TY - JOUR A1 - Herbst, Uta A1 - Franzke, Jochen A1 - Wicke, Markus A1 - Weber, Susann A1 - Dobrigkeit, Philipp A1 - Mikulcová, Anna A1 - Wanagas, Torsten A1 - Sim, Chu-Won A1 - Klosa, Sven A1 - Geißler-Grünberg, Anke A1 - Winter, Jean-Pierre A1 - Koch, Helvi A1 - Henrich, Lutz A1 - König, Julia A1 - Stab, Uwe A1 - Schmidt, Sina A1 - Knuth, Alexander T1 - Portal alumni T2 - Das Ehemaligen-Magazin der Universität Potsdam N2 - Die Beliebtheit von Medienberufen ist ungebrochen. Das zeigt sich unter anderem an der Zahl der Studieninteressierten. So haben sich allein in diesem Jahr mehr als 1 500 junge Leute auf einen der 44 Plätze für den Studiengang Medienwissenschaft an der Universität Potsdam beworben. Nach ihrem erfolgreichen Abschluss allerdings konkurrieren die Absolventen am Arbeitsmarkt mit Tausenden Abgängern anderer Hochschulen aus Film-, Medien- und Kommunikationsstudiengängen. Das sind allein in der Region Berlin-Brandenburg jährlich etwa 1 500. Doch nach jahrzehntelangem Boom der Medienbranche hat sich der Arbeitsmarkt im vergangenen Jahrzehnt drastisch verändert. Konjunkturkrise, Kursrückgänge und rückläufige Werbeinvestitionen schwächten die Medien deutlich. Es folgten daraus schlechte Gewinnergebnisse, Einsparungen und Personalreduzierung, insbesondere bei den Printmedien. Die Insolvenz der Frankfurter Rundschau oder die Einstellung der Financial Times Deutschland sind nur zwei eklatante Beispiele. Auf der anderen Seite boomt der dynamische Online-Markt aufgrund des veränderten Nutzerverhaltens insbesondere der jungen Generation, die ihre Informationen zunehmend aus Internet, Apps und sozialen Netzwerken gewinnen. Die Berufsaussichten für all Jene, die „Irgendwas mit Medien“ studieren wollen sind zwar aufgrund des Arbeitsmarktes schwieriger geworden, sie sind aber dennoch vielfältig. Guter Journalismus wird weiterhin benötigt und auch Öffentlichkeitsarbeiter sind gefragt. Darüber hinaus stehen Absolveninspiriert von den Fernsehbildern, als Tausende Flüchtlinge herzlich in München empfangen wurden, kam unserem Kollegen Eric Makswitat die Idee, sich auch auf lokaler Ebene für die hier ankommenden Flüchtlinge zu engagieren. Der Doktorand in der Politikwissenschaft sammelt über das Internet Bücher für Flüchtlinge und gibt sie dann direkt in den Flüchtlingsunterkünften ab. Eric Makswitat ist einer von Vielen, die derzeit einen wichtigen Beitrag zur Bewältigung der Herausforderungen des Flüchtlingszustroms nach Deutschland leisten. Die engagierten Helfer sind „ein Beweis dafür, wie weit die Selbstorganisationskräfte der organisierten Bürgerschaft in unserer Zivilgesellschaft mittlerweile entwickelt sind“, meint dazu der Verwaltungswissenschaftler Jochen Franzke. Unser Kollege Eric ist auch in anderer Hinsicht beispielgebend. Er ist einer von rund achtzig Prozent aller ehemaligen Studierenden, die nach dem Studienabschluss in der Region bleiben, wie eine kürzlich an der Uni veröffentlichte Studie zum Verbleib unserer Absolventinnen und Absolventen ermittelt hat. Unsere Alumni steigen ein in Berufsfeldern der Politik, Wirtschaft und Gesellschaft, sie gründen Firmen und sie engagieren sich beruflich, privat oder gesellschaftlich. Viele davon in Potsdam. Wenn die Universität Potsdam im nächsten Jahr ihr 25-jähriges Jubiläum in und mit der Stadt Potsdam feiern wird und mit Stolz auf hervorragende Leistungen aus Lehre und Forschung verweist, dann ist dies nicht zuletzt den Absolventinnen und Absolventen zu verdanken, die als hochqualifizierte Fachkräfte neueste wissenschaftliche Erkenntnisse in die Praxis überführen. Portal alumni ist deshalb in diesem Jahr hier, zu Hause in Potsdam geblieben. Wir haben Absolventen der Universität Potsdam gesucht, die heute in unterschiedlichen beruflichen und gesellschaftlichen Kontexten in der Region aktiv sind und sich engagieren. T3 - Portal alumni : das Ehemaligen-Magazin der Universität Potsdam - 12/2015 Y1 - 2015 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-445297 SN - 1613-2343 IS - 12 ER - TY - JOUR A1 - Schmidt, Martin A1 - Kaspar, Rüdiger A1 - Richter, Torsten ED - Kummer, Volker T1 - Ergebnisse der Tagung des BFA Mykologie (NABU) 2006 in Linowsee bei Rheinsberg/Brandenburg Y1 - 2008 ER - TY - JOUR A1 - Wende, Wolfgang A1 - Wojtkiewicz, Wera A1 - Marschall, Ilke A1 - Heiland, Stefan A1 - Lipp, Torsten A1 - Reinke, Markus A1 - Schaal, Peter A1 - Schmidt, Catrin T1 - Putting the plan into practice implementation of proposals for measures of local landscape plans JF - Landscape research N2 - The knowledge of the effectiveness of local landscape planning in Germany is in the main limited to particular cases and derives mostly from qualitative single case studies. This applies especially to the implementation of measures defined by landscape plans. To fill that gap, the paper focuses on the implementation of those measures. Furthermore, it discusses the factors and framework conditions which are crucial for this implementation. The potential factors and conditions of influence were derived from theory and compiled in 20 investigation hypotheses. In order to gain information on the execution of the measures, 28 randomly selected plans were first analysed, then interviews were carried out with administration representatives. It can be stated that landscape planning has positively influenced the development of nature and landscape in the investigated municipalities. A considerable number of measures had been implemented, although landscape planning as a supply-side instrument proposes generally a very large number of measures. Factors with a positive effect on the implementation of landscape planning measures are pointed out. KW - Landscape planning KW - nature conservation KW - effectiveness KW - quantitative research KW - Germany KW - municipality Y1 - 2012 U6 - https://doi.org/10.1080/01426397.2011.592575 SN - 0142-6397 VL - 37 IS - 4 SP - 483 EP - 500 PB - Routledge, Taylor & Francis Group CY - Abingdon ER - TY - JOUR A1 - Arnison, Paul G. A1 - Bibb, Mervyn J. A1 - Bierbaum, Gabriele A1 - Bowers, Albert A. A1 - Bugni, Tim S. A1 - Bulaj, Grzegorz A1 - Camarero, Julio A. A1 - Campopiano, Dominic J. A1 - Challis, Gregory L. A1 - Clardy, Jon A1 - Cotter, Paul D. A1 - Craik, David J. A1 - Dawson, Michael A1 - Dittmann-Thünemann, Elke A1 - Donadio, Stefano A1 - Dorrestein, Pieter C. A1 - Entian, Karl-Dieter A1 - Fischbach, Michael A. A1 - Garavelli, John S. A1 - Goeransson, Ulf A1 - Gruber, Christian W. A1 - Haft, Daniel H. A1 - Hemscheidt, Thomas K. A1 - Hertweck, Christian A1 - Hill, Colin A1 - Horswill, Alexander R. A1 - Jaspars, Marcel A1 - Kelly, Wendy L. A1 - Klinman, Judith P. A1 - Kuipers, Oscar P. A1 - Link, A. James A1 - Liu, Wen A1 - Marahiel, Mohamed A. A1 - Mitchell, Douglas A. A1 - Moll, Gert N. A1 - Moore, Bradley S. A1 - Mueller, Rolf A1 - Nair, Satish K. A1 - Nes, Ingolf F. A1 - Norris, Gillian E. A1 - Olivera, Baldomero M. A1 - Onaka, Hiroyasu A1 - Patchett, Mark L. A1 - Piel, Jörn A1 - Reaney, Martin J. T. A1 - Rebuffat, Sylvie A1 - Ross, R. Paul A1 - Sahl, Hans-Georg A1 - Schmidt, Eric W. A1 - Selsted, Michael E. A1 - Severinov, Konstantin A1 - Shen, Ben A1 - Sivonen, Kaarina A1 - Smith, Leif A1 - Stein, Torsten A1 - Suessmuth, Roderich D. A1 - Tagg, John R. A1 - Tang, Gong-Li A1 - Truman, Andrew W. A1 - Vederas, John C. A1 - Walsh, Christopher T. A1 - Walton, Jonathan D. A1 - Wenzel, Silke C. A1 - Willey, Joanne M. A1 - van der Donk, Wilfred A. T1 - Ribosomally synthesized and post-translationally modified peptide natural products overview and recommendations for a universal nomenclature JF - Natural product reports : a journal of current developments in bio-organic chemistry N2 - This review presents recommended nomenclature for the biosynthesis of ribosomally synthesized and post-translationally modified peptides (RiPPs), a rapidly growing class of natural products. The current knowledge regarding the biosynthesis of the >20 distinct compound classes is also reviewed, and commonalities are discussed. Y1 - 2013 U6 - https://doi.org/10.1039/c2np20085f SN - 0265-0568 VL - 30 IS - 1 SP - 108 EP - 160 PB - Royal Society of Chemistry CY - Cambridge ER - TY - GEN A1 - Ramezani Ziarani, Maryam A1 - Bookhagen, Bodo A1 - Schmidt, Torsten A1 - Wickert, Jens A1 - de la Torre, Alejandro A1 - Hierro, Rodrigo T1 - Using Convective Available Potential Energy (CAPE) and Dew-Point Temperature to Characterize Rainfall-Extreme Events in the South-Central Andes T2 - Postprints der Universität Potsdam Mathematisch-Naturwissenschaftliche Reihe N2 - The interactions between atmosphere and steep topography in the eastern south–central Andes result in complex relations with inhomogenous rainfall distributions. The atmospheric conditions leading to deep convection and extreme rainfall and their spatial patterns—both at the valley and mountain-belt scales—are not well understood. In this study, we aim to identify the dominant atmospheric conditions and their spatial variability by analyzing the convective available potential energy (CAPE) and dew-point temperature (Td). We explain the crucial effect of temperature on extreme rainfall generation along the steep climatic and topographic gradients in the NW Argentine Andes stretching from the low-elevation eastern foreland to the high-elevation central Andean Plateau in the west. Our analysis relies on version 2.0 of the ECMWF’s (European Centre for Medium-RangeWeather Forecasts) Re-Analysis (ERA-interim) data and TRMM (Tropical Rainfall Measuring Mission) data. We make the following key observations: First, we observe distinctive gradients along and across strike of the Andes in dew-point temperature and CAPE that both control rainfall distributions. Second, we identify a nonlinear correlation between rainfall and a combination of dew-point temperature and CAPE through a multivariable regression analysis. The correlation changes in space along the climatic and topographic gradients and helps to explain controlling factors for extreme-rainfall generation. Third, we observe more contribution (or higher importance) of Td in the tropical low-elevation foreland and intermediate-elevation areas as compared to the high-elevation central Andean Plateau for 90th percentile rainfall. In contrast, we observe a higher contribution of CAPE in the intermediate-elevation area between low and high elevation, especially in the transition zone between the tropical and subtropical areas for the 90th percentile rainfall. Fourth, we find that the parameters of the multivariable regression using CAPE and Td can explain rainfall with higher statistical significance for the 90th percentile compared to lower rainfall percentiles. Based on our results, the spatial pattern of rainfall-extreme events during the past ∼16 years can be described by a combination of dew-point temperature and CAPE in the south–central Andes. