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Longitudinal biases in the Seychelles Dome simulated by 35 ocean‐atmosphere coupled general circulation models
Author(s) -
Nagura Motoki,
Sasaki Wataru,
Tozuka Tomoki,
Luo JingJia,
Behera Swadhin K.,
Yamagata Toshio
Publication year - 2013
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1029/2012jc008352
Subject(s) - thermocline , upwelling , dome (geology) , geology , equator , climatology , kelvin wave , oceanography , atmosphere (unit) , coupled model intercomparison project , sea surface temperature , ocean general circulation model , climate model , general circulation model , climate change , latitude , geography , meteorology , geomorphology , geodesy
The Seychelles Dome refers to the shallow climatological thermocline in the southwestern Indian Ocean, where ocean wave dynamics efficiently affect sea surface temperature, allowing sea surface temperature anomalies to be predicted up to 1–2 years in advance. Accurate reproduction of the dome by ocean‐atmosphere coupled general circulation models (CGCMs) is essential for successful seasonal predictions in the Indian Ocean. This study examines the Seychelles Dome as simulated by 35 CGCMs, including models used in phase five of the Coupled Model Intercomparison Project (CMIP5). Among the 35 CGCMs, 14 models erroneously produce an upwelling dome in the eastern half of the basin whereas the observed Seychelles Dome is located in the southwestern tropical Indian Ocean. The annual mean Ekman pumping velocity in these models is found to be almost zero in the southern off‐equatorial region. This result is inconsistent with observations, in which Ekman upwelling acts as the main cause of the Seychelles Dome. In the models reproducing an eastward‐displaced dome, easterly biases are prominent along the equator in boreal summer and fall, which result in shallow thermocline biases along the Java and Sumatra coasts via Kelvin wave dynamics and a spurious upwelling dome in the region. Compared to the CMIP3 models, the CMIP5 models are even worse in simulating the dome longitudes.