| Term | Definition | Contributor | Modified |
|---|---|---|---|
| Leaves, Color of | No definition provided | Christopher Rauch | 2023.12.01 |
| Leaves--Morphology | No definition provided | Christopher Rauch | 2023.12.01 |
| Leaves--Photography | No definition provided | Christopher Rauch | 2023.12.01 |
| Lebbek tree | No definition provided | Christopher Rauch | 2023.12.01 |
| Le Bon’s rays | No definition provided | Christopher Rauch | 2023.12.01 |
| Le Boulengé chronograph | No definition provided | Christopher Rauch | 2023.12.01 |
| Lecanium corni | No definition provided | Christopher Rauch | 2023.12.01 |
| Lecanium nigrofasciatum | No definition provided | Christopher Rauch | 2023.12.01 |
| Lechatelierite | No definition provided | Ryan McGranaghan | 2023.04.16 |
| Lecithin | No definition provided | Christopher Rauch | 2023.12.01 |
| Lecontite | No definition provided | Ryan McGranaghan | 2023.04.16 |
| Lecturers | No definition provided | Christopher Rauch | 2023.12.01 |
| Lectures and lecturing | No definition provided | Christopher Rauch | 2023.12.01 |
| Lectures’and lecturing | No definition provided | Christopher Rauch | 2023.12.01 |
| Lecythi | No definition provided | Christopher Rauch | 2023.12.01 |
| Leda (Minor planet) | No definition provided | Christopher Rauch | 2023.12.01 |
| lee | No definition provided | Ryan McGranaghan | 2023.04.16 |
| Lee | Side of a slope that is opposite to the direction of flow of ice, wind, or water. Opposite of stoss. | GCW Glossary | 2023.03.27 |
| Leeches | No definition provided | Christopher Rauch | 2023.12.01 |
| leeside convergence | Region of convergence, often a line, downwind of a mountain or mountain ridge during fair-weather daytime conditions that are favorable for the formation of thermally forced upslope flow and deep conv ective mixing. Convergence forms between upslope (or sometimes light and variable) flow at lower elevations of the lee slopes and downslope flow at higher elevations, which results from the downward convective mixing of ambient momentum from the flow above ridgetops. With moist upslope flow and favorable conditions, updrafts produced by the convergence can lead to mountain cumulus formation, or trigger thunderstorm or severe weather activity. | Ryan McGranaghan | 2023.04.16 |