Zobrazeno 1 - 10
of 97
pro vyhledávání: '"Volker Klemann"'
Autor:
Dennis Höning, Matteo Willeit, Reinhard Calov, Volker Klemann, Meike Bagge, Andrey Ganopolski
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 6, Pp n/a-n/a (2023)
Abstract Understanding the future fate of the Greenland Ice Sheet (GIS) in the context of anthropogenic CO2 emissions is crucial to predict sea level rise. With the fully coupled Earth system model of intermediate complexity CLIMBER‐X, we study the
Externí odkaz:
https://doaj.org/article/375b696a59084fafbdf735e96d7fe9b1
Publikováno v:
Frontiers in Water, Vol 4 (2022)
We use a fully coupled hydro-thermal model (TH) to quantify changes in the pore pressure and temperature distribution following the Last Glacial Maximum (LGM) in the intracontinental basins in Central and Northern Europe. We demonstrate that even wit
Externí odkaz:
https://doaj.org/article/27ae83ce7bea4b76a7b623341cc7e059
Publikováno v:
Remote Sensing, Vol 14, Iss 16, p 3956 (2022)
The elastic response of solid earth to glacier and ice sheet melting, the most important consequences of climate change, is a contemporaneous uplift. Here, we use interferometric synthetic aperture radar (InSAR) measurements to detect crustal deforma
Externí odkaz:
https://doaj.org/article/d6b52d0615544d9b80cd1014292671bf
Publikováno v:
Remote Sensing, Vol 10, Iss 3, p 462 (2018)
We present ground deformations in response to water level variations at the Toktogul Reservoir, located in Kyrgyzstan, Central Asia. Ground deformations were measured by Envisat Advanced Synthetic Aperture Radar (ASAR) and Sentinel-1 Differential Int
Externí odkaz:
https://doaj.org/article/8c00f8c8d67a4365900cc85b56a358e0
Models of glacial isostatic adjustment (GIA) simulate the time-delayed viscoelastic response of the solid Earth to surface loading induced mainly by mass redistribution between ice and ocean during the last glacial cycle considering for rotational fe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86bac8674d32754550e60b971ebfe06a
https://doi.org/10.5194/egusphere-egu23-3351
https://doi.org/10.5194/egusphere-egu23-3351
Autor:
Pingping Huang, Roman Lucas Sulzbach, Volker Klemann, Yoshiyuki Tanaka, Henryk Dobslaw, Zdeněk Martinec, Maik Thomas
Publikováno v:
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth 127(11), nestránkováno. (2022)
Journal of Geophysical Research: Solid Earth 127(11), nestránkováno. (2022)
Ocean tide loading (OTL) and ocean tide dynamics (OTD) are known to be affected by Earth's internal structures, with the latter being affected by the self-attraction and loading (SAL) potential. Combining the 3D earth models Lyon and LITHO1.0, we con
The Antarctic Ice Sheet is the largest and most uncertain potential contributor to future sea level rise. Understanding involved feedback mechanisms require physically-based models. Confidence in future projections can be improved by models that can
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e4e16034997872b023ff581ab786845
https://doi.org/10.5194/egusphere-egu22-7609
https://doi.org/10.5194/egusphere-egu22-7609
Ocean tidal dynamics depend on several factors of which some have experienced considerable changes since the last glacial maximum (LGM). Mainly driven by deglaciation-induced sea-level rise and altered oceanographic conditions, these changes comprise
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4414a503c096189958ccce53f477f4e1
https://doi.org/10.5194/egusphere-egu22-9241
https://doi.org/10.5194/egusphere-egu22-9241
Autor:
Volker Klemann, Jacky Austermann, Meike Bagge, Natasha Barlow, Jeffrey Freymueller, Pingping Huang, Erik R. Ivins, Andrew Lloyd, Zdeněk Martinec, Glenn Milne, Alessio Rovere, Holger Steffen, Rebekka Steffen, Wouter van der Wal, Maryam Yousefi, Shijie Zhong
During the last decade there has been an increasing demand to improve models of present-day loading processes and glacial-isostatic adjustment (GIA). This is especially important when modelling the GIA process in tectonically active regions like the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5ee1827c7175add87f0df8f069191d7
https://doi.org/10.5194/egusphere-egu22-1447
https://doi.org/10.5194/egusphere-egu22-1447