Results 131 to 140 of about 2,782 (273)
Quantitative analysis of channel characteristics of distributive fluvial systems
ABSTRACT Distributive fluvial systems (DFSs) are characterised by a radial distributive channel pattern in planform and dominate modern‐day sedimentary basins. Where aggradation occurs, such as in sedimentary basins, there is increased preservation potential, and therefore, DFSs are hypothesised to constitute a significant portion of the continental ...
Kwetishe Joro Danjuma +4 more
wiley +1 more source
Super‐Resolution of Planetary Images Based on Generative Adversarial Network
Abstract Currently, satellite imagery serves as the primary means of observing terrestrial planets such as the Mars, the Moon, and Mercury. Enhancing the resolution and quality of these images can provide more detailed insights into planetary surfaces. However, improvements in image quality are often limited by the constraints of sensor technology and ...
Xiaoran Zhang, Yiran Wang, Miao Zhuo
wiley +1 more source
Permanent nearshore sediment loss and inevitable retreat of cohesive bluff‐backed beaches
Net volume in survey control areas at the dune‐backed beach (PB) and bluff‐backed beach (LD) is shown between surveys (‘interval’), where the first point is the difference between 2012 and 2020 JABLTCX LiDAR surveys. Cumulative totals are shown as square markers. Water levels during the same dates are shown in grey.
Chelsea A. Volpano +2 more
wiley +1 more source
Erosion rates were quantified using field methods (137Cs, sediment loading) and two landform evolution models (LEMs), SIBERIA and SSSPAM, on a grazed catchment analogous to nearby mining sites, filling the gap in field data comparisons. Model estimates aligned with field data, demonstrating both LEMs' predictive potential for erosion in grazed ...
Indishe P. Senanayake +2 more
wiley +1 more source
Classification and Characteristics of the Distribution of Glacial Landforms in the Japanese Alps.
Glaciations during the Last Glacial in the Japanese Alps can be classified “azonal glaciation” and “zonal glaciation”. The ELAg (geomorphological equilibrium line altitude) of each former type of glacier is determined by Hs (height of summit), and is depressed by microclimatological phenomena such as drifted snow.
openaire +1 more source
Future warming shifts precipitation from snow to rain across the Saskatchewan River Basin, reducing snow water equivalent and advancing snowmelt timing. Differences among precipitation phase‐partitioning methods propagate from snowpack accumulation to runoff magnitude and timing, producing earlier spring flows and higher peak discharge.
Fuad Yassin +5 more
wiley +1 more source
Abstract Accurate three‐dimensional (3D) lake bathymetry reconstruction is critical for water resources assessment and hydrological modeling yet remains constrained by data scarcity and oversimplified geometric assumptions. To address these challenges, we propose the Geomorphologically informed deep learning (GIDL) framework for high‐resolution 3D lake
Minglei Hou +7 more
wiley +1 more source
Towards a landform geodatabase : the automatic identification of landforms
If a geomorphologist is able to identify landforms from an aerial photograph or a Digital Terrain Model, then it should be possible for a computer to mimic the same process.
Maguire, Bradley David
core
Abstract The Taruntius crater, situated between Maria Fecunditatis, Crisium, and Tranquillitatis, is characterized by a prominent bright ray system and a floor‐fractured morphology and has long been interpreted as a relatively young Eratosthenian or Copernican crater.
Longjiao Yu +3 more
wiley +1 more source

