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  • 1
    Online Resource
    Online Resource
    Basel :Springer Basel AG,
    Keywords: Life sciences. ; Medicine. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (292 pages)
    Edition: 1st ed.
    ISBN: 9783034861083
    DDC: 570
    Language: German
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  • 2
    Online Resource
    Online Resource
    Basel :Springer Basel AG,
    Keywords: Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (316 pages)
    Edition: 1st ed.
    ISBN: 9783034876438
    Language: German
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  • 3
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 97 S. , Ill., graph Darst.
    Language: German
    Note: Hamburg, Univ., Diss., 1996
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Solar physics 177 (1998), S. 287-294 
    ISSN: 1573-093X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract We present a method for the determination of the center-to-limb variation (CLV) for Caii K spectroheliograms. It is based on the calculation of intensity histograms for rings of constant area. Using a simple cutoff criterion in the cumulative histograms, we are able to derive CLVs of the quiet Sun regardless of the solar activity level. Using an example from the literature, we show in which way different methods of normalization of the quiet-Sun CLV may affect the results.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Solar physics 187 (1999), S. 347-356 
    ISSN: 1573-093X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract A method for the improvement of resolution in an observed solar image is proposed. A blind deconvolution method is used for restoration of an atmospherically-degraded solar image, and a super-resolution method is applied to its restored image to improve the resolution. It is confirmed that a blind deconvolution process can restore fine structures that are blurred in an observed image, and that the super-resolution process can make a cutoff frequency in a blind-deconvolved image higher. A time series of super-resolved images of a sunspot observed with the 70-cm Vacuum Tower Telescope at Teide Observatory is presented.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Biologie in unserer Zeit 29 (1999), S. 151-157 
    ISSN: 0045-205X
    Keywords: Life and Medical Sciences
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Biology
    Notes: Generell ist der Markt für gentechnisch veränderte Pflanzen und daraus hergestellte Produkte in den letzten Jahren gewachsen. In Deutschland zeigen sich indessen eher verhaltene Auswirkungen dieser Entwicklung ‘3’. Die wirtschaftliche Entfaltung der Gentechnik und Biotechnologie ist in Deutschland noch gering. Als ein Maß für den Entwicklungsstand der Gentechnik in der Pflanzenzüchtung ‘2’ und damit unter anderem auch deren Auswirkung auf die Futter- und Lebensmittelproduktion kann die Anzahl von Freisetzungsvorhaben mit gentechnisch veränderten Organismen (GVO) gelten. Von den rund 1300 Freisetzungsvorhaben im Bereich der EU entfallen 90 auf Deutschland. Im Vergleich zu den anderen EU-Mitgliedsstaaten rangiert Deutschland damit auf dem siebenten Platz.
    Additional Material: 4 Ill.
    Type of Medium: Electronic Resource
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  • 7
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    In:  (PhD/ Doctoral thesis), Universität Hamburg, Hamburg, Germany, 99 pp
    Publication Date: 2019-08-08
    Type: Thesis , NonPeerReviewed
    Format: text
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  • 8
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    AGU (American Geophysical Union)
    In:  Journal of Geophysical Research: Oceans, 104 . 30,039-30,046.