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 771 KW - eastern south–central Andes KW - extreme rainfall KW - deep convection KW - convective available potential energy KW - dew-point temperature Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-438865 SN - 1866-8372 IS - 771 ER - TY - JOUR A1 - Ramezani Ziarani, Maryam A1 - Bookhagen, Bodo A1 - Schmidt, Torsten A1 - Wickert, Jens A1 - de la Torre, Alejandro A1 - Hierro, Rodrigo T1 - Using Convective Available Potential Energy (CAPE) and Dew-Point Temperature to Characterize Rainfall-Extreme Events in the South-Central Andes JF - Atmosphere N2 - The interactions between atmosphere and steep topography in the eastern south–central Andes result in complex relations with inhomogenous rainfall distributions. The atmospheric conditions leading to deep convection and extreme rainfall and their spatial patterns—both at the valley and mountain-belt scales—are not well understood. In this study, we aim to identify the dominant atmospheric conditions and their spatial variability by analyzing the convective available potential energy (CAPE) and dew-point temperature (Td). We explain the crucial effect of temperature on extreme rainfall generation along the steep climatic and topographic gradients in the NW Argentine Andes stretching from the low-elevation eastern foreland to the high-elevation central Andean Plateau in the west. Our analysis relies on version 2.0 of the ECMWF’s (European Centre for Medium-RangeWeather Forecasts) Re-Analysis (ERA-interim) data and TRMM (Tropical Rainfall Measuring Mission) data. We make the following key observations: First, we observe distinctive gradients along and across strike of the Andes in dew-point temperature and CAPE that both control rainfall distributions. Second, we identify a nonlinear correlation between rainfall and a combination of dew-point temperature and CAPE through a multivariable regression analysis. The correlation changes in space along the climatic and topographic gradients and helps to explain controlling factors for extreme-rainfall generation. Third, we observe more contribution (or higher importance) of Td in the tropical low-elevation foreland and intermediate-elevation areas as compared to the high-elevation central Andean Plateau for 90th percentile rainfall. In contrast, we observe a higher contribution of CAPE in the intermediate-elevation area between low and high elevation, especially in the transition zone between the tropical and subtropical areas for the 90th percentile rainfall. Fourth, we find that the parameters of the multivariable regression using CAPE and Td can explain rainfall with higher statistical significance for the 90th percentile compared to lower rainfall percentiles. Based on our results, the spatial pattern of rainfall-extreme events during the past ∼16 years can be described by a combination of dew-point temperature and CAPE in the south–central Andes. KW - eastern south–central Andes KW - extreme rainfall KW - deep convection KW - convective available potential energy KW - dew-point temperature Y1 - 2019 U6 - https://doi.org/10.3390/atmos10070379 SN - 2073-4433 VL - 10 IS - 7 PB - MDPI CY - Basel ER - TY - JOUR A1 - Ramezani Ziarani, Maryam A1 - Bookhagen, Bodo A1 - Schmidt, Torsten A1 - Wickert, Jens A1 - de la Torre, Alejandro A1 - Deng, Zhiguo A1 - Calori, Andrea T1 - A model for the relationship between rainfall, GNSS-derived integrated water vapour, and CAPE in the eastern central Andes JF - Remote Sensing N2 - Atmospheric water vapour content is a key variable that controls the development of deep convective storms and rainfall extremes over the central Andes. Direct measurements of water vapour are challenging; however, recent developments in microwave processing allow the use of phase delays from L-band radar to measure the water vapour content throughout the atmosphere: Global Navigation Satellite System (GNSS)-based integrated water vapour (IWV) monitoring shows promising results to measure vertically integrated water vapour at high temporal resolutions. Previous works also identified convective available potential energy (CAPE) as a key climatic variable for the formation of deep convective storms and rainfall in the central Andes. Our analysis relies on GNSS data from the Argentine Continuous Satellite Monitoring Network, Red Argentina de Monitoreo Satelital Continuo (RAMSAC) network from 1999 to 2013. CAPE is derived from version 2.0 of the ECMWF’s (European Centre for Medium-Range Weather Forecasts) Re-Analysis (ERA-interim) and rainfall from the TRMM (Tropical Rainfall Measuring Mission) product. In this study, we first analyse the rainfall characteristics of two GNSS-IWV stations by comparing their complementary cumulative distribution function (CCDF). Second, we separately derive the relation between rainfall vs. CAPE and GNSS-IWV. Based on our distribution fitting analysis, we observe an exponential relation of rainfall to GNSS-IWV. In contrast, we report a power-law relationship between the daily mean value of rainfall and CAPE at the GNSS-IWV station locations in the eastern central Andes that is close to the theoretical relationship based on parcel theory. Third, we generate a joint regression model through a multivariable regression analysis using CAPE and GNSS-IWV to explain the contribution of both variables in the presence of each other to extreme rainfall during the austral summer season. We found that rainfall can be characterised with a higher statistical significance for higher rainfall quantiles, e.g., the 0.9 quantile based on goodness-of-fit criterion for quantile regression. We observed different contributions of CAPE and GNSS-IWV to rainfall for each station for the 0.9 quantile. Fourth, we identify the temporal relation between extreme rainfall (the 90th, 95th, and 99th percentiles) and both GNSS-IWV and CAPE at 6 h time steps. We observed an increase before the rainfall event and at the time of peak rainfall—both for GNSS-integrated water vapour and CAPE. We show higher values of CAPE and GNSS-IWV for higher rainfall percentiles (99th and 95th percentiles) compared