* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Download Oceans - Sea level change
Instrumental temperature record wikipedia , lookup
Global warming wikipedia , lookup
IPCC Fourth Assessment Report wikipedia , lookup
Hotspot Ecosystem Research and Man's Impact On European Seas wikipedia , lookup
Climate change feedback wikipedia , lookup
Effects of global warming wikipedia , lookup
How will the sea level change over the next century from various sources (melting of continental glaciers and ice sheets,and seawater expansion)? And what will be the impacts on wildlife and ecosystems and society? Hypothesis As a group we have decided that the sea level will rise significantly over the next century due to a variety of factors such as increase in evaporation and melting of glaciers. This will not only be detrimental to humans but will also have a significant negative impact on wildlife. Key: Cesar- red Maria Jose- blue Mara- yellow Piyush- brown Research What is sea level? The sea level, or sometimes called the mean sea level is basically the average height of the ocean surface. This is calculated by taking the average of high and low tides of the ocean surface. Scientists who study the sea level must take into big consideration the rate at which the sea level rises as it helps obtain more reliable and useful data. The current sea level increase is 3.1 mm/year. There are many factors that affect sea level such as the earth’s temperature, tides and winds; and the change in sea level can be a measure of climate change and global warming. Source: http://www.nasa.gov/vision/earth/environm ent/sealevel_multimedia_prt.htm Types of sea level rise Eustatic sea level rise: This one is affected by climate change and happens mainly due to global warming. This occurs when sea water evaporates and it is then deposited onto land through precipitation, after a certain amount of time it will make its way back to the ocean however if a glacial period is to occur the water is then trapped in a glacier and cannot make its way back to the sea therefore changing the sea level. Vice versa if the glacier begins to melt the sea level will rise. It can also happen when the ocean basin changes therefore changing the amount of water it can hold; this happens with tectonic plate movements. If ocean basins get bigger the sea level will fall, conversely if they get smaller, sea level will rise. Eustatic sea level ALWAYS has a global effect. Types of Sea level rise Isostatic sea level rise: This happens due to the movement of the Earth’s crust, during a glacial period the sea would freeze and the ice accumulated in certain areas would press down on the crust this caused it to lower the land and sea level due to the weight of the ice. The same process occurs when the ice melts and pressure on the crust is less causing it to lift and raise the sea level. It can also happen due to tectonic uplift or depression however this only havens in plane boundaries so it can only happen in certain parts of the world. Change in land level Due to the fact that the surface of the land, as well as sea, changes over time the sea level changes are often defined as “relative” or “absolute”. “Relative changes may be observed even though the absolute height of the oceans remains the same. It is important to realise that when earth scientists talk about a rise in mean global sea level (what we call ‘eustatic’ sea level), local changes may be quite different. This is why local studies of sea level rise and fall are so important.” Sea level has increased an average of 1.7 ± 0.5 mm since the beginning of the 20th century Post-Glacial rebound Post-glacial rebound or continental rebound, is essentially the rise of land mass which was depressed by the great weight of ice sheets during the last glacial period. This course is called isostasy. This process began with yet another process called “ice sheet delegation” which started to occur about 19 000 years ago when most of the ice sheets found in North America and northern Europe began to melt. This water formed by the melting commenced to flow into the oceans, ultimately leading to an increase in sea level. Afterwards, the land which at one point had been beneath the ice began to rise or “rebound”; the process called “post-glacial rebound”. This process continues to take place today. And affects Northern Europe, Canada,Siberia and the United States. Post-Glacial rebound graph In Hudson Bay, as well as in central Scandinavia the land is still increasing 1cm a year. However, areas such as Baltic states and northern USA are currently subsiding. . Courtesy of Tom James at Natural Resources Canada http://www.antarcticglaciers.org/ glaciers-and-climate/sea-levelrise-2/sea-level-rise/ Thermohaline Circulation: Another impact of glacial retreat is the possible effect fresh melt water will have on the thermohaline circulation. Driven by density gradients