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Volume 14, issue 22
Atmos. Chem. Phys., 14, 12133-12142, 2014
https://doi.org/10.5194/acp-14-12133-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 14, 12133-12142, 2014
https://doi.org/10.5194/acp-14-12133-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 18 Nov 2014

Research article | 18 Nov 2014

Characteristics and sources of gravity waves observed in noctilucent cloud over Norway

T. D. Demissie et al.
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Cited articles  
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, 2009a.
Baumgarten, G., Gerding, M., Kaifler, B., and Müller, N.: A trans-European network of cameras for observation of noctilucent clouds from 37° N to 69° N, Proceedings 19th ESA Symposium on European Rocket and Ballon Programmes and Related Research, Bad Reichenhall, Germany, 7–11 June 2009, 2009b.
Chandran, A., Rusch, D. W., Palo, S. E., Thomas, G. E., and Taylor, M. J.: Gravity wave observations in the summertime polar mesosphere from the cloud imaging and particle size (CIPS) experiment on the AIM spacecraft, J. Atmos. Sol.-Terr. Phys., 71, 285–288, 2009.
Chandran, A., Rusch, D. W., Merkel, A. W., Palo, S. E., Thomas, G. E., Taylor, M. J., Bailey, S. M., and Russell III, J. M.: Polar Mesospheric Cloud structures observed from the CIPS experiment on the AIM spacecraft: atmospheric gravity waves as drivers for longitudinal variability in PMC occurrence, J. Geophys. Res., 115, D13102, https://doi.org/10.1029/2009JD013185, 2010.
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Summertime gravity waves detected in noctilucent clouds (NLCs) between 64◦ and 74◦N are found to have a similar climatology to those observed between 60◦ and 64◦N, and their direction of propagation is to the north and northeast as observed south of 64◦N. However, a unique population of fast, short wavelength waves propagating towards the SW is observed in the NLC. The sources of the prominent wave structures observed in the NLC are likely to be from waves propagating from near the tropopause.
Summertime gravity waves detected in noctilucent clouds (NLCs) between 64◦ and 74◦N are...
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