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First daytime thermospheric wind observation from a balloon‐borne Fabry‐Perot interferometer over Kiruna (68N)
Author(s) -
Wu Qian,
Wang W.,
Roble R. G.,
Häggström Ingemar,
Strømme Anja
Publication year - 2012
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2012gl052533
Subject(s) - daytime , airglow , thermosphere , ionosphere , atmospheric sciences , radar , altitude (triangle) , interferometry , environmental science , incoherent scatter , wind speed , doppler effect , remote sensing , snow , meteorology , f region , geology , physics , geophysics , astronomy , telecommunications , geometry , mathematics , computer science
HIWIND (High altitude Interferometer WIND Observation) is the first balloon Fabry‐Perot interferometer (FPI) to achieve successful thermospheric wind measurement for both day and night. By flying at ∼40 km altitude, HIWIND avoids the high solar scattering background and enables daytime remote sensing of Doppler shift in airglow for thermospheric wind observation. During its first flight in June 2011 from Kiruna, (68N, 65 MLAT), HIWIND observed persistent equatorward winds, while the NCAR TIEGCM model predicted poleward winds on the dayside. Combined with simultaneous EISCAT incoherent scatter radar observation, HIWIND yielded a daytime Burnside factor value of 0.85. HIWIND data appear to suggest that upward vertical winds near the auroral oval may be the cause for large differences between the FPI measured and radar derived winds near midnight.