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INTRODUCTION 1. in Explanation of His Point, Sperry Writes: 'It Is Not Just
Notes INTRODUCTION 1. In explanation of his point, Sperry writes: 'It is not just that the poetry is taken up in isolation from the life of the poet, from the deeper logic of his career both in itself and in relation to the history of his times, although that fact is continuously disconcerting. It is further that in reducing the verse to a structure of ideas, criticism has gone far toward depriving it of all emotional reality'(14). 2. See, in particular, Federico Olivero's essays on Shelley and Ve nice (1909: 217-25), Shelley and Dante, Petrarch and the Italian countryside (1913: 123-76), Epipsychidion (1918: 379-92), Shelley and Turner (1935); Corrado Zacchetti's Shelley e Dante (1922); and Maria De Courten's Percy Bysshe Shelley e l'Italia (1923). A more recent, and important, work is Aurelio Zanco's monograph, Shelley e l'Italia (1945). Other studies of note are by Tirinelli (1893); Fontanarosa (1897); Bernheimer (1920); Bini (1927); and Viviani della Robbia (1936). 3. In researching this field of study, Italian critics have found Shelley to be their best spokesman. 4. A work such as Anna Benneson McMahan's With Shelley in Italy (1907) comes to mind. Hers is a more inclusive anthology than John Lehmann's Shelley in Italy (1947) but needs to be brought up to date. 5. There has been a growing recognition of the importance of the Italian element in Shelley's poetry. Significant studies in English since those of Scudder (1895: 96-114), Toynbee (1909: 214-30), Bradley (1914: 441-56) and Stawell (1914: 104-31) are those of P. -
1 Week Elba Island & Capraia
CRUISE RELAX 1.3 CAPRAIA HARBOR 1 WEEK ELBA ISLAND & CAPRAIA CERBOLI • PORTOFERRAIO • LA BIODOLA • MARCIANA MARINA • CAPRAIA MARINA DI CAMPO • GOLFO STELLA • PORTO AZZURRO • CALA VIOLINA CRUISE RELAX CRUISE RELAX HARBOURS ANCHORS 1 WEEK ELBA ISLAND 1 WEEK ELBA ISLAND • MARINA DI SCARLINO • CERBOLI • PORTOFERRAIO • PORTOFERRAIO & CAPRAIA & CAPRAIA • MARCIANA MARINA • LA BIODOLA • CAPRAIA ISLAND • CAPRAIA ISLAND • MARINA DI CAMPO CHART ITINERARY • GOLFO STELLA • PORTO AZZURRO • CALA VIOLINA CAPRAIA TYRRHENIAN CAPRAIA ISLAND SEA TUSCANY PIOMBINO Cerboli Porto Ferraio Marciana Marina PALMAIOLA CERBOLI 1 - Marina di Scarlino - Cerboli - Portoferraio 5 - Marina di Campo - Golfo Stella - Porto Azzurro CALA VIOLINA Weigh anchor early in the morning and sail to Portoferraio, the Sail to Porto Azzurro, but first stop at Golfo Stella, where you can MARCIANA PORTOFERRAIO most populous town of Elba Island. You should not forget to take a swim in its uncontaminated sea. Only 18 miles far from MARINA PUNTA ALA LA BIODOLA take a break for a swim in Cerboli. Once in Portoferraio, you can Marina di Scarlino, Porto Azzurro is the best locality to spend PORTO MARINA AZZURRO moor in the ancient Greek/Roman mooring, the “Darsena Me- the last night. Its harbour during summer is really crowded. In DI CAMPO FETOVAIA GOLFO dicea”, or in the mooring of the yard “Esaom Cesa”. You can also this case you can have a safe anchorage in front of Porto Azzur- STELLA have a safe anchor. Not to be missed: the marvellous view from ro or in Golfo di Mola. the lighthouse of Forte Stella ELBA ISLAND 2 -Portoferraio - La Biodola - Marciana Marina After breakfast, leave to take a swim in La Biodola, one of the most famous and visited beaches of the Island. -
To Marine Meteorological Services
WORLD METEOROLOGICAL ORGANIZATION Guide to Marine Meteorological Services Third edition PLEASE NOTE THAT THIS PUBLICATION IS GOING TO BE UPDATED BY END OF 2010. WMO-No. 471 Secretariat of the World Meteorological Organization - Geneva - Switzerland 2001 © 2001, World Meteorological Organization ISBN 92-63-13471-5 NOTE The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the World Meteorological Organization concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. TABLE FOR NOTING SUPPLEMENTS RECEIVED Supplement Dated Inserted in the publication No. by date 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 CONTENTS Page FOREWORD................................................................................................................................................. ix INTRODUCTION......................................................................................................................................... xi CHAPTER 1 — MARINE METEOROLOGICAL SERVICES ........................................................... 