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High Level of Protection Against Water-Related Disease (Art
WHO Collaborating Centre for Health Promoting Water Management and Risk Communication Institute for Hygiene and Public Health University of Bonn WaMRi-Newsletter No. 9, February 2006 Dear Reader, The Protocol on Water and Health to the 1992 Convention on the Protection and Use of Transboundary Watercourses and International Lakes finally entered into force. On 4th August 2005 it became legally binding for the 16 ratifying countries. It is the first major international legal approach for prevention, control and reduction of water-related diseases in Europe. Please read more about it in our first contribution of the WaMRi-Newsletter. This issue also deals with the project Swist III , focussed on River Swist in North Rhine- Westphalia as an example for microbial load of watercourses due to diffuse polluters. The report from the Aral Sea Basin Water and Food Conference summarizes its main findings entitled as “ Managing Water and Food Quality in Central Asia ” which took place in Almaty, Kazakhstan, on 1-2 September 2005. We would like to inform you that only the authors are responsible for the content of their articles and they do not necessary reflect the opinions or positions of the WHO CC. Content The Protocol on Water and Health p. 2 River Swist in North Rhine-Westphalia as an example for microbial load of watercourses due to diffuse polluters – an interim result p. 5 News from the Aral Sea Basin Water and Food Conference p. 9 Special events on water, environment and health p.11 Links p.12 Selected books and articles p.13 Head of WHO CC : Dr. -
Die Swist Die Bäche Und Das Grundwasser Im Swistgebiet - Zustand, Ursachen Von Belastungen Und Maßnahmen
Die Swist Die Bäche und das Grundwasser im Swistgebiet - Zustand, Ursachen von Belastungen und Maßnahmen www.umwelt.nrw.de PE_ERF_1400.indd 1 14.12.2008, 15:34 PE_ERF_1400.indd 2 14.12.2008, 15:34 Inhalt 5 Vorworte 8 Wasser ist Leben 8 Die europäische Wasserrahmenrichtlinie: Fahrplan für unsere Flüsse, Seen und das Grundwasser 9 NRW ist aktiv 9 Mischen Sie sich ein! 10 Die Bewirtschaftungsplanung für das Swistgebiet 12 Das Swistgebiet 14 Die Fließgewässer und Seen 16 Zustand der Gewässer 17 Die Wasserqualität • Saprobie – die biologische Gewässergüte • Plankton, Algen, Wasserpfl anzen • Pfl anzenschutzmittel • Metalle • Sonstige Schadstoffe 22 Der ökologische Zustand der Gewässer • Die allgemeine Degradation • Die Fischfauna 24 Belastungsursachen und Maßnahmen 28 Das Grundwasser 31 Mit gutem Beispiel voran 33 Ansprechpartner 34 Impressum PE_ERF_1400.indd 3 14.12.2008, 15:34 Carpediem PE_ERF_1400.indd 4 14.12.2008, 15:34 5 Liebe Bürgerinnen und Bürger, in Nordrhein-Westfalen haben wir zwar eine gute Wasser- qualität, doch unsere Gewässer bieten oft noch nicht den ökologisch notwendigen Lebensraum, um auch Lebens- adern der Natur zu sein. Wir wollen deshalb die Gewässer- ökologie in Nordrhein-Westfalen verbessern und orientieren uns dabei an den europäisch vereinbarten Qualitätszielen. Wir möchten den Zustand der nordrhein-westfälischen Gewässer verbessern im Interesse der Artenvielfalt, des Hochwasserschutzes und der regionalen Entwicklung. Dieses ambitionierte Ziel können wir nur in Kooperation mit den Kommunen, den Wasserverbänden, der Land- und Forstwirtschaft, der Industrie, den Naturschutzverbänden und natürlich nur gemeinsam mit den Bürgerinnen und Bürgern erreichen. Wir werden jetzt überall im Land mit zahlreichen Maßnah- men beginnen und voraussichtlich bis 2027 die Ziele errei- chen. -
