Like many low-lying coastal cities around the world, Miami is threatened by rising seas. Whether the majority of the cause is anthropogenic or natural, the end result is indisputable: sea level is rising. It is not a political issue, nor does it matter if someone believes in it or not.
Tidal flooding on the corner of Dade Blvd and Purdy Ave in Miami Beach in 2010. (Steve Rothaus, Miami Herald)
The mean sea level has risen noticeably in the Miami and Miami Beach areas just in the past decade. Flooding events are getting more frequent, and some areas flood during particularly high tides now; no rain or storm surge necessary .
Diving Into Data
Measurements of sea level have been taken at the University of Miami’s Rosenstiel School on Virginia Key since 1994, with certified daily measurements available online since 1996 (Virginia Key is a small island just south of Miami Beach and east of downtown Miami) . Simple linear trends drawn through annual averages of all high tides, low tides, and the mean sea level are shown below, and all three lines are about 5.2 inches (13 cm) higher in 2016 than they were in 1994.
Annual averages of high tide, low tide, and mean sea level, with linear trend lines drawn through them. The trend line slopes for each time series are labeled. [This chart was updated in Jan 2017 to include verified data through the end of 2016.]
For the following chart, the daily high water mark (highest of the two high tides each day) for 21 years is plotted. The water levels at high tides are the most relevant because that is when flooding events are more prone to occur. For reference, the average seasonal cycle is shown by the thin black line, the daily high tide values are plotted with a thin light blue line, and the thick blue line is simply a smoothed version of the thin blue line. The “lunar nodal cycle” shown by the thin red line also impacts sea level and peaks every 18.6 years (it just peaked in 2016). The highest water marks in the dataset are annotated… they have historically been associated with the passage of hurricanes, until September 2015 and October 2016 when very high water levels were reached without a storm nearby.
[This chart was updated in Jan 2017 to include verified data through the end of 2016.]
The seasonal cycle has a total amplitude of approximately 10 inches (25 cm) and is highest during September through November. It was calculated using a 31-day running mean of all 21 years of daily data. In southeast Florida, the lunar nodal cycle has a total amplitude of approximately 2.1 inches (5.3 cm) and arises due to the precession of the moon’s orbital plane relative to the sun’s plane; it was calculated using a multiple linear regression of the detrended daily data . When the LNC is on an upward swing, its effects are added to the background sea level rise, creating an apparent very rapid rise in a few years. Similarly, when the LNC is on a downward swing, it can nearly counteract the background sea level rise creating an apparent stagnation for several years. But, it is important to look at long time series and to account for this cycle when calculating trends. Aside from these regular cycles, local sea level is influenced by land-based ice melt, thermal expansion of the ocean as it warms, the strength of the Gulf Stream ocean current, among others.
Once the mean, seasonal cycle, and lunar nodal cycle are accounted for and removed from the daily water level dataset, we can calculate a linear trend. Over the past 21 years, the average high tide has increased by roughly 0.25 inches/year, which is a slightly higher estimate compared to the trend shown in the first chart using annual averages (0.22 inches/year).
Be advised that simple linear trends of noisy time series are not reliable for extrapolating very far into the future, nor are the trend values reliable for shorter time periods. Longer data records allow for greater confidence in a linear trend, but cannot account for accelerating rates.
[This chart was updated in Jan 2017 and includes verified data through the end of 2016.]
The Miami metropolitan region has the greatest amount of exposed financial assets and 4th-largest population vulnerable to sea level rise in the world. The only other cities with a higher combined (financial assets and population) risk are Hong Kong and Calcutta .
Using a sea level rise projection of 3 feet by 2100 from the 5th IPCC Report  and elevation/inundation data, a map showing the resulting inundation is shown below. The areas shaded in blue would be flooded during routine high tides, and very easily flooded by rain during lower tides. Perhaps the forecast is too aggressive, but maybe not… we simply do not know with high confidence what sea level will do in the coming century. But we do know that it is rising and showing no sign of slowing down.
Map showing areas of inundation by three feet of sea level rise, which is projected to occur by 2100. (NOAA)
An Attack from Below
In addition to surface flooding, there is trouble brewing below the surface too. That trouble is called saltwater intrusion, and it is already taking place along coastal communities in south Florida. Saltwater intrusion occurs when saltwater from the ocean or bay advances further into the porous limestone aquifer. That aquifer also happens to supply about 90% of south Florida’s drinking water. Municipal wells pump fresh water up from the aquifer for residential and agricultural use, but some cities have already had to shut down some wells because the water being pumped up was brackish (for example, Hallandale Beach has already closed 6 of its 8 wells due to saltwater contamination ).
Schematic drawing of saltwater intrusion. Sea level rise, water use, and rainfall all control the severity of the intrusion. (floridaswater.com)
The wedge of salt water advances and retreats naturally during the dry and rainy seasons, but the combination of fresh water extraction and sea level rise is drawing that wedge closer to land laterally and vertically.
In other words, the water table rises as sea level rises, so with higher sea level, the saltwater exerts more pressure on the fresh water in the aquifer, shoving the fresh water further away from the coast and upward toward the surface.
Map of the Miami area, where colors indicate the depth to the water table. A lot of area is covered by 0-4 feet, including all of Miami Beach. (Dr. Keren Bolter, Center for Environmental Studies)
An Ever-Changing Climate
To gain perspective on the distant future, we should examine the distant past. Sea level has been rising for about 20,000 years, since the last glacial maximum. There were periods of gradual rise, and periods of rapid rise (likely due to catastrophic collapse of ice sheets and massive interior lakes emptying into the ocean). During a brief period about 14,000 years ago, “Meltwater Pulse 1A”, sea level rose over 20 times faster than the present rate. Globally, sea level has already risen about 400 feet, and is still rising.
Observed global sea level over the past 20,000 years… since the last glacial maximum. (Dr. Robert Rohde, Berkeley Earth).
With that sea level rise came drastically-changing coastlines. Coastlines advance and retreat by dozens and even hundreds of miles as ice ages come and go (think of it like really slow, extreme tides). If geologic history is a guide, we could still have up to 100 feet of sea level rise to go… eventually. During interglacial eras, the ocean has covered areas that are quite far from the coastline today.
Florida’s coastline through the ages. (Florida Geological Survey)
As environmental author Rachel Carson stated, “to understand the living present, and promise of the future, it is necessary to remember the past”.
What Comes Next?
In the next 20 years, what should we reasonably expect in southeast Florida? Using observed linear trends, sea level could be around 5 inches higher in 2034, but a realistic range is more like 5-9 inches.
Year by year, flooding due to heavy rain, storm surge, and high tides will become more frequent and more severe. Water tables will continue to rise, and saltwater intrusion will continue to contaminate fresh water supplies.
This is not an issue that will simply go away. Even without any additional anthropogenic contributions, sea level will continue to rise, perhaps for thousands of years. But anthropogenic contributions are speeding up the process, giving us less time to react and plan.
Coastal cities were built relatively recently, without any knowledge of or regard for rising seas and evolving coastlines. As sea level rises, coastlines will retreat inward. Sea level rise is a very serious issue for civilization, but getting everyone to take it seriously is a challenge. As Dutch urban planner Steven Slabbers said, “Sea level rise is a … storm surge in slow motion that never creates a sense of crisis”. It will take some creative, expensive, and aggressive planning to be able to adapt in the coming decades and centuries.
Special thanks to Dr. Keren Bolter and Dr. Shimon Wdowinski for their inspiration and assistance.