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Coping with the Long Term
Coping with the Long Term An Empirical Analysis of Time Perspectives, Time Orientations, and Temporal Uncertainty in Forestry Coping with the Long Term An Empirical Analysis of Time Perspectives, Time Orientations, and Temporal Uncertainty in Forestry Marjanke Alberttine Hoogstra Marjanke A. Hoogstra Coping with the Long Term An Empirical Analysis of Time Perspectives, Time Orientations, and Temporal Uncertainty in Forestry Marjanke Alberttine Hoogstra Promotoren: Prof. dr. H. (Heiner) Schanz Hoogleraar Märkte der Wald- und Holzwirtschaft Institut für Forst- und Umweltpolitik Albert-Ludwigs-Universität Freiburg, Duitsland Prof. dr. B.J.M (Bas) Arts Hoogleraar Bos- en Natuurbeleid Leerstoelgroep Bos- en Natuurbeleid Wageningen Universiteit, Nederland Promotiecommissie: Prof. dr. ir. G.M.J. Mohren (Wageningen Universiteit, Nederland) Prof. dr. G. Oesten (Albert-Ludwigs-Universität Freiburg, Duitsland) Dr. M. Pregernig (Universität für Bodenkultur Wien, Oostenrijk) Prof. dr. B.J. Thorsen (Københavns Universitet, Denemarken) Dit onderzoek is uitgevoerd binnen Mansholt Graduate School of Social Sciences Coping with the Long Term An Empirical Analysis of Time Perspectives, Time Orientations, and Temporal Uncertainty in Forestry Marjanke Alberttine Hoogstra Proefschrift ter verkrijging van de graad van doctor op gezag van de rector magnificus van Wageningen Universiteit, Prof. dr. M.J. Kropff, in het openbaar te verdedigen op dinsdag 16 december 2008 des middags te half twee in de Aula Hoogstra, M.A. [2008] Coping with the Long Term - An Empirical Analysis of Time Perspectives, Time Orientations, and Temporal Uncertainty in Forestry. PhD thesis Forest and Nature Conservation Policy Group, Wageningen University, Wageningen, the Netherlands. With references - with summary in Dutch and in English. ISBN 978-90-8585-242-1 The Road goes ever on and on Down from the door where it began. -
EGU2014-6135, 2014 EGU General Assembly 2014 © Author(S) 2014
Geophysical Research Abstracts Vol. 16, EGU2014-6135, 2014 EGU General Assembly 2014 © Author(s) 2014. CC Attribution 3.0 License. Dynamic aspects of windstorm Kyrill (January 2007) Patrick Ludwig (1), Joaquim G. Pinto (1,2), Simona A. Hoepp (1), Andreas H. Fink (3), and Suzanne L. Gray (2) (1) Institute for Geophysics and Meteorology, University of Cologne, Cologne, Germany ([email protected]), (2) Department of Meteorology, University of Reading, Reading, United Kingdom, (3) Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany Several dynamical and mesoscale aspects concerning severe windstorm Kyrill (January 2007) are analysed by results of high-resolution simulations with the regional climate model (RCM) COSMO-CLM. After explosive cyclogenesis south of Greenland takes place while crossing a very intense upper-level jet stream, Kyrill underwent secondary cyclogenesis over the North Atlantic Ocean just west of the British Isles. The secondary cyclogenesis (Kyrill II), was located on the occlusion front of the mature cyclone (Kyrill I), which is very unusual compared to typical frontal cyclogenesis generally occurring along the trailing cold fronts of existing cyclones. The mechanisms of secondary cyclogenesis are investigated based on moderate-resolution (0.0625◦ grid spacing) RCM simulations. The formation of Kyrill II along the occlusion front follows common mechanism for secondary cyclogenesis like breaking up of a local, low tropospheric PV strip along the front and diabatic heating with associated development of a vertical extended PV tower. Kyrill II propagated further towards Europe, and its development was favoured by a split jet structure aloft the surface cyclone, which maintained the deep core pressure (around 961 - 965 hPa) for at least 36 hours. -
Downloaded 10/05/21 02:25 PM UTC 3568 JOURNAL of the ATMOSPHERIC SCIENCES VOLUME 74
