Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Maria Zeitz"'
Autor:
Nico Bauer, David P Keller, Julius Garbe, Kristine Karstens, Franziska Piontek, Werner von Bloh, Wim Thiery, Maria Zeitz, Matthias Mengel, Jessica Strefler, Kirsten Thonicke, Ricarda Winkelmann
Publikováno v:
Environmental Research Letters, Vol 18, Iss 8, p 089501 (2023)
Externí odkaz:
https://doaj.org/article/872d804184fc4c94a20f3b8c86a1762e
Autor:
Nico Bauer, David P Keller, Julius Garbe, Kristine Karstens, Franziska Piontek, Werner von Bloh, Wim Thiery, Maria Zeitz, Matthias Mengel, Jessica Strefler, Kirsten Thonicke, Ricarda Winkelmann
Publikováno v:
Environmental Research Letters, Vol 18, Iss 5, p 054015 (2023)
Temperature targets of the Paris Agreement limit global net cumulative emissions to very tight carbon budgets. The possibility to overshoot the budget and offset near-term excess emissions by net-negative emissions is considered economically attracti
Externí odkaz:
https://doaj.org/article/4173fda6f3084526a8b1c2c9524487e9
Publikováno v:
The Cryosphere, Vol 15, Pp 5739-5764 (2021)
Surface melting of the Greenland Ice Sheet contributes a large amount to current and future sea-level rise. Increased surface melt, algae growth, debris, and dust deposition lower the reflectivity of the ice surface and thereby increase melt rates: t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c87219b74ce2467d5c30c43b658226e3
https://doi.org/10.5194/tc-15-5739-2021
https://doi.org/10.5194/tc-15-5739-2021
Interacting feedbacks play an important role in governing the stability of the Greenland Ice Sheet under global warming. Here we study the interaction between the positive melt-elevation feedback and the negative feedback from glacial isostatic adjus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e4cfaf569875779658589947d8e0be33
https://doi.org/10.5194/egusphere-egu22-9968
https://doi.org/10.5194/egusphere-egu22-9968
With a volume of 58 m sea-level equivalent, the Antarctic Ice Sheet represents the largest potential source of future sea-level rise under global warming. While the ice sheet gains mass through snowfall at the surface, it loses mass through dynamic d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::857af2b5c78a107038bdd1d5414fc805
https://doi.org/10.5194/egusphere-egu22-10008
https://doi.org/10.5194/egusphere-egu22-10008