1-1 1.1 Introduction .................................................................................................................................... 1-1 1.2 Requirements for marine meteorological information....................................................................... 1-1 1.2.1 -
Simulation of Urban Boundary and Canopy Layer Flows in Port Areas Induced by Different Marine Boundary Layer Inflow Conditions
Simulation of urban boundary and canopy layer flows in port areas induced by different marine boundary layer inflow conditions Citation for published version (APA): Ricci, A., Burlando, M., Repetto, M. P., & Blocken, B. (2019). Simulation of urban boundary and canopy layer flows in port areas induced by different marine boundary layer inflow conditions. Science of the Total Environment, 670, 876-892. https://doi.org/10.1016/j.scitotenv.2019.03.230 Document license: TAVERNE DOI: 10.1016/j.scitotenv.2019.03.230 Document status and date: Published: 20/06/2019 Document Version: Publisher’s PDF, also known as Version of Record (includes final page, issue and volume numbers) Please check the document version of this publication: • A submitted manuscript is the version of the article upon submission and before peer-review. There can be important differences between the submitted version and the official published version of record. People interested in the research are advised to contact the author for the final version of the publication, or visit the DOI to the publisher's website. • The final author version and the galley proof are versions of the publication after peer review. • The final published version features the final layout of the paper including the volume, issue and page numbers. Link to publication General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. -
Barry Lawrence Ruderman Antique Maps Inc
Barry Lawrence Ruderman Antique Maps Inc. 7407 La Jolla Boulevard www.raremaps.com (858) 551-8500 La Jolla, CA 92037 [email protected] Carte de L'Amerique Nouvellement dressee suivant les Nouvelles descouvertes . 1661 [and] Carte Nouvelle de L'Europe Asie & Afrique Nouvellement . Stock#: 74198 Map Maker: Tavernier Date: 1661 Place: Paris Color: Hand Colored Condition: VG+ Size: 24 x 12 inches Price: $ 3,400.00 Description: Rare pair of eastern and western hemispheric maps, published by Melchior Tavernier. Tavernier's map provides a fine blend of contemporary cartographic information with unique details in the concentric circles outside of the geographical hemisphere. In the outermost circle, Tavernier names the 32 compass point directions in French. In the center circle, are the names of the 12 Classical Winds described by Timothenes of Rhodes (circa 282 BC) in both Latin and the original Greek spellings (see below). In the innermost circle, the 8 Winds of the Mediterranean (the modern compass points) are named (Tramontane, Greco (Grecale), Levante, Sirocco, Austral (Ostro or Mezzogiorno), Sebaca (Libeccio or Garbino), Ponent (Ponente) and Maestral (Mistral or Maestro). Cartographically, the map is a marvelous blend of information and conjecture. Tavernier treats the massive northwestern landmass to the north of California as conjecture, employing a lighter coastal outline to signify that the lands depicted are not known with certainty. California is shown as a curiously shaped island, not consistent with either the Briggs or Sanson models. A single Great Lake is depicted. In the Arctic regions, a notation describes Thomas Button's search for a Northwest Passage. In South America, there is a small Lake Parime in Guiana, and both the Amazon and Rio de la Plata flow from the large interior Lago de los Xarayes. -
Lionello2005-Medwave
