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Responses of ring widths and maximum densities of Larix gmelinii to climate on contrasting north‐ and south‐facing slopes in central Siberia
Author(s) -
Kujansuu Joni,
Yasue Koh,
Koike Takayoshi,
Abaimov Anatoly P.,
Kajimoto Takuya,
Takeda Takashi,
Tokumoto Morihiko,
Matsuura Yojiro
Publication year - 2007
Publication title -
ecological research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.628
H-Index - 68
eISSN - 1440-1703
pISSN - 0912-3814
DOI - 10.1007/s11284-006-0062-4
Subject(s) - larix gmelinii , snowmelt , precipitation , snow , maximum density , dendrochronology , climatology , atmospheric sciences , physical geography , environmental science , geology , geography , ecology , larch , geomorphology , biology , meteorology , physics , paleontology , quantum mechanics
An analysis was performed of the climatic responses of the radial growth of Larix gmelinii (Rupr.) Rupr. at two sites—both of which included contrasting north‐ and south‐facing slopes—in Tura, central Siberia, with the development of ring width and maximum‐density chronologies for each slope. Both residual and standard chronologies of ring widths were positively correlated with temperature from late May until mid June on all four slopes. By contrast, standard chronologies of ring widths were negatively correlated with precipitation during the winter (from October to April) and in May on the north‐facing slope at site 1 and on the south‐facing slope at site 2 respectively. The negative correlations with precipitation during the winter and in May on some of the slopes suggested that delayed snowmelt in early spring might inhibit the radial growth of L. gmelinii , and the effects of snow are likely to vary with topography. Both residual and standard chronologies of maximum densities were positively correlated with temperature in early July on all four slopes. Maximum densities were also positively correlated with precipitation during summer of the previous year on all the slopes. These suggest that no major differences exist in terms of responses of maximum density to climatic factors between the north‐ and south‐facing slopes.