Articles | Volume 16, issue 10
https://doi.org/10.5194/tc-16-3971-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-3971-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
06 Oct 2022
Research article |
| 06 Oct 2022
| 06 Oct 2022
Simulations of firn processes over the Greenland and Antarctic ice sheets: 1980–2021
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center,
Greenbelt, MD, 20771, USA
Thomas A. Neumann
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center,
Greenbelt, MD, 20771, USA
H. Jay Zwally
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center,
Greenbelt, MD, 20771, USA
Benjamin E. Smith
Applied Physics Laboratory, University of Washington, Seattle, WA,
98105, USA
C. Max Stevens
Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center,
Greenbelt, MD, 20771, USA
Earth System Science Interdisciplinary Center, University of Maryland,
College Park, MD, 20740, USA
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Cited
31 citations as recorded by crossref.
- Polar firn properties in Greenland and Antarctica and related effects on microwave brightness temperatures H. Xu et al. 10.5194/tc-17-2793-2023
- Firn air content changes on Antarctic ice shelves under three future warming scenarios S. Veldhuijsen et al. 10.5194/tc-18-1983-2024
- Mapping the vertical heterogeneity of Greenland's firn from 2011–2019 using airborne radar and laser altimetry A. Rutishauser et al. 10.5194/tc-18-2455-2024
- Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models C. Needell & N. Holschuh 10.1029/2022GL102400
- Widespread slowdown in thinning rates of West Antarctic ice shelves F. Paolo et al. 10.5194/tc-17-3409-2023
- A Full-Link Simulation Method for Satellite Single-Photon LiDARs R. Liu et al. 10.1109/LGRS.2023.3334301
- Substantial contribution of slush to meltwater area across Antarctic ice shelves R. Dell et al. 10.1038/s41561-024-01466-6
- Firn on ice sheets C. Amory et al. 10.1038/s43017-023-00507-9
- Characteristics of the 1979–2020 Antarctic firn layer simulated with IMAU-FDM v1.2A S. Veldhuijsen et al. 10.5194/tc-17-1675-2023
- Glacier Energy and Mass Balance (GEMB): a model of firn processes for cryosphere research A. Gardner et al. 10.5194/gmd-16-2277-2023
- A new model of dry firn-densification constrained by continuous strain measurements near South Pole C. Stevens et al. 10.1017/jog.2023.87
- A comparison of contemporaneous airborne altimetry and ice-thickness measurements of Antarctic ice shelves A. Chartrand & I. Howat 10.1017/jog.2023.49
- An evaluation of a physics-based firn model and a semi-empirical firn model across the Greenland Ice Sheet (1980–2020) M. Thompson-Munson et al. 10.5194/tc-17-2185-2023
- Validation and Analysis of the ICESat-2 ATL11 Product: A Case Study of Lake Vostok Y. Gu et al. 10.1080/01490419.2024.2416661
- Quantifying Antarctic‐Wide Ice‐Shelf Surface Melt Volume Using Microwave and Firn Model Data: 1980 to 2021 A. Banwell et al. 10.1029/2023GL102744
- Analytical solutions for the advective–diffusive ice column in the presence of strain heating D. Moreno-Parada et al. 10.5194/tc-18-4215-2024
- Rapid disintegration and weakening of ice shelves in North Greenland R. Millan et al. 10.1038/s41467-023-42198-2
- A wind-driven snow redistribution module for Alpine3D v3.3.0: adaptations designed for downscaling ice sheet surface mass balance E. Keenan et al. 10.5194/gmd-16-3203-2023
- Direct measurements of firn-density evolution from 2016 to 2022 at Wolverine Glacier, Alaska C. Stevens et al. 10.1017/jog.2024.24
- Progress toward globally complete frontal ablation estimates of marine-terminating glaciers W. Kochtitzky et al. 10.1017/aog.2023.35
- How well can satellite altimetry and firn models resolve Antarctic firn thickness variations? M. Kappelsberger et al. 10.5194/tc-18-4355-2024
- Evaluating Greenland surface-mass-balance and firn-densification data using ICESat-2 altimetry B. Smith et al. 10.5194/tc-17-789-2023
- Antarctic-wide ice-shelf firn emulation reveals robust future firn air depletion signal for the Antarctic Peninsula D. Dunmire et al. 10.1038/s43247-024-01255-4
- Brief communication: Preliminary ICESat-2 (Ice, Cloud and land Elevation Satellite-2) measurements of outlet glaciers reveal heterogeneous patterns of seasonal dynamic thickness change C. Taubenberger et al. 10.5194/tc-16-1341-2022
- Ubiquitous acceleration in Greenland Ice Sheet calving from 1985 to 2022 C. Greene et al. 10.1038/s41586-023-06863-2
- Downscaled surface mass balance in Antarctica: impacts of subsurface processes and large-scale atmospheric circulation N. Hansen et al. 10.5194/tc-15-4315-2021
- Simulations of firn processes over the Greenland and Antarctic ice sheets: 1980–2021 B. Medley et al. 10.5194/tc-16-3971-2022
- Grain-size evolution controls the accumulation dependence of modelled firn thickness J. Kingslake et al. 10.5194/tc-16-3413-2022
- GENESIS: co-location of geodetic techniques in space P. Delva et al. 10.1186/s40623-022-01752-w
- Physics-based SNOWPACK model improves representation of near-surface Antarctic snow and firn density E. Keenan et al. 10.5194/tc-15-1065-2021
- Monitoring of Hydrological Resources in Surface Water Change by Satellite Altimetry W. Li et al. 10.3390/rs14194904
23 citations as recorded by crossref.
