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f | 1 | { | f | 1 | { |
2 | "author": "Christian Voigt, Heiner Denker", | 2 | "author": "Christian Voigt, Heiner Denker", | ||
3 | "author_email": "christian.voigt@gfz-potsdam.de", | 3 | "author_email": "christian.voigt@gfz-potsdam.de", | ||
4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | 4 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | ||
5 | "doi": "10.25835/0092586", | 5 | "doi": "10.25835/0092586", | ||
6 | "doi_date_published": "2018-08-16", | 6 | "doi_date_published": "2018-08-16", | ||
7 | "doi_publisher": "LUIS", | 7 | "doi_publisher": "LUIS", | ||
8 | "doi_status": "true", | 8 | "doi_status": "true", | ||
9 | "domain": "https://data.uni-hannover.de", | 9 | "domain": "https://data.uni-hannover.de", | ||
10 | "groups": [], | 10 | "groups": [], | ||
11 | "have_copyright": "Yes", | 11 | "have_copyright": "Yes", | ||
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13 | "isopen": false, | 13 | "isopen": false, | ||
14 | "license_id": "CC-BY-NC-3.0", | 14 | "license_id": "CC-BY-NC-3.0", | ||
15 | "license_title": "CC-BY-NC-3.0", | 15 | "license_title": "CC-BY-NC-3.0", | ||
16 | "maintainer": "Heiner Denker", | 16 | "maintainer": "Heiner Denker", | ||
17 | "maintainer_email": "denker@ife.uni-hannover.de", | 17 | "maintainer_email": "denker@ife.uni-hannover.de", | ||
18 | "metadata_created": "2021-10-14T10:15:53.041444", | 18 | "metadata_created": "2021-10-14T10:15:53.041444", | ||
n | 19 | "metadata_modified": "2021-10-14T10:15:53.041449", | n | 19 | "metadata_modified": "2023-01-12T13:14:08.013820", |
20 | "name": | 20 | "name": | ||
21 | etic-vertical-deflections-for-the-validation-of-gravity-field-models", | 21 | etic-vertical-deflections-for-the-validation-of-gravity-field-models", | ||
22 | "notes": "For high resolution gravity field modelling in Germany, | 22 | "notes": "For high resolution gravity field modelling in Germany, | ||
23 | global geopotential models are combined with terrestrial gravity field | 23 | global geopotential models are combined with terrestrial gravity field | ||
24 | data and topographic information from high resolution digital terrain | 24 | data and topographic information from high resolution digital terrain | ||
25 | models. In this context, it is vitally important to assess the quality | 25 | models. In this context, it is vitally important to assess the quality | ||
26 | of recent global geopotential models from GOCE and other satellite | 26 | of recent global geopotential models from GOCE and other satellite | ||
27 | missions, GPS-levelling data as well as high resolution gravimetric | 27 | missions, GPS-levelling data as well as high resolution gravimetric | ||
28 | quasigeoid models with an aspired accuracy of 1 cm. Within these | 28 | quasigeoid models with an aspired accuracy of 1 cm. Within these | ||
29 | analyses, the differences of the existing gravity field data sets have | 29 | analyses, the differences of the existing gravity field data sets have | ||
30 | to be enlightened.\r\n\r\nFor this purpose, a unique data set of | 30 | to be enlightened.\r\n\r\nFor this purpose, a unique data set of | ||
31 | astrogeodetic vertical deflections was observed in the period from | 31 | astrogeodetic vertical deflections was observed in the period from | ||
32 | 2006 to 2010 with the zenith camera system TZK2-D. The observations | 32 | 2006 to 2010 with the zenith camera system TZK2-D. The observations | ||
33 | were carried out on 394 stations in total along two profiles in | 33 | were carried out on 394 stations in total along two profiles in | ||
34 | north-south and west-east direction with a spacing of 3-4 km between | 34 | north-south and west-east direction with a spacing of 3-4 km between | ||
35 | adjacent stations and total lengths of approx. 600 km. The method of | 35 | adjacent stations and total lengths of approx. 600 km. The method of | ||
