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  • 1
    Monograph available for loan
    Monograph available for loan
    Führer zur Geologie von Berlin und Brandenburg; Nr. 4: Potsdam und Umgebung (2001)
    Berlin : Selbstverlag Geowissenschaftler in Berlin und Brandenburg e.V.
    Associated volumes
    Details Availability
    Call number: 9/M 03.0406 ; AWI G10-01-0242 ; 9/M 22.65041
    In: Führer zur Geologie von Berlin und Brandenburg, Nr. 4
    Type of Medium: Monograph available for loan
    Pages: VI, 277, XI Seiten , Illustrationen
    Edition: 2. erweiterte Auflage
    ISBN: 3928651099 , 3-928651-09-9
    ISSN: 0941-2980
    Series Statement: Führer zur Geologie von Berlin und Brandenburg 4
    Classification:
    Regional Geology
    Language: German
    Note: INHALT: Vorwort / J. H. Schroeder I GRUNDLAGEN I-1 Geologie des Untergrundes I-1.1 Der präquartäre Untergrund I-1.1.1 Geologische Entwicklung / W. Stackebrandt & H. Beer I-1.1.2 Geschichte und ausgewählte Ergebnisse der geologischen Tiefenerkundung / J. Kopp I-1.1.3 Wirtschaftliche Nutzung des tieferen Untergrundes / W. Stackebrandt I-1.2 Die Quartärbasis / H. Jortzig I-1.3 Das Quartär I-1.3.1 Quartär-Sedimentologie und -Stratigraphie / J. H. Schroeder mit Beiträgen von L. Lippstreu, R. Weiße, H. Ziermann & R. Zwirner I-1.3.2 Quartäre Fossilien aus dem Potsdamer Raum / N. Hermsdorf I-2 Oberflächennahe Glazialgeologie und Geomorphologie / R. Weiße I-2.1 Überblick I-2.2 Zur Geschichte der Erforschung I-2.3 Grundsätze der Aufnahme und Interpretation I-2.4 Morphographie des Potsdamer Gebietes I-2.5 Naturräumlicher Überblick I-2.6 Ausgewählte glazigene Sedimente (Tille) I-2.7 Glaziale Baustiltypen der Potsdamer Umgebung I-2.8 Die Entstehung der Ländchen- (Insel-, Platten-) Niederungs-Struktur I-2.9 Periglaziale Oberflächenformen und Strukturen I-3 Böden im Raum Potsdam / D. Knothe I-4 Klima und Vegetation I-4.1 Spätglaziale und holozäne Klimaentwicklung am Beispiel des großen Fercher Kesselmoors / V. Rowinsky I-4.2 Jungholozäne Vegetations- und Moorentwicklung / A. Brande, M. Müller & S. Wolters I-4.3 Vegetationskundliche Übersicht für die Gegenwart / H.-D. Krausch I-5 Die Entwicklung der Landnutzung / H.-D. Krausch II EXKURSIONEN II-1 Potsdamer Kulturlandschaft / R. Weiße II-2 Glazial- und Periglazialrelief der hohen Stauchmoräne der Kahleberge mit aufgesetzten Kames / R. Weiße II-3 Relief, Baustil und Genese des Templiner Innensanders / R. Weiße II-4 Nuthe-Niederung / R. Weiße, A. Brande & W. Linder II-5 Satzendmoräne auf gestauchtem Sockel in der Fresdorfer Heide / R. Weiße II-6 Die weichselkaltzeitliche Caputher Niedertau- (Kames-) Hügellandschaft / R. Weiße II-7 Die periglazial zertalte Stauch(end)moräne Wietkikenberg / R. Weiße II-8 Ferch und die Gletschertorrinne / R. Weiße II-9 Die Natur-Kulturlandschaft Petzow / R. Weiße II-10 Aussicht vom Fuchsberg; gestauchte Glindower Grundmoränenplatte / R. Weiße II-11 Die Ziegeleigruben Glindow; Geschichte der Ziegelproduktion / R. Weiße II-12 Die Dünen bei Bliesendorf / M. Müller, M. Böse & A. Brande II-13 Der Kiessandzug von Bochow-Damsdorf / R. Weiße II-14 Phöben II-14.1 Gestapelter Geschiebemergel an der Phöbener Kerbstauch(end)moräne / R. Weiße II-14.2 Siedlungsentwicklung im Bereich der Fundstelle Phöben 9 / R. Bräunig & J. Henker II-15 Der Kahle Berg bei Zachow / R. Weiße mit einem Beitrag von N. Hermsdorf II-16 Weichselkaltzeitlicher Sand-Durchspießungsrücken Mühlenberg bei Buchow-Karpzow / R. Weiße mit einem Beitrag von N. Hermsdorf III ERGÄNZENDE BEITRÄGE III-1 Hydrogeologische Verhältnisse / A . Hermsdorf, B. Rechlin III-2 Salzwasserquellen in Brandenburg / W. Schirrmeister lll-3 Hydrographie der Potsdamer Havelgewässer / E- Jungfer lII-4 Bodenschätze im Potsdamer Havelland: Geschichte der Nutzung / G . Stackebrandt III-5 Sedimentärgeschiebe im Exkursionsgebiet, insbesondere in der Kiesgrube Fresdorfer Heide / G . Engelhardt III-6 Geotope und deren Schutz / D. Göllnitz III-7 Naturschutz in der Nuthe-Nieplitz-Niederung / U. Hermel & R. Weiße III-8 Die "Römerschanze" bei Potsdam-Sacrow / B. Gramsch IV QUELLEN IV-1 Literatur / Alle Autoren IV-2 Karten / W. Bartmann V FACHWÖRTER / M . Müller VI INDIVIDUELLES EXKURSIONSVERZEICHNIS.
    Location: Reading room
    Location: AWI Reading room
    Location: Reading room
    Branch Library: GFZ Library
    Branch Library: AWI Library
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Warnsignal Klima: Extremereignisse : wissenschaftliche Fakten (2018)
    Hamburg : Wissenschaftliche Auswertungen
    Details Availability
    Call number: PIK N 456-21-94595
    Type of Medium: Monograph available for loan
