Abstract:The Vaccarès Lagoon System, located in the central part of the Rhône Delta (France), is a complex shallow coastal lagoon, exposed to a typical Mediterranean climate and a specific hydrological regime affected by man-controlled exchanges with the sea and agricultural drainage channels. In this article, we report the results obtained by a series of monitoring programs, with different spatial and temporal resolutions. Long-term datasets from 1999 to 2019 with data collected on a monthly basis and a high spatial r… Show more
“…Depending on the nature (hydraulic works, natural connection) and the characteristics of their connections with the sea, their watersheds or surrounding rivers, shallow coastal lagoons can exhibit very significant spatial and temporal heterogeneity in both salinity and water level. The importance of implementing different monitoring strategies to understand the hydrosaline functioning of these lagoons is reported in the recent literature [11].…”
Section: Discussionmentioning
confidence: 99%
“…An interesting aspect that emerged is the differentiation of the three probes with more defined conditions corresponding respectively to a stronger influence of fresh water input for the nearest position (P1) and a stronger influence of tide for the outermost position (P3), while more variable conditions were collected for the intermediate station (P2). Continuous measurements allow the acquisition of critical data for the development, calibration and validation of hydrodynamic models that can provide additional information on the hydro-saline functioning of lagoons [11,15,[45][46][47][48][49].…”
Section: Discussionmentioning
confidence: 99%
“…On the other hand, spatially-distributed profiles are also particularly useful for the validation of numerical modeling results in terms of spatial distribution of salinity patterns [11,15].…”
Section: Discussionmentioning
confidence: 99%
“…Salinity conditions are related to a complex interaction between different hydrological processes that involve discharge of fresh water, tidal regime and the exchanges with the sea, precipitation, interaction with the atmosphere (e.g., heat flux, evaporation rates) and wind-driven forces, which vary over a wide range of time-scales and that become relevant for really shallow waters, resulting in strong daily and seasonal variability [9,10]. All these drivers contribute to the high diversity in terms of salinity conditions between Mediterranean lagoons, ranging from oligohaline to hyperhaline waters [11].…”
Section: Introductionmentioning
confidence: 99%
“…During the different phases of this adaptive management approach, an intensive monitoring and modeling activity was carried out to support the assessment of the success of the implemented measures and of the identified mitigation actions. In microtidal lagoons, this monitoring activity needs to integrate different strategies able to capture, with the best resolution in time and space, variations of water levels, flows and salinity that are often encountered [11].…”
Large lagoons usually show a salinity gradient due to fresh water tributaries with inner areas characterized by lower mean values and higher fluctuation of salinity than seawater-dominated areas. In the Venice Lagoon, this ecotonal environment, characterized in the past by oligo-mesohaline waters and large intertidal areas vegetated by reedbeds, was greatly reduced by historical human environmental modifications, including the diversion of main rivers outside the Venice Lagoon. The reduction of the fresh water inputs caused a marinization of the lagoon, with an increase in salinity and the loss of the related habitats, biodiversity, and ecosystem services. To counteract this issue, conservation actions, such as the construction of hydraulic infrastructures for the introduction and the regulation of a fresh water flow, can be implemented. The effectiveness of these actions can be preliminarily investigated and then verified through the combined implementation of environmental monitoring and numerical modeling. Through the results of the monitoring activity carried out in Venice Lagoon in the framework of the Life Lagoon Refresh (LIFE16NAT/IT/000663) project, the study of salinity is shown to be a successful and robust combination of different types of monitoring techniques. In particular, the characterization of salinity is obtained by the acquisition of continuous data, field campaigns, and numerical modeling.
