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Long-duration balloon flight
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TIGER instrument was launched
from Williams Field in Antarctica which is about 6 miles northeast of
McMurdo Station (lat. -77.86° S) on December 21, 2001 at 12:30
AM. Antarctica is a particularly good place from which to launch
such a balloon for several reasons. The fact that the sun never
sets during the Austral summer means that the balloon will undergo
comparatively minor diurnal heating and cooling. Furthermore, the
winds set up
in a circumpolar pattern which allows the balloon payload to maintain
somewhat of a predictable trajectory over the continent. Since
Antarctica is virtually totally uninhabited, it is easy to avoid the
concern involved with flying a uncontrolled balloon payload.
Finally, TIGER can collect more data below a geomagnetic cutoff of
about 1 GV, which is possible only near the Earth's poles. Taken from excerpts of Jason
Link's doctoral thesis |
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This plot shows the balloon altitude over the course of the entire flight. The constant dips in altitude are due to diurnal heating and cooling. The plot shows that the balloon was constantly leaking during the flight. Sudden increases in altitude such as that seen near day 12 were caused by the dropping of ballast. |
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This plot shows the latitude of the balloon
during its flight. It is interesting to note that it deviated
very little from its initial latitude during the first orbit, while
during the second orbit, when the circumpolar winds were beginning to
fade, it began to venture further southward. |
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A bird's-eye view of the balloon flight. |
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