Tide gauges show that global sea level has risen about 7 inches during the 20th century, and recent satellite data show that the rate of sea-level rise is accelerating. As Earth warms, sea levels are rising mainly because ocean water expands as it warms; and water from melting glaciers and ice sheets is flowing into the ocean. Sea-level rise poses enormous risks to the valuable infrastructure, development, and wetlands that line much of the 1,600 mile shoreline of California, Oregon, and Washington. As those states seek to incorporate projections of sea-level rise into coastal planning, they asked the National Research Council to make independent projections of sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account regional factors that affect sea level.
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future explains that sea level along the U.S. west coast is affected by a number of factors. These include: climate patterns such as the El Nino, effects from the melting of modern and ancient ice sheets, and geologic processes, such as plate tectonics. Regional projections for California, Oregon, and Washington show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections. However, projections are lower north of Cape Mendocino because the land is being pushed upward as the ocean plate moves under the continental plate along the Cascadia Subduction Zone. However, an earthquake magnitude 8 or larger, which occurs in the region every few hundred to 1,000 years, would cause the land to drop and sea level to suddenly rise.
Table of Contents
|2 Measured Global Sea-Level Rise||23-32|
|3 Contributions to Global Sea-Level Rise||33-54|
|4 Sea-Level Variability and Change off the California, Oregon, and Washington Coasts||55-82|
|5 Projections of Sea-Level Change||83-108|
|6 Responses of the Natural Shoreline to Sea-Level Rise||109-136|
|Appendix A: Vertical Land Motion and Sea-Level Data Along the West Coast of the United States||153-162|
|Appendix B: Sea-Level Rise in the Northeast Pacific Ocean||163-174|
|Appendix C: Analysis of Sea-Level Fingerprint Effects||175-178|
|Appendix D: Long-Term Tide Gage Stability From Leveling Data||179-190|
|Appendix E: Cryosphere Extrapolations||191-196|
|Appendix F: Biographical Sketches of Committee Members||197-200|
|Appendix G: Acronyms and Abbreviations||201-202|
In this short video, committee member Gary Griggs shares key findings about sea-level rise projections in California, Oregon, and Washington.
The National Academies Press and the Transportation Research Board have partnered with Copyright Clearance Center to offer a variety of options for reusing our content. You may request permission to:
For most Academic and Educational uses no royalties will be charged although you are required to obtain a license and comply with the license terms and conditions.
For information on how to request permission to translate our work and for any other rights related query please click here.
For questions about using the Copyright.com service, please contact:
Copyright Clearance Center
22 Rosewood Drive
Danvers, MA 01923
Tel (toll free): 855/239-3415 (select option 1)
Loading stats for Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future...