METEOROLOGY Flashcards

1
Q

What is the typical weather in the UK? Why does UK get bad weather?

A

Area of low pressure with associated frontal activity
UK is situated in temperate climates between 50 and 60 degrees north. The polar front is the boundary in between cold polar air coming from the north and warm wet tropical air from the south.
Where these to air masses meet causes a pressure difference causing a Jetstream. Blows from West to East. Causes development of low pressure systems
Warm wet air is forced to rise quickly leading low pressure.
Surface air winds will blow in towards the centre of the low pressure.
The Coriolis force in the northern hemisphere causes the winds to be deflected to the right leading to an anticlockwise circulation of air around the Low pressure system.
The anticlockwise circulation of air draws a wedge of warm air into the cold air to the north, forming 2 distinctive fronts (warm front and cold front)
Movement of the Low pressure system itself is driven by the prevailing South westerly winds as well as the Jetstream which blows west to east.
Low pressure system generated on the eastern seabed of north America.

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2
Q

Describe the passage of a low pressure system in the UK

A

Warm fronts are slow moving, the warn air climbs above the cold air ahead.
Cold front are more active and vivacious. Moves faster as the cold air undercuts the warm air ahead. The cold front forces the air to rise.

As Low-pressure approaches
- Drop in barometric pressure (3 Hpa in 3 hours)
- Strengthening winds. (Higher pressure gradients mean stronger wind speeds)
- Initially cirrus clouds, then stratus clouds. Cloud level dropping.
- Moderate and persistent precipitation as the warm front approaches
As warm front passes
- Distinct veer in the wind direction (SE to SW)
- Temperature rises slightly
- Humidity increases significantly
- Barometer falls more slowly
- Rain ceases
- Skies clear for now

Warm sector
-	Wind strength and direction steady
-	Barometer falls slowly until we reach the closest point of the 
As Cold front passes
-	Wind veers (From Sw to NW)
-	Temperature falls dramatically
-	Humidity falls
-	High towering cumulous clouds form
-	Heavy precipitation and potentially thunderstorms
-	Barometer rises fast
In cold sector
-	Clear skies
-	Fair weather
-	Altocumulus clouds
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3
Q

What weather in an occlusion?

A
  • Stratocumulus cloud. Covers most of the sky and high vertical extent
  • High precipitation
  • Tend to occlude at the centre of the low pressure
  • High wind speeds
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4
Q

What is a trough?

A

An area of organised precipitation

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5
Q

What is a TRS?

A

An area of intense low pressure that forms over warm seas.

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6
Q

What are the conditions required for a TRS to form?

A
  • Minimum sea temperature of 26 degrees Celsius
  • A pre-existing low pressure system
  • Between latitudes 5 and 25 North or south of the equator.
  • Certain time of year
  • Minimum air turbulence
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7
Q

Draw a diagram of a TRS

A

Draw

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8
Q

How does a TRS form?

A

There required conditions for the formation of the TRS must be met
A pre-existing low pressure would find its way over the warm sea temp.
The sea temp will cause the air in the centre of the low pressure to start to rise rapidly. Rising warm wet air causes the pressure of the centre of the low pressure to deepen intensely.
Causing the surface winds to blow strongly towards the centre of the depression. The Coriolis force bends the wind to the right. Causes a very tight circulation of air around a column of rising air
A tight circulation of air causes the storm itself to rotate. The resultant vortex in the centre of the storm causes the air to rise even faster, which causes the pressure in the centre to deepen further.

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9
Q

You find that there is a TRS. What action do you take?

A
  • Revise voyage plan consider contingency plans
  • Consider ports of refuge
  • Brief the crew
  • Stow for sea
  • Close WTD
  • Ensure optimum stability
  • Monitor weather forecasts and navigational warnings
  • Stay in the navigable sector where possible
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10
Q

What are indications of a TRS?

A
  • Navigational warnings
  • Barometric fall. (Including corrections). If the barometric reading is 3 mb below the seasonal average, there is a possibility of a TRS. If it is 5 mb below the seasonal average, there is a TRS.
  • Change of wind direction than normal trade winds.
  • Long low swell from the direction of the storm
  • Dramatic clouds. (Cirrus clouds in a v point in the direction of the storm)
  • Vivid sunrises and sunsets
  • Lack of marine wildlife
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11
Q

What is diurnal variation?

A

Daily fluctuation of atmospheric pressure caused by the temperature

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12
Q

What is the dangerous quadrant of a TRS? What is the navigable semicircle? How to evade a TRS?

A

Dangerous quadrant. The reason it is called the dangerous quadrant is due to the
• increased wind speed due to the advance of the storm
• Due to the potential of being in the path of the storm
Signs that we are in the dangerous quadrant is that Wind veering. To evade the dangerous quadrant, put the wind on the SB bow
Navigable semicircle. Signs that we are in the navigable semicircle. Wind backing. Put the wind on the SB Quarter
If steady wind direction and barometer dropping, vessel is in the path of the storm.
1,2,3 rule.

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13
Q

What is the track of a TRS? What causes re-curvature of the TRS?

A

The predicted track of a hurricane is usually West – North West. Driven by prevailing winds.
Re-curvature could be caused by:
• Change in conditions in the leading edge of the storm
• Seeking warm water
• Coriolis force

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14
Q

What are the names and times of year of TRS?

