There are several reports which indicate that the c1imate over the Himalayan region is linked both with the monsoon variation on the Indian subcontinent and in the whole of South-East Asia as well as with the El-Niño/Southem Oscillation. To understand the behaviour ofthese c1imatic phenomena we need long-term high-resolution c1imatic records which are in generallacking in this part of the globe. Tree-ring studies have therefore been taken up in the tropical and Himalayan region in India to develop millennium-long c1imatic reconstructions.
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Bhattacharyya et al. (1999) studied this question.
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