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EPA's Report on the Environment: External Review Draft

Sea Level



Note to reviewers of this draft revised ROE: This indicator reflects data through 2011 (Exhibit 1) and 2012 (Exhibits 2 and 3). EPA anticipates updating this indicator in 2014.

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Click the legend to turn layers on or off. Hover your mouse over the display to reveal data. Click the "statistics" button above to add a 95% confidence interval to the display.

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Use the controls to pan or zoom the map.

  • Learn more about how to use this interactive exhibit
  • Save the complete indicator as a printer-friendly PDF
  • Download this image

Use the controls to pan or zoom the map. Click on each arrow symbol to reveal data.

Introduction

As the temperature of the Earth changes, so does sea level. Temperature and sea level are linked for two main reasons:

  1. Changes in the volume of water and ice on land (namely glaciers and ice sheets) can increase or decrease the volume of water in the ocean.
  2. As water warms, it expands slightly—an effect that is cumulative over the entire depth of the oceans.

Changing sea levels can affect human activities in coastal areas. For example, rising sea levels can lead to increased coastal flooding and erosion, which is a particular concern in low-lying areas. Higher sea level also makes coastal infrastructure more vulnerable to damage from storms. Sea level rise can alter ecosystems, transforming marshes and other wetlands into open water and freshwater systems into salt water systems. Documented consequences of sea level rise include loss of buffering against storms and floods, changes in bird populations and land cover, property losses, and infrastructure damage (Burkett et al., 2005; CCSP, 2009; Erwin, 2009; GCRP, 2009).

The sea level changes that affect coastal systems involve more than just expanding oceans, however, because the Earth’s continents can also rise and fall relative to the oceans. Land can rise through processes such as sediment accumulation (the process that built the Mississippi Delta) and geological uplift (for example, as glaciers melt and the land below is no longer weighed down by heavy ice). In other areas, land can sink because of erosion, sediment compaction, natural subsidence (sinking due to geologic changes), or engineering projects that prevent rivers from naturally depositing sediments along their banks. Changes in ocean currents such as the Gulf Stream can also affect sea levels by pushing more water against some coastlines and pulling it away from others, raising or lowering sea levels accordingly.

Scientists account for these types of changes by measuring sea level change in two different ways. Relative sea level change is how the height of the ocean rises or falls relative to the land at a particular location. In contrast, absolute sea level change refers to the height of the ocean surface above the center of the earth, without regard to whether nearby land is rising or falling.

This indicator presents trends in sea level based on measurements from tide gauges and from satellites that orbit the Earth. Tide gauges measure relative sea level change at points along the coast, while satellite instruments measure absolute sea level change over nearly the entire ocean surface. Many tide gauges have collected data for more than 100 years, while satellites have collected data since the early 1990s.

Exhibit 1 shows annual absolute sea level change averaged over the entire Earth’s ocean surface. The long-term trend is based on tide gauge data that have been adjusted to show absolute global trends through calibration with recent satellite data. Exhibit 2 shows how absolute change in sea level varies by location, while Exhibit 3 shows geographic differences in relative sea level change, highlighting the 1960 to 2012 change at 67 tide gauges along the Atlantic, Pacific, and Gulf coasts of the United States.

What the Data Show

After a period of approximately 2,000 years of little change (not shown here), global average sea level rose throughout the 20th century, and the rate of change has accelerated in recent years (Titus et al., 2009). When averaged over all the world’s oceans, absolute sea level increased at an average rate of 1.7 millimeters per year from 1880 to 2011 (Exhibit 1). From 1993 to 2011, however, average sea level rose at a rate of 2.7 to 3.2 millimeters per year—roughly twice as fast as the long-term trend. All of these trends are statistically significant, and the reliability of these conclusions is reinforced by the narrow 95 percent confidence bounds shown around the long-term reconstruction in Exhibit 1.

While global absolute sea level has increased steadily over the long term, recent trends show regional variability, and absolute sea level has decreased in some places (Exhibit 2). Relative sea level also has not risen uniformly because of regional and local changes in land movement and long-term changes in coastal circulation patterns. Relative sea level rose along much of the U.S. coastline between 1960 and 2012, particularly the Mid-Atlantic Coast and parts of the Gulf Coast, where some stations registered increases of more than 8 inches (Exhibit 3). Meanwhile, relative sea level fell at some locations in Alaska and the Pacific Northwest. At those sites, even though absolute sea level has risen, land elevation has risen more rapidly.

Limitations

  • Relative sea level trends represent a combination of absolute sea level change and any local land movement. Tide gauge measurements such as those in Exhibit 3 generally cannot distinguish between these two different influences without an accurate measurement of vertical land motion nearby.
  • Some changes in relative and absolute sea level can be due to multi-year cycles such as El Niño and La Niña, which affect coastal ocean temperatures, salt content, wind patterns, atmospheric pressure (and thus storm tracks), and currents. Obtaining a reliable trend can require many years of data, which is why the satellite record in Exhibit 1 has been supplemented with a longer-term reconstruction based on tide gauge measurements.

Data Sources

The absolute sea level trends in Exhibit 1 were provided by Australia’s Commonwealth Scientific and Industrial Research Organisation (CSIRO, 2012) and the National Oceanic and Atmospheric Administration (NOAA, 2012). These data are based on measurements collected by satellites and tide gauges.

Exhibit 2 was produced using data provided by the University of Colorado at Boulder (2013) (http://sealevel.colorado.edu). These data are based on measurements from the National Aeronautics and Space Administration’s (NASA’s) satellite altimeters.

The relative sea level trends in Exhibit 3 are based on data from NOAA (2013). NOAA publishes an interactive online map (http://tidesandcurrents.noaa.gov/sltrends/sltrends.shtml) with links to detailed data for each tide gauge.

For More Information


 

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