Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Witold Bagniewski"'
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-15 (2023)
Abstract How often have past climates undergone abrupt transitions? While our understanding of millennial variability during the past 130,000 years is well established, with precise dates available, such information on previous climate cycles is limi
Externí odkaz:
https://doaj.org/article/68fbd655314b46b1832b1ff75e115daf
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-13 (2023)
Abstract The Earth’s climate has experienced numerous critical transitions during its history, which have often been accompanied by massive and rapid changes in the biosphere. Such transitions are evidenced in various proxy records covering differe
Externí odkaz:
https://doaj.org/article/4a9109ba99814b16b9b871c823499d23
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-18 (2023)
Abstract Tipping points (TPs) in Earth’s climate system have been the subject of increasing interest and concern in recent years, given the risk that anthropogenic forcing could cause abrupt, potentially irreversible, climate transitions. Paleoclim
Externí odkaz:
https://doaj.org/article/e0a010fcac6e4fa081b067e49d1fdd21
The Earth's climate has experienced numerous critical transitions during its history, which have often been accompanied by massive and rapid changes in the biosphere. Such transitions are evidenced in various proxy records covering different timescal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8411ec3019cd38064a4ba8c4902a8465
http://arxiv.org/abs/2212.06239
http://arxiv.org/abs/2212.06239
Paleoclimate proxy records contain abrupt transitions that may represent former instances of the climate system crossing a tipping point (TP). Properly identifying these TPs in the Earth’s past helps determine critical thresholds in present-day cli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::166b8266c6ebbde8ee8c553d220644ad
https://doi.org/10.5194/egusphere-egu22-12501
https://doi.org/10.5194/egusphere-egu22-12501
The Earth’s climate has experienced numerous abrupt and critical transitions during its long history. Such transitions are evidenced in precise, high-resolution records at different timescales. This type of evidence suggests the possibility of iden
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::157985dd98d14fce4fc7e8467134f994
https://doi.org/10.5194/egusphere-egu22-2396
https://doi.org/10.5194/egusphere-egu22-2396
Publikováno v:
Climate of the Past Discussions
Climate of the Past Discussions, European Geosciences Union (EGU), 2021
Climate of the Past Discussions, European Geosciences Union (EGU), 2021
Abrupt climate changes constitute a relatively new field of research, which addresses variations occurring in a relatively short time interval of tens to a hundred years. Such time scales do not correspond to the tens or hundreds of thousands of year
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c7e2801d271e77d200b90d86e7811708
https://hal-insu.archives-ouvertes.fr/insu-03319020
https://hal-insu.archives-ouvertes.fr/insu-03319020
Tipping points (TPs) in the Earth system have been studied with growing interest and concern in recent years due to the potential risk of anthropogenic forcing causing abrupt, and possibly irreversible, climate transitions. Paleoclimate records are e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2ac77816cc96e5e19ce3869b9920c144
https://doi.org/10.5194/egusphere-egu21-9968
https://doi.org/10.5194/egusphere-egu21-9968
Early evidence of abrupt transitions in Camp Century and Dye 3 Greenland ice cores (Dansgaard et al. 1982) has recently been reinforced by the identification of additional abrupt transitions in the NGRIP ice core (Rasmussen et al. 2014). These additi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f4917b4d63a84657578bcaf47c42e09f
https://doi.org/10.5194/egusphere-egu21-7857
https://doi.org/10.5194/egusphere-egu21-7857