Abstract
The eruptive phase of a submarine volcano located 2 km away from the southern coast of El Hierro Island started on October 2011. This extraordinary event provoked a dramatic perturbation of the water column. In order to understand and quantify the environmental impacts caused, a regular multidisciplinary monitoring was carried out using remote sensing sensors. In this context, we performed the systematic processing of every MODIS and MERIS and selected high resolution Worldview-2 imagery to provide information on the concentration of a number of biological, physical and chemical parameters. On the other hand, the eruption provided an exceptional source of tracer that allowed the study a variety of oceanographic structures. Specifically, the Canary Islands belong to a very active zone of long-lived eddies. Such structures are usually monitored using sea level anomaly fields. However these products have coarse spatial resolution and they are not suitable to perform submesoscale studies. Thanks to the volcanic tracer, detailed studies were undertaken with ocean colour imagery allowing, using the diffuse attenuation coefficient, to monitor the process of filamentation and axisymmetrization predicted by theoretical studies and numerical modelling. In our work, a novel 2-step segmentation methodology has been developed. The approach incorporates different segmentation algorithms and region growing techniques. In particular, the first step obtains an initial eddy segmentation using thresholding or clustering methods and, next, the fine detail is achieved by the iterative identification of the points to grow and the subsequent application of watershed or thresholding strategies. The methodology has demonstrated an excellent performance and robustness and it has proven to properly capture the eddy and its filaments.
Highlights
Mesoscalar oceanic eddies are ubiquitous structures that can be found anywhere in the world’s oceans, with a predominance of anticyclonic over cyclonic vortexes [1]
Satellite data from AQUA/TERRA-Moderate-resolution Imaging Spectroradiometer (MODIS) and ENVISAT-MERIS sensors have been the main source of remote sensing image information for monitoring El Hierro submarine volcanic processes
MERIS data with the goal to get different water quality products in order to quantify environmental impacts caused by the submarine eruption of El Hierro Island
Summary
Mesoscalar oceanic eddies are ubiquitous structures that can be found anywhere in the world’s oceans, with a predominance of anticyclonic over cyclonic vortexes [1]. In the North East Atlantic Ocean, the presence of the Canary Archipelago acts as an obstacle to the oceanic and atmospheric flows, originating a rich mesoscale variability mainly represented by anticyclonic and cyclonic eddies spun off from the islands’ flanks [5,6]. The mechanisms of such variability are invoked through the perturbation of the Canary Current and Trades Winds by the tall topography islands such as El Hierro [7].
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