NOVEMBER 2017 B Ü ELER AND PFAHL 3567 Potential Vorticity Diagnostics to Quantify Effects of Latent Heating in Extratropical Cyclones. Part I: Methodology DOMINIK BÜELER AND STEPHAN PFAHL Institute for Atmospheric and Climate Science, ETH Zurich,€ Zurich, Switzerland (Manuscript received 9 February 2017, in final form 31 July 2017) ABSTRACT Extratropical cyclones develop because of baroclinic instability, but their intensification is often sub- stantially amplified by diabatic processes, most importantly, latent heating (LH) through cloud formation. Although this amplification is well understood for individual cyclones, there is still need for a systematic and quantitative investigation of how LH affects cyclone intensification in different, particularly warmer and moister, climates. For this purpose, the authors introduce a simple diagnostic to quantify the contribution of LH to cyclone intensification within the potential vorticity (PV) framework. The two leading terms in the PV tendency equation, diabatic PV modification and vertical advection, are used to derive a diagnostic equation to explicitly calculate the fraction of a cyclone’s positive lower-tropospheric PV anomaly caused by LH. The strength of this anomaly is strongly coupled to cyclone intensity and the associated impacts in terms of surface weather. To evaluate the performance of the diagnostic, sensitivity simulations of 12 Northern Hemisphere cyclones with artificially modified LH are carried out with a numerical weather prediction model. Based on these simulations, it is demonstrated that the PV diagnostic captures the mean sensitivity of the cyclones’ PV structure to LH as well as parts of the strong case-to-case variability. The simple and versatile PV diagnostic will be the basis for future climatological studies of LH effects on cyclone intensification. -
Severe Storm Xynthia Over Southwestern and Western Europe
Severe Storm Xynthia over southwestern and western Europe A severe storm named “Xynthia” affected Portugal, Spain, Switzerland, France, parts of south-east England, Belgium, the Netherlands, Luxembourg, Germany and Austria. Strong gusts on 27-28 February 2010 caused extended damage on traffic routes, electrical power outage, destruction due to flooding at the French Atlantic coast and more than 60 losses of lives. Most of the damage was in France and western Germany. The track of this storm and its rapid development were outstanding, but the magnitude of the gusts was comparable to other violent storms in the past. Synoptical development and weather conditions Xynthia arose from an initially shallow low pressure system which formed over the subtropical sea area south of the Azores Islands on Friday, 26 February 2010. The southward flow of colder air masses in the upper air caused the deepening of a broad trough over the central and eastern North Atlantic. A shortwave trough within this broader system and a high temperature difference between extremely warm air over Africa and colder air over the eastern Atlantic caused a strong cyclogenesis of Xynthia. On Saturday, February 27, the cyclone moved northeastwards over Portugal and the Bay of Biscay to the westernmost areas of France and intensified very rapidly to a core pressure of about 967 hPa around midnight which means a deepening of about 20 hPa within 24 hours (Fig. 1-3). During the following three days it began weakening and moved further northeastwards along the coastline of northern France and the North Sea, and then it crossed the southern Baltic Sea to southern Finland until March 3. -
Orkantief Sabine Löst Am 09./10. Februar 2020 Eine Schwere Sturmlage Über Europa Aus
Abteilung Klimaüberwachung Orkantief Sabine löst am 09./10. Februar 2020 eine schwere Sturmlage über Europa aus Autor(inn)en: Susanne Haeseler, Peter Bissolli, Jan Dassler, Volker Zins, Andrea Kreis Stand: 13.02.2020 Zusammenfassung Orkantief SABINE (in Westeuropa CIARA und in Norwegen ELSA benannt) löste am 9./10. Februar 2020 deutschlandweit Sturmböen bis Orkanstärke (12 Bft) aus. Die höchste Böe meldete der Feldberg im Schwarzwald am 10. Januar mit 49,1 m/s bzw. 177 km/h. Der Kern des Orkantiefs zog vom Atlantik kommend über Schottland nach Norwegen, wobei der Kerndruck zeitweise unter 945 hPa lag. Zwischen Nord- und Südeuropa bestanden Luftdruckunterschiede von etwa 80 hPa. Das dadurch generierte Sturmfeld erfasste weite Teile West-, Mittel- und Nordeuropas. In Deutschland war der Sturm, der sich von der Nordsee in Richtung Alpen ausweitete, von teils kräftigen Schauern und Gewittern begleitet. An der Nordsee gab es vom 10. bis 12. Januar mehrere teils schwere Sturmfluten (Abb. 1 und 4). Die extreme Sturmlage war schon Tage vorher angekündigt und es wurde von Tätigkeiten im Freien sowie Reisen während dieser Zeit abgeraten. Sport- und Musikveranstaltungen wurden vorsichtshalber abgesagt. Am 9./10. Februar stellte die Bahn in Deutschland den Verkehr zeitweise ein. Flüge und Fährverbindungen fielen aus. Viele Schulen und Kindergärten blieben am 10. Februar geschlossen. Der Sturm ließ in den betroffenen Ländern Bäume umstürzen und deckte Hausdächer ab. Auf den Britischen Inseln kam es zu Überschwemmungen. In einigen Regionen (auch in Deutschland) gab es Stromausfälle. Abbildung 1: Sturmflut am Weststrand von Norderney. Die Wellen laufen bis auf die Promenade, die als Küstenschutz dient, herauf. -
