Although the extent of future sea-level rise remains uncertain, sea-level rise generally is anticipated to have a range of economic, social, and environmental effects on U.S. coasts. Global sea level is rising due to warming and expanding oceans, melting glaciers, and melting ice sheets in Greenland and Antarctica, among other reasons. From 1901 to 2010, global sea levels rose an estimated 187 millimeters (mm; 7.4 inches), averaging a 1.7 mm rise annually; estimates are that from 1992 to 2010, the rate increased to 3.2 mm annually. The rates of relative sea-level rise at specific locations are likely more important to coastal communities and coastal ecosystems than the global sea-level average trends. Sea levels are rising between 9 mm and 12 mm per year (0.4 inches to 0.5 inches per year) along the Mississippi delta near New Orleans and between 1 mm and 2 mm (0.04 inches and 0.08 inches, or less) per year along some coastal shorelines in Oregon and Washington. Since the beginning of the 20 th century, coastal and tidal areas have seen significant population growth and associated development and infrastructure investments. The consequences of sea-level rise are of interest to Congress not only because of the local impacts on coastal communities and ecosystems but also because of the direct and indirect impacts and risks for the federal government. Following an introduction to sea-level rise issues for policymakers, the report is divided into three primary parts: Part I describes the phenomenon of sea-level rise. It introduces key terminology, measurements, trends, and causes. (See " Part I. What Is Sea-Level Rise? ") Part II describes the types of effects that sea-level rise can have on U.S. coasts. It addresses effects on shorelines and coastal ecosystems and on coastal development and society. Part II describes federal actions to address sea-level rise and the tension between the federal role and actions taken by state, local, and private stakeholders. (See " Part II. Sea-Level Rise and U.S. Coasts .") Part III provides a primer on policy considerations. It raises considerations and questions associated with policies to address the causes and effects of sea-level rise. It also discusses federalism issues and general considerations associated with sea-level rise policies and investments. (See " Part III. Policy Considerations and Questions .") In 2010, roughly 100 million people lived in U.S. coastal shoreline counties (exclusive of the Great Lakes) and 2.9 million people resided in coastal shoreline counties of the U.S. territories. Many of these people may not be directly exposed to sea-level rise but may experience indirect effects on their communities or shoreline amenities. Of the U.S. coastal shoreline population, nearly 8 million people live in the 1% coastal flood zone (i.e., area in which the annual probability of coastal flooding is 1 in 100 or higher). Sea-level rise represents an increase in coastal flood and erosion hazards for exposed and protected shorelines, potentially expanding inland the 1% coastal flood zone. Higher sea levels may allow coastal storms to affect more people and cause more damage, which can result in broader social and economic effects. Higher sea levels increase permanent or temporary coastal land inundation, change shoreline dynamics and coastal erosion, and increase saltwater intrusion and hydrodynamic changes to coastal freshwater aquifers. These impacts are anticipated to result in more nuisance flooding and impeded drainage, more loss of lands to inundation, more shifts in habitat types (e.g., freshwater wetlands converting to brackish wetlands), less freshwater supply, and potential water-quality impairment. These changes may affect coastal species as well as coastal developments and their amenities (e.g., sandy beaches). Sea-level rise affects the federal government both directly and indirectly. Federal facilities (e.g., military installations) and federal projects, such as navigation improvements and coastal storm damage reduction projects, often are located on U.S. coasts. Federally assisted infrastructure, such as roads and bridges, and docks, also may be affected by sea-level rise; they may experience more intermittent flooding or a decrease in their useful life. Private-sector enterprises and individuals own or control large portions of coastline real estate and infrastructure. If sea-level rise contributes to flooding and associated damages, the federal government can become involved through disaster assistance and the National Flood Insurance Program (NFIP) for homeowners and businesses. Much public infrastructure is uninsured. Several federal agencies are affected by sea-level rise and address sea-level rise in their work. The following are examples of how federal agencies are involved with sea-level rise: Science . Federal entities engaged in understanding sea-level rise include the National Oceanic and Atmospheric Administration (NOAA) in the Department of Commerce and the U.S. Geological Survey (USGS) in the Department of the Interior. NOAA, USGS, and other federal agencies survey coastlines and conduct research to understand coastal processes, hazards, and resources. Flood Mitigation and Recovery . The Federal Emergency Management Agency (FEMA) in the Department of Homeland Security works to reduce flood losses through risk-mitigation activities and disaster response and recovery, including the NFIP. Federal Facilities, Projects , and Programs . The Department of Defense, the U.S. Coast Guard, and the National Aeronautics and Space Administration (NASA) have extensive coastal facilities that are central to their missions. The U.S. Army Corps of Engineers (Army Corps) in the Department of Defense also has significant civil works in coastal areas, including its navigation improvements and its coastal flood risk reduction projects. A significant number of federal agencies have projects and programs that are relevant to or used in coastal areas that may be affected by sea-level rise, such as the Department of Transportation and the Department of Housing and Urban Development. Environmental Protection and Restoration . Department of the Interior agencies (e.g., U.S. Fish and Wildlife Service, National Park Service), NOAA, Army Corps, and U.S. Environmental Protection Agency (EPA) also are involved in coastal ecosystem restoration and protection activities. Regulatory and Planning . Much private and nonfederal coastal construction may also require Army Corps and EPA permits. Coastal states and territories develop and maintain their coastal zone management programs under the federal Coastal Zone Management Act (CZMA; P.L. 92-532, 16 U.S.C. §1451-1464) as implemented by NOAA. Future development and economic growth along U.S. coasts may depend, to a certain extent, on the perceived risk of coastal hazards and the efficacy and efficiency of policies and investments at the local, state, and federal levels to mitigate that risk. Arguably, rising sea levels and extreme coastal storms during the 20 th and now 21 st centuries generally have not curtailed growth and investments along U.S. coasts. A long-standing concern has been the extent to which the federal government may contribute to vulnerable coastal development directly or inadvertently (e.g., federal disaster assistance, federal infrastructure programs, and federal tax policies). For example, some contend that local stakeholders may make decisions that benefit them under the anticipation that they will receive federal disaster assistance when coastal flooding occurs. Two descriptions of sea level are commonly used by scientists: global sea level (GSL) and relative sea level (RSL). Global sea level (GSL, sometimes global mean sea level ) is the average height of the Earth's oceans, as measured by satellite altimetry relative to a calculated reference ellipsoid. These global measurements, available since the first satellite ocean altimeters were placed in orbit in 1992, are combined so that the height of the world's oceans can be averaged into one number. The GSL value is significant because it allows scientists to measure trends, namely GSL rise, without having to consider whether the land surface is moving up or down along the coastline. Since 1992, satellites have measured an average GSL rise of about 3.2 mm per year (with a measurement error of +/- 0.4 mm per year, so that the range of GSL