Pleistocene to Recent Tectonics in the Rhenish Massif (Germany)
Netherlands Journal of Geosciences / Geologie en Mijnbouw 81 (2): 217-221 (2002) Pleistocene to Recent tectonics in the Rhenish Massif (Germany) W.Meyer^&J.Stets1 1 Geologisches Institut der Universitat Bonn, Nussallee 8, D-53115 Bonn, Germany 2 corresponding author; e-mail: [email protected] Manuscript received: August 2000; accepted: January 2002 Abstract Uplift of the Rhenish Massif can be demonstrated by means of the stream-made river terrace system that accompanies the Rhine river and its tributaries along their way through or within this part of the Variscan fold and thrust belt. The height dif ference between a former valley floor, especially that of the Younger 'Hauptterrasse' (Main Terrace), and the recent one allows to quantify the uplift by the amount of downcutting erosion. The uplift velocity increased just after the BRUNHES / MATUYAMA boundary, i.e. about 0.8 Ma B.R Since that time, a domal uplift of more than 250 m is documented in the eastern Hunsriick and in the south-eastern Eifel.The area of this maximum height anomaly is situated just between the East- and West-Eifel Quaternary volcanic districts. Thus, causal connections are supposed. The domal uplift is affected by normal faulting partly inherited since Tertiary rifting. Keywords: Rhenish Massif, Pleistocene, fluvial terrace system, downcutting erosion, neotectonics, domal uplift, Eifel, Huns riick, Rhine, Mosel, Lower Rhine Basin, Neuwied Basin Introduction tionary stages of the ancient river system. Differences exist between the Pliocene as well as the Early Pleis Previous research work revealed uplift in the Rhenish tocene original valley floors and those of Middle and Massif during the Cenozoic (for detailed information Late Pleistocene to Recent age. -
DWA Water Quality Model - an Instrument to Support Water Management Planning Functions with the Example of the Erft River
DWA Water Quality Model - an instrument to support water management planning functions with the example of the Erft river E. Christoffels Erftverband, Bergheim, Germany Abstract The DWA water quality model can be used for a wide range of water management planning activities. Fields of application extend from data and system analysis, to the analysis of alternatives in water pollution control planning, to the implementation of alarm plans. The example of the Erft river is used to present the results of water quality simulations with a view to assessing current conditions and forecasting the future development of water quality. Keywords: Erft, water quality model, plausibility check, water temperature, oxygen, ammonium, sumpwater, combined sewer overflow, riparian vegetation. 1 Introduction In the course of progressive improvement of surface water quality, point sources are losing their significance as the dominant influence. Today water quality is affected to a high degree by many other important factors. Apart from external impacts, effects of internal processes within the water body are receiving greater attention than in the past. Predicting the impact of various water uses and the effects of measures to improve water quality is challenging because of the large number of relevant factors within a complex system. Despite this complexity, practical instruments are needed to predict the impact of human activities, to clearly demonstrate the need for measures based on existing water quality standards, and to foresee the outcome of such measures. The DWA water quality model is an efficient instrument to support water management planning functions. It serves as a simulation model for creeks, brooks and rivers which is available as a software tool. -