to the 90th percentile at a 6-h temporal scale. Based on our correlation analyses and the dynamics of the time series, we show that both GNSS-IWV and CAPE had comparable magnitudes, and we argue to consider both climatic variables when investigating their effect on rainfall extremes. KW - Global Navigation Satellite System (GNSS) KW - GNSS-integrated water vapour KW - convective available potential energy (CAPE) KW - extreme rainfall KW - TRMM Y1 - 2021 U6 - https://doi.org/10.3390/rs13183788 SN - 2072-4292 VL - 13 IS - 18 PB - MDPI CY - Basel ER - TY - JOUR A1 - Hierro, Rodrigo A1 - Burgos Fonseca, Y. A1 - Ramezani Ziarani, Maryam A1 - Llamedo, P. A1 - Schmidt, Torsten A1 - de la Torre, Alejandro A1 - Alexander, P. T1 - On the behavior of rainfall maxima at the eastern Andes JF - Atmospheric Research N2 - In this study, we detect high percentile rainfall events in the eastern central Andes, based on Tropical Rainfall Measuring Mission (TRMM) with a spatial resolution of 0.25 × 0.25°, a temporal resolution of 3 h, and for the duration from 2001 to 2018. We identify three areas with high mean accumulated rainfall and analyze their atmospheric behaviour and rainfall characteristics with specific focus on extreme events. Extreme events are defined by events above the 95th percentile of their daily mean accumulated rainfall. Austral summer (DJF) is the period of the year presenting the most frequent extreme events over these three regions. Daily statistics show that the spatial maxima, as well as their associated extreme events, are produced during the night. For the considered period, ERA-Interim reanalysis data, provided by the European Centre for Medium-Range Weather Forecasts (ECMWF) with 0.75° x0.75° spatial and 6-hourly temporal resolutions, were used for the analysis of the meso- and synoptic-scale atmospheric patterns. Night- and day-time differences indicate a nocturnal overload of northerly and northeasterly low-level humidity flows arriving from tropical South America. Under these conditions, cooling descending air from the mountains may find unstable air at the surface, giving place to the development of strong local convection. Another possible mechanism is presented here: a forced ascent of the low-level flow due to the mountains, disrupting the atmospheric stratification and generating vertical displacement of air trajectories. A Principal Component Analysis (PCA) in T-mode is applied to day- and night-time data during the maximum and extreme events. The results show strong correlation areas over each subregion under study during night-time, whereas during day-time no defined patterns are found. This confirms the observed nocturnal behavior of rainfall within these three hotspots. KW - South-America KW - rainy-season KW - part I KW - precipitation KW - TRMM KW - climate KW - summer KW - circulation KW - monsoon KW - systems Y1 - 2019 U6 - https://doi.org/10.1016/j.atmosres.2019.104792 SN - 0169-8095 VL - 234 PB - Elsevier CY - Amsterdam [u.a.] ER - TY - RPRT A1 - Thieken, Annegret A1 - Dierck, Julia A1 - Dunst, Lea A1 - Göpfert, Christian A1 - Heidenreich, Anna A1 - Hetz, Karen A1 - Kern, Julia A1 - Kern, Kristine A1 - Lipp, Torsten A1 - Lippert, Cordine A1 - Meves, Monika A1 - Niederhafner, Stefan A1 - Otto, Antje A1 - Rohrbacher, Christian A1 - Schmidt, Katja A1 - Strate, Leander A1 - Stumpp, Inga A1 - Walz, Ariane T1 - Urbane Resilienz gegenüber extremen Wetterereignissen – Typologien und Transfer von Anpassungsstrategien in kleinen Großstädten und Mittelstädten (ExTrass) BT - Verbundvorhaben „Zukunftsstadt“ (Definitionsprojekt) N2 - Weltweit verursachen Städte etwa 70 % der Treibhausgasemissionen und sind daher wichtige Akteure im Klimaschutz bzw. eine wichtige Zielgruppe von Klimapolitiken. Gleichzeitig sind Städte besonders stark von möglichen Auswirkungen des Klimawandels betroffen: Insbesondere extreme Wetterereignisse wie Hitzewellen oder Starkregenereignisse mit Überflutungen verursachen in Städten hohe Sachschäden und wirken sich negativ auf die Gesundheit der städtischen Bevölkerung aus. Daher verfolgt das Projekt ExTrass das Ziel, die städtische Resilienz gegenüber extremen Wetterereignissen in enger Zusammenarbeit mit Stadtverwaltungen, Strukturen des Bevölkerungsschutzes und der Zivilgesellschaft zu stärken. Im Fokus stehen dabei (kreisfreie) Groß- und Mittelstädte mit 50.000 bis 500.000 Einwohnern, insbesondere die Fallstudienstädte Potsdam, Remscheid und Würzburg. Der vorliegende Bericht beinhaltet die Ergebnisse der 14-monatigen Definitionsphase von ExTrass, in der vor allem die Abstimmung eines Arbeitsprogramms im Mittelpunkt stand, das in einem nachfolgenden dreijährigen Forschungsprojekt (F+E-Phase) gemeinsam von Wissenschaft und Praxispartnern umgesetzt werden soll. Begleitend wurde eine Bestandsaufnahme von Klimaanpassungs- und Klimaschutzstrategien/-plänen in 99 deutschen Groß- und Mittelstädten vorgenommen. Zudem wurden für Potsdam und Würzburg Pfadanalysen für die Klimapolitik durchgeführt. Darin wird insbesondere die Bedeutung von Schlüsselakteuren deutlich. Weiterhin wurden im Rahmen von Stakeholder-Workshops Anpassungsherausforderungen und aktuelle Handlungsbedarfe in den Fallstudienstädten identifiziert und Lösungsansätze erarbeitet, die in der F+E-Phase entwickelt und getestet werden sollen. Neben Maßnahmen auf gesamtstädtischer Ebene und auf Stadtteilebene wurden Maßnahmen angestrebt, die die Risikowahrnehmung, Vorsorge und Selbsthilfefähigkeit von Unternehmen und Bevölkerung stärken können. Daher wurde der Stand der Risikokommunikation in Deutschland für das Projekt aufgearbeitet und eine erste Evaluation von Risikokommunikationswerkzeugen