Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Jesse Velay-Vitow"'
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-10 (2024)
Abstract During the most recent deglaciation, the upwards trend of warmer Northern Hemisphere (NH) temperatures was punctuated by a rapid and intense return to glacial conditions: the Younger Dryas (YD). The end of this event marks the beginning of t
Externí odkaz:
https://doaj.org/article/8507082095e64158bb7e46bc069befdb
Publikováno v:
Quaternary Research. 101:13-25
The ocean floor sedimentological signature of Heinrich event 3 (H3) is markedly different from that of other Heinrich events that are known to have originated in Hudson Strait. It has therefore been suggested that the H3 contribution to iceberg flux
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f0742aeee6ece54136b1a700deeb817
https://doi.org/10.1017/qua.2020.84
https://doi.org/10.1017/qua.2020.84
Autor:
Richard Peltier, Tanghua Li, Gordan Stuhnne, Jesse Velay-Vitow, Matteo Vacchi, Simon Englehart, Benjamin Horton
A challenge to understanding Late Quaternary glaciation history is the mechanism(s) responsible for the asymmetry in an individual glaciation cycle between the slow pace of glaciation and the more rapid pace of deglaciation (e.g., Broecker and Van Do
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c7117bfaeef74d6491d1dddc4ee3ee1
https://doi.org/10.5194/egusphere-egu22-1343
https://doi.org/10.5194/egusphere-egu22-1343
Throughout the Quaternary, northern Africa has experienced recurring periods of intensified precipitation, known as African Humid Periods. The most recent such period began after the termination of the Younger Dryas (YD), which was a dramatic reversi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::123f0be98e8c54f9e6a118af3cedf9ce
https://doi.org/10.5194/egusphere-egu22-2987
https://doi.org/10.5194/egusphere-egu22-2987
By far the most prescient insights into the interior structure of the planet have been provided on the basis of elastic wave seismology. Analysis of the travel times of shear or compression wave phases excited by individual earthquakes, or through an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8a43d4535b16e1b91c476c69918b5d9b
https://hdl.handle.net/10356/168866
https://hdl.handle.net/10356/168866
Autor:
W. R. Peltier, Jesse Velay-Vitow
Although currently microtidal, the Arctic Ocean is known to have been megatidal at Last Glacial Maximum (LGM) due to the Arctic Ocean basin being nearly entirely enclosed, with only Fram Strait connecting it to the global ocean. This allowed for the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6ea6d843f016a0ba9da44e7ca02bd768
https://doi.org/10.5194/egusphere-egu21-29
https://doi.org/10.5194/egusphere-egu21-29
Autor:
W. Richard Peltier, Jesse Velay-Vitow
Publikováno v:
Geophysical Research Letters. 47
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::711a3589266aa99f182d18972845f4d7
https://doi.org/10.1029/2020gl089870
https://doi.org/10.1029/2020gl089870
With the recent demonstration that millennial timescale Dansgaard-Oeschger oscillations of MIS 3 are predictable in a modern coupled climate model following a Heinrich event-like reduction of AMOC strength (eg. Peltier and Vettoretti, 2014), the stag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2f2a6acea3c8e146bd92fc97b64c81e5
https://doi.org/10.5194/egusphere-egu2020-1955
https://doi.org/10.5194/egusphere-egu2020-1955
Autor:
Jesse Velay-Vitow, Richard Peltier
It has been established recently (Velay-Vitow, Peltier and Stuhne JGR-Oceans 2019) that a high amplitude M2 tide may have triggered and contributed to the forcing of the rapid deglaciations of the Hudson Strait ice stream, commonly referred to as Hei
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b47e4ff49bbbefeb9ea91233ca5b36db
https://doi.org/10.5194/egusphere-egu2020-1808
https://doi.org/10.5194/egusphere-egu2020-1808