GSK - Meteorology Flashcards
Items of Meteorological Information found on Routing charts
-ocean current - set/ rate/ drift
-wind direction and force of weather rose
-mean air temperature
-mean air pressure
-hurricane forecasting
-fog percentage
-low visibility percentage
-TRS winds
-Shipping Routes
-Limits of ice
Synoptic Chart
The synoptic chart shows pressure systems (High and Low), isobars and weather fronts (Warm & Cold) at a given level over a large area at a given date and time
Its used for weather forecasting and the weather to be expected
Warm Front
- cirrus, altostratus, Cumulus, Stratus Clouds
- light to moderate prolonged rain ahed of front, patchy behind
- moderate or poor visibility in Fog
- Wind increases and backs
- pressure drops
- temperature rises
Occluded Front
- happens when either warm or cold front is suspended due to one catching up with the other and so no longer reaches sea level
- the depression is filling and so no more pressure starts to rise
-persistant rain and showers with moderate visibility - light winds as the system is decaying and slowly advancing
- increased amount of mid-level clouds conditions like those in warm sector
Cold Front
-brief Period of clear skys ahead of front
- Cumulonimbus clouds
- heavy rain and thunder at the front,
- very poor visibility at the front, excellent after
- wind decreases and veers
- conditions rapidly improving after
- pressure rapidly increases after
- temperature falls
Factors determining strength and direction of wind
- geographical location
- proximity of High and Low pressure systems
- pressure gradient between High and Low pressure systems
- proximity of land
Meteorological indications of approaching TRS (Tropical revolving storm)
-Falling Pressure 3mb below normal
-long low swell from direction of TRS
-appreciable change in wind strength and direction
-extensive cirrus clouds followed by altostratus
-good visibility
Karabatic Winds
Dangers…
- Occurs when there is intense radiation on a clear night
- this causes cooling over sloping ground
- cold dense air ´falls´down the mountain slope when the air below is less dense under the influence of
gravity - producing the Katabatic wind.
Dangers: strong offshore wind arriving without warning
Mistral wind is example
Barometer
barometer
records pressure at a given time
by using fixed pointer from a previous reading the change over a period of time can be observed.
Barograph
barograph
gives a continual readout on graduated paper by use of a pen and revolving drum thus provides for the yachtsman the ‘trend/tendency’.
Land Fog
Land (Radiation)
- forms over low-lying land on clear nights, when conditions are ideal for maximum radiative cooling, especially during the winter months
- Radiation Fog forming over land is cool and so the air is denser and will flow downhill.
- Occasionally it drifts out to
sea, but it is found no farther than fifteen miles offshore, as the relatively
- high sea surface temperature causes the fog to disperse
Sea Fog
When warm moist air flows over a cold sea surface and cools it to its dew point (vapor condenses)
Sea (advection) fog is formed.
- main type of fog experienced at sea
- may form and persist with moderate or even strong winds
Most common in: - Polar regions
- Grand Banks of Newfoundtland (Canada)
- near cold ocean currents, California, Chile Peru
- SW approaches to English channel
- north west Pacific Ocean
Effect of Land masses on the general direction of winds
land masses disturbs the ideal distribution
- due to local heating and cooling, pressure systems move
Weather in ITCZ
- variable light winds
- squalls and thunder storms clouds
- very hot and humid
Weather in Variables
/ Subtropical Anticyclone (STACs)
- fairly nice weather
- small amounts rain and clouds
Buys Ballots Law
in the northern Hemisphere when standing with your back to the wind, Low Pressure will. be on your left
Land Breeze
- land cools at night faster than at sea
- Cool air is denser and falls creating a H Pressure
- Sea cools more slowly creating a relatively Low Pressure
- Wind blows offshore from H to L
Name 6 Air Masses UK experiences
- Arctic Maritime (very cold, moist)
- Polar Continental (cold and dry)
- Tropical Continental (hot and dry)
- Tropical Maritime (hot and moist)
- Returning Polar Maritime (cold, very moist)
- Polar maritime (cold, moist)
ITCZ
Inter Tropical Convergence Zone)
How do clouds form
form as result of condensation of water vapor in the atmosphere
- Ascent in convention currents
- Uplifting at a front
- air being forced over higher grounds (mountains)
- radiation cooling
Trade Winds Weather
- persistent strong winds
- fair and small cumulus clouds
- generally nice weather
Warm Sector Weather
- Stratus clouds
- light to moderate showers
- moderate to poor visibility
- steady wind
- steady low pressure
- steady warm Temperature
Sea Breeze
- Land heats faster than sea during the day
- Sea warms more slowly creating a relatively Low Pressure
- warm air rises creating Low pressure at surface and H pressure is formed aloft
-pressure aloft is higher then same level at sea and so High Pressure moves towards the Low Pressure above the sea to equal out - cooler air falls, creating High Pressure at sea surface
- sea breeze results blowing onshore
Hygrometer
- Obtain a range of readings of the dry and wet bulb Maisons Hygrometer.
- Take the difference between the two (depression) and enter Mariner’s Handbook Dewpoint Table
- Plot graph with time against temperature
- At the same time obtain regular readings of the sea surface temperature.
- where 2 lines cross, Fog is present
- Start of Advection fog is likely when the Dew Point of the air is within 5° C of the sea surface temperature