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Member Since 2009
Natalya A. Gomez
Associate Professor, McGill University
AGU Research
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Real‐Time Water Levels Using GNSS‐IR: A Potential Tool for Flood Monitoring
GEOPHYSICAL RESEARCH LETTERS
28 february 2024
David Purnell, Natalya A. Gomez, William G. Minari...

Global Navigation Satellite System Interferometric Reflectometry (GNSS‐IR) using low‐cost antennas is a practical solution for monitori...

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The role of the solid Earth in Antarctica’s contribution to future global sea levels
ANTARCTIC ICE-OCEAN INTERACTION AND ICE SHEET RETREAT: PAST, PRESENT, AND FUTURE III ORAL
cryosphere | 13 december 2023
Natalya A. Gomez, Maryam Yousefi, David Pollard, R...
The response of the Antarctic Ice Sheet (AIS) to climate change is the largest uncertainty in projecting future sea level rise over the coming centuri...
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Future Climate and Sea Level Projections Using a Coupled Antarctic Ice Sheet - Climate Model
ANTARCTIC ICE-OCEAN INTERACTION AND ICE SHEET RETREAT: PAST, PRESENT, AND FUTURE III ORAL
cryosphere | 13 december 2023
Shaina Sadai, Yue Dong, Ambarish Karmalkar, David ...
Dynamic interactions between the Antarctic Ice Sheet (AIS) and climate system will influence future climate and sea level, yet limitations in ice shee...
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The coupled dynamics of ice sheets, the solid Earth and global sea levels in a changing climate
2023 NEW GENERATION OF SCIENTISTS
union sessions | 12 december 2023
Natalya A. Gomez
Melting of the polar ice sheets in Greenland and Antarctica is expected to dominate future sea level change as climate warming continues. Observation ...
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The impact of regional-scale variability in upper mantle viscosity on GIA in West Antarctica
INVESTIGATIONS OF ICE SHEETS, SOLID EARTH, AND SEA LEVEL FROM A GLACIAL ISOSTATIC ADJUSTMENT PERSPECTIVE II POSTER
cryosphere | 11 december 2023
Erica M. Lucas, Natalya A. Gomez, Konstantin Latyc...
West Antarctica is underlain by a laterally heterogenous upper mantle, with localized regions of mantle viscosity reaching several orders of magnitude...
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How should individual ice-sheet contributions to sea level be calculated?
INVESTIGATIONS OF ICE SHEETS, SOLID EARTH, AND SEA LEVEL FROM A GLACIAL ISOSTATIC ADJUSTMENT PERSPECTIVE II POSTER
cryosphere | 11 december 2023
Natalya A. Gomez, David Pollard, Maryam Yousefi, H...
The contribution of an ice sheet to equivalent global sea level change is an important and widely used metric to quantify the response of the ice shee...
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Mapping Geodetically Inferred Antarctic Ice Height Changes Into Thickness Variations: A Sensitivity Study
INVESTIGATIONS OF ICE SHEETS, SOLID EARTH, AND SEA LEVEL FROM A GLACIAL ISOSTATIC ADJUSTMENT PERSPECTIVE II POSTER
cryosphere | 11 december 2023
Natasha Valencic, Linda Pan, Konstantin Latychev, ...
Determining recent ice volume changes from satellite altimeter measurements of ice height requires a correction for contemporaneous vertical crustal d...
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Glacial isostatic adjustment contributes to retreat of stable grounding line zones over the last deglaciation in the Ross Sea
INVESTIGATIONS OF ICE SHEETS, SOLID EARTH, AND SEA LEVEL FROM A GLACIAL ISOSTATIC ADJUSTMENT PERSPECTIVE II POSTER
cryosphere | 11 december 2023
Sam Kodama, Tamara Pico, Alexander Robel, John Eri...
Since the Last Glacial Maximum (26-19 ka; LGM; Clark et al., 2009), Antarctic ice streams in the Ross Sea (West Antarctica) retreated hundreds of kilo...
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