Tha Alpine List of Sites of Community Importance
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Project of Strategic Interest NEXTDATA
Project of Strategic Interest NEXTDATA WP 1.2 - GAW-WMO climate observatories Deliverable D1.2.5 Report on the upgrade of GAW-WMO stations with Italian management and related to the SHARE project. WP Coordinator: Angela Marinoni CNR-ISAC Partners: CNR-ISAC, URT Ev-K2-CNR 1 Report on upgrade carried out at GAW Global Stations “O. Vittori” at Monte Cimone and Nepal Climate Observatory Pyramid in the Himalayas 1. “O. Vittori” at Monte Cimone (2165 m, Northern Appenines) The upgrades carried out at Monte Cimone station concern aerosol, gases and radiation measurements. In particular the following measurement programs have been upgraded: - Aerosol size distribution from 10 nm to 800 nm has been completely renewed according to GAW/ACTRIS recommendations. - Aerosol scattering coefficient measured since 2007 at 525 nm has been upgraded with measurement in two additional wave lengths: 450 and 700 nm. Moreover, the following measurement programs have been newly started: - The aerosol size distribution from 500 nm to 20 µm based on time of flight was set up in July 2013. - Radiation measurement program (feasibility study). - Continuous nitrogen oxides (NOx), nitric oxide (NO) and nitrogen dioxide (NO2) measurements suitable for remote high-mountain stations (on test at Bologna laboratories). - Continuous of (SO2) sulfur dioxide measurements is on test in Bologna laboratories, ready for installation at CMN station. - Observations of aerosol vertical profiles have been carried out at Mt. Cimone. After a test installation in October 2012, several improvements were carried out in order to guarantee continuous observations also during winter season. I. Aerosol size distribution from 10 nm to 800 nm The number size distribution of atmospheric aerosol particles is a basic, but essential parameter required in calculations of the effects of aerosols on climate, human health, and eco-systems. -
Climate Signals in a Multispecies Tree-Ring Network from Central And
Clim. Past Discuss., doi:10.5194/cp-2017-48, 2017 Manuscript under review for journal Clim. Past Discussion started: 17 March 2017 c Author(s) 2017. CC-BY 3.0 License. 1 Climate signals in a multispecies tree-ring network from central and 2 southern Italy and reconstruction of the late summer temperatures 3 since the early 1700s 4 5 Giovanni Leonelli1, Anna Coppola2, Maria Cristina Salvatore2, Carlo Baroni2,3, Giovanna Battipaglia4,5, 6 Tiziana Gentilesca6, Francesco Ripullone6, Marco Borghetti6, Emanuele Conte7, Roberto Tognetti7, Marco 7 Marchetti7, Fabio Lombardi8, Michele Brunetti9, Maurizio Maugeri9,10, Manuela Pelfini11, Paolo 8 Cherubini12, Antonello Provenzale3, Valter Maggi1,3 9 10 1 Università degli Studi di Milano–Bicocca — Dept. of Earth and Environmental Science 11 2 Università degli Studi di Pisa — Dept. of Earth Science 12 3 Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche, Pisa 13 4 Università della Campania — Dept. DiSTABiF 14 5 University of Montpellier 2 (France) — PALECO EPHE 15 6 Università degli Studi della Basilicata — School of Agricultural, Forestry, Food and Environmental Sciences, Potenza 16 7 Università degli Studi del Molise — Dept. of Bioscience and Territory 17 8 Università Mediterranea di Reggio Calabria — Dept. of Agronomy 18 9 Istituto di Scienze dell’Atmosfera e del Clima, Consiglio Nazionale delle Ricerche, Bologna 19 10 Università degli Studi di Milano — Dept. of Physics 20 11 Università degli Studi di Milano — Dept. of Earth Science 21 12 Swiss Federal Institute for Forest, Snow and Landscape Research WSL (Switzerland) 22 Correspondence to: Giovanni Leonelli ([email protected]) 23 Abstract. A first assessment of the main climatic drivers that modulate the tree-ring width (RW) and maximum latewood 24 density (MXD) along the Italian Peninsula and northeastern Sicily was performed using 27 forest sites, which include conifers 25 (RW and MXD) and broadleaves (only RW). -
Moüjmtaiim Operations
