Jiachen Liu
@jiachenliu.bsky.social
PhD candidate at Peking University (she/her) | working on atmospheres on Earth, terrestrial planets, and sub-Neptunes! https://jiachenliu-atmos.github.io/
The detailed analysis of chemical structures will be presented in Part II, which is coming soon. Stay tuned!
July 1, 2025 at 8:28 AM
The detailed analysis of chemical structures will be presented in Part II, which is coming soon. Stay tuned!
In addition, we find that the surface inversion (SIV, surface cooler than its adjacent air) is also a distinct phenomenon in the hothouse climate.
This schematic shows how these two kinds of inversions form.
This schematic shows how these two kinds of inversions form.
April 8, 2025 at 8:17 AM
In addition, we find that the surface inversion (SIV, surface cooler than its adjacent air) is also a distinct phenomenon in the hothouse climate.
This schematic shows how these two kinds of inversions form.
This schematic shows how these two kinds of inversions form.
Near-surface atmospheric (NAIV) inversion is a phenomenon reported in previous hothouse climate simulation papers (e.g., Wordsworth & Pierrehumbert, 2013; Wolf & Toon, 2015), but its formation mechanisms remain unclear. In this paper we employ a hierarchy of models to investigate its mechanisms.
April 8, 2025 at 8:10 AM
Near-surface atmospheric (NAIV) inversion is a phenomenon reported in previous hothouse climate simulation papers (e.g., Wordsworth & Pierrehumbert, 2013; Wolf & Toon, 2015), but its formation mechanisms remain unclear. In this paper we employ a hierarchy of models to investigate its mechanisms.
The hothouse climate may occur following a Snowball Earth event in Earth’s history, on a future Earth under the brightening Sun, or on terrestrial planets near the inner edge of the habitable zone.
April 8, 2025 at 8:09 AM
The hothouse climate may occur following a Snowball Earth event in Earth’s history, on a future Earth under the brightening Sun, or on terrestrial planets near the inner edge of the habitable zone.