Sea Level Rise Paper

As it stands today the U.S. coast of the Gulf of Mexico is losing more and more land; the amount of land lost each year may seem relatively small to the average person, but to scientists who understand the unprecedented rate at which this is happening, there is reason to be alarmed. On the U.S. coast of the Gulf of Mexico there are more reasons for the rising sea level than simply global warming and melting ice sheets or ice caps. In the Mississippi delta, for example, the oil industry is taking so much fluid (oil) out of the ground that the land is sinking and compacting further. There is also a decrease in the amount of sediment reaching the delta due to many man-made structures, such as levees, drudging, dikes, and

The loss of Louisiana coastal land is one of the most major factors in our environment today. Louisiana has already loss 1,880 square miles of land in the past eight decades. This problem is effecting the state funding to help solve the problem before the state lose more coastal land. Human disturbance has had a massive impact on the balance of wetland growth and decline. (Wilson, 2013). In order to stop this situation the state needs to have a stronger structural protection for the coast line. (Wilson, 2013).

Many communities are suffering due to coastal erosion. One example is the village of Cocodrie, LA in Terrebonne Parish. This village’s small population and its 220 residential and commercial buildings are surrounded by marshes. In Cocodrie, there is no barrier against hurricanes. Local marinas play host to recreational and commercial fishing, and The Louisiana Universities Marine Consortium is located in Cocodrie. This facility of around 100,000 square ft houses laboratories, classrooms, and a research center. Infrastructure that will be affected by coastal erosion includes paved highway, dirt roads, a bridge, water supply systems, and natural gas lines. By 2050, Cocodrie will be surrounded by open water as the marshlands around the village give way to rising sea levels. Another community affected by this issue is Yscloskey, LA in St. Bernard Parish. The most important part of the economy here is fishing, and highways link the parish to New Orleans fishing communities. The Yscloskey area lies outside of the protective levees and is quite vulnerable to storms. Though losses in Yscloskey are not predicted to be as great as those in Cocodrie, a 16 percent loss by 2050 leaves the infrastructure of Yscloskey even more vulnerable (Coast 2050, 1998, p. 64-66). Local residents in these areas are watching the land disappear along with the beachfronts and Cyprus swamps that were on that land (Marshall, 2014).

Reports revealed that by 2080s, the projected flood heights for locations in Connecticut (e.g., Norwalk, Westport, Bridgeport, Greenwich Cove, Shippan Point, Stamford, and Stratford) could range from 11.5 to 13 feet for a Category 1 hurricane, and 14.5 to 15.7 feet for a Category 3 storm (Gornitz et al., 2004). Therefore, rising sea level could account for 18-22% of the increase in flood height (in the high sea-level rise scenario) or 6-8% in the lower case (Gornitz et al., 2004). With the rising sea level, floods generated by storms of this magnitude could approach 18 feet by the 2080s (Gornitz et al., 2004). The increase in the projected flood level cities in Connecticut will be greatly affected such as Bridgeport and New Haven. As an illustration, a significant portion of both Bridgeport and New Haven lies within the high-risk flood zone, and during severe storms this place a large population, private property, and infrastructure at high risk. In New Haven, some infrastructures that are at risk include the New Haven railroad station and track yards, the Tweed-New Haven Airport, ramps to the Connecticut

The changes to the coastline have affected the sustainability of the region. The loss of wetlands and other natural barriers have eliminated protection from higher and faster moving storm surges. New Orleans and other regions of the Louisiana deltaic plane could not be protected without proper account of the tremendous change that occurred to Louisiana's coastal landscape (IPET).

Throughout history, the coastline of Sandy Bay has been subject to erosion. The areas focussed on in this study are Nutgrove and Long Beach. Erosion was first documented in this area in 1813. Sea level rise and the increase in the frequency and severity of weather events is currently having an impact on the land cover of both Nutgrove and Long Beach and this is erosion is likely to increase as time passes and climate change progresses.

Preserving coastlines is important for the economy and the environment. The fact that the business world and the preservation world are on the same page is a good indicator that maintaining beaches are important for both people and animals. The data that has been collected by both parties, thus far will hopefully bring a more cost effective and more long term solution for beach replenishment. So the beach bums and the sea life may continue to enjoy one of the most beloved landscape for generations to

Most people wouldn’t pay any mind to care about coastal resilience and the sea-level rise in the Tidewater area of Virginia. However, they are very important to the community and its development. In the past I was one of those people as well until I knew how much the Tidewater area could be affected by an extreme weather storm or pipe malfunction. Growing up in Virginia Beach I've always questioned why the houses in Virginia didn’t have basements. Because Virginia's elevation is approximately 5,729 feet, the average elevation is 12 feet above sea level, it's considered below sea level. The Tidewater area in Virginia is known for flooding when there are rain storms or other serious weather conditions as well. This is not only because of Virginia's elevation level, but also because of the sewage and waste system.

