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Solving the Data Puzzle of Sea Level Rise

The new Sea Level Change Data Pathfinder highlights the diversity of datasets used to piece together the status and drivers of sea level rise.

Emily Cassidy, ESDS Science Writer

Cyndi Hall, ESDS Community Coordinator

Sea levels are rising at an average of 3.3 millimeters per year around the world. Rising seas are already having catastrophic effects in coastal communities through flooding, erosion, and storm-related hazards.

Satellite sea level observations from 1993 - present. Credit: NASA Physical Oceanography Distributed Active Archive Center (PO.DAAC)
Satellite sea level observations from 1993 to present. Credit: NASA Physical Oceanography Distributed Active Archive Center (PO.DAAC).

Scientists now have an unprecedented understanding of changing sea levels, thanks to data collected and distributed by NASA and partner space agencies. For example, international satellites have collected almost 30 years of data on sea surface height from satellite altimeters.

But no single satellite instrument can provide a complete picture of the status and drivers of rising seas around the world.

Melting ice sheets, thermal expansion of water, and terrestrial freshwater use are just some of the major factors contributing to rising sea levels. Piecing together the drivers of sea level change requires a diversity of datasets and a long time series from many satellite instruments.

The new Sea Level Change Data Pathfinder delves into many of the datasets scientists use to study the status of global and regional sea level change.

Sea Surface Height

When scientists refer to changes in sea level, they are referring to changes in the height of the mean sea surface relative to a mean sea level defined by the earth’s geoid. The earth’s geoid is defined as the mean sea surface due to the gravitational pull of solid earth on the ocean. Satellite altimeters very accurately provide measurements of sea surface height by timing a roundtrip radar signal from the satellite to the ocean surface and back to the satellite. These measurements are used to calculate Global Mean Sea Level.

Starting in August 1992, four satellite missions have provided a long time series of sea surface height: the TOPEX/Poseidon (T/P) altimetric mission, a joint effort between NASA and the French space agency Centre National d'Etudes Spatiales; Jason-1; the Ocean Surface Topography Mission (OSTM)/Jason-2; and now the ongoing Jason-3.

Launching in November, 2020, the new Sentinel-6 Michael Freilich mission is a follow-on to the Jason altimeter missions and will ensure the continuation of a decades-long record of sea level observations through at least 2030. The mission is being developed in collaboration with the European Space Agency, the European Organisation for the Exploitation of Meteorological Satellites, and NOAA.

Drivers of Sea Level Rise

The Pathfinder provides a thorough list of datasets scientists use to understand the different drivers of changing sea levels. Scientists use these datasets to piece together a sea level “budget". Some factors, like melting glaciers and thermal expansion, add to sea levels, while others, like damming freshwater on land, can take away from them. When we add up all of the factors, they should produce an estimate in line with an average observed change in sea levels, or global mean sea level rise.

The Intergovernmental Panel on Climate Change recently concluded that glacial melt and ice sheet loss are the dominant contributors to global mean sea level rise. Several satellite missions such as NASA's Gravity Recovery and Climate Experiment (GRACE), GRACE Follow-On (GRACE-FO), and Ice, Cloud and land Elevation Satellite (ICESat) and ICESat-2 are providing detailed measurements of ice loss.

Antarctica ice sheet mass loss with superimposed ice sheet velocity streamlines from 2002-2016.
Antarctic ice sheet mass loss with superimposed ice sheet velocity streamlines from 2002 to 2016. Credit: NASA's Goddard Space Flight Center.

GRACE is a joint partnership between NASA and the German space agency, Deutsche Forschungsanstalt für Luft und Raumfahrt. GRACE accurately maps variations in Earth's gravity field, including exchanges between ice sheets or glaciers and the ocean, variations in ocean currents, and groundwater storage. Changes in surface and groundwater storage can tell us about freshwater contributors to sea levels.

Another major factor driving sea level rise is thermal expansion of water. As the ocean warms, water expands. Sea surface temperature data from several missions help scientists understand how much sea temperatures are warming. Sea surface temperature data are available from the Moderate Resolution Imaging Spectroradiometer (MODIS) instruments aboard Terra and Aqua satellites, and the Visible Infrared Imaging Radiometer Suite (VIIRS) instruments aboard the Joint NASA/NOAA Suomi National Polar-orbiting Partnership (Suomi NPP) and the NASA/NOAA Joint Polar Satellite System (JPSS) NOAA-20.

The Pathfinder also provides information on vertical land motion and ocean currents, which can help inform regional trends in sea levels. Adding these pieces together gives researchers a good understanding of global sea level rise.

The Sea Level Change Data Pathfinder provides information on data availability, links to the datasets, and details on their spatial and temporal resolution. It also highlights datasets that merge multiple missions and in-situ data into cohesive long-term records.

Published October 30, 2020

Page Last Updated: Nov 2, 2020 at 1:14 PM EST