- Long-term sea-level change occurs on a timescale
Climate
Change Affecting Sea Level:
- Ice age build up and the climate begins to change.
- Less water in the sea and the sea-level falls.
- New land can also form by the release can still happen. T
- his means that sea level falls because waster goes over land which is built on snow so it builds up and stays there.
What
Causes Sea-Level Change:
- Ice age/glacial periods (long term)
- Global warming (short term)
- Other physical processes e.g tectonics and subsidence
Two
Types Of Sea Level Change:
- Eustatic: Volume of water changes e.g more water floating leads to a raised height
- Isostatic: Height of the coastal land changes so the land rises out or sinks into coastal water.
Eustatic:
- Ocean water warms on coasts so it changes volume. If the water is warmer it will expand slightly so the sea level will very slightly rise.
- Amount in the ocean increases from ice on land e.g glaciers therefore more water flows in the ocean raising the sea level
- Thermal Expansion: Water is heated and it expands, oceans are 4-8 thousand deep so a slight expansion adds some millimetres which can be significant.
- Ice Melt: Land ice melts and flows into the sea = more water in sea. Opposite can also occur.
Isostatic
Change:
- Weight of the ice is compressed, and rock is pushed into the mantle,
- sea levels fall because of thermal contraction and water is stored as ice.
- Thermal expansion occurs = raised sea level.
- The land rebounds slowly as the weight of ice has increased which causes local sea levels to fall.
Sea
Level Change Landforms:
Submergent:
- Landforms that form due to being under water (submergent) e.g Fjords, Rias and the Dalmatian Coast.
Fjords:
- Mainly in Norway
- Very large, deep, steep-sided valley that have flooded
How
Do They Form:
- Huge amount of snow and ice build-up in northern latitudes
- V-shaped valleys on the coast because rivers erode the land
- Glaciers flow out of ice sheets eroding the valley to make them U-shaped
- Ice melts and sea levels rises eustatically which is, submerged to form a fjord.
Rias:
- River valley that is v-shaped and flooded when sea levels rise, not been eroded
- Due to the eustatic sea level rising from the last ice age, rising sea level forms rias
- Example: Southern Ireland Coast near Cork.
Dalmatian
Coast, Croatia:
- Long parallel mountains formed via tectonic forces
- Sea levels rise because the ice ages have ended
- Eustatic sea level rise has flooded the coast
- Top of the mountain stick out as long parallel islands.
Emergent
Landforms:
- Landforms that form due to land coming out of the water e.g Raised beaches and fossil cliffs
- Marine erosion creates cliffs and a wave cut notch
- Ice age ends and all the weight of the ice sheets and glacial are removed from land
- Isostatic rebound occurs: Land rising back out of the mantle
- Raises the beaches and cliffs up so they are away from the coast
- Eustatic sea level fall can also produce the same features
Global
Sea Level Rise Due To Climate Change:
- If the sea level rises due to climate change, it will raise 60m and will flood the following areas: Amsterdam, London, Berlin, Venice and Baghdad
Bangladesh:
- One of the most at risk countries from climate change and global sea level rise
- Large river delta from the Ganges
- Delta: Very flat and low-lying areas of sediment deposited by rivers into coastal waters
Tectonic
Sea Level Change:
- Earthquakes and tectonics can also change sea levels isostatically. An earthquake in 2016 in New Zealand uplifted a long area of coast raising the sea floor out permanently.
Summary:
- Sea level rise and fall by many metres on a long-term timescale e.g mainly due to the ice ages
- Eustatic change is the volume of water changing from land ice melting and thermal expansion.
- Isostatic change means land levels rises or falls
- Submergent landforms include: fjords, rias and Dalmatian Coastline
- Emergent landforms include: raised beaches and fossil cliffs
- Global sea level rise is occurring at a rapid rate due to climate change and causing risk to low lying coastlines e.g Netherlands, Bangladesh and the Holderness Coastline in Yorkshire.