COSMOS-Europe : a European network of cosmic-ray neutron soil moisture sensors

We thank TERENO (Terrestrial Environmental Observatories), funded by the Helmholtz-Gemeinschaft for the financing and maintenance of CRNS stations. We acknowledge financial support by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) of the research unit FOR 2694 Cosmic Sense (grant no. 357874777) and by the German Federal Ministry of Education of the Research BioökonomieREVIER, Digitales Geosystem – Rheinisches Revier project (grant no. 031B0918A). COSMOS-UK has been supported financially by the UK’s Natural Environment Research Council (grant no. NE/R016429/1). The Olocau experimental watershed is partially supported by the Spanish Ministry of Science and Innovation through the research project TETISCHANGE (grant no. RTI2018-093717-BI00). The Calderona experimental site is partially supported by the Spanish Ministry of Science and Innovation through the research projects CEHYRFO-MED (grant no. CGL2017-86839- C3-2-R) and SILVADAPT.NET (grant no. RED2018-102719-T) and the LIFE project RESILIENT FORESTS (grant no. LIFE17 CCA/ES/000063). The University of Bristol’s Sheepdrove sites have been supported by the UK’s Natural Environment Research Council through a number of projects (grant nos. NE/M003086/1, NE/R004897/1, and NE/T005645/1) and by the International Atomic Energy Agency of the United Nations (grant no. CRP D12014). Acknowledgements. We thank Peter Strauss and Gerhab Rab from the Institute for Land and Water Management Research, Federal Agency for Water Management Austria, Petzenkirchen, Austria. We thank Trenton Franz from the School of Natural Resources, University of Nebraska–Lincoln, Lincoln, NE, United States. We also thank Carmen Zengerle, Mandy Kasner, Felix Pohl, and Solveig Landmark, UFZ Leipzig, for supporting field calibration, lab analysis, and data processing. We furthermore thank Daniel Dolfus, Marius Schmidt, Ansgar Weuthen, and Bernd Schilling, Forschungszentrum Jülich, Germany. The COSMOS-UK project team is thanked for making its data available to COSMOS-Europe. Luca Stevanato is thanked for the technical details about the Finapp sensor. The stations at Cunnersdorf, Lindenberg, and Harzgerode have been supported by Falk Böttcher, Frank Beyrich, and Petra Fude, German Weather Service (DWD). The Zerbst site has been supported by Getec Green Energy GmbH and Jörg Kachelmann (Meteologix AG). The CESBIO sites have been supported by the CNES TOSCA program. The ERA5-Land data are provided by ECMWF (Muñoz Sabater, 2021). The Jena dataset was retrieved at the site of The Jena Experiment, operated by DFG research unit FOR 1451.Peer reviewedPublisher PD

Surface circulation in the KwaZulu-Natal Bight and its impact on the connectivity of marine protected areas

The KwaZulu-Natal Bight is a small, coastal region along South Africa's north-east coast. It stretches from Richards Bay to Durban and has a wide shelf compared to the surrounding coastline. As a result, the Agulhas Current is forced offshore, allowing the formation of complex circulation features on the KwaZulu-Natal Bight's shelf that assist with recruitment and retention of marine organisms in this region. This study aims to gain a deeper understanding of the surface circulation within the KwaZulu-Natal Bight and its impact on the connectivity between several surrounding Marine Protected Areas. These include iSimangaliso, uThukela Banks, Aliwal Shoal and Protea Banks and the information about their connectivity contributes to the CAPTOR (Connectivity And disPersal beTween prOtected aReas) project. The aim of this study is met by using high-resolution CROCO model output over a 10-year period, in combination with particle tracking tools, wind and surface drifter data. According to the model's mean circulation, the KwaZulu-Natal Bight's surface currents have a strong south-westward flow on the continental shelf slope where the effects of the Agulhas Current are strongly felt, butare weak and variable on the shelf. Observed variabilities of the mean flow have no distinct seasonal pattern and include a north- eastward current that repeatedly dominates the shelf. It is referred to as the Natal Bight Coastal Counter Current, which originates within the semi-permanent Durban Eddy in the southern KwaZulu- Natal Bight, where it extends throughout the water column. The Natal Bight Coastal Counter Current stretches along the mid-shelf into the northern KwaZulu-Natal Bight, gradually becoming shallower, weaker and narrower. When anticyclonic eddies offshore of the Agulhas Current pass this region, they occasionally replace the Durban Eddy and its associated Natal Bight Coastal Counter Current with a southward flow on the KwaZulu-Natal Bight's shelf. Therefore, the circulation in the KwaZulu-Natal Bight appears to be primarily driven by perturbations at the Agulhas Current front. However, there is also some indication of a direct wind-driven influence in coastal waters inshore of the 50 m isobath. To investigate the impact of the KwaZulu-Natal Bight's circulation on the connectivity between the above-mentioned Marine Protected Areas, particle tracking tools are used. Virtual particles are released in each Marine Protected Area within the model, during multiple northward and southward KwaZulu-Natal Bight surface circulation events. Their pathways are tracked for 30 days and reveal an overall strong southward Marine Protected Area connectivity, which is driven by the Agulhas Current, while a northward connection is less commonly observed. The northward flow of the Natal Bight Coastal Counter Current increases the water retention within uThukela Banks, but it does not extend into iSimangaliso to establish a northward Marine Protected Area connection. However, when the Natal Bight Coastal Counter Current originates within Aliwal Shoal, it may result in a northward Marine Protected Area connection between Aliwal Shoal and uThukela Banks. In this study, the virtual particles represent passively drifting larvae that are buoyant. To make these simulations more realistic, the virtual particles should be able to sink and appropriate swimming behaviours could be considered. However, swimming abilities will likely be overpowered by the surrounding circulation and observations on these behaviours are difficult to make. Therefore, the passive dispersion used in this study to mimic their trajectories may be sufficient and provides valuable insight into the impact of the KwaZulu-Natal Bight's surface circulation on Marine Protected Area connectivity and larval dispersion. The virtual particle tracking tools used in this study are not limited to biological applications. Future studies could use them to investigate the path and accumulation regions of virtual pollutants, such as microplastics, to determine the regions in which clean-ups would be most effective

