Deutschlandwetter Im März 2013

The weather in Germany in March 2013 Cold March and lots of snow – many records in eastern and northern regions Offenbach, 28 March 2013 – After a relatively mild start, Germany was caught on the southern edge of a strong high pressure system over a large area of Northern Europe that, at times, drew in extremely cold air from the Arctic. This set a series of records for cold temperatures and quantities of snow, particularly for stations in the north and east. Only southern and central Germany experienced moments of spring-like weather. Altogether March was much too cold, with low levels of precipitation and above average sunshine nearly everywhere, as the initial analysis by the Deutscher Wetterdienst (DWD) of data from its around 2,000 weather stations shows. Initially, spring-like and mild but later bitter cold periods and continuous frost At 0.2 degrees Celsius (°C), the average temperature for Germany was 3.3 degrees below normal, as recorded by the international reference values for 1961 to 1990. Compared to the reference period 1981 to 2010, the negative deviation was as high as 4.1 degrees. This made March 2013 one of the six coldest March months nationwide since measurements began in 1881. The mild start was followed by an abrupt fall in temperature. While on 6 March, the temperature recorded at Dusseldorf airport was 20.2°C, which was a new record high for the first ten days of the month and thus the maximum for the month in Germany, seven days later the temperature was as low as -11.9°C. The sharpest frost of the month was on 16 March in Deutschneudorf-Brüderwiese in the Ore Mountain range, where the temperature was -21.3°C. Mid-March and then again 22 and 23 March saw a whole series of record cold temperatures at many measuring stations, particularly in the north and east of Germany. Coschen, to the south of Eisenhüttenstadt, reported a ten-day record of -18.9°C on 24 March. Wiesenburg, to the south-west of Potsdam, registered 15 days of continuous frost. It will become clearer where new negative records have been set for individual German federal States, once the DWD has made a precise analysis of results at the end of the month. Some areas under a continuous blanket of snow, yet much too dry Rainfall in March was around 36 litres per square metre (l/m²) and was therefore far below the long- term average of 57 l/m². In the north-east, almost all the precipitation fell as snow. The small-scale low pressure area “Xaver”, which crossed Germany from west to east on 12 March, had a great effect on the weather. It left a blanket of snow over a wide area, which – because of the low temperatures – did not melt for a long time. Consequently, since 10 March, Berlin has been blanketed by snow and this has been up to 20 cm deep in the last ten days of the month. There has been no snow this deep there in the last third of March since 1892. Total sunshine positive nearly everywhere The 124 hours of sunshine in Germany in March 2013 was 12 per cent more than the long-term average of 111 hours. The most sunshine was recorded in Grünow, to the north-east of Berlin, with around 190 hours. The least sunny place was Rheinfelden on the High Rhine at about 90 hours. .

Copy Link

Recommended publications

Annual Progress Report EU
Council Annual Progress Report on Actions taken under the CNL(21)36 Implementation Plan for the Calendar Year 2020 – EU – Germany Annual Progress Report on Actions taken under the Implementation Plan for the Calendar Year 2020 The Annual Progress Reports allow NASCO to evaluate progress on actions taken by Parties / jurisdictions to implement its internationally agreed Resolutions, Agreements and Guidelines and, consequently, the achievement of their objectives and actions taken in accordance with the Convention. The following information should be provided through the Annual Progress Reports: • any changes to the management regime for salmon and consequent changes to the Implementation Plan; • actions that have been taken under the Implementation Plan in the previous year; • significant changes to the status of stocks, and a report on catches; and • actions taken in accordance with the provisions of the Convention. In completing this Annual Progress Report please refer to the Guidelines for the Preparation and Evaluation of NASCO Implementation Plans and for Reporting on Progress, CNL(18)49. These reports will be reviewed by the Council. Please complete this form and return it to the Secretariat no later than 1 April 2021. Party: European Union Jurisdiction / Region: Germany 1: Changes to the Implementation Plan 1.1 Describe any proposed revisions to the Implementation Plan (Where changes are proposed, the revised Implementation Plans should be submitted to the Secretariat by 1 November). The response to question 4.3 (a)(i) will be revised in accordance with the recommendations of the NASCO IP Review Group and submitted to the Secretariat on time. 1.2 Describe any major new initiatives or achievements for salmon conservation and management that you wish to highlight.
