Mongolian Mountains Matter Most: Impacts of the Latitude and Height of Asian Orography on Pacific Wintertime Atmospheric Circulation

• Published in: Journal of climate 2017-06, Vol.30 (11), p.4065-4082
• Main Authors: White, R. H., Battisti, D. S., Roe, G. H.
• Format: Article
• Language: English
• Subjects: Amplitude; Atmosphere; Atmospheric circulation; Atmospheric circulation models; Atmospheric models; Atmospheric sciences; Circulation; Climate; Experiments; General circulation; General circulation models; Height; Jet stream; Jet streams (meteorology); Latitude; Latitudinal variations; Mountains; Northern Hemisphere; Orography; Plateaus; Potential vorticity; Precipitation; Rivers; Studies; Vorticity; Wave propagation; Wavelengths; Winter circulation
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-16-0401.1

The impacts of Asian orography on the wintertime atmospheric circulation over the Pacific are explored using altered-orography, semi-idealized, general circulation model experiments. The latitude of orography is found to be far more important than height. The Mongolian Plateau and nearby mountain ranges, centered at ∼48°N, have an impact on the upper-level wintertime jet stream that is approximately 4 times greater than that of the larger and taller Tibetan Plateau and Himalayas to the south. Key contributing factors to the importance of the Mongolian mountains are latitudinal variations in the meridional potential vorticity gradient and the strength of the impinging wind—both of which determine the amplitude of the atmospheric response—and the structure of the atmosphere, which influences the spatial pattern of the downstream response. Interestingly, while the Mongolian mountains produce a larger response than the Tibetan Plateau in Northern Hemisphere winter, in April–June the response from the Tibetan Plateau predominates. This result holds in two different general circulation models. In experiments with idealized orography, varying the plateau latitude by 20°, from 43° to 63°N, changes the response amplitude by a factor of 2, with a maximum response for orography between 48° and 53°N, comparable to the Mongolian mountains. In these idealized experiments, the latitude of the maximum wintertime jet increase changes by only ∼6°. It is proposed that this nearly invariant spatial response pattern is due to variations in the stationary wavenumber with latitude leading to differences in the zonal versus meridional wave propagation.