Combining Ecohydrological Catchment Modelling and Water Quality Monitoring to Assess Surface Water Pollution in the Swist River Basin
EGU2020-19842 https://doi.org/10.5194/egusphere-egu2020-19842 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Combining Ecohydrological Catchment Modelling and Water Quality Monitoring to Assess Surface Water Pollution in the Swist River Basin Alexander Ahring1,3, Marvin Kothe1, Christian Gattke1, Ekkehard Christoffels2, and Bernd Diekkrüger3 1Erftverband, River Basin Management, Germany ([email protected]) 2IBC Ingenieurtechnische Beratung Christoffels, Vettweiß, Germany 3Department of Geography, University of Bonn, Germany Inland surface waters like rivers, streams, lakes and reservoirs are subject to anthropogenic pollutant emissions from various sources. These emissions can have severe negative impacts on surface water ecology, as well as human health when surface waters are used for recreational activities, irrigation of cropland or drinking water production. In order to protect aquatic ecosystems and freshwater resources, the European Water Framework Directive (WFD) sets specific quality requirements which the EU member states must meet until 2027 for every water body. Implementing effective measures and emission control strategies requires knowledge about the important emission pathways in a given river basin. However, due to the abundance of pollution sources and the heterogeneity of emission pathways in time and space, it is not feasible to gain this knowledge via water quality monitoring alone. In our study, we aim to combine SWAT ecohydrological modelling and long term water quality monitoring data to establish a spatially differentiated nitrogen emission inventory on the sub-catchment scale. SWAT (short for Soil and Water Assessment Tool) is a semi-distributed, dynamic and process-driven watershed model capable of simulating long term hydrology as well as nutrient fluxes on a daily time step. -
Das Vorgebirge. Ein Beitrag Zur Rheinischen Landeskunde
Das Vorgebirge. Ein Beitrag zur rheinischen Landeskunde. Von Clotilde Ellscheid. Mit 6 Karten und Tafel IX u. X. Inhaltsbericht. Einführung: Lage, Abgrenzung und äußere Erscheinung Seite des G e b i e t e s ...............................................................................199—204 I. Teil: Die Natur der Landschaft........................................... 205—242 1 . Geologischer Bau, Oberflächenformen u. Boden 205 2. Das K lim a .......................................................... 222 8 . Die hydrologischen V e rh ä ltn isse.......... 228 4. Das Landschaftsbild im Wandel der Zeiten . 236 II. Teil: Die wirtschaftlichen V erhältnisse.......................... 242—276 1 . Die Nutzbarmachung der natürlichen Wasser vorräte .......................................................................... 242 2. Die W a ld w irtsch a ft..................................... 245 3. Die landwirtschaftlichen Verhältnisse. 248 a) Die Landwirtschaft am Osthang des Vor gebirges zwischen Bonn und Frechen . 248 b) Die Landwirtschaft auf der Hochfläche . 257 4. Die Industrie............................................................... 262 a) Der Eisenerzabbau als ausgestorbener Wirt schaftszweig. — Die Gewinnung und Ver wertung der B rau n k oh le.............. 262 b) Die Ausnutzung der Ton- und Sandlager 270 5. Der umgestaltende Einfluß der Industrie auf das Landschaftsbild.............................. 275 III. Teil: Die Verkehrswege........................................................ 276—280 IV. Teil: Zur Siedlungsgeographie -
