Editorial Introduction

2009 ◽  
Author(s):  
Jamie Woodward
Keyword(s):  
River Basin ◽  
Marine Environment ◽  
Environmental Changes ◽  
Physical Geography ◽  
Ecosystem Dynamics ◽  
Mediterranean Environment ◽  
Tectonic Plates ◽  
Spatial And Temporal Scales ◽  
The Mediterranean

By examining both contemporary processes and long-term records of change, this volume explores the climates, landscapes, ecosystems, and hazards that comprise the Mediterranean world. This is the only region on Earth where three continents meet and their interaction has produced a very distinctive physical geography. This book examines the landscapes and processes at the margins of the three continents and the distinctive marine environment between them. In broad terms, the physical geography of the Mediterranean is a product of long-term interplay between tectonic forces, climate change, river basin and marine processes, and biosphere dynamics, as well as the action of humans during the course of the Holocene. From the outset, it is important to keep in mind that this physical geography is an integration of energy, materials, and processes within a much wider global system. The Mediterranean is a zone of convergence and interaction. It is a meeting place not only for tectonic plates, but also for air masses, energy, and river flows from both temperate and tropical latitudes. The region also interacts directly with the global ocean, receiving cool North Atlantic waters in exchange for the warmer and saltier waters produced in the basins of the Mediterranean Sea. It is also a biodiversity hotspot; the Mediterranean has been a meeting place for plants, animals, and humans from three continents throughout much of its history. The chapters in Part I set out the physical and biological framework for the rest of the book and examine key debates about the evolution of the Mediterranean environment. They explore fundamental interactions between the lithosphere, atmosphere, hydrosphere, and biosphere across a range of spatial and temporal scales. The scene is set for later chapters that focus more closely on particular aspects of the Mediterranean environment such as ecosystem dynamics, river basin systems, karst environments, natural hazards, and land degradation. Chapter 1 examines the role of tectonic processes in the development of the Mediterranean landscape and its marine basins. Also highlighted are the dramatic environmental changes and the geomorphological legacy associated with the Messinian Salinity Crisis of the Late Miocene. Chapter 2 focuses on the marine environment, both ancient and modern.

The High Frequency coastal radar network in the Mediterranean: joint efforts towards a fully operational implementation

2021 ◽  
Author(s):  
Pablo Lorente ◽  
Keyword(s):  
Marine Environment ◽  
High Frequency ◽  
Production Management ◽  
Hot Spot ◽  
Coastal Areas ◽  
Coastal Hazards ◽  
Current Status ◽  
Wide Range ◽  
The Mediterranean

<p>The Mediterranean Sea is considered a relevant geostrategic region and a prominent climate change hot spot. This semi-enclosed basin has been the subject of abundant studies due to its vulnerability to sea-level rise and other coastal hazards. With the steady advent of new technologies, a growing wealth of observational data are nowadays available to efficiently monitor the sea state and properly respond to socio-ecological challenges and stakeholder needs, thereby strengthening the community resilience at multiple scales.</p><p>Nowadays, High-Frequency radar (HFR) is a worldwide consolidated land-based remote sensing technology since it provides, concurrently and in near real time, fine-resolution maps of the surface circulation along with (increasingly) wave and wind information over broad coastal areas. HFR systems present a wide range of practical applications: maritime safety, oil spill emergencies, energy production, management of extreme coastal hazards. Consequently, they have become an essential component of coastal ocean observatories since they offer a unique dynamical framework that complement conventional in-situ observing platforms. Likewise, within the frame of the Copernicus Marine Environment Monitoring Service (CMEMS), HFR are valuable assets that play a key pivotal role in both the effective monitoring of coastal areas and the rigorous skill assessment of operational ocean forecasting systems.</p><p>The present work aims to show a panoramic overview not only of the current status of diverse Mediterranean HFR systems, but also of the coordinated joint efforts between many multi-disciplinary institutions to establish a permanent HFR monitoring network in the Mediterranean, aligned with European and global initiatives. In this context, it is worth highlighting that many of the Mediterranean HFR systems are already integrated into the European HFR Node, which acts as central focal point for data collection, homogenization, quality assurance and dissemination and promotes networking between EU infrastructures and the Global HFR network.</p><p>Furthermore, priority challenges tied to the implementation of a long-term, fully integrated, sustainable operational Mediterranean HFR network are described. This includes aspects related to the setting up of such a system within the broader framework of the European Ocean Observing System (EOOS), and a long-term financial support required to preserve the infrastructure core service already implemented. Apart from the technological challenges, the enhancing of the HFR data discovery and access, the boosting of the data usage as well as the research integration must be achieved by building synergies among academia, management agencies, state government offices, intermediate and end users. This would guarantee a coordinated development of tailored products that meet the societal needs and foster user uptake, serving the marine industry with dedicated smart innovative services, along with the promotion of strategic planning and informed decision-making in the marine environment.</p>

scholarly journals Physical and biogeochemical parameters of the Mediterranean Sea during a cruise with RV <i>Maria S. Merian</i> in March 2018

