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Average annual rainfall in the Everglades is approximately 62 inches (160 cm), though fluctuations of precipitation are normal. [7] Droughts, floods, and tropical storms are normal occurrences in the area. [ 8 ]
Intense daytime heating of the ground causes the warm moist tropical air to rise, creating the afternoon thundershowers typical of tropical climates. 2:00 pm is the mean time of daily thundershowers across South Florida and the Everglades. Late in the wet season (August and September), precipitation levels reach their highest levels as tropical ...
Coinciding with the dedication of Everglades National Park, 1947 in south Florida saw two hurricanes and a wet season responsible for 100 inches (250 cm) of rain, ending the decade-long drought. Although there were no human casualties, cattle and deer were drowned and standing water was left in suburban areas for months.
The more you learn about Everglades National Park, ... August 19, 2023 at 5:07 AM. ... It gets about 60 inches of rain a year, ...
Over 20 inches of rain was clocked at Miami-Dade College - Hialeah Campus, over 19 inches in the Everglades, over 18 inches at the University of Miami and 13.51 inches at Miami Beach.
The heaviest rainfall to occur in 24 hours was measured in Yankeetown during Hurricane Easy (1950), 38.70 inches (983 mm). This is also the highest known point storm total maximum related to any tropical cyclone which has impacted Florida, [ 21 ] and by itself would be the highest known rainfall total for any month from any location within Florida.
This year, Port Everglades won a $32 million Resilient Florida Infrastructure Grant from the state which will fund a project to replace the aging bulkheads on the north end of the port. The new ...
Annual rainfall is projected to decrease across the Everglades National Park causing a hydrologic change across the entire region. Dry vegetative communities will outnumber hydric vegetative communities in this particular area. [39] Furthermore, a one-degree increase in atmospheric temperature is the result of a doubling of atmospheric CO 2.