Mette Bendixen
Biographic Data
| ID | 6021723 |
|---|---|
| NAME | Mette Bendixen |
| GIVEN NAMES | Mette |
| FAMILY NAME | Bendixen |
| SIGNATURE | BENDIXEN M |
| AFFILIATIONS | McGill University |
| ORCID | 0000-0003-2505-266X |
| VERIFIED | Yes |
| TOTAL WORKS | 10 |
| TOTAL CITATIONS | 17 |
| WORKS AS AUTHOR | 10 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2013 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 3 |
Continental mapping of African sand mining highlights limited benefits for local infrastructure and socio-economic development
Nation-wide mapping shows linkages between sand mining activities, human land use, and hydrology in Rwanda
Towards a holistic understanding of artisanal aggregate mining in Rwanda
Experience exceeds awareness of anthropogenic climate change in Greenland
Although Greenland is a hub for climate science, the climate perceptions of Greenland’s predominantly Indigenous population have remained largely unstudied. Here we present two nationally representative surveys and show that Greenlanders are more likely than residents of top oil-producing Arctic countries to perceive that climate change is happening and about twice as likely to have personally experienced its effects. However, half are unaware th…
Drivers and effects of construction-sand mining in Sub-Saharan Africa
Opportunistic climate adaptation and public support for sand extraction in Greenland
Sand, gravel, and UN Sustainable Development Goals
Promises and perils of sand exploitation in Greenland
Deltas, freshwater discharge, and waves along the Young Sound, NE Greenland
A wide range of delta morphologies occurs along the fringes of the Young Sound in Northeast Greenland due to spatial heterogeneity of delta regimes. In general, the delta regime is related to catchment and basin characteristics (geology, topography, drainage pattern, sediment availability, and bathymetry), fluvial discharges and associated sediment load, and processes by waves and currents. Main factors steering the Arctic fluvial discharges into…
Joint interpretation of beach-ridge architecture and coastal topography show the validity of sea-level markers observed in ground-penetrating radar data
Geological studies of past and present sea level rely on valid and robust features marking sea level in geological sections. Present sea-level markers around the upper shoreface to beachface transition are detected in a beach-ridge plain formed in a microtidal regime. These sea-level markers identify specific relative sea levels at the time of formation. Ground-penetrating radar (GPR) data collected across the youngest part of the beach-ridge sys…
Drivers and effects of construction-sand mining in Sub-Saharan Africa
Opportunistic climate adaptation and public support for sand extraction in Greenland
Promises and perils of sand exploitation in Greenland
Joint interpretation of beach-ridge architecture and coastal topography show the validity of sea-level markers observed in ground-penetrating radar data
Geological studies of past and present sea level rely on valid and robust features marking sea level in geological sections. Present sea-level markers around the upper shoreface to beachface transition are detected in a beach-ridge plain formed in a microtidal regime. These sea-level markers identify specific relative sea levels at the time of formation. Ground-penetrating radar (GPR) data collected across the youngest part of the beach-ridge sys…
Joint interpretation of beach-ridge architecture and coastal topography show the validity of sea-level markers observed in ground-penetrating radar data
Geological studies of past and present sea level rely on valid and robust features marking sea level in geological sections. Present sea-level markers around the upper shoreface to beachface transition are detected in a beach-ridge plain formed in a microtidal regime. These sea-level markers identify specific relative sea levels at the time of formation. Ground-penetrating radar (GPR) data collected across the youngest part of the beach-ridge sys…
Deltas, freshwater discharge, and waves along the Young Sound, NE Greenland
A wide range of delta morphologies occurs along the fringes of the Young Sound in Northeast Greenland due to spatial heterogeneity of delta regimes. In general, the delta regime is related to catchment and basin characteristics (geology, topography, drainage pattern, sediment availability, and bathymetry), fluvial discharges and associated sediment load, and processes by waves and currents. Main factors steering the Arctic fluvial discharges into…
Promises and perils of sand exploitation in Greenland
Sand, gravel, and UN Sustainable Development Goals
Opportunistic climate adaptation and public support for sand extraction in Greenland
Experience exceeds awareness of anthropogenic climate change in Greenland
Although Greenland is a hub for climate science, the climate perceptions of Greenland’s predominantly Indigenous population have remained largely unstudied. Here we present two nationally representative surveys and show that Greenlanders are more likely than residents of top oil-producing Arctic countries to perceive that climate change is happening and about twice as likely to have personally experienced its effects. However, half are unaware th…
Drivers and effects of construction-sand mining in Sub-Saharan Africa
Towards a holistic understanding of artisanal aggregate mining in Rwanda
Continental mapping of African sand mining highlights limited benefits for local infrastructure and socio-economic development
Nation-wide mapping shows linkages between sand mining activities, human land use, and hydrology in Rwanda
Geography (9 works) · Geology (7 works) · Economics (4 works) · Environmental planning (4 works) · Environmental Science (4 works) · Mining and Resource Management (4 works) · Oceanography (4 works) · Business (3 works) · Economic growth (3 works) · Environmental resource management (3 works)