Mittleres Ahrtal"1 Aus Naturkundlicher Sicht, Dargestellt Am Beispiel Des Naturschutzgebietes ,,Ahrschleife Bei Altenahr"
BEITRÄGE ZUR LANDESPFLEGE IN RHEINLAND-PFALZ 17 Das Naturschutzgebiet „Ahrschleife bei Altenahr" ( einschließlich angrenzender schutzwürdiger Bereiche) Fauna, Flora, Geologie und Landespflegeaspekte TeilII von WOLFGANGBÜCHS unter Mitarbeit von J. BECKER, T. BLICK, H.-J. HOFFMANN, J. C. KÜHLE, R. REMANE, V. SLEMBROUCK & W. WENDLING Herausgegeben vom Landesamt fürUmweltschutz und GewerbeaufsichtRheinland-Pfalz Oppenheim 2003 Beiträge Landespflege Rheinland-Pfalz 17 Seite 1-376 Oppenheim 2003 Verkauf nur durch das Landesamt für Umweltschutz und Gewerbeaufsicht Rheinland-Pfalz, Amtsgerichtsplatz 1, 55276 Oppenheim (zum Preise von 10,-Euro zzgl. Porto und Verpackungskosten) Einband: Hintergrund: Kartenaufnahme(ca. 1809) von Tranchot und von Von Müffling Abbildungen/Fotosund Bildautoren: oben links: Tunnel bei Altenahr. Lithographie von PONSART (1839). Repro aus Sammlung I. Görtz, Altenahr. oben rechts: Breite Lay,1989, Dr. Dr. Wolfgang Büchs (Braunschweig) unten links: Jugendherberge im Langfigtal,1989, Dr. Dr. Wolfgang Büchs (Braunschweig) unten Mitte: Hasenglöckchen (Hyacinthoides non-scripta), F. J.Fuchs,Mayschoß unten rechts: Raubwanzen-Art (Rhinocoris iracundus), Prof. Dr. E. Wachmann (Berlin) Einbandgestaltung: SOMMERDruck und Verlag Herausgeber: Landesamt fürUmweltschutz und Gewerbeaufsicht Rheinland-Pfalz,Am tsgerichtsplatz 1, 55276 Oppenheim Schriftleitung: Dr. Dr. Wolfgang Büchs (Braunschweig) Klaus Groh (Hackenheim) Dr. ManfredNiehuis (Albersweiler) Dr. Dieter Rühl (Oppenheim) Für die einzelnen Beiträge zeichnendie jeweiligen (Ko)autor(inn)en -
Die Ahr – Ein Echtes Kernstück Der Eifel
Die Ahr – ein echtes Kernstück der Eifel Dr. Bruno P. Kremer er Blick auf eine hydrographische Karte des tigen Hunsrück legt der nicht weniger enge DRheinlandes, in der nur das weit verzweigte und vielfach gewundene Talzug der Mosel fest. Gewässernetz dargestellt ist, überzeugt sofort Auch der Nachvollzug der Westgrenze gelingt davon, dass die naturräumliche Gliederung zumindest im Südwesten mit einem Talverlauf, in über- und untergeordnete Landschaftsteile nämlich von Our und vor allem Sauer: Deren nach den Eigenheiten des Reliefs sowie vor Tal ist hier gleichzeitig die politische Grenze allem nach Lage und Verlauf der Fließgewäs- zum Nachbarland Luxemburg. Im Nordwesten ser erfolgt. Bei der Eifel lässt sich dies gerade- ist die Abgrenzung der Eifel zu den westlich zu lehrbuchreif klar aufzeigen: Das untere und anschließenden Ardennen bzw. zu Belgien tief eingeschnittene Mittelrhein-Engtal zwi- in der Geländegestalt dagegen unscharf. Die schen Andernach und Bonn, im Rheinischen Nordgrenze ist wiederum eindeutig anzugeben: Schiefergebirge ohnehin die auffälligste Struk- Sie zeichnet sich – ausnahmsweise ganz ohne turachse, markiert klar und eindeutig die Ost- ein hilfreiches Flusstal – lediglich als markante grenze der Eifel. Ihre südliche Begrenzung zum Geländestufe zu den weiten Ebenen des nord- landschaftlich und geologisch völlig andersar- westdeutschen Tieflandes ab. Heimatjahrbuch Kreis Ahrweiler 2013 u 117 Das Gewässernetz der Eifel stellt sich gänz- lich anders dar als in den benachbarten Mittelgebirgsteilen. Ausschnitt aus: Strub J., Vonderstraß, I., Leibundgut, Ch., Kern, F.-J.: Orohydrogra- phie (Atlastafel 1.1), in: BMU (Hrsg.): Hydrologischer Atlas von Deutschland, 3. Lieferung 2003. Mit freundlicher Genehmi- gung des Bundesamtes für Gewässerkunde (Koblenz) Die hydrographische Karte zeigt ferner, dass verwendet man unter anderem die Flussord- zahlreiche Fließgewässer den nach seinem Ge- nungszahl. -
