Data collected during three expeditions to the Arabian Sea are examined to
characterise the changes in phytoplankton properties between the intermonso
on and monsoon seasons. The results are used to elucidate the key changes t
hat lead to the occurrence of phytoplankton blooms following the onset of t
he monsoon winds. Contrary to expectations, changes in the assimilation num
ber and the initial slope of the photosynthesis-light curve decreased in th
e SW monsoon season, apparently in the wrong sense for them to account for
the incidence of blooms in the Arabian Sea during this season. On the other
hand, there were strong differences between the intermonsoon and monsoon v
alues of the chlorophyll-specific absorption coefficient for the phytoplank
ton, probably arising from seasonal changes in cell size and community comp
osition. The sense of these changes was such as to increase substantially t
he maximum quantum yield for photosynthesis during the monsoon season compa
red with the intermonsoon. When these results are applied in a simple expre
ssion for the daily, primary production of the water column, they can expla
in the rapid accumulation of phytoplankton observed in the Arabian Sea foll
owing the start of the monsoon season. Thus, the occurrence of seasonal blo
oms in the Arabian Sea depends on combined variations in both the optical a
nd photosynthetic characteristics of phytoplankton in the region. (C) 1999
Elsevier Science Ltd. All rights reserved.