    Publication Date: 2018-04-17
    Description: In this paper we discuss two different methods of inferring characteristics of the interior ocean dynamics from radar signatures of internal solitary waves visible on synthetic aperture radar (SAR) images. The first one consists in the recognition and the interpretation of sea surface patterns of internal solitary waves; the second one consists in the analysis of the modulation depth of the normalized radar backscattering cross section (NRCS) associated with internal solitary waves. For this purpose we consider a data set composed of SAR and in situ measurements carried out from 1991 to 1997 in the region of the Strait of Messina. The recognition and the interpretation of sea surface patterns of internal solitary waves in the Strait of Messina can be used to study characteristics of the density distribution in the area: The internal wave field varies with seasonal variations in the vertical density stratification and with remotely induced variations, i.e., variations induced by the larger-scale circulation, in the horizontal density distribution. In order to inquire into the possibility of inferring parameters of the interior ocean dynamics by analyzing the modulation of the NRCS associated with internal solitary waves, several numerical simulations are carried out using a radar imaging model. These simulations are performed by assuming different wind conditions and internal wave parameters. It is shown that an accurate knowledge of wind conditions is crucial for deriving internal wave parameters and hence parameters of the interior ocean dynamics from the modulation of measured NRCS associated with internal solitary waves.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2017-11-24
    Description: A weakly nonhydrostatic, two-layer numerical model based on the Boussinesq equations is presented which is capable of describing, among others, the generation and propagation of nonlinear weakly dispersive internal waves in the Strait of Gibraltar. The model depends on one space coordinate only, but it retains several features of a fully three-dimensional model by including a realistic bottom profile, a variable channel width, and a trapezoidal channel cross section. The nonlinear primitive Boussinesq equations include horizontal diffusion, bottom friction, and friction between the two water layers. The model is driven by a height difference of the mean interface depth between the Atlantic and the Mediterranean boundaries and by semidiurnal tidal oscillations of the barotropic transport. The model presented in this paper describes (1) the mean and tidal flow in the Strait of Gibraltar, (2) the variation of the depth of the interface during a tidal cycle, (3) the generation of strong depressions of the interface at the western sides of the Spartel Sill and the Camarinal Sill, (4) the generation of strong eastward propagating internal bores, and (5) their disintegration into trains of internal solitary waves. The surface convergence patterns associated with depressions of the interface at the Camarinal Sill, internal bores, and internal solitary waves are calculated and compared with roughness patterns visible on synthetic aperture radar (SAR) images of the first European Remote Sensing Satellite ERS 1. In total, 155 ERS 1 SAR scenes from 94 satellite overflights over the Strait of Gibraltar, which were acquired in the period from January 1992 to March 1995, have been analyzed. It is shown that the proposed model is capable of explaining the observed temporal and spatial evolution of surface roughness patterns associated with eastward propagating internal waves inside the Strait of Gibraltar as well as the observed east-west asymmetry of the internal wave field.
    Type: Article , PeerReviewed
    Format: text
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  • 10
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    AMS (American Meteorological Society)
    In:  Journal of Physical Oceanography, 27 . pp. 648-663.
    Publication Date: 2018-04-06
    Description: A new numerical two-layer model is presented, which describes the generation of internal tidal bores and their disintegration into internal solitary waves in the Strait of Messina. This model is used to explain observations made by the synthetic aperture radar (SAR) from the European Remote Sensing satellites ERS 1 and ERS 2. The analysis of available ERS 1/2 SAR data of the Strait of Messina and adjacent sea areas show that 1) northward as well as southward propagating internal waves are generated in the Strait of Messina, 2) southward propagating internal waves are observed more frequently than northward propagating internal waves, 3) sea surface manifestations of southward as well as northward propagating internal waves are stronger during periods where a strong seasonal thermocline is known to be present, 4) southward propagating internal bores are released from the sill between 1 and 5 hours after maximum northward tidal flow and northward propagating internal bores are released between 2 and 6 hours after maximum southward tidal flow, and 5) the spatial separation between the first two internal solitary waves of southward propagating wave trains is smaller in the period from July to September than in the period from October to June. The numerical two-layer model is a composite of two models consisting of 1) a hydrostatic “generation model,” which describes the dynamics of the water masses in the region close to the strait’s sill, where internal bores are generated, and 2) a weakly nonhydrostatic “propagation model,” which describes the dynamics of the water masses outside of the sill region where internal bores may disintegrate into internal solitary waves. Due to a technique for movable lateral boundaries, the generation model is capable of simulating the dynamics of a lower layer that may intersect the bottom topography. The proposed generation–propagation model depends on one space variable only, but it retains several features of a fully three-dimensional model by including a realistic channel depth and a realistic channel width. It is driven by semidiurnal tidal oscillations of the sea level at the two open boundaries of the model domain. Numerical simulations elucidate several observed characteristics of the internal wave field in the Strait of Messina, such as north–south asymmetry, times of release of the internal bores from the strait’s sill, propagation speeds, and spatial separations between the first two solitary waves of internal wave trains.
    Type: Article , PeerReviewed
    Format: text
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