Weather Flashcards

1
Q

What is the ITCZ?
Where is it found (does it move)?
What weather do you get there?

A
  • Intertropical Convergence Zone is a belt of low pressure where the trades winds of the North and South Hemispheres meet.
  • It is found on or near the equator. It moves seasonally, following the sun.
  • Light winds alternating with squalls and thundery showers.
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2
Q

What is the STAC?
Weather at STAC?

A
  • The Sub Tropical Anti Cyclone (STAC) is an area of high pressure.
  • Calm winds, sunny skies, little precipitation.
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3
Q

When is the NE Monsoon and typical weather?

A
  • In N hemisphere winter, anticyclone develops over COLD Asian continent (high pressure).
  • November to March
  • Winds mod to fresh, weather cool, fair, broken clouds, (their dry season).
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4
Q

When is the SW Monsoon and typical weather?

A
  • In N hemisphere summer, land heats up, creates an area of low pressure
  • Persistent SW Monsoon winds from May to September
  • Winds fresh to strong, larger seas, significant amount of clouds and rain, there wet season.
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5
Q

When is the inter-monsoon period and typical weather?

A
  • April to May and October to November
  • Usually light variable winds and warm weather. However, this is also the time that TRSs can occur.
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6
Q

How is fog formed?

A
  • When air is cooled to its dew point it becomes saturated with water vapour and the condensation of this water vapour is what causes fog.
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7
Q

What are the different types of fog?

A
  • Advection (Sea) Fog
  • Radiation Fog
  • Sea Smoke
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8
Q

When does Advection fog occur?

A
  • When warm moist air flows over a cold sea.
  • Typical in areas where a warm and cold current meet (e.g. Labrador and Gulf Stream off New Found land)
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9
Q

When does sea smoke occur?

A
  • Occurs in high lats when very cold air blow over a relatively warm sea.
  • The water vapour evaporating from the sea cannot be held by the very cold air so it condenses and forms fog.
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10
Q

When does radiation fog occur?

A
  • Occurs over low lying land, on clear nights, typically.
  • The heat trapped in the earth cools and forms fog.
  • Can blow out onto the sea but never more then 10-15 miles
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11
Q

How can you forecast sea fog?

A
  • Difference between the wet and dry bulb can be used to work out dewpoint using the dewpoint table in the Mariners handbook
  • When the dewpoint is within 5° of the sea surface temperature then fog can be expected
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12
Q

What is a TRS?
Where do they form?
Typical movement and speed?

A

TRS = Tropical revolving storm (Typhoon, Cyclone, Hurricane)

  • A very low depression.
  • Form in warm water (≧26°C) of the tropics.
  • Start off around 10-15 knots in a WNW direction (N HEMP), WSW (S HEMP).
  • They may recurve around the STAC but movement can be erratic.
  • If a TRS does recurve then it usually slows down, possibly even stop, and then speed up again to 20-25 knots.
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13
Q

Describe the signs of an approaching TRS

A
  • Possible TRS if barometer is 3mb below mean for that area (mean found in sailing directions)
  • Definite TRS if the barometer is 5mb below mean
  • Significant change in wind strength and direction
  • Long low swell from the direction of the TRS
  • Squally heavy rainfall in the vicinity of TRS
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14
Q

Imagine you are on a ship whose course will pass through the eye of an approaching TRS. Describe the weather you would expect?

A

Edge of Storm (200 to 250 miles from eye)
- Pressure 5mb below seasonal mean.
- Winds F 6/7.
- Some rain from outer bands may be encountered.

125 miles from centre
- Gale force winds.
- Cloud and rain becoming more continuous.

80 miles from centre
- Pressure 10mb below mean, falling rapidly
- Hurricane force winds

Eye Wall
- Pressure 20mb below mean
- Driving wind and spray reducing visibility to zero

Eye
- Winds light or mod
- Clear sky
- Vis still near zero due to high, confused seas

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15
Q

What is the dangerous semi-circle and actions to take?

A
  • The dangerous half will always be in the direction that the TRS recurves
  • Put the wind on a bow and alter course to the same side as the wind backs/veers
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16
Q

Three reasons why the the advance quadrant of the dangerous semi-circle is the most dangerous?

A
  • Strongest winds.
  • Wind is pushing you towards centre of the storm.
  • The would recurve towards the vessel.
17
Q

What is the navigable semi-circle and actions to take?

A
  • Navigable semi-circle is opposite to the dangerous side. Storm would recurve away from the vessel
  • Put the wind on a quarter and alter course to the opposite side as wind backs
18
Q

How can determine the centre of the storm?

A

Apply Buy’s Ballots Law
- Face the wind, storm centre will lie 12 points to right in N.hemp and 12 points to the left in S.hemp.

19
Q

How can I determine if I am behind or in front of the trough line?

A
  • If pressure is decreasing you are in front
  • If pressure is increasing you are behind
20
Q

If I am in a TRS but the wind does not appear to be backing or veering, where am I and what action should I take?

A
  • You are in the path of the storm.
  • Take action as you would in a navigable semi-circle.
21
Q

Which way does the wind rotate in N.hemp and S.hemp?

A

N.hemp
- Anti-cyclone - clockwise
- Cyclone - anti-clockwise

S.hemp
- Anti-cyclone - anti-clockwise
- Cyclone - clockwise

22
Q

What information should be reported by the master when encountering a TRS?

A
  • Time, date, position of ship at time of observation
  • Pressure
  • Pressure trend
  • True wind direction
  • Wind force
  • Sea
  • Swell
  • True course and speed
23
Q

After the Masters first report how often should further reports be made?

A
  • Ideally every hour, not exceeding 3 hours
24
Q

Define Relative Humidity?

A
  • A ratio expressed in percent, of the amount of atmospheric moisture present relative to the amount that would be present if the air were saturated.
25
Q

Why do TRS not form in the South Atlantic

A
  • Water temp is not warm enough, cold water is brought up from the South Pole by the Benquella current
  • There is a high amount of wind shear in the atmosphere which stops a TRS from forming is vertical column of circulating air therefore stops it from forming