Impact of Mountains on Tropical Circulation in Two Earth System Models

• Published in: Journal of climate 2017-06, Vol.30 (11), p.4149-4163
• Main Authors: Naiman, Zachary, Goodman, Paul J., Krasting, John P., Malyshev, Sergey L., Russell, Joellen L., Stouffer, Ronald J., Wittenberg, Andrew T.
• Format: Article
• Language: English
• Subjects: Anomalies; Atmosphere; Atmospheric models; Circulation; Climate; Climate system; Convection; Curl (vectors); Dynamics; Earth; El Nino; El Nino phenomena; El Nino-Southern Oscillation event; Experiments; Fluid dynamics; Hadley circulation; La Nina; Laboratories; Monsoon circulation; Monsoons; Mountains; Orography; Precipitation; Southern Oscillation; Strength; Studies; Thermocline; Time; Topography; Tropical circulation; Tropical climate; Tropical climates; Walker circulation; Wind; Wind stress; Wind stress curl; Winds
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/jcli-d-16-0512.1

Two state-of-the-art Earth systemmodels (ESMs) were used in an idealized experiment to explore the role of mountains in shaping Earth’s climate system. Similar to previous studies, removing mountains fromboth ESMs results in the winds becoming more zonal and weaker Indian and Asian monsoon circulations. However, there are also broad changes to the Walker circulation and El Niño–Southern Oscillation (ENSO). Without orography, convection moves across the entire equatorial Indo-Pacific basin on interannual time scales. ENSO has a stronger amplitude, lower frequency, and increased regularity. A wider equatorial wind zone and changes to equatorial wind stress curl result in a colder cold tongue and a steeper equatorial thermocline across the Pacific basin during La Niña years. Anomalies associated with ENSO warm events are larger without mountains and have greater impact on the mean tropical climate than when mountains are present. Without mountains, the centennial-mean Pacific Walker circulation weakens in both models by approximately 45%, but the strength of the mean Hadley circulation changes by less than 2%. Changes in the Walker circulation in these experiments can be explained by the large spatial excursions of atmospheric deep convection on interannual time scales. These results suggest that mountains are an important control on the large-scale tropical circulation, impacting ENSO dynamics and the Walker circulation, but have little impact on the strength of the Hadley circulation.