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Orbital, Latitudinal, and Diurnal Variations in Meteoroid Influx, Atmospheric Ablation and Ionization, and Micrometeorite Accretion at Venus

  • Authors: Juan Diego Carrillo-Sánchez, Diego Janches, John M. C. Plane, Petr Pokorný

Juan Diego Carrillo-Sánchez et al 2026 The Planetary Science Journal 7 .

  • Provider: AAS Journals

Caption: Figure 10.

Orbital variability of the total injection rates, expressed in atoms m−3 s−1, of ablated Fe estimated by the CABMOD–MIF model as a function of the height and Venusian latitude for the most relevant orbital positions: the first crossing of the ecliptic plane (panel (a), LS = 18°), the minimum vertical distance from the ecliptic plane from the first crossing of the ecliptic plane (panel (b), LS = 108°), the second crossing of the ecliptic plane (panel (c), LS = 108°), and perihelion (panel (d), LS = 254°). An animation of the ablation rates of CO2, Na, Fe, and Al as a function of altitude and latitude is available; the animation cycles through all solar longitudes, starting from aphelion LS = 73°, going to LS = 0°, and then to LS = 73°.

(An animation of this figure is available in the online article.)

(An animation of this figure is available.)

The video/animation of this figure is available in the online journal.

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