Surface currents

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Smithtown High School West

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SURFACE CURRENTS

[object Object],[object Object],[object Object],[object Object],[object Object]

Coriolis Effect

Coriolis Effect ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

main gyres in the world’s ocean northern hemisphere - clockwise southern hemisphere - counterclockwise

WIND PATTERNS

wind patterns and Coriolis effect result in the major currents in the ocean

Western Boundary Currents ,[object Object],[object Object],[object Object],[object Object],[object Object]

Eastern Boundary Currents ,[object Object],[object Object],[object Object]

western boundary currents are stronger than eastern boundary currents

The Gulf Stream ,[object Object],[object Object],[object Object],[object Object],[object Object]

The Gulf Stream ,[object Object],[object Object],[object Object]

The Gulf Stream Current

Eddies ,[object Object],[object Object],[object Object],[object Object]

how eddies form

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Every continent or island is bordered by a long or short coastline. Coastline is the line separating the land and sea. Coastal zones are the transition zones between terrestrial and marine habitat. They form an interface between land and oceanic natural processes. Coastal areas also are varied in their topography, climate and vegetation. Some are sandy beaches, rocky shores, with or without tidal inlets. The climate of a coast are controlled by the land and sea breezes and the humidity controlled by marine water. Waves are powerful tools for constructive and destructive activities. Hence. the geomorphology of beach, materials and processes are always not constant due to the impact of everlasting action of tides, waves and currents.

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There are two types of currents in the ocean: 1) surface currents move the water above the pycnocline a) ≈ 10% of the ocean b) horizontal motion c) wind powered = solar powered 2) thermohaline = deep currents move the water below the pycnoline (zone of rapid change of water density) a) ≈ 90% of the ocean b) horizontal and vertical motion c) density driven density depends temperature and salinity these are also solar powered 3) these two sets of current are interconnected Chapter 7 – Ocean Circulation Surface currents are moved by friction between the surface winds and the water surface = wind driven. max speed is 3% of wind speed Since winds are solar powered, surface currents are solar powered. The overall pattern of surface currents is controlled by the Coriolis effect, gravity, and the shape of the ocean basin. Like Fig 7.7, p. 205 Ekman Transport – the net (or average) motion of wind driven water, is 90° to the direction of the wind. In a perfect world, this movement is: 90° to the right in the Northern Hemisphere, 90° to the left in the Southern Hemisphere, WHY?...........the Coriolis Effect Fig. 9-, p. 236 In the northern hemisphere, the Westerlies tends to move water southeast, while the Trade winds move water northwest! wind direction wind-driven water movement (Ekman Transport) The Westerlies (30° - 60°) and the Trade Winds (0° – 30°) are the strongest winds,* and are the main winds causing ocean currents! Largest change in temperature causes the strongest wind! Remember, according to Ekman Transport, wind - driven water moves 90° to the wind direction. In the northern hemisphere, the Westerlies tends to move water southeast, while the Trade winds move water northwest! The movement of wind-driven water can be described with a vector = an arrow pointing in the direction of travel and scaled to the speed. This vector can be broken up into a component moving toward the edge of the ocean and a component moving toward the center of the ocean. wind direction water movement vectors of water movement The water moving east or west (toward the edge of the basin) bounces off of the land. In the northern hemisphere, the water current turns right! Current bounces off land Current bounces off land Subtropical Convergence = a short (≈ 6.5 feet tall) hill of water formed when part of the wind blow water moves to the center of the ocean basin. Can water stand in a hill? No! Gravity works to move the water back downhill. BUT the wind is still working to push water uphill again So – The winds build the hill taller, and The taller the hill the more gravity pulls the water back downhill The hill continues to grow until wind driven Coriolis deflected motion in = gravity driven motion out. Then – only the circular movement around the edge of the hill is left. THIS IS THE SURFACE CURRENT! Garrison, 2009, Essentials of Oceanography Under the hill of wa ...

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Surface currents

1. SURFACE CURRENTS

2.

3. Coriolis Effect

4.

5. main gyres in the world’s ocean northern hemisphere - clockwise southern hemisphere - counterclockwise

6. WIND PATTERNS

7. wind patterns and Coriolis effect result in the major currents in the ocean

8.

9.

10.

11.

12.

13.

14.

15.

16.

17.

18. western boundary currents are stronger than eastern boundary currents

19.

20.

21. The Gulf Stream Current

22.

23. how eddies form