Abstract
In the context of the regional gravity field modelling, the smoothing effect of the topographical correction on the high-frequency part of the gravity signal is well documented. In this study, the effect of the long-wavelength topographic correction on the low-degree Earth's gravity potential and attraction is investigated. For this purpose, the Earth's gravity field and the topography-corrected gravity field are compared for various spectral resolutions. The topography-corrected gravity field is obtained from the low-degree Earth's gravity field after subtracting the long-wavelength gravitational field generated by the topography. The Earth's gravity field is computed from a global geopotential model (GGM). The gravitational field generated by the topography is modelled from a global elevation model (GEM), adopting the constant topographical mass-density distribution.
| Original language | English |
|---|---|
| Title of host publication | Gravity, Geoid and Earth Observation - IAG Commission 2 |
| Subtitle of host publication | Gravity Field |
| Pages | 355-360 |
| Number of pages | 6 |
| Volume | 135 |
| DOIs | |
| Publication status | Published - 1 Dec 2010 |
| Externally published | Yes |
| Event | IAG International Symposium on "Gravity, Geoid and Earth Observation 2008" - Chania, Crete, Germany Duration: 23 Jun 2008 → 27 Jun 2008 |
Conference
| Conference | IAG International Symposium on "Gravity, Geoid and Earth Observation 2008" |
|---|---|
| Country/Territory | Germany |
| City | Chania, Crete |
| Period | 23/06/08 → 27/06/08 |
Keywords
- Gravity field
- Topographical correction
ASJC Scopus subject areas
- Computers in Earth Sciences
- Geophysics
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