in ocean waters, the thermohaline (deep ocean overturning) circulation is made up of the global ocean flow of ocean currents. As ocean waters move around, different water masses are formed as evaporation removes fresh water and precipitation and river runoff add fresh water, each changing the ocean salinity and therefore the density of the waters. This results in a change in sea levels. Diagrams of Thermohaline Circulation: Image Sources: Left -http://essayweb.net/geology/quicknotes/ocean_currents.shtml RIght:http://mail.tku.edu.tw/086138/EnvFutures/WebPages/Global%20warming/Ther mohaline%20Circulation.files%5Cthermohalinemodel.gif Global Warming Global warming is the gradual increase in the overall temperature in the Earth’s atmosphere attributed to the greenhouse effect caused by excess carbon dioxide emissions, ChloroFluoroCarbons (CFC), and other pollutants. Ice is melting worldwide, especially at the Earth’s poles. This includes mountain glaciers, ice sheets covering West Antarctica and Greenland, and Arctic sea ice. A rise in global temperature means melting of snow in the poles. This will result in drastic rises in sea levels. It also causes thermal expansion. Other impacts include: ● Increase in precipitation (rain and snow) globally on an average. ● Changes in ecosystems: Some butterflies, foxes and alpine plants have moved farther north or to higher, cooler regions. Thermal Expansion As silly as it sounds; sea level rises due to global warming by the simple fact that water molecules gain kinetic energy due to heat. The particles in the upper level of sea are quickly released on to the atmosphere, however those in the deeper levels of the sea will take longer to be released; keeping them in the ocean and contributing greatly to seawater warming which causes an expansion of the total water in the ocean causing a rise in sea level. This happens because warm seawater has greater density than colder seawater.The oceans store more than 90% of the heat in Earth’s climate system and act as a temporary buffer against the effects of climate change.For instance, an average temperature increase of the entire world ocean by 0.01 degree Celsius may seem small, but in fact it represents a very large increase in heat content. Graph showing the relation between thermal expansion and melting of land ice in inches per decade. Melting of land ice is much higher from 1993-2008 as compared to 1972-2008. Melting of continental glaciers Glaciers, alongside with ice-sheets cover up to 10% of the entire planet's land. The melting and ablation of glaciers is mainly due to the increase in temperature as it affects the overall mass balance of glaciers and ice-sheets decreasing it at a fast rate. It is also affected by evaporation and wind scouring. The global sea level has risen by 20 cm since 1970. http://www.climate.org/topics/sea-level/ Melting Ice caps and Glaciers Ice caps and Glaciers melt during the summer each year and during the winter the snow which forms from sea water is usually enough to balance the melting and maintain the sea level constant however higher temperatures cause by global warming have increased the average melting of the glaciers and ice caps and decreasing the amount of snow during the winter causing an imbalance and as a consequence of that the sea level begins to rise. 60% of the contribution to sea level rise comes from melting of icecaps and glaciers not including those of Greenland and Iceland whose rate of melting has increased drastically over these past few years due to Global warming. Water cycles between ocean, glaciers and the atmosphere. Image: http://en.wikipedia.org/wiki/File:Mass_balance_atmospheric_circulation.png Antarctica and its influence on the sea level Antarctica holds the most ice in the whole world with 27 million Km2. Fortunately not all of it has melted because if it did, the sea level would rise up to 58 metres. “The Antarctic Peninsula Ice Sheet currently contributes around 0.22 ± 0.16 mm per year of sea level rise[11], but has the potential to raise sea levels by up to 0.24 m if all the ice melted” (See references). West Antarctic Area However, not only is the Antarctic Peninsula vulnerable, the West Antarctic Area can also have a big impact on the sea level. The main support (bedrock) of the west antarctic area is below sea level. This makes the land unstable as the ice discharge has a bigger increase. What this means is that when water gets deeper more icebergs are calved. Definition of calved: (of an iceberg or glacier) split and shed (a smaller mass of ice).