A mooring instrumented with optical and physical sensors within the upper 300 m was deployed for two consecutive 6-month periods (October 15, 1994 through October 20, 1995; sampling intervals of a few minutes) in the central Arabian Sea (15°30'N, 61°30'E). Both the Northeast Monsoon (November 1, 1994-February 15, 1995) and Southwest Monsoon (June 1-September 15, 1995) were observed. During the NE Monsoon, wind speeds averaged 6 m s-1 and reached up to 15 m s-1 during the SW Monsoon. Intermonsoon periods (Spring February 16-May 31, 1995; and Fall September 16-October 15, 1995) were characterized by weak and variable winds. Shortwave radiation and photosynthetically available radiation (PAR) displayed half-yearly cycles, peaking during the Intermonsoon periods. Two mixed-layer depth definitions have been used to describe our results. The first is based on a temperature difference of 0.1°C of the surface temperature, MLD(01°C), and the second is based on a difference of 1.0°C, MLD(1.0°C). The maximum Winter mixed layer depth (MLD(1.0°C) ~ 110 m) was deeper than the Summer mixed layer (MLD(1.0°C) 80 m), primarily because of surface cooling and convection. A half-yearly cycle in chlorophyll a was evident with greater values occurring during each Monsoon and into the Intermonsoon periods. High chlorophyll a values associated with cool mesoscale features were also apparent during each Monsoon. These mesoscale features and others have been identified using remotely sensed sea-surface height anomaly maps. Time-series of the 1% light level depth, h(1%) tracked the depth-integrated chlorophyll a. In general, h(1%) was deeper than MLD(1.0°C) during the latter half of the Spring Intermonsoon (SIM) (with low chlorophyll a periods) and shallower than MLD(1.0°C) during the latter portions of the Monsoons (high chlorophyll a periods). During the SIM, the penetrative components of net solar radiation at the base of the mixed layers, E(n)(MLD(1.0°C)) and E(n)(MLD(0.1°C)), reached values of ~40 and 75 W m-2, respectively, when the net surface heat flux was 120 W m-2. The highest mixed layer radiant heating rates occurred during the Intermonsoon periods with peak values greater than 0.2 and 0.1°C d-1 for MLD(0.1°C) and MLD(1.0°C), respectively. Our results indicate that biological variability is significant for the upper ocean heat budget of the central Arabian Sea during the SIM. The present results, in conjunction with those presented in Marra et al. (1998) and Honjo et al. (1998), demonstrate strong coupling of upper ocean biological processes with deep ocean particulate organic carbon fluxes. These collective results suggest that the timing and amplitudes of phytoplankton blooms associated with both seasonal stratification and eddies are quite well-correlated with relatively rapid export flux of organic carbon to the deep ocean.
|Original language||English (US)|
|Number of pages||25|
|Journal||Deep-Sea Research Part II: Topical Studies in Oceanography|
|State||Published - Aug 1998|
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