Climate Change

The new normal: Hurricane Michael reminds us that climate change is real

By Dan Broadbent

October 10, 2018

Storms like this are undoubtedly pushing more water into the coast because sea levels are higher. So when we have these types of storms and storm surge, the storm will be pushing a higher level of water than it would 50 or 70 years ago. That is something that I’m very comfortable saying, but I think only the studies over time will play out whether the warmer oceans — because of our broader, background climate change — are fueling more higher-octane storms.

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A review of existing studies, including the ones cited above, lead us to conclude that: it is likely that greenhouse warming will cause hurricanes in the coming century to be more intense globally and have higher rainfall rates than present-day hurricanes. … the hurricane model also projects that the lifetime maximum intensity of Atlantic hurricanes will increase by about 5% during the 21st century in general agreement with previous studies.
We also conclude that it is likely that climate warming will cause Atlantic hurricanes in the coming century have higher rainfall rates than present-day hurricanes, and medium confidence that they will be more intense (higher peak winds and lower central pressures) on average. In our view, it is uncertain how the annual number of Atlantic tropical storms will change over the 21st century. … Based on our published results and as well as those of other modeling groups, we conclude that at the global scale: a future increase in tropical cyclone precipitation rates is likely; an increase in tropical cyclone intensity is likely; an increase in very intense (category 4 and 5) tropical cyclones is more likely than not; and there is medium confidence in a decrease in the frequency of weaker tropical cyclones. Existing studies suggest a tropical cyclone windspeed increase of about 1-10% and a tropical cyclone precipitation rate increase of about 10-15% for a moderate (2 degree Celsius) global warming scenario.