L f\f¿ áfó b^i,. ‘<& t¿ ytn) ¿L0d àw 1 /1 ^ / / /This publication contains copyright material. *FM 90-6 FieW Manual HEADQUARTERS No We DEPARTMENT OF THE ARMY Washington, DC, 30 June 1980 MOÜJMTAIIM OPERATIONS PREFACE he purpose of this rUanual is to describe how US Army forces fight in mountain regions. Conditions will be encountered in mountains that have a significant effect on. military operations. Mountain operations require, among other things^ special equipment, special training and acclimatization, and a high decree of self-discipline if operations are to succeed. Mountains of military significance are generally characterized by rugged compartmented terrain witn\steep slopes and few natural or manmade lines of communication. Weather in these mountains is seasonal and reaches across the entireSspectrum from extreme cold, with ice and snow in most regions during me winter, to extreme heat in some regions during the summer. AlthoughNthese extremes of weather are important planning considerations, the variability of weather over a short period of time—and from locality to locahty within the confines of a small area—also significantly influences tactical operations. Historically, the focal point of mountain operations has been the battle to control the heights. Changes in weaponry and equipment have not altered this fact. In all but the most extreme conditions of terrain and weather, infantry, with its light equipment and mobility, remains the basic maneuver force in the mountains. With proper equipment and training, it is ideally suited for fighting the close-in battfe commonly associated with mountain warfare. Mechanized infantry can\also enter the mountain battle, but it must be prepared to dismount and conduct operations on foot. -
Chapter 4 Member States of the European Union and The
CHAPTER 4 membeR StAteS oF tHe EuroPean UnioN and tHe EuroPean EcoNomic AReA 4.1 Austria ............................................. 18 4.15 Latvia .............................................. 50 4.2 belgium ........................................... 20 4.16 lithuania ......................................... 52 4.3 Cyprus ............................................. 24 4.17 luxembourg ................................... 55 4.4 Czech Republic ............................... 26 4.18 Malta ............................................... 59 4.5 denmark ......................................... 29 4.19 Netherlands ..................................... 61 4.6 estonia ............................................. 31 4.20 Norway ............................................ 64 4.7 Finland ............................................ 33 4.21 Poland .............................................. 66 4.8 France.............................................. 35 4.22 Portugal ........................................... 69 4.9 Germany ......................................... 37 4.23 Slovakia ........................................... 71 4.10 Greece .............................................. 39 4.24 Slovenia ........................................... 74 4.11 Hungary .......................................... 41 4.25 Spain ................................................ 76 4.12 Iceland ............................................. 43 4.26 Sweden ............................................. 81 4.13 Ireland ............................................ -
Rifugio Campo Imperatore + Center for Ecotourism and Cultural Creativity
CAMPO IMPERATORE Center for Ecotourism + Cultural Creativity ANALYSIS, RESEARCH AND DESIGN FOR THE REQUALIFICATION OF NEGLECTED SPACES Prepared by Elsa G. De Leon ENVIRONMENT LOCATION Parco Nazionale del Gran Sasso e Monti della Laga Provincia di Terramo Urbino Provincia Marche di Pescara Abruzzo Campo L’Aquila Provincia Imperatore Lazio di Chieti Roma Campo Imperatore Parco Nazionale della Parco Nazionale Provincia Majella dell’Aquila d’Abruzzo ABRUZZO - ITALY. Italian Region. PROVINCIA DELL’AQUILA. Abruzzo Province. GRAN SASSO. National Park. CAMPO IMPERATORE. Alpine meadow. ASCOLIPICENO CULTURAL + VALUES SAN GIACOMO L’ecomuseo di Valle Castellana Ripe Valle Castellana Lago di CEPPO Campotosto L’ecomuseo di Lago di Valle Castellana Campotosto TERAMO AMATRICE CAMPOTOSTO PIETRACAMELA ISOLA DEL GRAN SASSO Arsita Prati di Tivo S. Pietro CAMPO IMPERATORE Museo del Camoscio Orto Botanico Appenninico