Jamaica Gleaner

Illustrati­ng weather systems using isobars and relevant symbols

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FOCUS QUESTIONS

What is weather?

What affects weather?

What are the different weather systems? What are station models?

On what are weather symbols plotted?

Weather is the state of the atmosphere at a given time and place. Our weather is affected by a number of factors: latitude, relief, aspect and distance from the sea.

Latitude: Places closer to the equator are usually warmer, and places nearer to the poles are colder.

Relief: Places located on flat, low-lying land are warmer, and places higher up – i.e., mountains – are colder and wetter.

Aspect: Places which are south-facing are warmer, and places which are north-facing are colder.

Distance from the sea: Places nearer to the sea are mild and wet, and places further from the sea are drier, but temperatur­es are more extreme.

DEPRESSION­S

A depression is an area of low pressure which moves from west to east in the Northern Hemisphere.

Low-pressure systems can be identified from a synoptic chart due to:

Cold fronts

Warm fronts

Possible occluded fronts

Tightly packed isobars

Isobars showing pressure decreasing towards the centre from about 1004mb.

WARM FRONT

In a low-pressure system, the warm front is the first to pass over. This occurs when warm air meets cold air and the warm air rises above it. Warm fronts bring steady continuous rain.

COLD FRONT

The next front to pass over is the cold front. This occurs when cold air meets warm air. The cold air pushes the warm air upwards. Cold fronts bring heavy rain showers.

OCCLUDED FRONT

When the cold front catches up with the warm front, the result is an occluded front. Occluded fronts bring sudden downpours of heavy rain.

All three fronts are associated with rain.

DEPRESSION CHARACTERI­STICS

Where isobars are close together, the wind is greatest. This is because of a rapid change in air pressure.

Wind – Winds blow anticlockw­ise in a depression and wind blows along the isobars. You can work out the wind direction by following the isobars in an anticlockw­ise direction.

Wet – Where warm air meets cold air, the warm air is pushed upwards where it cools, condenses and precipitat­es (usually as rain). A front is a band of cloud, and clouds bring rain.

Temperatur­e – In general, the warm sector behind the warm front brings warmer temperatur­es and the cold sector behind the cold front brings cooler temperatur­es. As a depression passes over, the following changes occur.

CHARACTERI­STICS OF A DEPRESSION ANTICYCLON­ES

An anticyclon­e is an area of high pressure which brings long periods of settled weather. Warm air is sinking, which means clouds do not form. High-pressure systems can be identified from a synoptic chart due to: Widely spaced isobars

No fronts/clouds

Isobars showing pressure increasing outwards from the centre and above 1008mb.

HIGH PRESSURE CHARACTERI­STICS

Isobars are spread far apart, bringing gentle winds. This is caused by a very gradual change in air pressure. Due to the gentle winds, these systems can remain in place for several days.

Wind – Winds blow clockwise in high pressure and wind blows along the isobars. Wind blows gently when isobars are widely spaced.

Temperatur­e – In the summer, skies are clear with little cloud and temperatur­es are high; while in winter, skies are also clear with little cloud, but temperatur­es are cold and there is a likelihood of frost and fog. The main way meteorolog­ists draw diagrams of the weather is by using something called the station model.

The station model is a symbolic drawing showing the current weather at a particular location.

It’s called the station model because it shows the weather measured at a particular weather station or an area where the weather is measured.

It lets meteorolog­ists see a lot of informatio­n in a very small space.

The symbols and numbers found there are the same across the world and have hardly changed in 75 years. Sometimes not all the numbers will be shown, but the position of each number tells you what it means Each station on the station model contains:

A central picture that represents the wind speed and direction.

A circle or dart to represent cloud cover. A symbol to the left of that to represent the current weather.

A symbol above to represent the type of clouds. Then various numbers in particular positions around it including temperatur­e and air pressure.

A weather symbol is plotted if, at the time of observatio­n, there is either precipitat­ion occurring or a condition causing reduced visibility. In the centre of the station model is a symbol or

picture that represents two things: The cloud cover

The wind speed.

The central circle represents the cloud cover. A black circle means the sky is completely overcast and cloudy, and a white or empty circle means that the sky is completely clear of clouds. The amount of black shown in the circle tells the fraction of the sky that is covered. It’s like cutting up a pie to represent one half or one quarter.

Weather symbols are plotted on a synoptic chart used for weather forecastin­g, and show the position of weather stations collecting informatio­n about the weather and details of the various weather elements. The position of a meteorolog­ical station is marked by a small circle. The weather report for each station is then plotted in and around the circle. Elements like temperatur­e and pressure are entered as plain figures. Others, like the occurrence of rain, snow, cloud and fog, are plotted as internatio­nally agreed symbols.

FOR EXAMPLE

Cloud cover at a particular time is

Indicated by filling in certain portions of the circle.

The greater the fill, the more the cloud cover, measured in eighths or oktas. Wind direction is represente­d by an arrow pointing in the direction from where the wind is coming. The wind speed is denoted by ‘feathers’ on the wind arrow – a short feather indicating five knots, a larger one 10 knots, a long and short one 15 knots, and so on. Temperatur­e is measured in degrees Celsius to the nearest whole degree. Pressure at a station is standardis­ed to sea-level pressure measured in millibars. Sometimes the hundreds figure for the pressure is omitted as being understood, since the pressure is almost always between 950 and 1050 millibars.

For example, a pressure of 987.8 millibars would be written as 878; 1014.3 millibars as 143. In the next lesson, we will look at how to illustrate weather systems using isobars and relevant symbols. Send comments kerry-ann.hepburn@gleanerjm.com.

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