rise is 2.8 mm-3.6 mm per year). (See Table 1 and Figure 1 .) Thermal expansion of the oceans and melting from glaciers have been the dominant contributors to 20 th -century GSL rise. Meltwaters from the Greenland and Antarctic ice sheets have also contributed to GSL rise, and these contributions may have increased in the 21 st century. Another contributing factor comes from water storage on land—water impounded behind dams would reduce the amount of GSL rise because less water reaches the oceans, whereas groundwater pumped from wells would contribute to GSL rise because more water reaches the oceans as runoff or in other parts of the hydrologic cycle. Since the early 1990s, the satellite record has provided a relatively direct measurement of GSL. However, this record is short—about 25 years—compared with other sea-level measurements using tide gages. Tide gage records stretch back to the 18 th century in Europe, and systematic tide gage measurements began in the United States in the 19 th century. Several investigations have applied a variety of techniques to estimate the trend in GSL since the beginning of the 20 th century using tide gage data. (See Figure 2 .) The IPCC reported that even though different strategies were employed to account for changes in land motion, it is very likely that GSL rose an average of 1.7 mm per year (+/- 0.2 mm per year) from 1901 to 2010 (about 187 mm total, or approximately 7.4 inches). The IPCC also reported that it is likely that the rate of GSL rise increased from the 19 th century to the 20 th century. The average rate of 1.7 mm per year since 1901 is less than the rate measured by satellite altimeters since 1992; however, the rise in GSL has not been constant, according to the IPCC. For example, the IPCC reported that the trend of GSL rise in the satellite era is very likely higher than the average rate since 1901 but noted that it is also likely that GSL rose between 1920 and 1950 at a rate similar to that observed since 1992. Other factors complicate interpretation of satellite measurements, such as the role of volcanic eruptions. One recent study noted that the eruption of Mt. Pinatubo in 1991 had a cooling effect on the atmosphere, which affected sea-level rise, suggesting that the era of satellite measurements began in a highly anomalous environment. The study used a combination of modeling and analysis of satellite altimeter data to surmise that the Mt. Pinatubo eruption may have masked an acceleration of GSL that might otherwise have occurred. The study further concluded that barring another volcanic eruption, satellites may detect an acceleration of GSL rise in the coming decade. GSL represents the average value for the elevation of the surface of the world's oceans, but any particular location in Earth's oceans will likely differ from the average value. Several factors influence sea-surface height at any particular location on Earth. For example, average sea-surface heights off Bermuda are typically 1 meter higher than average sea-surface heights off Charleston, SC, because the Gulf Stream changes direction toward Bermuda. For the United States, average sea-surface heights are about 20 centimeters higher on the Pacific Ocean side than the Atlantic Ocean side because the water is less dense, on average, in the Pacific due to prevailing weather and ocean conditions. Overall GSL is rising, as Figure 1 , Figure 2 , and Table 1 show; however, significant regional variation in trends of sea-surface height around the globe—in addition to the factors discussed above—adds further complexity. For example, coastal communities on the U.S. West Coast did not experience significant sea-level rise from 1993 to 2012, even though the global average rose 3.2 mm per year, because the eastern Pacific Ocean exhibited a decrease in sea-surface height (shown in blue on Figure 3 ). That decrease in sea-surface height has been attributed to natural climate variability, such as El Niño, and the resulting changes to winds, ocean currents, temperature, and salinity, all of which affect sea level. However, some research indicates that the trend may have stopped and even reversed since 2012. This research indicates that another natural source of climate variability, the Pacific Decadal Oscillation (PDO), is undergoing a shift that is leading to higher sea levels in the eastern Pacific and lower sea levels in the western Pacific since 2012, the opposite of what is shown in Figure 3 . Relative sea level (RSL) refers to the elevation of sea level relative to the land surface from which it is measured. In many parts of the U.S. coastline, the elevation of the land surface is changing, due to a number of different causes. A change in RSL represents the combination of the change in land surface elevation and the change in GSL. At any two spots along the U.S. coastline, the trend in RSL value may be significantly different. This variation occurs because of the regional variation in GSL (discussed above) combined with regional variation in how the land surface elevation is changing. Figure 4 illustrates how different the change in the trend of RSL can be within the United States. As the colored dots on Figure 4 indicate, the trend and direction of RSL varies dramatically in the United States. RSL is rising at a rate of 9 mm-12 mm per year along Louisiana's Mississippi Delta region near New Orleans, and RSL is dropping along parts of the Pacific Northwest coastline and southern Alaska. The land surface is sinking in places such as coastal southern Louisiana, increasing the rate of RSL rise, and the land surface is rising in parts of Alaska, outpacing the rise of GSL. RSL rise has been recorded primarily using tide gages. In the United States, the National Water Level Observation Network, currently operated by NOAA, provides tide gage sea-level data from 210 stations, two of which date to the 1850s. The tide gage network was established to ensure that nautical maps; shoreline maps; and elevations of homes, levees, and other coastal infrastructure were accurately referenced to sea level. Trends detected in the tide gage network data, along with other sources of information, provide the long-term record of RSL for the U.S. coastlines. GSL and RSL pose different policy challenges. Figure 5 illustrates the factors contributing to GSL and RSL rise. The drivers for rising GSL since 1900 are predominantly thermal expansion of the oceans due to warming ocean water and melting glaciers and ice sheets ( Table 2 ). The oceans have warmed due to a combination of natural variability and the influence of greenhouse gas (GHG) emissions on atmospheric temperatures. Similarly, glaciers and polar ice sheets have melted since 1900 due to a combination of natural variability and GHG-induced climate change and deposition of pollutants. The global factors driving RSL change include those that influence GSL, but in some cases regional or local factors are responsible for the largest changes in RSL along the coastlines. These regional or local factors can be natural, such as the land rebounding upward after continental ice sheets melted at the end of the last ice age, or they can be due to human activities, such as groundwater pumping, oil and gas extraction, sediment compaction, land management practices, or other factors. (See Table 2 .) Understanding the relative contributions from these different drivers of RSL rise is important for crafting responses to help coastal communities predict, mitigate, and adapt to the changing risks that sea-level rise brings. According to some studies, precise satellite measurements of the Earth's energy budget and other global measurements since 1970 indicate that the net energy inflow to the climate system has increased and that the oceans have stored more than 90% of the increase in recent decades. These studies also indicate that the expansion of seawater associated with this energy storage has contributed about 40% of the associated GSL rise since 1971. Melting glaciers, combined with seawater expansion, explain about 75% of the rise in GSL over that period. The contribution to GSL rise from the Greenland and Antarctic ice sheets is considered to have increased since the early 1990s, although the precise amounts are not well understood. Global GHG emissions have increased significantly since the late 19 th century, and there is broad scientific agreement that the