Name
Abstract | ||
|---|---|---|
The Venusian geological features are poorly gravity-resolved, and the state of the core is not well constrained, preventing an understanding of Venus' cooling history. The EnVision candidate mission to the ESA's Cosmic Vision Programme consists of a low-altitude orbiter to investigate geological and atmospheric processes. The gravity experiment aboard this mission aims to determine Venus' geophysical parameters to fully characterize its internal structure. By analyzing the radio-tracking data that will be acquired through daily operations over six Venusian days (four Earth's years), we will derive a highly accurate gravity field (spatial resolution better than similar to 170 km), allowing detection of lateral variations of the lithosphere and crust properties beneath most of the geological features. The expected 0.3% error on the Love number k(2), 0.1 degrees error on the tidal phase lag and 1.4% error on the moment of inertia are fundamental to constrain the core size and state as well as the mantle viscosity. |
Year | DOI | Venue |
|---|---|---|
2021 | 10.3390/rs13091624 | REMOTE SENSING |
Keywords | DocType | Volume |
planetary interior structure, gravity field determination, deep space mission | Journal | 13 |
Issue | Citations | PageRank |
9 | 0 | 0.34 |
References | Authors | |
0 | 4 | |
Name | Order | Citations | PageRank |
|---|---|---|---|
| Pascal Rosenblatt | 1 | 0 | 0.34 |
| Caroline Dumoulin | 2 | 0 | 0.34 |
| Jean-Charles Marty | 3 | 0 | 0.34 |
| Antonio Genova | 4 | 0 | 0.68 |