40
R. I. CURRIE, A. E. FISHER and P. M. HARGREAVES:
show a lift upwards to the coast. Likewise there was a markedly higher dissolved
inorganic PO/--P concentration in the upper layers near the coast (Fig. 3 b). The level
of the 1.0 mg-at m- 3 isoline for PO/--p which lay at a depth of 100 m in March,
reached the surface in May.
Fig. 3 b
~ _ _ - 2-0
/'"
2 -5
Fig. 3 c
The "Discovery" observations in the summer of 1963 provide the most complete
picture of the circulation at the peak of the SW monsoon (Royal Society, 1963). Five
lines of stations, roughly normal to the Arabian coast, were worked at the end of June
and beginning of July, and on 4 of these sections there is evidence of very active upwelling
in the coastal belt. The extent of this can be seen from the depression of sea surface
R. I. CURRIE, A. E. FISHER and P. M. HARGREAVES:
show a lift upwards to the coast. Likewise there was a markedly higher dissolved
inorganic PO/--P concentration in the upper layers near the coast (Fig. 3 b). The level
of the 1.0 mg-at m- 3 isoline for PO/--p which lay at a depth of 100 m in March,
reached the surface in May.
Fig. 3 b
~ _ _ - 2-0
/'"
2 -5
Fig. 3 c
The "Discovery" observations in the summer of 1963 provide the most complete
picture of the circulation at the peak of the SW monsoon (Royal Society, 1963). Five
lines of stations, roughly normal to the Arabian coast, were worked at the end of June
and beginning of July, and on 4 of these sections there is evidence of very active upwelling
in the coastal belt. The extent of this can be seen from the depression of sea surface