increased concentration of GHG in the atmosphere has exerted a discernible warming influence on both air and ocean temperatures, at least since the 1970s. Global atmospheric temperatures have risen since the late 1800s, but what portion of warming can be attributed to human activities over that time period is not precisely known. GSL has risen at an average of 1.7 mm per year since about 1880, as shown in Figure 2 . As with atmospheric temperatures, it is difficult to precisely attribute what proportion of GSL rise stems from human activities and what has been driven by natural influences (this is discussed further below in " Uncertainties in Future Global Sea-Level Rise Projections "). The three different studies of GSL rise plotted in Figure 2 show variations at the interannual and decadal-scale time spans, but overall all three studies indicate a fairly similar upward slope over the century. As mentioned above, satellite measurements show that GSL rise has averaged about 3.2 mm per year since the early 1990s, an increase compared with the 100+ year average of 1.7 mm per year. The current average rate of GSL probably is not unprecedented; studies indicate that a similar rate of GSL rise likely also occurred from 1920 to 1950. A challenge for policymakers and coastal communities is how to anticipate, plan for, and mitigate the effects of a longer-term overall rise in sea levels. The significant variations in sea-level rise occurring regionally and at the decadal time scale, such as those influenced by El Niño or the PDO, are superimposed on and may temporarily mask long-term trends of GSL rise. Policymakers may contend with a pattern of GSL rise that could look very different in the 21 st century compared to what Figure 2 shows, as the longer-term trends accumulate over time and regional trends change. The IPCC, for example, concludes that it is very likely that the rate of GSL rise in the 21 st century will exceed the rate observed in the 20 th century. Further, the IPCC states that sea level will continue to rise for centuries, with the amount dependent on future GHG emissions. In its assessment of future GSL rise, the U.S. National Climate Assessment expressed very high confidence that GSL will rise at least 0.2 meters but no more than 2.0 meters by 2100 (i.e., at least 8 inches to as much as 6.6 feet). For coastal communities, highly confident assertions that sea level will rise are significant for planning. However, the difference between a rise of 0.2 meters and a rise of 2.0 meters between now and the year 2100 could signify different approaches to planning for, mitigating, and responding to the effects of sea-level rise. This is discussed in more detail below in " Part II. Sea-Level Rise and U.S. Coasts ." Both the rate of future global sea-level rise and its exact dependence on future GHG emissions appear uncertain for several reasons. Probably the biggest uncertainty is the future behavior of the Greenland and Antarctic ice sheets. Estimates of the Antarctic ice sheet contributions to GSL rise between now and 2100 vary widely. Continued GHG-driven warming in the future could create instability in the large ice sheets of West and East Antarctica and lead to collapse. The collapse of large Antarctic ice sheets presents the largest potential for sudden GSL rise, but current scientific understanding of ice sheet dynamics does not identify what factor or factors would unambiguously lead to a rapid and unstable ice sheet retreat. In Greenland, melting has exceeded snow accumulation over the last few decades, so its ice sheet appears to have contributed to GSL rise. This trend is expected to continue and even increase in the next century. Unlike Antarctica, however, Greenland does not appear to be at risk of sudden ice sheet collapse. Because the future behavior of both the Greenland and Antarctic ice sheets is relatively uncertain, an additional GSL rise of a few tenths of a meter on top of current projections is possible in the latter half of this century. GHG-driven climate forcing appears to be the main driver for future GSL rise. This implies that policies directed toward reducing sea-level rise would need to address the issue of global GHG emissions as a long-term approach to mitigating the effects of GSL rise. However, many scientists conclude that GSL will continue to rise for centuries even if GHG concentrations in the atmosphere are stabilized and that other measures may be needed to address the consequences of such rise. In many locations along the U.S. coastline, the elevation of the land surface near the shore is changing in a vertical direction. Where the land is moving down, the rate of RSL rise increases; where the land is moving up, the rate of RSL rise decreases. Several natural and human-caused factors influence RSL rise locally. Many of these factors could be amenable to regional and local policy alternatives to mitigate risks to communities and ecosystems. Some of these factors are discussed below. Some of the changes in land elevation are caused by natural forces, such as post-glacial rebound (also called glacial isostatic adjustment, or GIA). GIA raising land elevation is occurring most rapidly where the ice was thickest in North America about 20,000 years ago, during the peak of the last ice age, in the region around Hudson Bay and in parts of the southern Alaskan coastline (see Figure 4 ). However, as the land previously buried under thick ice is now rising, land in most of the contiguous United States is sinking. This land is sinking in response to GIA because as the ice pressed down on the crust in the north 20,000 years ago, the land not buried under ice tilted up. Now the reverse is happening, and land previously tilted up is tilting back down, like a continent-sized seesaw. For much of the U.S. coastline, downward tilting is occurring at rates between 0.5 mm and 2 mm per year. For the U.S. East Coast, land subsidence from GIA is about 1 mm-2 mm per year. Policymakers cannot change GIA, but coastal communities could account for its contribution to RSL in their planning, mitigation, and response activities. Plate tectonics and natural compaction of sedimentary layers in places such as river deltas are two other naturally occurring processes that cause vertical land movement. Regional uplift in parts of the Pacific Northwest coastline is likely occurring in response to tectonic activity associated with the Cascadia subduction zone (see Figure 4 ). Loading of sediments from the Mississippi River, shallow and deep compaction of sediments, and possibly faulting are likely responsible for some of the high rates of land subsidence in southern Louisiana, including the New Orleans area. Despite the contributions from natural forces, most land subsidence in the United States is caused by human activities. (See Table 2 .) Groundwater withdrawals in excess of recharge to the aquifer from precipitation are responsible for about 80% of land subsidence in the United States. Groundwater pumped to the surface decreases pressure in the aquifer, and the aquifer system compacts, resulting in land subsidence. For example, groundwater withdrawals in the southern Chesapeake Bay region have accounted for more than half of overall land subsidence in the region—about 1 mm-5 mm per year. Combined with GIA, these withdrawals have resulted in the region having the highest rate of RSL rise on the U.S. East Coast ( Figure 6 ). On the West Coast, land subsidence due to groundwater pumping was first recognized in the Santa Clara Valley in California. At the northern end of the valley, land adjacent to San Francisco Bay dropped 2 feet-8 feet in elevation by 1969 since groundwater pumping began in the early 20 th century, resulting in 17 square miles of formerly dry land sinking below high-tide level. In some locations, oil and gas extraction also causes land subsidence. Oil and gas pumped to the surface decreases pressure in the reservoir, and the reservoir system compacts, resulting in land subsidence. Land subsidence in the Houston-Galveston area in Texas from both groundwater and oil and gas extraction has resulted in RSL rates exceeding 25 mm per year in some locations at different times in the 20 th century. Oil and gas pumping-induced subsidence is largely restricted to the production field, whereas subsidence from groundwater pumping may have a more regional effect. Land subsidence in the