Julian Rogger
@julrogger.bsky.social
Postdoc at ETH Zurich on paleoclimate and ecosystem dynamics 🌳🌎 Hyperthermals, mass extinctions and long-term climate regulation.
Hi! If there is space, would be great if you could add me to this! :)
November 18, 2024 at 8:05 PM
Hi! If there is space, would be great if you could add me to this! :)
Hi there! If there is space, would be great if you could add me to this! :)
November 18, 2024 at 5:13 PM
Hi there! If there is space, would be great if you could add me to this! :)
Would be great if you could add me to this!
November 18, 2024 at 5:08 PM
Would be great if you could add me to this!
Would be great if you could add me to this!
November 18, 2024 at 5:07 PM
Would be great if you could add me to this!
A loss of vegetation can cause a super severe and long-lasting hyperthermal, like after the Permian-Triassic mass extinctiomn. And an incomplete recovery could even cause a shift into a warmer climate steady state!
August 9, 2024 at 3:15 PM
A loss of vegetation can cause a super severe and long-lasting hyperthermal, like after the Permian-Triassic mass extinctiomn. And an incomplete recovery could even cause a shift into a warmer climate steady state!
Applying an eco-evolutionary vegetation and carbon cycle model to different Phanerozoic LIPs, we find that the capacity of vegetation to adapt through evolution or to disperse in a specific paleogeography can result in a large range of possible climate trajectories!
August 9, 2024 at 3:14 PM
Applying an eco-evolutionary vegetation and carbon cycle model to different Phanerozoic LIPs, we find that the capacity of vegetation to adapt through evolution or to disperse in a specific paleogeography can result in a large range of possible climate trajectories!