[Show full text]
7.9 Biological Water Quality Classification (2000)
7.9 Biological Water Quality Classiﬁ cation (2000) The water courses in the mostly densely populated landscapes of Germany are subject to more or less intensive human use. This includes water abstraction for industries, small businesses, agriculture and public water supply and also the discharge of treated waste water. Waste water discharge is generally a point source of pollution and may have different impacts according to the discharge volume in relation to the river‘s runoff and the effectiveness of sewage treat- ment. Other impacts are from diffuse sources such as drainage from agricultural land or from livestock. The biological water quality chart of the LAWA (“saprobe chart”) describes the pollution affect- ing the oxygen balance of the water courses. It is essentially caused by carbon and nitrogen oxidation of easily bio-degradable sewage constituents. Methodology The basis of the method is the biological water analysis based on the saprobe system (DIN 38 410). The method of the LAWA for the indication and assessment of biological water quality is only applicable in flowing water courses, streams and rivers of Central Europe, and not in still waters. It is easily applicable, on the basis of uniform guidelines, for most water courses. There may be problems in the assessment of water courses which do not continuously flow, in very slow-flowing and barrier-regulated waters, in acidified waters or waters devastated by toxic substances, and in canals without adequate bank structure. Stretches of this kind are assigned a special symbol in the quality chart. If, in such cases, biological analysis is not possible, or Fig.
[Show full text]
The Present Status of the River Rhine with Special Emphasis on Fisheries Development
121 THE PRESENT STATUS OF THE RIVER RHINE WITH SPECIAL EMPHASIS ON FISHERIES DEVELOPMENT T. Brenner 1 A.D. Buijse2 M. Lauff3 J.F. Luquet4 E. Staub5 1 Ministry of Environment and Forestry Rheinland-Pfalz, P.O. Box 3160, D-55021 Mainz, Germany 2 Institute for Inland Water Management and Waste Water Treatment RIZA, P.O. Box 17, NL 8200 AA Lelystad, The Netherlands 3 Administrations des Eaux et Forets, Boite Postale 2513, L 1025 Luxembourg 4 Conseil Supérieur de la Peche, 23, Rue des Garennes, F 57155 Marly, France 5 Swiss Agency for the Environment, Forests and Landscape, CH 3003 Bern, Switzerland ABSTRACT The Rhine basin (1 320 km, 225 000 km2) is shared by nine countries (Switzerland, Italy, Liechtenstein, Austria, Germany, France, Luxemburg, Belgium and the Netherlands) with a population of about 54 million people and provides drinking water to 20 million of them. The Rhine is navigable from the North Sea up to Basel in Switzerland Key words: Rhine, restoration, aquatic biodiversity, fish and is one of the most important international migration waterways in the world. 122 The present status of the river Rhine Floodplains were reclaimed as early as the and groundwater protection. Possibilities for the Middle Ages and in the eighteenth and nineteenth cen- restoration of the River Rhine are limited by the multi- tury the channel of the Rhine had been subjected to purpose use of the river for shipping, hydropower, drastic changes to improve navigation as well as the drinking water and agriculture. Further recovery is discharge of water, ice and sediment. From 1945 until hampered by the numerous hydropower stations that the early 1970s water pollution due to domestic and interfere with downstream fish migration, the poor industrial wastewater increased dramatically.