Houston-Galveston area and the high rates of RSL rise likely have increased the frequency and severity of flooding in the region. Land subsidence also occurs when organic rich soils (often called peats ) are drained of water for agricultural or other purposes. Organic rich soils can be up to 80%-90% water by volume. When these soils are drained, the effects of compaction, desiccation, and oxidation can result in subsidence. Reclamation of organic rich soils mainly for agricultural purposes in the Sacramento-San Joaquin Delta in California led to land subsidence of up to 25 mm-75 mm per year in places, resulting in some Delta islands subsiding as much as 15 feet below sea level. Groundwater withdrawal, oil and gas extraction, and draining of organic soils have long been recognized as factors leading to land subsidence. Land subsidence along the coastline exacerbates sea-level rise and increases the risks of flooding, seawater intrusion, and other impacts. Unlike for GIA or tectonic movements, policymakers could enact policies that mitigate land subsidence and potentially alter the rate of RSL rise along the coastlines. For example, some conclude that subsidence in the Houston-Galveston region led the Texas legislature to create the Harris-Galveston Subsidence District, which has the authority to restrict groundwater withdrawal. In the Santa Clara Valley, local management of groundwater resources reduced land subsidence that had dropped 2 feet-8 feet in elevation by 1969 caused by groundwater pumping since the beginning of the century. After a brief introduction to the effects of sea-level rise on U.S. coasts, Part II of the report is divided into the following three sections: effects on shorelines and ecosystems, which discusses how coastal processes and topography influence how U.S. shorelines and ecosystems may change with sea-level rise; effects on development and society, which describes U.S. coastal development and its coastal storm and nuisance flooding risks; and actions addressing the impacts of sea-level rise, which describes the activities of various federal agencies, existing federal coastal management statutes, and the role of public and private actions. The effects of sea-level rise on U.S. coasts can be broadly categorized as permanent or episodic inundation of low-lying lands, increased erosion and shoreline change (e.g., barrier island migration), increased impacts and damages from coastal storms, and saltwater intrusion of estuaries and aquifers. These physical effects have both environmental and societal consequences. Figure 7 illustrates how a rising sea level influences coastal processes and resources and shows some of the societal implications. A suite of potential policy response options exists for each effect. Policy choices on how to respond to sea-level rise may influence not only human behavior and investments along the coast but also what types of physical response (e.g., hard or nature-based shoreline stabilization) are undertaken to manage the impacts for undeveloped, somewhat developed, and extensively developed coastlines. For policymakers, choosing a response is challenging because of the difficult tradeoffs that each response represents (e.g., short- versus long-term costs and benefits, environmental or development losses or benefits). As previously noted, uncertainty in future rates of sea-level rise also complicates the decision context; for example, the estimated range of 0.2 meter (8 inches) to 2.0 meter (6.6 feet) of sea-level rise by 2100 makes it challenging to agree upon how to evaluate and compare the costs and benefits of alternative responses, policies, and investments. The effects of sea-level rise are dependent on a shoreline's topography and hydrodynamics. Coastal topography varies dramatically across the United States. Shorelines have varied forms—marsh, rocks, bluffs, beach, forest, and developed areas and infrastructure; each is affected differently by rising sea levels. Some shorelines are directly exposed to wave action, whereas others are sheltered. Some shorelines are highly erodible; others are resistant to erosion. Because of natural coastal processes, some less-developed and undeveloped coastal areas may not necessarily be inundated by sea-level rise; instead, these areas may adapt to rising sea levels. Recent research suggests that 70% of the coastal landscape of the northeastern United States may have some capacity to adapt to sea-level rise—that is, many low-lying areas may be able to adapt rather than be inundated (e.g., marshes may build vertically in response to sea-level rise). For example, unconsolidated sandy coasts have the capacity to adjust to changing conditions if nearby sand sources are available. The availability of sand can be influenced by forces and events that shape coastal sediment transport and dispersion. For developed and rocky areas, a direct relationship between sea-level rise and inundation is likely. This diversity in vulnerability to sea-level rise is captured by the U.S. Geological Survey's effort to assess the U.S. Atlantic, Pacific, and Gulf of Mexico coasts, as shown in Figure 8 . For small islands and their populations, the options for adjustment to higher sea levels are particularly constrained. Understanding where inundation and dynamic coastal responses may occur is significant for understanding how coasts may evolve. How coasts evolve may determine which policies and investments are likely to be most effective for adjusting to higher sea levels. In addition to sea-level rise, other local physical factors shape how higher sea levels affect shorelines. These factors include coastal slope, tidal range, wave height, sediment availability, and other geomorphic characteristics. Short-term events, such as a large storm with intense surge and wave action, may contribute to rapid and concentrated coastal land loss or, in some other cases, cause land growth through accretion. Discerning where and under what climate conditions coastal processes are dominated by short-term events, such as storms, rather than long-term processes, such as sea-level rise, is part of the challenge of anticipating the evolution of U.S. coasts. Assessing the potential effects of sea-level rise depends in part on the accuracy of coastal data and mapping, especially elevation information. Advances in research, monitoring, and data analyses—combined with greater incorporation of morphologic, ecologic, and anthropogenic factors—are anticipated to improve understanding of coastal dynamics and to enhance the efficacy of sea-level rise planning efforts. Some effects of sea-level rise are particularly hard to predict. For example, complex interactions may influence the extent to which sea-level rise contributes to coastal lagoons experiencing changes in circulation, tidal exchange, and turbidity. How coastal changes may ultimately affect societal concerns, such as commercial fishing harvests, is challenging to predict. Moreover, fisheries changes may be more influenced by factors other than sea-level rise, such as higher water temperatures, coastal development impacts on habitat, and mortality from fishing activities. Wetlands' ability to adjust to higher sea levels may depend in part on their ability to adjust vertically and to migrate inland. Inland migration is partially determined by topography, as well as by the presence or absence of human settlements and coastal flood defenses. For undeveloped coasts, the types of habitat and species in wetlands, bays, and estuaries may change with higher sea levels due to alterations in inundation frequency, salinity, and shoreline dynamics. For example, parts of a low-lying terrestrial ecosystem, such as the Florida Everglades, may transition from freshwater-dependent species to salt-tolerant species. To illustrate variation in the effects of sea-level rise, one study attempted to identify how six coastal estuaries in Florida would lose or gain certain coastal terrestrial ecosystems under a 1-meter sea-level rise scenario. Certain coastal habitat types—most notably coastal forest and undeveloped dry land—are likely to be lost, whereas other coastal habitats, such as mangroves, transitional saltmarsh, and saltmarsh, may become more common. Habitat transitions may take decades depending on the plant species involved. Changes in estuaries are of particular interest because of estuaries' productivity