Supraglacial trees are becoming a common feature on debris-covered glaciers (DCGs). The Miage Glacier (Mont Blanc Massif) is the only DCG on the Southern side of the European Alps characterized by the presence of a supraglacial forest. Trees are negatively affected by glacier surface movements, and growth disturbances are recorded in tree rings. We have analyzed the glacier parameters influencing the establishment and growth of supraglacial trees at the Miage Glacier and we have compared the tree-ring growth patterns and stable isotopes, as well as the needle volatile organic compounds (VOCs), of supraglacial trees ("glacier" site) with respect to trees located on a lateral moraine ("control" site). We found that supraglacial trees are pres...
The increase of temperatures in the last decades is a well-established process. Middle latitude glac...
The rise of the global mean temperature with an unprecedented recorded rate is well documented. Neve...
The ongoing climate changes and global warming affect high elevation areas more than other environme...
Supraglacial trees are a useful source of data for reconstructing past glacier surface movements and...
First results of an innovative multi-proxy approach applied to glacier-related trees for assessing c...
First results of an innovative multi-proxy approach applied to glacier-related trees for assessing c...
The number of debris-covered glaciers featuring supraglacial tree vegetation is increasing worldwide...
Supraglacial debris cover allows vegetation to colonize glacier surface, and whenever it is enough s...
Debris-covered glaciers may host several biological forms that colonize the debris cover, especially...
Dendroglaciological analysis of supraglacial trees represents an example of applied dendrogeornorpho...
Two tree-ring chronologies of stone pine (Pinus cembra L.) and two of Norway spruce (Picea abies Kar...
Dendrochronology has often been used to study past and present glacier dynamics and fluctuations. Mi...
With the aim of evaluating the influence of glacial meltwater signature on tree-ring stable isotopes...
International audienceWith the aim of evaluating the influence of glacial meltwater signature on tre...
With the aim of evaluating the influence of glacial meltwater signature on tree-ring stable isotopes...
The increase of temperatures in the last decades is a well-established process. Middle latitude glac...
The rise of the global mean temperature with an unprecedented recorded rate is well documented. Neve...
The ongoing climate changes and global warming affect high elevation areas more than other environme...
Supraglacial trees are a useful source of data for reconstructing past glacier surface movements and...
First results of an innovative multi-proxy approach applied to glacier-related trees for assessing c...
First results of an innovative multi-proxy approach applied to glacier-related trees for assessing c...
The number of debris-covered glaciers featuring supraglacial tree vegetation is increasing worldwide...
Supraglacial debris cover allows vegetation to colonize glacier surface, and whenever it is enough s...
Debris-covered glaciers may host several biological forms that colonize the debris cover, especially...
Dendroglaciological analysis of supraglacial trees represents an example of applied dendrogeornorpho...
Two tree-ring chronologies of stone pine (Pinus cembra L.) and two of Norway spruce (Picea abies Kar...
Dendrochronology has often been used to study past and present glacier dynamics and fluctuations. Mi...
With the aim of evaluating the influence of glacial meltwater signature on tree-ring stable isotopes...
International audienceWith the aim of evaluating the influence of glacial meltwater signature on tre...
With the aim of evaluating the influence of glacial meltwater signature on tree-ring stable isotopes...
The increase of temperatures in the last decades is a well-established process. Middle latitude glac...
The rise of the global mean temperature with an unprecedented recorded rate is well documented. Neve...
The ongoing climate changes and global warming affect high elevation areas more than other environme...