(of a mass of ice) split off from an iceberg or glacier..This would lead to a collapse of the West Antarctic Area which would increase the sea level significantly. http://takvera.blogspot.mx/ 2012/09/southern-oceanwarming-impact-on.html Future Sea Level Rise Recent studies suggest that the sea level will rise between 0.2 and 2.0 metres by 2100, although the best estimate is 0.6m, it could swamp many cities along the US East Coast. Likewise, a complete meltdown of Greenland and Iceland would cause a 7.0 m rise which would be enough to submerge London. A collapse of the West Antarctic Ice Sheet could result in a global sea level rise of 3.3 m, which could occur within the next 500 years. Impacts of Future Sea Level Rises: If greenhouse gas concentrations were stabilized today,sea level would nonetheless continue to rise for hundreds of years. Sea level rise threatens low lying areas around the world. Island nations, such as the Maldives and Comoros, are particularly at risk. Coastal cities, such as New York City and Mumbai, India must also prepare for higher sea levels. Hurricanes and other storms are likely to become stronger. Some diseases will spread, such as malaria carried by mosquitoes. Less fresh water will be available. If the Quelccaya ice cap in Peru continues to melt at its current rate, it will be gone by 2100, leaving thousands of people who rely on it for drinking water and electricity without a source of either. How does the sea level rising affect us? The sea level rising increases the chances of coastal and low lying regions suffering from flooding and storms, which can cause the people living in that area to abandon their homes and move to a safer place, as one possibility is that the area is completely submerged, this can also happen to small islands.Coastal areas will be greatly affected by sea level rise; Tourism, aquaculture, fisheries, agriculture, forestry, recreation, and infrastructure would all be greatly affected since some of them such as agriculture tourism and fishery them depend on the sea, and the other such as infrastructure and forestry could be swamped and destroyed by a rise in sea level. How does the sea level rising affect us? Another way that the rise of sea level can affect us is the contamination of groundwater by saltwater, this can cause erosion and impeded drainage. Moreover, the contamination of groundwater and flooding allows the spread of diseases such as cholera and malaria within the communities. How does the sea level rising affect us? About 40% of the world’s population lives within 100 km from coastal regions. Thus endangering millions of lives and billions of dollars worth infrastructure and property. Saltwater Intrusion: Rise in sea level translates to saltwater being included in groundwater thus endangering water supply for drinking water, irrigation, and overrunning agricultural fields. Furthermore low-lying areas which are gently sloping are more susceptible to water contamination. How will the sea level rising affect us? Here are a few maps showing how the potential sea rise in 100-300 years would affect five coastal Us cities. Charleston South Carolina The atlantic coast would push several miles inward flooding the city by 19% The Charles River would flood downtown Cambridge. Logan Airport would start to disappear. Boston Harbour begins to encroach on downtown. There would be a large widespread of flooding around the Altantic Ocean coastline. Most of suburban Miami, and the Miami surrounding areas are submerged. Almost the whole city and it’s surrounding areas would flood. How are ecosystems affected by sea level rise? Ecosystems are affected by sea level rise because habitats are destroyed and the patterns that are usually followed are changed; currents can change and it can have an impact on migrating species as well as changes in temperatures can place animals in risk of extinction or force a species to migrate to a warmer or colder area. Sea level rise obviously changes the depth of the ocean in some areas this can cause ecosystems to suffer as they are not used to those depths or the sun may not reach them as well as making it hard for photosynthesis to take place. It can also slow down the reproduction of plankton which is a crucial part of food chains as the temperature gets warmer. Mangroves and Climate Change: The mangrove ecosystem provides income from the collection of the mollusks, crustaceans, and fish that live there. Mangroves can adapt to sea-level rise if it occurs slowly enough, if adequate expansion space exists, and if other environmental conditions are met. If sea level is rising relative to the mangrove surface, the mangroves seaward and landward margins retreat landward, where unobstructed, as mangrove species zones migrate inland in order to maintain their preferred environmental conditions, such as period, frequency and depth of inundation and salinity. Recent study has also shown that the the rise in sea level is having a worse effect and making survival harder for mangroves since the sea level rise has been accelerating. Image Courtesy: http://www.coastalwiki.org/w/images/5/5b/Fig_5.jpg Impact on Wildlife Sea level rise can cause the loss of habitats of fish and birds as well as