Geoscience Reference
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Fig. 6: As in Fig. 5, but for tropical cyclones with maximum surface winds
exceeding 33 m/s at some point in their lifetime.
response to simulated ENSO variability is quite encouraging, particularly in
the Pacific regions, and also to some extent in the Indian Ocean basins.
Summary
Present-day simulations of intense tropical cyclones in the North Indian Ocean
region are being performed and assessed as a preliminary step before climate
change simulations being undertaken. While reasonable results have been
obtained so far for the North Atlantic and Northwest Pacific basins, the North
Indian Ocean simulations exhibit a substantially larger intensity bias, including
a distribution of storm intensities that is much more clustered around ~40-50
m/s than is the case for the distribution of observed (JTWC) TC intensities in
the region.
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