durchgeführt. Der Bericht endet mit einer Kurzfassung des Arbeitsprogramms 2018-2021. N2 - Cities are responsible for around 70 % of the global greenhouse gas emissions and are hence important for climate mitigation; consequently they are a crucial target group of climate policies. At the same time, cities are also severely affected by potential impacts of climate change: extreme weather events such as heat waves or heavy precipitation (pluvial floods) cause high economic losses in urban areas and have adverse effects on the health of the urban population. Therefore, the project ExTrass is aimed at measurably enhancing cities’ resilience against extreme weather events jointly with representatives of urban administrations, disaster assistance and civil society. The project focusses on small metropolises and medium-sized cities with 50,000 to 500,000 inhabitants, in particular on the case study cities of Potsdam, Remscheid and Würzburg. The report summarizes the results of a 14-month definition phase whose main purpose was to define the research program of the successive 3-year-R+D-project, to be implemented jointly by researchers and practitioners. In addition, an inventory of climate change adaptation and climate mitigation strategies and plans of 99 German metropolises and medium-sized cities was created. Moreover, an in-depth analysis of the pathways of climate policies in the cities of Potsdam and Würzburg was conducted, which particularly revealed the relevance of key personalities. Furthermore, current challenges in climate adaptation and needs for action were identified during stakeholder workshops in the case study cities. In addition, possible solutions were discussed which will be implemented and tested during the R+D-project. Besides measures on the city level and on the level of urban districts, options that improve risk awareness, preparedness and coping capacities of enterprises and residents are strived for. Thus the state-of-the-art of risk communication in Germany was reviewed for the project and a first evaluation of a serious game was performed. The report ends with a brief outline of the work program 2018-2021. KW - Klimaanpassung KW - Klimaschutz KW - Pfadanalysen KW - Stadtentwicklung KW - Hitze KW - Starkregen KW - Risikokommunikation KW - Potsdam KW - Würzburg KW - Deutschland KW - Climate Adaptation KW - Climate Mitigation KW - analysis of pathways KW - urban development KW - heat KW - pluvial flooding KW - risk communication KW - city of Potsdam KW - city of Wuerzburg KW - Germany Y1 - 2018 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-416067 ER - TY - RPRT A1 - Huber, Bettina A1 - Miechielsen, Milena A1 - Otto, Antje A1 - Schmidt, Katja A1 - Ullrich, Susann A1 - Deppermann, Lara-Helene A1 - Eckersley, Peter A1 - Haupt, Wolfgang A1 - Heidenreich, Anna A1 - Kern, Kristine A1 - Lipp, Torsten A1 - Neumann, Nina A1 - Schneider, Philipp A1 - Sterzel, Till A1 - Thieken, Annegret T1 - Instrumente und Maßnahmen der kommunalen Klimaanpassung T1 - Instruments and measures of municipal climate adaptation BT - Empirische Befunde für einen erfolgreichen Transfer BT - Empirical findings for a successful transfer N2 - Städte sind aufgrund ihrer Agglomeration von Bevölkerung, Sachwerten und Infrastrukturen in besonderem Maße von extremen Wetterereignissen wie Starkregen und Hitze betroffen. Zahlreiche Überflutungsereignisse infolge von Starkregen traten in den letzten Jahren in verschiedenen Regionen Deutschlands auf und führten nicht nur zu Schäden in zwei- bis dreistelliger Millionenhöhe, sondern auch zu Todesopfern. Und auch Hitzewellen, wie sie in den vergangenen Jahren vermehrt aufgetreten sind, bergen gesundheitliche Risiken, welche sich auch in verschiedenen Schätzungen zu Hitzetodesfällen wiederfinden. Um diesen Risiken zu begegnen und Schäden infolge von Wetterextremen zu reduzieren, entwickeln viele Kommunen bereits Strategien und Konzepte im Kontext der Klimaanpassung und/oder setzen Anpassungsmaßnahmen um. Neben der Entwicklung und Umsetzung eigener Ideen orientieren sich Städte dabei u. a. an Leitfäden und Beispielen aus der Literatur, Erfahrungen aus anderen Städten oder an Ergebnissen aus Forschungsprojekten. Dieser Lern- und Transferprozess, der eine Übertragung von Maßnahmen oder Instrumenten der Klimaanpassung von einem Ort auf einen anderen beinhaltet, ist bislang noch unzureichend erforscht und verstanden. Der vorliegende Bericht untersucht deshalb ebendiesen Lern- und Transferprozess zwischen sowie innerhalb von Städten sowie das Transferpotenzial konkreter Wissenstransfer-Medien, Instrumente und Maßnahmen. Damit wird das Ziel verfolgt, ein besseres Verständnis dieser Prozesse zu entwickeln und einen Beitrag zur Verbesserung des Transfers von kommunalen Klimaanpassungsaktivitäten zu leisten. Der vorliegende Inhalt baut dabei auf einer vorangegangenen Analyse des Forschungsstands zum Transfer von Policies durch Haupt et al. (2021) auf und versucht, den bereits generierten Wissensstand auf der Ebene von Policies nun um die Ebene konkreter Instrumente und Maßnahmen zu ergänzen sowie durch empirische Befunde zu ausgewählten Maßnahmen zu untermauern. Die Wissens- und Datengrundlage dieses Berichts umfasst einen Mix aus verschiedenen (Online)-Befragungen und Interviews mit Vertreter:innen relevanter Akteursgruppen, vor allem Vertreter:innen von Stadtverwaltungen, sowie den Erfahrungswerten der drei ExTrass-Fallstudienstädte Potsdam, Remscheid und Würzburg. Nach einer Einleitung beschäftigt sich Kapitel 2 mit übergeordneten Faktoren der Übertragbarkeit bzw. des Transfers. Kapitel 2.1 bietet hierbei eine Zusammenfassung zum aktuellen