NOAA GLOBEC ACTIVITIES IN THE ARABIAN SEA
Principal Investigator:
Peter B. Ortner
Collaborating
scientist(s):
Sharon Smith (RSMAS), Van Holliday (Tracor)
Objective:
The objectives of the GLOBEC cruise were to:
(1) to collect data
on plankton and mesopelagic animal communties, and how they are affected
by monsoonal forcing
(2) to deploy satellite-tracked Langrangian drifters and collect
ancilliary data on the interconnection of Somali coastal waters and
the central basin of the Arabian Sea,
(3) to support the acoustic sampling being conducted at the ONR central
mooring site and across the Arabian Sea as part of the Joint Global Ocean
Flux (JGOFS) and ONR/ARI (Accelerated Research Initiative) and
(4) to support the OACES
(Ocean-Atmosphere Carbon Exchange Study) and RITS (Radiatively
Important Trace Species) programs in extending their geographic
and temporal coverage.
Rationale:
Among the strongest atmospheric forcing of the upper water column
observable anywhere in the world ocean, recurs in the Arabian Sea.
Seasonally reversing monsoonal winds drive strong currents,
produce complex eddy fields, deepen the mixed layer and induce both
coastal and open ocean upwelling. These physical
changes directly affect primary production processes but also may be expected to
influence the abundance, distribution and diversity of the animals
dependent upon that production. US.JGOFS, ONR and WOCE all
planned studies in the Arabian Sea in FY95. These
provided GLOBEC investigators a chance to study zooplankton and
mesopelagic fish in an exhaustively detailed physical, chemical and
biological context that will be provided from research cruises,
satellite remote-sensing, long-term mooring and modelling
activities conducted by other U.S. Global Change Program research
components.
Method:
While underway the epipelagic and mesopelagic animal distribution
were continuously sampled using hull-mounted transducers (12 and
100KHz) as well as a acoustic doppler current profiler (ADCP) by P. Ortner, AOML, S. Smith, RSMAS, and V. Holliday, TRACOR. At
the same time the atmospheric boundary layer was continuously
sampled (0 and CO) as well as surface
waters (salinity, temperature, chlorophyll fluorescence, pCO,
pH, NO, DIC) by R. Wanninkhof, AOML, and the epipelagic
plankton community (optical particle
size, 880nm backscatter, acoustic backscatter from 256khz to 30000khz and real-
time video imagery) by P. Ortner, AOML. The boundary layer was sampled by an air
sampler mounted on the bridge, surface waters by a continuous clean
pump system mounted amidships and surface plankton by instruments
mounted aboard the AOML towed aquashuttle vehicle. A continuous
pump system was intermittently sampled for nutrients by J-Z Zhang, AOML, extracted
plant pigment determination and, zooplankton. At least
daily along the transect (and at most of the demarcated station
positions) the plankton and mesopelagic fish communties were
sampled with a 1m MOCNESS (multiple-opening-closing-net system) by S. Smith, RSMAS, and
a 10m MOCNESS by L. Madin, WHOI et al., respectively. At each MOCNESS deployment station the AOML
aquashuttle was bounced to 150m while maneuvering prior to
the launch. Instrumented drifters (temperature, fluorescence)
were deployed off the Somali coast by G. Hitchcock, RSMAS and regular (at least daily)
CTD casts made by RSMAS and NIOZ investigators to obtain baseline information on temperature, salinity, chlorophyll, nutrient and oxygen distribution and to
obtain material for microbiological experiments other academic collaborators made additional net tows throughout the cruise to obtain live animals for
experimental purposes. These included both neuston tows and
vertical net tows. As near as possible to the ONR mooring site a
series of shallow (<150m) MOCNESS tows were made by P. Ortner et al. every three
hours with a specially configured 1m MOCNESS equipped with the high
frequency acoustic system from the aquashuttle. Weather permitting small-boat dive operations were conducted by L. Madin, WHOI and P. Kremer, UC.
The objective of this effort was to collect live animals for experiments and to
observe their in-situ behavior. Additional
physical measurements included the deployment of ARGOS-tracked
lagrangian drifters (M. Bushnell, AOML) and continuous collection
of ADCP data (D. Wilson, AOML) as well as logging the standard
meteorological data.