A Viking-Age Settlement in the Hinterland of Hedeby Tobias Schade
L. Holmquist, S. Kalmring & C. Hedenstierna-Jonson (eds.), New Aspects on Viking-age Urbanism, c. 750-1100 AD. Proceedings of the International Symposium at the Swedish History Museum, April 17-20th 2013. Theses and Papers in Archaeology B THESES AND PAPERS IN ARCHAEOLOGY B New Aspects on Viking-age Urbanism, c. 750-1100 AD. Proceedings of the International Symposium at the Swedish History Museum, April 17–20th 2013 Lena Holmquist, Sven Kalmring & Charlotte Hedenstierna-Jonson (eds.) Contents Introduction Sigtuna: royal site and Christian town and the Lena Holmquist, Sven Kalmring & regional perspective, c. 980-1100 Charlotte Hedenstierna-Jonson.....................................4 Sten Tesch................................................................107 Sigtuna and excavations at the Urmakaren Early northern towns as special economic and Trädgårdsmästaren sites zones Jonas Ros.................................................................133 Sven Kalmring............................................................7 No Kingdom without a town. Anund Olofs- Spaces and places of the urban settlement of son’s policy for national independence and its Birka materiality Charlotte Hedenstierna-Jonson...................................16 Rune Edberg............................................................145 Birka’s defence works and harbour - linking The Schleswig waterfront - a place of major one recently ended and one newly begun significance for the emergence of the town? research project Felix Rösch..........................................................153 -
Rapid Attribution of Heavy Rainfall Events Leading to the Severe Flooding in Western Europe During July 2021
Rapid attribution of heavy rainfall events leading to the severe flooding in Western Europe during July 2021 Contributors Frank Kreienkamp1, Sjoukje Y. Philip2, Jordis S. Tradowsky1,4, Sarah F. Kew2, Philip Lorenz1, Julie Arrighi7,8,9, Alexandre Belleflamme16, Thomas Bettmann18, Steven Caluwaerts13,19, Steven C. Chan14, Andrew Ciavarella22, Lesley De Cruz13, Hylke de Vries2, Norbert Demuth18, Andrew Ferrone17, Erich M. Fischer6, Hayley J. Fowler14, Klaus Goergen16, Dorothy Heinrich7, Yvonne Henrichs18, Geert Lenderink2, Frank Kaspar10, Enno Nilson15, Friederike E L Otto11, Francesco Ragone13,20, Sonia I. Seneviratne6, Roop K. Singh7, Amalie Skålevåg, Piet Termonia13,19, Lisa Thalheimer11, Maarten van Aalst7,8,21, Joris Van den Bergh13, Hans Van de Vyver13, Stéphane Vannitsem13, Geert Jan van Oldenborgh2,3, Bert Van Schaeybroeck13, Robert Vautard5, Demi Vonk8, Niko Wanders12 1 - Deutscher Wetterdienst (DWD), Regionales Klimabüro Potsdam, Potsdam, Germany; 2 - Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands; 3 - Atmospheric, Oceanic and Planetary Physics, University of Oxford, UK; 4 - Bodeker Scientific, Alexandra, New Zealand; 5 - Institut Pierre-Simon Laplace, CNRS, Paris, France; 6 - Institute for Atmospheric and Climate Science, Department of Environmental Systems Science, ETH Zurich, Zurich, Switzerland; 7 - Red Cross Red Crescent Climate Centre, The Hague, the Netherlands; 8 - Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, the Netherlands; 9 - Global Disaster -
