scholarly journals Rheological profiles in the Central- Eastern Mediterranean

1997 ◽  
Vol 40 (4) ◽  
Author(s):  
M. Viti ◽  
D. Albarello ◽  
E. Mantovani
Keyword(s):  
Heat Flow ◽  
Large Scale ◽  
Eastern Mediterranean ◽  
Mediterranean Area ◽  
Geological Time ◽  
Western Turkey ◽  
Geological Time Scale ◽  
Total Strength ◽  
The Mediterranean ◽  
Wet Rocks

Seismological investigations have provided an estimate of the gross structnral features of the crust/upper mantle system in the Mediterranean area. However, this information is only representative of the short-term me- chanical behaviour of rocks and cannot help us to understand slow deformations and related tectonic processes on the geological time scale. In this work strength envelopes for several major structural provinces of the Mediterranean area have been tentatively derived from seismological stratification and heat flow data, on the assumption of constant and uniforrn strain rate (10-16 S-1), wet rocks and conductive geotherm. It is also shown how the uncertainties in the reconstruction of thermal profiles can influence the main rheological prop- erties of the lithosphere, as thickness and total strength. The thickest (50-70 km) and strongest mechanical lithospheres correspond to the coldest zones (with heat flow lower than or equal to 50 mW m-2), i.e., the Io- nian and Levantine mesozoic basins, the Adriatic and Eurasian foreland zones and NW Greece. Heat flows larger than 65 mW m-2, generally observed in extensional zones (Tyrrhenian, Sicily Channel, Northern Aegean, Macedonia and Western Turkey), are mostly related to mechanical lithospheres thinner than 20 km. The characteristics of strength envelopes, and in particular the presence of soft layers in the crust, suggest a reasonable interpretation of some large-scale features which characterize the tectonic evolution of the Central- Eastem Mediterranean.

Tsunamis

2009 ◽  
Author(s):  
Gerassimos Papadopoulos
Keyword(s):  
Large Scale ◽  
Aegean Sea ◽  
Volcanic Eruptions ◽  
Mediterranean Area ◽  
Wave System ◽  
Submarine Landslides ◽  
Plate Convergence ◽  
Long Wave ◽  
The Mediterranean ◽  
Steep Terrain

According to Imamura (1937: 123), the term tunami or tsunami is a combination of the Japanese word tu (meaning a port) and nami (a long wave), hence long wave in a harbour. He goes on to say that the meaning might also be defined as a seismic sea-wave since most tsunamis are produced by a sudden dip-slip motion along faults during major earthquakes. Other submarine or coastal phenomena, however, such as volcanic eruptions, landslides, and gas escapes, are also known to cause tsunamis. According to Van Dorn (1968), ‘tsunami’ is the Japanese name for the gravity wave system formed in the sea following any large-scale, short-duration disturbance of the free surface. Tsunamis fall under the general classification of long waves. The length of the waves is of the order of several tens or hundreds of kilometres and tsunamis usually consist of a series of waves that approach the coast with periods ranging from 5 to 90 minutes (Murty 1977). Some commonly used terms that describe tsunami wave propagation and inundation are illustrated in Figure 17.2. Because of the active lithospheric plate convergence, the Mediterranean area is geodynamically characterized by significant volcanism and high seismicity as discussed in Chapters 15 and 16 respectively. Furthermore, coastal and submarine landslides are quite frequent and this is partly in response to the steep terrain of much of the basin (Papadopoulos et al. 2007a). Tsunamis are among the most remarkable phenomena associated with earthquakes, volcanic eruptions, and landslides in the Mediterranean basin. Until recently, however, it was widely believed that tsunamis either did not occur in the Mediterranean Sea, or they were so rare that they did not pose a threat to coastal communities. Catastrophic tsunamis are more frequent on Pacific Ocean coasts where both local and transoceanic tsunamis have been documented (Soloviev 1970). In contrast, large tsunami recurrence in the Mediterranean is of the order of several decades and the memory of tsunamis is short-lived. Most people are only aware of the extreme Late Bronge Age tsunami that has been linked to the powerful eruption of Thera volcano in the south Aegean Sea (Marinatos 1939; Chapter 15).

scholarly journals Hidden geographies of the ‘Mediterranean migration crisis’

2020 ◽  
pp. 239965442093590
Author(s):  
Vicki Squire
Keyword(s):  
Social Movement ◽  
Large Scale ◽  
Eastern Mediterranean ◽  
Critical Dimension ◽  
Migration Forms ◽  
Historical Dynamics ◽  
The Mediterranean ◽  
Political Act ◽  
Migration Crisis ◽  
Mediterranean Migration

