1B.2 Weather Systems Flashcards
Define air mass.
A large body of air with similar temperature and moisture characteristics all the way through it.
Describe polar maritime air masses.
These come from the north-west and originate over the north Atlantic. They bring cool, moist conditions. In summer they bring sunny intervals with scattered showers and temperatures of 10-14°C. In winter temperatures are much lower (4-8°C) and sleet showers may occur. Winds may be strong as these air masses follow behind a depression.
Describe polar continental air masses.
These come from the east and originate over Scandinavia and Russia. They bring cold conditions in winter, with temperatures below freezing. It may snow in eastern Britain as moisture is picked up over the North Sea. In summer conditions are drier and warmer with fresh winds.
Describe tropical maritime air masses.
These come from the south-west and originate over the Azores or the Caribbean. They bring mild, damp, cloudy weather as they pick up moisture from the Atlantic Ocean. In winter they bring temperatures of around 8-12°C and in summer 14-18°C. The air is often humid as it lies within the warm sector of a depression.
Describe tropical continental air masses.
These come from the south and originate over dry northern Africa. They bring hot, dry weather and summer heatwaves with temperatures of 20°C. They may reach the south coast of England during summer but the cooling effect of the Atlantic Ocean reduces its influence on Northern Ireland. The air masses can last for several days and often end with thunderstorms.
Describe arctic air masses.
These come from a northerly direction and bring cold, snowy weather in winter and cool, damp weather in summer.
What is meant by a variable climate?
The weather changes from day to day, which makes it difficult to forecast.
What does an equable climate mean?
Extremes of heat or cold, drought or prolongued rainfall are rare.
What is a front?
The boundary between warm and cold air masses.
What is a depression?
A system or area of low pressure that can bring cloud, rain and windy weather.
Describe fully how a depression forms.
- The warm, moist Tropical Maritime air meets the colder, moist Polar Maritime air along the polar front, over the Atlantic Ocean.
- The warm air, being lighter and less dense than the colder air, starts to rise over the cold air. A low pressure is created on the ground.
- The warm air is sucked into the low pressure area to create a warm sector. The cold air is sucked in behind the warm air. This causes the entire air mass to start swirling in an anticlockwise direction.
- Where the warm air starts to rise over the cold air, is called the warm front. Where the cold air pushes in behind the warm air, is called the cold front. Between the fronts is a mass of tropical maritime air known as the warm sector.
What does a depression look like on a weather map?
A circular pattern of isobars (lines which join equal areas of pressure) with the lowest pressure in the centre and the winds blowing into the centre.
Describe and explain how temperature changes during the passing of a depression.
❄ As a depression approaches, the temperature remains low because colder, polar air dominates.
❄ As the warm sector passes over, the temperature rises because this is a pocket of tropical maritime, warm, southerly air.
❄ As the cold front passes, the temperature falls back because the wind swings from the north-west, bringing cold, polar air back once more.
Describe and explain how precipitation changes during a depression.
❄ Ahead of the warm front, there is higher pressure, so the air sinks, no clouds form and no rain occurs.
❄ As the warm front arrives, air is forced to rise over the dense, cold air. It cools, condenses and heavy rain occurs. There is less rain within the warm sector because the air is not forced to rise.
❄ At the cold front the cold sector is undercutting the warm sector forcing air to rise, cool and condense. This rapid uplift creates high clouds and heavy rain. Scattered showers follow the cold front because the polar maritime air crosses the ocean, picking up moisture.
Describe and explain how cloud type changes during a depression.
❄ As the warm front approaches, clear skies change to cirrus clouds due to the warm air rising, cooling and condensing along the front. These soon develop into thick nimbostratus clouds.
❄ In the warm sector, lower stratus clouds dominate as the uplift of air is less.
❄ At the cold front, air is forced to rise steeply because of the undercutting by cold air. This rapid uplift creates towering cumulonimbus clouds. After the cold front there is less uplift of air so the clouds are smaller, pathy cumulus.