di San Colombo FONTE VETICA FONTE CERRETO Farindola Arischia Assergi LAGO RACOLLO S. Stefano di Sessanio L’AQUILA Barisciano Calascio PARCO NAZIONALE L’Aquila Centro GRAN SASSO E MONTI DELLA LAGA Visite Fiume Tirino Bussi sul Tirino Historic Center km 0 1 2 3 4 5 km ENVIRONMENTAL + CULTURAL VALUES 150.000 3 5 44 HECTARES REGIONS PROVINCES MUNICIPALITIES BIODIVERSITY AGRO-BIODIVERSITY 51 In danger flora Cereals Solina, Farro Rosso 59 Spontaneous Orchids Legumes Lentils of Santo Stefano di Sessanio 2 Carnivorous plants Vegetables Red Potato Aromatic Plants Tansy, Customary 2364 Register Plants Fruit Trees Apples, figs, Mediterranean hack berry, almonds -
Bare Bedrock Erosion Rates in the Central Appalachians, Virginia
W&M ScholarWorks Undergraduate Honors Theses Theses, Dissertations, & Master Projects 5-2009 Bare Bedrock Erosion Rates in the Central Appalachians, Virginia Jennifer Whitten College of William and Mary Follow this and additional works at: https://scholarworks.wm.edu/honorstheses Part of the Geology Commons Recommended Citation Whitten, Jennifer, "Bare Bedrock Erosion Rates in the Central Appalachians, Virginia" (2009). Undergraduate Honors Theses. Paper 326. https://scholarworks.wm.edu/honorstheses/326 This Honors Thesis is brought to you for free and open access by the Theses, Dissertations, & Master Projects at W&M ScholarWorks. It has been accepted for inclusion in Undergraduate Honors Theses by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. BARE BEDROCK EROSION RATES IN THE CENTRAL APPALACHIANS, VIRGINIA A thesis submitted in partial fulfillment of the requirement for the degree of Bachelors of Science in Geology from The College of William and Mary by Jennifer Whitten Accepted for ___________________________________ (Honors, High Honors, Highest Honors) ________________________________________ Gregory Hancock, Director ________________________________________ Christopher Bailey ________________________________________ James Kaste ________________________________________ Scott Southworth Williamsburg, VA April 30, 2009 Table of Contents Abstract......................................................................................................................................................3 -
Picturing France
Picturing France Classroom Guide VISUAL ARTS PHOTOGRAPHY ORIENTATION ART APPRECIATION STUDIO Traveling around France SOCIAL STUDIES Seeing Time and Pl ace Introduction to Color CULTURE / HISTORY PARIS GEOGRAPHY PaintingStyles GOVERNMENT / CIVICS Paris by Night Private Inve stigation LITERATURELANGUAGE / CRITICISM ARTS Casual and Formal Composition Modernizing Paris SPEAKING / WRITING Department Stores FRENCH LANGUAGE Haute Couture FONTAINEBLEAU Focus and Mo vement Painters, Politics, an d Parks MUSIC / DANCENATURAL / DRAMA SCIENCE I y Fontainebleau MATH Into the Forest ATreebyAnyOther Nam e Photograph or Painting, M. Pa scal? ÎLE-DE-FRANCE A Fore st Outing Think L ike a Salon Juror Form Your Own Ava nt-Garde The Flo ating Studio AUVERGNE/ On the River FRANCHE-COMTÉ Stream of Con sciousness Cheese! Mountains of Fra nce Volcanoes in France? NORMANDY “I Cannot Pain tan Angel” Writing en Plein Air Culture Clash Do-It-Yourself Pointillist Painting BRITTANY Comparing Two Studie s Wish You W ere Here Synthétisme Creating a Moo d Celtic Culture PROVENCE Dressing the Part Regional Still Life Color and Emo tion Expressive Marks Color Collectio n Japanese Prin ts Legend o f the Château Noir The Mistral REVIEW Winds Worldwide Poster Puzzle Travelby Clue Picturing France Classroom Guide NATIONAL GALLERY OF ART, WASHINGTON page ii This Classroom Guide is a component of the Picturing France teaching packet. © 2008 Board of Trustees of the National Gallery of Art, Washington Prepared by the Division of Education, with contributions by Robyn Asleson, Elsa Bénard, Carla Brenner, Sarah Diallo, Rachel Goldberg, Leo Kasun, Amy Lewis, Donna Mann, Marjorie McMahon, Lisa Meyerowitz, Barbara Moore, Rachel Richards, Jennifer Riddell, and Paige Simpson. -
Sedimentological Constraints on the Initial Uplift of the West Bogda Mountains in Mid-Permian
