The intensity of the climatic signal in the dynamics of the inсrement of Scots pine (Pinus silvestris L.) of the Khrenovskii forest (Voronezh region, Russia)

Matveev, S., Timashchuk, D., Matskovsky, V.

for dendrochronological analysis were collected from 30 trees (1 core per tree). The climatic characteristics are taken

Tree wave migration across an elevation gradient in the Altai Mountains, Siberia

Viacheslav I. Kharuk, Sergei T. Im, Maria L. Dvinskaya, Kenneth J. Ranson, Il’ya A. Petrov

Mountains and its response to observed air temperature increase was considered. At the upper limit of tree

Zooplankton community of a small river under abnormal climatic conditions (on the example of the Kazanka river, Russian federation)

Derevenskaya O., Mingazova N., Yakovlev V.

© 2015 Begell House, Inc. Global warming is one of the peculiarities of climate changes

Ranking of tree-ring based temperature reconstructions of the past millennium

EsperJan, Krusic, Paul J., Ljungqvist, Fredrik, Luterbacher, Jürg, Carrer, Marco, Cook, Ed, Davi, Nicole K., Hartl-Meier, Claudia, Kirdyanov, A., Konter, O., Myglan, V., Timonen, Mauri, Treydte, Kerstin, Trouet, Valerie, Villalba, Ricardo, Wilson, Rob S., Yang, Bao, Büntgen, Ulf

Tree-ring chronologies are widely used to reconstruct high-to low-frequency variations in growing

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