scholarly journals The Mediterranean Sea system: a review and an introduction to the special issue

Ocean Science ◽  
2013 ◽  
Vol 9 (5) ◽  
pp. 789-803 ◽  
Author(s):  
T. Tanhua ◽  
D. Hainbucher ◽  
K. Schroeder ◽  
V. Cardin ◽  
M. Álvarez ◽  
...  

Abstract. The Mediterranean Sea is a semi-enclosed sea characterized by high salinities, temperatures and densities. The net evaporation exceeds the precipitation, driving an anti-estuarine circulation through the Strait of Gibraltar, contributing to very low nutrient concentrations. The Mediterranean Sea has an active overturning circulation, one shallow cell that communicates directly with the Atlantic Ocean, and two deep overturning cells, one in each of the two main basins. It is surrounded by populated areas and is thus sensitive to anthropogenic forcing. Several dramatic changes in the oceanographic and biogeochemical conditions have been observed during the past several decades, emphasizing the need to better monitor and understand the changing conditions and their drivers. During 2011 three oceanographic cruises were conducted in a coordinated fashion in order to produce baseline data of important physical and biogeochemical parameters that can be compared to historic data and be used as reference for future observational campaigns. In this article we provide information on the Mediterranean Sea oceanographic situation, and present a short review that will serve as background information for the special issue in Ocean Science on "Physical, chemical and biological oceanography of the Mediterranean Sea". An important contribution of this article is the set of figures showing the large-scale distributions of physical and chemical properties along the full length of the Mediterranean Sea.

2013 ◽  
Vol 10 (2) ◽  
pp. 581-617 ◽  
Author(s):  
T. Tanhua ◽  
D. Hainbucher ◽  
K. Schröder ◽  
V. Cardin ◽  
M. Álvarez ◽  
...  

Abstract. The Mediterranean is a semi-enclosed sea characterized by high salinities, temperatures and densities. The net evaporation exceeds the precipitation, driving an anti-estuarine circulation through the Strait of Gibraltar, contributing to very low nutrient concentrations. The Mediterranean Sea has an active overturning circulation, one shallow cell that communicates directly with the Atlantic Ocean, and two deep overturning cells, one in each of the two main basins. It is surrounded by populated areas and is thus sensitive to anthropogenic forcing. Several dramatic changes in the oceanographic and biogeochemical conditions have been observed during the past several decades, emphasising the need to better monitor and understand the changing conditions and their drivers. During 2011 three oceanographic cruises were conducted in a coordinated fashion in order to produce base-line data of important physical and biogeochemical parameters that can be compared to historic data and be used as reference for future observational campaigns. In this article we provide information on the Mediterranean Sea oceanographic situation, and present a short review that will serve as background information for the special issue in Ocean Science on "Physical, chemical and biological oceanography of the Mediterranean Sea". An important contribution of this article is the set of figures showing the large-scale distributions of physical and chemical properties along the full length of the Mediterranean Sea.


2021 ◽  
Author(s):  
Alba de la Vara ◽  
William Cabos ◽  
Dmitry V. Sein ◽  
Claas Teichmann ◽  
Daniela Jacob

AbstractIn this work we use a regional atmosphere–ocean coupled model (RAOCM) and its stand-alone atmospheric component to gain insight into the impact of atmosphere–ocean coupling on the climate change signal over the Iberian Peninsula (IP). The IP climate is influenced by both the Atlantic Ocean and the Mediterranean sea. Complex interactions with the orography take place there and high-resolution models are required to realistically reproduce its current and future climate. We find that under the RCP8.5 scenario, the generalized 2-m air temperature (T2M) increase by the end of the twenty-first century (2070–2099) in the atmospheric-only simulation is tempered by the coupling. The impact of coupling is specially seen in summer, when the warming is stronger. Precipitation shows regionally-dependent changes in winter, whilst a drier climate is found in summer. The coupling generally reduces the magnitude of the changes. Differences in T2M and precipitation between the coupled and uncoupled simulations are caused by changes in the Atlantic large-scale circulation and in the Mediterranean Sea. Additionally, the differences in projected changes of T2M and precipitation with the RAOCM under the RCP8.5 and RCP4.5 scenarios are tackled. Results show that in winter and summer T2M increases less and precipitation changes are of a smaller magnitude with the RCP4.5. Whilst in summer changes present a similar regional distribution in both runs, in winter there are some differences in the NW of the IP due to differences in the North Atlantic circulation. The differences in the climate change signal from the RAOCM and the driving Global Coupled Model show that regionalization has an effect in terms of higher resolution over the land and ocean.


2007 ◽  
Vol 37 (2) ◽  
pp. 338-358 ◽  
Author(s):  
Ichiro Fukumori ◽  
Dimitris Menemenlis ◽  
Tong Lee

Abstract A new basin-wide oscillation of the Mediterranean Sea is identified and analyzed using sea level observations from the Ocean Topography Experiment (TOPEX)/Poseidon satellite altimeter and a numerical ocean circulation model. More than 50% of the large-scale, nontidal, and non-pressure-driven variance of sea level can be attributed to this oscillation, which is nearly uniform in phase and amplitude across the entire basin. The oscillation has periods ranging from 10 days to several years and has a magnitude as large as 10 cm. The model suggests that the fluctuations are driven by winds at the Strait of Gibraltar and its neighboring region, including the Alboran Sea and a part of the Atlantic Ocean immediately to the west of the strait. Winds in this region force a net mass flux through the Strait of Gibraltar to which the Mediterranean Sea adjusts almost uniformly across its entire basin with depth-independent pressure perturbations. The wind-driven response can be explained in part by wind setup; a near-stationary balance is established between the along-strait wind in this forcing region and the sea level difference between the Mediterranean Sea and the Atlantic Ocean. The amplitude of this basin-wide wind-driven sea level fluctuation is inversely proportional to the setup region’s depth but is insensitive to its width including that of Gibraltar Strait. The wind-driven fluctuation is coherent with atmospheric pressure over the basin and contributes to the apparent deviation of the Mediterranean Sea from an inverse barometer response.


