Indian summer monsoon variability forecasts in the North American multimodel ensemble
Bohar Singh1, Ben Cash2, James L Kinter Iii2
11George Mason University, Fairfax, VA 22031 USA.
Summary
Global coupled models show modest skill in predicting Indian summer monsoon rainfall (ISMR) and its variability. Phase 2 models offer no significant improvement over Phase 1, despite skillful sea surface temperature prediction.
Area of Science:
- Climate Science
- Atmospheric Science
- Oceanography
Background:
- The Indian summer monsoon rainfall (ISMR) is crucial for South Asia's climate and economy.
- Accurate representation of ISMR in climate models is vital for predicting regional climate variability.
- The North American Multimodal Ensemble (NMME) provides a platform for evaluating global coupled models.
Purpose of the Study:
- To evaluate the performance of NMME phase 1 and phase 2 global coupled models in simulating ISMR.
- To assess the models' ability to capture seasonal mean and interannual variability of ISMR.
- To investigate the representation of sea surface temperature (SST) and its teleconnections with ISMR.
Main Methods:
- Analysis of seasonal mean and interannual variability of ISMR from NMME:1 and NMME:2 (1982-2009).
- Evaluation over the Indo-Pacific domain using May initial conditions.
- Assessment of model-simulated SST and its relationship with rainfall, comparing with observations.
Main Results:
- The multi-model ensemble (MME) shows modest skill and systematic biases in representing ISMR.
- No significant improvement in ISMR forecast skill or variability was found in NMME:2 compared to NMME:1.
- Models skillfully predict seasonal mean SST and some teleconnections, but SST-rainfall links are overestimated, and extremes are poorly captured.
Conclusions:
- Current NMME global coupled models exhibit limitations in accurately simulating ISMR and its variability.
- The models struggle to capture observed SST-rainfall teleconnections and extreme rainfall events.
- Further improvements are needed in model physics and parameterizations to enhance ISMR representation.
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