2020 ◽  
Vol 12 (4) ◽  
pp. 2747-2763
Author(s):  
Dagmar Hainbucher ◽  
Marta Álvarez ◽  
Blanca Astray Uceda ◽  
Giancarlo Bachi ◽  
Vanessa Cardin ◽  
...  
Keyword(s):  
Mediterranean Sea ◽  
Western Mediterranean ◽  
Spatial And Temporal Scales ◽  
Circulation Patterns ◽  
Report Data ◽  
Zonal Section ◽  
The Mediterranean ◽  
Biogeochemical Parameters ◽  
Anthropogenic Contributions

Abstract. The last few decades have seen dramatic changes in the hydrography and biogeochemistry of the Mediterranean Sea. The complex bathymetry and highly variable spatial and temporal scales of atmospheric forcing, convective and ventilation processes contribute to generate complex and unsteady circulation patterns and significant variability in biogeochemical systems. Part of the variability of this system can be influenced by anthropogenic contributions. Consequently, it is necessary to document details and to understand trends in place to better relate the observed processes and to possibly predict the consequences of these changes. In this context we report data from an oceanographic cruise in the Mediterranean Sea on the German research vessel Maria S. Merian (MSM72) in March 2018. The main objective of the cruise was to contribute to the understanding of long-term changes and trends in physical and biogeochemical parameters, such as the anthropogenic carbon uptake and to further assess the hydrographical situation after the major climatological shifts in the eastern and western part of the basin, known as the Eastern and Western Mediterranean Transients. During the cruise, multidisciplinary measurements were conducted on a predominantly zonal section throughout the Mediterranean Sea, contributing to the Med-SHIP and GO-SHIP long-term repeat cruise section that is conducted at regular intervals in the Mediterranean Sea to observe changes and impacts on physical and biogeochemical variables. The data can be accessed at https://doi.org/10.1594/PANGAEA.905902 (Hainbucher et al., 2019), https://doi.org/10.1594/PANGAEA.913512 (Hainbucher, 2020a) https://doi.org/10.1594/PANGAEA.913608, (Hainbucher, 2020b) https://doi.org/10.1594/PANGAEA.913505, (Hainbucher, 2020c) https://doi.org/10.1594/PANGAEA.905887 (Tanhua et al., 2019) and https://doi.org/10.25921/z7en-hn85 (Tanhua et al, 2020).

Editorial Introduction

2009 ◽  
Author(s):  
Jamie Woodward
Keyword(s):  
Climate Change ◽  
Air Quality ◽  
Water Resources ◽  
Land Degradation ◽  
Environmental Changes ◽  
Urban Expansion ◽  
Monitoring Networks ◽  
Resource Exploitation ◽  
Mediterranean Environment ◽  
The Mediterranean

This volume has traced the development of the Mediterranean landscape over very long timescales and has examined modern processes in a wide range of settings. Earlier chapters have explored tectonic processes and the evolution of the topography and biota, the nature and impact of Quaternary climate change, and natural hazards, as well as the increasing role of human activity in shaping geomorphological processes and ecosystems during the course of the postglacial period. A core theme in several chapters is the nature of the relationship between humans and the Mediterranean environment. Over the last one hundred years or so, and especially in the period since the Second World War, this relationship has changed dramatically. Resource exploitation, urban expansion, and rural depopulation have all taken place at unprecedented rates, with major impacts upon the quality of land, water, air, and ecosystems. The final part of this volume examines four key topics of environmental concern; its four chapters explore, respectively, land degradation, water resources, interactions between air quality and the climate system, and biodiversity and conservation. Where possible, it is important to place these issues within an appropriate historical perspective. Many components of the Mediterranean environment have responded in a sensitive way to past environmental changes, but the pressures on land and water resources have never been more intense. Improved monitoring networks and new modelling efforts are needed to predict more effectively the impact of climate and social change on all environmental systems and to help inform policymakers seeking a more sustainable use of the region’s resources. Chapter 20 examines the ecological aspects of land degradation and sets out new ideas on productivity dynamics. It explores some of the interactions between land use change, vegetation dynamics, grazing patterns and wildfires. The uneven geography of water resources and water use are highlighted in Chapter 21. Water resource issues have become an increasingly important factor in the geopolitics of the region against a background of climate change uncertainty, rising demand, and a diminishing resource base. Chapter 22 analyses the interactions between climate, air quality, and the water cycle.

