The performance of natural guide star adaptive-optics systems for telescopes located on the Antarctic plateau is evaluated and compared with adaptive-optics systems operated with the characteristic mid-latitude atmosphere found at Mauna Kea. A 2-m telescope with tip-tilt correction and an 8-m telescope equipped with a high-order adaptive-optics system are considered. Because of the large isoplanatic angle of the South Pole atmosphere, the anisoplanatic error associated with an adaptive-optics correction is negligible, and the achievable resolution is determined only by the fitting error associated with the number of corrected wave-front modes, which depends on the number of actuators on the deformable mirror. The usable field of view of an ...
Modeling of astronomically important atmospheric parameters, and the impact these parameters have on...
From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200 m thic...
From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200 m thic...
Abstract. The turbulence structure of the atmosphere is the primary limitation to adaptive optics sy...
The turbulence structure of the atmosphere is the primary limitation to adaptive optics system perfo...
The turbulence structure of the atmosphere is the primary limitation to adaptive optics system perfo...
The unique atmospheric characteristics found at Dome C on the Antarctic plateau offer significant ad...
The unique atmospheric characteristics found at Dome C on the Antarctic plateau offer significant ad...
The unique atmospheric characteristics found at Dome C on the Antarctic plateau offer significant ad...
The high plateau that covers half of the continent of Antarctica contains the best astronomical obse...
This thesis presents an analysis of the potential for high dynamic range direct imaging of exoplanet...
Ground layer Adaptive Optics (GLAO) is a new variant of adaptive optics that aims at correcting the ...
The internal antarctic plateau revealed in the last years to be a site with interesting potentialiti...
The unique advantages for astronomy on the Antarctic plateau are now well established. In particular...
Modeling of astronomically important atmospheric parameters, and the impact these parameters have on...
Modeling of astronomically important atmospheric parameters, and the impact these parameters have on...
From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200 m thic...
From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200 m thic...
Abstract. The turbulence structure of the atmosphere is the primary limitation to adaptive optics sy...
The turbulence structure of the atmosphere is the primary limitation to adaptive optics system perfo...
The turbulence structure of the atmosphere is the primary limitation to adaptive optics system perfo...
The unique atmospheric characteristics found at Dome C on the Antarctic plateau offer significant ad...
The unique atmospheric characteristics found at Dome C on the Antarctic plateau offer significant ad...
The unique atmospheric characteristics found at Dome C on the Antarctic plateau offer significant ad...
The high plateau that covers half of the continent of Antarctica contains the best astronomical obse...
This thesis presents an analysis of the potential for high dynamic range direct imaging of exoplanet...
Ground layer Adaptive Optics (GLAO) is a new variant of adaptive optics that aims at correcting the ...
The internal antarctic plateau revealed in the last years to be a site with interesting potentialiti...
The unique advantages for astronomy on the Antarctic plateau are now well established. In particular...
Modeling of astronomically important atmospheric parameters, and the impact these parameters have on...
Modeling of astronomically important atmospheric parameters, and the impact these parameters have on...
From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200 m thic...
From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200 m thic...