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

w10=
Найдено документов в текущей БД: 2

    The application of tree-rings and stable isotopes for reconstructions of climate conditions in the Russian Altai
[Text] / O. V. Sidorova [et al.] // Clim. Change. - 2013. - Vol. 120, Is. 01.02.2013. - P153-167, DOI 10.1007/s10584-013-0805-5. - Cited References: 32. - The work was supported by Marie Curie IIF (EU-ISOTREC 235122) awarded to Olga Sidorova, SNSF 200021_121838/1, and SNSF - SCOPES Iz73z0-128035/1, MK-1675.2011.6, Russian Scientific School 5327.2012.4 and RFBR grant 13-05-00620. Neil J. Loader thanks the UK NERC (NE/B501504) and C3W for support. We thank Eugene Vaganov for the suggestions in the manuscript and five reviewers for their constructive and helpful comments. . - 15. - ISSN 0165-0009
РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: We present new tree-ring width, delta C-13, and delta O-18 chronologies from the Koksu site (49A degrees N, 86A degrees E, 2,200 m asl), situated in the Russian Altai. A strong temperature signal is recorded in the tree-ring width (June-July) and stable isotope (July-August) chronologies, a July precipitation signal captured by the stable isotope data. To investigate the nature of common climatic patterns, our new chronologies are compared with previously published tree-ring and stable isotope data from other sites in the Altai region. The temperature signal preserved in the conifer trees is strongly expressed at local and regional scales for all studied sites, resulting in even stronger temperature and precipitation signals in combined average chronologies compared to separate chronologies. This enables the reconstruction of June-July and July-August temperatures for the last 200 years using tree-ring and stable carbon isotopes. A July precipitation reconstruction based on oxygen isotopic variability recorded in tree-rings can potentially improve the understanding of hydrological changes and the occurrence of extreme events in the Russian Altai.

Полный текст,
WOS,
Scopus

Держатели документа:
[Sidorova, O. V.
Siegwolf, R. T. W.
Saurer, M.] Paul Scherrer Inst, CH-5232 Villigen, Switzerland
[Myglan, V. S.
Shishov, V. V.] Siberian Fed Univ, Krasnoyarsk 660049, Russia
[Ovchinnikov, D. V.] VN Sukachev Inst Forest SB RAS, Krasnoyarsk 660036, Russia
[Helle, G.] German Ctr GeoSci GFZ, Helmholz Ctr Potsdam, D-14473 Potsdam, Germany
[Loader, N. J.] Swansea Univ, Dept Geog, Swansea SA2 8PP, W Glam, Wales

Доп.точки доступа:
Sidorova, O.V.; Siegwolf, RTW; Myglan, V.S.; Ovchinnikov, D.V.; Shishov, V.V.; Helle, G...; Loader, N.J.; Saurer, M...; Marie Curie IIF [EU-ISOTREC 235122]; SNSF [200021_121838/1]; SNSF - SCOPES [Iz73z0-128035/1, MK-1675.2011.6]; Russian Scientific School [5327.2012.4]; RFBR [13-05-00620]; UK NERC [NE/B501504]; C3W

    A forward modeling approach to paleoclimatic interpretation of tree-ring data
[Text] / M. N. Evans [et al.] // J. Geophys. Res.-Biogeosci. - 2006. - Vol. 111, Is. G3. - Ст. G03008, DOI 10.1029/2006JG000166. - Cited References: 57 . - 13. - ISSN 0148-0227
РУБ Environmental Sciences + Geosciences, Multidisciplinary

Аннотация: We investigate the interpretation of tree-ring data using the Vaganov-Shashkin forward model of tree-ring formation. This model is derived from principles of conifer wood growth, and explicitly incorporates a nonlinear daily timescale model of the multivariate environmental controls on tree-ring growth. The model results are shown to be robust with respect to primary moisture and temperature parameter choices. When applied to the simulation of tree-ring widths from North America and Russia from the Mann et al. (1998) and Vaganov et al. (2006) data sets, the forward model produces skill on annual and decadal timescales which is about the same as that achieved using classical dendrochronological statistical modeling techniques. The forward model achieves this without site-by-site tuning as is performed in statistical modeling. The results support the interpretation of this broad-scale network of tree-ring width chronologies primarily as climate proxies for use in statistical paleoclimatic field reconstructions, and point to further applications in climate science.

Полный текст,
WOS,
Scopus

Держатели документа:
Univ Arizona, Tree Ring Res Lab, Tucson, AZ 85721 USA
Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA
Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
Russian Acad Sci, Inst Forest, Krasnoyarsk, Russia

Доп.точки доступа:
Evans, M.N.; Reichert, B.K.; Kaplan, A...; Anchukaitis, K.J.; Vaganov, E.A.; Hughes, M.K.; Cane, M.A.