Ch 6b: Hydrosphere (Oceans) Flashcards

(40 cards)

1
Q

Oceans cover:

A

71% of Earth’s surface, uneven distribution.

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2
Q

Max depth of the ocean, average depth, volume of water

A

11km, 4.5km, 1.35x10^18

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3
Q

Ocean structure

A

Changing layers: fresh water influx, ocean size, more land exposure. Temperature, salinity, density

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4
Q

Ocean layer changes are more

A

noticeable at the surface and near coastlines.

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5
Q

Ocean water properties: Density

A

Variable and Temperature dependent, pycnocline.

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6
Q

Ocean water properties: Salinity

A

varies from 32-37%. Increases with depth, salinity is high where evaporation is high. Low where river water enters ocean

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7
Q

Temperature and Salinity with Depth

A

saline water is denser sinks

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8
Q

Halocline:

A

is region of rapid salinity change

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9
Q

Thermocline:

A

is zone of rapid temperature change

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10
Q

Ocean Temperature:

A

surface varies from 0 to 28degrees, still remains above 0 at depth. Lowest is 0.4 as salt doesn’t allow the water to freeze.

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11
Q

Ocean composition

A

relatively constant, proportions do not change but the amounts can change. Species maintain

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12
Q

Ocean movement: surface currents

A

Wind driven surface currents, 10% by volume. Caused by atmospheric circulation and Earth’s rotation. Affects upper 100m

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13
Q

Large scale movement: subsurface

A

Density driven subsurface currents, 90% by volume. Drives the thermohaline circulation

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14
Q

ENSO

A

El Nino -southern oscillation, occurs in the pacific ocean. Extreme ends are termed El Nino and La Nina

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15
Q

La Nina

A

lower pacific ocean temperature than normal

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16
Q

El Nino

A

higher pacific ocean temperature than normal

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17
Q

Coriolis Effect

A

Objects moving in a straight line appear to curve relative to observer on solid Earth

18
Q

Coriolis Effect: Rotates about its vertical axis

A

CCW in Northern Hemisphere,

CW in Southern Hemisphere

19
Q

Ekman Effect

A

Coriolis deflects wind driven currents in Northern hemisphere. Slightly CW of actual wind direction, deeper currents are progressively rotated CW. Overall average water movement is 90degrees CW of wind

20
Q

Ekman Transport: Upwelling occurs…

A

where Ekman Transport is offshore

21
Q

Ekman Transport: Downwelling occurs…

A

where Ekman transport is onshore

22
Q

Geological Aspects

A

dominated by plate tectonics, sedimentation

23
Q

Continental Margins

A

Type depends greatly on plate tectonic activity, type determines coastal shape and properties.

24
Q

Continental Margins: Active Margin

A

occur along subduction zones or transform faults. Volcanically and tectonically active regions. Sediments of variable thickness. (terrigeneous, carbonates, volcanics)

25
Continental Margins: Passive Margin
Occur far from plate boundaries, flat lying, gentler gradients. Abundant shallow water sediments. (terrigeneous, carbonates)
26
Coastlines Modified by:
waves, tides, mass wasting events, uplift.
27
Coastlines are regions of
erosion and deposition
28
Waves created ...
primarily by the friction between water and wind.
29
Larger waves are created by:
earthquakes, landslides, volcanic eruptions, extraterrestrial impacts
30
Wave depth is about
1.2 the wavelength
31
In deep water, the wave speed is
V = L/T
32
Wave strikes the beach at an angle, explain
Part of the wave nearest the shore hits the shallow water first and slows down, creates a bend in the wave and rest of the wave follows the bend
33
Longshore Transport is
a shallow water current, moves parallel to the shoreline. Caused by wave refraction. Controls depositional shoreline features and erosion and transport of sediment.
34
Tides are due to
gravitational pull of the sun and the moon.
35
Types of Tides:
Spring and Neap
36
Tides: Neap
low difference between low and high tides
37
Tides: Spring
big difference between low and high tides
38
Beaches are
gently sloping surfaces, washed over by waves, covered with sediment, deposition or erosion dominated, short-term and unstable features
39
Sea Level Changes are usually
local to regional in effect: tectonic uplife or subsidence, isostatic rebound, global warming, human causes
40
Sea Level ups and downs
Glaciation promotes drops and global warming promotes rises.