RIS3 Regional Assessment: South Aegean
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Developing a Regional Climate Change Adaptation Plan for Island Regions
Developing a Regional Climate Change Adaptation Plan for Island Regions. The case of South Aegean Region in Greece. Apostolos P. Siskos1, Dimitrios Voloudakis1, Dimitrios Lalas1, Nikolaos Gakis1, Grigorios Andronikos2, Dionysios Gkoutis1, Maria Strataki1 1Envirometrics Technical Consultants and Engineers Ltd, 20 Karea str. Athens, 11636, Greece 2South Aegean Region's Managing Authority, 22 Saki Karagiorga str., Ermoupolis, Syros, 841 00, Greece Keywords: Climate change, adaptation, region, island, South Aegean Presenting author email: [email protected] ABSTRACT The overall purpose of the Regional Adaptation Plan to Climate Change (RAPCC) of the South Aegean Region (SAR) is to contribute to enhancing the region's resilience to climate change in all sectoral policies as outlined in the National Climate Change Adaptation Strategy. This means increasing preparedness and capacity to address the impacts of climate change at local and regional level, developing a coherent approach and improving coordination. The methodology used to assess the climatic vulnerability of the individual sectors and geographical areas of the SAR and ultimately the climate risk assessment comprised nine solid steps beginning from defining “reference" changes of climatic variables to assess the vulnerability of the different activities and ending with ranking sectors and activities as to the magnitude of the risk. The analysis of the climatic vulnerability and danger and hence risk of the different sectors and activities of the South Aegean Region was carried out for the short and medium term (2021-2050) and long-term horizons (2071-2100) and distinct for the geographical units of Cyclades and Dodecanese. According to these findings the proposed measures in the RAPCC were based on island specific characteristics such as financial-social activities, geomorphology and developed both in horizontal and sectoral actions and classified into High, Medium and Low priority. -
Report on Territorial Diagnosis
CREADIS3: REPORT ON TERRITORIAL DIAGNOSIS. WESTERN GREECE Regional Development Fund on behalf of Region of Western Greece June 2018 2 INDEX 1. General Introduction ........................................................................................................... 3 1.1. The Project .......................................................................................................................3 1.2. The Region of Western Greece and the Project ........................................................4 2. Regional contexts ................................................................................................................ 5 2.1. Territory`s General Profile ..............................................................................................5 2.2. Territory`s CCI Profile ....................................................................................................8 3. CCI Sector Analysis: Evolution and Current Situation ................................................12 3.1. Evolution .........................................................................................................................12 3.2. Current Situation...........................................................................................................14 3.3. Creative Districs ............................................................................................................15 4. CCI Sector characterization .............................................................................................17 4.1. Stakeholders -
Greece | Forest Fires in Peloponnese and Rhodes and EU Response
