OOIR: Observatory of International Research

Papers

(The H4-Index of Geomorphology is 27. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2022-05-01 to 2026-05-01.)

Article	Citations
Segmentation and deformation mechanisms of the North Tuole Shan fault in the Qilian Mountains: Insights from channel steepness index (k) and fault activity	187
From hypogenic to biogenic speleogenesis in semi-arid climate: Bat guano-driven carbonate weathering and cave modification in Chariton Cave, Israel	76
Multivariate analysis of inlet morphodynamics: The mixed sand-gravel ebb-tidal delta of Deben Estuary, Suffolk	51
Point cloud does matter. Selected issues of using airborne LiDAR elevation data in geomorphometric studies of rugged sandstone terrain under forest – Case study from Central Europe	49
Editorial Board	46
Reconstruction of historical suspended particulate matter contributions of Rhône River tributaries to the Mediterranean Sea	40
Editorial Board	38
Subsurface structures of solution dolines inferred from electrical resistivity tomography: A hypothesis on the evolutionary process of solution dolines at the Akiyoshi-dai Plateau, southwest Japan	37
Spatial variation of surface erosion rate in a fault zone and its controlling factors	37
Editorial Board	37
Editorial Board	36
Editorial Board	36
Investigating cost-effective single-beam survey configurations for accurate river bathymetry construction	35
Use of GIS tools, enhanced by FFT filtering methods, to detect blurred craters in Synthetic Digital Elevation Models, to improve their location and morphological characterisation	35
Quaternary fluvial archives from Asian rivers: Reflections of tectonic activity, crustal processes and climatic variation	33
The uncertain future of mountaintop-removal-mined landscapes 1: How mining changes erosion processes and variables	32
Hurricane-triggered cascading hazards: Geomorphic responses and flood hazard dynamics in a tropical mountain region	32
Plio-Pleistocene drainage reorganization in the middle Yellow River of China, revealed by provenance and paleocurrent analysis of fluvial sediments	32
Tectonic influence on the evolutionary dynamics of deep-water channel systems along the active accretionary prism margin in the Rakhine Basin, Myanmar: A high-resolution 3d seismic analysis	31
Topographic constraints on the rock avalanche erosion mechanisms and sliding effects	31
Coastal cliff evolution: Modelling the long-term interplay between marine erosion, initial topography, and uplift in an arid environment	31
How do international boundary river dynamics affect riparian land? Insights from the China-Russia Ussuri River	30
Quantifying five decades of shoreline change in relation to river sediment supply along the Phu Yen Coast, Central Vietnam	30
Deformation and failure mechanisms of slopes in the Loess Plateau with structural planes under engineering excavation	30
Rockfall susceptibility mapping from topography perspective combing slope units and physical model-based negative sample strategy in the Yangtze Three Gorges	30

Hydration caves and cavities from the recent weathering zone of anhydrites at Dingwall (Nova Scotia, Canada)	29
Late-Quaternary activity of parallel normal faults along the southern margin of the Yuguang Basin in the Shanxi Rift, China and its seismogeological implications	29
Submerged reef and inter-reef morphology in the Western South Atlantic, Abrolhos Shelf (Brazil)	27
CoMMa: A GIS geomorphometry toolbox to map and measure confined landforms	27
Inventory of active rock glaciers and their distribution characteristics on the Qinghai-Tibet Plateau and its adjacent mountainous regions	27
Remotely mapping gullying and incision in Maryland Piedmont headwater streams using repeat airborne lidar	27
Mapping release and propagation areas of permafrost-related rock slope failures in the French Alps: A new methodological approach at regional scale	27
Glacial to periglacial transition at the end of the last ice age in the subtropical semiarid Andes	27
Distinctive shear zones demonstrate pervasive laminar cataclastic flow throughout the gigantic Iymek rock avalanche	27