    Pages: 384 Seiten , Illustrationen
    ISBN: 978-3-9820067-0-3
    Language: German
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Electronic Resource
    Electronic Resource
    Influence of the spectral bandwith of the spectrometer on the sensitivity using continuum source AAS (1996)
    Springer
    Fresenius' Zeitschrift für analytische Chemie 355 (1996), S. 300-303 
    Details
    ISSN: 1618-2650
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Abstract The influence of the spectral bandwidth of the spectrometer on the performance of the spectrometer is of great importance in atomic absorption spectrometry using continuum source (CS-AAS). For a theoretical analysis of the detection of small absorbances two cases have to be taken into account: as long as the limiting noise of the signal is given by the detector noise an increase in spectral bandwidth of the spectrometer implies an improvement in the limit of detection. In contrast, if the noise of the signal is dominated by the photon shot noise the detection limit should become independent of the spectral bandwidth. In this case the spectral bandwidth of the spectrometer should be chosen equal to the bandwidth of the absorption line to avoid spectral interferences. Theoretical calculations are presented for the dependence of the characteristic mass on the spectral bandwidth in case of CS-AAS measurements. The results are compared with experimental measurements for six different elements using continuum source as well as line sources. The investigations were done using a double echelle monochromator (DEMON) which offers a high spectral resolution λ/Δλ of about 140,000.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s0021663550300
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  • 4
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    The North Sea — A shelf sea in the Anthropocene. (2015)
    Elsevier
    In:  EPIC3Journal of Marine Systems, Elsevier, 141, pp. 18-33
    Details
    Publication Date: 2018-02-16
    Description: Global and regional change clearly affects the structure and functioning of ecosystems in shelf seas. However, complex interactions within the shelf seas hinder the identification and unambiguous attribution of observed changes to drivers. These include variability in the climate system, in ocean dynamics, in biogeochemistry, and in shelf sea resource exploitation in the widest sense by societies. Observational time series are commonly too short, and resolution, integration time, and complexity of models are often insufficient to unravel natural variability from anthropogenic perturbation. The North Sea is a shelf sea of the North Atlantic and is impacted by virtually all global and regional developments. Natural variability (from interannual to multidecadal time scales) as response to forcing in the North Atlantic is overlain by global trends (sea level, temperature, acidification) and alternating phases of direct human impacts and attempts to remedy those. Human intervention started some 1000 years ago (diking and associated loss of wetlands), expanded to near-coastal parts in the industrial revolution of the mid-19th century (river management, waste disposal in rivers), and greatly accelerated in the mid-1950s (eutrophication, pollution, fisheries). The North Sea is now a heavily regulated shelf sea, yet societal goals (good environmental status versus increased uses), demands for benefits and policies diverge increasingly. Likely, the southern North Sea will be re-zoned as riparian countries dedicate increasing sea space for offshore wind energy generation with uncertain consequences for the system's environmental status. We review available observational and model data (predominantly from the southeastern North Sea region) to identify and describe effects of natural variability, of secular changes, and of human impacts on the North Sea ecosystem, and outline developments in the next decades in response to environmental legislation, and in response to increased use of shelf sea space.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 5
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    Structure of NDP-forming Ac-CoA synthetase [Biochemistry] (2016)
    National Academy of Sciences
    Details
    Publication Date: 2016-02-03
    Description: The NDP-forming acyl-CoA synthetases (ACDs) catalyze the conversion of various CoA thioesters to the corresponding acids, conserving their chemical energy in form of ATP. The ACDs are the major energy-conserving enzymes in sugar and peptide fermentation of hyperthermophilic archaea. They are considered to be primordial enzymes of ATP synthesis in...
