The near‐surface boundary layer can mediate the response of mountain glaciers to external
climate, cooling the overlying air and promoting a density‐driven glacier wind. The …

Quantification of land surface–atmosphere fluxes of carbon dioxide (CO 2) and their trends
and uncertainties is essential for monitoring progress of the EU27+ UK bloc as it strives to …

The presence of a developed boundary layer decouples a glacier's response from ambient
conditions, suggesting that sensitivity to climate change is increased by glacier retreat. To …

Near-surface air temperature (T a) is highly important for modelling glacier ablation, though
its spatio-temporal variability over melting glaciers still remains largely unknown. We present …

Air temperature inversions, a situation in which atmospheric temperature increases with
height, are key components of the Arctic planetary boundary layer. The present study …

Glacier albedo determines the net shortwave radiation absorbed at the glacier surface and
plays a crucial role in glacier energy and mass balance. Remote sensing techniques are …

The climatic response of mountain permafrost and glaciers located in high-elevation
mountain areas has major implications for the stability of mountain slopes and related …

Atmospheric boundary layer (ABL) dynamics over glaciers mediate the response of glacier
mass balance to large‐scale climate forcing. Despite this, very few ABL observations are …

Albedo plays a key role in regulating the absorption of solar radiation within ice surfaces and
hence strongly regulates the production of meltwater. A combination of Landsat and Sentinel …

Near-surface air temperature variability and the reliability of temperature extrapolation within
glacierized regions are important issues for hydrological and glaciological studies that …