Past break-monsoon conditions detectable by high resolution intra-annual δ18O analysis of teak rings

Mathematics – Logic

Scientific paper

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Atmospheric Processes: Paleoclimatology (0473, 4900), Oceanography: Biological And Chemical: Stable Isotopes (0454, 1041), Global Change: Climate Variability (1635, 3305, 3309, 4215, 4513), Atmospheric Processes: Tropical Meteorology, Hydrology: Precipitation (3354)

Scientific paper

Intra-annual variations in the cellulose oxygen isotopic composition (δ18O) of several annual growth rings of three teak (Tectona grandis L.F.) trees from central India show a clear seasonal cycle with higher values in the early and late growing seasons and lower values in the middle. This cycle is useful to identify growth occurring during different phases of the growing season. Relative humidity (RH) appears to control the intra-annual δ18O variations rather than rainfall, and therefore past break-monsoon conditions associated with lower RH, could be detected by high resolution sub-sampling of annual rings for δ18O analysis.

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