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Constraints on the strength of faults from the geometry of rider blocks in continental and oceanic core complexes: RIDER BLOCKS AND FAULT STRENGTH (1) · Continental scale, high order, high spatial resolution, ice sheet modeling using the Ice Sheet System Model (ISSM): ICE SHEET SYSTEM MODEL (1) · Dissolved inorganic phosphorus export to the coastal zone: Results from a spatially explicit, global model: A GLOBAL MODEL OF RIVER DIP EXPORT (1) · Flow network derivation from a high resolution DEM in a low relief, agrarian landscape: FLOW NETWORK DERIVATION IN A LOW RELIEF, AGRARIAN LANDSCAPE (1) · Global distribution and sources of dissolved inorganic nitrogen export to the coastal zone: Results from a spatially explicit, global model: GLOBAL DIN EXPORT TO COASTAL WATERS (1) · Global patterns and sources of dissolved organic matter export to the coastal zone: Results from a spatially explicit, global model: GLOBAL DISSOLVED ORGANIC MATTER EXPORT (1) · Ice flux divergence anomalies on 79north Glacier, Greenland: THE 79NORTH GLACIER (1) · Increase in the rate and uniformity of coastline erosion in Arctic Alaska: HIGHER AND MORE UNIFORM ARCTIC EROSION (1) · Millennium Ecosystem Assessment scenario drivers (1970-2050): Climate and hydrological alterations: GLOBAL NEWS HYDROLOGY (1) · Positive-Definite and Monotonic Limiters for Unrestricted-Time-Step Transport Schemes (1) · Sea ice loss enhances wave action at the Arctic coast: SEA ICE LOSS ENHANCES EROSION (1) · Sorted bedform pattern evolution: Persistence, destruction and self-organized intermittency: SORTED BEDFORM PATTERN EVOLUTION (1) · Sources and delivery of carbon, nitrogen, and phosphorus to the coastal zone: An overview of Global Nutrient Export from Watersheds (NEWS) models and their application: GLOBAL EXPORT OF C, N, AND P TO COASTAL SYSTEMS (1) · Topographical and ecohydrological controls on land surface temperature in an alpine catchment (1) · Using hilltop curvature to derive the spatial distribution of erosion rates: HILLTOP CURVATURE PREDICTS EROSION RATES (1) · Widespread late Cenozoic increase in erosion rates across the interior of eastern Tibet constrained by detrital low-temperature thermochronometry: EROSION HISTORY OF EASTERN TIBET (1)
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