Abstract

<p>Currently hydrological models are not generally coupled to coastal and regional ocean models because, even if regarded as a powerful and useful tool, they do not fully accomplish to estimate accurately the right volume of water reaching the coastal zone for many reasons including water management activities such as human consumption, irrigation, etc. For this reason, many coastal and ocean models continue to use river climatologies as boundary conditions for representing such an active boundary. Furthermore, continuous salinity observations in the coastal area are scarce and sensors are highly unreliable while current Earth Observation (EO) products for salinity poorly represents the coastal gradients.</p><p>In this presentation, the current state-of-the-art and the results of the LAMBDA Project (λ) (LAnd-Marine Boundary Development and Analysis) will be shown. The main aim of the project was to demonstrate an improvement in the thermohaline circulation in coastal areas by a better characterisation of the land-marine boundary conditions, with special regard to the salinity fields. The LAMBDA project analysed the opportunity of improving the land-marine boundary conditions by exploring the capacities of state-of-the-art hydrologic models. In order to achieve those objectives, the project strategy used an integrated approach that went from watershed models to validation in the coastal area by fit-for-purpose EO products, developed by SMOS, and passing through methods and proxies for integrating the freshwater flows into regional mesoscale grids. The watershed and estuarine proxies were modelled using the MOHID Water modelling system (http://www.mohid.com/) an open source model capable of simulating a wide range of processes, i.e. hydrodynamics, transport, water quality, oil spills, in surface water bodies (oceans, coastal areas, estuaries and reservoirs).</p><p>The project products were evaluated in Portugal Continental waters, tested in CMEMS regional products and evaluated by local experts in Germany, Ireland, Portugal, UK and Spain.</p>

Highlights

  • Background map layerLAMBDA products The user can select one item only

  • ▪ The present methodology can complete temporally, spatially and cover the data gaps provided by monitoring equipment and field surveys in fresh water, estuarine and ocean environment to produce forecasts

  • ▪ The set of numerical tools implemented in the LAMBDA project significantly improve salinity fields and aid to the delimitation of region of freshwater influence and salinity fronts which are relevant to coastal activities management

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Summary

Conclusions from watershed modelling

Best results are obtained from higher resolution and single watershed domains. Meteorological forcing from ERA5 is inadequate in Germany, but adequate everywhere else. Rivers without available observations can not be further calibrated. Proxy consist on basic 2D MOHID Water configuration with 10x3 cells domain Modelled Temperature. Stats MOHID 2D estuary proxy (LAMBDA) vs observed: R2 = 0.65, RMSE = 3.50,, MAE = 2.60. Slides describe the LAMBDA boundary conditions and show some results from the different scenarios during the month of February and an extreme event in late March 2018. V1 product; Complete: best forcing conditions: Observed data corrected by Guadalquivir estuarine proxy at 6 estuaries. Forcing completed with other 45 direct discharges with modelled temperature and constant. ▪ January and February salinity drop overrepresented in the direct discharge scenarios (Observed, LAMBDA_V1 and Climatology). Same situation for temperature, January and February temperature drops in excess in the direct discharge scenarios (Observed, LAMBDA_V1 and Climatology). The complete scenario is the one that recovers better the temperature while other scenarios are lower than observations

A Guarda Meridional velocity
Conclusions
Methods for validation
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