A
N Atlantic Hurricane May – December
NE Pacific Hurricane May – Nov
NW pacific Typhoon Apr - Dec
N Indian Ocean cyclone Mar – Dec
S Indian Ocean cyclone Nov - May
Australasia Hurricane Nov – May
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15
Q

What is a barometer? What is a barograph? What is a precision aneroid barometer?

A

Metal chamber, partially exhausted of air and hermetically sealed. It is susceptible to the slightest changes of pressure, which causes it to expand or contract. These movements are mechanically amplified and displayed on a dial.
Barograph The mechanical linkage movements are recorded on a chart attached to a revolving drum.
Precision aneroid barometer. The mechanical linkage between the cell and the display is replaced by an electronic link with increased accuracy

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16
Q

What is an anemometer?

A

Measures wind speed and direction relative to the vessel. The acoustic resonance anemometer is commonly found on ships due to its size and lack of moving parts.

17
Q

What is a hygrometer? What is a wet/dry bulb thermometer? What is a whirling pshycrhometer?

A

A hygrometer is an instrument used for measuring the moisture content in the atmosphere.
Wet/dry bulb thermometer. Consists of two thermometers, one that is dry (dry-bulb) which measures the air temperature and another that is covered in muslin and kept moist (wet-bulb) with distilled water and wick. Evaporation of water from the wick lowers the temperature of the wet bulb. The rate of evaporation is inversely proportionate to the relative humidity. These thermometers are kept in a well-ventilated louvered screen, painted white (Stevenson’s screen) which provides protection from radiation, sea spray, rain and wind.
Whirling or sling Psychrometer. It works on the same principle as the marine screen, except the 2 thermometers are attached to a handle and swung around for a certain amount of time. It is used for field measurements, although it is less accurate.

18
Q

What is fog? Describe 2 different types of fog

A

Fog is supercooled water droplets suspended in the atmosphere. Dew point is the temperature of the air mass at which water molecules will condensate.
Radiation fog. The cooling of land overnight by thermal radiation cools the air close to the surface, causing condensation of vapour particles leading to fog. It usually dissipates soon after sunrise as the ground warms.
Advection fog. Advection fog occurs when moist air passes over cooler water. The air reaches dew point, condensates and forms fog. It lasts longer than other types of fog. It requires a wind to be present to shift the air mass. Has a limited vertical extent. Commonly found in the following areas:
• Grand banks of nova scotia. Warm air from the south. Labrador current.
• West coast of the US. Warm air from the West meeting cold currents which run down the west coast.
• English channel. Warm south westerlies blow over the English channel March and April

19
Q

How do you predict fog?

A

Using a hygrometer. Take a series of temperature readings from the wet-bulb and dry-bulb. Also take readings of the sea temperature.
With the dry bulb reading and the depression of the wet-bulb, relative humidity and dew point can be obtained from the dew point table provided in the Mariner’s Handbook.
Plot the dew point temperatures and sea surface temperatures against the time, in order to predict the likelihood as well as the time of formation of fog.

20
Q

What if the dry-bulb and wet-bulb thermometers read the same?

A

Then we have reached dew point. If the conditions are adequate for the formation of fog, I would expect fog.

21
Q

Describe the formation of land breeze, sea breeze and katabatic winds.

A

Sea breeze. On a clear day, the sun heats the land, which in turn heats the air above. The air rises leaving an area of low pressure which is filled by the cool dense air above the sea surface
Land breeze. At night, the land cools rapidly, which in turn cools the air above, the cool dense air fills the low pressure created by the relatively warm air over the sea rising
Katabatic winds. Cool dense air is pushed towards the sea by predominent winds, it is then accelerated by gravity due to the high inclination of the topography.
The Anabatic Winds are the mild uphill reverse of the Katabatic winds

22
Q

What causes the NE and SW monsoon in the Indian ocean?

A

The monsoon circulation is a continental wind pattern which undergoes a seasonal reversal in direction.
NE Monsoon. In the northern hemisphere winter the great land mass of Asia becomes very cold, and an intense area of high pressure becomes established over Siberia.
SW Monsoon. In the summer the Asiatic high disappears to be replaced by a deep and extensive area of low pressure centred over NW India, due to the great heating of southern Asia

23
Q

Weather forecast terminology

A

Wind speed
• Gale Winds of at least Beaufort force 8 (34–40 knots) or gusts reaching 43–51 knots
• Severe Gale Winds of force 9 (41–47 knots) or gusts reaching 52–60 knots
• Storm Winds of force 10 (48–55 knots) or gusts reaching 61–68 knots
• Violent Storm Winds of force 11 (56–63 knots) or gusts of 69 knots or more
• Hurricane Force Winds of force 12 (64 knots or more)
Visibility
• Very Poor/Fog Visibility less than 1,000 meters
• Poor Visibility between 1,000 meters and 2 nautical miles
• Moderate Visibility between 2 and 5 nautical miles
• Good Visibility more than 5 nautical miles
Time
• Imminent Expected within six hours of time of issue
• Soon Expected within six to 12 hours of time of issue
• Later Expected more than 12 hours from time of issue
Sea state
• Smooth Wave height less than 0.5 m
• Slight Wave height of 0.5 to 1.25 m
• Moderate Wave height of 1.25 to 2.5 m
• Rough Wave height of 2.5 to 4.0 m
• Very Rough Wave height of 4.0 to 6.0 m
• High Wave height of 6.0 to 9.0 m
• Very High Wave height of 9.0 to 14.0 m
• Phenomenal Wave height more than 14.0 m