Results 191 to 200 of about 14,782 (212)

Outlines of the Quaternary geology of Latvia [PDF]

open access: yes, 2014
Nartišs, Māris, Zelčs, Vitālijs
core   +1 more source

Leveraging airborne imaging spectroscopy and multispectral satellite imagery to map glacial sediment plumes in Kachemak Bay, Alaska.

open access: yesJ Hydrol Reg Stud
Hartl L   +8 more
europepmc   +1 more source

Acceleration of ice loss across the Himalayas over the past 40 years. [PDF]

open access: yesSci Adv, 2019
Maurer JM   +3 more
europepmc   +1 more source

A submerged Stone Age hunting architecture from the Western Baltic Sea. [PDF]

open access: yesProc Natl Acad Sci U S A
Geersen J   +15 more
europepmc   +1 more source

Underestimated mass loss from lake-terminating glaciers in the greater Himalaya

Nature Geoscience, 2023
Guoqing Zhang   +9 more
openaire   +2 more sources

Ice-flow adjustments during the transition from land- to lake-terminating status of Jiagai Glacier, Eastern Himalaya

Geomorphology
Yunyi Luo   +6 more
openaire   +2 more sources

Insights into the seasonal dynamics of the lake-terminating glacier Fjallsjökull, south-east Iceland, inferred using ultra-high resolution repeat UAV imagery

, 2021
Proglacial lakes are becoming ubiquitous at the termini of many glaciers worldwide, leading to increased glacier mass loss and terminus retreat due to the influence such lakes are having upon ice dynamics.
Nathaniel R. Baurley, J. Hart
semanticscholar   +1 more source

Evolution of the seasonal dynamics of the lake-terminating glacier Fjallsjökull, southeast Iceland, inferred using high-resolution repeat UAV imagery

2022
Proglacial lakes are becoming ubiquitous at the termini of many glaciers worldwide, leading to increased glacier mass loss and terminus retreat, yet an understanding of the key processes forcing their behaviour is lacking. This study utilised high-resolution repeat uncrewed aerial vehicle (UAV)-Structure from Motion (SfM) imagery to provide insights ...
Nathaniel Baurley, Jane Hart
openaire   +1 more source

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