NN204 Test II Review
David Underhill
Rules of the Road 1 to 12 –
10 points (PPT #09)
- The rules apply to all vessels in the great
lakes and inland US waters
- Deviate from the rules rather than get in an
accident
- Definitions of vessels (sailboat is … etc)
-
- All ships will maintain a proper lookout
- Safe speed – maintain a speed such that you
can avoid collision and stop in a reasonable distance
- Risk of Collision – assume you will collide if
you aren’t sure; don’t make assumptions on scanty radar information
- Action to Avoid Collision – alteration of
course and speed must be significant and easily noticeable to the other
ship
- Narrow Channels – stay close to the starboard
side; don’t impede less maneuverable ships
- Traffic Separation – cross at right angles,
enter at small angle if entering in the middle of the lane
- Overtaking, meeting, and crossing rules only
apply to ships in visual contact
- Sailing Vessels – a) if wind on different
side, then port has right of way; b) if wind on same side, leeward vessel
has right of way
Weather – 10 points (PPT
#10)
- Air Masses – large air body with similar properties
at a given height
- Types
- 1) Low Pressure – cyclonic, surface
convergence (upward vertical motion)
- 2) High Pressure – anti-cyclonic,
surface divergence
- Classifications by Temperature and
Humidity Properties
- Humidity
- c = continental (over land :: dry)
- m = maritime (over water :: moist)
- Temperature
- P = polar (cold)
- T = tropical (hot)
- Combinations of these are
classifications: cP, etc.
- Other classifications
- cA = c Artic = dry, extremely cold
- mE = m Equatorial = moist, extremely
hot
- Modifications to Air Masses as they move
(stability)
- Warm over cold is stable à little vertical
mixing (warm air is less dense so it rises)
- Dry air more dense and more stable
- Fronts
- Fast-moving fronts – 1:50 (vertical rise to
horizontal distance; km)
- Steep slope pushes front alongside or
ahead of the front
- Slow-moving fronts – gentler slope
(1:150, etc)
- Has cloud cover behind the front
(slide #22)
- Frontolysis – temperature contrast lessens
causing the front to break up
- Frontogenesis – temperature contrast
increases, strengthening the front
- Occluded Front – combination of a warm
and cold front; severe weather
- Cold Occlusion – cold air in the back
- Warm Occlusion – air is slightly
warmer in the back (cold up front, cool in the back)
- Triple Point – warm, cold, and
occluded front all touching; most severe weather
- Ways to locate a front: changes in
1.
Temperature
2.
Moisture
(dew point)
3.
Wind
direction
4.
Pressure
5.
Clouds
Navy Weather – 5 points
(PPT #11)
- Synoptic weather messages
- Every 6 hours: PRIORITY à wind < 33kts,
seas <12ft
- Every 3 hours: IMMEDIATE à wind > 33kts,
seas >12ft (sustained)
- Plain voice if cyclone, etc. sighted
- Weather report contents – type of
observation, cloud cover, visibility, pressure, air temp. (dew point and
dry bulb), water temp., true wind, altimeter setting, sea
height/dir/period, ice
- Services available
- Tropical Cyclone Alert
- High Wind and Seas Warning
- Local Severe Storms Warning
- WEAX – forecast request in MOVEREP;
periodic
- OTSR – Optimum Track Ship Routing –
ship specific weather and safe track
- Hurricane conditions of readiness (for
shore when winds > 50kts, for ships when winds >35kts)
- Condition of Readiness (COR) IV –
72hrs … COR III – 48 hrs … COR II – 24hrs … COR I – 12 hrs
- Weather changes
- Sand storms near Iraq
- Decreased comms, radar equipment
performance drops during bad atmospheric conditions
- Fog forms when the dew point temp
approaches the dry bulb temp (within 3°)
- Worsening conditions: falling
