Zobrazeno 1 - 10
of 73
pro vyhledávání: '"Jonathan M. Harbor"'
Autor:
Martim Mas e Braga, Richard S. Jones, Jorge Bernales, Jane Lund Andersen, Ola Fredin, Mathieu Morlighem, Alexandria J. Koester, Nathaniel A. Lifton, Jonathan M. Harbor, Yusuke Suganuma, Neil F. Glasser, Irina Rogozhina, Arjen P. Stroeven
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-13 (2023)
Abstract Ice streams regulate most ice mass loss in Antarctica. Determining ice stream response to warmer conditions during the Pliocene could provide insights into their future behaviour, but this is hindered by a poor representation of subglacial t
Externí odkaz:
https://doaj.org/article/c55f1988ac9d40979e2198fe032c0e41
Autor:
Jane L. Andersen, Jennifer C. Newall, Ola Fredin, Neil F. Glasser, Nathaniel A. Lifton, Finlay M. Stuart, Derek Fabel, Marc Caffee, Vivi K. Pedersen, Alexandria J. Koester, Yusuke Suganuma, Jonathan M. Harbor, Arjen P. Stroeven
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-12 (2023)
The Heimefrontfjella escarpment in Dronning Maud Land, East Antarctica divides inland precipitation-dominated ice dynamics from coastal dynamics dominated by grounding line migration, suggest inverse model simulations constrained by cosmogenic nuclid
Externí odkaz:
https://doaj.org/article/2a4d2cceec1e4c31a1eb4cae7b995bd8
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
Autor:
Jingdong Zhao, Jinkun Qiu, Jonathan M. Harbor, Huihan Ji, Marc W. Caffee, Wanqin Guo, Huijun Zheng
Publikováno v:
Quaternary Science Reviews. 306:108038
Transfer of Training, Trainee Attitudes and Best Practices in Training Design: a Multiple-Case Study
Publikováno v:
TechTrends. 64:280-301
Transfer of training has not been perceived as successful for training programs in bringing about targeted knowledge, skills, and attitudes (KSA). The review of current literature revealed a lack of consensus of the nature of transfer and ambiguity o
Autor:
Jonathan M. Harbor, Feng Yu
Publikováno v:
Hydrological Processes. 33:1403-1419
Autor:
Jakob Heyman, Arjen P. Stroeven, Ping Fu, Jonathan M. Harbor, Marc W. Caffee, Clas Hättestrand
Publikováno v:
Earth Surface Processes and Landforms. 44:918-932
Quantifying glacial erosion contributes to our understanding of landscape evolution and topographic relief production in high altitude and high latitude areas. Combining in situ Be-10 and Al-26 ana ...
Autor:
Ola Fredin, Finlay M. Stuart, Sarah E. Sams, Yusuke Suganuma, Jane Lund Andersen, Marc W. Caffee, Irina Rogozhina, Jonathan M. Harbor, Neil F. Glasser, Robin Blomdin, Alexandria J. Koester, Nathaniel A. Lifton, Arjen P. Stroeven, Jennifer C. Newall, Derek Fabel
Reconstructing past ice surface changes is key to test and improve ice-sheet models. Yet, data constraining the past behaviour of the East Antarctic Ice Sheet are sparse, limiting our understanding of its response to past and future climate changes.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ba07da61a9efb22dd85a1f9524ef147
https://doi.org/10.5194/egusphere-egu2020-17965
https://doi.org/10.5194/egusphere-egu2020-17965
Autor:
Natacha Gribenski, Robin Blomdin, Jakob Heyman, Arjen P. Stroeven, Clas Hättestrand, Jonathan M. Harbor
We use a domain-wide geomorphometric analysis to investigate spatial patterns of glacial landforms. We focus or analysis on glacial depositional landforms (e.g. marginal moraines), as well as larger erosional landforms (e.g. glacial valleys), because
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eeee7a5aed7e1626ef30f27f3a633ee1
https://doi.org/10.5194/egusphere-egu2020-21574
https://doi.org/10.5194/egusphere-egu2020-21574
Publikováno v:
Geomorphology. 318:128-138
Understanding interactions between topography and glacial erosion is a key to advancing knowledge of mountain landscape evolution and is often hampered by the lack of quantitative data for glacial erosion. Here, we examine spatial variations in glaci