Cite
The interaction between synoptic-scale balanced flow and a finite-amplitude mesoscale wave field throughout all atmospheric layers: weak and moderately strong stratification.
MLA
Achatz, U., et al. “The Interaction between Synoptic-Scale Balanced Flow and a Finite-Amplitude Mesoscale Wave Field throughout All Atmospheric Layers: Weak and Moderately Strong Stratification.” Quarterly Journal of the Royal Meteorological Society, vol. 143, no. 702, Jan. 2017, pp. 342–61. EBSCOhost, https://doi.org/10.1002/qj.2926.
APA
Achatz, U., Ribstein, B., Senf, F., & Klein, R. (2017). The interaction between synoptic-scale balanced flow and a finite-amplitude mesoscale wave field throughout all atmospheric layers: weak and moderately strong stratification. Quarterly Journal of the Royal Meteorological Society, 143(702), 342–361. https://doi.org/10.1002/qj.2926
Chicago
Achatz, U., B. Ribstein, F. Senf, and R. Klein. 2017. “The Interaction between Synoptic-Scale Balanced Flow and a Finite-Amplitude Mesoscale Wave Field throughout All Atmospheric Layers: Weak and Moderately Strong Stratification.” Quarterly Journal of the Royal Meteorological Society 143 (702): 342–61. doi:10.1002/qj.2926.