The backbarrier tidal flats in the southern North Sea - A multidisciplinary approach to reveal the main driving forces shaping the system
The present article is by courtesy of Ocean Dynamics, where it was originally published .
Tidal flats are an important feature of many coastlines affected by tides in various climate zones of the world. They belong to the most productive natural ecosystems on earth and play an important role in global biogeochemical cycles. Tidal areas not only provide a habitat for many species of birds, but are also the nursery for a wide variety of marine organisms. In addition, tidal flats may provide significant protection against marine erosion.
Throughout history, coastal regions have been major centres of human activity. Today, more than 50% of the world's population live in coastal areas, and it has been estimated that this number will increase to 75% by the year 2025. The demand for exploitation of this space will therefore increase. This applies to natural resources like oil and gas as well as marine organisms, marine biotechnology and the production of renewable energy in coastal wind and wave power installations. Exploitation of resources always carries by the risk of detrimental effects on the vulnerable coastal ecosystem. Knowledge of the ecological processes and the health status of the flats, which can be derived from this knowledge, is therefore of great importance to the costal population.
The study area
The flat relief of the southern North Sea basin and the pronounced tides have created extensive tidal flats along its coast. The tidal range varies between about one and four metres in the south-eastern part of the North Sea. The tidal flat system encompasses supralitoral salt marshes, dunes and beaches that extend above the mean high-tide level, intertidal flats that are exposed only at low tide, and subtidal creeks and depressions that are permanently under water and run like rivers through the tidal landscape.
One of the largest continuous tidal flat zones of the world extends along the North Sea coast from Blåvands Huk in Jutland, Denmark, in the North down via Schleswig-Holstein and Lower Saxony in Germany to Den Helder in the Netherlands in the Southwest (Fig. 1). Particularly characteristic are the barrier islands, which were created a few thousand years ago by sand deposits off the coasts of the northern Netherlands, Lower Saxony and southwestern Denmark, whereas the islands off the coast of Schleswig-Holstein are mainly remnants of a former land mass that has been scoured by mediaeval storm surges (cf. Streif 1990). During the most recent ice age about 18,000 years ago, the coastline was situated far out in the North Sea and only reached the modern shores after the continental ice masses melted some 9,000 years ago, forming today’s coastal landscape in the course of the rising sea level (Behre 1993, 2003 ).
The time series station
Similarly, the effects of severe winters, when ice floes freeze to the surface of the sediment at low tide and possibly carry this layer out into the open North Sea during flood tide, were also not yet fully understood. To overcome these limitations, the research group planned and installed a permanent, storm- and ice-proof time-series measuring station (Fig. 2) in the tidal inlet (Otzumer Balje) between the islands of Spiekeroog and Langeoog (Fig. 1) in August 2002. With this station, continuous measurements of the concentration and transport of suspended material in the water column even under harsh weather conditions became possible by means of a multi-spectral transmissometer (MST) and an upward-looking acoustic Doppler current profiler (ADCP). The MST was mounted to the station close to the sea surface, the ADCP about 1 m above the seabed on an eight-meter long outrigger arm from the station in about 15 m of water depth. Long-term changes in the sediment budget will most likely affect the ecosystem because conditions for colonization on the seabed will change as a function of the grain-size distribution of the surface sediment. To protect and manage the Wadden Sea ecosystem, as stipulated in the National Park regulations of the State of Lower Saxony, it is important to be able to differentiate between the delayed effects of dike construction and sea-level rise on the one hand, and local human impact (agriculture, fishery, industry, tourism) on the other.
During the time of inaccessibility, bio-fouling in the flow-through tubes proceeded to the extent that the shut-off valves inside the pole could not be operated anymore. Thus, divers had to mount flanges onto the external openings of the tubes so that these could be removed for cleaning from the inside without flooding the pole. Even for professional divers, safe underwater operations were limited to half-an-hour around each slack-water period due to the strong currents in the tidal inlet. Furthermore, because visibility is almost zero in the turbid water, all work had to be performed with almost no visual aids.
Pore water and sediment sampling
In order to monitor and elucidate the biogeochemical transformation processes in the Janssand pore-water system, a new multilevel in situ-pore water sampler was developed that allows collection of pore water down to 5 m sediment depth (Fig. 5, left). After insertion into the sediment, the sampler stays on site, allowing repetitive sampling at identical locations and depth intervals. The sampler has in the meantime been successfully tested for more than two years and has produced depth profiles of several redox-sensitive elements at high resolution. Because of variations in advection and microbial activity in the course of a year, seasonal signals became apparent for some element species even at sediment depths of 3 m. Conventionally, sampling occurred at low tide when the Janssand falls dry for a few hours, but in order to study the processes “under hydrostatic pressure” at high tide, sampling was also performed from the top of a platform that was erected above the pore-water sampler locations (Fig. 5, right) – but, of course, only in good weather.
