From a network of teak chronologies in northern Thailand, 75 trees wit
hin one province were evaluated regarding their climatic signal. The r
aw tree-ring series revealed a high mean sensitivity of 0.50 and a mod
erate first-order autocorrelation of 0.48, The first principal compone
nt of the standardized data explained 44% of the total variation in th
e tree-ring data, indicating a considerable climatic influence on tree
growth. The climate-growth relationship suggested that growth of teak
in this study area is mainly controlled by rainfall from April to Jun
e. Thus, there is some promise that the whole network of teak chronolo
gies in northern Thailand can contribute to reconstructing climate ove
r at least the last three centuries.