Abstract

Tropical storms and hurricanes (collectively hereafter,tropical cyclones) are among the most destructive forces in nature. These threats are of particular concern to human populations and ecosystems of coastal areas of the southeastern United States, most especially in the State of Florida. This review begins with an overview of the effects of tropical cyclones on Florida’s most conspicuous terrestrial ecosystem—longleaf pine. Environmental factors leading to tropical cyclogenesis will also be reviewed, with a specific focus on (1) landfall history in Florida, and (2) the potential relationship between climate change and the frequency/intensity of tropical cyclones in the North Atlantic Ocean. Given its geographical distribution, it is not surprising that longleaf pine has long been impacted by tropical cyclones of the North Atlantic. Tropical cyclones are formed from a complex combination of meteorological conditions, driven initially by the release of excess heat from the surface waters of the ocean, along with an unstable atmosphere comprising air temperatures decreasing and wind speeds increasing with altitude. Among the coastal counties from Texas to Maine, those of Florida have experienced by far the highest frequency of tropical cyclones, especially the southern tip of peninsular Florida, with its most populous county (Miami-Dade) receiving 25 hits from 1900 to 2010, second only to Monroe County (32 hits) during that period. Frequencies of all categories of cyclones have increased significantly from 1850 to the present. Cyclone frequencies were significantly correlated with increases in air and ocean temperatures, both of which have increased over the past, suggesting a causal relationship with anthropogenic climate change. Of future concern is how increases in frequencies and intensities of tropical cyclones will negatively affect the structure and function of these ecologically and economically important longleaf pine ecosystems.

Highlights

  • Tropical storms and hurricanes comprise among the most formidable, destructive forces in nature

  • Because of currently enhanced sophistication of methods of measurement and computer-driven models, increasingly more is known about tropical cyclogenesis

  • The Coriolis force is synoptic in scale, increasing with distance from the Equator and exhibiting essentially no diurnal variation; this explains the virtual absence of tropical cyclones along the Equator (Figure 4)

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Summary

INTRODUCTION

Tropical storms and hurricanes ( called typhoons, but collectively hereafter, tropical cyclones) comprise among the most formidable, destructive forces in nature. As dramatic an event as was the 1980 eruption of Mt. St. Helens (Washington State, United States), its total energy yield was 1,000-fold lower than a typical single tropical cyclone.

Tropical Cyclones of the North Atlantic
TROPICAL CYCLOGENESIS
Sufficiently High Coriolis Force
Small Tropospheric Vertical Wind Shear
TROPICAL CYCLONE FREQUENCIES AND FLORIDA LANDFALL EVENTS
TROPICAL CYCLONES AND CLIMATE CHANGE
Highest category
Hurricanes Majors GTemp NHemTemp OTemp preGlobal preNHem preOcean
SUMMARY AND CONCLUSIONS
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