83Rd Division Radio News, Germany, Vol IV #32, March 2, 1945
VOLUME VI NO. 32 - 2 MARCH 1945 CEPMANY: AMERICAN INFAiMTh.Yiv.EN OF THE U. S. 83RD DIVISION HAVE REACHED THE WESTERN BANK OF THE RHINE RIVER NEAR THE CITY OF NEUSS. MAJOR GENERAL MACON'S MEN ARE DIGGING IN ALONG THE BANK OF THE GREAT RIVER WHILE ARiflORED UNITS LOB SHELLS ACROSS THE RHINE AT 'GERMAN POSITIONS ON THE FAR SIDE.. THE. YANKS FOUGHT THEIR WAY TO THE RHINE AFTER PUSHING UP ALONG THE ERFT CANAL. TROOPS OF THE SAME DIVISION ARE ALSO FIGHTING IN THE CITY OF NEUSS. ' THIS STARTLING ANNOUNCEMENT WAS MADE AFTER THE SECURITY BLACKOUT COVERING THE MOVEMENTS OF THE AMERICAN NINTH ARMY WAS LIFTED. IT' WAS ALSO ENOUNCED THAT AM• EBIC AN-TROOPS HAVE ENTERED THE BIG .CITY OF KREFELD NORTHWEST OF DUSSELDORF AND THAT OTHER AMERICAN FORCES HAVE TAKEN THE CITY. OF VENLO CN THE EASTERN B,NK OF THE RIVER MAAS. THE AMERICANS, BY CAPTURING VENLO, HAVE OUTHANKED THE WHOLE GEKMAN FRONT FACING THE BRITISH SECOND ARMY, GENERAL SIMPSON'S MEN RACED ANYWHERE FROM 6 TO 15 MILES IN THE I IGHTIN& YESTERDAY AND THEY BAGGED ANOTHER 3000 PRISONERS. THE BIG TOWN OF MUN CHEN GLAD BACK HAS FALLEN TO NINTH ARMY TROTS AND THERE ARE SIGNS THAT THE GERMANS ARE BEGINNING TO PULL THEIR VEHICLES 'ACROSS THE RHINE AT THE BRIDGES NEAR KREFELD AND NORTH OF COLOGNE. TODAY AJMEKICAN t LGHTER BOMBERS HAVE BEEN ATTACKING GERVIAN TRANSPORT HEADLNG FOR THE RHINE RIVER uRuSSINGS. AMEILCAN FIRST ARteY TROOPS HaVE NOW LINKED' UP THEIR BRIDGEHEADS OVER THE ERFT RIVER AND HOLD A 9 MILE STRETCH ON THE FAR SIDE OF THE RIVER. -
Introduction of an Experimental Terrestrial Forecasting
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 26 October 2018 doi:10.20944/preprints201810.0625.v1 1 Article 2 Introduction of an experimental terrestrial 3 forecasting/monitoring system at regional to 4 continental scales based on the Terrestrial System 5 Modeling Platform (v1.1.0) 6 Stefan Kollet1,2,*, Fabian Gasper1,2,**, Slavko Brdar3,2, Klaus Goergen1,2, Harrie-Jan 7 Hendricks-Franssen1,2, Jessica Keune1,4,2,***, Wolfgang Kurtz1,2,****, Volker Küll4, Florian 8 Pappenberger5, Stefan Poll4, Silke Trömel4, Prabhakar Shrestha4, Clemens Simmer4,2, and Mauro 9 Sulis4,***** 10 1 Agrosphere Inst., IBG-3, Inst. of Bio-Geosciences, Forschungszentrum Jülich GmbH, Jülich, Germany 11 2 Centre for High-Performance Scientific Computing, Geoverbund ABC/J, Germany 12 3 Jülich Supercomputing Centre, Forschungszentrum Jülich GmbH, Jülich, Germany 13 4 Meteorological Institute, Bonn University, Germany 14 5 European Centre for Medium-Range Weather Forecasts 15 * Correspondence: [email protected]; Tel.: +49-2461-61-9593 16 ** Now at CISS TDI GmbH, Sinzig, Germany 17 *** Now at the Department of Forest and Water Management, Ghent University, Belgium 18 **** Now at Environmental Computing Group, Leibnitz Supercomputing Centre, Germany 19 ***** Now at the Department of Environmental Research and Innovation, Luxembourg Institute of 20 Technology, Luxembourg 21 22 23 Abstract: Operational weather and also flood forecasting has been performed successfully for 24 decades and is of great socioeconomic importance. Up to now, forecast products focus on 25 atmospheric variables, such as precipitation, air temperature and, in hydrology, on river discharge. 26 Considering the full terrestrial system from groundwater across the land surface into the 27 atmosphere, a number of important hydrologic variables are missing especially with regard to the 28 shallow and deeper subsurface (e.g.