Glacier surface albedo strongly affects glacier mass balance by controlling the energy budget. As an indicator of equilibrium line altitude (ELA), snowline (SLA) at end melt season can reflect variations in balance. Therefore, it is extremely crucial to investigate changes and SLA for calculating evaluating loss. In this study, from 2011 2021, Muz Taw was derived Landsat images with a spatial r...

A widespread loss of glacier area and volume has been observed in the European Alps since the 1980s. In addition to differences among various regions of the Alps, different responses to climate change characterize neighboring glaciers within the same region. In this study we describe the glacier changes in the Ortles-Cevedale group, the largest glacierized area in the Italian Alps. We analyze t...

Glaciation has affected the shape of mountain ranges and has induced a global increase in erosion rates during the past 2 m.y. The observed increase in erosion rates appears to vary with latitude, reaching a maximum at mid-latitudes that is particularly well defined in the Southern Hemisphere. Although it is likely that climate played an important role, the processes responsible for such latitu...

Observations of protoplanetary disks have revealed them to be complex and dynamic, with vertical radial transport gas dust occurring simultaneously chemistry planet formation. Previous models focused primarily on chemical evolution in a static disk, or dynamical solids chemically passive disk. In this paper, we present new 1D method for modelling pebble growth simultaneously. Gas small particle...