barometer, wind shifts, sea swells, cloud patterns
Tropical Storm – 8 points
(PPT #12)
- Heavy weather terms
- Closed cyclonic – rotating storms
- Tornado – violent rotating storm,
small diameter, over land, >150mph
- Waterspout – tornado over water (less
destructive)
- Squall – intense wind due to
atmospheric instability; comes and goes quickly; sometimes accompanied
by precipitation
- Monsoon – steady winds with frequent
squalls and thunderstorms
- Tropical Storm Types (based on wind
speed):
Hurricane > 63kts
- Tropical Storm 34 to 63kts
- Tropical Depression < 34 knots
- Noncyclonic – produced by prevailing
winds; predictable
- Gale: 34-47mph … Storm: >48mph
Semicircles
- Evasion in the Dangerous Semicircle
- 1) Get wind on the stbd bow (45° rel)
- 2) Make headway
- 3) Hold wind on the stbd bow
- 4) The storm will pass astern
- Evasion in the Less Dangerous
Semicircle – same as above except get the wind on your starboard quarter
(130° rel)
- Evasion on the Storm Track
- 1) Get wind on the stb quarter (160° rel)
- 2) Run for less dangerous semi-circle
- 3) If wind stays the same or moves
clockwise, then you are still in its path
- 4) Once winds shift to
counter-clockwise, you are in the less dangerous semi-circle
(follow its evasion procedure)
- Never cross in front of a storm
(“crossing the T”)
Sunrise/Sunset – 7 points
(PPT #13)
- Sunrise – when the sun’s
upper limb (UL) comes above the horizon
- Sunset – when the sun’s UL goes below the
horizon
- Civil Twilight – when the sun’s center is 6°
from the horizon
- Clear horizon; 1st and 2nd
magnitude stars visible
- Nautical Twilight – when the sun’s center is
12° from the horizon until Civil Twilight
- First chance to shoot a celestial fix
- 15° = 1 hr
- Sunrise is earlier for those
in the east
- Calculating sunrise/sunset
1.
Determine
approximate position
2.
Apply
latitude correction
3.
Apply
longitude correction (use closest std meridian)
- Days longer in summer (N hemisphere) b/c N
tilts towards the sun; occurs between 21 Mar (Vernal E) and 22 Sep
(Autumnal Equinox)
- Tropic of Cancer (north) and Tropic of
Capricorn (south); 23.5° latitude from equator
- Sun is directly overhead at solstices:
21 June (Cancer) and 21 Dec (Capricorn)
Celestial Navigation Theory – 20 points (PPT
#14, 14a)
Celestial Sphere Elements (PPT14)
- Celestial Sphere – infinite radius with
its center on Earth; has a North and South Celestial Pole and Celestial
Equator (in line with Earth’s)
- Hour Circle – great circles going
through the poles of the celestial sphere
- Celestial Meridian – great circles through
the poles and zenith
- Declination – degrees above or below
the celestial equator (0 is on it, 90 is upwards from the pole…)
- Parallel of Declination – circle
parallel to the celestial equator; path on which a star appears to move as
the Earth rotates
- Identifying a point on the celestial
sphere – requires declination and an hour angle
- Hour angles are from 0 to 360° and
referenced from one of three types:
- Sidereal Hour Angle (SHA) - angle
west of vernal equinox (Aries)
- Greenwich Hour Angle (GHA) –
angle west of Greenwich celestial meridian
- Local Hour Angle (LHA) angle west of
the observer’s celestial meridian
- Which references are used by different
bodies
- SHA: stars GHA: sun, moon, planets, and Aries
Motion
Earth rotates clockwise which makes the
celestial sphere appear to move slowly counter-clockwise (diurnal motion)
- GHAstar = GHAAries
+ SHAStar
- LHAstar = LHAAries
+ SHAStar
- GHAstar = LHAstar
+ longitude
Elements of the Horizon Coordinate System
- Zenith – position directly above the
observer
- Nadir – directly below the observer
- Observer’s Horizon – perpendicular to
zenith-nadir line / axis
- Celest.