Use of the European Severe Weather Database to Verify Satellite-Based Storm Detection Or Nowcasting
USE OF THE EUROPEAN SEVERE WEATHER DATABASE TO VERIFY SATELLITE-BASED STORM DETECTION OR NOWCASTING Nikolai Dotzek1,2, Caroline Forster1 1 Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, 82234 Wessling, Germany 2 European Severe Storms Laboratory, Münchner Str. 20, 82234 Wessling, Germany Abstract Severe thunderstorms constitute a major weather hazard in Europe, with an estimated total damage of € 5-8 billion each year. Yet a pan-European database of severe weather reports in a homogeneous data format has become available only recently: the European Severe Weather Database (ESWD). We demonstrate the large potential of ESWD applications for storm detection and forecast or now- casting/warning verification purposes. The study of five warm-season severe weather days in Europe from 2007 and 2008 revealed that up to 47% of the ESWD reports were located exactly within the polygons detected by the Cb-TRAM algorithm for three different stages of deep moist convection. The cool-season case study of extratropical cyclone “Emma” on 1 March 2008 showed that low-topped winter thunderstorms can provide a challenge for satellite storm detection and nowcasting adapted to warm-season storms with high, cold cloud tops. However, this case also demonstrated how ESWD reports alone can still be valuable to identify the hazardous regions along the cold front of the cyclone. 1. INTRODUCTION Severe thunderstorms, with their attendant strong winds, hail, flooding, and tornadoes, are common phenomena in many European countries, leading to a total damage estimate of 5 to 8 billion euros per year (source: Munich Re Group). Extreme events like an F4 tornado in France and an F3 downburst in Austria in 2008 exemplify these damage totals. -
Annual Report 2018 YEARS Local Leader, Global Partner CONTENTS
Annual Report 2018 YEARS Local Leader, Global Partner CONTENTS General Information Financial Status 2 Vision-Mission 44 Economic Outlook 3 Shareholder Structure 50 Turkish Insurance Industry 4 Corporate Profile 52 Turkish Reinsurance Market and Milli Re in 2018 6 Milestones 56 Global Reinsurance Market and Milli Re in 2018 12 Chairman’s Message 63 Financial Strength, Profitability and Solvency 14 General Manager’s Message 64 Key Financial Indicators 20 Board of Directors 66 The Company Capital 23 Participation of the Members of the Board of Directors in 67 2018 Technical Results Relevant Meetings during the Fiscal Period 69 2018 Financial Results 24 Senior Management 71 General Assembly Agenda 25 Internal Systems Managers 72 Report by the Board of Directors 26 Organization Chart 74 Dividend Distribution Policy 27 Human Resources Applications 75 Dividend Distribution Proposal 28 2018 Annual Report Compliance Statement 29 Independent Auditor’s Report on the Annual Report of the Board Risks and Assessment of the Governing Body of Directors 77 Risk Management 81 Assessment of Capital Adequacy Financial Rights Provided to the Members of the Governing 81 Transactions Carried Out with Milli Re’s Risk Group Body and Senior Executives 81 The Annual Reports of the Parent Company in the Group of 32 Financial Rights Provided to the Members of the Governing Body Companies and Senior Executives Unconsolidated Financial Statements Together with Research & Development Activities Independent Auditors’ Report Thereon 32 Research & Development Activities -
Extreme Weather Events in Europe: Preparing for Climate Change Adaptation