This article explores the hidden geographies of what has been widely referred to as the ‘Mediterranean migration crisis’ of 2015 and 2016. Specifically, it draws on a large-scale analysis of migratory testimonies from across the central and eastern Mediterranean routes, in order to explore the claims or demands posed to European policy-makers by people on the move. Reflecting on the idea that migration forms a subversive political act that disrupts spatialised inequalities and longer histories of power and violence, the article sets out the argument advanced by scholars of the autonomy of migration approach that migration forms a ‘social movement’ involving subjective acts of escape. It makes the case for a move beyond an abstract account of migration as a social movement, to emphasise the importance of an analysis that unpacks the concrete ways in which multiple ‘nonmovements’ expose the hidden geographies of the so-called ‘crisis’. In so doing, it draws attention to two specific ways in which migration forms a political act. First, the article highlights anti-colonial acts that contest the spatialised inequalities of global migration along with longer-standing historical dynamics of exploitation and dispossession that these implicate. Second, it highlights anti-war acts that reject securitised responses to cross-border migration along with longer-standing spatial and historical dynamics of masculinist violence. While imperceptibility remains a critical dimension of many migratory acts, the article concludes that paying attention to the perceptible claims to justice that subversive political acts of migration involve is crucial in understanding the distinct transformations put into motion by people on the move.

Some Pleistocene Faunas of the Mediterranean Coastal Areas

1961 ◽  
Vol 27 ◽  
pp. 144-154 ◽  
Author(s):  
E. S. Higgs
Keyword(s):  
Mediterranean Coast ◽  
Time Span ◽  
Geological Time ◽  
Geological Time Scale ◽  
Carbon 14 ◽  
Cave Deposits ◽  
Cave Sediments ◽  
Short Time Span ◽  
The Mediterranean ◽  
Short Time

The object of this paper is to compare the fauna from sites on the Mediterranean coast having a similar physiography at the present day and which may have responded to climatic change in a similar way during the Pleistocene.Carbon 14 dating has shown a relatively short time span for the Late Pleistocene, and it is no longer possible to think of the correlation of cave deposits on a geological time scale. A thousand years or less is of some importance. It is possible and indeed probable that faunas and cave sediments may have been at the same point of time quite different in caves on the shore of the Mediterranean from, say, inland caves at 1,000 or 2,000 feet above sea level, such as those of the Judean Desert.

scholarly journals Chlorophyll signatures and nutrient cycles in the Mediterranean Sea: a model sensitivity study to nitrogen and phosphorus atmospheric inputs

2007 ◽  
Vol 4 (2) ◽  
pp. 909-959 ◽  
Author(s):  
M. Pacciaroni ◽  
G. Crispi
Keyword(s):  
Large Scale ◽  
Eastern Mediterranean ◽  
Three Dimensional ◽  
Sensitivity Study ◽  
Nitrogen And Phosphorus ◽  
State Response ◽  
Atmospheric Depositions ◽  
The Mediterranean ◽  
Atmospheric Inputs ◽  
External Loads

Abstract. In this work, the relative importance of nitrogen and phosphorus, considered as external loads, on Mediterranean biogeochemical cycles is evaluated. Biomass concentrations are analysed considering the steady state response of the three-dimensional ECHYM model to three nitrogen and phosphorus atmospheric depositions, considered as continuous in time. After reaching stationary evolutions, chlorophyll surficial maps and vertical transects are compared with existing datasets, showing a good agreement at their large scale sampling. The distributions of nutrients within the biochemical compartments are analysed, highlighting, inside the Mediterranean oligotrophic environment, the role played by ultraplankton, the smaller phytoplankton compartment. For all the three different atmospheric loads, western primary production estimation is about twice than that in the eastern basin, while western secondary production is about three times the eastern one. This numerical exercise suggests that the Eastern Mediterranean, cycling at low nutrient sill, is eventually pushed toward an higher nutrient depletion, when loading new nitrogen and phosphorus.

scholarly journals Precipitation climatology over Mediterranean Basin from ten years of TRMM measurements

2008 ◽  
Vol 17 ◽  
pp. 87-91 ◽  
Author(s):  
A. V. Mehta ◽  
S. Yang
Keyword(s):  
Mediterranean Sea ◽  
Rainy Season ◽  
Mediterranean Region ◽  
Large Scale ◽  
Eastern Mediterranean ◽  
Tropical Rainfall Measuring Mission ◽  
Western Mediterranean ◽  
Sea Temperature ◽  
Maximum Rainfall ◽  
The Mediterranean