Emergency Response Coordination Centre (ERCC) – DG ECHO Daily Map | 04/08/2021 Greece | Forest fires in Peloponnese and Rhodes and EU response Fire in Aigialeia Municipality, EU response A Fire danger ▪ On 3 August at 18:30 UTC, Greece made a request of assistance through the Western Greece Region forecast1 Union Civil Protection Mechanism (UCPM). Burnt area (ha): 394.9* 3-9 August ▪ On 4 August at 3:31 UTC, Cyprus offered 1 ground forest fire fighting module Source: JRC-EFFIS (40 pax) and 2 air tractors with 8 pax. The offer was accepted by the Greek Moderate authorities and the deployment is ongoing. ▪ On 4 August at 8:48 UTC, Sweden offered 1 aerial forest fire fighting module High A (2 fireboss via the rescEU). The offer was accepted by the Greek authorities. Very high Source: DG ECHO, as of 4 August Extreme Impact and national response ▪ According to the Civil Protection Operation Center, in Aigialeia Municipality, Aegean 230 firefighters with 116 vehicles were operating in the area, assisted by 5 Sea ground force groups, 8 helicopters and 8 planes. ▪ In Rhodes Municipality, 159 firefighters with 34 vehicles were operating in the area, assisted by 6 ground force group, 6 helicopters and 3 planes. ▪ There are no reported injuries or fatalities, and although damaged buildings have been reported there are no official figures available Source: Greek Civil Protection, as of 3 August at 18:36 UTC Approximately Gulf of Corinth 10 km to Patras B GREECE Sea of Crete MEDITERRANEAN SEA 1The maximum value of the fire danger forecast module of EFFIS, which generates daily maps of forecasted fire danger level using numerical weather predictions. -
Grading - Overview Map 01 0 0 0 0 4 4 4 4 2 2
580000 581000 582000 583000 584000 585000 586000 587000 588000 589000 21°54'40"E 21°55'20"E 21°56'0"E 21°56'40"E 21°57'20"E 21°58'0"E 21°58'40"E 21°59'20"E 22°0'0"E 22°0'40"E 22°1'20"E N " 0 GLIDE number: N/A Activation ID: EMSR525 4 ' 0 2 ° N Int. Charter Act. ID: N/A Product N.: 01ZIRIA, v1 8 " 3 0 4 ' 0 2 ° 8 3 Ziria - GREECE Wildfire - Situation as of 02/08/2021 0 0 Grading - Overview map 01 0 0 0 0 4 4 4 4 2 2 4 4 Sterea Ellada Fokida ! ! ! ! ! ! ! ! Black ! ! Bulgaria ! ! ! ! Sea ! ! Ionian Sea ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! Albania ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! Greec e ! ! ! ! ! ! ! N ! ! ! ! ! Aegean ! ! ! ! " ! ! ! ! ! ! ! 0 ' ! ! Sea 0 ! ! 2 ! ! ! ! ! ° ! ! ! ! Ziria ! 8 ! N ! " 3 ! ! Turkey ! (! ! ! 0 ! ! ' ! ! ! ! ! ! ! 0 ! Athens ! Ionian ! ^ ! 2 ° ! ! Sea ! ! 8 ! ! 3 ! ! ! ! ! ! 0 0 ! ! Sea of ! ! 0 0 ! ! Achaia ! ! ! ! ! ! ! ! ! ! Crete 0 0 ! ! ! ! ! ! ! ! 3 3 ! ! ! ! 4 4 ! ! Mediterranean ! ! 2 2 ! ! Dytiki Ellada ! 4 4 ! Sea ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 3 ! ! ! ! km ! ! ! ! ! ! ! ! ! ! Π αναγοπούλα ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! Cartographic Information ! ! ! ! ! ! ! ! ! ! ! ! ! ! Full color A1, 200 dpi resolution ! ! 1:15500 ! ! ! ! ! ! N ! ! " ! ! ! ! ! ! ! ! ! 0 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 2 ! ! 0 0.325 0.65 1.3 ' ! ! 0 0 ! ! ! ! ! 9 ! ! ! ! ! 0 0 1 ! ! ! ! ! ! ! ° ! ! ! ! ! km ! N ! ! ! ! 0 0 ! ! 8 " ! ! ! ! ! ! ! 2 2 3 ! 0 -
Cyanobacterial Toxins and Peptides in Lake Vegoritis, Greece
toxins Article Cyanobacterial Toxins and Peptides in Lake Vegoritis, Greece Sevasti-Kiriaki Zervou 1 , Kimon Moschandreou 2, Aikaterina Paraskevopoulou 1, Christophoros Christophoridis 1 , Elpida Grigoriadou 3, Triantafyllos Kaloudis 1, Theodoros M. Triantis 1 , Vasiliki Tsiaoussi 2 and Anastasia Hiskia 1,* 1 Laboratory of Photo-Catalytic Processes and Environmental Chemistry, Institute of Nanoscience & Nanotechnology, National Center for Scientific Research “Demokritos”, Patriarchou Grigoriou E & 27 Neapoleos Str, 15310 Agia Paraskevi, Athens, Greece; [email protected] (S.-K.Z.); [email protected] (A.P.); [email protected] (C.C.);[email protected] (T.K.); [email protected] (T.M.T.) 2 The Goulandris Natural History Museum—Greek Biotope/Wetland Centre, 14th km Thessaloniki-Mihaniona, Thermi P.O. Box 60394, 57001 Thessaloniki, Greece; [email protected] (K.M.); [email protected] (V.T.) 3 Water Resources Management Agency of West Macedonia, 50100 Kozani, Decentralized Administration of Epirus—Western Macedonia, Greece; [email protected] * Correspondence: [email protected] Abstract: Cyanotoxins (CTs) produced by cyanobacteria in surface freshwater are a major threat for public health and aquatic ecosystems. Cyanobacteria can also produce a wide variety of other understudied bioactive metabolites such as oligopeptides microginins (MGs), aeruginosins (AERs), aeruginosamides (AEGs) and anabaenopeptins (APs). This study reports on the co-occurrence of CTs and cyanopeptides (CPs) in Lake Vegoritis, Greece and presents their variant-specific profiles obtained during 3-years of monitoring (2018–2020). Fifteen CTs (cylindrospermopsin (CYN), anatoxin (ATX), nodularin (NOD), and 12 microcystins (MCs)) and ten CPs (3 APs, 4 MGs, 2 AERs and aeruginosamide Citation: Zervou, S.-K.; (AEG A)) were targeted using an extended and validated LC-MS/MS protocol for the simultaneous Moschandreou, K.; Paraskevopoulou, determination of multi-class CTs and CPs. -