Accomplishment:
Two cruises were made, one in May prior to the true onset of the SW
Monsoon and another in August toward the end of the monsoon aboard the
NOAA Ship MALCOLM BALDRIDGE. The effect of the monsoon is readily
apparent in AVHRR imagery from each of the cruises ( (figure 2). Incipient Upwelling along Somalia has
become full blown coastal upwelling by August while overall temperatures
have cooled throughout the basin. The primary responsibility of the
NOAA/AOML group was analysis of optical and acoustic data in relation to
vertical and along track hydrography. These data included continuous along
track data, Acoustic Doppler Current Profiler and 12/100kHz hull
transducers as well as profiles with a Tracor multifrequency (256kHz -
3.0mHz) acoustic plankton sampler (TAPS) and an optical plankton counter
(OPC) mounted both upon a MOCNESS net system and an Aquashuttle. To date
we have focused primarily upon the offshore station Central Basin at the
center of the mooring ar ray near the axis of the Findlater wind jet.
Hydrographic data confirms a substantial mixing as a result of the winds
of the southwest monsoon (figure 3).
The mixed layer had deepened and
the subsurface chlorophyll maximum had been eroded along with the
subsurface oxygen peak indicative of the productivity maximum. Nutrients
now available in the near surface permitted a considerable increase in
mixed layer chlorophyll values. However the data are not unambiguous
since they also indicate the presence of considerably fresher surface
waters. Remote-sensing and mooring data are being carefully examined to
determine the source of this water.
A multiple-opening/closing net system (MOCNESS) was used to sample
zooplankton and larval fishes at the Central Basin station on both
cruises. Displacement volume estimates made from the actual net catches
of replicate tows indicate a more than five fold increase in biomass in
August as compared to May
(figure 4). Using acoustic sensors can
negate avoidance problems. Data from a TAPS mounted on this MOCNESS
confirm this difference as well as a particular increase in larger forms
(figure 5).
ADCP backscatter intensity is used to estimate animal biomass. Data from
the second cruise is depicted as a curtain plot following the cruise
tract. Particularly offshore diel vertical migration is the dominant
signal resulting in higher biomass in the surface each night. Looking more
closely at some data from the Central Basin station we can compare our
observations in May and August. Considerably higher biomass was evident
in August. Compare figure 6 with
figure 7. Fitting these data to a line
representing the center of mass we can calculate the speed of vertical
migration. It approached 10cm/sec suggesting that these migrators were
substantial in size, most likely decapods and mesopelagic fishes
(figure 8).
The Aquashuttle developed at AOML for the GLOBEC cruises housed an
integrated plankton sampler including a CTD, fluorometer, IR backscatter,
multifrequency acoustic subsystem, optical plankton counter and in-situ
video. Optical plankton
counter data were taken at ca. the same time of day at the Central Basin
station on each cruise (compare figure 10
and figure 11). They indicate not
only a substantial increase in overall abundance in August but also a
shift toward larger organism size.
By an odd coincidence the first NOAA GLOBEC cruise with its focus upon
faunal change rather than the JGOFS cruises that focused more directly
upon upwelling per se. was the only cruise to sample the Somali upwelling,
the first to sample the Omani coastal upwelling and, perhaps, to have
documented open ocean upwelling as well. The effects of oceanic
upwelling, eddy passage and perhaps the offshore advection of coastal
upwelling plankton populations are apparent in our data. MOCNESS net tow
displacement volume, OPC, ADCP, and TAPS data are consistent in confirming
a more than fourfold increase in animal abundance in August. This
difference exceeds any observed by researchers aboard the RV/Thomas
Thompson which sampled the same site just before our first and after our
second cruise. Combining the data from the THOMPSON and BALDRIDGE cruises
we will yield a rigorous understanding of the biological response to the
monsoon.
Key reference:
U.S. GLOBEC Report Nine: Implementation Plan and Workshop Report for U.S. GLOBEC
studies in the Arabian Sea, May 1993.
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