Across-slope relations between the biological populations, the euphotic zone and the oxygen minimum layer off the coast of Oman during the southwest monsoon (August, 1994)

• Published in: Progress in oceanography Vol. 41; no. 1; pp. 69 - 109
• Main Authors: HERRING, P. J, FASHAM, M. J. R, WEEKS, A. R, HEMMINGS, J. C. P, ROE, H. S. J, PUGH, P. R, HOLLEY, S, CRISP, N. A, ANGEL, M. V
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier 1998
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; Biological and medical sciences; Coastal oceanography, estuaries. Regional oceanography; Earth, ocean, space; Exact sciences and technology; External geophysics; Fundamental and applied biological sciences. Psychology; Marine; Physics of the oceans; Sea water ecosystems; Synecology; Indian Ocean; Gulf of Oman; Arabian Sea; ISW, Oman; Oxygen; Floristic composition; Acoustic measurement; Monsoon; Biomass; Biogeochemical cycle; Time variation; Coastal zone; Marine environment; Euphotic zone; Marine hydrography; Phytoplankton; Zooplankton; Vertical migration; Ecological abundance; Necton
• ISSN: 0079-6611; 1873-4472
• DOI: 10.1016/s0079-6611(98)00019-6

An area some 120 x 70 km off the eastern coast of Oman (containing the UK JGOFS Arabesque station) was intensively studied over a 17 day period in August 1994, with the objective of determining the relationships between the biological populations, the oxygen minimum layer and the dynamic hydrography of the euphotic zone. The outer margin of the area was delimited by a rectangle of 15 full depth CTD casts and the hydrography was further defined by two Seasoar surveys within the box. Midwater trawls were used to sample the populations at three stations, oceanic, slope and shelf edge respectively. Day and night samples of macroplankton and micronekton were taken at each station to determine the extent of diel vertical migration and the effect of the hypoxic region on these migrations. Concurrent ADCP data were used to follow the migrations and spatial changes in real time. Despite the limited area studied the patterns of upwelling and their temporal and spatial changes were complex. Coastal upwelling was observed directly only at the southwestern edge of the area during both Seasoar surveys. Persian Gulf Water was a consistent but spatially discrete feature of the region at depths of 200-300 m. Arabian Sea Surface Water was present at the eastern margin of the first survey.