and value. Estuarine fish and shellfish species comprise a substantial portion of commercial and recreational catch. The rate of sea-level rise also may determine whether the coasts experience rapid and irreversible change or whether marshes, beaches, and barrier islands are able to adapt. For example, slower rates of sea-level rise may allow for some coastal ecosystems (mangroves, estuarine beach, and ocean beach) to adjust and persist. However, these ecosystem types may convert into open water with faster rates of sea-level rise. The relatively rapid rate of RSL rise in portions of Louisiana and the low elevation of coastal lands make portions of the state particularly susceptible to the conversion of land into open water. How sea-level rise may alter coastal erosion is a function of the land forms and the nearshore hydrodynamics (e.g., the changing role of reefs and wetlands in dampening wave energy as the result of higher water levels and potential changes in storm surges). The extent to which erosion can be attributed to sea-level rise versus other human activities (e.g., dredged navigation channels, shoreline armoring, inland dams' capture of sediment) is often difficult to distinguish. For the mid-Atlantic, erosion is anticipated to dominate changes in shoreline position in response to sea-level rise and storms over the next century. For some higher sea-level rise scenarios, some barrier islands may undergo significant changes, such as segmentation or rapid island migration. Research on coastal erosion in Hawaii found that shoreline change rates varied greatly around each island; the study estimated that the average shoreline recession in 2050 would be nearly twice the historical extrapolation of past recession rates. In addition to the anticipated effects of sea-level rise on shorelines and coastal ecosystems, sea-level rise may have broader societal implications through its effects on developed areas of the U.S. coast. For developed coastal areas, higher relative sea levels can increase the frequency and duration of nuisance flooding, as well as contribute to the risk associated with coastal storms. Saltwater intrusion into estuaries and aquifers may also affect freshwater availability for coastal communities. (For more, see the box "Sea-Level Rise and Groundwater.") Sea-level rise may pose particular physical, economic, and cultural challenges for islands and their economies (e.g., Hawaiian islands, Florida Keys) as well as the islands of U.S. territories and freely associated states. Some U.S. coastal activities and developments are located at the coast due to necessity, such as ports and fishing operations and certain military installations, or for cultural reasons, such as communities of indigenous coastal peoples. Other investors and households choose to locate on the coast. The recreational, aesthetic, and lifestyle amenities of the coasts often are a particular attraction. Some coastal areas are known for high property values and incomes. Other coastal areas have populations with more limited economic means or are otherwise considered to be socially vulnerable; these groups may have fewer resources available to prepare for sea-level rise or to cope with some of the consequences. U.S. states vary in how much of their coasts are developed, intermediately developed, undeveloped, or actively conserved. For example, along the Atlantic coast, the jurisdictions (including areas that are tidally influenced) with the highest percentage of developed lands within 1 meter of sea level are the District of Columbia (82%), Connecticut (80%), and New York (73%). The Atlantic coastal states with the most land within 1 meter of sea level that is either undeveloped or conserved are Maryland (65%), North Carolina (58%), and Georgia (57%). Many factors shape development patterns, including state and local restrictions on land use and coastal structures, as well as demand and financing for such development. Land use in the United States, other than federal lands, is the jurisdiction of state and local governments. Similarly, state and local entities adopt building requirements and building codes (although some federal programs may require compliance with certain standards and requirements). Some states have considerably more assets, people, and businesses at risk than others. For example, many of Florida's coastal counties have vulnerable roads, ports, airports, and energy facilities and a significant coastal recreation economy, as well as significant population centers and private property, which may be impacted by rising sea levels. For a discussion of the implications of sea-level rise for California's shorelines and the state's water supply system, see "California and Sea-Level Rise" box. Sea-level rise exacerbates the risks associated with flooding from coastal storms and precipitation. The extent to which sea-level rise may increase the risk of flooding from coastal storms to developed areas depends on the specifics of the storm (e.g., occurrence during high or low tide) as well as on the local characteristics of the coast. In some locations, new coastal and tidal areas may be at risk of coastal storm flooding due to higher seas allowing storm surge and floodwaters to penetrate further inland. Sea-level rise also may increase flood damages by inhibiting drainage of precipitation and floodwaters in low-lying areas. Coastal storms can result in some of the most expensive natural disasters in the United States; therefore, potential increases in damages may raise federal, state, and local financial concerns related to disaster response and recovery. A U.S. Environmental Protection Agency report using climate change projections estimated the potential future economic impacts of combined storm surge and sea-level rise on U.S. coastal property. The report estimated that cumulatively during this century (2000-2100), adaptation to and damages from the combined coastal flood hazard to infrastructure and property could cost $0.8 trillion in the United States; these costs represent investments in cost-effective protective measures, storm damages (not addressed by the protective measures), and abandoned property. Sea-level rise increases flood risk by increasing the flood hazard from storms and precipitation; the higher hazard means that more coastal areas are more vulnerable. Flood and other types of natural-disaster risk are often expressed as a probabilistic function of a hazard, which is the local threat of an event (e.g., probability of a Category 5 hurricane storm surge); vulnerability, which allows a threat to cause consequences (e.g., level of protection and performance of shore-protection measures); and consequences of an event (e.g., loss of life, property damage, economic loss, environmental damage, reduced health and safety, and social disruption). For sea-level rise, some stakeholders promote policies to reduce the hazard (e.g., climate change mitigation, reduced groundwater withdrawal). Others are interested in reducing vulnerability (e.g., shore-protection measures, storm-surge gates). Other stakeholders support policies to reduce consequences through hazard-mitigation measures, such as development restrictions, building codes, flood-proofing of structures, buyouts of vulnerable properties, and improved evacuation routes. Relative sea-level rise contributes not only to flooding from large storms but also to the incidence and duration of lesser flood events (e.g., regular flooding during high tides); these events are known as nuisance flooding, because a main impact is public inconvenience, or sometimes referred to as "sunny day" flooding because the flooding often is not associated with a storm or precipitation. Nuisance flooding often consists of shallow flooding of infrastructure and buildings, as shown in Figure 11 . According to NOAA's 2014 report, Sea Level Rise and Nuisance Flood Frequency Changes around the United States , nuisance flooding has increased dramatically in many U.S. coastal regions since the mid-20 th century. Some scholars argue that the widespread, cumulative annualized costs associated with regular nuisance flooding may be much greater than the costs associated with the annual average flood damages from larger storms. Nuisance or minor flooding can also contribute to environmental change in affected areas. Nuisance flooding, when considered as a single event, is high