CUPRI SYSTEM CONFIGURATION FOR NLC-91 AND OBSERVATIONS OF PMSE DURINGSALVO-A

Citation
We. Swartz et al., CUPRI SYSTEM CONFIGURATION FOR NLC-91 AND OBSERVATIONS OF PMSE DURINGSALVO-A, Geophysical research letters, 20(20), 1993, pp. 2287-2290
Citations number
24
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
00948276
Volume
20
Issue
20
Year of publication
1993
Pages
2287 - 2290
Database
ISI
SICI code
0094-8276(1993)20:20<2287:CSCFNA>2.0.ZU;2-N
Abstract
The Cornell University Portable Radar Interferometer (CUPRI) provided nearly continuous monitoring of the mesosphere above Esrange, Sweden d uring the noctilucent cloud rocket and radar campaign of the summer of 1991 (NLC-91). CUPRI probed the mesosphere above Esrange from 78 to 9 1 km altitude with 300-meter resolution and was sensitive to the enhan ced Polar Mesospheric Summer Echoes (PMSE) that occur in the same alti tude range as NLC formations. Out of the total of 264 hours of CUPRI o bservation time, PMSE were present for 140 hours. Rocket Salvo A was f lown on the night of August 9-10 into an NLC event that occurred simul taneously with a thin and weakening PMSE layer. High-resolution Dopple r spectrograms of this PMSE event revealed sawtooth-like discontinuiti es at approximately 83 km altitude, which we interpret to be a distort ed partial reflection layer which was advected across the radar beam.