36 | astronomical-topographic levelling was used to compute quasigeoid | 36 | astronomical-topographic levelling was used to compute quasigeoid | ||
37 | heights. With regard to the aspired accuracy of 1 cm/100 km, | 37 | heights. With regard to the aspired accuracy of 1 cm/100 km, | ||
38 | systematic effects within the astrogeodetic gravity field modelling | 38 | systematic effects within the astrogeodetic gravity field modelling | ||
39 | had to be analysed, i.e. particularly, the effects of the underlying | 39 | had to be analysed, i.e. particularly, the effects of the underlying | ||
40 | reference frames as well as temporal variations of the observations. | 40 | reference frames as well as temporal variations of the observations. | ||
41 | Commonly used approximations within astrogeodetic gravity field | 41 | Commonly used approximations within astrogeodetic gravity field | ||
42 | modelling were analysed using rigorous formulas.\r\n\r\nConsidering | 42 | modelling were analysed using rigorous formulas.\r\n\r\nConsidering | ||
43 | the identified systematic effects, the comparison between the | 43 | the identified systematic effects, the comparison between the | ||
44 | astrogeodetic vertical deflections and corresponding values from the | 44 | astrogeodetic vertical deflections and corresponding values from the | ||
45 | gravimetric quasigeoid model EGG2008 (Denker, 2013) reveals the stated | 45 | gravimetric quasigeoid model EGG2008 (Denker, 2013) reveals the stated | ||
46 | accuracy of the astrogeodetic vertical deflections of 0.08\". By means | 46 | accuracy of the astrogeodetic vertical deflections of 0.08\". By means | ||
47 | of comparisons with the astrogeodetic data, the accuracy of vertical | 47 | of comparisons with the astrogeodetic data, the accuracy of vertical | ||
48 | deflections from global geopotential models is estimated to be between | 48 | deflections from global geopotential models is estimated to be between | ||
49 | 0.18\" and 0.40\" for the ultra-high resolution model EGM2008 and | 49 | 0.18\" and 0.40\" for the ultra-high resolution model EGM2008 and | ||
50 | 0.20\" up to a spatial resolution of 100 km for the recent GOCE models | 50 | 0.20\" up to a spatial resolution of 100 km for the recent GOCE models | ||
51 | of the third generation, being fully compatible with the relevant | 51 | of the third generation, being fully compatible with the relevant | ||
52 | error estimates of the models. The comparisons between the height | 52 | error estimates of the models. The comparisons between the height | ||
53 | anomalies from the astronomical-topographic levellings and | 53 | anomalies from the astronomical-topographic levellings and | ||
54 | GPS-levelling data as well as high resolution gravimetric quasigeoid | 54 | GPS-levelling data as well as high resolution gravimetric quasigeoid | ||
55 | models in Germany show an agreement of 1.2 cm to 2.9 cm RMS. The short | 55 | models in Germany show an agreement of 1.2 cm to 2.9 cm RMS. The short | ||
56 | wavelength differences can be assigned to the ellipsoidal heights of | 56 | wavelength differences can be assigned to the ellipsoidal heights of | ||
57 | the GPS-levelling data, while the analyses of the long wavelength | 57 | the GPS-levelling data, while the analyses of the long wavelength | ||
58 | differences of a few centimetres over several 100 km is very complex, | 58 | differences of a few centimetres over several 100 km is very complex, | ||
59 | as the differences include uncertainties of all involved data sets. In | 59 | as the differences include uncertainties of all involved data sets. In | ||
60 | this context, the astrogeodetic quasigeoid solutions provide a | 60 | this context, the astrogeodetic quasigeoid solutions provide a | ||
61 | valuable additional control. On the whole, the results reveal the high | 61 | valuable additional control. On the whole, the results reveal the high | ||
