Ems. Woodward et al., The influence of the south-west monsoon upon the nutrient biogeochemistry of the Arabian Sea, DEEP-SEA II, 46(3-4), 1999, pp. 571-591
Citations number
45
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
Variations in the nutrient concentrations were studied during two cruises t
o the Arabian Sea. The situation towards the end of the southwest monsoon s
eason (September/October 1994) was compared with the inter-monsoonal season
during November and December 1994. Underway surface transects showed the i
nfluence of an upwelling system during the first cruise with deep, colder,
nutrient-rich water being advected into the surface mixed layer. During the
southwesterly monsoon there was an area of coastal Ekman upwelling, bringi
ng colder water (24.2 degrees C) into the surface waters of the coastal mar
gin. Further offshore at about 350 km there was an area of Ekman upwelling,
as a result of wind-stress curl, north of the Findlater Jet axis; this are
a also had cooler surface water (24.6 degrees C). Further offshore ( >1000
km) the average surface temperatures increased to >27 degrees C. These wate
rs were oligotrophic with no evidence of the upwelling effects observed fur
ther inshore. In the upwelling regions nutrient concentrations in the close
inshore coastal zone were elevated (NO3 = 18 mu moll(-1), PO4 = 1.48 mu mo
ll(-1)); higher concentrations also were measured at the region of offshore
upwelling off the shelf, with a maximum nitrate concentration of 12.5 mu m
oll(-1) and a maximum phosphate concentration of 1.2 mu moll(-1). Nitrate a
nd phosphate concentrations decreased with increasing distance offshore to
the oligotrophic waters beyond 1400 km, where typical nitrate concentration
s were 35.0 nmoll(-1) (0.035 mu moll(-1))in the surface mixed layer. A CTD
section from the coastal shelf, to 1650 km offshore to the oligotrophic wat
ers, clearly showed that during the monsoon season, upwelling is one of the
major influences upon the nutrient concentrations in the surface waters of
the Arabian Sea off the coast of Oman. Productivity of the water column wa
s enhanced to a distance of over 800 km offshore. During the intermonsoon p
eriod a stable surface mixed layer was established, with a well-defined the
rmocline and nitracline. Surface temperature was between 26.8 and 27.4 degr
ees C for the entire transect from the coast to 1650 km offshore. Nitrate c
oncentrations were typically between 2.0 and 0.4 mu moll(-1) for the transe
ct, to about 1200 km where the waters became oligotrophic, and nitrate conc
entrations were then typically 8-12 nmoll(-1). Ammonia concentrations for t
he oligotrophic waters were typically 130 nmoll(-1), and are reported for t
he first time in the Indian Ocean. The nitrogen/phosphorus (N/P) ratios sug
gest that phytoplankton production was potentially nitrogen-limited in all
the surface waters of the Arabian Sea, with the greatest nitrogen limitatio
n during the intermonsoon period. (C) 1999 Elsevier Science Ltd. All rights
reserved.