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Key Largo is located at (25.106637, -80.429917 It shares the island of Key Largo with Tavernier to the southwest and North Key Largo to the northeast. U.S. Route 1, the Overseas Highway, runs the length of the community, leading north 57 miles (92 km) to Miami and southwest 97 miles (156 km) to Key West.
Much of the year's 61.9 inches (1,570 mm) of rainfall occurs during this period. Extreme temperatures range from 27 F [3] on February 3, 1917, [4] to 100 °F on July 21, 1942, (−2.8 to 38 °C), the only triple-digit (°F) reading on record; [5] the more recent freezing temperature seen at Miami International Airport was on December 25, 1989. [6]
For example, a climograph with a narrow range in temperature over the year might represent a location close to the equator, or alternatively a location adjacent to a large body of water exerting a moderating effect on the temperature range. Meanwhile, a wide range in annual temperature might suggest the opposite.
The blue numbers are the amount of precipitation in either millimeters (liters per square meter) or inches. The red numbers are the average daily high and low temperatures for each month, and the red bars represent the average daily temperature span for each month. The thin gray line is 0 °C or 32 °F, the point of freezing, for orientation.
The state-sanctioned Everglades National Park Commission proposed a national park for the Everglades, including the reefs off Key Largo. Opposition from property owners, outdoorsmen, and Monroe County Commissioners stopped the plan. When Everglades National Park was created in 1947, the boundaries did not include Key Largo or any of the reefs. [3]
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The low pressure measured from an extratropical cyclone was 28.84 inches/976.7 hPa during the Storm of the Century (1993). [3] From a tropical cyclone, the lowest pressure measured was 26.35 inches/892 hPa in the Florida Keys during the Labor Day Hurricane of 1935. [4]
The sea level has risen almost six inches (15 cm) at Key West since 1913, and one foot (30 cm) since 1850. This rise in sea level increases the volume of water in Florida Bay significantly, and increases the exchange of water between the Bay and the water over the reefs.