polar bears, seals and some species of penguins are at risk of extinction for they rely on the existence of ice caps to survive. It also affect turtle nesting beaches because habitats are lost, as well as extreme rainfalls can flood the nests and transfer sediment to coral reefs, sea level rise can affect sea currents which can change migration paths. Species that depend on one another may become out of sync. For instance plants could bloom earlier than their pollinating insects become active, thus causing disruption in the ecosystem. Impacts on marine ecosystems As the sea level rises the amount of light that reaches offshore plants such as algae is reduced and this could affect the ability of the plant to photosynthesise. Mangroves are also affected because they need a stable sea level for their survival however if it happens slowly enough they might be able to adapt. Marine migration organisms will probably be able to adapt, however a lot of organism’s rate of successful migration will be affected. Similarly low lying area and coastal ecosystems will flood. Coral reefs will suffer for sea level rise can increase sedimentation due to erosion, this can cause reduction of sunlight reaching the reef and allowing coral to photosynthesise. CONCLUSION As a group and through our research, we came to the conclusion that the sea level will rise between 0.8 to 2.0 metres by 2100 causing floodings in many areas throughout the world and possibly submerging many islands, damaging animal wildlife as well as human. This will occur due to the increase in temperature in the atmosphere leading to global warming,ice sheet melting, glacial melting and thermal expansion. References British Geological Survey. (2014). Sea Level and Coastal Services. Retrieved November 15, 2014, from British Geological Services: http://www.bgs.ac.uk/discoveringGeology/climateChange/general/coastal.html?src=topNa v Climate Citizen. (2012, September 28). Southern Ocean warming impact on Antarctic ice sheet and global sea level. Retrieved November 23, 2014, from Climate Citizen: http://takvera.blogspot.mx/2012/09/southern-ocean-warming-impact-on.html Climate Institute. (2014). Climate Institute. Retrieved November 22, 2014, from Oceans and Sea Level Rise: http://www.climate.org/topics/sea-level/ Coastal Wiki, Panwad Wongthong. Retrieved on November 23, 2014 : http://www.coastalwiki.org/wiki/Potential_Impacts_of_Sea_Level_Rise_on_Mangroves Coastal Wiki. (2014). Retrieved November 23, 2014, from Coastal Wiki: http://www.coastalwiki.org/w/images/5/5b/Fig_5.jpg Copeland, B., Keller, J., & Marsh, B. (2012, November 24). What Could Disappear? Retrieved November 23, 2014, from New York Times: http://www.nytimes.com/interactive/2012/11/24/opinion/sunday/what-could- Davis, B. (2014, February 17). Sea Level Rise. Retrieved November 23, 2014, from Antartic Glaciers: http://www.antarcticglaciers.org/glaciers-and-climate/sea-level-rise2/sea-level-rise/ Drews, C. (2007, September 2007). WWFCA. Retrieved November 22, 2014, from Sea turtles threatened by rising seas: http://www.wwfca.org/?19554/Sea-turtles-threatenedby-rising-seas Jackson, A. (2014). Sea Level Change. Retrieved November 23, 2014, from Geography AS Notes: https://geographyas.info/coasts/sea-level-change/ National Geographic. (2014). Sea Level Rise. Retrieved November 22, 2014, from National Geographic: http://ocean.nationalgeographic.com/ocean/critical-issues-sealevel-rise/ National Geographic, global warming. Retrieved 23rd November 2014 http://environment.nationalgeographic.com/environment/global-warming/gw-effects/ Union of Concerned Scientists. (2011). Sea Level. Retrieved November 23, 2014, from Climate Hot Page: http://www.climatehotmap.org/global-warming-effects/sea-level.html Weather Underground. (2014). Sea Level Rise. Retrieved November 22, 2014, from Weather Underground: http://www.wunderground.com/climate/SeaLevelRise.asp?MR=1 Wikipedia. (2014, September 27). Wikipedia. Retrieved November 22, 2014, from Post Glacial Rebounds: http://en.wikipedia.org/wiki/Post-glacial_rebound#Effects http://www.antarcticglaciers.org/glaciers-and-climate/sea-level-rise-2/recovering-from-anice-age/ http://www.antarcticglaciers.org/2013/01/antarcticas-contribution-to-global-sea-level-rise/ Wikipedia. (2005, May 23). Mass Balance Atmospheric Circulation. Retrieved November 23, 2014, from Wikipedia: http://en.wikipedia.org/wiki/File:Mass_balance_atmospheric_circulation.png Wikipedia. (2014, November 2014). Sea Level. Retrieved November 2014, 2014, from Wikipedia: http://en.wikipedia.org/wiki/Sea_level Wilson, D. M. (2005). SFU Museum. Retrieved November 22, 2014, from Glaciation and Sea Level: http://www.sfu.museum/journey/an-en/secondaire2emesecondary/niveaux_marins-sea_levels WWF. (2014). WWF. Retrieved November 22, 2014, from Marine problems: climate change: http://wwf.panda.org/about_our_earth/blue_planet/problems/climate_change/