www.nature.com/scientificreports OPEN Sedimentological constraints on the initial uplift of the West Bogda Mountains in Mid-Permian Received: 14 August 2017 Jian Wang1,2, Ying-chang Cao1,2, Xin-tong Wang1, Ke-yu Liu1,3, Zhu-kun Wang1 & Qi-song Xu1 Accepted: 9 January 2018 The Late Paleozoic is considered to be an important stage in the evolution of the Central Asian Orogenic Published: xx xx xxxx Belt (CAOB). The Bogda Mountains, a northeastern branch of the Tianshan Mountains, record the complete Paleozoic history of the Tianshan orogenic belt. The tectonic and sedimentary evolution of the west Bogda area and the timing of initial uplift of the West Bogda Mountains were investigated based on detailed sedimentological study of outcrops, including lithology, sedimentary structures, rock and isotopic compositions and paleocurrent directions. At the end of the Early Permian, the West Bogda Trough was closed and an island arc was formed. The sedimentary and subsidence center of the Middle Permian inherited that of the Early Permian. The west Bogda area became an inherited catchment area, and developed a widespread shallow, deep and then shallow lacustrine succession during the Mid- Permian. At the end of the Mid-Permian, strong intracontinental collision caused the initial uplift of the West Bogda Mountains. Sedimentological evidence further confrmed that the West Bogda Mountains was a rift basin in the Carboniferous-Early Permian, and subsequently entered the Late Paleozoic large- scale intracontinental orogeny in the region. The Central Asia Orogenic Belt (CAOB) is the largest accretionary orogen on Earth, which was formed by the amalgamation of multiple micro-continents, island arcs and accretionary wedges1–5. -
Modelling the Snow Cover of Dome C (Antarctica) with SNOWPACK
Modelling the snow cover of Dome C (Antarctica) with SNOWPACK January 2008 ARPAV Dipartimento Regionale per la Sicurezza del Territorio Servizio Centro Valanghe di Arabba Responsabile: Dr Francesco Sommavilla Realizzazione Franziska Stössel, Christine Groot Zwaaftink, Charles Fierz and Michael Lehning WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland Collaborazioni Dr Anselmo Cagnati Dr Andrea Crepaz P.M. Mauro Valt CONTENTS 1 INTRODUCTION........................................................................................................................... 5 2 POLAR SNOW COVER: REVIEW DIGEST................................................................................ 5 2.1 Models used for the modelling of polar snow.................................................................5 2.2 Antarctica..............................................................................................................................5 2.2.1 Modelling temperature variations in polar snow using DAISY. (Morris and others, 1997) ............................................................................................................................... 5 2.2.2 Modelling mass and energy exchange over polar snow using the daisy model. (Morris and others, 1994)............................................................................................................ 6 2.2.3 Numerical modeling of snow cover over polar ice sheets. (Dang and others, 1997).... 6 2.2.4 Impact of snow drift on the Antarctic ice sheet surface mass balance: -
SNOWCRAFT and AVALANCHES. Gerald Seligman
• . SNOWCRAFT AND AVALANCHES energy and we regained our sleeping qu.arters. after twelve hours. By British standards the climb might be classed just ' very difficult., Apart from these two climbs I was only able to take part in two other 'big expeditions : a second traverse of the Corno Piccolo S. ridge led by one of the L.R.D.G. and the ascent of Torrione Cambi by the -Camino Iannetta and central peak of the Corno Grande, led by J ames Joyce. This was our last expedition and to me at all events it was severe. The route followed the s. face of the Corno Grande to the Forchetta del Ca:lderone. Here the serious work started and the ·next 300 ft. took fo~r hours. The lower part of the chimney ·was ·steep ice up which steps had to be cut. Hal~way up the gradient ·eased off to be followed by a perpendicular, if not overhanging section. 'This latter part was severe. From the summit of the Torrione Cambi the central summit was gained quite easily. For th~ descent we roped =down using a very rickety piton _for the bottom section. · · _There are many other magnificent ~limbs in this area: the traverse of all three peaks of the Corno Grande done by Douglas Side, E. toW., in fourteen hours from the hotel ~ . the Tre Spalle or W. ridge of the ~ Corno ·Piccolo which was done twice, I think, by James Joyce probably one of the finest climbs in the district ; 8 .S .E. arete of the :Corno Grande which should only be attempted under summer condi tions and defeated a strong American party, and many more climbs of all shades of difficulty. -
