Competence 1 (Deck) assesses knowledge in maritime navigation, focusing on tidal current data, echo sounder operations, magnetic compass adjustments, chart types, and DGPS accuracy. It's designed for learners aiming to enhance their navigational skills for maritime applications.
Parabolic
Directional
Hyperbolic
Linear
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It corrects the semi-quadrantal error at intercardinal headings.
It compensates for the error caused by the vertical component of the earth's magnetic field.
It allows the magnetic compass to move freely in the fluid.
It reduces the deviation into half.
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Large scale chart
General chart
Coastal chart
Small scale chart
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Sh
Cl
Co
R
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100 m
50 m
20 m
10 m
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960
760
23.25
29.92
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Astronomical twilight
Civil twilight
Nautical twilight
Observational twilight
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Black band with above and below yellow band
Black band above and below yellow band
Black band below yellow band
Black band above yellow band
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"Night effect" is most prevalent late at night
During "night effect", polarization is at a minimum
"Night effect" is caused by all of the polarized ground waves being vertical
"Night effect" is caused by rapid changes in the ionosphere
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15deg. E
7 1/2deg. E
0deg.
7 1/2deg. W
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1 degree
0.2 degree
0.5 degree
0.1 degree
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1 astronomical unit (AU)
1 celestial unit
1 parsec
4.3 light years
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1. 50,000
Not more than 1. 25,000
1. 200,000
1. 1,000,000
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1013.25 millibars of mercury
1012.45 millibars of mercury
1013.52 millibars of mercury
1012.35 millibars of mercury
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234deg. T
063deg. T
270deg. T
243deg. T
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3 mins and 26 secs
3 mins and 36 secs
3 mins and 06 secs
3 mins and 56 secs
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Astern and equal to the ship's speed
Ahead and equal to the ship's speed
Ahead and equal to twice the ship's speed
Astern and equal to twice the ship's speed
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Increase the scope of anchor cable
Shorten the scope of anchor cable
Put over a stern anchor
Dropped another anchor
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Taking a radar range and radar bearing
Taking several radar bearings
Taking several radar ranges
Taking a radar range and visual bearing
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Dead-reckoning
Probable position
Applied position
Fix
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1010.35 millibars
1012.35 millibars
1013.25 millibars
1015.25 millibars
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Difference is assumed latitude and actual latitude
Inaccuracies in the reading and reference level
Double-second difference
Chronometer error and dip
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Nautical Almanac
Mariner's Guide
Tide Tables
Tidal Current Tables
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1.5 kilometers per second
1.3 kilometers per second
0.8 kilometer per second
1.1 kilometers per second
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24 kHz
18 kHz
27.5 kHz
33.3 kHz
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Event marker
Timing device
Unt selector switch
Range switch
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It remains the same.
It increases.
It decreases.
It fluctuates.
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Directional
Parabolic
Hyperbolic
Linear
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Blue-diode
Magnetostriction
Piezo-hydraulic
Diesel-electric
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Schools of big fish
Turbulence from the interaction of tidal streams with solid particles in suspension
Protruding rocks from the seabed
Bioluminescent microorganisms in the water
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Torque-induced precession
Equinoctial eccentricity
Gyroscopic inertia
Wobble parallax
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Error of collimation
Rapid error
Parallax error
Stream error
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It allows the magnetic compass to move freely in the fluid.
It compensates for the error caused by the vertical component of the earth's magnetic field.
It reduces the deviation into half.
It corrects the semi-quadrantal error at intercardinal headings.
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7â—‹W
0â—‹
4â—‹E
3â—‹W
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0â—‹
3â—‹W
4â—‹E
7â—‹W
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4â—‹E
0
7â—‹W
3â—‹W
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Great circle
Mercator
Rhumb line
Small circle
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Small scale chart
General chart
Coastal chart
Large scale chart
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Points of Zero variation
Point of equal variation
Magnitic dip
The Magnetic Latitude
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Quiz Review Timeline (Updated): Mar 21, 2023 +
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