Editorial Introduction

2009 ◽  
Author(s):  
Jamie Woodward
Keyword(s):  
Bronze Age ◽  
Physical Geography ◽  
Urban Environments ◽  
Pyroclastic Flows ◽  
Human Society ◽  
Sediment Yields ◽  
Pliny The Younger ◽  
Base Level ◽  
The Mediterranean

Catastrophic earthquakes, explosive volcanic eruptions, and devastating storms and floods are intimately bound up within the history and mythology of the Mediterranean world. It is a key region for the study of natural hazards because it offers unrivalled access to long records of hazard occurrence and impact through documentary, archaeological and geological archives. Early texts and archaeological data have provided unique insights into the nature and impact of past eruptions, earthquakes, tsunamis, and other hazards. Notable events were carefully documented in Antiquity and the archaeological record provides insights into the impact of catastrophic events on past human societies. The eruption of Vesuvius in AD 79, for example, was famously documented by Pliny the Younger, and the excavations at Pompeii have provided extraordinarily rich insights into the dynamics and impacts of tephra falls and pyroclastic flows. The significance of environmental hazards in the demise of civilizations such as Minoan Crete (tsunami) and the Early Bronze Age in the Near East (drought) has been vigorously debated for decades. While such events have undoubtedly threatened people in the region since prehistoric times, the actual threat to human society has increased dramatically in the historical and modern periods as urban environments and their populations have rapidly expanded. This part of the volume analyses hazards associated with both endogenic and exogenic Earth processes and the interactions between them. It includes volcanic processes, crustal instability, tsunamis, fluvial floods, extreme weather phenomena, and wildfires. Each chapter explores the basic controls and the geography of a particular hazard and related processes, and, over a range of timescales, magnitude and frequency relationships and the nature of the threat to human society. High-magnitude events are a fundamental part of the physical geography of the Mediterranean and play a key role in long-term landscape evolution and ecosystem change. Even though the processes associated with each hazard typically take place over very short timescales, they can set in motion long-term adjustments to geomorphological and ecosystem processes. Tephra falls can change soil properties and vegetation communities, for example, and earthquakes may trigger base-level change and landslips in river basins that enhance fluvial sediment yields for many centuries.

Trade-offs of Participation in the Long-Term Ecological Research Program: Immediate and Long-Term Consequences

2016 ◽  
Author(s):  
Lawrence R. Walker ◽  
Michael R. Willig
Keyword(s):  
Ecosystem Dynamics ◽  
Data Sets ◽  
Ecological Research ◽  
Temporal Scales ◽  
Spatial And Temporal Scales ◽  
Trade Offs ◽  
Long Term Ecological Research ◽  
Collaboration And Communication ◽  
Program Change

For those who may have skipped to this chapter and not read the 3 introductory chapters, the 36 essays, or the 4 evaluative chapters of this book, the answer to the burning question “Does participation in the Long-Term Ecological Research (LTER) program change scientists?” is an unequivocal “Yes!” As Boyer and Brown (Chapter 41) point out, however, those changes are mostly in the realms of knowledge acquisition and behavior adoptions in the practice of science. Participation in the program did not appear to have a substantial effect on the development of attitudes. Could such changes have occurred outside of the LTER program? Schlesinger (Chapter 40) thinks so. He suggests that the LTER program provides “some structure and modest standardization to a set of common measurements” but that it has not substantially broadened or deepened the ecological sciences. Yet the effect of the LTER program on science, while a fascinating and often-addressed question, is not the focus of this book (see Willig and Walker, Chapter 1). Of course, to address how scientists change also involves understanding how they approach and conduct science. In addition, personal change occurs in a broad societal context. For example, the LTER program has coincided with and helped promote a transition in ecology from research done by one or a few investigators on a particular organism or process in a particular habitat to investigations involving multidisciplinary teams working together to test models about how ecosystem dynamics unfold across large spatial and temporal scales. However, going to “big programs” and “big data sets” does not mean losing a sense of place or being divorced from the natural history of particular organisms. Even as spatial and temporal scales increase, ecological research is ideally still “place aware” (Bestelmeyer, Chapter 19). Using the essays of this book as a rich source of information to address fundamental questions about the nature of scientists, we provide some final thoughts on how the LTER program has affected its participants, particularly on how they view time and space, collaboration, and communication. We end with reflections on the future of ecology and society, based on the views expressed in this book and on our own participation in the LTER program.

