Abstract
Projections of the potential impacts of global warming on regional tropical cyclone activity are challenging owing to multiple sources of uncertainty in model physical schemes and different assumptions for future sea surface temperatures. A key factor in projecting climate change is to derive robust signals of future changes in tropical cyclone activity across different model physical schemes and different future patterns in sea surface temperature. A suite of future warming experiments (2075-2099), using a state-of-the-art high-resolution global climate model, robustly predicts an increase in tropical cyclone frequency of occurrence around the Hawaiian Islands. A physically based empirical model analysis reveals that the substantial increase in the likelihood of tropical cyclone frequency is primarily associated with a northwestward shifting of the tropical cyclone track in the open ocean southeast of the islands. Moreover, significant and robust changes in large-scale environmental conditions strengthen in situ tropical cyclone activity in the subtropical central Pacific. These results highlight possible future increases in storm-related socio-economic and ecosystem damage for the Hawaiian Islands.
| Original language | English |
|---|---|
| Pages (from-to) | 749-754 |
| Number of pages | 6 |
| Journal | Nature Climate Change |
| Volume | 3 |
| Issue number | 8 |
| DOIs | |
| State | Published - Aug 2013 |
Funding
This work was conducted under the framework of the ‘Projection of the Change in Future Weather Extremes Using Super-High-Resolution Atmospheric Models’ supported by the KAKUSHIN and SOUSEI programmes of the Ministry of Education, Culture, Sports, Science and Technology (MEXT) of Japan. H.M. was supported by the ‘Research on Prediction of Climate and Environmental Change to Contribute to Mitigation Plan Decision Against Climate Change’ of the MRI of Japan. B.W. acknowledges the support from the Global Research Laboratory (GRL) Program of the Korean Ministry of Education, Science and Technology (MEST, 2011-0021927). Calculations were performed on the Earth Simulator. This contribution is School of Ocean and Earth Science and Technology publication No. 8917 and International Pacific Research Center publication No. 975.
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