[Show full text]
No Frontiers for the Rhine ICBR Inventory 2004 in the Rhine River Basin
IKSR CIPR No frontiers for the Rhine ICBR Inventory 2004 in the Rhine river basin Co-ordinating Committee RHINE INVENTORY ALONG THE RHINE CHANCES OFFERED BY AN EU DIRECTIVE the European Union aim at water Reduce pollution protection at a high level, no matter, whether groundwater, The status of waters may not dete- rivers, lakes or coastal waters are riorate under any circumstances. concerned. The EU Member States must take appropriate measures to improve waters which are expected to The target probably not meet the environ- is the good status mental objectives by 2015. All uses must be taken into account By 2015, rivers, lakes, coastal which directly or indirectly affect waters and groundwater are to the state of waters, no matter Photo: Stanko Petek, www.luftbild.com The Falls of the Rhine at Schaffhausen have reached a good status. The whether industry, navigation, the reference is the natural state of use of hydroelectric power or water bodies with their variety of agriculture is concerned. A central In 2004, a large scale inventory of plants and animals, an unaltered task in the Rhine river basin will be form and water regime and the to reduce polluting agents and to the Rhine and the waters in its natural quality of surface waters keep dangerous substances away catchment was concluded. Nine and groundwater. Distinctions are from waters. Apart from that the states were involved in this work made between: to which the European Water - the good ecological and chemical status for surface Framework Directive had given waters (rivers, lakes, transitional rise. This directive modernises and and coastal waters).
[Show full text]
Deutsche Bahn Integrated Interim Report January – June 2019 Germany Needs a Strong Rail System MORE ROBUST, MORE POWERFUL, MORE MODERN
Deutsche Bahn Integrated Interim Report January – June 2019 Germany needs a strong rail system MORE ROBUST, MORE POWERFUL, MORE MODERN STRONG RAIL Germany needs a strong rail system more than ever before. This will enable DB Group to fully focus on making a strong rail system possible in Germany in the future. Further Information µ3 ff. A strong rail system for our climate [ 1 ] A strong rail system for our climate means: a reduction in total CO₂ emis sions by 10 million tons per year. This corresponds to the annual CO₂ foot print of one million people. A strong rail system for the people [ 2 ] A strong rail system for the people means: twice as many rail passengers and five million car trips and 14,000 air flights less in Germany every day. A strong rail system for the economy [ 3 ] A strong rail system for the economy means: increasing the rail freight transport market share in Germany to 25%. This corresponds to 13 million fewer truck trips per year on German roads. A strong rail system for Europe [ 4 ] A strong rail system for Europe means: a joint implementation of European networking by means of a strong rail system, which is the decisive factor for achiev ing European climate protection targets and economic growth. At a glance H 1 Change Selected key figures 2019 2018 absolute % KEY FINANCIAL FIGURES (€ MILLION) Revenues adjusted 22,013 21,548 + 465 + 2.2 Revenues comparable 21,926 21,548 + 378 + 1.8 Profit before taxes on income 277 560 – 283 – 50.5 Net profit (after taxes) 205 562 – 357 – 63.5 EBITDA adjusted 1) 2,534 2,304
[Show full text]
Projected Changes in Rhine River Flood Seasonality Under
https://doi.org/10.5194/hess-2020-605 Preprint. Discussion started: 23 November 2020 c Author(s) 2020. CC BY 4.0 License. Projected changes in Rhine River flood seasonality under global warming Erwin Rottler1, Axel Bronstert1, Gerd Bürger1, and Oldrich Rakovec2,3 1Institute of Environmental Science and Geography, University of Potsdam, Karl-Liebknecht-Straße 24–25, 14476 Potsdam, Germany 2UFZ-Helmholtz Centre for Environmental Research, Permoserstraße 15, 04318 Leipzig, Germany 3Faculty of Environmental Sciences, Czech University of Life Sciences Prague, Kamýcká 129, Praha – Suchdol, 165 00, Czech Republic Correspondence: Erwin Rottler ([email protected]) Abstract. Climatic change alters the frequency and intensity of natural hazards. In order to assess potential future changes in flood seasonality in the Rhine River Basin, we analyse changes in streamflow, snowmelt, precipitation, and evapotranspiration at 1.5, 2.0 and 3.0 ◦C global warming levels. The mesoscale Hydrological Model (mHM) forced with an ensemble of climate projection scenarios (five general circulation models under three representative concentration pathways) is used to simulate the 5 present and future climate conditions of both, pluvial and nival hydrological regimes. Our results indicate that the interplay between changes in snowmelt- and rainfall-driven runoff is crucial to understand changes in streamflow maxima in the Rhine River. Climate projections suggest that future changes in flood characteristics in the entire Rhine River are controlled by both, more intense precipitation events and diminishing snow packs. The nature of this interplay defines the type of change in runoff peaks. On the sub-basin level (the Moselle River), more intense rainfall 10 during winter is mostly counterbalanced by reduced snowmelt contribution to the streamflow.