The Physical Geography of the Mediterranean

2009 ◽  
Keyword(s):  
Volcanic Eruptions ◽  
Environmental Issues ◽  
Physical Geography ◽  
Ecosystem Change ◽  
Wide Range ◽  
Mediterranean World ◽  
Explosive Volcanic Eruptions ◽  
The Mediterranean ◽  
Long Timescales

This volume explores the climates, landscapes, ecosystems and hazards that comprise the Mediterranean world. It traces the development of the Mediterranean landscape over very long timescales and examines modern processes and key environmental issues in a wide range of settings. The Mediterranean is the only region on Earth where three continents meet and this interaction has produced a very distinctive Physical Geography. This book examines the landscapes and processes at the margins of these continents and the distinctive marine environment between them. Catastrophic earthquakes, explosive volcanic eruptions and devastating storms and floods are intimately bound up within the history and mythology of the Mediterranean world. This is a key region for the study of natural hazards because it offers unrivalled access to long records of hazard occurrence and impact through documentary, archaeological and geological archives. The Mediterranean is also a biodiversity hotspot; it has been a meeting place for plants, animals and humans from three continents throughout much of its history. The Quaternary records of these interactions are more varied and better preserved than in any other part of the world. These records have provided important new insights into the tempo of climate, landscape and ecosystem change in the Mediterranean region and beyond. The region is unique because of the very early and widespread impact of humans in landscape and ecosystem change - and the richness of the archaeological and geological archives that chronicle this impact. This book examines this history and these interactions and places current environmental issues in long term context.

Climate change and water resources in the Lower Mekong River Basin: putting adaptation into the context

2010 ◽  
Vol 1 (2) ◽  
pp. 103-117 ◽  
Author(s):  
M. Keskinen ◽  
S. Chinvanno ◽  
M. Kummu ◽  
P. Nuorteva ◽  
A. Snidvongs ◽  
...  
Keyword(s):  
Climate Change ◽  
River Basin ◽  
Climate Change Adaptation ◽  
Environmental Changes ◽  
Hydrological Cycle ◽  
Climate Change Impacts ◽  
Mekong River ◽  
Adaptation To Climate Change ◽  
Mekong River Basin ◽  
Spatial And Temporal Scales

Adaptation to climate change has become one of the focal points of current development discussion. This article summarises the findings from a multidisciplinary research project looking at climate change impacts and adaptation in the Mekong River Basin in Southeast Asia. The research highlights the central role that the hydrological cycle has in mediating climate change impacts on ecosystems and societies. The findings indicate that climate change should not be studied in isolation, as there are several other factors that are affecting the hydrological cycle. In the Mekong, the most important such factor is the on-going hydropower development that is likely to induce changes at least as radical as climate change, but with shorter timescales. The article concludes that climate change adaptation should broaden its view to consider environmental changes likely to occur due to different factors at various spatial and temporal scales. It is also important to recognise that climate change adaptation is a dynamic, development-orientated process that should consider also broader socio-political context. To enable this, we propose that an area-based adaptation approach should be used more actively to complement the dominant sector-based approaches.

scholarly journals Variability and Trends in Physical and Biogeochemical Parameters of the Mediterranean Sea during a Cruise with RV MARIA S. MERIAN in March 2018

2020 ◽  
Author(s):  
Dagmar Hainbucher ◽  
Marta Álvarez ◽  
Blanca Astray Uceda ◽  
Giancarlo Bachi ◽  
Vanessa Cardin ◽  
...  
Keyword(s):  
Mediterranean Sea ◽  
Western Mediterranean ◽  
Spatial And Temporal Scales ◽  
Circulation Patterns ◽  
German Research ◽  
Zonal Section ◽  
The Mediterranean ◽  
Biogeochemical Parameters ◽  
Anthropogenic Contributions

