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| 91 | "notes": "A comparison study between 10 Mediterranean lagoons has | 101 | "notes": "A comparison study between 10 Mediterranean lagoons has | ||
| 92 | been carried out by means of the 3-D numerical model SHYFEM. The | 102 | been carried out by means of the 3-D numerical model SHYFEM. The | ||
| 93 | investigated basins are the Venice and Marano-Grado lagoons in the | 103 | investigated basins are the Venice and Marano-Grado lagoons in the | ||
| 94 | Northern Adriatic Sea, the Lesina and Varano lagoons in the Southern | 104 | Northern Adriatic Sea, the Lesina and Varano lagoons in the Southern | ||
| 95 | Adriatic Sea, the Taranto basin in the Ionian Sea, the Cabras Lagoon | 105 | Adriatic Sea, the Taranto basin in the Ionian Sea, the Cabras Lagoon | ||
| 96 | in Sardinia, the Ganzirri and Faro lagoons in Sicily, the Mar Menor in | 106 | in Sardinia, the Ganzirri and Faro lagoons in Sicily, the Mar Menor in | ||
| 97 | Spain, and the Nador Lagoon in Morocco. This study has been focused on | 107 | Spain, and the Nador Lagoon in Morocco. This study has been focused on | ||
| 98 | hydrodynamics in terms of exchange rates, transport time scale, and | 108 | hydrodynamics in terms of exchange rates, transport time scale, and | ||
| 99 | mixing. Water exchange depends mainly on the inlet shape and tidal | 109 | mixing. Water exchange depends mainly on the inlet shape and tidal | ||
| 100 | range, but also on the wind regimes in the case of multi-inlet | 110 | range, but also on the wind regimes in the case of multi-inlet | ||
| 101 | lagoons. Water renewal time, which is mostly determined by the | 111 | lagoons. Water renewal time, which is mostly determined by the | ||
| 102 | exchange rate, is a powerful concept that allows lagoons to be | 112 | exchange rate, is a powerful concept that allows lagoons to be | ||
| 103 | characterized with a time scale. In the case of the studied lagoons, | 113 | characterized with a time scale. In the case of the studied lagoons, | ||
| 104 | the renewal time ranged from few days in the Marano-Grado Lagoon up to | 114 | the renewal time ranged from few days in the Marano-Grado Lagoon up to | ||
| 105 | 1 year in the case of the Mar Menor. The analysis of the renewal time | 115 | 1 year in the case of the Mar Menor. The analysis of the renewal time | ||
| 106 | frequency distribution allows identifying subbasins. The numerical | 116 | frequency distribution allows identifying subbasins. The numerical | ||
| 107 | study proved to be a useful tool for the intercomparison and | 117 | study proved to be a useful tool for the intercomparison and | ||
| 108 | classification of the lagoons. These environments range from a leaky | 118 | classification of the lagoons. These environments range from a leaky | ||
| 109 | type to a choked type of lagoons and give a representative picture of | 119 | type to a choked type of lagoons and give a representative picture of | ||
| 110 | the lagoons situated around the Mediterranean basin. Mixing efficiency | 120 | the lagoons situated around the Mediterranean basin. Mixing efficiency | ||
| 111 | turns out to be a function of the morphological complexity, but also | 121 | turns out to be a function of the morphological complexity, but also | ||
| 112 | of the forcings acting on the system.", | 122 | of the forcings acting on the system.", | ||
| 113 | "notes_translated": { | 123 | "notes_translated": { | ||
| 114 | "es": "A comparison study between 10 Mediterranean lagoons has | 124 | "es": "A comparison study between 10 Mediterranean lagoons has | ||
| 115 | been carried out by means of the 3-D numerical model SHYFEM. The | 125 | been carried out by means of the 3-D numerical model SHYFEM. The | ||
| 116 | investigated basins are the Venice and Marano-Grado lagoons in the | 126 | investigated basins are the Venice and Marano-Grado lagoons in the | ||
| 117 | Northern Adriatic Sea, the Lesina and Varano lagoons in the Southern | 127 | Northern Adriatic Sea, the Lesina and Varano lagoons in the Southern | ||
| 118 | Adriatic Sea, the Taranto basin in the Ionian Sea, the Cabras Lagoon | 128 | Adriatic Sea, the Taranto basin in the Ionian Sea, the Cabras Lagoon | ||
| 119 | in Sardinia, the Ganzirri and Faro lagoons in Sicily, the Mar Menor in | 129 | in Sardinia, the Ganzirri and Faro lagoons in Sicily, the Mar Menor in | ||
| 120 | Spain, and the Nador Lagoon in Morocco. This study has been focused on | 130 | Spain, and the Nador Lagoon in Morocco. This study has been focused on | ||
| 121 | hydrodynamics in terms of exchange rates, transport time scale, and | 131 | hydrodynamics in terms of exchange rates, transport time scale, and | ||
| 122 | mixing. Water exchange depends mainly on the inlet shape and tidal | 132 | mixing. Water exchange depends mainly on the inlet shape and tidal | ||
| 123 | range, but also on the wind regimes in the case of multi-inlet | 133 | range, but also on the wind regimes in the case of multi-inlet | ||
| 124 | lagoons. Water renewal time, which is mostly determined by the | 134 | lagoons. Water renewal time, which is mostly determined by the | ||
| 125 | exchange rate, is a powerful concept that allows lagoons to be | 135 | exchange rate, is a powerful concept that allows lagoons to be | ||
| 126 | characterized with a time scale. In the case of the studied lagoons, | 136 | characterized with a time scale. In the case of the studied lagoons, | ||
| 127 | the renewal time ranged from few days in the Marano-Grado Lagoon up to | 137 | the renewal time ranged from few days in the Marano-Grado Lagoon up to | ||
| 128 | 1 year in the case of the Mar Menor. The analysis of the renewal time | 138 | 1 year in the case of the Mar Menor. The analysis of the renewal time | ||
| 129 | frequency distribution allows identifying subbasins. The numerical | 139 | frequency distribution allows identifying subbasins. The numerical | ||
| 130 | study proved to be a useful tool for the intercomparison and | 140 | study proved to be a useful tool for the intercomparison and | ||
| 131 | classification of the lagoons. These environments range from a leaky | 141 | classification of the lagoons. These environments range from a leaky | ||
| 132 | type to a choked type of lagoons and give a representative picture of | 142 | type to a choked type of lagoons and give a representative picture of | ||
| 133 | the lagoons situated around the Mediterranean basin. Mixing efficiency | 143 | the lagoons situated around the Mediterranean basin. Mixing efficiency | ||
| 134 | turns out to be a function of the morphological complexity, but also | 144 | turns out to be a function of the morphological complexity, but also | ||
| 135 | of the forcings acting on the system." | 145 | of the forcings acting on the system." | ||
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| 292 | "title_translated": { | 302 | "title_translated": { | ||
| 293 | "es": "Comparative hydrodynamics of 10 Mediterranean lagoons by | 303 | "es": "Comparative hydrodynamics of 10 Mediterranean lagoons by | ||
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