Abstract. Climatological features of mesoscale rain activities over the Mediterranean region between 5° W–40° E and 28° N–48° N are examined using the Tropical Rainfall Measuring Mission (TRMM) 3B42 and 2A25 rain products. The 3B42 rainrates at 3-hourly, 0.25°×0.25° spatial resolution for the last 10 years (January 1998 to July 2007) are used to form and analyze the 5-day mean and monthly mean climatology of rainfall. Results show considerable regional and seasonal differences of rainfall over the Mediterranean Region. The maximum rainfall (3–5 mm day−1) occurs over the mountain regions of Europe, while the minimum rainfall is observed over North Africa (~0.5 mm day−1). The main rainy season over the Mediterranean Sea extends from October to March, with maximum rainfall occurring during November–December. Over the Mediterranean Sea, an average rainrate of ~1–2 mm day−1 is observed, but during the rainy season there is 20% larger rainfall over the western Mediterranean Sea than that over the eastern Mediterranean Sea. During the rainy season, mesoscale rain systems generally propagate from west to east and from north to south over the Mediterranean region, likely to be associated with Mediterranean cyclonic disturbances resulting from interactions among large-scale circulation, orography, and land-sea temperature contrast.

Seasonal assessments of future precipitation extremes in the Mediterranean area considering nonstationarities in predictor-predictand relationships

2020 ◽  
Vol 80 (1) ◽  
pp. 19-42
Author(s):  
C Merkenschlager ◽  
E Hertig
Keyword(s):  
Iberian Peninsula ◽  
Large Scale ◽  
Heavy Precipitation ◽  
Mediterranean Area ◽  
Precipitation Extremes ◽  
Max Planck ◽  
Northern Spain ◽  
Central Mediterranean ◽  
Censored Quantile Regression ◽  
The Mediterranean

Within the context of analyzing daily heavy precipitation events in the Mediterranean under enhanced greenhouse gas forcing in the 21st century, a new method considering non-stationarities in the relationships of large-scale circulation predictors and regional precipitation extremes was applied. The Mediterranean area was split into up to 22 precipitation regions, and analyses were performed separately for 3 different seasons (autumn, winter and spring) and 3 different quantiles (90th, 95th and 99th). Estimations are based on a three-step censored quantile regression. Future estimations are performed by means of 3 model runs of the Max Planck Institute Earth System Model with Low Resolution (MPI-ESM-LR) for representative concentration pathways (RCPs) 4.5 and 8.5. Overall, the Mediterranean is mainly characterized by decreasing quantile values. Especially in the regions in the southeast, declines are significant, with up to 71.7% (-1.65 mm) in the Levante region (autumn) and over 16 mm (-38.2%) on Crete (winter). Increased precipitation quantiles were only assessed for a more or less extended region in the northern parts of the Central Mediterranean (winter and spring), for the northeastern coast of the Iberian Peninsula (autumn) and for northern Spain (spring). Overall, analyses showed that non-stationarities seriously affect precipitation behavior in most parts of the Mediterranean. Results indicated that 2 different regimes (western and eastern) inducing non-stationarities are predominant in the Mediterranean area. In autumn (winter), the western (eastern) regime is limited to the Iberian Peninsula (Levante), whereas in spring, the area of influence of both regimes is of equal size.

scholarly journals NEW NAMES IN THE ‘CYNOGLOSSUM MONTANUM GROUP’ (BORAGINACEAE) IN THE MEDITERRANEAN AREA

2016 ◽  
Vol 73 (3) ◽  
pp. 265-275
Author(s):  
K. Sutorý
Keyword(s):  
Eastern Mediterranean ◽  
Mediterranean Area ◽  
New Combination ◽  
The Mediterranean

Two new names and one new combination are created in the artificial Cynoglossum montanum group (Boraginaceae – Cynoglosseae): Cynoglossum natolicum (Bornm.) Sutorý and Cynoglossum brandii Sutorý from the Eastern Mediterranean, and Cynoglossum maghrebicum Sutorý from Morocco and Algeria. All taxa are discussed, their lectotypes are designated and their distributions are outlined.

scholarly journals Trends in Mediterranean gridded temperature extremes and large-scale circulation influences

