When Will Florida Be Underwater From Sea Level Rise?

Sea level rise is a growing concern, particularly in coastal regions like Florida. While the state being entirely “underwater” is a complex scenario, significant landscape and community alterations are anticipated. This article explores the scientific mechanisms driving sea level changes, Florida’s vulnerabilities, projections for its coastlines, and adaptation strategies.

The Mechanics of Rising Seas

Global sea levels are rising primarily due to two physical processes linked to a warming planet. The first is thermal expansion: as ocean water absorbs heat, its volume increases. Even small temperature changes lead to considerable volume increases.

The second major contributor is the melting of land-based ice, including glaciers and vast ice sheets in Greenland and Antarctica. As these ice masses melt, the water flows into the oceans, directly adding to their total volume. Human activities, particularly greenhouse gas emissions, are accelerating these processes, leading to an observed increase in the rate of global sea level rise.

Florida’s Unique Susceptibility

Florida’s geography and geology make it particularly sensitive to rising sea levels. A substantial portion of the state’s landmass lies at a very low elevation, often just a few feet above current sea level. This renders large areas vulnerable to inundation even with modest increases in ocean levels.

The state’s porous limestone bedrock significantly compounds its vulnerability. This permeable rock allows saltwater to intrude inland, both over the surface and through the ground. This subsurface intrusion can contaminate freshwater aquifers, a primary drinking water source, and affect underground infrastructure. This geological characteristic also contributes to “sunny day flooding,” where streets flood during high tides even without rain, as water pushes up through the porous ground.

Florida also has one of the longest coastlines in the contiguous United States, exposing extensive land to rising waters. Coastal areas have experienced substantial development, resulting in high population densities and extensive infrastructure along the shoreline. This combination of low elevation, porous geology, vast coastline, and dense coastal development intensifies the risks associated with sea level rise.

Timelines and Projections for Florida

Sea levels across Florida have risen significantly over past decades. Since 1950, sea levels in some parts of the state are approximately 8 inches higher. In Miami, sea levels have risen about 8 inches since 1992, with the rate accelerating to roughly 1 inch every three years over the last decade in areas like Virginia Key.

Future projections for sea level rise in Florida vary based on different scenarios for greenhouse gas emissions. The Southeast Florida Regional Climate Change Compact projects sea levels to be 10 to 17 inches higher by 2040, relative to 2000 levels. By 2070, these projections indicate a potential rise of 21 to 54 inches, and by 2120, a range of 40 to 136 inches is anticipated.

Specific regions face challenges. In Miami, another foot of rise is expected within 30 years, with the subsequent foot potentially occurring in less than 10 years due to accelerating impacts. The Tampa Bay region could experience an additional 1 to 2.5 feet of sea level rise by 2050, with projections for 2100 ranging from 2 to 8.5 feet. For the Everglades, a 4-foot rise by 2100 could submerge large portions of the park during high tides.

These increases mean more frequent and severe tidal flooding, known as “King Tides,” which already impact daily life in many coastal communities. Saltwater intrusion into freshwater aquifers and deeper into the Everglades is an ongoing concern, threatening drinking water supplies and natural habitats. While near-term projections out to 2050 are considered more certain, long-term projections beyond that period carry greater uncertainty, particularly concerning the rate of ice sheet melt.

Adapting to a Changing Coastline

Florida communities are developing strategies to respond to ongoing sea level changes. Adaptation measures focus on living with changes, encompassing structural and natural solutions. Elevating existing structures and constructing new buildings on higher foundations are common approaches.

Traditional defenses like seawalls are considered, though their effectiveness can be limited by Florida’s porous limestone, which allows water to seep underneath. Restoring natural coastal habitats, such as mangrove forests, oyster reefs, and dunes, offers a natural defense by absorbing wave energy and providing ecological benefits. Innovative solutions like “Living Seawalls,” designed to mimic natural structures and support marine life, are also explored.

Improving drainage systems and implementing land-use planning that discourages new development in highly vulnerable areas are part of comprehensive adaptation efforts. Addressing saltwater intrusion involves building salinity control structures at canal entrances and restoring canals with plug barriers to separate fresh and saltwater. Local and state governments, including Miami-Dade County and the Florida Office of Resilience and Coastal Protection, are spearheading these initiatives. These responses also consider economic and social implications, recognizing potential property value impacts and the need to address displacement for vulnerable populations.