Greek Alternative Tourism Workshop
Welcome! GREEK NATIONAL TOURISM ORGANIZATION REGION OF CRETE REGION OF EPIRUS TOURISM ORGANISATION OF HALKIDIKI TOURISM ORGANISATION OF LOUTRAKI TOURISM ORGANISATION OF THESSALONIKI THIS IS ATHENS - ATHENS CONVENTION BUREAU MUNICIPALITY OF ARTA MUNICIPALITY OF KARYSTOS MUNICIPALITY OF RETHYMNO MUNICIPALITY OF TINOS AEGEAN AIRLINES AVEDIS TRAVEL & AVIATION AXIA HOSPITALITY DIVANI COLLECTION HOTELS HYATT REGENCY THESSALONIKI LESVOS GEOPARK MARBELLA COLLECTION PSILORITIS NATURAL PARK-UNESCO GLOBAL GEOPARK YES HOTELS ZEUS INTERNATIONAL Greek Alternative Tourism Workshop GREEK BREAKFAST ALPHA PI ANGEL FOODS DELICARGO DRESSINGS EVER CRETE KOUKAKIS FARM MANA GI TRIPODAKIS WINERY & VINEGAR PRODUCTION Greek Gastronomy Workshop Greek Alternative Tourism Workshop Greek Participants ALL YOU WANT IS GREECE. It has been quite a year. A year you’d probably prefer to leave behind and move on. You put your wants on hold and stayed patiently inside, waiting for better days to come. Now that these days are just around the corner, you can start listening again to your wants and do whatever it takes to satisfy them. Always while keeping yourself and those around you safe. If you keep really quiet for a moment, you will hear your inner voice asking you one simple question. “What do you want?” Do you want to experience a little about everything or a lot about one thing? All you want is one place. A place tailor-made for you. #AllYouWantIsGreece REGION OF CRETE Crete is a jewel in the Med- iterranean Sea, the cradle of European civilization. The hospitable Cretan peo- ple are famous for their cul- ture, innovative spirit and nu- tritional habits. The Cretan diet is highly esteemed as one of the healthiest diets in the world, whereas Crete boasts a vast array of quality products such as olive oil, wine, honey, cheese, rusk, herbs. -
Ganas, A., Serpelloni, E., Drakatos, G., Kolligri, M., Adamis, I., Tsimi, Ch
This article was downloaded by: [HEAL-Link Consortium] On: 20 October 2009 Access details: Access Details: [subscription number 772810551] Publisher Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Earthquake Engineering Publication details, including instructions for authors and subscription information: http://www.informaworld.com/smpp/title~content=t741771161 The Mw 6.4 SW-Achaia (Western Greece) Earthquake of 8 June 2008: Seismological, Field, GPS Observations, and Stress Modeling A. Ganas a; E. Serpelloni b; G. Drakatos a; M. Kolligri a; I. Adamis a; Ch. Tsimi a; E. Batsi a a Institute of Geodynamics, National Observatory of Athens, Athens, Greece b Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Bologna, Italy Online Publication Date: 01 December 2009 To cite this Article Ganas, A., Serpelloni, E., Drakatos, G., Kolligri, M., Adamis, I., Tsimi, Ch. and Batsi, E.(2009)'The Mw 6.4 SW- Achaia (Western Greece) Earthquake of 8 June 2008: Seismological, Field, GPS Observations, and Stress Modeling',Journal of Earthquake Engineering,13:8,1101 — 1124 To link to this Article: DOI: 10.1080/13632460902933899 URL: http://dx.doi.org/10.1080/13632460902933899 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.informaworld.com/terms-and-conditions-of-access.pdf This article may be used for research, teaching and private study purposes. Any substantial or systematic reproduction, re-distribution, re-selling, loan or sub-licensing, systematic supply or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date. -
Contemporary Kinematics of the South Aegean Area (Greece) Detected with Continuous GNSS Measurements