2021 ◽  
Author(s):  
David Crookall ◽  
Isabel Caballero-Leiva ◽  
Laksh Sharma ◽  
Pimnutcha Promduangsri ◽  
Pariphat Promduangsri

<p>Modern, educational simulation/games (s/g) have a rich legacy, stretching back to the 1960s.  They are used today for communicating science in educational, environmental or governmental organizations.  Other uses are to help groups and organizations conduct research, solve complex problems or make collective decisions.</p><p>Over the last two decades, a particularly powerful, but underused, form of s/g has developed, called participatory simulation (PS).  It contains (elements of) game, simulation, role-play, experience, human interaction, decision-making, negotiation, engagement, stakeholder, etc.  It is often large scale, open ended, goal and results oriented, free form and data driven.  Of course, debriefing is a crucial component.</p><p>Last summer (2020), the International Oceans-Climate School (IOCS), of the Ocean Open University (OOP), France, planned to organize an in-person summer school with a PS as its capstone event.  We then postponed and made it an autumn school.  It then became clear that this also was impossible, and so, after some hesitation, we scrambled to turn it into an online PS (OPS).</p><p>The theme was “<em>The Mediterranean and climate change: Impacts, people, action</em>”.  Our overarching goal was to help participants understand the <strong>oceans-climate nexus</strong> and to become better <strong>ocean-climate-literate stakeholders</strong>.  The IOCS is an official event of the <strong>Intergovernmental Oceanographic Commission</strong> (IOC) of UNESCO, as part of the <strong>UN Decade of Ocean Science for Sustainable Development</strong>.</p><p>The school ran over three days, with the OPS over two days.  We searched for a platform that would accommodate the flexibility needed for the OPS; we chose Discord.  We had participants originating from Brazil, France, India, Italy, Iran, Spain, Tunisia and the UK; ages ranged from 19 to 60 years.  It was a great success.  A detailed, online feedback form two weeks after the event collected participants’ opinions, including:</p><ul><li><em>“It was a wonderful experience.”, :I felt very good with all the participants.”, “When I describe the experience to friends I always say that it was something really useful for my personal and professional growth.”, “It was a very enriching experience for me to meet all these people with different training and knowledge, coming from different countries.”, “Enriching moments, so much more to discover.”, “What a great experience! I felt happy, engaged and surrounded by beautiful minds.”</em></li> </ul><p>We will run the event again in the Spring and the late summer or autumn, with different geoscience themes.  The success of the October 2020 event raises several research questions, including:</p><ul><li>How do the online and the in-person versions compare?</li> <li>What are the advantages and drawbacks of each?</li> <li>Which is more effective for what objectives and what results?</li> <li>How do the two versions stack up in regard to conducting research on such events?</li> <li>What are the implications of OPS for geoliteracy?</li> </ul><p>Our presentation will describe the event in more detail, offer tentative answers to the above questions, and help you decide if you wish to participate in the next event.  Co-authors include both organizers and participants.</p>


2019 ◽  
Vol 6 (1) ◽  
pp. 1661112 ◽  
Author(s):  
D. Pantusa ◽  
G.R. Tomasicchio ◽  
B.Chitti Babu

2015 ◽  
Vol 130 ◽  
pp. 65-74 ◽  
Author(s):  
Victoria Granger ◽  
Jean-Marc Fromentin ◽  
Nicolas Bez ◽  
Giulio Relini ◽  
Christine N. Meynard ◽  
...  

2016 ◽  
Author(s):  
Antonio Sánchez-Román ◽  
Simón Ruiz ◽  
Ananda Pascual ◽  
Baptiste Mourre ◽  
Stéphanie Guinehut

Abstract. In this work an Observing System Simulation Experiment (OSSE) approach is used to investigate the Argo array spatial sampling necessary in the Mediterranean Sea to recover the mesoscale signal as seen by altimetry. The monitoring of the mesoscale features is not an initial objective of the Argo network. However, it is an interesting question in the perspective of future network extensions in order to improve the ocean state estimates. A quality assessment of the performances of the altimeter product is carried out to quantify the differences between Argo and altimetry needed to conduct the simulation experiments. The method used here to evaluate the altimeter data is based on the comparison of Sea Level Anomalies (SLA) from altimetry and Dynamic Height Anomalies (DHA) referred to both 400 and 900 dbar computed from the in-situ Argo network. A standard deviation of the differences between SLA and DHA of 4.92 cm is obtained when comparing altimetry and Argo data referred to 400 dbar. The simulation experiments show that a configuration similar to the current Argo array in the Mediterranean (with a spatial resolution of 2° × 2°) is only able to recover the large-scale signals of the basin. On the contrary, the SLA field reconstructed from a 0.75° x 0.75° Argo network can retrieve most of the mesoscale signal. Such an Argo array of around 450 floats in the Mediterranean Sea would be enough to recover the SLA field with an RMSE of 3 cm for spatial scales higher than 150 km, similar to those captured by the altimetry.


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