Horizon – parallel to observer’s horizon but passes through center of the
Earth
- Altitude – star’s angle above the
horizon
- Sextant Altitude (Hs) – altitude
measured by a sextant
- Corrected Sextant Altitude (Hc) – Hs corrected for height of eye
- Observed Altitude (Ho) – altitude after
further corrections made to Hc
- Vertical Circle – great circle that
passes through zenith and nadir; perp. to the celest. horizon
- Principal Vertical
Circle – v. circle passing through the N and S
celest. poles
- Zenith – angle from the direction of
the north pole to the angle where the altitude is measured (angle from the
principle vertical circle to the vertical circle on which the star lies)
- Geographic Position – point on earth
over which a star is located (found by drawing a line from the star to the
center of the Earth)
Celestial Triangles
- Three points: (North) Celestial Pole,
Celestial Body, Observer’s Zenith
- Three sides:
- Co-altitude – from zenith to
celestial body = 90° - altitude
- Co-latitude – from zenith to
celestial pole = 90° – latitude
- Polar Distance – angular dist. from
celest body to celest pole = 90° +/- declin.
- Add
90 if the celestial body and pole are in different hemispheres;
subtract if in the same hemisphere
- Three inner angles (two important
ones):
- Meridian angle (-t-) – at celestial pole; related to LHA
- Azimuth Angle (-Z-) – at zenith
- Note: Given latitude, declination, and
a meridian angle, you may solve for altitude and azimuth angle
PPT14a
- Light from a star hits Earth at an
angle (changes over time as the Earth moves, etc)
- Co-altitude – angle between your
position and a star’s GP; angle from the vertical; = 90 - Ho
- Circle of Equal Altitudes – a set of
points on a circle centered on the star’s GP on which the altitude appears
the same for the star
- Radius is the co-altitude … 1min arc =
1nm so if co-alt. is 40 then your distance from GP is 40*60’/deg * 1°/nm
= 2400nm
- Getting a fix
- True Azimuth – Zn – direction to the
star’s GP … plot this
- Plot circle of equal altitude which is
a line perpendicular to the direction to the star’s GP
- Intercept – the difference between
radii of two circles of equal attitudes (on from Ho, one from Hc)
- Intercept is the distance between
your DR position and LOP position along your DR track
- If Observed Altitude (Ho) >
Computed Altitude (Hc) draw the LOP intercept
distance closer to the GP than your DR
- Ho Mo To à if Ho more then draw towards
GP
- Otherwise, draw the LOP intercept distance away from the
GP from your DR
- Once you have three LOPs in this
manner, you can get a running fix
Latitude Determination by
Local Apparent Noon or Polaris; Gyro Error – 10 points (PPT #15)
- Latitude by Local Apparent Noon
- 1st Case: Latitude =
Declination + 90° – Altitude à sun in the same hemisphere; sun latitude < your
latitude
- 2nd Case: Latitude =
Declination - 90° – Altitude à sun in the same
hemisphere; sun latitude > your latitude
- 3rd Case: Latitude = 90° –
Altitude - Declination à sun in a different
hemisphere
- Latitude by Polaris
- Polaris – named because it is almost
directly on the celestial north pole … makes the triangle “collapse” on
itself so that:
- Observed Altitude = Latitude
- Colatitude = Coaltitude
- Polaris is actually ¾° off of the pole – a
correction table is in the Nautical Almanac
- Gyro Error by Polaris
- Usable in the northern hemisphere
between the equator and 65° latitude
- Maximum desired Observed Altitude (Ho)
is 25°
- Compare Ho to value in the Nautical
Almanac; difference between the two determines gyro error
- Gyro Error by Sun Azimuth
- Compare calculated and observed
azimuth of the sun; difference between the two determines gyro error
Stella – 20 points