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 invest

Responses to hazard

Responses to hazard:  Preparedness,  Trauma and aftermath,  Resilience and capacity development Responses to hazard A hazard is an agent which has the potential to cause harm to a vulnerable target. Hazards can be both natural or human induced. According to Alexander (2000, p. 7), “a  hazard is an extreme geophysical event that is capable of  causing a disaster.” The word “extreme” is used here to signify a substantial departure  (either in the positive or the negative direction) from a mean or a trend. Although Alexander did not specify the distinction between these two terms in his definition, it does suggest that hazards may transform into disasters and thus become sequential events. That is, every disaster starts with a hazard (Thywissen, 2006). Hazards are harmful to people, but it fails  to recognize people’s role in causing or  amplifying the impacts associated with hazards. For example, floods can originate either from a natural variability in meteorolo

Cyclone: Factors, vulnerability, consequences and management

A cyclone is a vast, violent whirl in the atmosphere which moves from the high seas towards the coastal areas. A cyclone will often bring with it heavy rains that can cause flooding. In order for a cyclone to form, the ocean waters need to be warm, at least 26°C. Above the warm ocean, water evaporates and forms clouds. If there is low air pressure where the clouds are formed, it pulls them in and they begin to rotate. It is the earth rotating and spinning on its axis that causes  the cyclone’s clouds to rotate. Cyclones are caused by atmospheric disturbances around a low -pressure area distinguished by swift and often destructive air circulation. Cyclones are usually accompanied by violent storms and bad weather. The air circulates inward in an anticlockwise direction in the Northern hemisphere and clockwise in the Southern hemisphere. Cyclones are classified as: (i) extra tropical cyclones (also called temperate cyclones); and (ii) tropical cyclones. Fig: Major Disaster in Indi