David Rounce
@davidrounce.bsky.social
Assistant Professor at Carnegie Mellon University. Glaciers, Sea-Level Rise, Climate Adaptation and Mitigation, Compound Hazards, Water Resources
The study also introduces a new phenomenon referred to as "trough water", where glacier regrowth after the period of overshoot will actually reduce water availability for decades to centuries. This trough water occurs in approximately half of the glacier basins that were investigated.
May 28, 2025 at 3:22 PM
The study also introduces a new phenomenon referred to as "trough water", where glacier regrowth after the period of overshoot will actually reduce water availability for decades to centuries. This trough water occurs in approximately half of the glacier basins that were investigated.