Results 71 to 80 of about 2,916 (208)
Delays and declines in hydrological extremes in nivo‐glacial rivers of Mendoza, Argentina
Hydrological changes (1956–2023) in the Mendoza River Basin on Argentinean Central Andes, reveal variations in flow pulses, magnitude, and timing in the context of climate variability. These changes affect ecosystems, water supply, and energy, highlighting the need for adaptive water management and conservation in high‐mountain regions.
Carolina Lauro +2 more
wiley +1 more source
Glacial lake outburst floods (GLOFs) are a severe natural hazard on the eastern Tibetan Plateau, posing a risk to infrastructure safety (e.g. the Sichuan–Tibet Railway) and regional socioeconomic development.
Bingshu Xu +4 more
doaj +1 more source
Trends, Breaks, and Biases in the Frequency of Reported Glacier Lake Outburst Floods
Thousands of glacier lakes have been forming behind natural dams in high mountains following glacier retreat since the early 20th century. Some of these lakes abruptly released pulses of water and sediment with disastrous downstream consequences.
Georg Veh +5 more
doaj +1 more source
Abstract In high‐mountain Third Pole (TP), increasing transboundary fluvial floods (TFFs) threaten nearly one billion people downstream. However, the changing roles of glacier and snow melt in the future TFFs and their socio‐economic impacts remain unclear.
Hu Liu +4 more
wiley +1 more source
High‐resolution elevation data revealed numerous smaller subglacial meltwater corridors (sSMCs) in south‐central British Columbia. The sSMCs are eroded into the surrounding landscape and consist of an erosional unconformity with curvilinear ridges, discontinuously covered by a broad corridor fill, which is sometimes capped by an esker.
Alexander D. Sodeman, Tracy A. Brennand
wiley +1 more source
Hydrological regime of remote catchments with extreme gradients under accelerated change: the Baker basin in Patagonia [PDF]
The Baker basin (27 000 km2) is located in one of the most pristine and remote areas of the planet. Its hydrological regime is poised to undergo dramatic changes in the near future due to hydropower development and climate change.
Alejandro Dussaillant J. +17 more
core +1 more source
Abstract Quantifying the supply‐demand dynamics of the flood regulation service (FRS) is crucial for effective flood risk management. However, current methods cannot adequately capture high‐altitude hydrological processes, leading to flawed assessments of climate change impacts on FRS in such regions. Here, we improve the methodology for estimating the
Lei Li +7 more
wiley +1 more source
Rapid atmospheric warming, especially at high altitude, leads to alpine mountain landscapes becoming more vulnerable to mass movements and consequently unstable. For example, decay of mountain permafrost contributes to rockfalls, landslides and debris flows; glaciers are retreating and losing mass at alarming rates, exposing unstable slopes that are ...
Nazimul Islam +5 more
wiley +1 more source
Accelerating River Discharge in High Mountain Asia
Abstract High Mountain Asia (HMA) plays a crucial role in Asian hydrology—its vast snow and glacier‐covered landscape significantly influences downstream river water supply for billions of people. Understanding the spatiotemporal pattern of river discharge in HMA aids effective water resource management and infrastructure planning.
J. A. Flores +23 more
wiley +1 more source