Extreme Weather Events in Europe: preparing for climate change adaptation October 2013 ISBN (print) 978-82-7144-100-5 ISBN (electronic) 978-82-7144-101-2 In cooperation with This report can be found at www.dnva.no Produced by the Norwegian Meteorological Institute Extreme Weather Events in Europe: preparing for climate change adaptation Øystein Hov, Ulrich Cubasch, Erich Fischer, Peter Höppe, Trond Iversen, Nils Gunnar Kvamstø, Zbigniew W. Kundzewicz, Daniela Rezacova, David Rios, Filipe Duarte Santos, Bruno Schädler, Ottó Veisz, Christos Zerefos, Rasmus Benestad, John Murlis, M. Donat, Gregor C. Leckebusch, Uwe Ulbrich. Extreme Weather Events in Europe: preparing for climate change adaptation In cooperation with CONTRIBUTORS Professor Øystein Hov, Norwegian Meteorological Institute, Norway† Professor Ulrich Cubasch, Free University of Berlin, Germany* Dr Erich Fischer, Institute for Atmospheric and Climatic Science, ETH Zurich, Switzerland* Professor Peter Höppe, Geo Risks Research/Corporate Climate Centre, Munich Re, Germany* Professor Trond Iversen, Norwegian Meteorological Institute, Norway* Professor Nils Gunnar Kvamstø, Department of Geophysics, University of Bergen, Norway* Professor Zbigniew W. Kundzewicz, Polish Academy of Sciences, Warsaw, Poland* Professor Daniela Rezacova, Institute of Atmospheric Physics, Academy of Sciences of the Czech Republic, Prague, Czech Republic* Professor David Rios, Royal Academy of Sciences, Spain* Professor Filipe Duarte Santos, Lisbon University, Portugal* Dr Bruno Schädler, University of Berne, Switzerland* Professor Ottó Veisz, Agricultural Research Institute of the Hungarian Academy of Sciences, Budapest, Hungary* Professor Christos Zerefos, University of Athens, Greece* Dr Rasmus Benestad (Working Group Researcher), Norwegian Meteorological Institute, Oslo, Norway Professor John Murlis, EASAC Environment Programme Secretary Dr M. Donat, Institut für Meteorologie, Freie Universität Berlin, Germany; now at Climate Change Research Centre, University of New South Wales, Sydney, Australia Dr Gregor C. -
Title Author(S)
th 5 European Conference on Severe Storms 12 - 16 October 2009 - Landshut - GERMANY ECSS 2009 Abstracts by session ECSS 2009 - 5th European Conference on Severe Storms 12-16 October 2009 - Landshut – GERMANY List of the abstract accepted for presentation at the conference: O – Oral presentation P – Poster presentation Session 09: Severe storm case studies and field campaigns, e.g. COPS, THORPEX, VORTEX2 Page Type Abstract Title Author(s) An F3 downburst in Austria - a case study with special G. Pistotnik, A. M. Holzer, R. 265 O focus on the importance of real-time site surveys Kaltenböck, S. Tschannett J. Bech, N. Pineda, M. Aran, J. An observational analysis of a tornadic severe weather 267 O Amaro, M. Gayà, J. Arús, J. event Montanyà, O. van der Velde Case study: Extensive wind damage across Slovenia on July M. Korosec, J. Cedilnik 269 O 13th, 2008 Observed transition from an elevated mesoscale convective J. Marsham, S. Trier, T. 271 O system to a surface based squall line: 13th June, Weckwerth, J. Wilson, A. Blyth IHOP_2002 08/08/08: classification and simulation challenge of the A. Pucillo, A. Manzato 273 O FVG olympic storm H. Bluestein, D. Burgess, D. VORTEX2: The Second Verification of the Origins of Dowell, P. Markowski, E. 275 O Rotation in Tornadoes Experiment Rasmussen, Y. Richardson, L. Wicker, J. Wurman Observations of the initiation and development of severe A. Blyth, K. Browning, J. O convective storms during CSIP Marsham, P. Clark, L. Bennett The development of tornadic storms near a surface warm P. Groenemeijer, U. Corsmeier, 277 O front in central England during the Convective Storm C. -
Homo Erectus, Became Extinct About 1.7 Million Years Ago
Bear & Company One Park Street Rochester, Vermont 05767 www.BearandCompanyBooks.com Bear & Company is a division of Inner Traditions International Copyright © 2013 by Frank Joseph All rights reserved. No part of this book may be reproduced or utilized in any form or by any means, electronic or mechanical, including photocopying, recording, or by any information storage and retrieval system, without permission in writing from the publisher. Library of Congress Cataloging-in-Publication Data Joseph, Frank. Before Atlantis : 20 million years of human and pre-human cultures / Frank Joseph. p. cm. Includes bibliographical references. Summary: “A comprehensive exploration of Earth’s ancient past, the evolution of humanity, the rise of civilization, and the effects of global catastrophe”—Provided by publisher. print ISBN: 978-1-59143-157-2 ebook ISBN: 978-1-59143-826-7 1. Prehistoric peoples. 2. Civilization, Ancient. 