Results 181 to 190 of about 86,383 (345)

Palaeoglacier reconstruction and dynamics of Cordillera Vilcanota in the tropical high Peruvian Andes

open access: yesEarth Surface Processes and Landforms, Volume 51, Issue 2, February 2026.
We provide a geomorphological analysis of Cordillera Vilcanota and use morphostratigraphic principles to reconstruct palaeo icefield extent and palaeoglacier readvances, likely during the Antarctic Cold Reversal and Younger Dryas. We find evidence of temperate and polythermal ice margins, with limited glaciofluvial landform generation.
Bethan Davies   +11 more
wiley   +1 more source

Author Correction: Global methane emissions from rivers and streams. [PDF]

open access: yesNature
Rocher-Ros G   +7 more
europepmc   +1 more source

Scour hole behaviour: A field study of the Dutch Rhine Delta

open access: yesEarth Surface Processes and Landforms, Volume 51, Issue 2, February 2026.
Scour hole behaviour can be divided into dynamic and stable. Dynamic scour holes grow in area, depth and volume during seasonal discharge variations and are typically located in discharge‐dominated river reaches. Stable scour holes are found in tidal rivers with heterogeneous riverbeds and show nearly fixed dimensions.
Marthe Oldenhof   +3 more
wiley   +1 more source

Seasonal variations in proglacial lake area revealed by high spatial resolution planetscope satellite imagery

open access: yesEarth Surface Processes and Landforms, Volume 51, Issue 2, February 2026.
High‐resolution PlanetScope imagery reveals seasonal variations in proglacial lake area are underestimated by ~7% in moderate‐resolution data, while use of a single summer image can underestimate annual maximum area by ~2%. Capturing these seasonal variations provides valuable insights into the factors driving lake dynamics at Fjallsárlón, Iceland ...
Amelia Andrews   +3 more
wiley   +1 more source

Index to Limnology and Oceanography [PDF]

open access: bronze, 1957
Domingo Martinez   +10 more
openalex   +1 more source

The southwest Kalahari dune field does not emit dust post‐fire despite a lack of vegetation and above‐threshold winds

open access: yesEarth Surface Processes and Landforms, Volume 51, Issue 2, February 2026.
The southwest Kalahari dune field has resident fine grains which may be emitted as mineral dust after protective vegetation is removed by fire. However, low wind speeds, high initial surface cover, and the protective effect of biocrusts result in the low possibility of the southwest Kalahari emitting dust post‐fire.
Rosemary A. Huck   +2 more
wiley   +1 more source

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