HelioWebAarhus University, Institute for Physics and Astronomy
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I[Aarhus University, Institute for Physics and Astronomy]
PI["Parent Institutions (1)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (21)"]
CA["Linked Collaborating Authors (1)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Magnetic properties of dust on Mars - Results from the Mars Exploration Rovers
- Resolving Codependent Processes Within Natural Dust Devil Vortices
- Multispectral Pancam images of dust patterns on Opportunity's Capture and Filter magnets analyzed by a Computational Fluid Dynamics model.
- Comparison of tephrochronological and radiocarbon based age models for marine sedimentary records in the northern North Atlantic
- Compilation of Marine Radiocarbon Bomb-Pulse from the Temperate North Atlantic Using Annually-Resolved Time-Series From Arctica islandica
- Phoenix Magnetic Properties Experiments Using the Surface Stereo Imager and the MECA Microscopy Station
- Phoenix Mars Lander: Vortices and Dust Devils at the Landing Site
- Reconstructing Radiocarbon Reservoir Ages North of Iceland During the Last Millennium: Implications for Ocean Circulation and Climate Change
- Temperature and Pressure at the Phoenix Landing Site
- Winds at the Phoenix Landing Site
- The Torsional Oscillation and the Solar Minimum
- The internal dynamics and magnetism of the sun -- the perspective from global helioseismology (Invited)
- A European Mars Simulation Wind Tunnel Facility
- Aerosol nucleation induced by a high energy particle beam
- Erosion Induced Mineral Alteration on Mars (Invited)
- Coherent hydrographic changes in the North Atlantic during the last millennium: insights from marine radiocarbon reservoir ages
- Experimental studies of the formation of cluster ions formed by corona discharge in an atmosphere containing SO<SUB>2</SUB>, NH<SUB>3</SUB>, and H<SUB>2</SUB>O
- Late glacial and Holocene monsoon variability in southern Tibet (Invited)
- Spatial pattern of mass loss processes across the Greenland Ice Sheet from the Little Ice Age to 2010
- Continuous 'Passive' Registration of Non-Point Contaminant Loads Via Agricultural Subsurface Drain Tubes
- Origin of the CO<SUB>2</SUB> fluxes of the Icelandic Hotspot