Irene challenges forecasters on storm intensity
Tropical storm Irene illustrates improvements that forecasters have made in forecasting a hurricane's track. But it also highlights needed improvements in forecasting storm intensity.
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Still, based on today's understanding of how these storms work and climate simulations built on that knowledge, "future projections consistently indicate that greenhouse gas warming" will boost the average intensity of tropical cyclones around the world by 2 percent to 11 percent by 2100.Skip to next paragraph
In Pictures Hurricane Irene
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And while the overall number of storms in a given season is expected to drop by 6 percent to 34 percent by century's end, a higher proportion of the storms that do form are expected to muscle their way into the top intensity rankings.
In Irene's case, forecasters at the National Hurricane Center in Miami had a bead on the storm's path up the US East Coast by early evening last Tuesday.
As Irene began its encounter with the southern Bahamas, forecasters had the track moving across the eastern tip of North Carolina and up the eastern seaboard. Forecasts of the storm's post-Carolina track wobbled back and forth slightly as NOAA and US Air Force Reserve hurricane hunters took the storm's measure as often as once every three hours.
But the shifts were relatively small. And the storm was large – hurricane winds as far as 90 miles from the center and tropical-storm winds out to 250 miles at the storm's peak.
Where track forecasts can by off by as much as 250 miles at the fifth day out, this time Irene took no significant deviation from the path along the mid-Atlantic and Northeast coasts forecasters had indicated early in the week.
Last Tuesday's forecasts expected Irene would strike North Carolina as a major hurricane, with maximum sustained winds of at least 110 miles an hour. When the storm made landfall near Cape Lookout at 11:30 a.m. Saturday morning, however, maximum sustained winds had dropped to 85 miles an hour.
Friday morning, forecasters noticed that dry air – anathema to tropical cyclones – was moving in from the west. And the storm was encountering increasing shear – rapid changes in wind speed and direction with height. Indeed, later in the day, forecasters noted that by the time Irene reached southern New England, the storm could become a high-end tropical storm, rather than a low-end hurricane.
But the tiny differences in effect between the two, especially along exposed coastlines, prompted forecasters to stick with Irene as a weak hurricane into New England a bit longer.
As Irene's center cleared North Carolina, it moved into an increasingly hostile atmospheric environment, as well as over cooler ocean waters.
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