Wissensstand hinsichtlich des Transfers von Policies im Bereich der städtischen Klimapolitik gemäß Haupt et al. (2021). Hier werden zentrale Kriterien für einen erfolgreichen Transfer herausgearbeitet, um einen Anknüpfungspunkt für die folgenden Inhalte und empirischen Befunde auf der Ebene konkreter Instrumente und Maßnahmen zu bieten. Kapitel 2.2 schließt hieran an und präsentiert Erkenntnisse aus einer weitreichenden Kommunalbefragung. Hierbei wurde untersucht ob und welche Klimaanpassungsmaßnahmen in den Städten bereits umgesetzt werden, welche fördernden und hemmenden Aspekte es dabei gibt und welche Erfahrungen beim Transfer von Wissen und Ideen bereits vorliegen. Kapitel 3 untersucht die Rolle verschiedener Medien des Wissenstransfers und widmet sich dabei beispielhaft Leitfäden zur Klimaanpassung und Maßnahmensteckbriefen. Kapitel 3.1 beantwortet dabei Fragen nach der Relevanz und Zugänglichkeit von Leitfäden, deren Stärken und Schwächen, sowie konkreten Anforderungen vonseiten befragter Personen. Außerdem werden acht ausgewählte Leitfäden vorgestellt und komprimiert auf ihre Transferpotenziale hin eingeschätzt. Kapitel 3.2 betrachtet Maßnahmensteckbriefe als Medien des Wissenstransfers und arbeitet zentrale Aspekte für einen praxisrelevanten inhaltlichen Aufbau heraus, um basierend darauf einen Muster-Maßnahmensteckbrief für Klimaanpassungsmaßnahmen zu entwickeln und vorzuschlagen. Kapitel 4 beschäftigt sich mit sehr konkreten kommunalen Erfahrungen rund um den Transfer von sieben ausgewählten Instrumenten und Maßnahmen und bietet zahlreiche empirische Befunde aus den Kommunen, basierend auf der Kommunalbefragung, verschiedenen Interviews und den Erfahrungen aus der Projektarbeit. Die folgenden sieben Instrumente und Maßnahmen wurden ausgewählt, um eine große Breite städtischer Klimaanpassungsaktivitäten zu betrachten: 1) Klimafunktionskarten (Stadtklimakarten), 2) Starkregengefahrenkarten, 3) Checklisten zur Klimaanpassung in der Bauleitplanung, 4) Verbot von Schottergärten in Bebauungsplänen, 5) Fassadenbegrünungen, 6) klimaangepasste Gestaltung von Grün- und Freiflächen sowie 7) Handlungsempfehlungen für Betreuungseinrichtungen zum Umgang mit Hitze und Starkregen. Für jede dieser Klimaanpassungsaktivitäten wird auf Ebene der Kommunen Ziel, Verbreitung und Erscheinungsformen, Umsetzung anhand konkreter Beispiele, fördernde und hemmende Faktoren sowievorliegende Erfahrungen zu und Hinweisen auf Transfer dargestellt. Kapitel 5 schließt den vorliegenden Bericht ab, indem zentrale Transfer-Barrieren aus den gewonnenen Erkenntnissen aufgegriffen und entsprechende Empfehlungen an verschiedene Ebenen der Politik ausgesprochen werden. Diese Empfehlungen zur Verbesserung des Transfers von klimaanpassungsrelevanten Instrumenten, Strategien und Maßnahmen umfassen 1) die Verbesserung des Austauschs zwischen verschiedenen Städten, 2) die Verbesserung der Zugänglichkeit von Wissen und Erfahrungen, 3) die Schaffung von Vernetzungsstrukturen innerhalb von Städten sowie 4) bestehende Wissenslücken zu schließen. Die Autor:innen des vorliegenden Berichts hoffen, durch die vielfältigen Untersuchungsaspekte einen Beitrag zum besseren Verständnis der Lern- und Transferprozesse und zur Verbesserung des Transfers kommunaler Klimaanpassungsaktivitäten zu leisten. N2 - Due to their agglomeration of population, material assets and infrastructures, cities are particularly affected by extreme weather events such as heavy rain and heat. Numerous flooding events as a result of heavy rainfall occurred in various regions of Germany in the last years, not only resulted in losses in the double- to triple-digit million range, but also in fatalities. And heat waves which became more frequent in recent years pose health risks, including numerous cases of death. To counter these risks and to reduce damage resulting from weather extremes, many cities are already developing strategies and concepts in the context of climate adaptation and/or implement measures. In addition to developing and implementing their own ideas, cities are guided by guidelines and examples from literature, experiences from other cities, or results from research projects, among other things. This learning and transfer process, which involves the transfer of climate adaptation measures or instruments from one place to another, has not yet been sufficiently researched and understood. This report therefore examines this learning and transfer process between and within cities as well as the transfer potential of specific knowledge transfer media, instruments and measures. The aim is to develop a better understanding of these processes and to contribute to improving the transfer of municipal climate adaptation activities. This content builds on a previous analysis of the state of research on policy transfer by Haupt et al. (2021) and attempts to complement the already generated state of knowledge on the level of policies with the level of concrete instruments and measures and to substantiate it with empirical findings. The knowledge and data basis of this report comprises a mix of various (online) surveys and interviews with representatives of relevant stakeholder groups, especially representatives of city administrations, as well as the experiences of the three case study cities within the ExTrass-project, namely Potsdam, Remscheid and Würzburg. After an introduction, chapter 2 deals with overarching factors of transferability. Chapter 2.1 provides a summary of the current state of knowledge regarding the transfer of policies in the field of urban climate policy according to Haupt et al. (2021). Here, central criteria for a successful