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1
Presented by:-
Ulagadde R.P.
Dept.Of Applied Geology (M.sc.Part-Ii] School Of
Earth Science Solapur University, Solapur
Seminar on
Sea level processes & changes
2
3
4
Learning Objectives
The shape of the planet: difference between Geoids and
Ellipsoid
The concept of Mean Sea Level
Processes that control the Mean Sea Level and its changes
Sea level changes over millions of year
Measuring sea level (tide gauges, altimetry, δ18
)
Sea level rise in the last century and global warming
Economic implications of Sea level changes
5
Gravitational field effects on sea level
Sea Level Variation
Astronomical Tidal Forces
Earth’s water closest to the moon is acted on more strongly by the
moon’s gravity
The solid Earth is pulled harder than the water on the side opposite
the moon
The Sun produces similar tidal forces and accounts for about 1/3 of
ocean tides
7
What does it mean to be at an altitude
of 4000 m?
It mean that I am 4000 m above the
Mean Sea Level (MSL)
Causes of Sea Level Change
Terrestrial water storage,Terrestrial water storage,
Extraction of groundwater,Extraction of groundwater,
Building reservoirsBuilding reservoirs
Subsidence in river delta,Subsidence in river delta,
Land movements,Land movements,
Tectonic displacementsTectonic displacements
Seepage into aquifersSeepage into aquifers
Circulation changes,Circulation changes,
Storm surges,Storm surges,
Water expands as it warmsWater expands as it warms
Exchange of ocean waterExchange of ocean water
withwith
glaciers and ice sheetsglaciers and ice sheets
9
10
by definition:
Mean Sea Level = 0 m = equilibrium level
 Changes in volume of water
 Changes in shape and volume of ocean basins
Changes are measured as relative changes to a
reference datum
This reference datum can be a fixed one (e.g.
distance from the center of the earth) or local
(coastline).
11
A change in volume of seawater in one ocean
will affect the level in all others. Any such world-
wide change in sea-level is called EUSTATIC
SEA-LEVEL change
12
13
14
15
Sea Level Change
16
Other effects of plate tectonics
e.g. Upper Cretaceous (90 Ma) MSL > 300 m
17
Summary of spatial-temporal scale of
processes contributing to Mean Sea Level
TIME (years)
∆MSL(meters)
100 1000 100 Ka 10 Ma 100 Ma
1 cm
1 m
10 m
100 m
1 day
(A) Exchange of water with continents (Groundwater, Lakes, etc.)
(B) Temperature expansion
(D) Plate Tectonics(C) Melting of ICE
• Thickness and area of continental crust
• Thermal state of crust
• Load on oceanic by land mass and sediments
(can generate localized changes in MSL,
e.g. subsidence of North Sea )
A,B,C  change in volume of water
D  change in shape of container
NOTE:
18
Sea Level Change in the last 100 yr (from Tidal Gauges)
Tides
Atmospheric
Pressure
+
=
Observations
of Sea Level
Res. Curve = Obs. – Tides - Atmos. Press.
WOCE Sea Level Stations as of February 2000 (from Tidal Gauges)
20
Arica
Iquique
Coquimbo
6/23/2001 6/24/2001
What can we say about these
tide gauges record?
21
The Earth's climate has warmed about 1°C (1.8°F) during the last 100 years.
(the warming follows the Little Ice Age (19th
century)  1-2 mm/yr sea level rise)
reduction in volume of ice caps, ice fields,
and mountain glaciers
thermal expansion of ocean water
Increase in greenhouse-gas emissions:
 Global Warming  expansion of oceans
 many of the world's mountain glaciers will disappear
 sea level rise acceleration
IMPACTS of HUMAN on SEA LEVEL:
Numerical models of the Climate System
can be used to predict future changes in Sea Level
FUTURE:
22
23
Thank You……

