Floristic changes at Khersan Glacier Territory, Alamkuh Mountain, Central Alborz, North of Iran

Considering the data gap in the accumulation region, it was not possible to properly calculate the mass balance of the glacier, but results on volume and elevation changes of

Himalayan glaciers show large uncertainty regarding their present and future state due to their sensitive reaction towards change in climatic condition. Himalayan glaciers are unique

collected during a 2.5 yr period are used to calculate sur- face mass and energy balances at 5324 m a.s.l. on Gua- naco Glacier, a cold-based glacier in the semi-arid Andes of

For this study, the glacier CMB model was modified to in- clude a treatment for supraglacial debris according to two cases: (1) one with no treatment of moisture fluxes or phase

tion Correlation. C.: Slow surge of Trapridge Glacier, Yukon Territory, Canada, J. S.: How much do we really know about glacier surging?, Ann. and Kääb, A.: Evaluation of existing

In conclusion, our study demonstrated a non-adaptive territory selection in a central- Polish mute swan population, where territory preferences measured with a long-term

In this article, we examine the consequence of submarine frontal melting and the ice mélange on glacier dynamics and on the behavior of the glacier front using a full- Stokes

Elevation profiles of (a) annual runo ff height over debris-free glacier (Glacier) and debris- covered (Debris) surfaces, and of (b) responses under conditions of warming