62 | quality of the existing gravity field data sets in Germany, including | 62 | quality of the existing gravity field data sets in Germany, including | ||
63 | the astrogeodetic data set determined by this research.\r\n\r\nThe | 63 | the astrogeodetic data set determined by this research.\r\n\r\nThe | ||
64 | astrodeodetic data set is part of Voigt (2013) and as such compiled in | 64 | astrodeodetic data set is part of Voigt (2013) and as such compiled in | ||
65 | the appendix of this thesis. The digital archive includes the | 65 | the appendix of this thesis. The digital archive includes the | ||
66 | astrogeodetic data along two profiles (versions 2.0) in north-south | 66 | astrogeodetic data along two profiles (versions 2.0) in north-south | ||
67 | and west-east direction (as ASCII text files), i.e.\r\n\r\n1. The | 67 | and west-east direction (as ASCII text files), i.e.\r\n\r\n1. The | ||
68 | files \"ns-2.0-obs.txt\" and \"wo-2.0-obs.txt\" include the original | 68 | files \"ns-2.0-obs.txt\" and \"wo-2.0-obs.txt\" include the original | ||
69 | astronomical and ellipsoidal observations. The ellipsoidal coordinates | 69 | astronomical and ellipsoidal observations. The ellipsoidal coordinates | ||
70 | refer to ETRS89, whereas the astronomical coordinates refer to | 70 | refer to ETRS89, whereas the astronomical coordinates refer to | ||
71 | ITRF2005 and the corresponding epochs.\r\n\r\n2. The files | 71 | ITRF2005 and the corresponding epochs.\r\n\r\n2. The files | ||
72 | \"ns-2.0-red.txt\" and \"wo-2.0-red.txt\" include the reduced | 72 | \"ns-2.0-red.txt\" and \"wo-2.0-red.txt\" include the reduced | ||
73 | astronomical and ellipsoidal coordinates according to Figure 5.1 of | 73 | astronomical and ellipsoidal coordinates according to Figure 5.1 of | ||
74 | Voigt (2013). Both ellipsoidal and astronomical coordinates refer to | 74 | Voigt (2013). Both ellipsoidal and astronomical coordinates refer to | ||
75 | ETRS89 and the mean Earth's crust with the astronomical coordinates | 75 | ETRS89 and the mean Earth's crust with the astronomical coordinates | ||
76 | additionally referring to the zero-tide potential. This allows for the | 76 | additionally referring to the zero-tide potential. This allows for the | ||
77 | computation of the vertical deflections according to Helmert either by | 77 | computation of the vertical deflections according to Helmert either by | ||
78 | the widely used linear approximation or according to (3.43) of Voigt | 78 | the widely used linear approximation or according to (3.43) of Voigt | ||
79 | (2013) without losing accuracy. For the comparison with vertical | 79 | (2013) without losing accuracy. For the comparison with vertical | ||
80 | deflections derived from the interpolation of quasigeoid models | 80 | deflections derived from the interpolation of quasigeoid models | ||
81 | especially in rough terrain, the terrain inclination should be taken | 81 | especially in rough terrain, the terrain inclination should be taken | ||
82 | into account. For further details see section 7.1 of Voigt | 82 | into account. For further details see section 7.1 of Voigt | ||
83 | (2013).\r\n\r\n3. The files \"ns-2.0-zeta.txt\" and | 83 | (2013).\r\n\r\n3. The files \"ns-2.0-zeta.txt\" and | ||
84 | \"wo-2.0-zeta.txt\" include the astrogeodetic quasigeoid heights | 84 | \"wo-2.0-zeta.txt\" include the astrogeodetic quasigeoid heights | ||
85 | relative to the first station of each profile. These are computed from | 85 | relative to the first station of each profile. These are computed from | ||
86 | the reduced vertical deflections (\"ns-2.0-red.txt\" and | 86 | the reduced vertical deflections (\"ns-2.0-red.txt\" and | ||
87 | \"wo-2.0-red.txt\") by astronomical-topographic levellings. The | 87 | \"wo-2.0-red.txt\") by astronomical-topographic levellings. The | ||