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sea level-paleoocean

  • 1. 1 Presented by:- Ulagadde R.P. Dept.Of Applied Geology (M.sc.Part-Ii] School Of Earth Science Solapur University, Solapur Seminar on Sea level processes & changes
  • 2. 2
  • 3. 3
  • 4. 4 Learning Objectives The shape of the planet: difference between Geoids and Ellipsoid The concept of Mean Sea Level Processes that control the Mean Sea Level and its changes Sea level changes over millions of year Measuring sea level (tide gauges, altimetry, δ18 ) Sea level rise in the last century and global warming Economic implications of Sea level changes
  • 6. Sea Level Variation Astronomical Tidal Forces Earth’s water closest to the moon is acted on more strongly by the moon’s gravity The solid Earth is pulled harder than the water on the side opposite the moon The Sun produces similar tidal forces and accounts for about 1/3 of ocean tides
  • 7. 7 What does it mean to be at an altitude of 4000 m? It mean that I am 4000 m above the Mean Sea Level (MSL)
  • 8. Causes of Sea Level Change Terrestrial water storage,Terrestrial water storage, Extraction of groundwater,Extraction of groundwater, Building reservoirsBuilding reservoirs Subsidence in river delta,Subsidence in river delta, Land movements,Land movements, Tectonic displacementsTectonic displacements Seepage into aquifersSeepage into aquifers Circulation changes,Circulation changes, Storm surges,Storm surges, Water expands as it warmsWater expands as it warms Exchange of ocean waterExchange of ocean water withwith glaciers and ice sheetsglaciers and ice sheets
  • 9. 9
  • 10. 10 by definition: Mean Sea Level = 0 m = equilibrium level  Changes in volume of water  Changes in shape and volume of ocean basins Changes are measured as relative changes to a reference datum This reference datum can be a fixed one (e.g. distance from the center of the earth) or local (coastline).
  • 11. 11 A change in volume of seawater in one ocean will affect the level in all others. Any such world- wide change in sea-level is called EUSTATIC SEA-LEVEL change
  • 12. 12
  • 13. 13
  • 14. 14
  • 16. 16 Other effects of plate tectonics e.g. Upper Cretaceous (90 Ma) MSL > 300 m
  • 17. 17 Summary of spatial-temporal scale of processes contributing to Mean Sea Level TIME (years) ∆MSL(meters) 100 1000 100 Ka 10 Ma 100 Ma 1 cm 1 m 10 m 100 m 1 day (A) Exchange of water with continents (Groundwater, Lakes, etc.) (B) Temperature expansion (D) Plate Tectonics(C) Melting of ICE • Thickness and area of continental crust • Thermal state of crust • Load on oceanic by land mass and sediments (can generate localized changes in MSL, e.g. subsidence of North Sea ) A,B,C  change in volume of water D  change in shape of container NOTE:
  • 18. 18 Sea Level Change in the last 100 yr (from Tidal Gauges) Tides Atmospheric Pressure + = Observations of Sea Level Res. Curve = Obs. – Tides - Atmos. Press.
  • 19. WOCE Sea Level Stations as of February 2000 (from Tidal Gauges)
  • 20. 20 Arica Iquique Coquimbo 6/23/2001 6/24/2001 What can we say about these tide gauges record?
  • 21. 21 The Earth's climate has warmed about 1°C (1.8°F) during the last 100 years. (the warming follows the Little Ice Age (19th century)  1-2 mm/yr sea level rise) reduction in volume of ice caps, ice fields, and mountain glaciers thermal expansion of ocean water Increase in greenhouse-gas emissions:  Global Warming  expansion of oceans  many of the world's mountain glaciers will disappear  sea level rise acceleration IMPACTS of HUMAN on SEA LEVEL: Numerical models of the Climate System can be used to predict future changes in Sea Level FUTURE:
  • 22. 22

Editor's Notes

  1. The Earth and Moon orbit their mutual center of gravity. Diameter of Earth is ~8,000 miles Fgravity = (GmEarthmMoon)/r2 - The moon pulls most strongly on oceans closest to it It pulls on the solid Earth at its center of gravity 4,000 miles further away Pulls weakest on the water on the far side, another 4,000 miles away (Earth is being yanked away from the water, creating the tide opposite the moon)
  2. Many factors must be taken into account when predicting changes to the sea level Local sea level tends to drop over time at river deltas if mangroves and other vegetation is present When ocean currents change (El Niño and La Niña), sea levels change The amount of water on land (lakes & ice) is changing