2011 ◽  
Vol 11 (8) ◽  
pp. 2199-2214 ◽  
Author(s):  
D. Efthymiadis ◽  
C. M. Goodess ◽  
P. D. Jones
Keyword(s):  
Large Scale ◽  
Eastern Mediterranean ◽  
Temperature Extremes ◽  
Global Trends ◽  
Atmospheric Circulation Patterns ◽  
Circulation Patterns ◽  
Rate Of Increase ◽  
The Mediterranean ◽  
Large Scale Atmospheric Circulation ◽  
Cold Extremes

Abstract. Two recently-available daily gridded datasets are used to investigate trends in Mediterranean temperature extremes since the mid-20th century. The underlying trends are found to be generally consistent with global trends of temperature and their extremes: cold extremes decrease and warm/hot extremes increase. This consistency is better manifested in the western part of the Mediterranean where changes are most pronounced since the mid-1970s. In the eastern part, a cooling is observed, with a near reversal in the last two decades. This inter-basin discrepancy is clearer in winter, while in summer changes are more uniform and the west-east difference is restricted to the rate of increase of warm/hot extremes, which is higher in central and eastern parts of the Mediterranean over recent decades. Linear regression and correlation analysis reveals some influence of major large-scale atmospheric circulation patterns on the occurrence of these extremes – both in terms of trend and interannual variability. These relationships are not, however, able to account for the most striking features of the observations – in particular the intensification of the increasing trend in warm/hot extremes, which is most evident over the last 15–20 yr in the Central and Eastern Mediterranean.

scholarly journals Hydrographic situation during cruise M84/3 and P414 (spring 2011) in the Mediterranean Sea

2013 ◽  
Vol 10 (6) ◽  
pp. 2399-2432 ◽  
Author(s):  
D. Hainbucher ◽  
A. Rubino ◽  
V. Cardin ◽  
T. Tanhua ◽  
K. Schroeder ◽  
...  
Keyword(s):  
Mediterranean Sea ◽  
Large Scale ◽  
Water Mass ◽  
Eastern Mediterranean ◽  
Physical Parameters ◽  
Strait Of Gibraltar ◽  
Mass Properties ◽  
The Mediterranean ◽  
Geostrophic Velocities ◽  
Lebanese Coast

Abstract. Hydrography and large scale circulation observed in the Mediterranean Sea during the M84/3 and P414 cruises (April and June 2011, respectively) are presented. In contrast to most of the recent expeditions, which were limited to special areas of the basin, these two cruises, especially the M84/3, offered the opportunity of delineating a quasi-synoptic picture of the distribution of the relevant physical parameters through the whole Mediterranean. A section was observed from the Lebanese coast up to the Strait of Gibraltar. The focus of our analysis are the water mass properties, also in the context of the recently observed variability, and a comparison between the velocity fields observed using a vessel-mounted ADCP and those calculated from the observed density fields. Overall, a distribution of temperature, salinity, and geostrophic velocities emerges, which seems far from that observed before the beginning of the so-called "Eastern Mediterranean Transient", a major climatic shift in the hydrography and circulation of the Mediterranean Sea occurred at the end of 1980s. Here, our focus is a discussion of the observed water mass properties analysed through T–S diagrams and through an Optimum Multiparameter (OMP) analysis. Additionally, ADCP velocities are compared to geostrophic calculations.

scholarly journals Filling the gap: new precise Early Cretaceous radioisotopic ages from the Andes

2015 ◽  
Vol 152 (3) ◽  
pp. 557-564 ◽  
Author(s):  
BEATRIZ AGUIRRE-URRETA ◽  
MARINA LESCANO ◽  
MARK D. SCHMITZ ◽  
MAISA TUNIK ◽  
ANDREA CONCHEYRO ◽  
...  
Keyword(s):  
Early Cretaceous ◽  
Time Scale ◽  
Lower Cretaceous ◽  
Geological Time ◽  
Geological Time Scale ◽  
Standard Sequence ◽  
Lower Horizon ◽  
The Andes ◽  
Upper Hauterivian ◽  
The Mediterranean

AbstractTwo tuffs in the Lower Cretaceous Agrio Formation, Neuquén Basin, provided U–Pb zircon radioisotopic ages of 129.09±0.16 Ma and 127.42±0.15 Ma. Both horizons are well constrained biostratigraphically by ammonites and nannofossils and can be correlated with the ‘standard’ sequence of the Mediterranean Province. The lower horizon is very close to the base of the Upper Hauterivian and the upper horizon to the Hauterivian/Barremian boundary, indicating that the former lies atc. 129.5 Ma and the latter atc. 127 Ma. These new radioisotopic ages fill a gap of over 8 million years in the numerical calibration of the current global Early Cretaceous geological time scale.

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