Assessing glacier features supporting supraglacial trees
A case study of the Miage debris-covered Glacier (Italian Alps)
Bibliographic Data
| ID | 12266151 |
|---|---|
| Authors | L C Vezzola (0000-0001-7305-9335, University of Milan, corresponding author), Guglielmina Diolaiuti (0000-0002-3883-9309, University of Milan), Guglielmina Adele Diolaiuti (University of Milan), C D’Agata (0000-0002-3337-7301, University of Milan), Claudio Smiraglia (0000-0001-6635-2074, University of Milan), Manuela Pelfini (0000-0002-3258-1511, University of Milan) |
| Year | 2016 |
| Volume | 26 |
| Issue | 7 |
| Pages | 1138-1148 |
| Publication date | 2016-03-11 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | The Holocene (JOURNAL) |
| Journal identifiers | ISSN: 0959-6836 • E-ISSN: 1477-0911 |
| Publisher | SAGE Publishing (PUBLISHER • US) |
| DOI | 10.1177/0959683616632883 |
| OpenAlex | W2346943633 |
| Language | EN |
| References cited | 56 |
The number of debris-covered glaciers featuring supraglacial trees is increasing worldwide as a response of high mountain environments to climate warming. Generally, their distribution on the glacier surface is not homogeneous, thus suggesting that some glacier parameters influence germination and growth of trees. In this study, we focused our attention on the widest Italian debris-covered glacier, the Miage Glacier (Mont Blanc massif). We analyzed the ablation area in the range from 1730 to 2400 m a.s.l. where continuous debris coverage is present and trees are found. Using data obtained by remote sensing investigations and field surveys, we defined a record of glacier parameters to be analyzed with respect to the presence and abundance of trees. We found that supraglacial trees are present at the Miage Glacier (1) whenever exceeding a debris thickness threshold (⩾19 cm), (2) with a gentle slope (⩽10°), (3) with a low glacier surface velocity (⩽7.0 m/yr), and (4) where the vertical changes due to glacier dynamics are positive (i.e. prevalent increase ranging between +7 and +28 m over 28 years due to both slow debris accumulation and preservation of ice flow inputs). The statistical analysis supports our findings. The analysis of the same parameters might be conducted on other debris-covered glaciers featuring supraglacial trees, in order to evaluate whether such conditions are local ones or whether they are general factors driving germination and growth of trees. By identifying the features supporting the presence and growth of trees in these environments, and their thresholds, a contribution is given for a better understanding of the importance of debris-covered glaciers and, in general, of debris-covered ice, as a refuge for trees during glacial and warm intervals of the Holocene
Accumulation zone · Climatology · Cryosphere · Debris · Geography · Geomorphology · Glacier · Glacier mass balance · Glacier morphology · Hydrology (agriculture · Ice stream · Physical geography · Rock glacier · Cryospheric studies and observations · Geology and Paleoclimatology Research · Tree-ring climate responses · Geology · Oceanography
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| Highly cited | No |
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