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Gas exchange/Deliberate tracer | Rivers and Estuaries | Hydrology | Oceanography | WOCE | Others |
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INTRODUCTION The main goals of
the World Ocean Circulation Experiment (WOCE) are (1) to develop models
that are capable of describing the present state of the ocean and to predict
its evolution in relation to long-term climate changes, and (2) to collect
the data required for the development and calibration of such models (WCRP.
1986). The measurements required for a successful WOCE were summarized
in the WOCE Implementation Plan (Volumes I and II; WCRP, 1988). Due to the nature of their delivery to the ocean, the transient tracers are a close analogue to any perturbation imprinted onto the surface of the ocean such as a climate signal. They can be viewed as a gigantic dye experiment that allows us to visualize the penetration of this perturbation into the interior of the ocean, as well as to determine the time scale on which it occurs. The 'steady-state' tracers, on the other hand provide information on the averaged spreading patterns of waters tagged with tracer at specific source locations (e.g., the mid-ocean ridges for 3He or glacial ice for 4He). Such information is important for understanding the basic dynamics of the ocean, as well as for calibration of ocean circulation models. During the WOCE survey, samples for measurement of tritium and helium isotopes were collected on most WHP sections. This site is intended to provide an overview of the WOCE tritium/helium isotope survey and the developing results. The site contains information on:
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May 12, 2006 |
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