[Show full text]
Rare Earth Elements As Emerging Contaminants in the Rhine River, Germany and Its Tributaries
Rare earth elements as emerging contaminants in the Rhine River, Germany and its tributaries by Serkan Kulaksız A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geochemistry Approved, Thesis Committee _____________________________________ Prof. Dr. Michael Bau, Chair Jacobs University Bremen _____________________________________ Prof. Dr. Andrea Koschinsky Jacobs University Bremen _____________________________________ Dr. Dieter Garbe-Schönberg Universität Kiel Date of Defense: June 7th, 2012 _____________________________________ School of Engineering and Science TABLE OF CONTENTS CHAPTER I – INTRODUCTION 1 1. Outline 1 2. Research Goals 4 3. Geochemistry of the Rare Earth Elements 6 3.1 Controls on Rare Earth Elements in River Waters 6 3.2 Rare Earth Elements in Estuaries and Seawater 8 3.3 Anthropogenic Gadolinium 9 3.3.1 Controls on Anthropogenic Gadolinium 10 4. Demand for Rare Earth Elements 12 5 Rare Earth Element Toxicity 16 6. Study Area 17 7. References 19 Acknowledgements 28 CHAPTER II – SAMPLING AND METHODS 31 1. Sample Preparation 31 1.1 Pre‐concentration 32 2. Methods 34 2.1 HCO3 titration 34 2.2 Ion Chromatography 34 2.3 Inductively Coupled Plasma – Optical Emission Spectrometer 35 2.4 Inductively Coupled Plasma – Mass Spectrometer 35 2.4.1 Method reliability 36 3. References 41 CHAPTER III – RARE EARTH ELEMENTS IN THE RHINE RIVER, GERMANY: FIRST CASE OF ANTHROPOGENIC LANTHANUM AS A DISSOLVED MICROCONTAMINANT IN THE HYDROSPHERE 43 Abstract 44 1. Introduction 44 2. Sampling sites and Methods 46 2.1 Samples 46 2.2 Methods 46 2.3 Quantification of REE anomalies 47 3. Results and Discussion 48 4.
[Show full text]
Download Trias, Eine Ganz Andere Welt: Europa Im Fru¨Hen Erdmittelalter Pool/Steinsalzverbreitung.Pdf)
Swiss J Geosci (2016) 109:241–255 DOI 10.1007/s00015-016-0209-4 Reorganisation of the Triassic stratigraphic nomenclature of northern Switzerland: overview and the new Dinkelberg, Kaiseraugst and Zeglingen formations Peter Jordan1,2 Received: 12 November 2015 / Accepted: 9 February 2016 / Published online: 3 March 2016 Ó Swiss Geological Society 2016 Abstract In the context of the harmonisation of the Swiss massive halite deposits. It continues with sulfate and marl stratigraphic scheme (HARMOS project), the stratigraphic sequences and ends with littoral stromatolitic dolomite. In nomenclature of the Triassic sedimentary succession of the WSW–ENE trending depot centre total formation northern Switzerland has been reorganised to six forma- thickness is 150 m and more, and thickness of salt layers tions (from base to top): Dinkelberg, Kaiseraugst, Zeglin- reaches up to 100 m. In the High Rhine area, the thickness gen, Schinznach, Ba¨nkerjoch, and Klettgau Formation. is reduced due to subrecent subrosion. At some places The ﬁrst three are formally introduced in this paper. evidence points to syn- to early-post-diagenetic erosion. The Dinkelberg Formation (formerly «Buntsandstein») For practical reasons, the six formations are organised in encompasses the siliciclastic, mainly ﬂuvial to coastal three lithostratigraphic groups: Buntsandstein Group (with marine sediments of Olenekian to early Anisian age. The the Dinkelberg Formation), Muschelkalk Group (combin- formation is some 100 m thick in the Basel area and ing the Kaiseraugst, Zeglingen and Schinznach Forma- wedges out towards southeast. The Kaiseraugst Formation tions) and Keuper Group (combining the Ba¨nkerjoch and (formerly «Wellengebirge») comprises fossiliferous silici- Klettgau Formations). clastic and carbonate sediments documenting a marine transgressive—regressive episode in early Anisian time.
