Oceanography Basics Flashcards

(50 cards)

1
Q

Describe the three layer ocean model

A

Mixed layer (isothermal)

Thermocline (transition to cold water)

Deep water (deep and cold)

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2
Q

What is the limiting ray

A

Sound ray which grazes or is tangential to a boundary layer

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3
Q

What is the critical angle ray

A

Sound ray which strikes a boundary or surface at steepest gradient

More than this (steeper) causes reflection loses

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4
Q

Shadow zones

A

Sound rays reflect away from depths at acoustic maxima. Little sound penetrates causing shadow zones

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5
Q

What are the 5 transmission paths

A

Direct path

Convergence zone

Surface duct

Bottom bounce

Sound channel

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6
Q

What are the different types of channel

A

DSC/SOFAR channel (deep/bottom)

Shallow sound channel (45-180m)

Secondary sound channel ??

Half channel ??

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7
Q

How does CZ occur

A

Sounds rays penetrate the SLD and then refract upwards

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8
Q

What are the conditions for CZ

A

Deep water (5000’ +)

Bottom velocity larger that SLD velocity

Cx of 10MS +
DE of 360m

Large Signal Excess

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9
Q

What is the annulus on CZ

A

Ring of energy around source at the surface (10% of CZ Range)

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10
Q

What is the CZ depth excess?

A

Depth at which the SOS matches and supersedes the SLD.

Depth excess needs to be 360m + for a 50% chance.

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11
Q

Give examples of CZ ranges for the North Atlantic & Med

A

NA: 25-30nm

MED: 12-17nm

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12
Q

Explain the letters in relation to CZ

A
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13
Q

Explain the letters in relation to CZ

A
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14
Q

Where does BB prevail

A

SLD less that 15m

Shallow water - lots of interference

Deep water (1000’+) - BB ranges exist similar to CZ ranges

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15
Q

Name the two types of ocean fronts

A

Semipermanent

Temporary

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16
Q

Describe semi-permanent fronts

A

Associated with water mass boundaries

Stay static for long periods of time

Example: East Icelandic Front (Iceland-FAR-NOR)

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17
Q

Temporary Fronts

A

Temp changes to ocean structure due to abnormal weather or storms

Causes wind induced currents resulting in upwelling of cold water

Example: summer snow run off - Norwegian Sea

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18
Q

Name the Effects of fronts on sound

A

Abrupt changes is SVP

Higher AN (bio and fishing)

Errors in bearings (refracts to cold)

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19
Q

What are eddies and what effect do they have acoustically

A

Circular current flows that form on either sides for ocean currents

Up to 100nm in diameter

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20
Q

What are the 2 types of vertical ocean currents

A

Sinking of surface water

Upwelling

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21
Q

Describe upwelling and it’s Aco properties

A

In costal areas wind blows surface water seaward allowing cold water to rise in its place

High AN due to rich water - Bio/Fishing
Reduction in surface temp

22
Q

Describe sinking of surface water and its acoustic properties

A

Occurs at front boundaries where the denser cold water sinks

Causes currents, rip-tides, trapped debris

23
Q

Name the three types of bottom and their properties

A

Rock - smooth rocky bottoms are best reflectors but are rare and often covered in sediment (600m thick in Atlantic)

Sand - exploitable for BB when flat

Mud/Silt - poor reflector due to smaller particles. <300hz can be refracted

24
Q

Explain the continental shelf

A

Continental shelf - Smooth sand or mud
Shallow gentle decrease to 600’
High AN, good BB

Contains areas of continental borderland:
Irregular areas of shelf containing peaks and valleys (poor Aco properties)

25
3 types of bottom typography
Shelf Slope Deep ocean basin
26
Explain the areas to continental Slope (3)
Slope - sharp decrease from shallow to deep. Steep, jagged Rock Rise - base of slope, begins to flatten Sea fans - deposits of sediment at the mouth of submarine canyons Sub canyon - ancient valleys cut into the rise. Subs hide due to scattering
27
Explain the deep ocean basin
Deep regions between slopes
28
Describe the 4 areas of deep ocean basin
Abyssal plain - deep layer of sediment/mud, smooth, BB Trenches - very deep canyons in ocean floor Ridge - underwater mountains, barriers to sound (mid-Atlantic/reykjanes) Seamounts - isolated mountains
29
Explain the two types of seamount & Atolls
Guyot - flat topped Pinnacles - jagged Atoll - ring of reef islands
30
SPL
Sound pressure level
31
Name the two types of transmission losses
Spreading - distribution of energy as it moves from source Attenuation
32
Name the 3 types of spreading and their dB losses
Spherical - unbounded - 6dB Cylindrical - sound channel - 3dB Dipolar - source at SLD break - 12dB
33
What are the Types of attenuation loss
Absorption Scattering Leakage and boundary effects
34
Describe absorption
Energy converted to heat through molecular action Salinity up, temp down, frequency up = more loss
35
What are the 4 types of scattering
Volume - bio Bottom - sediment Deep Scattering Layer - bio Surface - wave action, wind.
36
What is the DSL
Deep scattering layer - daily migration of plankton and bio causing higher volume scattering 200m night 900m day
37
Describe leakage and boundary effects
Low frequencies can leak out of channels due to diffraction and scattering. Deeper and higher frequencies mean more ducting chance
38
Describe the active equation
SE = SL - 2PL - AN - RD + TS
39
Describe the passive equation
SE = SL - AN - RD - (DI) - PL
40
Describe passive FOM equation
FOM = SL - AN - RD - (DI)
41
Types of AN and frequencies (5)
Shipping - low freq (<500) Seismic - low Sea state - 500hz + Bio - various Precipitation - 10000hz
42
Describe the 5 layer ocean model
Mixed layer Seasonal thermocline - temporary where temp decrease Transient thermocline - mixing affect, short term (hours) Perm thermocline Deep water
43
Describe upslope transmission
A source in deeper water may send sound rays into shallower water Causes more reflection loss at boundaries causing less detectable sound
44
Describe down slope enhancement
Source in shallow water may reflect sound down slope til the water is deep enough for refraction into channels Larger range, more detection
45
Describe the Diurnal effect
The heating and cooling of the surface layer by the sun Means daily or during the day Heating causes more shadow zones/transient channels
46
What is the MLD
Depth at greatest temperature Captures heat and effects bio/plankton depth (AN)
47
Rarefaction
Pressure decrease point in a medium
48
Describe half channels
Sound rays refract upwards (if a + BLG exists)
49
Describe Compression
Pressure increase at a point in a medium caused by sound energy
50
Factors effecting SOS
Salinity 2 ft/s per 1/1000 increase Pressure 4ft/s per 100ft depth increase Temperature 6-8ft/s per F increase