The microbial world; Höpner and Oelschläger 1997).
The role of the bacteria that live in the anaerobic sediment zone below the surface was a complete mystery at the start of the project. Many were unknown organisms, and because they were impossible or at least difficult to grow in culture, their physiological characteristics could not be studied. In the course of the studies, the cultivation success rate increased by an order of magnitude from about 0.5% of microorganisms in the tidal flat sediments to about 5%, or even 25% in the uppermost oxic sediment layer (Köpke et al., 2005). Although several other bacteria and archaea present could at least be addressed at a more general level by their molecular traces found in the sediments, 90% or more of these escaped detailed laboratory studies. As a consequence, it is still not evident whether the microorganisms, particularly in the deeper anoxic strata, extract their nourishment from hard-to-decompose organic matter left over by the surface bacteria, or whether the pore water in the sediments provides nutrients that can be utilised more easily. They may, perhaps, even be relatives of bacteria that live in similarly inhospitable conditions under more than a thousand metres of sediment in the oceans (Fry et al., 2008).
The tidal flats in mathematical models
Over the last eight years, numerical models have been used to investigate the area-specific hydrodynamics and the suspended particulate matter (SPM) dynamics in the East Frisian Wadden Sea under the umbrella of the research group. Modelling in combination with high-resolution measurements at the Wadden Sea time-series station and new theoretical approaches have revealed various new and exciting insights into this complex system. The available suite of numerical models integrates worldwide experience with innovative concepts such as state-of-the-art parameterizations of physical processes and novel concepts of SPM transport. These models have been widely used for various research applications in the Wadden Sea and the German Bight at different horizontal resolutions. Sub-domains with higher resolution are nested within the areas of lower-resolution models, thus allowing a better description of small-scale processes in the sub-domain, whilst keeping the amount of information needed from the larger-scale models at a manageable level.
The Wadden Sea area can be characterized as a well mixed estuary, although the extent of stratification associated with freshwater flux from the coast can locally substantially affect vertical overturning. To address this complex system, a model accounting for the most important processes, e.g. the vertical overturning, wind- and wave-induced turbulence, drying and flooding, has been developed.
The theoretical concepts reveal the effect of topography – caused by the bottom slope – on the drying and flooding of the tidal basins, while the exchange of water with the open sea varies with time. For most intertidal basins it takes about twice as long from low-water slacks to maximum flood current than from high-water slacks to maximum ebb current. There clearly is an ebb dominance in the deep tidal channels of the Wadden Sea, whereas in their shallow extensions and on the tidal flats transport during flood is larger than during ebb tide. In addition, distinct differences were found between the temporal variability of the transport near the surface and that in deeper layers of the tidal inlets. The near-surface transport is dominated by the tidally induced drift, whereas transport in the deeper layer is asymmetrical due to the topographic properties of the intertidal basins.
Sediment dynamics in tide-dominated environments is strongly controlled by the joint actions of transport and turbulence. This process is complex because the concentration of SPM is not only controlled by changes in the individual levels of turbulence and advection, but also by the correlation between the two. Such situations require up-to-date numerical models to reveal the important processes in space and time.
Modelling of the tidal flat ecosystem required several improvements on existing ecosystem models. Neither the simulation on a grid nor the traditional box model approach gave satisfying results. Consequently, a semi-Lagrangian model is suggested as the optimal solution because it combines the advantages of a Lagrangian tracer approach with those of an Eulerian box approach. The Ecological Tidal Model (EcoTiM) simulates the cycling of carbon, nitrogen, phosphate and silicate, and describes the tidal, diurnal, and annual dynamics within the back-barrier system. An important challenge in theoretical ecology is to find good representations of complex food webs. In a generalized modelling approach it is shown that it may be possible to formulate a coarse-graining algorithm that conserves the local dynamics of the model exactly. They show examples of food webs with a different number of species that have exactly identical local bifurcation diagrams. Based on these observations, a mathematical algorithm has been developed which identifies and groups several populations of complex food webs into a single variable without changing the local dynamics.
In the course of their studies the modellers in the research group developed a set of models describing the physical processes, water column ecology and transformations in the sediment to investigate specific processes at different temporal and spatial resolutions.
- Dynamics and structure of the water and matter ex-change between the Wadden Sea and the German Bight
- The heat budget of tidal flats
- Carrying capacity and development of the Wadden Sea
- Large scale mapping of intertidal areas
- Seagrass recovery and restoration in the Wadden Sea
- Rullkötter J., 2009. The back-barrier tidal flats in the southern North Sea—a multidisciplinary approach to reveal the main driving forces shaping the system. Ocean Dyn. 59, 157-165. doi:10.1007/s10236-009-0197-2
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