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
    Published by National Academy of Sciences
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  • 6
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    Observed mean sea level changes around the North Sea coastline from 1800 to present (2013)
    Elsevier
    Details
    Publication Date: 2013-09-01
    Print ISSN: 0012-8252
    Electronic ISSN: 1872-6828
    Topics: Geography , Geosciences
    Published by Elsevier
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  • 7
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    Storminess over the North Atlantic and northwestern Europe-A review (2014)
    Wiley
    Details
    Publication Date: 2014-05-19
    Print ISSN: 0035-9009
    Electronic ISSN: 1477-870X
    Topics: Geography , Physics
    Published by Wiley
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  • 8
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    Wave climatology in the Arkona Basin, the Baltic Sea (2011)
    Copernicus
    Details
    Publication Date: 2011-11-21
    Description: The basic features of the wave climate in the South-Eastern Baltic Sea are studied based on available long-term measurements and simulations. The analysis of average, typical and extreme wave conditions, frequency of occurrence of different wave parameters, variations in wave heights from weekly to decadal scales, etc., is performed based on waverider measurements at the Darss Sill since 1991. The measured climatology is compared against numerical simulations with the WAM wave model driven by downscaled reanalysis of wind fields for 1958–2002 and by adjusted geostrophic winds for 1970–2007. The wave climate in this region is typical for semi-enclosed basins of the Baltic Sea. The maximum wave heights are about half of those in the Baltic Proper. The overall reliably recorded maximum significant wave height HS =4.46 m occurred during a severe S-SW storm in 1993 when the 10-min average wind speed reached 28 m s−1. The long-term average significant wave height (0.75 m) shows modest interannual (about 12 % of the long-term mean) and substantial seasonal variation. The wave periods are mostly concentrated in a narrow range of 2.5–4 s and their distribution is almost constant over decades. The role of remote swell is very small. The annual wave properties show large interannual variability but no long-term trends in average and extreme wave heights can be observed.
    Print ISSN: 1812-0806
    Electronic ISSN: 1812-0822
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 9
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    Wave climate in the Arkona Basin, the Baltic Sea (2012)
    Copernicus
    Details
    Publication Date: 2012-04-17
    Description: The basic features of the wave climate in the Southwestern Baltic Sea (such as the average and typical wave conditions, frequency of occurrence of different wave parameters, variations in wave heights from weekly to decadal scales) are established based on waverider measurements at the Darss Sill in 1991–2010. The measured climate is compared with two numerical simulations with the WAM wave model driven by downscaled reanalysis of wind fields for 1958–2002 and by adjusted geostrophic winds for 1970–2007. The wave climate in this region is typical for semi-enclosed basins of the Baltic Sea. The maximum wave heights are about half of those in the Baltic Proper. The maximum recorded significant wave height HS =4.46 m occurred on 3 November 1995. The wave height exhibits no long-term trend but reveals modest interannual (about 12 % of the long-term mean of 0.76 m) and substantial seasonal variation. The wave periods are mostly concentrated in a narrow range of 2.6–4 s. Their distribution is almost constant over decades. The role of remote swell is very small.
    Print ISSN: 1812-0784
    Electronic ISSN: 1812-0792
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 10
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    Multi-decadal atmospheric modeling for Europe yields multi-purpose data (2001)
    American Geophysical Union
    Details
    Publication Date: 2001-01-01
    Print ISSN: 0096-3941
    Electronic ISSN: 2324-9250
    Topics: Geosciences
    Published by American Geophysical Union
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