[Show full text]
Four Headwaters Trail Through the St Gotthard Massif
A hike to the headwaters of the Rivers Rhine, Reuss, Ticino and Rhone. Four Headwaters Trail through the St Gotthard Massif Lak e Grim - r Lake Göscheneralp sel e e i La n Göschenen ke O c Sidelen be o a raar Source of the l h Hut SAC R G Rhone Belvédère Grimsel Pass Lake 5 Tiefenbach Tote Andermatt - otthard Oberalp Pass orn-G B) Furk Matterh y (MG a mo Railwa Furka Pass (st unt Oberwald eam ain ake ra s L lp ilw e bera a ct O Gletsch y) io ne n l Realp Ulrichen ho e Hospental R n ) n s tu s e Münster e r s p Headwaters 4 a x B E B - - l GB) r B of the Rhine ne hn (M a e hi rd-Ba k e d R ha i d n S ott Obergesteln r r -G c r l orn u s n a erh F a a e att l s u h h Lake Toma M G u t t n ( t t e t n d o o u R a t G G o Tschamut y r a Vermigel Sedrun w l i Maighels Lake a Hut SAC r Hut SAC Headwaters Lucendro s of the lp Gotthard Pass a 2 1 N Nufenen Pass Gotthard-Reuss e Lake Val Maighels k a Piansecco Sella L Hut SAC Lucendro Pass Maighels Pass Lake Gries Cruina 3 Ti Headwaters cin Bedretto o Villa Airolo of the Ticino All’Acqua Ronco Stage 1 Stage 2 Stage 3 Stage 4 Stage 5 Reproduced by permission of swisstopo (BA120056) 2044 m 2345 m 2314 m 2421 m 2042 m 2042 m 2375 m 2701 m 2776 m 2256 m 2091 m 2091 m 2182 m 2522 m 2128 m 2015 m 1996 m 1938 m 1982 m 1982 m 2093 m 2003 m 2440 m 1925 m 1762 m 1533 m 1355 m 1355 m 1368 m 1550 m 1757 m 2170 m 2429 m 2271 m Oberalp Lake Maighel Maighel Vermigel Vermigel Summer- Sella Giübin Lake Gotthard Gotthard Alpe di Lucendro Rosso Ri di Ri di Ri di Piansecco Piansecco Nufenen Alpe di Nufenen Ladstafel
[Show full text]
Climate Indices in Historical Climate Reconstructions: a Global State-Of-The-Art
Climate indices in historical climate reconstructions: A global state-of-the-art David J. Nasha,b, George C.D. Adamsonc, Linden Ashcroftd,e, Martin Bauchf, Chantal Camenischg,h, Dagomar Degrooti, Joelle Gergisj,k, Adrian Jusopovićl, Thomas Labbéf,m, Kuan-Hui Elaine Linn,o, Sharon D. Nicholsonp, Qing Peiq, María del Rosario Prietor†, Ursula Racks, Facundo Rojasr and Sam Whitet a School of Environment and Technology, University of Brighton, Brighton, United Kingdom b School of Geography, Archaeology and Environmental Studies, University of the Witwatersrand, Johannesburg, South Africa c Department of Geography, King’s College London, London, United Kingdom d School of Earth Sciences, University of Melbourne, Melbourne, Australia e ARC Centre of Excellence for Climate Extremes, University of Melbourne, Melbourne, Australia f Leibniz Institute for the History and Culture of Eastern Europe, University of Leipzig, Leipzig, Germany g Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland h Institute of History, University of Bern, Bern, Switzerland i Department of History, Georgetown University, Washington DC, USA j Fenner School of Environment & Society, Australian National University, Canberra, Australia k ARC Centre of Excellence for Climate Extremes, Australian National University, Canberra, Australia I Institute of History, Polish Academy of Sciences, Warsaw, Poland m Maison des Sciences de l'Homme de Dijon, University of Burgundy, Dijon, France n Research Center for Environmental Changes, Academia Sinica, Taipei,
[Show full text]
Odonatological Abstract Service
