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Changing Sea Levels Changing Sea Levels

Changing Sea Levels - PowerPoint Presentation

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Changing Sea Levels - PPT Presentation

Beren TOMO Maddie AmyJane Emily and Lucia March 2014 Updated 180315 G36 Introduction What is sea level change Sea level change is the height of the sea with reference to the land ID: 323358

land sea change level sea land level change ice coastal levels rise isostatic water features coast rising area raised global fjords valleys

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Slide1

Changing Sea Levels

Beren, TOMO, Maddie, Amy-Jane, Emily and Lucia: March 2014 Updated: 18/03/15

G3.6Slide2

IntroductionWhat is sea level change?Sea level change is the height of the sea with reference to the land.

Isostatic sea level change is caused by vertical movements of the land relative to the sea. Any downward movement of the land causes sea level to rise locally while the rise in land causes sea level to fall. The effects are always local.Eustatic sea level change is caused by a change in the volume of water in the sea or by a change in the shape of ocean basins. The effects are always global.Slide3

EUSTATIC CHANGE Eustatic change is the global rise or fall of sea levels. This change is a

GLOBAL changeA factor that can affect this is global warming. This happens because the increased heat changes the amount of ice stored on land as water, thus changing the sea levels. A rise in temperature will cause the ice caps to melt, and sea levels will rise, and vice versa.The second factor that can affect this is the Steric effect. This is where the density of the water increases or decreases as the temperature rises or falls. If the temperature rises the water expands and if it falls the water contracts. It is estimated that sea levels can rise up to 0.4mm per year. Slide4

ISOSTATICIsostatic change is the adjustment of land levels.

This change is LOCAL.3 main physical factors affect this:iceupliftseismic activity Slide5

Ice is the first way that can adjust the land. This can happen when the land is covered by ice in one place. For example in the last ice-age, North Western Britain was covered in 1.5 km of ice. This immense pressure causes this area land to subside, whilst any other land (South Britain) will rise, like a see-saw. When the glacier ice melts, the weight is taken off the land, and so the land will begin to rise again, whilst the other area will sink.

This happens very slowly, and is known as glacial (isostatic) rebound. Uplift: Underlying tectonic forces, including uplift through folding and faulting can result in isostatic uplift (rise in land level) The land may rise as a result of tectonic plates pushing each other or removal of weight. Seismic activity: earthquakes can cause both uplift and depression of land as a result of movement along fault planes. Isostatic change can also happen due to human interference. The extraction of resources from low lying coastal areas may lead to compaction of land followed by subsidence (sinking).Slide6

ISOSTATIC

Isostatic sea level change can be attributed to the wait of ice. And is a local change because the ice only covers a local area. Slide7

Eustatic YOU STATIC change – caused by you as you cause global warming which cause ice cap melt which adds water to the see.Slide8

Landforms associated with rising sea levels.SUBMERGENT FEATURES Dalmatian coastline:In areas where valleys lie parallel to the coast an increase in sea level can form a DALMATIAN COASTLINE. Valleys are flooded leaving islands parallel to the coastline. This can be seen along the Dalmatian coast in Croatia.

Fjords-They’re drowned glacial valleys rather then drowned river valleys. They're relatively straight and narrow with very steep sides. They have a shallow mouth caused by a raised bit of ground (called the threshold) formed by the deposition of material by the glacier. They're very deep further inland e.g Sognefjorden in Norway is over 1000m deep in places.Rias- are formed when river valleys are partially submerged. They’re wide and deep near the mouth becoming narrower and shallower the further inland they reach. An example of this would be the dart estuary in Devon. Fjords LinkSlide9

Dalmatian Coast Croatia

Dart EstuarySognefjordenSlide10

Uses of features created by sea Level changeSUBMERGENT Features

FJORDS Uses of Fjords: 1. Tourism – Cruise ships 2. HEP – Dams 3. Agriculture 4. Settlements A Fjord is a drowned river valley due to rising sea level. Slide11

USES of Fjords SOCIAL : Agriculture: Subsistence farming

Transhumance Summer and winter pastures. Settlements Off grid Isolated and rural Housing Animals Tourism: Cruises - Deep Water Leisure Environmental/ Economic

Cold /Harsh Tourism HEP

Area’s of outstanding natural beauty Slide12

Uses of features created by sea Level changeSUBMERGENT Features

RIASFlooded river mouth and lower course Ports/ industrial Tourism Agriculture

Settlements Slide13

Emergent LandformsDue to FALL IN SEA LEVEL

Appear towards end of Ice ageIsostatic rebound takes place faster than a Eustatic rise in sea levelEmergent Features-wave-cut platforms, coastal plains and raised beaches.Raised beaches are wave-cut platforms & beaches that are above the current sea level. Over time beach sediment becomes vegetated and develops into soil.You can normally find some old cliffs (relict cliffs) too behind these raised beaches with wave-cut notches, arches, stacks etc. along them.These emergent features no longer experience coastal erosion and slowly get covered by vegetation but they are still weathered, often being weathered biologically, chemically and via freeze-thaw weathering.Common along the West coast of the UK this

is because the area experienced the greatest weight of ice during the last Ice Age (about 10,000 years ago).Slide14

Portland-Raised BeachPortland-South West Coast of the UKWarm interglacial phase of the Pleistocene ice ages approx. 200,000 years ago

Pebbles represent a beach when the sea was approx. 15m above the present level.The loam (sandy slit) above the raised beach was originally wind deposited, and is capped by a "head" formed during the last major glacial episode to have affected Britain – The Devensian. The head contains much limestone rubble broken up under severe arctic conditions. Slide15

Coastal PlainsA coastal plain is a flat, low-lying piece of land next to the ocean. Coastal plains are separated from the rest of the interior by nearby landforms, such as mountains.Coastal plains start as a continental shelf, a flat piece of land located below sea level. When the ocean level falls, the land is exposed, creating a coastal plain.

The Gulf Coastal plain of North America extends northwards from the Gulf of Mexico to the Ohio river. During the crustaceous period the central area of the United States was covered by a shallow sea which disappeared as the land rose.Slide16

IMPACTS of rising sea levels Sea Level Change Map

Higher mean sea levels could have an impact on underground water resources. Rising sea levels could also affect coastal habits, particularly wetlands and salt marshes. A number of areas around the British coastline are potentially at risk from rising sea level. These include major Cities, such as London, hull and Middlesbrough, and high grade agricultural land. Major road and rail links near the coast are also at risk, and several power stations are situated on low lying ground.Much of the east coast of Britain is at serious risk of flooding due to inadequate sea defences and the willingness of planning authorities to allow development along low lying area.

The increased concentration of housing and other developments of land at risk of flooding is likely to raise insurance costs. Farmers are paid up to £600 for each hectare of land that reverts to salt marsh.Slide17

EXAM QUESTION Discuss the impact(s) of rising sea levels on coastal

environments (15)NASA Quiz

Discuss

the

impact(s)

of

rising sea

levels on coastal environments (15)