Results 171 to 180 of about 23,309 (270)
Deep Groundwater Total Dissolved Solids Mapping in the Dakota Group, Williston Basin, USA
Abstract Growing concern about the quantity of available freshwater around the world has led to interest in surveying groundwater total dissolved solids (TDS) below water well depths. Deep TDS has not been systematically mapped, and there is much to learn about the distribution and controls on deeper groundwater. In sedimentary basins across the United
Michael J. Stephens +3 more
wiley +1 more source
Rethinking flood resilience: systemic risk, governance failures, and the social production of vulnerability in the Himalayan-Indus region. [PDF]
Hamidi AR +4 more
europepmc +1 more source
Integrated glacier and snow hydrological modelling in the Urumqi No.1 glacier catchment
Civil Engineering and ...
Gao, H. (author) +2 more
openaire +1 more source
Abstract The 6 June 2023 failure of the Kakhovka Dam generated a catastrophic outburst flood, leading to loss of life and infrastructure damage. During the flood, daily measurements of water surface elevation were collected by the SWOT satellite, providing the first direct, high‐resolution 2D measurements of a large outburst flood.
K. E. Lehnigk +2 more
wiley +1 more source
Mutual effects of ablation and ice temperature in a firn-free glacier: Observations from Aug 1st glacier on northeast Tibetan plateau. [PDF]
Liu G +9 more
europepmc +1 more source
Abstract Bedload transport of sediment mixtures is fundamental to river morphology and impacts aquatic ecology. Adding fine grains enhances coarse‐grain transport, yet controlling mechanisms remain elusive. Employing discrete element simulations, we examine how fine‐grain size and proportion influence coarse‐grain flux.
Yu Zhang +4 more
wiley +1 more source
Increased rainfall-runoff drives flood hazard intensification in Central Himalayan river systems. [PDF]
Pink I, Reaney SM, Hardy RJ, Bovolo CI.
europepmc +1 more source
Abstract The long‐standing hypothesis that an ice sheet covered the Tibetan Plateau during the Last Glacial Maximum (LGM) has been refuted. Further research has indicated that the Plateau experienced more extensive glacial expansion during Marine Isotope Stage (MIS) 6 than during the LGM.
Weicheng Wang +4 more
wiley +1 more source
Future projections of glacier mass change in High Mountain Asia using GRACE and climatemodel data. [PDF]
Dharpure JK, Howat IM, Patel A.
europepmc +1 more source
Abstract Rivers transport sediments from mountains to oceans, shaping landscapes and transmitting environmental signals. This transfer is repeatedly interrupted by storage and remobilization, complicating efforts to reconstruct erosion histories. Luminescence‐based methods, which exploit the progressive zeroing of the luminescence signals (bleaching ...
Louise Karman‐Besson +7 more
wiley +1 more source