probability but relatively low consequence; its full impacts are often due to the cumulative damages from repeated nuisance flooding. Although this flooding may be regularly repeated, it often may fall outside the purview or priorities of many federal disaster programs and efforts, which target their efforts on events that overwhelm local and state emergency response resources or on more disruptive and costly events. Decisionmakers in developed areas subject to nuisance flooding and other persistent sea-level rise impacts are turning to a variety of engineering solutions to cope with the near-term impacts. These solutions include adding pumping capacity and control valves to storm sewers; armoring sewer systems to keep storm water out; raising roadways; using gravity, injection wells, and trenches to drain neighborhoods; adding salinity control structures; and injecting water into aquifers to retard salinity intrusion. Decisionmakers in these areas also are employing public communication campaigns and developing public health efforts, as well as using public acquisition of at-risk properties in some instances. Adjusting to sea-level rise presents an array of policy challenges and raises federalism questions regarding decisionmaking and responsibility. Part of the reason that the federal response to sea-level rise is particularly challenging is that regulations for coastal land use and requirements for coastal buildings and developments often are central to adjustment choices. According to a 2009 report by the U.S. Climate Change Science Program, Key opportunities for preparing for sea level rise include: provisions for preserving public access along the shore; land-use planning to ensure that wetlands, beaches, and associated coastal ecosystem services are preserved; siting and design decisions such as retrofitting (e.g., elevating buildings and homes); and examining whether and how changing risk due to sea-level rise is reflected in flood insurance rate maps. For coastal developments, the fundamental question for public and private decisionmakers is under what circumstances to protect, accommodate, or retreat in light of sea-level rise and other coastal hazards and their risks. In general, restrictions on private land-use decisions are largely the domain of local and state governments. Similarly, the requirements for coastal developments (e.g., required coastal setbacks) and buildings (e.g., building codes related to elevation of structures and equipment) have been set by local and state governments. The federal government, however, bears part of the financial burden associated with the consequences of coastal flooding through its disaster assistance and the National Flood Insurance Program (NFIP). A challenge will be that the options some local stakeholders may want to pursue may not be affordable or sustainable in the long run or when evaluated from a national perspective. That is, local stakeholders may make decisions that produce benefits for them if they anticipate being protected from negative outcomes; this is known as a "moral hazard" problem. For example, local entities may approve coastal developments that are at risk and make related public infrastructure investments in roads, schools, water systems, and the like, if the local entities believe federal disaster assistance (and related federal tax treatment of disaster losses) would be available when a coastal disaster occurs. This is also the case for decisionmaking by private interests. Some of the burden of the risk is transferred from the private interest and local government to the federal taxpayers. Another aspect that may be shaping decisionmaking behavior is a decision bias to underrate the risks, especially related to low-probability, high-consequence events such as large coastal storm surges. A public policy challenge related to sea-level rise is the intergenerational transfer of risk. Sea-level rise trends indicate that the coastal community will likely be at more risk in 25 years and 50 years. To not develop because of those future risks would represent a decision to forgo current use and enjoyment benefits to avoid future costs. Some view this as an unnecessary sacrifice given the uncertainty related to sea-level rise at the end of the 21 st century and the ability to adapt to some sea-level rise. For others, this choice would be altering current practices to reduce the potential consequences of sea-level rise for future generations. For Congress, a related policy question is to what extent federal programs, regulations, and funding influence how coasts develop, redevelop after extreme events, and respond to coastal erosion and shoreline dynamics. For example, most communities in the United States adopt minimum floodplain management standards as a condition of their participation in the NFIP. Other examples of how federal programs are directly involved in preparing for sea-level rise are described in the box "Selected Examples of Sea-Level Rise-Related Federal Action Since 2012" and the later box on the "Proposed 'Living Shoreline' General Permit." In addition to federal agencies that are directly involved in sea-level rise science and research and coastal regulatory activities, several federal agencies are indirectly involved in coastal projects and programs that address or could respond to, be affected by, or be exacerbated by sea-level rise. The effect of these federal actions will be determined as they are implemented. The primary federal statutes that directly address coastal development pressures are the Coastal Zone Management Act of 1972, as amended (CZMA, P.L. 92-532, 16 U.S.C. §1451-1464) and the Coastal Barrier Resources Act of 1982, as amended (CBRA, P.L. 97-348 ). CBRA designates undeveloped coastal barriers and adjacent areas. Most federal spending that would support additional development is prohibited in the CBRA designated areas. Under the CZMA, NOAA approves the coastal zone management programs developed by participating coastal states and U.S. territories and provides limited funding for coastal zone planning and management. The CZMA was enacted to encourage planning to protect natural resources while fostering wise development in the coastal zone. The CZMA recognizes that states (and, in some states, local government) have the lead responsibility for planning and managing their coastal zones. The CZMA authorizes grants to states and territories to develop and implement coastal management programs to address competing development, economic, and recreation pressures. Thirty-four of the 35 eligible states and 5 territories participate in CZMA. CZMA grants can be used for numerous CZMA-defined coastal zone enhancement objectives, including managing the effects of sea-level rise and reducing threats to life and property. Participating states and territories have developed widely varying programs that emphasize different elements of coastal management. The state programs are intended to discourage unwise development in flood-prone and exposed areas and to encourage protection of natural protective features along the coast, including beach systems, coastal barriers, and wetlands. For more on the act, see CRS Report RL34339, Coastal Zone Management: Background and Reauthorization Issues , by Harold F. Upton. The CBRA and subsequent amendments to it have designated undeveloped or relatively undeveloped coastal barriers and adjacent areas, where most federal spending that would support additional development is prohibited. There are 585 of these "system units" encompassing nearly 1.3 million acres of land and associated aquatic areas. The units are along the Gulf of Mexico, the Atlantic Coast, and the Great Lakes and around Puerto Rico and the U.S. Virgin Islands. Every CBRA unit is identified in law and with a reference to a map. The designation of units and the drawing of boundaries have been contentious for some units. Only Congress can modify the unit boundaries, and it has enacted numerous site-specific amendments. This program does not prohibit or regulate any activity; it merely prohibits the federal government and federal programs from being used to support additional development within any designated unit. Even with the CBRA prohibitions on federal programs, development has occurred at some units, especially along the southeast Atlantic coast. Also, CBRA does not preclude federal expenditures to