Winter Frosts Reduce Flower Bud Survival in High-Mountain Plants
plants Article Winter Frosts Reduce Flower Bud Survival in High-Mountain Plants Johanna Wagner *, Karla Gruber, Ursula Ladinig, Othmar Buchner and Gilbert Neuner * Department of Botany, Functional Plant Biology, University of Innsbruck, Sternwartestrasse 15, A-6020 Innsbruck, Austria; [email protected] (K.G.); [email protected] (U.L.); [email protected] (O.B.) * Correspondence: [email protected] (J.W.); [email protected] (G.N.); Tel.: +43-512-507-51026 (G.N.) Abstract: At higher elevations in the European Alps, plants may experience winter temperatures of −30 ◦C and lower at snow-free sites. Vegetative organs are usually sufficiently frost hardy to survive such low temperatures, but it is largely unknown if this also applies to generative structures. We investigated winter frost effects on flower buds in the cushion plants Saxifraga bryoides L. (subnival- nival) and Saxifraga moschata Wulfen (alpine-nival) growing at differently exposed sites, and the chionophilous cryptophyte Ranunculus glacialis L. (subnival-nival). Potted plants were subjected to short-time (ST) and long-time (LT) freezing between −10 and −30 ◦C in temperature-controlled freezers. Frost damage, ice nucleation and flowering frequency in summer were determined. Flower bud viability and flowering frequency decreased significantly with decreasing temperature and exposure time in both saxifrages. Already, −10 ◦C LT-freezing caused the first injuries. Below −20 ◦C, the mean losses were 47% (ST) and 75% (LT) in S. bryoides, and 19% (ST) and 38% (LT) in S. moschata. Winter buds of both saxifrages did not supercool, suggesting that damages were caused by freeze dehydration. -
CORDEX Regional Climate Models
1 Future snowfall in the Alps: Projections based on the EURO- 2 CORDEX regional climate models 3 Prisco Frei, Sven Kotlarski, Mark A. Liniger, Christoph Schär 4 5 6 - Response to Referees – 7 8 General 9 We thank the three referees for their careful revision of the manuscript and for their constructive comments. 10 Please find below our replies to all major comments and our suggestions on how to address these issues in a 11 revised manuscript. We hope that we satisfactorily addressed all referee comments and that the proposed 12 changes are considered as being appropriate. In case that not, we’d be looking forward to discuss individual 13 remaining issues in more detail. 14 As several referee comments addressed the RCM evaluation and the evaluation of the 2 km snowfall reference 15 itself, we’d like to put in front the following two statements on the scope of the paper: 16 17 (1) Our work is primarily concerned with the analysis of future snowfall projections. However, a basic notion on 18 the quality of raw RCM snowfall and, hence, the general ability of RCMs to represent our variable of interest is 19 required for such an exercise in our opinion. In the manuscript this is accomplished by comparing RCM raw 20 snowfall against site-scale measurements obtained from new snow sums (Figure 3). Such a comparison is 21 subject to considerable uncertainties, mostly originating from the scale gap between RCM grid cells and site-scale 22 observations and from representativity issues of observed snow cover. Due to a missing high-quality 23 observational reference at the scale of the RCM resolution (in our opinion also the HISTALP dataset has its 24 shortcomings; see below) we refrain from evaluating RCM snowfall in more detail and, at least when interpreting 25 raw snowfall change signals, implicitly assume stationary model biases.