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EurOCEAN 2000 - Vlaams Instituut voor de Zee

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publications to be produced will introduce a new strategy to study physical-biological<br />

couplings and thus create markets for the MITEC profiler.<br />

The links between industry (SME’s) and aca<strong>de</strong>mic research are strengthened in or<strong>de</strong>r to<br />

improve technology transfer and ensure effective and continuing industrial exploitation of the<br />

results of MAST fun<strong>de</strong>d research. The <strong>de</strong>velopment of such technologies will promote<br />

ecosystem research. It will also contribute to the un<strong>de</strong>rstanding of bio-geochemical fluxes, the<br />

influence of small-scale physical processes on the dynamics of marine ecosystems, the impact<br />

of climatic change on atmosphere-sea exchange processes and the study of the dynamic<br />

properties of coastal systems.<br />

After the partial successful completion of the project there is a precompetitive prototype<br />

available, which will form the base for a forthcoming project, to qualify the system for<br />

industrial production (possibly within EUREKA/EUROMAR).<br />

MITEC provi<strong>de</strong>s a new and advanced tool for observations and flux studies in the near surface<br />

layer. This tool will help to improve the un<strong>de</strong>rstanding of the processes in the near surface<br />

layer. This will benefit both marine science itself as well as the application of Remote Sensing<br />

in the marine environment, by improving the quality of the Remote Sensing <strong>de</strong>rived data<br />

products of the marine environment. The European value-ad<strong>de</strong>d industry will make use of the<br />

results to enhance its products and services to governments, marine research institutions and<br />

the marine-related industry.<br />

MITEC is expected to support and stimulate research activities in aquatic systems including<br />

international marine programmes such as WOCE, JGOFS, GOOS, ELOISE and international<br />

lacustrine programmes such as EROS (Black Sea), ALPE (European Program on Alpine lakes),<br />

IDEAL (East African Lakes) and BICER (Baikal International Center for Ecological<br />

Research).<br />

ACKNOWLEDGEMENT:<br />

The present project <strong>de</strong>scription results from contributions and the collaboration of all scientists<br />

of the MAST-III project MITEC, but especially valuable were the contributions of Dr. Hartmut<br />

Prandke and Dr. Kurt Holtsch.<br />

REFERENCES:<br />

Anis, A. and Moum, J. N. 1992, The superadiabatic surface layer of the ocean during<br />

convection. J. Phys. Oceanogr. 22, 1221-1227.<br />

Anis, A. and Moum, J. N. 1995, Surface wave-turbulence interactions: Scaling ε(z) near the sea<br />

surface. J. Phys. Oceanogr. 25, 2025-2045.<br />

Caldwell, D. R. and J. N. Moum (1995). Turbulence and mixing in the ocean, Reviews of<br />

Geophysics, Supplement, Pages 1385-1394, July 1995, U.S. national Report to<br />

International Union of Geo<strong>de</strong>sy and Geophysics 1991-1994.<br />

Kiorboe, T. 1993. Turbulence, phytoplankton cell size and the structure of pelagic food webs.<br />

Adv. Mar. Biol. 29: 1-72.<br />

Stips, A. H. Prandke, T. Neumann, 1998. The structure and<br />

dynamics of the Bottom Boundary Layer in shallow sea areas<br />

without tidal influence: an experimental approach. Progress in<br />

Oceanography, 41, 383-453.<br />

Thomas, W.H. and Gibson, C.H. 1990. Effects of small-scale turbulence on microalgae. J.<br />

Appl. Phycol 2: 71-77.<br />

Thomas, W.H. and Gibson, C.H. 1990. Quantified small-scale turbulence inhibits a red ti<strong>de</strong><br />

dinoflagellate, Gonyaulax polyedra Stein, Deep-Sea Res. 37: 1583-1593.<br />

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