Paul Maidowski
@ppmv.bsky.social
Language, systems analysis, climate policy, CCS. Fletcher School/Fulbright d|e|f|i|中
Reposted by Paul Maidowski
In this and following posts I summarise some key findings.
Firstly, the last remaining area of ice shelf in front of Thwaites Glacier, the Thwaites Eastern Ice Shelf, is nearing break-up.
doi.org/10.1017/jog....
Firstly, the last remaining area of ice shelf in front of Thwaites Glacier, the Thwaites Eastern Ice Shelf, is nearing break-up.
doi.org/10.1017/jog....
October 26, 2025 at 9:44 PM
In this and following posts I summarise some key findings.
Firstly, the last remaining area of ice shelf in front of Thwaites Glacier, the Thwaites Eastern Ice Shelf, is nearing break-up.
doi.org/10.1017/jog....
Firstly, the last remaining area of ice shelf in front of Thwaites Glacier, the Thwaites Eastern Ice Shelf, is nearing break-up.
doi.org/10.1017/jog....
Nein, wäre es nicht. Fossile Brennstoffe bringen neues Kohlenstoff in den globalen CO2-Kreislauf ein, während Holz beim Verrotten (!) oder Verbrennen nur das freisetzt, was es vorher aufgenommen hatte. Es ändert am globalen Kreislauf nichts. Biodiversität & andere Aspekte hier außen vor.
October 30, 2025 at 8:48 AM
Nein, wäre es nicht. Fossile Brennstoffe bringen neues Kohlenstoff in den globalen CO2-Kreislauf ein, während Holz beim Verrotten (!) oder Verbrennen nur das freisetzt, was es vorher aufgenommen hatte. Es ändert am globalen Kreislauf nichts. Biodiversität & andere Aspekte hier außen vor.
“Such moderate thresholds for permafrost absence highlight the climate sensitivity of North Greenland.”
October 30, 2025 at 8:05 AM
“Such moderate thresholds for permafrost absence highlight the climate sensitivity of North Greenland.”