Annual surface mass balance (SMB) and components of Svalbard glaciers statistically downscaled to 500 m spatial resolution (1958-2018)
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| Auteurs principaux: | , , , , , , , , , , |
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2020
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| _version_ | 1867168205447888896 |
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| author | Noël, Brice P Y Jakobs, Constantijn L van Pelt, Ward Lhermitte, Stef Wouters, Bert Kohler, Jack Hagen, Jon Ove Luks, Bartłomiej Reijmer, Carleen H van de Berg, Willem Jan van den Broeke, Michiel R |
| author_facet | Noël, Brice P Y Jakobs, Constantijn L van Pelt, Ward Lhermitte, Stef Wouters, Bert Kohler, Jack Hagen, Jon Ove Luks, Bartłomiej Reijmer, Carleen H van de Berg, Willem Jan van den Broeke, Michiel R |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Compared to other Arctic ice masses, Svalbard glaciers are low-elevated with flat interior accumulation areas, resulting in a marked peak in their current hypsometry (area-elevation distribution) at ~450 m above sea level. Since summer melt consistently exceeds winter snowfall, these low-lying glaciers can only survive by refreezing a considerable fraction of surface melt and rain in the porous firn layer covering their accumulation zones. We use a high-resolution climate model to show that modest atmospheric warming in the mid-1980s forced the firn zone to retreat upward by ~100 m to coincide with the hypsometry peak. This led to a rapid areal reduction of firn cover available for refreezing, and strongly increased runoff from dark, bare ice areas, amplifying mass loss from all elevations. As the firn line fluctuates around the hypsometry peak in the current climate, Svalbard glaciers will continue to lose mass and show high sensitivity to temperature perturbations. The data set includes annual cumulative SMB and components statistically downscaled from the output of the Regional Atmospheric Climate Model RACMO2.3 to 500 m spatial resolution (1958-2018). SMB components include total precipitation (snowfall and rainfall), snowfall, runoff, melt, refreezing and retention (mm w.e. per year), as well as summer (June-July-August) 2 m air temperature (K). The data set also includes modelled (RACMO2.3; 1958-2018) and observed (MODIS; 2000-2018) bare ice area, and modelled ablation zone area (1958-2018; km2). The mask file includes longitude/latitude (ºN/ºW), land-sea, ice and sector masks from the Randolph Glacier Inventory version 6, and surface topography (m above sea level) from the S0 Terreng Digital Elevation Model (Norwegian Polar Institute) on the 500 m grid. Daily downscaled SMB and components are available from the authors upon request and without conditions (b.p.y.noel@uu.nl). |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_920984 |
| institution | PANGAEA |
| language | en |
| publishDate | 2020 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Annual surface mass balance (SMB) and components of Svalbard glaciers statistically downscaled to 500 m spatial resolution (1958-2018) Noël, Brice P Y Jakobs, Constantijn L van Pelt, Ward Lhermitte, Stef Wouters, Bert Kohler, Jack Hagen, Jon Ove Luks, Bartłomiej Reijmer, Carleen H van de Berg, Willem Jan van den Broeke, Michiel R Binary Object; Binary Object (File Size); Binary Object (Media Type); MULT; Multiple investigations; RACMO; SMB; Svalbard Compared to other Arctic ice masses, Svalbard glaciers are low-elevated with flat interior accumulation areas, resulting in a marked peak in their current hypsometry (area-elevation distribution) at ~450 m above sea level. Since summer melt consistently exceeds winter snowfall, these low-lying glaciers can only survive by refreezing a considerable fraction of surface melt and rain in the porous firn layer covering their accumulation zones. We use a high-resolution climate model to show that modest atmospheric warming in the mid-1980s forced the firn zone to retreat upward by ~100 m to coincide with the hypsometry peak. This led to a rapid areal reduction of firn cover available for refreezing, and strongly increased runoff from dark, bare ice areas, amplifying mass loss from all elevations. As the firn line fluctuates around the hypsometry peak in the current climate, Svalbard glaciers will continue to lose mass and show high sensitivity to temperature perturbations. The data set includes annual cumulative SMB and components statistically downscaled from the output of the Regional Atmospheric Climate Model RACMO2.3 to 500 m spatial resolution (1958-2018). SMB components include total precipitation (snowfall and rainfall), snowfall, runoff, melt, refreezing and retention (mm w.e. per year), as well as summer (June-July-August) 2 m air temperature (K). The data set also includes modelled (RACMO2.3; 1958-2018) and observed (MODIS; 2000-2018) bare ice area, and modelled ablation zone area (1958-2018; km2). The mask file includes longitude/latitude (ºN/ºW), land-sea, ice and sector masks from the Randolph Glacier Inventory version 6, and surface topography (m above sea level) from the S0 Terreng Digital Elevation Model (Norwegian Polar Institute) on the 500 m grid. Daily downscaled SMB and components are available from the authors upon request and without conditions (b.p.y.noel@uu.nl). |
| title | Annual surface mass balance (SMB) and components of Svalbard glaciers statistically downscaled to 500 m spatial resolution (1958-2018) |
| topic | Binary Object; Binary Object (File Size); Binary Object (Media Type); MULT; Multiple investigations; RACMO; SMB; Svalbard |
| url | https://doi.org/10.1594/PANGAEA.920984 |