This study was carried out at 500 m elevation in a pure forest of Sal (Shor
ea robusta) (trees generally above 25 m in height) in Kumaun region of Cent
ral Himalaya (between 29 degrees 8' latitude and 79 degrees 20' longitude)
where the average rainfall is approximately 1800 mm of which 80% occurs in
the monsoon period to determine the seasonal changes in soil water potentia
l tree water potential and leaf conductance. Seasonal fluctuations in soil
water potential were not reflected in predawn tree water potential and leaf
conductance. However, leaf conductance declined sharply during the peak su
mmer drought as a result of stomatal closure. No significant correlation (r
= 0.148i) existed between soil water potential (at 60 cm depth) and predaw
n tree water potential. The relatively high values of leaf conductance thro
ughout the study (except summers) supports the fact that S. robusta seems t
o keep its stomata open throughout the year, carrying out photosynthesis in
all seasons las leaf conductance is assumed to be related to photosynthesi
s). However, the species different in degree of fall in leaf conductance in
response to adverse climatic conditions showing a significant decrease in
leaf conductance during the peak summer time of year 2, and winters of year
1.