3. Atlantis (Legendary place) I. Title. GN740.J68 2013 930—dc23 2012037131 Chapter 8 is a revised, expanded version of the original article that appeared in The Barnes Review (Washington, D.C., Volume XVII, Number 4, July/August 2011), and chapter 9 is a revised and expanded version of the original article that appeared in The Barnes Review (Washington, D.C., Volume XVII, Number 5, September/October 2011). Both are republished here with permission. To send correspondence to the author of this book, mail a first-class letter to the author c/o Inner Traditions • Bear & Company, One Park Street, Rochester, VT 05767, and we will forward the communication. BEFORE ATLANTIS “Making use of extensive evidence from biology, genetics, geology, archaeology, art history, cultural anthropology, and archaeoastronomy, Frank Joseph offers readers many intriguing alternative ideas about the origin of the human species, the origin of civilization, and the peopling of the Americas.” MICHAEL A. -
Originally Published As
Originally published as: Klaus, M., Holsten, A., Hostert, P., Kropp, J. P. (2011): Integrated methodology to assess windthrow impacts on forest stands under climate change. - Forest Ecology and Management, 261, 11, 1799-1810 DOI: 10.1016/j.foreco.2011.02.002 An integrated methodology to assess windthrow impacts on forest stands under climate change M. Klausa,b, A. Holstena, P. Hostertb, J.P. Kroppa aPotsdam Institute for Climate Impact Research, P.O. Box 60 12 03, 14412 Potsdam, Germany bGeography Department, Humboldt-Universit¨at zu Berlin, Unter den Linden 6, 10099 Berlin, Ger- many Corresponding author: Anne Holsten: Tel.: +49 0 331 288 2689, E-mail address: holsten@pik- potsdam.de Abstract Storms have a high potential to cause severe ecological and economic losses in forests. We performed a logistic regression analysis to create a storm damage sen- sitivity index for North Rhine-Westphalia, Germany, based on damage data of the storm event “Kyrill”. Future storm conditions were derived from two regional climate models. We combined these measures to an impact metric, which is embedded in a broader vulnerability framework and quantifies the impacts of winter storms un- der climate change until 2060. Sensitivity of forest stands to windthrow was mainly driven by a high proportion of coniferous trees, a complex orography and poor quality soils. Both climate models simulated an increase in the frequency of severe storms, whereby differences between regions and models were substantial. Potential impacts will increase although they will vary among regions with the highest impacts in the mountainous regions. Our results emphasise the need for combining storm damage sensitivity with climate change signals in order to develop forest protection measures. -
The Characteristics and Structure of Extra-Tropical Cyclones in a Warmer Climate Victoria A
https://doi.org/10.5194/wcd-2019-2 Preprint. Discussion started: 27 August 2019 c Author(s) 2019. CC BY 4.0 License. The characteristics and structure of extra-tropical cyclones in a warmer climate Victoria A. Sinclair1, Mika Rantanen1, Päivi Haapanala1, Jouni Räisänen1, and Heikki Järvinen1 1Institute for Atmospheric and Earth System Research / Physics, Faculty of Science, University of Helsinki, PO BOX 64, FI-00014 Correspondence: Victoria Sinclair (Victoria.Sinclair@helsinki.fi) Abstract. Little is known about how the structure of extra-tropical cyclones will change in the future. In this study aquaplanet simulations are performed with a full complexity atmospheric model. These experiments can be considered as an intermediate step towards increasing knowledge of how, and why, extra-tropical cyclones respond to warming. A control simulation and a warm simulation in which the sea surface temperatures are increased uniformly by 4 K are run for 11 years. Extra-tropical 5 cyclones are tracked, cyclone composites created, and the omega equation applied to assess causes of changes in vertical motion. Warming leads to a 3.3% decrease in the number of extra-tropical cyclones, no change to the median intensity nor life time of extra-tropical cyclones, but to a broadening of the intensity distribution resulting in both more stronger and more weaker storms. Composites of the strongest extra-tropical cyclones show that total column water vapour increases everywhere relative to the cyclone centre and that precipitation increases by up to 50% with the 4 K warming. The spatial structure 10 of the composite cyclone changes with warming: the 900–700-hPa layer averaged potential vorticity, 700-hPa ascent and precipitation maximums associated with the warm front all move polewards and downstream and the area of ascent expands in the downstream direction.