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  • Other Sources  (5)
  • Geophysikalische Satellitenfernerkundung  (5)
  • GFZ, Helmholtz-Zentrum  (5)
  • American Institute of Physics (AIP)
  • Cambridge University Press
  • Copernicus Publications (EGU)
  • Institut für Meereskunde
  • Nature Publishing Group (NPG)
  • 2010-2014  (5)
  • 1985-1989
  • 1955-1959
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  • Other Sources  (5)
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  • 2010-2014  (5)
  • 1985-1989
  • 1955-1959
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  • 1
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    GFZ, Helmholtz-Zentrum | [Bibliothek des Wiss.-Parks Albert Einstein] [Vertrieb], [Potsdam]
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551 ; VAE 300 ; TQI 000 ; UNH 100 ; Epirogenese {{Geologie}} ; Geophysikalische Satellitenfernerkundung ; GPS {Praktische Geodäsie}
    Language: English
    Type: article , publishedVersion
    Format: 28 S.
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  • 2
    Publication Date: 2021-03-29
    Description: thesis
    Keywords: 551 ; TOF 000 ; TQA 000 ; TQI 000 ; Schwerkraft {Geophysik} ; Gravimetrische Verfahren {Geophysik} ; Geophysikalische Satellitenfernerkundung
    Language: German
    Type: monograph , publishedVersion
    Format: 141 S.
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  • 3
    Publication Date: 2021-03-29
    Description: After a gap of nearly two decades since the Magsat mission in 1980, the dedicated low-orbit potential field mission CHAMP is now in the third of its seven year mission. Already, the new magnetic total intensity and vector data have yielded maps of the global crustal field of unprecedented accuracy and resolution. Here, we assess the value of these maps to infer deep crustal structure of regions overlain by younger cover. A GIS based modelling technique has been developed to model the various geological units of the continents starting from the geological map of the world. Depending upon the known rock types of the region, they are assigned a standard susceptibility value and using the global seismic crustal structure, a vertically integrated susceptibility (VIS) model is computed at each point of the region. Starting with this initial VIS model, the vertical field anomaly is computed at a satellite altitude of 400 km and compared with the corresponding CHAMP vertical field anomaly map. The first comparison is carried out against a model using the lateral extent of a cratonic region as given by published tectonic maps. In the subsequent modelling step, depending upon the extent of the observed anomaly pattern of that region, the surface geology is extended beneath the sediments until the recomputed map fits the observed magnetic anomaly map. Here, we focus on modelling results for the selected few provinces of the world where the initial model does not agree with the observed anomaly map. Similar modelling of CHAMP satellite magnetic anomalies can constrain the subsurface structure hidden by Phanerozoic cover in many parts of the world.
    Description: thesis
    Keywords: 551 ; TOD 200 ; TOT 330 ; TOT 100 ; TQI 000 ; TQB 000 ; Erdkruste {Geophysik} ; Anomalien {Geophysik: Erdmagnetismus} ; Methodik {Geophysik: Erdmagnetismus} ; Geophysikalische Satellitenfernerkundung ; Erdmagnetische Verfahren {Geophysik}
    Language: German
    Type: monograph , publishedVersion
    Format: 137 S.
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  • 4
    Publication Date: 2021-03-29
    Description: Recently released global gravity field models generated solely from CHAMP and GRACE satellite observations allow with an unprecedented accuracy and resolution the recovery of the mean sea surface topography from the difference between an altimetry-based mean sea surface height model and the gravity model's derived geoid. Here the CHAMP EIGEN-2 gravity field model, and the first GFZ GRACE gravity model, EIGEN-GRACE01S, are used. The mean sea surface height model has been compiled from four years'; worth of TOPEX altimeter data. To evaluate the accuracy and resolution limits of the CHAMP and GRACE geoids for the envisaged application, a low pass filter in the spatial domain with different cut-off wavelengths has been applied to the geoid and sea surface data before subtraction. The minimum wavelength, where noisy and erroneous features in the recovered sea surface topography are minimised, can be interpreted as an indicator for the best suited common spatial resolution. The EIGEN-2 model's geoid has been tested to have a resolution of 1800 km, which corresponds to a truncation degree of l = 22 in terms of spherical harmonics. Using the EIGEN-GRACE01S model, the resolution could be extended to 1000 km (l = 40). These boundaries can be attributed to the geoid's error, exceeding 2 cm in case of the CHAMP model, and in case of the GRACE model to spurious systematic signals increasing with increasing spherical harmonic degree. The calculated sea surface topography models have been used to derive absolute geostrophic sea surface velocities. An error propagation shows that the requirement of 1 cm/s for geoid induced velocity errors is fulfilled at the given resolutions for all latitudes excluding a narrow equatorial band. Maximum geostrophic velocities are derived in the 1000 km-resolution model for the Kuroshio region with 40 cm/s, and for the Gulf Stream east off Cape Hatteras with 25 cm/s.
    Description: report
    Keywords: 551 ; TQI 000 ; Geophysikalische Satellitenfernerkundung
    Language: English
    Type: article , publishedVersion
    Format: 22 S.
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  • 5
    Publication Date: 2021-03-29
    Description: thesis
    Keywords: 551 ; VAE 850 ; TQC 220 ; TSI 000 ; TQI 000 ; VBJ 000 ; VEI 400 ; Festländische Lineamente {Geologie} ; Reflexionsseismik {Geophysik} ; Vorderasien {Geophysik} ; Geophysikalische Satellitenfernerkundung ; Satellitenbildgeologie ; Israel, Palästina {Geologie}
    Language: English
    Type: monograph , publishedVersion
    Format: 98 S.
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