Hurricane Grace Research Paper
Meteorological history[ edit ] Map plotting the track and the intensity of the storm, according to the Saffir—Simpson scale Tropical Storm Grace originated from a large extratropical cyclone that formed along a cold front on September 27, roughly mi km east of Cape Race, Newfoundland. The storm featured relatively deep http://pinsoftek.com/wp-content/custom/human-swimming/5th-viscount-howe-essays.php around an eye-like feature.
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Although Grace was over waters normally not warm enough for tropical cyclone development, low wind shear allowed the convection to persist. A steady northeastward track was taken by the storm in response to a southerly flow over the northwestern Atlantic.
Just prior to merging, the lowest pressure in relation to the storm was recorded at mbar hPa; In Ireland, 1. This marked the second northernmost formation of a tropical storm in the Atlantic on record; only Tropical Storm Alberto of had formed farther north. The first mention http://pinsoftek.com/wp-content/custom/human-swimming/seikichi-in-sunichio-tanizakis-tattoo.php the precursor low on October 1 predicted that it would not Hufricane into a tropical or subtropical cyclone.
Over the following three days, the system was not mentioned in the NHC's tropical weather outlooks until just prior to Grace's classification. The lack of preceding outlooks was attributed to the storm's unusual location and the sparsity of data for storms in the region.]
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