Guide Estuaries: Monitoring and Modeling the Physical System

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Modeling a Cyber Physical System with Uppaal

Why use conceptual models? Conceptual diagrams of estuarine vegetation. Conceptual diagrams are useful because they: Facilitate communication. Conceptual models are a tool through which detailed technical concepts can be summarised in a non-technical way, and presented to end users such as environmental managers and other coastal zone stakeholders. Integrate knowledge across disciplines. Conceptual models provide a physical background upon which the understanding derived from various scientific disciplines e.

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Increase understanding. Conceptual models help users to understand the often complex processes in a system e. Identify knowledge gaps. Conceptual models can help users to identify any gaps in scientific understanding , monitoring or natural resource management plans. Help with decision making and planning.


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Facilitate participation. Conceptual models can facilitate participation of stakeholders , and assist with interaction between different stakeholder and government groups. Using models to determine indicators To develop an appropriate set of indicators to monitor an estuary there is a logical process that needs to be followed see Fig. Home Contact About. Search for: Search. Earth Surf. Landforms 43 10 : Mestdagh, S. Functional trait responses to sediment deposition reduce macrofauna-mediated ecosystem functioning in an estuarine mudflat.

Biogeosciences 15 9 : Spatio-temporal variation in contribution of biodiversity and environment to benthic ecosystem functioning in the Scheldt estuary, in : Mees, J. Moerdijk-Poortvliet, T. Production and consumption of extracellular polymeric substances in an intertidal diatom mat. Mortensen, J. Local coastal water masses control heat levels in a west Greenland tidewater outlet glacier fjord.

ASSESSING HYDRODYNAMICS IN TWO PORTUGUESE ESTUARIES: NUMERICAL MODEL COMPARISONS

Journal of Geophysical Research-Oceans 11 : Neijenhuis, P. Effects of benthic macrofauna on the oxygen and nutrient dynamics in the Oosterschelde, Zeeland. Nieuwhof, S.

The use of remote sensing to reveal landscape-scale ecosystem engineering by shellfish reefs. University of Twente: Enschede. Shellfish reefs increase water storage capacity on intertidal flats over extensive spatial scales. Ecosystems 21 2 : Methode ontwikkeling van zure suikers m. Subtidal benthic recruitment in a sub-arctic glacial fjord system: Temporal and spatial variability and potential drivers. Perry, C. Loss of coral reef growth capacity to track future increases in sea level. Nature Lond.

Estuarine & Delta Systems

Petersen, J. Biogeosciences 15 1 : Pozzato, L. Renz, J. Community bioirrigation potential BIP c , an index to quantify the potential for solute exchange at the sediment-water interface. Rix, L. Reef sponges facilitate the transfer of coral-derived organic matter to their associated fauna via the sponge loop. Salvador de Paiva, J. Understanding the conditionality of ecosystem services: The effect of tidal flat morphology and oyster reef characteristics on sediment stabilization by oyster reefs.

Schulz, K. An inversion of the estuarine circulation by sluice water discharge and its impact on suspended sediment transport.

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Schwarz, C. Self-organization of a biogeomorphic landscape controlled by plant life-history traits. Nature Geoscience 11 7 : Shi, B. Journal of Geophysical Research-Oceans 12 : — Slangen, A.

How humans and rising seas affect each other. Snelgrove, P. Global carbon cycling on a heterogeneous seafloor. Trends Ecol. Soissons, L. Seasonal and latitudinal variation in seagrass mechanical traits across Europe: The influence of local nutrient status and morphometric plasticity. Stocchi, P. W; Vermeersen, B. MIS 5e relative sea-level changes in the Mediterranean Sea: Contribution of isostatic disequilibrium. Benthic ecosystem response to polymetallic nodule extraction in the deep sea.

Ghent University: Ghent. XXV, pp.

Estuarine & Delta Systems - NIOZ

Abyssal plain faunal carbon flows remain depressed 26 years after a simulated deep-sea mining disturbance. Biogeosciences 15 13 : Has phytodetritus processing by an abyssal soft-sediment community recovered 26 years after an experimental disturbance? Recovery of Holothuroidea population density, community composition, and respiration activity after a deep-sea disturbance experiment. Living in the intertidal: desiccation and shading reduce seagrass growth, but high salinity or population of origin have no additional effect. PeerJ 6 : e Sweetman, A.

Key role of bacteria in the short-term cycling of carbon at the abyssal seafloor in a low particulate organic carbon flux region of the eastern Pacific Ocean. Taillardat, P. Assessing the contribution of porewater discharge in carbon export and CO 2 evasion in a mangrove tidal creek Can Gio, Vietnam. Taramelli, A. Indications of dynamic effects on scaling relationships between channel sinuosity and vegetation patch size across a salt marsh platform. Tarya, A.

Exposure of coastal ecosystems to river plume spreading across a near-equatorial continental shelf. Shelf Res.


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