Skip to main content

Causes of Sea level Change

Sea level change is relative change in level of the sea surface that rise or fall with respect to the land surface.
The sea level changes have been caused by several possible causes, these are-
A.)Long Term Causes of Sea Level Changes:
i.)Changes in Ocean water volume: Changes in volume occurs due to melting & freezing of ice sheets. When ice sheet melts, volume of ocean water increases & sea level also rises. This sea level changes is called Eustatic change. If all of the in Antarctica were to melt, world sea level would rise between about 60 to 75m, & the Greenland in cap would add add about 5m. it glaciations develops then ocean water changes into ice & sea level subsides.
ii.)Changes in Ocean Basin Volume: Changes in the volume of ocean basins have been the most important factor in the influencing the broad trend of global sea level. Such changes can arise from a variety of causes. These causes are-
a)     Sediment causes,
b)    Trench formation,
c)     Subsidence of ocean crust,
d)    Uplift of mid oceanic crust,
e)     An increase or decrease in the length of the ridge system,
f)     Effect of orogenesis,
g)    Desiccation of small ocean basins, 
iii.)Geoidal Effects: The changes in the volume of water in the sea adjustment by adjusting the bottom of the ocean.
Characteristics of Lithosphere, Hydrosphere, Atmosphere & Biosphere.
Sea Level Condition
Green House State
Oxigeneted State
1.
Sea level
High
Low
2.
Ocean Basin
Wide & Shallow
Narrow & Steep
3.
Latitudinal Temperature Gradient
High
Low
4.
Plate Tectonics
Rapid Mental Convection
Slow Convection
5.
Volcanism
High
Low
6.
Continental Relief
Low
High
7.
Erosion & Weathering
Slow
High
8.
Biomass
Low
High 
9.
CO2
High 
Low 
10.
Temperature
Warm 
Cool 
11.
Atmospheric & Ocean Circulation
High 
Low 
12.
Dissolve O
Low 
High 

B.)Short Term Causes of Sea Level Changes:
The short term changes, which are effective during a year are mainly due to change in volume of water. The short term causes of sea level changes as follow-
i.)Sea Density: This is controlled mainly by temperature & to a much lesser extent by salinity, the lower the temperature & the greater salinity the higher the density & the lower is sea level.
ii.)Atmospheric Pressure: High atmospheric pressure give lower local sea level.
iii.)Speed of Ocean Currents: These speeds vary with total global energy budget & there may be as much as 18 cm difference in sea levels on opposite sides of curving, fast-flowing current.
iv.)Water Locked Up in Winter Snow: water locked up in winter snow in the Northern Hemisphere leads to the lowering of the level.

v.)Seasonal Pilling Up of Water: Seasonal pilling up of water along windward coast increase the sea level, e.g. South & East Asia during the summer monsoon.

Comments

Popular posts from this blog

Behaviouralism in geography

Behaviouralism Behaviouralism is an approach in human geography that came to prominence in the human geography of the 1960s and 1970s. It goes out of the idea that people are the determining factor in the explanation of space. Behaviouralism tries to give an explanation of the spatiallity of human activities. And thereby they use a complex universally applicable model.  Definition of Behaviouralism: The particular aspect with which geographical content is analyzed using mathematical statistics & human sensitivity, is called behavioralism. Concept of Behaviouralism: The Behaviouralism revolution is a theoretical concept. Its theories are not based on assumptions, but are actually explored through ascending methods based on the experience of human behavior. An analysis of the significance of geographical issues in behavioral perspectives within a system, so therefore is no definite boundary to behavioral geography. The main purpose of behaviouralism geography is to in...

Positive and Negative Impact of Tide

Tide has many effects on human life. The impact of tide discuss below- Positive Impact of Tide: Shipping:  Tides are helpful in making rivers navigable for large vessels. During the high tide, the amount of river water & height of river water increases. At that time, large vessels/ships can easily come to rive port. Again, during the low tide, ships can be returned from port to sea.  For example - London & Kolkata have become important ports because of the tidal waves in the Thames & the Hooghly rivers respectively. Pollution-free Environment:  When tidal water flows, rivers are free of garbage. As a result, the environment is not pollutant near the river areas. Obstruction of Sediments deposited & Delta Formation:  As a result of the tide, sediments not to deposited & prevents delta formation.  For example-  In the Sundarbans, small creeks are capable of navigating during tides.  Regular Water flow:  During th...

Concentric zone theory

Theories of City Structure-Concentric Zone Theory Introduction: The Concentric or Zonal Theory of urban landuse was first proposed in 1923 by E.W. Burgess. He was a sociologist. The idea behind the concentric model is that the development of a city takes place outwards from its central area in a series of concentric circles to form zones.  Assumption:        i.           Cultural & social heterogeneity of the population.       ii.           Commercial-industrial base to the economy of the city.     iii.           Private ownership of property & economic competition for space.     iv.           Expanding area & population of the city.       v.    ...