transfer are elaborated in order to provide a starting point for the following contents and empirical findings on the level of concrete instruments and measures. Chapter 2.2 follows on from this and presents findings from a wide-ranging municipal survey. Here, it was investigated whether and which climate adaptation measures are already implemented in the cities, which supporting and inhibiting aspects are present in this context, and which experiences regarding the transfer of knowledge and ideas already exist. Chapter 3 examines the role of different knowledge transfer media, focusing on guidelines on climate adaptation and fact sheets for adaptation measures as examples. Chapter 3.1 answers questions about the relevance and accessibility of guidelines, their strengths and weaknesses, as well as concrete requirements articulated by interviewees. In addition, eight selected guidelines are shortly presented and assessed in terms of their transfer potential. Chapter 3.2 looks at fact sheets for adaptation measures and elaborates central aspects for a practicable content structure and ultimately results in a proposed template fact sheet for climate adaptation measure. Chapter 4 deals with very concrete municipal experiences regarding the transfer of seven selected instruments and measures and offers numerous empirical findings from municipalities, based on the municipal survey, various interviews and the experiences drawn from the project work. The following seven tools and measures were selected to look at a broad range of urban climate adaptation activities: 1) climate function maps (urban climate maps), 2) heavy rainfall hazard maps, 3) climate adaptation checklists in urban land use planning, 4) prohibition of gravel gardens in development plans, 5) facade greening, 6) climate-adapted design of green and open spaces, and 7) recommendations for care facilities to deal with heat and heavy rain. For each of these instruments or measures at the municipality level the purpose or goal, its dissemination and manifestations, its implementation through practical examples, its supporting and inhibiting factors as well as existing experiences with and evidence of transfer are presented. Chapter 5 concludes this report by addressing key transfer barriers and making formulating recommendations for different political levels. These recommendations for improving the transfer of climate adaptation-related instruments, strategies and measures include: 1) improving the exchange between different cities, 2) improving the accessibility of knowledge and experience, 3) creating networking structures within cities and 4) closing existing knowledge gaps. The authors of this report hope to contribute to a better understanding of the learning and transfer processes and to the improvement of the transfer of municipal climate adaptation activities through the manifold aspects of this study. KW - Klimaanpassung KW - Übertragbarkeit KW - Anpassungsmaßnahmen KW - Wissenstransfer KW - Climate adaptation KW - Transferablity KW - adapatation measures KW - knowledge transfer KW - Modellstadt KW - model city KW - Pilotmaßnahmen KW - pilot measures Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-563456 ER - TY - GEN A1 - Ramezani Ziarani, Maryam A1 - Bookhagen, Bodo A1 - Schmidt, Torsten A1 - Wickert, Jens A1 - de la Torre, Alejandro A1 - Deng, Zhiguo A1 - Calori, Andrea T1 - A model for the relationship between rainfall, GNSS-derived integrated water vapour, and CAPE in the eastern central Andes T2 - Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - Atmospheric water vapour content is a key variable that controls the development of deep convective storms and rainfall extremes over the central Andes. Direct measurements of water vapour are challenging; however, recent developments in microwave processing allow the use of phase delays from L-band radar to measure the water vapour content throughout the atmosphere: Global Navigation Satellite System (GNSS)-based integrated water vapour (IWV) monitoring shows promising results to measure vertically integrated water vapour at high temporal resolutions. Previous works also identified convective available potential energy (CAPE) as a key climatic variable for the formation of deep convective storms and rainfall in the central Andes. Our analysis relies on GNSS data from the Argentine Continuous Satellite Monitoring Network, Red Argentina de Monitoreo Satelital Continuo (RAMSAC) network from 1999 to 2013. CAPE is derived from version 2.0 of the ECMWF’s (European Centre for Medium-Range Weather Forecasts) Re-Analysis (ERA-interim) and rainfall from the TRMM (Tropical Rainfall Measuring Mission) product. In this study, we first analyse the rainfall characteristics of two GNSS-IWV stations by comparing their complementary cumulative distribution function (CCDF). Second, we separately derive the relation between rainfall vs. CAPE and GNSS-IWV. Based on our distribution fitting analysis, we observe an exponential relation of rainfall to GNSS-IWV. In contrast, we report a power-law relationship between the daily mean value of rainfall and CAPE at the GNSS-IWV station locations in the eastern central Andes that is close to the theoretical relationship based on parcel theory. Third, we generate a joint regression model through a multivariable regression analysis using CAPE and GNSS-IWV to explain the contribution of both variables in the presence of each other to extreme rainfall during the austral summer season. We found that rainfall can be characterised with a higher statistical significance for higher rainfall quantiles, e.g., the 0.9 quantile based on goodness-of-fit criterion for quantile regression. We observed different contributions of CAPE and GNSS-IWV to rainfall for each station for the 0.9 quantile. Fourth, we identify the temporal relation between extreme rainfall (the 90th, 95th, and 99th percentiles) and both GNSS-IWV and CAPE at 6 h time steps. We observed an increase before the rainfall event and at the time of peak rainfall—both for GNSS-integrated water vapour and CAPE. We show higher values of CAPE and GNSS-IWV for higher rainfall percentiles (99th and 95th percentiles) compared to the 90th percentile at a 6-h temporal scale. Based on our correlation analyses and the dynamics of the time series, we show that both GNSS-IWV and CAPE had comparable magnitudes, and we argue to consider both climatic variables when investigating their effect on rainfall extremes. