Dynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnection

• Published in: Climate dynamics Vol. 57; no. 9-10; pp. 2615 - 2636
• Main Authors: Beverley, Jonathan D., Woolnough, Steven J., Baker, Laura H., Johnson, Stephanie J., Weisheimer, Antje, O’Reilly, Christopher H.
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.11.2021; Springer; Springer Nature B.V
• Subjects: Anomalies; Atmospheric circulation; Barotropic mode; Climatology; Earth and Environmental Science; Earth Sciences; Environmental aspects; Experiments; Geophysics/Geodesy; Heating; Mathematical models; Monsoon precipitation; Monsoons; Northern Hemisphere; Northern Hemisphere circulation; Oceanography; Planetary waves; Precipitation; Precipitation (Meteorology); Rossby waves; Seasonal forecasting; Summer monsoon; Teleconnections; Wave packets; Wave propagation; Wave trains; India; Asia; North America; Europe; Barotropic model; Circumglobal teleconnection; Indian monsoon; Seasonal forecasting; Relaxation experiment
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-021-05825-6

The circumglobal teleconnection (CGT) is an important mode of circulation variability, with an influence across many parts of the northern hemisphere. Here, we examine the excitation mechanisms of the CGT in the ECMWF seasonal forecast model, and the relationship between the Indian summer monsoon (ISM), the CGT and the extratropical northern hemisphere circulation. Results from relaxation experiments, in which the model is corrected to reanalysis in specific regions, suggest that errors over northwest Europe are more important in inhibiting the model skill at representing the CGT, in addition to northern hemisphere skill more widely, than west-central Asia and the ISM region, although the link between ISM precipitation and the extratropical circulation is weak in all experiments. Thermal forcing experiments in the ECMWF model, in which a heating is applied over India, suggest that the ISM does force an extratropical Rossby wave train, with upper tropospheric anticyclonic anomalies over east Asia, the North Pacific and North America associated with increased ISM heating. However, this eastward-propagating branch of the wave train does not project into Europe, and the response there occurs largely through westward-propagating Rossby waves. Results from barotropic model experiments show a response that is highly consistent with the seasonal forecast model, with similar eastward- and westward-propagating Rossby waves. This westward-propagating response is shown to be important in the downstream reinforcement of the wave train between Asia and North America.