Zobrazeno 1 - 10
of 123
pro vyhledávání: '"Glenn A. Milne"'
At present, exploring the space of rheological parameters in models of glacial isostatic adjustment (GIA) and relative sea level (RSL) which incorporate laterally variable Earth structure is computationally expensive. A single simulation using the Se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43ce56a898e665ab4339d0bb38be3472
https://doi.org/10.5194/egusphere-egu23-7921
https://doi.org/10.5194/egusphere-egu23-7921
Autor:
Marisa Borreggine, Konstantin Latychev, Sophie Coulson, Evelyn M. Powell, Jerry X. Mitrovica, Glenn A. Milne, Richard B. Alley
Publikováno v:
Proceedings of the National Academy of Sciences. 120
The first records of Greenland Vikings date to 985 CE. Archaeological evidence yields insight into how Vikings lived, yet drivers of their disappearance in the 15th century remain enigmatic. Research suggests a combination of environmental and socioe
Autor:
Jaap H. Nienhuis, Wonsuck Kim, Glenn A. Milne, Melinda Quock, Aimée B.A. Slangen, Torbjörn E. Törnqvist
Future sea-level rise poses an existential threat for many river deltas, yet quantifying the effect of sea-level changes on these coastal landforms remains a challenge. Sea-level changes have been slow compared to other coastal processes during the i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3c892bc177e42cacaa8a92da1a635689
http://imis.nioz.nl/imis.php?module=ref&refid=359230
http://imis.nioz.nl/imis.php?module=ref&refid=359230
Publikováno v:
Geophysical Journal International. 226:91-113
SUMMARYThe Pacific Coast of Central North America is a geodynamically complex region which has been subject to various geophysical processes operating on different timescales. Glacial isostatic adjustment (GIA), the ongoing deformational response of
Many coastal cities are an early casualty in climate-related coastal flooding because of processes resulting in land subsidence and thus enhanced relative sea-level (RSL) rise. Much of the Atlantic coast of North America has been sinking for thousand
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::58d1b6d1d59b20de68395f871082fcd3
https://doi.org/10.5194/egusphere-egu22-50
https://doi.org/10.5194/egusphere-egu22-50
Publikováno v:
Earth System Dynamics, Vol 12, Pp 783-795 (2021)
Global patterns of sea-level change – often termed “sea-level fingerprints” – associated with future changes in ice/water mass re-distribution are a key component in generating regional sea-level projections. Calculation of these fingerprints
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9bd365eaea03e786f1a387e9b607e01a
https://esd.copernicus.org/articles/12/783/2021/
https://esd.copernicus.org/articles/12/783/2021/
Publikováno v:
Earth and Planetary Science Letters. 512:236-245
The isostatic response of the Earth to past mass exchange between ice sheets and oceans, so-called glacial isostatic adjustment (GIA), is an important geodynamic process in North America. Modelling GIA observables provides one of the few direct metho
Autor:
Linda Pan, Glenn A. Milne, Konstantin Latychev, Samuel L. Goldberg, Jacqueline Austermann, Mark J. Hoggard, Jerry X. Mitrovica
Publikováno v:
Quaternary Science Reviews. 290:107644
Autor:
Eric Larour, Johan Nilsson, Surendra Adhikari, Kristian K. Kjeldsen, Lambert Caron, Glenn A. Milne, Erik R. Ivins, Shfaqat Abbas Khan
The observed crustal uplift rates in Greenland are caused by the combined response of the solid Earth to both ongoing and past surface mass changes. Existing elastic Earth models and Maxwell linear...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::859c53c9f68627760720952405d8eb91
https://doi.org/10.1002/essoar.10507038.1
https://doi.org/10.1002/essoar.10507038.1
Reconciling geodetic and geologic estimates of coastal vertical land motion around the British Isles
Karegar et al. (2016, GRL) showed that independent estimates of vertical land motion from geodetic and geologic techniques are critical for understanding coastal surface motion caused by geological versus human-induced processes along the Atlantic co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5d7563e213543192cc1b9c09eb0949d
https://doi.org/10.5194/egusphere-egu21-10710
https://doi.org/10.5194/egusphere-egu21-10710