Articles | Volume 12, issue 4
https://doi.org/10.5194/amt-12-2139-2019
https://doi.org/10.5194/amt-12-2139-2019
Research article
 | 
08 Apr 2019
Research article |  | 08 Apr 2019

Multi-scale measurements of mesospheric aerosols and electrons during the MAXIDUSTY campaign

Tarjei Antonsen, Ove Havnes, and Andres Spicher

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Cited articles

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Alcala, C., Kelley, M., and Ulwick, J.: Nonturbulent layers in polar summer mesosphere: 1. Detection of sharp gradients using wavelet analysis, Radio Sci., 36, 875–890, 2001. a, b
Antonsen, T. and Havnes, O.: On the detection of mesospheric meteoric smoke particles embedded in noctilucent cloud particles with rocket-borne dust probes, Rev. Sci. Instrum., 86, 033305, https://doi.org/10.1063/1.4914394, 2015. a, b, c, d, e, f
Antonsen, T., Havnes, O. and Mann, I.: Estimates of the Size Distributionof Meteoric Smoke Particles From Rocket-Borne Impact Probes, J. Geophys. Res.-Atmos., 122, 12353–12365, https://doi.org/10.1002/2017JD027220, 2017. a, b
Antonsen, T., Havnes, O., and Spicher, A.: Replication Data for: Multi-scale Measurements of Mesospheric Aerosols and Electrons During the MAXIDUSTY campaign, DataverseNO, https://doi.org/10.18710/N8GF1U, V2, 2018. 
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Short summary
This paper presents measurements of changes in mesospheric aerosol populations on different length scales, as detected by the DUSTY and MUDD probes on the MAXIDUSTY-1B rocket on 8 July 2016. Identical probes recorded very different currents, which we attribute to adverse flow effects. We find a general anti-correlation for charged aerosols and electrons, but not consistently on all length scales. We conclude that there is no simple relationship between aerosols and PMSE (radar echoes).