restore designated units to former levels of development after natural disasters (e.g., reconstruction of roads and water or sewer systems to former dimensions and capacity). In addition to system units, the CBRA system also includes 272 "otherwise protected areas" encompassing 1.9 million acres, which generally coincide with existing conservation or recreation areas, such as state parks and national wildlife refuges. Unlike the broader prohibitions of the system units, the only CBRA spending prohibition in these areas is the prohibition on federal flood insurance. Decisions of how to respond to coastal hazards are largely made by individual landowners, communities, and states. The result is a wide variety of responses across the United States. Historically, landowners and communities facing coastal erosion and coastal flood risks have invested in protection, typically using hard coastal defenses, such as seawalls or groins, or nonstructural approaches, such as dune construction and beach replenishment. Some researchers estimate that as much as 14% of the shoreline of the contiguous United States on the Pacific Ocean, Atlantic Ocean, and Gulf of Mexico has hardened infrastructure, such as seawalls, jetties, and groins. Much of this shoreline armoring has occurred along the sheltered shorelines of the Atlantic and Pacific coasts (e.g., estuaries, lagoons, tidally influenced rivers). According to NOAA, if shoreline hardening continues at the current rate of around 200 kilometers per year (125 miles per year), nearly one-third of the contiguous U.S. shoreline may be hardened by 2100. Hardened shorelines generally support fewer species than the more complex habitats of natural shorelines and may require additional financial investments in operation and maintenance and in rehabilitation and replacement. Given some of the less-desirable unintended effects of coastal armoring (e.g., beach loss following seawall or jetty construction), alternative means to manage erosion and reduce storm-surge impacts are also being pursued, such as protection of natural dunes and bluffs and investments in oyster-reef restoration or marsh creation. Researchers have identified that 50% of the tidal wetlands of the South Atlantic and Gulf of Mexico are threatened by potential future hardening based on population, development, and storm trends. Although softer approaches to shoreline stabilization may require maintenance investments over time (e.g., replantings), they often become more stable as plants, roots, or oyster reefs grow. Many private and local government efforts to manage erosion require a federal permit under the Clean Water Act. Advocates for nature-based approaches for stabilizing shorelines have argued that the current regulatory programs have favored the use of hard solutions rather than nature-based approaches. In 2016, the Army Corps of Engineers proposed a general permit for "living shorelines" that may facilitate the permitting, and therefore the adoption, of nature-based approaches for managing coastal erosion. (For more on this proposal, see the box "Proposed 'Living Shoreline' General Permit.") Sea-level rise raises several questions: What does sea-level rise portend for future economic development of U.S. coasts? How does sea-level rise affect the safety and quality of life of coastal residents? How does sea-level rise alter the coastal ecosystems and potentially alter the benefits that society derives from those ecosystems, such as recreation and commercial fisheries? Near-term choices on managing and adapting to sea-level rise have the potential to significantly shape the responses to these questions and the future of U.S. coastal development. General categories of policy options related to sea-level rise include the following: Maintaining the status q uo . Current government programs, policies, and funding would continue. Reducing the g lobal r ise in sea l evel . Policies for addressing the human activities influencing sea-level rise could include pursuing domestic and international GHG-mitigation efforts. Reducing the r elative r ise in sea l evel . Policies to address the local or regional drivers of sea-level rise could focus on activities that contribute to land subsidence. Reducing v ulnerabilities to sea-level r ise . Policies could foster reducing vulnerability to the effects of sea-level rise (e.g., coastal flood risk reduction projects using dunes or storm-surge gates). Policies also could attempt to foster environmental and social resilience; these policies could include protection of certain coastal habitats, including those that contribute to natural coastal flood defenses. Reducing c onsequences of sea-level r ise . Policies could promote actions that reduce the consequences of the effects of sea-level rise. These actions could include various hazard-mitigation measures, such as development restrictions, building codes, flood-proofing of structures, buyouts of vulnerable properties, and improved evacuation routes. For all of the policy options, there are the underlying questions of the policies' costs and benefits and of who will bear the costs of not pursuing or pursuing the policies. Future rates and levels of sea-level rise are uncertain and likely will be determined by a complex mix of phenomena and activities. This uncertainty complicates public and private decisionmaking regarding policies and investments related to coastal development and protection. Considerations for Congress related to the causes of sea-level rise include the following: How well understood is the current and projected rate of sea-level rise? What factors contribute to changes in sea level, and which of these represent natural variability and which may be influenced by human activities? How may factors that affect sea level change in the future? What are the local, state, and federal responsibilities for managing and mitigating activities that may exacerbate the rate of relative sea-level rise? Policymakers may contend with a pattern of sea-level rise that could look very different in the 21 st century compared to the 20 th century. Global sea levels may rise at least 0.2 meters (about 8 inches) but could rise 10 times that amount, or even higher, depending on the behavior of the Antarctic and Greenland ice sheets, according to many scientists. A better scientific understanding of how the two large ice sheets will contribute to sea-level rise may assist coastal communities with their approaches to planning for, mitigating, and responding to potential impacts. Further, recognizing the multiple factors that contribute to relative sea-level rise, such as the local and regional activities that exacerbate or mitigate land subsidence, may be of first-order importance. A 2007 report of the National Academy of Sciences entitled Mitigating Shore Erosion Along Sheltered Coasts stated that "sea-level rise is chronic and progressive, requiring a response that is correspondingly progressive. Attempts to follow a 'hold the line' mitigation strategy against erosion and sea-level rise by coastal armoring will result in a steady escalation in both the costs of maintenance and the consequences of failure." The report's statement acknowledges that actions may be taken to manage the impacts of sea-level rise and that significant financial investments in protective and stabilization actions may be cost-effective for some developed areas. However, these actions will have costs, and the consequences of failure may be significant. Some responses may work well for a few decades but may eventually lose their utility or efficacy in the face of steadily higher sea levels. Communities and nature, however, have been adjusting to shoreline dynamics and coastal hazards for centuries; the current question is how to respond efficiently and effectively. Considerations for Congress associated with the impacts of sea-level rise include the following: What is the risk of sea-level rise to the nation, its population, federal facilities, federal operations, critical infrastructure and systems, and the national economy? What are the guiding principles for the federal role in coastal projects and activities given sea-level rise and other coastal hazards (e.g., what defines the boundaries and nature of the federal role in erosion control, shoreline stabilizations, and nuisance flooding)? What is the role for federal funding in adjusting to sea-level