Lesson 12- How are coastal landforms influenced by isostatic and eustatic sea level rise? Flashcards

1
Q

What would happen if all the ice melted on earth?

A
  • 3% of all water is fresh-70% of this is frozen
  • 95% of ice is land based
  • 10% of global population would be displaced up to 10m of sea level
  • White ice melts which has a high albedo effect but then theres more blue/green which has a low albedo effect and therefore holds heat more and warms up the planet
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2
Q

What acctually is sea level change?

A
  • Change in short-term period such as day-to-day or minute to minute due to factors such as high tide and low tide, wind strength and changes in direction or changes in atmospheric pressure
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3
Q

How has sea level changed?

A
  • IPCE predicts sea level rise between 0.3-1m by 2100
  • Since records began they have always been rising from 120m below what they are now
  • Since 1880 and the industrial revelution, sea levels have increased by around 235mm which may not seem a lot but is significant enough to overwhelm some sea defences with storm surges as well
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4
Q

What are the possible causes of the sea level change?

A
  • During cold glacial periods global sea levels are much lower which affects the location of coastal landforms and processes
  • Current changes in the global carbon cycle affect physical processes at the coast but also human ones as coastal regions are eroding faster and at greater risk of coastal flooding
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5
Q

Eustatic change

A
  • This is global. In cold glacial periods, precipitation falls as snow (rather than rain) and forms huge ice sheets that store water that is usually held in the oceans
    -As a result sea levels fall. As temperatures rise at the end of glacial periods, the ice sheets begin to melt and expand as water warms due to thermal expansion.
    -magma rising to surface lifts the crust and reduces capacity of the ocean causing higher sea level
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6
Q

Isostatic change

A
  • This occurs locally. During glacial periods, the enormous weight of the ice sheets makes the land sink – isostatic subsidence. As ice begins to melt at the end of a glacial period, the reduced weight of the ice causes the land to readjust and rise – isostatic recovery.
    -folding of sedimentary rock can increase the height of the land compared to the sea
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7
Q

What impacts does changing sea level acctually have?

A
  • Current sea levels stabalised around 3,000 years ago
  • More than 1 billion people live on high risk coasts
    -75% of cities are coastal
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8
Q

What are the different types of coastline created by sea level change?

A
  • Emergent have features associating with falling relative sea levels. E.g relict cliffs
    -where land has risen or sea levels drop
  • Submergent have features that suggest relative sea levels like Fjords
    -where sea levels have risen at the end of the ice age
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9
Q

Emergent landforms

A
  • Raised beaches-beach above sea level unreachable at high tide-sometimes called marine terrice
    Relict cliffs-Where land has risen from the sea in the past as a result of isostatic processes
    -steep slope at back of beach
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10
Q

Submergent landforms

A
  • Rias-A drowned river
    -rising sea levels relative to the land rebranding flood river valleys leaving only high land visable
  • Fjords-A drowned glacial valley- U shaped valleys left by glaciers are submerged
  • Dalmatian Coasts-Formed in areas where valleys lie paralell to each other
    -when valleys get flooded, the tops remain above the surface
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