Articles | Volume 13, issue 5
https://doi.org/10.5194/tc-13-1473-2019
© Author(s) 2019. 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-13-1473-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Quantifying the snowmelt–albedo feedback at Neumayer Station, East Antarctica
Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, the Netherlands
Carleen H. Reijmer
Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, the Netherlands
Peter Kuipers Munneke
Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, the Netherlands
Gert König-Langlo
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
Michiel R. van den Broeke
Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, the Netherlands
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- The long-term sea-level commitment from Antarctica A. Klose et al. 10.5194/tc-18-4463-2024
- Spatial Variability of the Snowmelt‐Albedo Feedback in Antarctica C. Jakobs et al. 10.1029/2020JF005696
- Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland G. Traversa et al. 10.3390/rs13040799
- Mapping the albedo of the active surface at different stages of the growing season using data from various sources P. Bartmiński & M. Siłuch 10.1016/j.rsase.2022.100818
- Greenland Ice Sheet Daily Surface Melt Flux Observed From Space L. Zheng et al. 10.1029/2021GL096690
29 citations as recorded by crossref.
- Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica J. Calleja et al. 10.3390/s19163569
- Automated mapping of the seasonal evolution of surface meltwater and its links to climate on the Amery Ice Shelf, Antarctica P. Tuckett et al. 10.5194/tc-15-5785-2021
- Contrasting current and future surface melt rates on the ice sheets of Greenland and Antarctica: Lessons from in situ observations and climate models M. van den Broeke et al. 10.1371/journal.pclm.0000203
- Melt in Antarctica derived from Soil Moisture and Ocean Salinity (SMOS) observations at L band M. Leduc-Leballeur et al. 10.5194/tc-14-539-2020
- On the relationship between ENSO diversity and the ENSO atmospheric teleconnection to high‐latitudes D. Gushchina et al. 10.1002/joc.7304
- On the Differences in Precipitation Type Between the Arctic, Antarctica and Tibetan Plateau D. Yang et al. 10.3389/feart.2021.607487
- A physics-based Antarctic melt detection technique: combining Advanced Microwave Scanning Radiometer 2, radiative-transfer modeling, and firn modeling M. Dattler et al. 10.5194/tc-18-3613-2024
- Time-series snowmelt detection over the Antarctic using Sentinel-1 SAR images on Google Earth Engine D. Liang et al. 10.1016/j.rse.2021.112318
- Subsurface heat conduction along the CHINARE traverse route, East Antarctica D. Yang et al. 10.1017/jog.2022.97
- The evolution of future Antarctic surface melt using PISM-dEBM-simple J. Garbe et al. 10.5194/tc-17-4571-2023
- A benchmark dataset of in situ Antarctic surface melt rates and energy balance C. Jakobs et al. 10.1017/jog.2020.6
- Atmospheric River Signatures in Radiosonde Profiles and Reanalyses at the Dronning Maud Land Coast, East Antarctica I. Gorodetskaya et al. 10.1007/s00376-020-9221-8
- Variable temperature thresholds of melt pond formation on Antarctic ice shelves J. van Wessem et al. 10.1038/s41558-022-01577-1
- Evaluation of a new snow albedo scheme for the Greenland ice sheet in the Regional Atmospheric Climate Model (RACMO2) C. van Dalum et al. 10.5194/tc-14-3645-2020
- Observed and Parameterized Roughness Lengths for Momentum and Heat Over Rough Ice Surfaces M. van Tiggelen et al. 10.1029/2022JD036970
- Combined GNSS reflectometry–refractometry for automated and continuous in situ surface mass balance estimation on an Antarctic ice shelf L. Steiner et al. 10.5194/tc-17-4903-2023
- Changes in the Antarctic’s Summer Surface Albedo, Observed by Satellite since 1982 and Associated with Sea Ice Anomalies Y. Sun et al. 10.3390/rs15204940
- The surface energy balance during foehn events at Joyce Glacier, McMurdo Dry Valleys, Antarctica M. Hofsteenge et al. 10.5194/tc-16-5041-2022
- Distribution and seasonal evolution of supraglacial lakes on Shackleton Ice Shelf, East Antarctica J. Arthur et al. 10.5194/tc-14-4103-2020
- Surface melt on the Shackleton Ice Shelf, East Antarctica (2003–2021) D. Saunderson et al. 10.5194/tc-16-4553-2022
- Impact of updated radiative transfer scheme in snow and ice in RACMO2.3p3 on the surface mass and energy budget of the Greenland ice sheet C. van Dalum et al. 10.5194/tc-15-1823-2021
- Continuous monitoring of surface water vapour isotopic compositions at Neumayer Station III, East Antarctica S. Bagheri Dastgerdi et al. 10.5194/tc-15-4745-2021
- Meteorological drivers of melt at two nearby glaciers in the McMurdo Dry Valleys of Antarctica M. Hofsteenge et al. 10.1017/jog.2023.98
- An exploratory modelling study of perennial firn aquifers in the Antarctic Peninsula for the period 1979–2016 J. van Wessem et al. 10.5194/tc-15-695-2021
- Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3 C. van Dalum et al. 10.5194/tc-16-1071-2022
- The long-term sea-level commitment from Antarctica A. Klose et al. 10.5194/tc-18-4463-2024
- Spatial Variability of the Snowmelt‐Albedo Feedback in Antarctica C. Jakobs et al. 10.1029/2020JF005696
- Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland G. Traversa et al. 10.3390/rs13040799
- Mapping the albedo of the active surface at different stages of the growing season using data from various sources P. Bartmiński & M. Siłuch 10.1016/j.rsase.2022.100818
1 citations as recorded by crossref.
Latest update: 03 Oct 2024
Short summary
We use 24 years of observations at Neumayer Station, East Antarctica, to calculate the surface energy balance and the associated surface melt, which we find to be mainly driven by the absorption of solar radiation. Meltwater can refreeze in the subsurface snow layers, thereby decreasing the surface albedo and hence allowing for more absorption of solar radiation. By implementing an albedo parameterisation, we show that this feedback accounts for a threefold increase in surface melt at Neumayer.
We use 24 years of observations at Neumayer Station, East Antarctica, to calculate the surface...