EGU2020-7656, updated on 03 Oct 2021 https://doi.org/10.5194/egusphere-egu2020-7656 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Contemporary Kinematics of the South Aegean Area (Greece) Detected with Continuous GNSS Measurements Vassilis Sakkas, Chrysa Doxa, Andreas Tzanis, and Haralambos Kranis National & Kapodistrian University of Athens, Department of Geology and the Geoenvironment, Athens, Greece ([email protected]) We examine the kinematic characteristics of the crustal deformation in the broader southern Aegean region using 47 permanent GNNS stations distributed across the eastern Peloponnesus, Attica, Cyclades, Dodecanese, Crete and the coast of western Anatolia. Our analysis is based on the study of velocity vectors relative to local reference points at the western and eastern halves of the study area, as well as on the strain field calculated from absolute velocity vectors across the study area. We demonstrate that the South Aegean region undergoes complex distributed block deformation. At the eastern end of the study area this varies from N210°-N220° extension and with crustal thinning across NE Peloponnesus – Attica, to N210°-N220° compression between the central- eastern Peloponnesus and western Crete, both consistent with the geodynamic setting of the Hellenic Subduction System. A principal feature of the S. Aegean crust appears to be a broad shear zone extending between the islands of Samos/Ikaria and Kalymnos, Paros/Naxos and Amorgos and Milos – Santorini; It exhibits left-lateral kinematics and its southern boundary appears to coincide with the Amorgos – Santorini ridge and comprise the Anhydros basin and associated volcanic field (including Columbo and Santorini). -
Atlas of the Islands
The ESPON 2013 Programme The Development of the Islands – European Islands and Cohesion Policy (EUROISLANDS) Targeted Analysis 2013/2/2 Atlas of the Islands EUROPEAN UNION Part-financed by the European Regional Development Fund INVESTING IN YOUR FUTURE ESPON EUROISLANDS Project - Atlas of the Islands List of authors Lead Partner - University of Aegean, Mytilini, Greece Ioannis SPILANIS Department of Environment, Laboratory of Local and Insular Development Contents Thanasis KIZOS, Department of Geography Foreword ______________________________________________________ 3 Michalis VAITIS, Department of Geography, Laboratory of Geo-informatics Introduction ___________________________________________________ 4 Nikoletta KOUKOUROUVLI, Laboratory of Geo-informatics 1. A Typology of European Islands __________________________________ 5 2. A note on methodology: indexes for the state of islands, changes and their attractiveness __________________________________________________ 6 3. The Atlas ____________________________________________________ 8 3.1. The State of European Islands _________________________________________ 9 3.1.1. Efficiency of Islands’ economy __________________________________________________________ 9 3.1.2. Social equity_______________________________________________________________________ 12 3.1.3. Environmental conservation ___________________________________________________________ 18 3.1.4. Synthesis on the State of Islands ______________________________________________________ 20 3.2. Analysis of Attractiveness parameters -
Greece): Results from Geomorphological Studies and Fission-Track Analysis
© Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at fission-track dating geomorphology palaeokarst neotectonics . Hellenides Cretaceous Palaeokarst and Cenozoic Erosion of the North Sporades (Greece): Results from Geomorphological Studies and Fission-Track Analysis EWALD HEJL1, HELMUT RIEDL2 AND HERBERT WEINGARTNER2 9 Figures and 2 Tables Content Zusammenfassung 67 Abstract .' 67 1. Introduction 68 2. Geological setting 68 3. Palaeokarst features 69 3.1 Bauxite karst and laterite karst 69 3.2 Preflysch karst 72 4. Neogene-Quaternary planation surfaces of Skopelos Island 72 4.1 Planation system A 72 4.2 Planation system B 72 4.3 Planation system C 72 4.4 Pediment system D 74 4.5 Coastal marginal pediment system E 74 5. Apatite fission-track analysis 74 6. Discussion of thermochronological data 75 7. Conclusions 81 8. Acknowledgements 81 References 81 Der kreidezeitliche Paläokarst und die känozoische Reliefgeschichte der Nordsporaden (Griechenland): Geomorphologische Befunde und Spaltspurenanalysen Zusammenfassung Die Reliefentwicklung der Magnesischen Inseln (Nordsporaden) wurde anhand geomorphologischer Geländebeobachtungen auf Skopelos und mittels Spaltspurdatierungen an Gesteinen von Skiathos, Skopelos und Alonnisos untersucht. Die gemessenen Spaltspuralter und modellierten Abkühlpfade weisen auf regionale und zeitliche Schwankungen der posteozänen Abtragungsgeschwindigkeiten hin. Zwei präeozäne Generationen von Paläokarst sind auf Skopelos zu beobachten. Die erste entwickelte sich während der Unterkreide auf triadischen Dolomiten des alten pelagonischen Schelfs. Die Bauxite und Laterite, mit denen dieser Palaeokarst versiegelt ist, sind aus verschwemmtem Material der Eohellenischen Decke hervorgegangen. Eine zweite Generation von Paläokarst entwickelte sich auf oberkretazi- schen Rudistenkalken und wurde unter palaeogenem Flysch begraben. Drei Generationen neogener Verflachungen treten auf Skopelos oberhalb von 300 m Seehöhe auf. -