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/227091499 Mediterranean wave climate variability and its links with NAO and Indian Monsoon Article in Climate Dynamics · November 2005 DOI: 10.1007/s00382-005-0025-4 CITATIONS READS 119 399 2 authors: P. Lionello Antonella Sanna Università del Salento Centro Euro-Mediterraneo sui Cambiamenti Climatici 237 PUBLICATIONS 7,233 CITATIONS 24 PUBLICATIONS 1,169 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: RISES-AM View project CIRCE project View project All content following this page was uploaded by P. Lionello on 21 May 2014. The user has requested enhancement of the downloaded file. Climate Dynamics (2005) 25: 611–623 DOI 10.1007/s00382-005-0025-4 P. Lionello Æ A. Sanna Mediterranean wave climate variability and its links with NAO and Indian Monsoon Received: 29 March 2004 / Accepted: 1 April 2005 / Published online: 11 August 2005 Ó Springer-Verlag 2005 Abstract This study examines the variability of the inter-annual and inter-decadal variability and a statisti- monthly average significant wave height (SWH) field in cally significant decreasing trend of mean winter values. the Mediterranean Sea, in the period 1958–2001. The The winter average SWH is anti-correlated with the analysed data are provided by simulations carried out winter NAO (North Atlantic Oscillation) index, which using the WAM model (WAMDI group, 1988) forced by shows a correspondingly increasing trend. During sum- the wind fields of the ERA-40 (ECMWF Re-Analysis). mer, a minor component of the wave field inter-annual Comparison with buoy observations, satellite data, and variability (associated to the second EOF) presents a simulations forced by higher resolution wind fields statistically significant correlation with the Indian shows that, though results underestimate the actual Monsoon reflecting its influence on the meridional SWH, they provide a reliable representation of its real Mediterranean circulation. -
Experiencing the Water Lands
TOSCANA Experiencing the water lands Livorno, Capraia Island and Collesalvetti between history, culture and tradition www.livornoexperience.com Livorno Experience Experiencing the water lands S E A R C H A N D S H A R E #livornoexperience livornoexperience.com IN PARTNERSHIP WITH S E A R C H A N D S H A R E #livornoexperience Information livornoexperience.com TOURIST INFORMATION OFFICES LIVORNO CAPRAIA ISLAND COLLESALVETTI INDICE Via Alessandro Pieroni, 18 Via Assunzione, Porto Sportello Unico per le Attività Ph. +39 0586 894236 (next to la Salata) Produttive e Turismo EXPERIENCING THE WATER LANDS PAG. 5 [email protected] Ph. +39 347 7714601 Piazza della Repubblica, 32 3 TRAVEL REASONS PAG. 8 www.turismo.li [email protected] Ph. +39 0586 980213 www.visitcapraia.it [email protected] LIVORNO PAG.10 www.comune.collesalvetti.li.it CAPRAIA ISLAND PAG. 30 COLLESALVETTI PAG. 42 EVENTS PAG. 50 HOW TO GET THERE BY CAR BY BUS Coming from Milan, you can take the A1 From Livorno Central Station, the main lines motorway, reaching Parma, and then take the leave to reach the city centre, “Lam Blu” which A15 motorway towards La Spezia and then the crosses the city centre and seafront, “Lam A12 towards Livorno, while from Rome you take Rossa” which crosses the city centre and arrives the A12 motorway, the section which connects at the hamlets of Montenero and Antignano. Rome to Civitavecchia, and then continue The urban Line 12 connects the city centre of along the Aurelia, now called E80, up to Livorno. -
The Urban Heat Island Effect in Malta and the Adequacy of Green Roofs in Its Mitigation Jonathan Scicluna James Madison University
James Madison University JMU Scholarly Commons Masters Theses The Graduate School Spring 2016 The urban heat island effect in Malta and the adequacy of green roofs in its mitigation Jonathan Scicluna James Madison University Follow this and additional works at: https://commons.lib.jmu.edu/master201019 Part of the Environmental Health and Protection Commons, Environmental Studies Commons, Other Earth Sciences Commons, and the Sustainability Commons Recommended Citation Scicluna, Jonathan, "The urban heat island effect in Malta and the adequacy of green roofs in its mitigation" (2016). Masters Theses. 