“…Depending on the nature (hydraulic works, natural connection) and the characteristics of their connections with the sea, their watersheds or surrounding rivers, shallow coastal lagoons can exhibit very significant spatial and temporal heterogeneity in both salinity and water level. The importance of implementing different monitoring strategies to understand the hydrosaline functioning of these lagoons is reported in the recent literature [11].…”
Section: Discussionmentioning
confidence: 99%
“…An interesting aspect that emerged is the differentiation of the three probes with more defined conditions corresponding respectively to a stronger influence of fresh water input for the nearest position (P1) and a stronger influence of tide for the outermost position (P3), while more variable conditions were collected for the intermediate station (P2). Continuous measurements allow the acquisition of critical data for the development, calibration and validation of hydrodynamic models that can provide additional information on the hydro-saline functioning of lagoons [11,15,[45][46][47][48][49].…”
Section: Discussionmentioning
confidence: 99%
“…On the other hand, spatially-distributed profiles are also particularly useful for the validation of numerical modeling results in terms of spatial distribution of salinity patterns [11,15].…”
Section: Discussionmentioning
confidence: 99%
“…Salinity conditions are related to a complex interaction between different hydrological processes that involve discharge of fresh water, tidal regime and the exchanges with the sea, precipitation, interaction with the atmosphere (e.g., heat flux, evaporation rates) and wind-driven forces, which vary over a wide range of time-scales and that become relevant for really shallow waters, resulting in strong daily and seasonal variability [9,10]. All these drivers contribute to the high diversity in terms of salinity conditions between Mediterranean lagoons, ranging from oligohaline to hyperhaline waters [11].…”
Section: Introductionmentioning
confidence: 99%
“…During the different phases of this adaptive management approach, an intensive monitoring and modeling activity was carried out to support the assessment of the success of the implemented measures and of the identified mitigation actions. In microtidal lagoons, this monitoring activity needs to integrate different strategies able to capture, with the best resolution in time and space, variations of water levels, flows and salinity that are often encountered [11].…”
Large lagoons usually show a salinity gradient due to fresh water tributaries with inner areas characterized by lower mean values and higher fluctuation of salinity than seawater-dominated areas. In the Venice Lagoon, this ecotonal environment, characterized in the past by oligo-mesohaline waters and large intertidal areas vegetated by reedbeds, was greatly reduced by historical human environmental modifications, including the diversion of main rivers outside the Venice Lagoon. The reduction of the fresh water inputs caused a marinization of the lagoon, with an increase in salinity and the loss of the related habitats, biodiversity, and ecosystem services. To counteract this issue, conservation actions, such as the construction of hydraulic infrastructures for the introduction and the regulation of a fresh water flow, can be implemented. The effectiveness of these actions can be preliminarily investigated and then verified through the combined implementation of environmental monitoring and numerical modeling. Through the results of the monitoring activity carried out in Venice Lagoon in the framework of the Life Lagoon Refresh (LIFE16NAT/IT/000663) project, the study of salinity is shown to be a successful and robust combination of different types of monitoring techniques. In particular, the characterization of salinity is obtained by the acquisition of continuous data, field campaigns, and numerical modeling.
Human activities are not only increasing salinization of rivers, they might also be altering the temporal dynamics of salinity. Here, we assess the effect of human activities on the temporal dynamics of electrical conductivity (EC) in 91 Spanish rivers using daily measures of EC from 2007 to 2011. We expected rivers weakly affected by human activities to have low and constant ECs, whereas rivers strongly affected by human activities should have high and variable ECs throughout the year. We collected information on land use, climate, and geology that could explain the spatiotemporal variation in EC. We identified four groups of rivers with differences in EC trends that covered a gradient of anthropogenic pressure. According to Random Forest analysis, temporal EC patterns were mainly driven by agriculture, but de-icing roads, mining, and wastewater discharges were also important to some extent. Linear regressions showed a moderate relationship between EC variability and precipitation, and a weak relationship to geology. Overall, our results show strong evidence that human activities disrupt the temporal dynamics of EC. This could have strong effects on aquatic biodiversity (e.g., aquatic organisms might not adapt to frequent and unpredictable salinity peaks) and should be incorporated into monitoring and management plans.
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