Besides the direct effect of sea level rise, coastal flooding may also be a more prevalent and severe issue. For example, “sea level rise of two feet, without any changes in storms, would more than triple the frequency of dangerous coastal flooding throughout most of the Northeast” (Horton 374). The higher seas would increase the initial level, so that the flooding level would be much greater, especially during hurricanes. Recent hurricanes have become a good example of how much damage can occur to both humans and animals. For example, much of the coastal infrastructure is in danger of damage, which can affect commerce and the public’s health and safety: “In New York State, two feet of sea level rise is estimated...To flood or render unusable 212 miles of road, 77 miles of rail, 3,647 acres of airport facilities, and 539 acres of runways” (Horton 379). This loss of infrastructure may occur in every coastal Northeast state, especially in the south. In these southern Northeast states, the land is flat, which makes them easier to inundate with water. In addition to infrastructure, transportation is also at risk, with much of the major highways (I-95) and trains (Amtrak) at risk of coastal damage (Horton 380). More affected by sea level rise, ecosystems near water may be permanently damaged in upcoming years, and according to Rob Deconto, a climate scientist at University of

According to the National Oceanic and Atmospheric Administration, almost 40% of the population lives in high population-dense coastal areas. Around the world, eight of the world’s ten largest cities are situated near a coast, with about 250 million people living by a coast line less than 5 feet above sea level. It is projected that all of these people will be directly affected in some way by seawater rising in the future (Siegert, 2017). For the county of Orleans Parish, the rapid loss of coastal land is not a future scenario, but a current reality. Due to our unique geography, Louisiana loses about 16 square miles a year; the rapid erosion of Louisiana’s cost is only expected to accelerate over time. (Wernick, 2014).

The Sea Level has increased over the past 200 years as average global temperatures have increased. The rise is due to two factors, the freshwater being added to the oceans from ice melt in the cryosphere, and the thermal expansion of the oceans due to rises in sea temperature. The sea level has risen 6 to 8 inches in the past 100 years. It is predicted to rise another 50 to 90 centimeters in the next century. As the sea level rises it’s jeopardizing rapidly growing coastal communities, which causes evacuation in some areas causing people to lose their homes. Sea level is the effect

The combination of these and other trends was an estimated average sea-level increase of 1.5mm per year between 1961 and 2003, which reached 2.4mm per year in the decade from 1993 to 2003. The decades prior to this trend showed only minor fluctuations in sea-level, suggesting that the current rate exceeds what could be caused by natural cycles. While the exact impact of rising oceans is difficult to determine, it is certain that the consequences will include some degree of flooding, integration of salt water into water tables, and a loss of land due to coastal erosion and submersion.6

Some amount of natural erosion is necessary to provide the sediment for beaches in estuaries and coastal bays. However, excessive erosion has occurred in the past due to development. Industrial and private development along the world’s coastlines has increased dramatically since the 1970s (Nepf). Developers and builders completed much of this construction without taking into account the effects of coastal erosion. New buildings were often placed too close to the existing shoreline so that

Attention Getting Device: On November 21, 2017 NASA published an article on the issue of global climate change which quoted this, ''NASA tool link port-city seal levels to regional ice melts''. NASA has been working to minimize the effect of global climate change and recently it has developed 'NASA tools'. This particular tool links changes in sea level of around 293 global port cities. Most specifically, the tool links changes seen in vulnerable regions, such as Greenland and the Antarctic Peninsula, where ice lands are melting rapidly. Such development will allow coastal planners to be aware and prepare for rising seas level for years to come.

Seagrasses are essential primary producers that provide habitat and refuge to fauna. Anthropogenic influences have caused global loss of seagrasses and a major contributor is eutrophication, which increases phytoplankton and algal populations, reduces light availability, and causes daily hypoxic conditions. Eutrophication is commonly linked to declines in temperate conditions and is more difficult to link to tropical systems since decreases are typically related to physical damage and diminishing light conditions from runoff. Climate change, herbivore declines, disease and overfishing, along with anthropogenic impacts from coastal development, run-off, eutrophication, and aquaculture have caused declines in coral reefs and mangrove systems. These three systems are interconnected and when one system is impacted, secondary impacts are observed in the other systems; coastal ecosystems will be adversely effected and decline. Additional research, conservation, and ways to reduce anthropogenic impacts have been discussed. Restoration is used to reverse habitat loss, although success is varied. Coastal systems and the biological and ecosystem services they provide, may take decades to establish. Marine Protected Areas (MPAs) are instituted to protect systems from further degradation, restore communities and allow them to flourish naturally. However, local residents are affected by MPAs and may become displaced, have restriction placed on their livelihood, or elimination of their