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Color camera observations of sprites and blue jets from 1994 provided
the first information about the energy processes producing middle
atmospheric optical emissions (Sentman et al.(1995b),Wescott et al.(1995)). The
optical signature from sprites appeared primarily in the red channel
of the color camera with some blue emissions from the lower portions
of sprites. Blue jets appear solely in the blue channel.
Spectrographic observations of sprites in 1995 identified the
brightest red emissions as the molecular nitrogen first positive group
(N2(1PG)) (Hampton et al.(1996),Mende et al.(1995)). Ground based blue filtered
photometer observations and blue and red filtered observations were
made in the summers of 1996, 1997, and 1998 to understand the blue
emissions of sprites (Armstrong et al.(1998),Suszcynsky et al.(1998)). Most
observations of optical emissions above thunderstorms are made at low
slant angles (10o or less), so severe Rayleigh scattering is
present and atmospheric transmission in the blue is poor (c.f.
Section 2 of (Morrill et al.(1998))). The EXL98 (Energetics of
Upper Atmospheric Excitation by Lightning,
1998) campaign was designed specifically to study microphysical energy
processes of sprites, blue jets, and elves. EXL98
(Sentman et al.(1998)) was centered on a series of aircraft flights
during July 1998 with several intensified cameras. These cameras
covered wavelengths from the near-UV (320 nm) to the near-IR
(>1500 nm) and provided a unique opportunity to study the energetics
of these phenomena. One reason for the use of aircraft in 1998 was to
get above the dense atmosphere to facilitate blue observations.
Subsections
Next: Energetics of Sprites-Observations
Up: Sprites, Blue Jets, and
Previous: Elves
Matt Heavner
2002-02-13