Articles | Volume 2, issue 2
https://doi.org/10.5194/wcd-2-413-2021
https://doi.org/10.5194/wcd-2-413-2021
Research article
 | 
06 May 2021
Research article |  | 06 May 2021

Zonal scale and temporal variability of the Asian monsoon anticyclone in an idealised numerical model

Philip Rupp and Peter Haynes

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Cited articles

Amemiya, A. and Sato, K.: A two-dimensional dynamical model for the subseasonal variability of the Asian monsoon anticyclone, J. Atmos. Sci., 75, 3597–3612, https://doi.org/10.1175/JAS-D-17-0208.1, 2018. a, b, c
Battisti, D. S., Sarachik, E., and Hirst, A.: A Consistent Model for the Large-Scale Steady Surface Atmospheric Circulation in the Tropics, J. Climate, 12, 2956–2964, 1999. a
Bourassa, A. E., Robock, A., Randel, W. J., Deshler, T., Rieger, L. A., Lloyd, N. D., Llewellyn, E. T., and Degenstein, D. A.: Large volcanic aerosol load in the stratosphere linked to Asian monsoon transport, Science, 337, 78–81, 2012. a
Butler, A. H., Thompson, D. W., and Heikes, R.: The steady-state atmospheric circulation response to climate change – like thermal forcings in a simple general circulation model, J. Climate, 23, 3474–3496, 2010. a, b
Chen, G. and Plumb, R. A.: Effective isentropic diffusivity of tropospheric transport, J. Atmos. Sci., 71, 3499–3520, 2014. a
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Short summary
We study a range of dynamical aspects of the Asian monsoon anticyclone as the response of a simple numerical model to a steady imposed heating distribution with different background flow configurations. Particular focus is given on interactions between the monsoon anticyclone and active mid-latitude dynamics, which we find to have a zonally localising effect on the time-mean circulation and to be able to qualitatively alter the temporal variability of the bulk anticyclone.