Odonatological Abstract Service published by the INTERNATIONAL DRAGONFLY FUND (IDF) in cooperation with the WORLDWIDE DRAGONFLY ASSOCIATION (WDA) Editors: Dr. Martin Lindeboom, Silberdistelweg 11, D-72113 Ammerbuch, Germany. Tel. ++49 (0)7073 300770; E-mail: [email protected] Dr. Klaus Reinhardt, Dept Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, UK. Tel. ++44 114 222 0105; E-mail: [email protected] Martin Schorr, Schulstr. 7B, D-54314 Zerf, Germany. Tel. ++49 (0)6587 1025; E-mail: [email protected] Published in Rheinfelden, Germany and printed in Trier, Germany. ISSN 1438-0269 1997 than 500 taxa below the family level were inventoried, and each listing includes relative frequency of en- 7574. He, J.-r.; Jiang B.-h.; Chen, T.-s. (1997): The counter, life stages collected, and dominant role in the aquatic insects of Rainbow Lake. Conservation Quar- greenleaf manzanita community. Specific host relation- terly, summer quarterly, June,1997,18: 37-41. (in Chi- ships are included for some predators and parasitoids. nese) [Rainbow Lake is an alpine Lake in Taiwan. The Herbivores, predators, and parasitoids comprised the paper provides brief information on Aeshna petalura majority (80 percent) of identified insects and related and Polycanthagyna erythromelas. (Abstract by Hao- taxa." (Authors) The list of Odonata includes the follow- miao Zhang)] ing taxa: Aeshna palmata, Anax junius, Cordulegaster dorsalis, Libellula sp., Pantala hymenea, Tarnetrum cor- 7575. Liebherr, J.K.; Polhemus, D.A. (1997): R.C.L. rupturn, Lestidae species undet., and Coenagrionidae Perkins: 100 years of Hawaiian entomology. Pacif. Sci. species undet..] Address: http://www.fs.fed.us/psw/pub- 51(4): 343-355, 1 pl.
[Show full text]
Case Study Rhine
International Commission for the Hydrology of the Rhine Basin Erosion, Transport and Deposition of Sediment - Case Study Rhine - Edited by: Manfred Spreafico Christoph Lehmann National coordinators: Alessandro Grasso, Switzerland Emil Gölz, Germany Wilfried ten Brinke, The Netherlands With contributions from: Jos Brils Martin Keller Emiel van Velzen Schälchli, Abegg & Hunzinger Hunziker, Zarn & Partner Contribution to the International Sediment Initiative of UNESCO/IHP Report no II-20 of the CHR International Commission for the Hydrology of the Rhine Basin Erosion, Transport and Deposition of Sediment - Case Study Rhine - Edited by: Manfred Spreafico Christoph Lehmann National coordinators: Alessandro Grasso, Switzerland Emil Gölz, Germany Wilfried ten Brinke, The Netherlands With contributions from: Jos Brils Martin Keller Emiel van Velzen Schälchli, Abegg & Hunzinger Hunziker, Zarn & Partner Contribution to the International Sediment Initiative of UNESCO/IHP Report no II-20 of the CHR © 2009, KHR/CHR ISBN 978-90-70980-34-4 Preface „Erosion, transport and deposition of sediment“ Case Study Rhine ________________________________________ Erosion, transport and deposition of sediment have significant economic, environmental and social impacts in large river basins. The International Sediment Initiative (ISI) of UNESCO provides with its projects an important contribution to sustainable sediment and water management in river basins. With the processing of exemplary case studies from large river basins good examples of sediment management prac- tices have been prepared and successful strategies and procedures will be made accessible to experts from other river basins. The CHR produced the “Case Study Rhine” in the framework of ISI. Sediment experts of the Rhine riparian states of Switzerland, Austria, Germany and The Netherlands have implemented their experiences in this publication.
[Show full text]