rise and its impacts given that coastal development is determined largely by local and state policies and private decisions? To what extent do federal regulations, programs, and funding influence the adoption and approaches used for managing coastal sea-level rise impacts or decisions that unintentionally exacerbate the impacts? What is the appropriate way to manage risks posed by sea-level rise to existing infrastructure, new infrastructure, and economic and social systems (e.g., multimodal transportation network)? Although most decisions about coastal land development and protection are made by states, localities, and other stakeholders, the federal government has an interest in how coasts are developing and adjusting to sea-level rise. A challenge for federal lawmakers and other policymakers is how to deal with the tension between federal efforts to manage national and federal government risks (e.g., federal disaster costs, coastal ecosystem shifts) related to sea-level rise and the local, state, and private roles in shaping coastal development and ecosystem health. States and local governments have significant discretion in coastal land use and development decisions. At the same time, local adoption of minimum floodplain management standards as a requirement for NFIP participation influences the locations and design of coastal structures. Past and future land-use, development, and building-code choices and the resulting public and private investments are factors shaping the future financial impacts of sea-level rise for the nation. Among the policy questions associated with sea-level rise facing federal policymakers are the following: In the U.S. federalist system of shared responsibilities, who is responsible for the costs associated with adjusting to sea-level rise? Is the federal role and responsibility related to coastal flood hazards clearly articulated and consistently applied across federal agencies, programs, projects, and disasters? Who is currently bearing the costs associated with sea-level rise and related coastal erosion, coastal storms, and habitat shifts? Are local, regional, and state land-use and development decisions and building requirements contributing to or eroding resilience to sea-level rise and coastal hazards, and what are the implications for the federal role in addressing sea-level rise? To what extent do federal programs transfer the risk associated with coastal development to the federal taxpayer? How does the suite of federal disaster assistance and coastal programs harm or bolster coastal resilience? Are federal investments in infrastructure and mitigation of flood damages in coastal areas coordinated? Various federal agencies are providing guidance and data to inform state, local, and private efforts to prepare for and respond to sea-level rise. Some stakeholders are concerned that insufficient attention is paid to the risk posed by sea-level rise, as well as to the existing risk associated with coastal hazards. Because of the value of coastal developments at risk from coastal flood hazards and how the risk may increase with sea-level rise, decisionmakers may invest in more coastal protections in many locations. What types of protections (hard, soft, hybrid) and policy choices (e.g., restricting human activities that exacerbate subsidence) are implemented may determine the future of U.S. coastal communities and coastal habitats. Other stakeholders are concerned that overestimating the risk of sea-level rise could result in overinvesting and overdesigning protections and mitigations to sea-level rise. Decisions about coastal land use and land protections, coastal development and infrastructure, and building codes and the resulting public and private investments can shape the future financial impacts of sea-level rise for the nation. Future growth in coastal areas may be shaped by the perceived risk from coastal hazards, such as sea-level rise and coastal storms, and by the efficacy of private and public responses to mitigate that risk. 

Summary: Policymakers are interested in sea-level rise because of the risk to coastal populations and infrastructure and the consequences for coastal species and ecosystems. From 1901 to 2010, global sea levels rose an estimated 187 millimeters (mm; 7.4 inches), averaging a 1.7 mm (0.07 inch) rise annually. Estimates are that the annual rate rose to 3.2 mm (0.13 inches) from 1992 to 2010. Although the extent of future sea-level rise remains uncertain, sea-level rise is anticipated to have a range of effects on U.S. coasts. It is anticipated to contribute to flood and erosion hazards, permanent or temporary land inundation, saltwater intrusion into coastal freshwaters, and changes in coastal terrestrial and estuarine ecosystems. Some states, such as Florida and Louisiana, and U.S. territories have a considerable share of their assets, people, economies, and water supplies vulnerable to sea-level rise. In 2010, roughly 100 million people lived in U.S. coastal shoreline counties. Increased flood risk associated with sea-level rise may increase demand for federal disaster assistance and challenge the National Flood Insurance Program. Federal programs support local and state infrastructure investments that may be damaged or impaired, such as roads, bridges, and municipal water facilities. Sea-level rise also is anticipated to affect numerous federal facilities. Global and Relative Sea Levels. Sea levels are expressed in terms of global sea levels, which is the average value of sea surface heights around the globe, and relative sea levels, which is the sea level relative to the land surface. Since 1900, expanding oceans due to warming ocean water and melting glaciers and ice sheets have been the main drivers of global sea-level rise. Oceans have warmed due to a combination of natural variability and the influence of greenhouse gas emissions on atmospheric temperatures. Similarly, glaciers and ice sheets since 1900 have been melting due to both natural variability and greenhouse gas emissions. In 2012, the U.S. National Climate Assessment expressed very high confidence in global sea levels rising at least 0.2 meters (8 inches) but no more than 2.0 meters (6.6 feet) by 2100. There are regional and local variations in the rate of sea-level rise. Regional or local factors can be natural, such as the land rebounding upward after continental ice sheets melted at the end of the last ice age, or they may be due to human activities, such as groundwater pumping, oil and gas extraction, sediment compaction, and land management practices, among others. With few exceptions, sea levels are rising relative to the coastlines of the contiguous United States, as well as parts of the Alaskan and Hawaiian coastlines. Policy Considerations. Policy choices related to sea-level rise have the potential to shape the future development and resiliency of U.S. coasts. Policy options include a continuation of current government programs and policies, actions that address the forces contributing to sea-level rise globally or locally, and actions that reduce the vulnerability to and consequences of sea-level rise on U.S. coasts. For all the policy options, there are underlying questions of costs and benefits and who bears the costs of pursuing or not pursuing the policies. A challenge for federal lawmakers is how to deal with the tension between federal efforts to manage national and federal government risks (e.g., federal disaster costs, coastal ecosystem shifts) related to sea-level rise and the local and state roles in shaping coastal development and ecosystem health. Related policy questions include the following: To what extent do federal programs, regulations, and funding influence how coasts develop and redevelop? Who is responsible for the costs associated with adjusting to sea-level rise? Who will bear the risks associated with vulnerable coastal development and infrastructure? Some stakeholders are concerned that governments at all levels are paying insufficient attention to the risks posed by sea-level rise; others are concerned that overestimating the risk of sea-level rise could result in foregoing current uses of coastal areas and promoting overinvestment and overdesign of sea-level rise mitigation and adaptation. CRS In Focus IF10468, Sea-Level Rise and U.S. Coasts, also provides a brief overview of sea-level rise science and policy options.