The Natal Bight Coastal Counter-Current: A modeling study

International audienceOutput from a high-resolution ocean model, a wind reanalysis and a particle tracking tool are used to improve our understanding of the shelf circulation in an embayment off South Africa's east coast, known as the KwaZulu-Natal Bight. This region spans across roughly 140 km of coastline and is located between 29°S and 30°S. It is influenced by the strong, south-westward flowing Agulhas Current on its offshore edge, while its shelf is dominated by weak and variable currents. On the KwaZulu-Natal Bight's shelf, realistic high-resolution model simulations indicate the presence of a mean north-eastward flow: the Natal Bight Coastal Counter-Current. The mean surface circulation depicts a Natal Bight Coastal Counter Current stretching along the 50 m isobath from the southern to the northern section of the KwaZulu-Natal Bight while progressively becoming narrower and weaker northwards. The mean vertical structure of this counter current extends throughout the water column and at its origin, it almost connects with the Agulhas Undercurrent. In this region, the Natal Bight Coastal Counter-Current is about 20 km wide and has an average speed of 20 cm/s at its core, which may exceed 100 cm/s during individual events. The passage of southward propagating anticyclonic eddies offshore of the Agulhas Current are associated with a southward flow along the southern KwaZulu-Natal Bight region and the interruption of the otherwise north-eastward shelf currents. While the circulation in the KwaZulu-Natal Bight is primarily driven by perturbations at the Agulhas Current front, there is also some indication of a direct wind-driven influence in coastal waters, inshore of the 50 m isobath and north of 29.5°S. Virtual particle tracking experiments show that the Natal Bight Coastal Counter Current may increase connectivity between Marine Protected Areas within the KwaZulu-Natal Bight, where the current greatly increases the water retention. This may trap nutrients from coastal origins on the shelf, together with any suspended particles such as larvae. Therefore, the Natal Bight Coastal Counter-Current has the potential to increase the suitability of this habitat for larval settlement

DataSheet_2_Performance of European oysters (Ostrea edulis L.) in the Dutch North Sea, across five restoration pilots.csv

IntroductionThe European flat oyster (Ostrea edulis) is a biogenic reef former, internationally recognised as threatened and declining in the NE Atlantic by OSPAR and one of the focal species in nature inclusive designs in offshore windfarms in The Netherlands. Oyster reefs offer habitat to many other benthic hard substrate and fish species and provide ecosystem functions such as shelter and feeding grounds. European flat oyster reefs have disappeared from the Dutch North Sea in the early 1900s due to overfishing and diseases but are now subject of nature restoration under the Dutch Marine Strategy.MethodSince 2018, pilot projects have started in the Dutch North Sea to restore European flat oysters at suitable locations, such as offshore windfarms or natural reefs, which are protected from bottom trawling. We compared European flat oyster performance in five pilot projects, using translocated adult oysters sourced from Ireland, Norway, and the Netherlands. The aim of this research was to assess the performance of translocated oysters between pilots, to assess the installation and monitoring techniques, and to come forward with recommendations for future pilot projects.ResultsWe found that translocation of both foreign sourced flat oyster populations (Ireland and Norway in nearshore and offshore areas) and local oysters (in nearshore areas) result in good oyster performance. Oysters were able to grow (max 3.67 mm/month) and reproduce (larvae present) in their new environment. We found that growth rate was explained by origin and average water temperature, to a lesser extent by number of months, location and salinity and not to other environmental factors such as pH and O2. Correlations between growth and environmental conditions need to be considered with caution, since not all pilots were sampled just before and after the growing season. Oysters were Bonamia-negative at the start and end of the pilots, indicating that the offshore Dutch North Sea is still Bonamia-free.Discussion, conclusions, recommendationsBy the year 2050 more than ten new offshore farms will be constructed in the Dutch North Sea and some sites will be suitable for oyster restoration. We conclude that local and foreign sourced oysters performed well at all locations. Based on the success and failure of the different outplacement and monitoring techniques, we provide recommendations on good practice for the future, including developing standardized monitoring protocols. This will enable better inter-site comparisons in upcoming oyster restoration pilots.</p

