Results 131 to 140 of about 927,992 (225)
Glacio-limnological interactions at lake-calving glaciers [PDF]
Iceberg calving is an efficient ablation process which introduces mechanical instability to glacier systems and can cause non-linear climatic response.
Haresign, Eleanor C.
core +1 more source
Correcting Unwrapping Errors Toward Reliable Rock Glacier Velocity From InSAR Time Series
Abstract Rock Glacier Velocity is an Essential Climate Variable Permafrost Quantity, providing a quantifiable indicator of mountain permafrost evolution. Despite its wide usage, multi‐temporal InSAR often substantially underestimates rock glacier velocities compared to ground‐based measurements, limiting its reliability.
Mengze Li +5 more
wiley +1 more source
Supraglacial debris strongly modifies melt rates on debris-covered glaciers, yet simulating this effect remains challenging because modelling the full surface energy balance (SEB) and the vertical conduction of heat through the debris layer requires many
Yoni Verhaegen +3 more
doaj +1 more source
Abstract Temperature and precipitation variability in monsoonal Asia is central to understanding regional climate dynamics and global teleconnections. How post‐LGM warming and hydroclimate change unfolded in Northeast Asia, and how they were linked to external forcing, remain poorly constrained.
Deke Xu +19 more
wiley +1 more source
Analysis of the temporal variations in glaciers’ surface area in Alaknanda River Basin, Uttarakhand
This study presented detailed analysis of glacier surface extent in the Alaknanda river basin, Western Himalaya, using Landsat series data, land surface temperature and digital elevation model (DEM).
V. Nunchhani +4 more
doaj +1 more source
High‐ and Low‐Latitude Insolation Forcing Drives the Half‐Precession Cycle in Winter Arctic Sea Ice
Abstract The half‐precession cycle is a key climatic signal in global climate system, linking high‐ and low‐latitude climate variability and bridging orbital‐ and millennial‐scale climate changes. While it characterizes tropical insolation, its origin in high‐latitude climate records remains unclear. Based on a transient climate simulation spanning the
Zhipeng Wu +6 more
wiley +1 more source
Debris-covered glaciers are glaciers with the largest part of the ablation zone covered by a debris layer. Recent papers showed that debris-covered glaciers are able to support plant and arthropod life, advancing the hypothesis that such landforms could ...
C. Compostella +21 more
core +1 more source
International audienceDebris-covered glaciers are very frequent geomorphological features in Khumbu Himal (Nepal). Rock debris on the glacier surface play a significant role in glacier-climate relationships and glacier dynamics.
Schimmelpfennig, Irene +13 more
core +1 more source
Bacterial community structure on two alpine debris-covered glaciers and biogeography of Polaromonas phylotypes. [PDF]
Franzetti A +9 more
europepmc +1 more source
Heat Flux Modeling on Debris-Covered Glaciers
A one-dimensional heat flux model has been developed in this study to analyze changes in heat propagation within debris cover on a glacier and the subsequent melt. The model can accept data collected in situ for calculations of real modeled melt, and also synthetic data based on simple wave forms and debris physical characteristics.
openaire +1 more source