The Geodynamics of the Aegean and Anatolia: Introduction
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The geodynamics of the Aegean and Anatolia: introduction T. TAYMAZ1, Y. YILMAZ2 & Y. DILEK3 1Department of Geophysical Engineering,˙ Istanbul Technical University, Maslak, TR–34469,˙ Istanbul, Turkey (e-mail: [email protected]) 2Kadir Has University, Fatih, I˙stanbul, Turkey 3Department of Geology, Miami University, Oxford, OH 45056, USA The complexity of the plate interactions and and volcanism in Anatolia and the Aegean region associated crustal deformation in the Eastern (Taymaz et al. 2004). Mediterranean region is reflected in many destruc- tive earthquakes that have occurred throughout Regional synthesis its recorded history, many of which are well documented and intensively studied. The Eastern Given its location in the Alpine–Himalayan Mediterranean region, including the surrounding orogenic belt, and at the collisional boundary areas of western Turkey and Greece, is indeed one between Gondwana and Laurasia, the geological of the most seismically active and rapidly deform- history of the Aegean region and Anatolia involves ing regions within the continents (Fig. 1). Thus, the Mesozoic–Cenozoic closure of several Neo- the region provides a unique opportunity to tethyan oceanic basins, continental collisions and improve our understanding of the complexities of subsequent post-orogenic processes (e.g. Sengo¨r continental tectonics in an actively collisional & Yılmaz 1981; Bozkurt & Mittwede 2001; Okay orogen. The major scientific observations from et al. 2001; Dilek & Pavlides 2006; Robertson & this natural laboratory have clearly been helping Mountrakis 2006). The opening of oceanic branches us to better understand the tectonic processes in of Neotethys commenced in the Triassic and active collision zones, the mode and nature of they closed during the Late Cretaceous to Eocene continental growth, and the causes and distribution time interval. -
Network Biogeography of a Complex Island System: the Aegean
Journal of Biogeography (J. Biogeogr.) (2016) ORIGINAL Network biogeography of a complex ARTICLE island system: the Aegean Archipelago revisited Konstantinos Kougioumoutzis1,2*, Anna Thalassini Valli1, Elisavet Georgopoulou3, Stylianos Michail Simaiakis4, Kostas A. Triantis2 and Panayiotis Trigas1 1Laboratory of Systematic Botany, Faculty of ABSTRACT Crop Science, Agricultural University of Aim The Aegean Archipelago has been the focal research area for identifying Athens, GR-118 55 Athens, Greece, 2 and testing several ecological and evolutionary patterns, yet its biogeographical Department of Ecology & Systematics, Faculty of Biology, National & Kapodistrian subdivision has been somewhat overlooked, with the processes driving the University of Athens, GR-157 03 Athens, assembly of the Aegean island plant communities still remaining largely Greece, 3Geological-Paleontological unclear. To bridge this gap, we identify the biogeographical modules (highly Department, Natural History Museum, 1010 linked subgroups of islands and plant taxa) within the Aegean Archipelago. 4 Vienna, Austria, Natural History Museum of Location The Aegean Archipelago, Greece. Crete, University of Crete, Heraklion GR- 71409 Crete, Greece Methods We used a network approach to detect island biogeographical roles and modules, based on a large and detailed database including 1498 Aegean endemic and subendemic plant taxa distributed on 59 Aegean Islands and five adjacent mainland areas. Results The Aegean was divided into six biogeographical modules; the net- work was significantly modular. None of the modules displayed all four possi- ble biogeographical roles (connectors, module hubs, network hubs, peripherals). Six new biogeographical regions in the Aegean were identified. Main conclusions The borders of the six biogeographical regions in the Aegean correspond well to the region’s palaeogeographical evolution from the middle Miocene to the end of the Pleistocene.