- Polar firn properties in Greenland and Antarctica and related effects on microwave brightness temperatures H. Xu et al. 10.5194/tc-17-2793-2023
- Firn air content changes on Antarctic ice shelves under three future warming scenarios S. Veldhuijsen et al. 10.5194/tc-18-1983-2024
- Mapping the vertical heterogeneity of Greenland's firn from 2011–2019 using airborne radar and laser altimetry A. Rutishauser et al. 10.5194/tc-18-2455-2024
- Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models C. Needell & N. Holschuh 10.1029/2022GL102400
- Widespread slowdown in thinning rates of West Antarctic ice shelves F. Paolo et al. 10.5194/tc-17-3409-2023
- A Full-Link Simulation Method for Satellite Single-Photon LiDARs R. Liu et al. 10.1109/LGRS.2023.3334301
- Substantial contribution of slush to meltwater area across Antarctic ice shelves R. Dell et al. 10.1038/s41561-024-01466-6
- Firn on ice sheets C. Amory et al. 10.1038/s43017-023-00507-9
- Characteristics of the 1979–2020 Antarctic firn layer simulated with IMAU-FDM v1.2A S. Veldhuijsen et al. 10.5194/tc-17-1675-2023
- Glacier Energy and Mass Balance (GEMB): a model of firn processes for cryosphere research A. Gardner et al. 10.5194/gmd-16-2277-2023
- A new model of dry firn-densification constrained by continuous strain measurements near South Pole C. Stevens et al. 10.1017/jog.2023.87
- A comparison of contemporaneous airborne altimetry and ice-thickness measurements of Antarctic ice shelves A. Chartrand & I. Howat 10.1017/jog.2023.49
- An evaluation of a physics-based firn model and a semi-empirical firn model across the Greenland Ice Sheet (1980–2020) M. Thompson-Munson et al. 10.5194/tc-17-2185-2023
- Validation and Analysis of the ICESat-2 ATL11 Product: A Case Study of Lake Vostok Y. Gu et al. 10.1080/01490419.2024.2416661
- Quantifying Antarctic‐Wide Ice‐Shelf Surface Melt Volume Using Microwave and Firn Model Data: 1980 to 2021 A. Banwell et al. 10.1029/2023GL102744
- Analytical solutions for the advective–diffusive ice column in the presence of strain heating D. Moreno-Parada et al. 10.5194/tc-18-4215-2024
- Rapid disintegration and weakening of ice shelves in North Greenland R. Millan et al. 10.1038/s41467-023-42198-2
- A wind-driven snow redistribution module for Alpine3D v3.3.0: adaptations designed for downscaling ice sheet surface mass balance E. Keenan et al. 10.5194/gmd-16-3203-2023
- Direct measurements of firn-density evolution from 2016 to 2022 at Wolverine Glacier, Alaska C. Stevens et al. 10.1017/jog.2024.24
- Progress toward globally complete frontal ablation estimates of marine-terminating glaciers W. Kochtitzky et al. 10.1017/aog.2023.35
- How well can satellite altimetry and firn models resolve Antarctic firn thickness variations? M. Kappelsberger et al. 10.5194/tc-18-4355-2024
- Evaluating Greenland surface-mass-balance and firn-densification data using ICESat-2 altimetry B. Smith et al. 10.5194/tc-17-789-2023
- Antarctic-wide ice-shelf firn emulation reveals robust future firn air depletion signal for the Antarctic Peninsula D. Dunmire et al. 10.1038/s43247-024-01255-4
8 citations as recorded by crossref.
- Brief communication: Preliminary ICESat-2 (Ice, Cloud and land Elevation Satellite-2) measurements of outlet glaciers reveal heterogeneous patterns of seasonal dynamic thickness change C. Taubenberger et al. 10.5194/tc-16-1341-2022
- Ubiquitous acceleration in Greenland Ice Sheet calving from 1985 to 2022 C. Greene et al. 10.1038/s41586-023-06863-2
- Downscaled surface mass balance in Antarctica: impacts of subsurface processes and large-scale atmospheric circulation N. Hansen et al. 10.5194/tc-15-4315-2021
- Simulations of firn processes over the Greenland and Antarctic ice sheets: 1980–2021 B. Medley et al. 10.5194/tc-16-3971-2022
- Grain-size evolution controls the accumulation dependence of modelled firn thickness J. Kingslake et al. 10.5194/tc-16-3413-2022
- GENESIS: co-location of geodetic techniques in space P. Delva et al. 10.1186/s40623-022-01752-w
- Physics-based SNOWPACK model improves representation of near-surface Antarctic snow and firn density E. Keenan et al. 10.5194/tc-15-1065-2021
- Monitoring of Hydrological Resources in Surface Water Change by Satellite Altimetry W. Li et al. 10.3390/rs14194904
Latest update: 20 Nov 2024
Short summary
Satellite altimeters measure the height or volume change over Earth's ice sheets, but in order to understand how that change translates into ice mass, we must account for various processes at the surface. Specifically, snowfall events generate large, transient increases in surface height, yet snow fall has a relatively low density, which means much of that height change is composed of air. This air signal must be removed from the observed height changes before we can assess ice mass change.
Satellite altimeters measure the height or volume change over Earth's ice sheets, but in order...
