Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3
<p>This study investigates the sensitivity of modeled surface melt and subsurface heating on the Antarctic ice sheet to a new spectral snow albedo and radiative transfer scheme in the Regional Atmospheric Climate Model (RACMO), version 2.3p3 (Rp3). We tune Rp3 to observations by performing sev...
| Main Authors: | , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2022-03-01
|
| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/16/1071/2022/tc-16-1071-2022.pdf |
| _version_ | 1818744626835619840 |
|---|---|
| author | C. T. van Dalum W. J. van de Berg M. R. van den Broeke |
| author_facet | C. T. van Dalum W. J. van de Berg M. R. van den Broeke |
| author_sort | C. T. van Dalum |
| collection | DOAJ |
| description | <p>This study investigates the sensitivity of modeled surface melt and subsurface heating on the Antarctic ice sheet to a new spectral snow albedo and radiative transfer scheme in the Regional Atmospheric Climate Model (RACMO), version 2.3p3 (Rp3). We tune Rp3 to observations by performing several sensitivity experiments and assess the impact on temperature and melt by incrementally changing one parameter at a time. When fully tuned, Rp3 compares well with in situ and remote sensing observations of surface mass and energy balance, melt, near-surface and (sub)surface temperature, albedo and snow grain specific surface area. Near-surface snow temperature is especially sensitive to the prescribed fresh snow specific surface area and fresh dry snow metamorphism. These processes, together with the refreezing water grain size and subsurface heating, are important for melt around the margins of the Antarctic ice sheet. Moreover, small changes in the albedo and the aforementioned processes can lead to an order of magnitude overestimation of melt, locally leading to runoff and a reduced surface mass balance.</p> |
| first_indexed | 2024-12-18T02:47:18Z |
| format | Article |
| id | doaj.art-6e50cec2f046477eb96820e753ad6806 |
| institution | Directory Open Access Journal |
| issn | 1994-0416 1994-0424 |
| language | English |
| last_indexed | 2024-12-18T02:47:18Z |
| publishDate | 2022-03-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | The Cryosphere |
| spelling | doaj.art-6e50cec2f046477eb96820e753ad68062022-12-21T21:23:32ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242022-03-01161071108910.5194/tc-16-1071-2022Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3C. T. van DalumW. J. van de BergM. R. van den Broeke<p>This study investigates the sensitivity of modeled surface melt and subsurface heating on the Antarctic ice sheet to a new spectral snow albedo and radiative transfer scheme in the Regional Atmospheric Climate Model (RACMO), version 2.3p3 (Rp3). We tune Rp3 to observations by performing several sensitivity experiments and assess the impact on temperature and melt by incrementally changing one parameter at a time. When fully tuned, Rp3 compares well with in situ and remote sensing observations of surface mass and energy balance, melt, near-surface and (sub)surface temperature, albedo and snow grain specific surface area. Near-surface snow temperature is especially sensitive to the prescribed fresh snow specific surface area and fresh dry snow metamorphism. These processes, together with the refreezing water grain size and subsurface heating, are important for melt around the margins of the Antarctic ice sheet. Moreover, small changes in the albedo and the aforementioned processes can lead to an order of magnitude overestimation of melt, locally leading to runoff and a reduced surface mass balance.</p>https://tc.copernicus.org/articles/16/1071/2022/tc-16-1071-2022.pdf |
| spellingShingle | C. T. van Dalum W. J. van de Berg M. R. van den Broeke Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3 The Cryosphere |
| title | Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3 |
| title_full | Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3 |
| title_fullStr | Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3 |
| title_full_unstemmed | Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3 |
| title_short | Sensitivity of Antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in RACMO2.3p3 |
| title_sort | sensitivity of antarctic surface climate to a new spectral snow albedo and radiative transfer scheme in racmo2 3p3 |
| url | https://tc.copernicus.org/articles/16/1071/2022/tc-16-1071-2022.pdf |
| work_keys_str_mv | AT ctvandalum sensitivityofantarcticsurfaceclimatetoanewspectralsnowalbedoandradiativetransferschemeinracmo23p3 AT wjvandeberg sensitivityofantarcticsurfaceclimatetoanewspectralsnowalbedoandradiativetransferschemeinracmo23p3 AT mrvandenbroeke sensitivityofantarcticsurfaceclimatetoanewspectralsnowalbedoandradiativetransferschemeinracmo23p3 |