Table_1_Performance of European oysters (Ostrea edulis L.) in the Dutch North Sea, across five restoration pilots.docx

IntroductionThe European flat oyster (Ostrea edulis) is a biogenic reef former, internationally recognised as threatened and declining in the NE Atlantic by OSPAR and one of the focal species in nature inclusive designs in offshore windfarms in The Netherlands. Oyster reefs offer habitat to many other benthic hard substrate and fish species and provide ecosystem functions such as shelter and feeding grounds. European flat oyster reefs have disappeared from the Dutch North Sea in the early 1900s due to overfishing and diseases but are now subject of nature restoration under the Dutch Marine Strategy.MethodSince 2018, pilot projects have started in the Dutch North Sea to restore European flat oysters at suitable locations, such as offshore windfarms or natural reefs, which are protected from bottom trawling. We compared European flat oyster performance in five pilot projects, using translocated adult oysters sourced from Ireland, Norway, and the Netherlands. The aim of this research was to assess the performance of translocated oysters between pilots, to assess the installation and monitoring techniques, and to come forward with recommendations for future pilot projects.ResultsWe found that translocation of both foreign sourced flat oyster populations (Ireland and Norway in nearshore and offshore areas) and local oysters (in nearshore areas) result in good oyster performance. Oysters were able to grow (max 3.67 mm/month) and reproduce (larvae present) in their new environment. We found that growth rate was explained by origin and average water temperature, to a lesser extent by number of months, location and salinity and not to other environmental factors such as pH and O2. Correlations between growth and environmental conditions need to be considered with caution, since not all pilots were sampled just before and after the growing season. Oysters were Bonamia-negative at the start and end of the pilots, indicating that the offshore Dutch North Sea is still Bonamia-free.Discussion, conclusions, recommendationsBy the year 2050 more than ten new offshore farms will be constructed in the Dutch North Sea and some sites will be suitable for oyster restoration. We conclude that local and foreign sourced oysters performed well at all locations. Based on the success and failure of the different outplacement and monitoring techniques, we provide recommendations on good practice for the future, including developing standardized monitoring protocols. This will enable better inter-site comparisons in upcoming oyster restoration pilots.</p

DataSheet_1_Performance of European oysters (Ostrea edulis L.) in the Dutch North Sea, across five restoration pilots.csv

IntroductionThe European flat oyster (Ostrea edulis) is a biogenic reef former, internationally recognised as threatened and declining in the NE Atlantic by OSPAR and one of the focal species in nature inclusive designs in offshore windfarms in The Netherlands. Oyster reefs offer habitat to many other benthic hard substrate and fish species and provide ecosystem functions such as shelter and feeding grounds. European flat oyster reefs have disappeared from the Dutch North Sea in the early 1900s due to overfishing and diseases but are now subject of nature restoration under the Dutch Marine Strategy.MethodSince 2018, pilot projects have started in the Dutch North Sea to restore European flat oysters at suitable locations, such as offshore windfarms or natural reefs, which are protected from bottom trawling. We compared European flat oyster performance in five pilot projects, using translocated adult oysters sourced from Ireland, Norway, and the Netherlands. The aim of this research was to assess the performance of translocated oysters between pilots, to assess the installation and monitoring techniques, and to come forward with recommendations for future pilot projects.ResultsWe found that translocation of both foreign sourced flat oyster populations (Ireland and Norway in nearshore and offshore areas) and local oysters (in nearshore areas) result in good oyster performance. Oysters were able to grow (max 3.67 mm/month) and reproduce (larvae present) in their new environment. We found that growth rate was explained by origin and average water temperature, to a lesser extent by number of months, location and salinity and not to other environmental factors such as pH and O2. Correlations between growth and environmental conditions need to be considered with caution, since not all pilots were sampled just before and after the growing season. Oysters were Bonamia-negative at the start and end of the pilots, indicating that the offshore Dutch North Sea is still Bonamia-free.Discussion, conclusions, recommendationsBy the year 2050 more than ten new offshore farms will be constructed in the Dutch North Sea and some sites will be suitable for oyster restoration. We conclude that local and foreign sourced oysters performed well at all locations. Based on the success and failure of the different outplacement and monitoring techniques, we provide recommendations on good practice for the future, including developing standardized monitoring protocols. This will enable better inter-site comparisons in upcoming oyster restoration pilots.</p