Free Practice Question
RC · Reading Comprehension
705-805
Short Passage - Social Science
Reading Passage
Hurricane forecasters have difficulty determining maximum sustained surface-level winds. Reconnaissance aircraft usually obtain data from a flight level of 10,000 feet. However, in 1997, reconnaissance aircraft began deploying dropwindsondes in hurricanes. These weather instruments, carrying global positioning systems and affixed to parachutes, acquire detailed data from flight level down to surface level. Near the eyewall—the ring of towering thunderstorms surrounding a hurricane's eye—the strongest winds are usually found at around 1,600 feet, about 20 percent stronger than at flight level. In the hurricanes' outer reaches, however, wind maximums are typically found at higher elevations. The data also show that, near the eyewall, winds on top of a thirty-story building average about twenty miles per hour stronger than at ground level. Given the collective dropwindsonde data, forecasters typically estimate eyewall surface-level winds at about 90 percent of flight-level winds, with surface-level winds in the outer reaches at about 78 percent.
Hurricane Mitch in 1998, however, exhibited maximum flight-level winds no stronger than 150 miles per hour, yet dropwindsondes indicated much stronger surface-level winds. In this case, Mitch appeared to be weakening from the top down; the circulation at flight levels was decreasing but had yet to decrease at surface levels. This storm is a reminder that the typical estimates often need modification based on certain real-time factors, especially convective (warm-air updraft) intensity and sea-surface temperature.
Hurricane Mitch in 1998, however, exhibited maximum flight-level winds no stronger than 150 miles per hour, yet dropwindsondes indicated much stronger surface-level winds. In this case, Mitch appeared to be weakening from the top down; the circulation at flight levels was decreasing but had yet to decrease at surface levels. This storm is a reminder that the typical estimates often need modification based on certain real-time factors, especially convective (warm-air updraft) intensity and sea-surface temperature.
The passage most strongly suggests that circulation in hurricanes
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weakens at the eyewall before it begins to weaken in the outer reaches of a storm
B
near the outer reaches is typically strongest at elevations above the usual flight level of reconnaissance aircraft
C
is typically the same from flight level down to surface level before the hurricane begins to weaken
D
is usually faster at flight level than it is at surface level after a storm has begun to weaken
E
will not increase if sea-surface temperatures remain constant
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Difficulty
705-805
Type
RC
Category