Zobrazeno 1 - 10
of 59
pro vyhledávání: '"Takashi, Obase"'
Autor:
Yusuke Suganuma, Heitaro Kaneda, Martim Mas e Braga, Takeshige Ishiwa, Takushi Koyama, Jennifer C. Newall, Jun’ichi Okuno, Takashi Obase, Fuyuki Saito, Irina Rogozhina, Jane Lund Andersen, Moto Kawamata, Motohiro Hirabayashi, Nathaniel A. Lifton, Ola Fredin, Jonathan M. Harbor, Arjen P. Stroeven, Ayako Abe-Ouchi
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-11 (2022)
Regional sea-level highstand triggered rapid Holocene upstream thinning of the East Antarctic Ice Sheet in Dronning Maud Land, suggest ice sheet and crustal rebound model simulations constrained by cosmogenic nuclide chronometry.
Externí odkaz:
https://doaj.org/article/c160a9e904ac47c4b0ddfdff01e486a6
Mass loss of the Antarctic ice sheet until the year 3000 under a sustained late-21st-century climate
Publikováno v:
Journal of Glaciology, Vol 68, Pp 605-617 (2022)
Ice-sheet simulations of Antarctica extending to the year 3000 are analysed to investigate the long-term impacts of 21st-century warming. Climate projections are used as forcing until 2100 and afterwards no climate trend is applied. Fourteen experime
Externí odkaz:
https://doaj.org/article/166d45e509f6497cb69da9a958984a68
Autor:
Tristan Vadsaria, Sébastien Zaragosi, Gilles Ramstein, Jean-Claude Dutay, Laurent Li, Giuseppe Siani, Marie Revel, Takashi Obase, Ayako Abe-Ouchi
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-13 (2022)
Abstract Between the Last Glacial Maximum and the mid-Holocene, the Mediterranean Sea experienced major hydrological changes. The deposition of the last sapropel, S1, during the Early Holocene is a consequence of these changes. In order to cause anox
Externí odkaz:
https://doaj.org/article/01279c7f67a0471ea8a0d91e7ff9e262
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
Abstract There were significant differences between the last two deglaciations, particularly in Atlantic Meridional Overturning Circulation (AMOC) and Antarctic warming in the deglaciations and the following interglacials. Here, we present transient
Externí odkaz:
https://doaj.org/article/286a1302ba79481889866e07e0c4b563
Autor:
Tristan Vadsaria, Sébastien Zaragosi, Gilles Ramstein, Jean-Claude Dutay, Laurent Li, Giuseppe Siani, Marie Revel, Takashi Obase, Ayako Abe-Ouchi
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-2 (2023)
Externí odkaz:
https://doaj.org/article/ce9f666662fc45b0bc2cb339ed99b893
Autor:
Takashi Obase, Menviel, Laurie, Ayako Abe-Ouchi, Vadsaria, Tristan, Ivanovic, Ruza, Snoll, Brooke, Sherriff-Tadano, Sam, Valdes, Paul, Gregoire, Lauren, Kapsch, Marie-Luise, Mikolajewicz, Uwe, Bouttes, Nathaelle, Roche, Didier, Lhardy, Fanny, Chengfei He, Otto-Bliesner, Bette, Zhengyu Liu, Wing-Le Chan
Publikováno v:
Climate of the Past Discussions; 12/4/2023, p1-45, 45p
Publikováno v:
Climate of the Past Discussions; 11/13/2023, p1-26, 26p
Stable water isotopes in polar ice cores are widely used to reconstruct past temperature variations over several orbital climatic cycles. One way to calibrate the isotope-temperature relationship is to apply the present-day spatial relationship as a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ea04deb10e8d59d1eaed056c953f6d36
https://doi.org/10.5194/cp-2023-3
https://doi.org/10.5194/cp-2023-3
