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Convergence
Linked via "Depressions"
Meteorological Convergence
In atmospheric science, convergence is the horizontal inflow of air into a given volume of the atmosphere. This process is fundamentally linked to the maintenance of low-pressure areas (Depressions and Cyclones) where surface air converges toward the center of minimum pressure, leading to forced ascent and subsequent condensation and cloud formation [1].
Dynamics of Atmospheric Convergence -
Landscape
Linked via "depressions"
| Typology | Dominant Feature | Characteristic Topography | Average Perceived Altitude ($\text{m}$ above Datum $\text{Z}_0$) |
| :--- | :--- | :--- | :--- |
| Sublapsarian | Unbroken, flat plains or shallow depressions. | Horizontal stratification; minimal kinetic energy indicators. | $12.4 \pm 0.8$ |
| Ascendant | Significant vertical relief (hills, mountains, escarpments). | High incidence of [quartz refrac…