Articles | Volume 44, issue 1
https://doi.org/10.5194/angeo-44-331-2026
https://doi.org/10.5194/angeo-44-331-2026
Regular paper
 | 
18 May 2026
Regular paper |  | 18 May 2026

Studies of noctilucent clouds from the stratosphere during the 2024 TRANSAT balloon flight

Peter Dalin, Hidehiko Suzuki, Nikolay Pertsev, Vladimir Perminov, Linda Megner, Johan Kero, Peter Voelger, Jonas Hedin, Gerd Baumgarten, Anne Réchou, and Denis Efremov

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Cited articles

Bailey, S. M., Thomas, G. E., Rusch, D. W., Merkel, A. W., Jeppesen, C., Carstens, J. N., Randall, C. E., McClintock, W. E., and Russell, J. M.: Phase functions of polar mesospheric cloud ice as observed by the CIPS instrument on the AIM satellite, J. Atmos. Sol.-Terr. Phy., 71, 373–380, https://doi.org/10.1016/j.jastp.2008.09.039, 2009. 
Baumgarten, G.: Doppler Rayleigh/Mie/Raman lidar for wind and temperature measurements in the middle atmosphere up to 80 km, Atmos. Meas. Tech., 3, 1509–1518, https://doi.org/10.5194/amt-3-1509-2010, 2010. 
Baumgarten, G. and Fritts, D. C.: Quantifying Kelvin-Helmholtz instability dynamics observed in noctilucent clouds: 1. Methods and observations, J. Geophys. Res.-Atmos., 119, 9324–9337, https://doi.org/10.1002/2014JD021832, 2014. 
Baumgarten, G., Fiedler, J., Fricke, K. H., Gerding, M., Hervig, M., Hoffmann, P., Müller, N., Pautet, P.-D., Rapp, M., Robert, C., Rusch, D., von Savigny, C., and Singer, W.: The noctilucent cloud (NLC) display during the ECOMA/MASS sounding rocket flights on 3 August 2007: morphology on global to local scales, Ann. Geophys., 27, 953–965, https://doi.org/10.5194/angeo-27-953-2009, 2009. 
Baumgarten, G., Chandran, A., Fiedler, J., Hoffmann, P., Kaifler, N., Lumpe, J., Merkel, A., Randall, C. E., Rusch, D., and Thomas, G.: On the horizontal and temporal structure of noctilucent clouds as observed by satellite and lidar at ALOMAR (69N), Geophys. Res. Lett., 39, L01803, https://doi.org/10.1029/2011GL049935, 2012. 
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Short summary
A transatlantic scientific balloon flight (TRANSAT) was conducted in June 2024. The TRANSAT balloon floated in the stratosphere at approximately 40 km altitude between Sweden and Canada for about 4 days. An optical imager was installed on the TRANSAT balloon to study noctilucent cloud (NLC). Nearly continuous observations of NLC were obtained during the entire flight. A complex NLC structures exhibiting different motions were found to result from wind rotation with altitude between 80 and 94 km.
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