Executive summary: The amount of auroral X-ray emission in the PoGOLite energy band has been estimated using data from an Antarctic balloon flight in 2000. It is noted that this flight took place during solar maximum conditions and so represents a worse-case compared to the expected flight of PoGOLite in 2009. Auroral emission exceeding a few 10’s of mCrab is expected for approximately 5-10 % of the flight time, within the auroral zone. Typical PoGO-Lite observational targets range from 200 to 1000 mCrab. Outside this zone the auroral sky coverage is of course lower, whereby its emission can be avoided by appropriate choice of targets. It is proposed to monitor the in-flight auroral activity in a number of independent ways: using flight mag...
In the Polar Patrol Balloon (PPB) project, two balloons named PPB-8 and -10 were launched in rapid s...
International audienceA polarised radiative transfer model (POMEROL) has been developed to compute t...
An auroral event which occurred over Spitsbergen at 17:25-17:30 UT on 26 January 2006 has been studi...
The PoGOLite balloon experiment, to be launched from Kiruna in August 2010 will investigate polarisa...
第8回極域科学シンポジウム/個別セッション:[OS] 宙空圏12月5日(火)国立極地研究所 1階交流アトリウムThe Eighth Symposium on Polar Science/Ordinar...
Balloon observations of auroral X-rays using different detector systems were carried out twice over ...
The uniquely beautiful light display of an aurora is the result of charged particles colliding with ...
The polarisation degree and angle of the X-ray flux emitted by astrophysical objects holds valuable ...
Three sounding rockets were launched in 1984 from Syowa Station in Antarctica into different types o...
Results of a study of techniques for imaging the aurora from a high altitude satellite at X-ray wave...
Polar Patrol Balloon (PPB) No.6 experiment was performed over Antarctica, in order to observe wide-a...
The intensity ratios of auroral emissions at different wavelengths are widely used for reconstructio...
All-sky auroral images acquired at Ny-Ålesund were used in conjunction with observations of a Polar ...
Abstract: Observations of auroral oxygen ion emission at 732/733 nm were made at the Aurora station ...
A lack of observable quantities renders it generally difficult to confront models of Space Weather w...
In the Polar Patrol Balloon (PPB) project, two balloons named PPB-8 and -10 were launched in rapid s...
International audienceA polarised radiative transfer model (POMEROL) has been developed to compute t...
An auroral event which occurred over Spitsbergen at 17:25-17:30 UT on 26 January 2006 has been studi...
The PoGOLite balloon experiment, to be launched from Kiruna in August 2010 will investigate polarisa...
第8回極域科学シンポジウム/個別セッション:[OS] 宙空圏12月5日(火)国立極地研究所 1階交流アトリウムThe Eighth Symposium on Polar Science/Ordinar...
Balloon observations of auroral X-rays using different detector systems were carried out twice over ...
The uniquely beautiful light display of an aurora is the result of charged particles colliding with ...
The polarisation degree and angle of the X-ray flux emitted by astrophysical objects holds valuable ...
Three sounding rockets were launched in 1984 from Syowa Station in Antarctica into different types o...
Results of a study of techniques for imaging the aurora from a high altitude satellite at X-ray wave...
Polar Patrol Balloon (PPB) No.6 experiment was performed over Antarctica, in order to observe wide-a...
The intensity ratios of auroral emissions at different wavelengths are widely used for reconstructio...
All-sky auroral images acquired at Ny-Ålesund were used in conjunction with observations of a Polar ...
Abstract: Observations of auroral oxygen ion emission at 732/733 nm were made at the Aurora station ...
A lack of observable quantities renders it generally difficult to confront models of Space Weather w...
In the Polar Patrol Balloon (PPB) project, two balloons named PPB-8 and -10 were launched in rapid s...
International audienceA polarised radiative transfer model (POMEROL) has been developed to compute t...
An auroral event which occurred over Spitsbergen at 17:25-17:30 UT on 26 January 2006 has been studi...