Tropical influence on boreal summer mid-latitude stationary waves

• Published in: Climate dynamics 2011-11, Vol.37 (9-10), p.1783-1798
• Main Authors: Douville, Hervé, Bielli, S., Cassou, C., Déqué, M., Hall, N. M. J., Tyteca, S., Voldoire, A.
• Format: Article
• Language: English
• Subjects: Atmospheric circulation; Atmospheric models; Case studies; Climate; Climate models; Climatology; Climatology. Bioclimatology. Climate change; Drought; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Exact sciences and technology; Experimental design; External geophysics; Geophysics/Geodesy; Greenhouse gases; Heat waves; Latitude; Marine; Meteorology; Monsoons; Ocean temperature; Ocean, Atmosphere; Oceanography; Sciences of the Universe; Sea surface temperature; Summer
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-011-0997-1

While organized tropical convection is a well-known source of extratropical planetary waves, state-of-the-art climate models still show serious deficiencies in simulating accurately the atmospheric response to tropical sea surface temperature (SST) anomalies and the associated teleconnections. In the present study, the remote influence of the tropical atmospheric circulation is evaluated in ensembles of global boreal summer simulations in which the Arpege-Climat atmospheric General Circulation Model (GCM) is nudged towards 6-h reanalyses. The nudging is applied either in the whole tropical band or in a regional summer monsoon domain. Sensitivity tests to the experimental design are first conducted using prescribed climatological SST. They show that the tropical relaxation does not improve the zonal mean extratropical climatology but does lead to a significantly improved representation of the mid-latitude stationary waves in both hemispheres. Low-pass filtering of the relaxation fields has no major effect on the model response, suggesting that high-frequency tropical variability is not responsible for extratropical biases. Dividing the nudging strength by a factor 10 only decreases the magnitude of the response. Model errors in each monsoon domain contribute to deficiencies in the model’s mid-latitude climatology, although an exaggerated large-scale subsidence in the central equatorial Pacific appears as the main source of errors for the representation of stationary waves in the Arpege-Climat model. Case studies are then conducted using either climatological or observed SST. The focus is first on summer 2003 characterized by a strong and persistent anticyclonic anomaly over western Europe. This pattern is more realistic in nudging experiments than in simulations only driven by observed SST, especially when the nudging domain is centred over Central America. Other case studies also show a significant tropical forcing of the summer mid-latitude stationary waves and suggest a weak influence of prescribed observed SST in the northern extratropics. Results therefore indicate that improving the tropical divergent circulation and its response to tropical SST anomalies remains a key issue for increasing the skill of extratropical seasonal predictions, not only in the winter hemisphere but also in the boreal summer hemisphere where the prediction of heatwave and drought likelihood is expected to become an important challenge with increasing concentrations of greenho