//1.b. Water in the world’s oceans varies horizontally and vertically Flashcards
What is salinity
This is the concentration of sodium chloride. It is expressed a grams of salt per 1000g of water
How does salinity vary horizontally and vertically
- fresh water is usually <0.5ppt. The pacific can be 30-35ppt
- salinity varies with depth and becomes lower at the surface (a gradient know as the halocline)
- salinity influences water desnity-this affects movements such as ocean currents which affect climate
- different desnities created affect the vertical movement of water in oceans
How does temperature vary horizontally and vertically
- high levels of energy are needed to heat water
- once heated, water retains heat efficiently
- the rise and fall of temperature on land surfaces is much more rapid and this has an impact on weather and climate from global to local scales
- the surface layer varies in depth based on season and location
- at depth, temperature hardly varies
What are the two types of ocean currents
Surface currents and deep water currents
What are surface currents
- surface cirulation
- these waters make up 10% of all the water in the oceab and form the uper 400m of the ocean
What are deep water currents
- thermohaline circulation
- these waters make up the other 90% of the ocean and move around the ocean basins driven by forces of density (a function of salinity and temperature differences)
- ocean currents are influenced by solar heating, winds, gravity and the Coriolis force
Explain the process of thermohaline circulation
This is a continuous, slow moving flow of ocean currents around the globe
1) most oceans hold warm water at the surface and cold water in their depths
2) surface water tends to move from low to high latitudes
3) in polar regions, ocean surfaces are cooler, more saline and denser
4) water sinks and moves horizontally
5) deep currents flow back to the equator where water rises
How does temperature vary horizontally and vertically-warm currents
- warm currents found at the surface are waem at the equator
- they are cool as they more towards the poles
- warm currents found at the Indian and Pacific ocean
How does temperature vary horizontally and vertically-cold currents
- cold currents found at depth are cold at poles
- warm when they rise to the surface at the equator
- colder currents at depth are dound in the Southern and Atlantic ocean
The pattern of circulation in the North Atlantic-warm saline water
- warm saline water flows from the coast of Florida in a north easterly direction as the Gulf Stream
- the transfer of heat influences the climate of western Europe
- The North Atlantic Drift in its northern course, this warm current flows up to the Arctic
- as the water cools, its density increases and it sinks
- the water then travels back towards the equator where it will surface 150-250 years later
The pattern of circulation in the North Atlantic-Northwest Atlantic
-in the northwest Atlantic, the cold Labrador Current flows south from the Arctic
The pattern of circulation in the North Atlantic-warm salty water
- the North Atlantic receives warm, salty water from the Mediterranean via the Straits of Gibraltar
- eventually its desnity matches that of the surrounding water and mixing occurs