467. https://commons.lib.jmu.edu/master201019/467 This Thesis is brought to you for free and open access by the The Graduate School at JMU Scholarly Commons. It has been accepted for inclusion in Masters Theses by an authorized administrator of JMU Scholarly Commons. For more information, please contact [email protected]. THE URBAN HEAT ISLAND EFFECT IN MALTA AND THE ADEQUACY OF GREEN ROOFS IN ITS MITIGATION Jonathan Scicluna A dissertation submitted to the UNIVERSITY OF MALTA and JAMES MADISON UNIVERSITY In Partial Fulfilment of the Requirements for the degree of Master of Science in Sustainable Environmental Resources Management/ Master of Science in Integrated Science and Technology 2016 To my Family ii Acknowledgements I would like to express my gratitude to my supervisors Mr Antoine Gatt and Dr Wayne S. Teel as well as to Prof Louis F. Cassar. I would also like to thank the course coordinators Dr Elisabeth Conrad and Dr Maria Papadakis as well as the administrative staff at the Valletta Campus especially Mr Mario Cassar and Ms Mersia Mackay Zammit. -
Mathematical Models Supporting the Monitoring of Civitavecchia Harbour (Rome)
Computational Methods and Experimental Measurements XVII 443 Mathematical models supporting the monitoring of Civitavecchia harbour (Rome) S. Bonamano1 , F. Paladini de Mendoza1 , V. Piermattei1 , R. Martellucci1 , A. Madonia1 , V. Gnisci1 , E. Mancini1 , G. Fersini3, C. Burgio3 , M. Marcelli1 & G. Zappalà2 1DEB Experimental Oceanology and Marine Ecology Laboratory, Tuscia University, Italy 2Istituto per l’Ambiente Marino Costiero (IAMC), National Research Council, Italy 3Port Authority of Civitavecchia-Fiumicino-Gaeta, Italy Abstract Knowledge of the sources and types of pollutants, of the hydrodynamic field and of the health status of the marine ecosystems subjected to stress is needed to monitor coastal marine environments. The building of new piers and docks and the extension of a breakwater in Civitavecchia harbour have required extensive dredging that was authorised by the Minister of Environment with the prescription to monitor the coastal marine ecosystems with reference to Posidonia oceanica and benthic biocenoses. The structure of benthic communities and the health status of P. oceanica meadows are important indicators of the Ecological Quality Status of coastal marine waters (WFD, 2000/60/CE). In 2012, a multi-platform observing system (C-CEMS) was tested taking into account: a) the distribution of benthic biocenoses; b) physical and biological data acquired by fixed stations and periodic in situ samplings; and c) the results of numerical simulations of sediment particle tracking. This approach was used along the coastline of Northern Latium (Italy) between Tarquinia and Santa Severa. The dispersion of suspended and deposited materials calculated by numerical model is strongly related to the decrement of the shoots density of P. oceanica and to changes of benthic community’s structures. -
More Prominent and Larger, One Or Two Measuring More Than Tion
10 the boundary of the elevation, and then separates gradually half an inch in diameter. In this region the cuticle covering from the surface beneath; the central piece separating to- them was dry and corrugated, and in some few instances wards the centre of the convexity of the papule ; the peri- exfoliation had commenced. pheral piece separating towards the sound skin, and forming On the back of the neck, and between the shoulders, were- a kind of frill around its margin. A crop of papules may about fifty of these papules, for the most part isolated; some- sometimes be seen presenting every gradation of this process few, however, were grouped in pairs, and in two instances, a of desquamation at the same moment. There are some in pair had become blended together. They were all exactly which the crack has just taken place; others, in which the circular, and more prominent than those of the neck, but the edge of the central piece has been worn away, and has become most prominent, even here, measured only three-quarters of a. reduced to a small disk, occupying only the central part of line in elevation. In breadth, the extremes of measurement the convexity; others, in which the central piece is- entirely ranged between one line and six (half an inch), the size of gone; some, in which the peripheral position is distinct; others the greater number was five lines; the next common size in which it is partly, and others again in which it is wholly, measured two lines and a half; while below these, were a gone. -
