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Member Since 2013
Glenn A. Milne
University of Ottawa
AGU Research
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Projecting 21st Century Sea Level Change Along Coastal Greenland
ADVANCES IN OUR UNDERSTANDING OF PAST, PRESENT, AND FUTURE SEA LEVEL CHANGE III POSTER
geodesy | 15 december 2023
Lauren Lewright, Jacqueline Austermann, Surendra A...
Rising sea levels are an immediate threat to coastal communities around the world. The Greenland Ice Sheet (GrIS), vulnerable to increased atmospheric...
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Time Scales of Glacial Isostatic Adjustment in Greenland: Is Transient Rheology Required?
EARTH’S TRANSIENT BEHAVIOR THROUGH SYNTHESIS OF OBSERVATIONAL, LABORATORY, AND THEORETICAL APPROACHES I ELIGHTNING
study of earth's deep interior | 13 december 2023
Linda Pan, Jerry X. Mitrovica, Glenn A. Milne, Mar...
The possibility of a transient rheological response to ice age loading, first discussed in the literature of the 1980s, has received renewed attention...
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River deltas and sea-level rise
PREDICTING THE FATE OF RIVER DELTAS AND COASTAL WETLANDS: OBSERVATIONS, MODELING, AND EXPERIMENTATION II ORAL
earth and planetary surface processes | 13 december 2023
Jaap Nienhuis, Wonsuck Kim, Glenn A. Milne, Melind...
Sea-level change is a first-order control on delta morphodynamics, however, quantifying delta change under future sea-level rise remains difficult. He...
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Holocene terrestrial ice mass loss precedes floating ice tongue collapse in NW Greenland – Insights from revised high-precision relative sea level curves and cosmogenic exposure ages
HOW STABLE IS THE GREENLAND ICE SHEET? PAST, PRESENT, AND FUTURE II POSTER
cryosphere | 16 december 2022
Anna Glueder, Alan C. Mix, Jorie Clark, Brendan T....
Recent reconstructions of the floating ice-tongues in Petermann and Ryder Fjord in northwest Greenland reveal a picture of frequent ice margin fluctua...
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The Influence of Lateral Earth Structure on Inferences of Global Ice Volume During the Last Glacial Maximum
ICE-SHEET VARIABILITY AND BEHAVIOR THROUGH THE LENS OF GEOLOGIC DATA AND NUMERICAL MODELING I ORAL
paleoceanography and paleoclimatology | 15 december 2022
Linda Pan, Glenn A. Milne, Konstantin Latychev, Sa...
The mapping from far-field relative sea level (RSL) records to changes in ice volume involves a correction for glacial isostatic adjustment (GIA), and...
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Assessing Holocene Fault Movement along the Hinagu Fault Zone using Paleo-Sea Level Extents at Kawata Machinishi, Kumamoto, Japan
MULTISCALE CRUSTAL DEFORMATION IN SUBDUCTION ZONES AND THE MEGATHRUST EARTHQUAKE CYCLE: PROGRESS FROM OBSERVATIONS AND MODELS II POSTER
tectonophysics | 14 december 2022
Evan Tam, Yusuke Yokoyama, Yukari Miyashita, Glenn...
Kumamoto Prefecture, located in Kyushu, Japan, has previously been assessed as relatively tectonically inactive (National Astronomical Observatory, 19...
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Partitioning early Holocene North American v. Antarctic ice melt from high-resolution reconstructions of sea-level rise and glacial isostatic adjustment modeling
PAST CLIMATE, ICE SHEET, AND SEA-LEVEL CHANGES: HOW MUCH, HOW FAST? I ORAL
paleoceanography and paleoclimatology | 17 december 2021
Udita Mukherjee, Torbjorn E. Tornqvist, Lael Vette...
According to the IPCC SROCC report, under RCP8.5, the rate of sea level rise in 2100 CE will be 10-20 mm/yr and extreme sea level events will become c...
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Time-Varying Mantle Viscosity as an Explanation for the High Modern Crustal Uplift Rates in Greenland
NEITHER ELASTIC NOR HARMONIC: THE EARTH’S TRANSIENT BEHAVIOR ACROSS TIME/LENGTH SCALES I ORAL
study of earth's deep interior | 16 december 2021
Surendra Adhikari, Glenn A. Milne, Lambert Caron, ...
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. E...
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