88 | quasigeoid heights refer to the zero-tide potential.\r\n\r\nThis work | 88 | quasigeoid heights refer to the zero-tide potential.\r\n\r\nThis work | ||
89 | was carried out at the Institut f\u00fcr Erdmessung of the Leibniz | 89 | was carried out at the Institut f\u00fcr Erdmessung of the Leibniz | ||
90 | Universit\u00e4t Hannover within the framework of the project REAL | 90 | Universit\u00e4t Hannover within the framework of the project REAL | ||
91 | GOCE as part of the R&D-Programme GEOTECHNOLOGIEN, funded by the | 91 | GOCE as part of the R&D-Programme GEOTECHNOLOGIEN, funded by the | ||
92 | German Ministry of Education and Research (BMBF) and the German | 92 | German Ministry of Education and Research (BMBF) and the German | ||
93 | Research Foundation (DFG) through Grant (03G0726C).\r\n\r\n__Selected | 93 | Research Foundation (DFG) through Grant (03G0726C).\r\n\r\n__Selected | ||
94 | publications:__\r\n\r\n* Denker, H. (2013) Regional gravity field | 94 | publications:__\r\n\r\n* Denker, H. (2013) Regional gravity field | ||
95 | modeling: Theory and practical results. Monograph in: Xu G. (ed.), | 95 | modeling: Theory and practical results. Monograph in: Xu G. (ed.), | ||
96 | Sciences of Geodesy \u2013 II, Chapter 5: 185-291, Springer Verlag, | 96 | Sciences of Geodesy \u2013 II, Chapter 5: 185-291, Springer Verlag, | ||
97 | Berlin, Heidelberg, https://doi.org/10.1007/978-3-642-28000-9_5 | 97 | Berlin, Heidelberg, https://doi.org/10.1007/978-3-642-28000-9_5 | ||
98 | \r\n\r\n* Voigt, C. (2013) Astrogeod\u00e4tische Lotabweichungen zur | 98 | \r\n\r\n* Voigt, C. (2013) Astrogeod\u00e4tische Lotabweichungen zur | ||
99 | Validierung von Schwerefeldmodellen, PhD Thesis, Universit\u00e4t | 99 | Validierung von Schwerefeldmodellen, PhD Thesis, Universit\u00e4t | ||
100 | Hannover. Fachrichtung Geod\u00e4sie und Geoinformatik: | 100 | Hannover. Fachrichtung Geod\u00e4sie und Geoinformatik: | ||
101 | Wissenschaftliche Arbeiten der Fachrichtung Geod\u00e4sie und | 101 | Wissenschaftliche Arbeiten der Fachrichtung Geod\u00e4sie und | ||
102 | Geoinformatik der Leibniz Universit\u00e4t Hannover 305, Fachrichtung | 102 | Geoinformatik der Leibniz Universit\u00e4t Hannover 305, Fachrichtung | ||
103 | Geod\u00e4sie und Geoinformatik der Leibniz-Universit\u00e4t Hannover, | 103 | Geod\u00e4sie und Geoinformatik der Leibniz-Universit\u00e4t Hannover, | ||
104 | ww.dgk.badw.de/fileadmin/user_upload/Files/DGK/docs/c-702.pdf\r\n\r\n* | 104 | ww.dgk.badw.de/fileadmin/user_upload/Files/DGK/docs/c-702.pdf\r\n\r\n* | ||
105 | Voigt, C. and Denker, H. (2014) Regional Validation and Combination of | 105 | Voigt, C. and Denker, H. (2014) Regional Validation and Combination of | ||
106 | GOCE Gravity Field Models and Terrestrial Data. In: Flechtner, F., | 106 | GOCE Gravity Field Models and Terrestrial Data. In: Flechtner, F., | ||
107 | Sneeuw, N., Schuh, W. D.(Eds.), Observation of the System Earth from | 107 | Sneeuw, N., Schuh, W. D.(Eds.), Observation of the System Earth from | ||
108 | Space - CHAMP, GRACE, GOCE and Future Missions, GEOTECHNOLOGIEN | 108 | Space - CHAMP, GRACE, GOCE and Future Missions, GEOTECHNOLOGIEN | ||
109 | Science Report 20 (Advanced Technologies in Earth Sciences), Springer, | 109 | Science Report 20 (Advanced Technologies in Earth Sciences), Springer, | ||
110 | pp. 139-145, https://doi.org/10.1007/978-3-642-32135-1_18\r\n\r\n* | 110 | pp. 139-145, https://doi.org/10.1007/978-3-642-32135-1_18\r\n\r\n* | ||
111 | Voigt, C. and Denker, H. (2015) Validation of GOCE Gravity Field | 111 | Voigt, C. and Denker, H. (2015) Validation of GOCE Gravity Field | ||
112 | Models in Germany. Newton's Bulletin 5, | 112 | Models in Germany. Newton's Bulletin 5, | ||
113 | http://www.isgeoid.polimi.it/Newton/Newton_5/05_Voigt_37_48.pdf", | 113 | http://www.isgeoid.polimi.it/Newton/Newton_5/05_Voigt_37_48.pdf", | ||
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