C. Goyet et al., TEMPORAL VARIATIONS OF PCO(2) IN SURFACE SEAWATER OF THE ARABIAN SEA IN 1995, Deep-sea research. Part 1. Oceanographic research papers, 45(4-5), 1998, pp. 609
As part of the JGOFS program in the Arabian Sea we continually measure
d the partial pressure of CO, gas in surface seawater (pCO(2)(sea)) an
d in the atmosphere above the sea surface (pCO(2)(air)) along six simi
lar cruise tracks in January, February, March, July, November, and Dec
ember of 1995. The observed variations of pCO(2)(sea) reached over 260
mu atm close to the Omani coast in January-February and July-August.
Offshore the pCO(2)(sea) variations with time were relatively small(<
40 mu atm). The pCO(2)(air) shifted by 15 mu atm between the northeast
and southwest monsoons. In order to estimate monthly and annual mean
of CO, flux in the Arabian Sea, we used sea surface temperature and wi
nd speed data, given on a 2.5 degrees x 2.5 degrees resolution, from F
NMOC and interpolated the observed pCO(2)(sea) data both in time and s
pace. Close to the Omani coast, the estimated monthly mean CO, efflux
across the air-sea interface varies from 8.3 to 44 mmol m(-2) month(-1
) during most of the year and up to 312.8 mmol m(-2) month(-1) during
the southwest monsoon season (July/August). Overall, the annual mean C
O2 flux from the northern Arabian Sea to the atmosphere is estimated t
o be 0.46mol m(-2) yr(-1) or 7.0 Tg Cyr(-1). (C) 1998 Elsevier Science
Ltd. All rights reserved.