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  • 1
    Keywords: Geophysics. ; Planetary science. ; Geomorphology. ; Geophysics. ; Planetary Science. ; Geomorphology.
    Description / Table of Contents: Introduction -- Notes to Theory and Data -- Gravity field of the Moon -- Magnetic field of the Moon -- Surface topography of the Moon -- Geology and geomorphology of the Moon – a necessary introduction -- Geophysics of the Moon – a necessary introduction -- Atlas of the Moon -- Limits and possibilities of interpretation.
    Abstract: This book presents gravity aspects (gravity disturbance, Marussi tensor, two gravity invariants, their certain ratio, the strike angles, and the virtual deformations) which are computed and evaluated for the Moon, using the recent static global gravity field model (GRGM1200A) to degree and order of 600 in spherical harmonic expansion. The magnetic anomaly model and surface topography (from the LOLA mission) are added. Results are shown for the whole Moon, for its segments around the Moon and as zooms for selected impact craters, maria and catenae; they are shortly interpreted and opened for further selenologic applications. The book contains information about the geology of the Moon, together with basic information about the magnetic field, mapping and topography models.
    Type of Medium: Online Resource
    Pages: XV, 263 p. 306 illus., 303 illus. in color. , online resource.
    Edition: 1st ed. 2022.
    ISBN: 9783031088674
    Series Statement: Springer Geophysics,
    DDC: 550
    Language: English
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  • 2
    Call number: 21/STR 00/22
    In: Scientific technical report
    Type of Medium: GFZ publications
    Pages: 44 S.
    Series Statement: Scientific technical report / Geoforschungszentrum Potsdam 00/22
    Classification:
    Geodetic Measurement Systems
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Earth, moon and planets 57 (1992), S. 123-138 
    ISSN: 1573-0794
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The correlation between the undulations of the equipotential and topography surface of Venus have been investigated over 16 meridional sections as well as, in the global scale. The correlation is, in general high. However, the figure parameters of the ellipsoids best fitting the surface in question differ significantly. The global features like figures of the best-fitting ellipsoids are mutually strange.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 15 (1971), S. 241-245 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Notes: Резюме Исnользовaн неmрa¶rt;uцuонныŭ сnособ выво¶rt;a основных формул мamемamuческоŭгео¶rt;езuu ¶rt;ля эллunсa, эллunсоu¶rt;a врaщенuя u mрехосного эллunсоu¶rt;a — uменно nрuмененa оnорнaя функцuя выnуклоŭ фuгуры, m. е. nоняmuе, вве¶rt;енное в мamемamuку Мuнковскuм.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 29 (1985), S. 319-325 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Description / Table of Contents: Summary The computation of the secular variation of the inclination and eccentricity of the Moon's orbit due to tidal forces is revised. Also the effect of the Earth's ellipticity, which amounts to 10−6 to 10−5 of the value for the spherical earth, is estimated and found to be negligible. The results agree well with the computations of Kaula [7], as opposed to MacDonald's results [8] which display an order-of-magnitude difference in the variation of the eccentricity, apparently due to a printing error. Finally, solutions are presented for various values of the dissipation factor.
    Notes: Резюме Пересмamрuвaюmся вычuсленuя вековых uзмененuŭ нaклонa u эксценmрuцumеma лунноŭ орбumы, вызвaнных nрuлuвнымu сuлaмu. Кроме mо о nрове¶rt;енa оценкa влuянuя сжamuя Землu; эmо влuянuе сосmaвляеm оm 10−5 ¶rt;о 10−6 знaченuя ¶rt;ля шaрообрaзноŭ Землu u сле¶rt;овamельно nренебрежuмо. Резульmamы хорошо со лaсуюmся с вычuсленuямu Кaулa [7], в оmлuчuе оm резульmamов МaкДонaль¶rt;a [8], ¶rt;е рaзнuцa нa nоря¶rt;ок в uзмененuu эксценmрuцumеma очевu¶rt;но вызвaнa оnечamкоŭ. Нaконец ¶rt;aно решенuе ¶rt;ля рaзных знaченuŭ фaкmорa ¶rt;uссunaцuu.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 30 (1986), S. 112-112 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 36 (1992), S. 101-108 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Description / Table of Contents: Резюме По ¶rt;aнным сnуmнuковоŭ aльmuмеmрuu вычuслен мaсщmaбныŭ фaкmор еоnоmенцuaлa R 0 =GM/W 0 =(6 363 672,5±0,3) m u/uлu знaченuе еоnоmенцuaлa нa nоверхносmu еоu¶rt;a W 0 =(62 636 256,5±3) m2 s−2. Оmмечено, чmо R 0 u/uлu W 0 не зaвuсum оm nосmоянноŭ чaсmu зонaльно о членa nрuлuвных ¶rt;еформaцuŭ nоверхносmu W=W 0 .
    Notes: Summary The geopotential scale factor R 0 =GM/W 0 has been determined on the basis of satellite altimetry as R 0=(6 363 672·5±0·3) m and/or the geopotential value on the geoid W 0 =(62 636 256·5±3) m 2 s −2 . It has been stated that R 0 and/or W 0 is independent of the tidal distortion of surface W=W 0 due to the zero frequency tide.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 36 (1992), S. 302-306 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Notes: Summary Oceanography, seismology, gravimetry, lunar laser ranging (LLR) and satellite observations yield various values of the amplitude of the phase lag of body (solid) tides. These results are discussed, the probable value of δ is lower than 0.3 deg, but a sufficiently accurate value is not yet known.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 36 (1992), S. 297-301 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Notes: Summary The Banach theorem is applied to the Lagrange planetary equation for the semimajor axis of a geostationary satellite orbit to estimate the stability of near-geostationary satellite orbits. To achieve a graveyard (disposal) orbit, which will not interfere (=cross) the “initial” geostationary orbit, the geostationary semi-major axis ag have to be increased at least by 50 km. Numerical results for a variety of graveyard orbits show that the increase of ag by about 100 km will yield “sufficiently stable” orbits (accounting for the Earth's gravitational perturbations only) during the next 150 years.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Studia geophysica et geodaetica 37 (1993), S. 232-232 
    ISSN: 1573-1626
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Type of Medium: Electronic Resource
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