2006 PSD Seminars


Understanding the Tropical Biases in GCMs: Double-ITCZ, ENSO, MJO and Convectively Coupled Equatorial Waves

Jialin Lin

NOAA ESRL and CIRES Climate Diagnostics Center

blue_bar.gif (1106 bytes)

Abstract

The tropical mean climate and tropical variability, such as the El Nino/Southern Oscillation (ENSO) and the Madden-Julian Oscillation (MJO), play a key role for weather predictions, climate predictions and climate projections. However, they are not well simulated by the state-of-the-art general circulation models (GCMs) used for predictions and projections, and the problems are generally referred to as the tropical biases. The most prominent tropical biases are the double-ITCZ problem, the ENSO problem, and the MJO problem. These tropical biases have been persisting in the last several generations of GCMs. The major difficulties for understanding and alleviating these biases are twofold:

  • They all involve some forms of feedback, such as the ocean-atmosphere feedback and the wave-heating feedback, making it difficult to determine the real cause of the bias; and
  • The biases need to be traced back to specific model characteristics, such as certain aspect of the physical parameterizations, in order to provide useful guidance on how to improve the model simulations.

Multiple-model intercomparison, when combined with in-depth feedback analysis and direct model physics evaluation, provide a good way to overcome these difficulties. It can help us to understand the physical reasons of the tropical biases, find systematic dependence of the biases on specific model characteristics, and transfer the success of some of the models to other more bias-challenged models. We will present the results of several recent studies including:

  • An analysis of the physical mechanisms of the double-ITCZ problem in 22 IPCC AR4 coupled GCMs;
  • A newly discovered coupled wave oscillator mechanism of ENSO, and its implications for the ENSO problem in coupled GCMs;
  • The MJO and convectively coupled equatorial waves simulated by 14 IPCC AR4 coupled GCMs, and GCM sensitivity experiments trying to improve these tropical intraseasonal variability.

Figure 1

Figure 2

Figures: Annual mean SST (shading) and precipitation (contour) for observation and 22 IPCC AR4 CGCMs. Contour starts at 5 mm/day with an interval of 2 mm/day. Models with heat flux adjustment are denoted by (adj). (b) shows the names used in this paper for the different geographical regions.

blue_bar.gif (1106 bytes)

Wednesday 4 October, 2006
2:00 PM (Refreshments at 1:50 pm)
PSD-South Conference Room (1D403)


Back to PSD seminar list.