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Surface Currents

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Surface Currents and their characteristics

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À propos de Compléter
geology
hs4
oceanography
aquatic science
 Âge recommandé: 17 ans
192 fois fait

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Billie Jean Warta
Billie Jean Warta
United States

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Surface Currents

Surface Currents and their characteristics

Billie Jean Warta
1

eddies Currents

can twist and pinch off rings of water called .

2

equator

North Atlantic deep water flows toward the .

3

intensificatio western

The phenomena of stronger currents in western N . Pacific than in the eastern N . Pacific is called

4

dopplers drift bottles megaphones hydrophone

Microphones placed in the water to detect sound are called

5

gyre

The large , roughly circular cells of water that rotate around ocean basins & are driven by prevailing winds are called

6

Drif Wind West

The far southern current that circles the globe around Antarctica is called the

7

countercurren

The eastward flowing current along the equator , under the doldrums , is called the equatorial

8

geostrophic flo

Water movement that occurs as a result of a balance between gravity and the Coriolis effect is called

9

momentu

Wind driven currents will continue to move after the winds cease because of

10

Florida

The Gulf Stream is fed by the curren t

11

clockwis

Gyres in the Northern Hemisphere rotate

12

Transpor Ekman

Water is driven into the center of gyres by

13

drift bottle

Bottles that carry postcards in them are sometimes called

14

spira Ekman

The changing direction of water movement with depth in response to the overlying wind is called the

15

effec doppler

Measuring current directions and speeds by changes in the frequency of sound is based on the

16

meters Current

are the most common instruments used to measure the speed and direction of current s

17

convergenc

Surface water sinks in areas of

18

divergenc

Deep water rises to the surface in areas of

19

Sargasso

An excellent example of the transport of water into the center of a large gyre is the Sea in the North Atlanti c

20

Milankovitch

Cyclical changes in global climate are known as cycle s

21

divergence

Zones of permanent along the western sides of continents are good fishing ground s

22

90

Ekman transport is degrees to the direction of the win d

23

dense

There is no source for bottom water in the North Pacific similar to the North Atlanti c

24

surface

Deep water comes to the in areas of divergenc e

25

s m

Typical speeds for surface currents are usually about 0 . 1 to 0 . 5 / ( 0 . 3 - 1 . 5 ft / s )

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