Titlebook: Geoenvironmental Changes in the Cordillera Blanca, Peru; Vít Vilímek,Bryan Mark,Adam Emmer Book 2024 The Editor(s) (if applicable) and The

发起

Circumscribe

扩大

https://doi.org/10.1007/978-3-663-16088-5on. In the Cordillera Blanca, the implications for current and future proglacial landscape management and cascading ecological and societal consequences are numerous. Proglacial landscapes can act as hydrological buffers and filters, store carbon, and function as refuges for cold-adapted species, th

GRAIN

extinct

喧闹

Climate of the Cordillera Blanca,vior for the next decades is the absence of a clear trend; the CB cryosphere remains one of the last remaining tropical glacier bodies with significant paleoclimatic data, and the CB’s climate is characterized by a heterogenous cryosphere-atmosphere interaction, i.e., future projections suggest drie

inflate

Hydrology and Hydrogeology in the Cordillera Blanca,of the Cordillera Blanca. After describing the regional hydrosphere, including the hydroclimatic controls, seasonality, runoff regimes, reservoirs, fluxes and water uses, the impact of ongoing climate changes is discussed, and the future challenges ahead. An emphasis is placed on taking an integrate

彩色的蜡笔

Climate-Morphogenetic and Morphodynamic Zones of the Western Cordillera in Peru,s (local names: Yunga, Quechua, Suni, Puna, and Janca). The regionalization is based on similar conditions in terms of elevation, temperature, precipitation (including rainfall, snow, mist etc.), air pressure, and vegetation, and is usually related to specific morphological units.

lacrimal-gland

headlong

,Stability of Moraine and Rock Slopes at Glacial Lakes—Two Case Studies in the Cordillera Blanca,oraine and a rock slope. Other factors need to contribute to low slope stability and material strength to allow failure initiation. These are water saturation of both, soils and rocks within a slope, seismicity, favorable slope dips and structural conditions, and long-term rock strength deterioratio