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 1172 KW - Global Navigation Satellite System (GNSS) KW - GNSS-integrated water vapour KW - convective available potential energy (CAPE) KW - extreme rainfall KW - TRMM Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-523256 SN - 1866-8372 IS - 1172 ER - TY - JOUR A1 - Dahm, Torsten A1 - Stiller, Manfred A1 - Mechie, James A1 - Heimann, Sebastian A1 - Hensch, Martin A1 - Woith, Heiko A1 - Schmidt, Bernd A1 - Gabriel, Gerald A1 - Weber, Michael T1 - Seismological and geophysical signatures of the deep crustal magma systems of the cenozoic volcanic fields Beneath the Eifel, Germany JF - Geochemistry, geophysics, geosystems N2 - The Quaternary volcanic fields of the Eifel (Rhineland-Palatinate, Germany) had their last eruptions less than 13,000 years ago. Recently, deep low-frequency (DLF) earthquakes were detected beneath one of the volcanic fields showing evidence of ongoing magmatic activity in the lower crust and upper mantle. In this work, seismic wide- and steep-angle experiments from 1978/1979 and 1987/1988 are compiled, partially reprocessed and interpreted, together with other data to better determine the location, size, shape, and state of magmatic reservoirs in the Eifel region near the crust-mantle boundary. We discuss seismic evidence for a low-velocity gradient layer from 30-36 km depth, which has developed over a large region under all Quaternary volcanic fields of the Rhenish Massif and can be explained by the presence of partial melts. We show that the DLF earthquakes connect the postulated upper mantle reservoir with the upper crust at a depth of about 8 km, directly below one of the youngest phonolitic volcanic centers in the Eifel, where CO(2)originating from the mantle is massively outgassing. A bright spot in the West Eifel between 6 and 10 km depth represents a Tertiary magma reservoir and is seen as a model for a differentiated reservoir beneath the young phonolitic center today. We find that the distribution of volcanic fields is controlled by the Variscan lithospheric structures and terrane boundaries as a whole, which is reflected by an offset of the Moho depth, a wedge-shaped transparent zone in the lower crust and the system of thrusts over about 120 km length. KW - magma reservoirs KW - distributed volcanic fields KW - reflection seismic KW - crustal magma chamber KW - deep low-frequency earthquakes KW - low velocity zone Y1 - 2020 U6 - https://doi.org/10.1029/2020GC009062 SN - 1525-2027 VL - 21 IS - 9 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Hensch, Martin A1 - Dahm, Torsten A1 - Ritter, Joachim A1 - Heimann, Sebastian A1 - Schmidt, Bernd A1 - Stange, Stefan A1 - Lehmann, Klaus T1 - Deep low-frequency earthquakes reveal ongoing magmatic recharge beneath Laacher See Volcano (Eifel, Germany) JF - Geophysical journal international N2 - The occurrence of deep low-frequency (DLF) microearthquakes beneath volcanoes is commonly attributed to mass transport in the volcanic plumbing system and used to infer feeding channels from and into magma reservoirs. The key question is how magmas migrate from depth to the shallow crust and whether magma reservoirs are currently being recharged. For the first time since the improvement of the local seismic networks in the East Eifel region (Rhineland-Palatinate, Germany), we detect and locate recurrent DLF earthquakes in the lower crust and upper mantle beneath the Laacher See Volcano (LSV), using a joint data set of permanent sensors and a temporary deployment. So far, eight DLF earthquake sequences were observed in four distinct clusters between 10 and 40 km depth. These clusters of weak events (M-L< 2) align along an approximately 80. southeast dipping line south of the LSV. Moment tensor solutions of these events have large shear components, and the irregular dispersion and long coda of body waves indicate interaction processes between shear cracks and fluids. We find a rotation of P-axes orientation for shallow tectonic earthquakes compared to DLF events, indicating that the stress field in the depth interval of DLF events might favour a vertical migration of magma or magmatic fluids. The caldera of the LSV was formed by the last major eruption of the East Eifel Volcanic Field only 12.9 kyr ago, fed by a shallow magma chamber at 5-8 km depth and erupting a total magma volume of 6.7 km(3). The observed DLF earthquake activity and continuous volcanic gas emissions around the LSV indicate an active magmatic system, possibly connected with an upper mantle melt zone. KW - Waveform inversion KW - Volcano seismology KW - Magma migration and fragmentation KW - Volcano monitoring Y1 - 2019 U6 - https://doi.org/10.1093/gji/ggy532 SN - 0956-540X SN - 1365-246X VL - 216 IS - 3 SP - 2025 EP - 2036 PB - Oxford Univ. Press CY - Oxford ER -