water and ocean structure Flashcards

1
Q

what is heat

A

Energy produced by the vibration of atoms/molecules

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2
Q

what is temperature

A

Records only how rapidly the molecules of a substances are vibrating
*water molecules in hot water vibrate more rapidly than in cold water

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3
Q

what two pure water’s significant properties is Celsius (o C) based on

A

Freezing point – 0 o C
Boiling Point 100 o C

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4
Q

what is heat capacity

A

A measure of heat required to raise the temperature of 1gram of a substances by 1 o C

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5
Q

what is a calorie

A

the amount of heat required to raise the temperature of 1 gram of pure water by 1 o C

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6
Q

how does water temp affect its density

A
  • Close to freezing point, water density actually decreases when temperature continues to cool
  • Ice is lighter than an equal volume of water
  • Ice density increases with colder temperature, but never reaches that of water
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7
Q

how does evaporative cooling work

A

Water takes energy from somewhere to evaporate and remove heat from surfaces as it does e.g. water sweat takes heat energy from our bodies to evaporate, cooling us down

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8
Q

how does Seawater and pure water have slightly different thermal properties

A
  • Seawater is ~ 96.5% pure water and ~3.5% dissolved solids and gases
  • Lowers freezing point
  • Also changes calories needed to raise temperature
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9
Q

what is thermal inertia

A

tendency to resist a change in temperature
- ~18,000 cubic km of ice thaws and refreezes in the Southern Hemisphere every year – moderates Earth’s temperature

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10
Q

what moderates Earth’s temperature

A

Weather and Currents

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11
Q

where is the most evaporation

A

peaks in subtropics not tropics – need colder air over warm water for evaporation – air and ocean are both warm in tropics

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12
Q

3 Ocean density stratification zones

A

Surface zone / mixed layer – 2%
Pycnocline – 18%
Deep zone – 80%

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13
Q

how do conditions change in all 3 zones

A
  • Surface layer conditions are rather constant – good mixing due to surface wind mixing
  • Pycnocline changes rapidly (cline = quick change)
  • Deep zone – minor changes
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14
Q

what is a Thermocline essentially

A

difference in temp on surface vs depths
- Polar waters lack a strong thermocline

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15
Q

how does Thermocline depth and intensity vary

A

with season, local conditions (e.g. storms), currents, as well as other factors

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16
Q

what is refraction

A

bending of waves
- can Bend the Paths of Light and Sound Through Water
- can create shadow zones - regions where sound waves are blocked or do not travel effectively due to sound refraction

17
Q

what is Refractive index

A

degree that light is bent traveling from one medium to another

18
Q

2 main light zones in the ocean

A

Photic zone – sunlit portion
Aphotic zone – no light

19
Q

does light or sound travel further in the the ocean

A

Sound Travels Much Farther Than Light Through the Ocean – but varies with depth (effected by temp and pressure)

20
Q

whats the SOFAR layer

A

naturally occurring, deep-ocean sound channel where sound waves can travel long distances with minimal loss of energy - due to the unique way temperature + pressure affect the speed of sound in water

21
Q

what can be used to detect Underwater Objects and its 2 types

A

Sonar Systems
- Active sonar (sound navigation and ranging)
- Passive sonar – listening only

22
Q

what can be used to monitor the changing climate

A

sound through ocean - as its influenced by temperature, pressure, and salinity