Oliu Di Corsica: the Challenge of Adapting Geographical Indications to Climate Change
Oliu di Corsica: The challenge of adapting geographical indications to climate change Fabrice Mattei Climate Change & IP Group Head Oliu di Corsica: The challenge of adapting geographical indications to climate change OLIU DI CORSICA: THE CHALLENGE OF ADAPTING GEOGRAPHICAL INDICATIONS TO CLIMATE CHANGE “Beauty island” and “the mountain in the sea” are the most common terms to designate Corsica. They capture the insular topography characterized by the dual alpine and Mediterranean climates. As one the most wooded Mediterranean island, olive trees (Olea europaea L.) are abundant and imbricated with the island’s history, culture and development. The recognition of “Oliu di Corsica” (Corsican olive oil) as an Appellation Of Origin (“AOP”) encodes that exclusive terroir-based causal link where the primary input is climate. Although olive trees grow well under harsh conditions, studies reveal that climate change and its effect on aspects of terroirs such as rainfall, water availability, soil quality, and temperature is already having an effect on some production aspects, quantity and quality, crucial to what brings distinctiveness to Oliu di Corsica (“OdC”) These feedbacks raise question as to how conceptions of terroir underpinning the uniqueness of OdC are evolving in the face of climate change. In this commissioned research, we review the impacts of climate change on the terroir where OdC is produced and explore adaptation strategies to climate change to provide an incentive for producers to adapt their production and post-harvest systems to evolving agronomic conditions at the horizon of 2050. These adaptations raise critical issues including as to how the rules underpinning the distinctiveness of the AOP could evolve in the face of climate changes especially in relation to expanding the plantations under non raid-fed conditions (Marescotti et al. -
Table 2.3: Named Winds Found Throughout the Mediterranean
Chapter 2: The Mediterranean environment Table 2.3: Named winds found throughout the Mediterranean. Summarised from Rudloff (1981), Barry and Chorley (1992), and Kostopoulou (2003). France Mistral o Cold, dry, northerly or northwesterly katabatic flow. o Blows along the southern coast, as far as Genoa, most prevalent between Montpellier and Toulon (Gulf du Lyon) o Accompanied by clear weather and bright sunshine o Associated with depressions in the Gulf of Genoa and a high pressure ridge from the Azores Bize o Cold, dry, northerly, northeasterly or northwesterly winter wind o Blows in the mountainous regions of southern France in Languedoc o Accompanied by heavy clouds Spain Levante o Strong, moist, cool, easterly spring (Feb. – May) and autumn (Oct. – Dec,) wind o Blows on the east and south coasts of Spain o Associated with the Azores anticyclone Leveche o Hot, dry, southwesterly wind o Blows across south-east Spain o Associated with the eastward moving depressions in front of which it occurs Solano o Hot, humid south easterly or easterly summer wind o Occurs on the east coast of Spain and in the strait of Gibraltar Tramontana o Cold, dry, northerly, a form of Bora o Blows along the northern Catalan coast and parts of Italy Galerna o Cold, wet, north-westerly, all year round but especially in winter o Blows onto the north Spanish coast from the Atlantic Cierzo o Cold, dry, north-westerly, active for an extended (6 month) winter period o Blows along the Ebro valley 68 Chapter 2: The Mediterranean environment Table 2.3: Continued Italy Maestro o North-westerly summer wind o Blows in the Adriatic when pressure is low over the Balkan peninsula o Associated with fine weather and light clouds Gregale o Strong, cold north-easterly wind (mainly winter) o Blows in the Ionian Sea, usually lasting two-three days, frequently reaches gale force o Usually accompanied by rainfall.