Abstract. The last decades have seen dramatic changes in the hydrography and biogeochemistry of the Mediterranean Sea. The complex bathymetry, highly variable spatial and temporal scales of atmospheric forcing and internal processes contribute to generate complex and unsteady circulation patterns and significant variability in biogeochemical systems. Part of this variability can be influenced by anthropogenic contributions. Consequently, it is necessary to document details and to understand trends in place to better relate the observed processes and to possibly predict the consequences of these changes. In this context we report on data from an oceanographic cruise in the Mediterranean Sea on the German research vessel MARIA S. MERIAN (MSM72) in March 2018. The main objective of the cruise was to contribute to the understanding of long-term changes and trends in physical and biogeochemical parameters, such as the anthropogenic carbon uptake and to further assess the hydrographical situation after the major climatological shifts in the eastern and western part of the basin, known as the Eastern and Western Mediterranean Transients. During the cruise, multidisciplinary measurements were conducted on a predominantly zonal section throughout the Mediterranean Sea, contributing to the global GO-SHIP repeating hydrography program and adhering to the GO-SHIP requirements.

Tectonic Setting and Landscape Development

2009 ◽  
Author(s):  
Anne Mather
Keyword(s):  
Mediterranean Sea ◽  
Eastern Mediterranean ◽  
Tectonic Setting ◽  
Complex Mixture ◽  
Global Scale ◽  
Physical Geography ◽  
Tectonic Plates ◽  
Physically Based ◽  
The Mediterranean ◽  
Tethys Ocean

The Mediterranean is the westernmost part of the global-scale Alpine-Himalayan orogenic belt which stretches from Spain to New Zealand. The landscapes of the region have a long and complex history that includes both horizontal and vertical crustal movements and the creation and destruction of oceans. This began with the break up of the super-continent Pangea around 250 Ma, which generated the Tethys Ocean—the forerunner to the present-day Mediterranean Sea. Collision of the African and European tectonic plates over the last 30 Ma led to the destruction of the Tethys Ocean, although a few remnants of its geology are preserved within the eastern Mediterranean. It is the collision of Africa and Eurasia, and the associated tectonics that have been largely responsible for generating the Mediterranean Sea, its subsequent history, and the landscapes that surround it. This collisional history progressively reduced the connectivity of the Mediterranean Sea with surrounding marine bodies by closing and restricting marine gateways. During the Miocene, for example, the Mediterranean basin became completely isolated from surrounding marine bodies in what is known as the ‘Messinian Salinity Crisis’. This period saw major changes to the regional water balance leading to evaporation and draw-down of the Mediterranean Sea. This had profound impacts on all aspects of the physical geography of the region including the climatology, biogeography, and geomorphology and its legacy can be seen across the region today. The more recent Quaternary geodynamics of the Mediterranean have generated an area which includes a complex mixture of zones of plate subduction of various ages and stages (Figure 1.1b). The modern Mediterranean includes zones of active subduction associated with volcanic activity—such as the Calabrian arc—and older zones of now quiescent subduction such as the Betic-Rif arc. There is a wide range of seismic activity associated with these regions from deep (600 km) to shallow (<50 km) and ranging in magnitude up to 8.0Mw (earthquake moment magnitude; a quantitative and physically based scale for measuring earthquakes).

scholarly journals The Effects of Physical-Geographic Factors on Flood Episodes Extremity in the Vydra River Basin

Geografie ◽  
2011 ◽  
Vol 116 (3) ◽  
pp. 335-353 ◽  
Author(s):  
Jakub Čurda ◽  
Bohumír Janský ◽  
Jan Kocum
Keyword(s):  
River Basin ◽  
Field Survey ◽  
Physical Geography ◽  
Geographic Factors ◽  
Runoff Regime ◽  
Special Respect ◽  
Assessment Research ◽  
Function Assessment ◽  
Runoff Dynamics

The paper summarizes findings about the Vydra River basin (sw. Czechia) runoff regime including its sources with a special respect to observed flood situations formation and course. The main focus is concentrated on explanation of runoff dynamics relation to physical-geographic conditions of chosen subcatchments. In this term, special emphasis is adverted to peat land hydrological function assessment. Research is based on analyses of long-term time series of Czech Hydrometeorological Institute and of data acquired within more than three years field survey which is carried out in the study area by the Charles University in Prague, Faculty of Science, Department of Physical Geography and Geoecology.

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