Zobrazeno 1 - 10
of 165
pro vyhledávání: '"Pierre‐Henri Blard"'
Autor:
Pierre-Henri Blard, Marie Protin, Jean-Louis Tison, François Fripiat, Dorthe Dahl-Jensen, Jørgen P. Steffensen, William C. Mahaney, Paul R. Bierman, Andrew J. Christ, Lee B. Corbett, Vinciane Debaille, Thomas Rigaudier, Philippe Claeys, ASTER Team
Publikováno v:
Journal of Glaciology, Vol 69, Pp 1011-1029 (2023)
We present new data from the debris-rich basal ice layers of the NEEM ice core (NW Greenland). Using mineralogical observations, SEM imagery, geochemical data from silicates (meteoric 10Be, εNd, 87Sr/86Sr) and organic material (C/N, δ13C), we chara
Externí odkaz:
https://doaj.org/article/0745c87b00e3461894becead77175cc5
Autor:
Lionel L. Siame, Lucas Espíndola Rosa, Luis Felipe Soares Cherem, José Guilherme de Oliveira, Olivier Evrard, Houda Barhoumi, Laëtitia Leanni, Adrien Duvivier, Pierre‐Henri Blard, Didier L. Bourlès, ASTER Team, Sophie Cornu
Publikováno v:
Earth's Future, Vol 11, Iss 8, Pp n/a-n/a (2023)
Abstract Land degradation resulting from increased continental surface erosion is a worldwide and systemic phenomenon due to unsustainable human activities. Already fragile, the intertropical zone is likely to be further affected by climate change li
Externí odkaz:
https://doaj.org/article/695c72fe5b5546c2842d25213e16f838
Autor:
Matt Rowberry, Jan Balek, Miloš René, Pierre-Henri Blard, Filip Hartvich, Stavros Meletlidis, Jan Blahůt, Ivo Baroň, Ivanka Mitrovic-Woodell
Publikováno v:
Tectonophysics
Tectonophysics, Elsevier, 2020, 776, pp.228317. ⟨10.1016/j.tecto.2019.228317⟩
Tectonophysics, Elsevier, 2020, 776, pp.228317. ⟨10.1016/j.tecto.2019.228317⟩
Volcanic flank collapses often result in giant debris avalanches that are capable of travelling tens of kilometres across the ocean floor and generating tsunamis that devastate distant communities. The San Andres Landslide on El Hierro, Canary Island
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6d2d736e976454ae0cef1b374f464a68
https://hal.univ-lorraine.fr/hal-02931460/document
https://hal.univ-lorraine.fr/hal-02931460/document
Publikováno v:
MethodsX, Vol 6, Iss , Pp 1547-1556 (2019)
Methods based on cosmic-ray produced nuclides are key to improve our understanding of the Earth surface dynamic. Measuring multiple cosmogenic nuclides in the same rock sample has a great potential, but data interpretation requires rigorous and often
Externí odkaz:
https://doaj.org/article/eac0f7d7da984844ac30e393f0397695
Numerous hyperthermal events have been documented through the Paleocene-Eocene transition. The best known hyperthermal event is the Paleocene-Eocene Thermal Maximum (PETM; around 56Ma), a period that led to surface and bottom water warming of about 5
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee662b56fc2426b36e62e370bebc7c9f
https://doi.org/10.5194/egusphere-egu23-8719
https://doi.org/10.5194/egusphere-egu23-8719
Autor:
Agathe Defourny, Pierre-Henri Blard, Laurent Zimmermann, Patrick Jobé, Arnaud Collignon, Frédéric Nguyen, Alain Dassargues
Publikováno v:
Hydrology and Earth System Sciences. 26:2637-2648
Although natural CO2-rich groundwaters of eastern Belgium have been known for centuries, the exact origin of their gas is still unclear. This paper presents the results of a sampling campaign in Belgium (Spa, Stoumont, Malmedy): 30 samples of both ca
Publikováno v:
Quaternary Research. 109:183-194
We use PRISM climatic data (1981–2010) and Landsat images (2012–2013) to establish an empirical relationship linking annual temperature and precipitation to the equilibrium line altitude (ELA) of glaciers in the Sierra Nevada (36–41°N, Califor
Publikováno v:
Science Advances
Science Advances, 2023, 9 (6), ⟨10.1126/sciadv.adf8119⟩
Science Advances, 2023, 9 (6), ⟨10.1126/sciadv.adf8119⟩
Terrestrial amplification (TA) of land warming relative to oceans is apparent in recent climatic observations. TA results from land-sea coupling of moisture and heat and is therefore important for predicting future warming and water availability. How
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10103eb173f86ac25c773cc6a2ca74c1
https://hal.science/hal-03993339/file/sciadv.adf8119.pdf
https://hal.science/hal-03993339/file/sciadv.adf8119.pdf
Autor:
Masa Kageyama, Pierre-Henri Blard, Stella Bourdin, Julien Charreau, Lukas Kluft, Guillaume Leduc, Etienne Legrain
Publikováno v:
EGU22
EGU22, 0000, à renseigner, Unknown Region. ⟨10.5194/egusphere-egu22-11955⟩
EGU22, 0000, à renseigner, Unknown Region. ⟨10.5194/egusphere-egu22-11955⟩
The amplitude of the Last Glacial Maximum (LGM) cooling compared to pre-industrial has long been a topic of debate, which partly arises from the fact that this cooling is spatially heterogeneous. Paleotemperature reconstructions shows that this cooli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9905948761a97d7f4a4535e97675dacf
https://insu.hal.science/insu-03938064
https://insu.hal.science/insu-03938064
Autor:
Pierre-Henri BLARD, Baptiste SUCHERAS-MARX, Guillaume SUAN, Blandine GODET, Jade DUTILLEUL, Taous MEZINE, Thierry Adatte
Marl-limestone alternations are rhythmical inter-bedded deposits that commonly occur in many sedimentological environments. It is quite well established that these lithological variations originate from astronomically-driven climatic variations paced
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::39513dc222fa33fb53a6af7217868fa5
https://doi.org/10.31223/x5807j
https://doi.org/10.31223/x5807j