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NATIONAL 4 and 5 GEOGRAPHY
WEATHER ST. ANDREW’S HIGH SCHOOL MRS CARRUTHERS, MISS CURLEY AND MS LYNAS
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Checklist – What do I need to know?
What will I learn? What factors affect temperature What factors affect precipitation How to read synoptic symbols How to read a synoptic weather chart and base forecasts on it What the main air masses affecting the UK are What type of weather we associate with a cold front, warm front and depressions How wind speed and direction is connected to isobar patterns What type of weather we associate with anticyclones
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INTRODUCTION Visibility Sunshine Cloud Cover Wind Speed Air Pressure
WEATHER ELEMENTS Precipitation Cloud Cover Wind Speed Sunshine Air Pressure Humidity Visibility
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Factors that affect Weather in the UK
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1. LATITUDE (how far North or South you are from the Equator)
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- Places closer to the equator are warmer
- The further North or South you travel the colder it gets - This is because the Sun’s energy is concentrated at the equator - The distance that energy travels through the atmosphere is less at the equator so less heat is reflected by clouds, gas and dust - The equator is green and absorbs the sun’s energy but the poles are white and reflect the sun’s energy
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2. ALTITUDE (how high up you are)
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- The higher up you go the colder it gets
- E.g. as you climb a mountain the temperature drops - Wind speed also increases at altitude - Rain is common higher up as warm air is forced to rise and starts to condense
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3. ASPECT - In the Northern Hemisphere, north facing slopes make good ski runs as they receive little sunlight during the day - South facing properties often have conservatories as they receive a lot of sunlight during the day. - South facing slopes are better for growing crops on In the Southern hemisphere the opposite would be true In the UK, West facing slopes receive more rain because the Atlantic Ocean is to the west, bringing moist winds.
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Distance from the sea affects temperature.
In summer places which are inland are usually warmer than places near the coast. In winter, inland places are colder than places near the coast. Distance from the sea affects temperature since the sea takes longer to heat up than the land. Once warm, however, the sea keeps its heat for longer.
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Inland areas are away from the influence of sea air.
4. DISTANCE FROM THE SEA (continued) In summer, the sea is cooler than the land and coastal regions are cooled by sea air. In winter, the sea is warmer than the land and coastal regions are warmed by sea air. Inland areas are away from the influence of sea air. Inland areas get very hot in summer. Inland areas get very cold in winter.
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Coastal Area Cooled By Sea Breeze on A Summer’s Day
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Coastal Area Warmed By Sea Breeze on a Winter’s Day
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AIR MASSES
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Main Air Masses affecting the UK
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QUICK SUMMARY OF AIR MASSES
Area air mass has come from Weather characteristics Arctic Cold Tropics Warm Land Dry Water Wet
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WINTER WEATHER CONDITIONS SUMMER WEATHER CONDITIONS
AIR MASS WHERE IT CAME FROM WINTER WEATHER CONDITIONS SUMMER WEATHER CONDITIONS Arctic Maritime Arctic Ocean Very cold and snow Cold and wet Polar Continental Northern Europe and Siberia in Russia Very cold and dry Hot, dry and sunny Polar Maritime North Atlantic Ocean Cool, cloudy and rain showers Tropical Continental Northern Africa and Southern Europe Mild, dry and sunny Very hot, dry and sunny Tropical Maritime South Atlantic Ocean Mild and wet Warm and wet
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QUESTION CLEARER ON NEXT SLIDE
2014 n5 EXAM QUESTION QUESTION CLEARER ON NEXT SLIDE (3 marks)
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Describe how a prolonged spell with a tropical continental air mass in summer would affect the people of the British Isles? (3 marks)
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MARKING SCHEME ANSWER A tropical continental air mass will bring hot dry weather in summer which could result in droughts (1); there might need to be hosepipe bans (1); grass might wither and die causing problems for livestock farmers (1); ice cream sales might rise (1) as people make the most of the sunny weather and head for the beach (1); it could be very hot and difficult to do physical work outside (1); heavy rain from thunderstorms might cause flash floods (1).
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WEATHER STATION CIRCLES
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Weather station circles
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LETS TRY TO MAKE YOUR OWN WEATHER STATION CIRCLES
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A B Temperature 14 C 3C Wind Speed 10 knots 25 knots Wind Direction
3C Wind Speed 10 knots 25 knots Wind Direction West North Weather Rain Snow Cloud Cover 6 Oktas 8 Oktas
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C D Temperature 22 C -5C Wind Speed 15 knots Calm Wind Direction
-5C Wind Speed 15 knots Calm Wind Direction South West Weather Drizzle Fog Cloud Cover 8 Oktas Sky Obscured
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Weather Fronts
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What happens at fronts? A warm front means that warm air is coming.
At a warm front, warm air is rising over cold air. This usually produces clouds and rain. A cold front means that cold air is coming. At a cold front, cold air pushes under the warm air. This produces strong winds and heavy rain.
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AIR PRESSURE SYSTEMS (Depressions & Anticyclones)
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AIR PRESSURE SYSTEMS Cold air falling causes HIGH pressure.
LOW pressure is when air is light and rises up into the upper atmosphere. HIGH pressure is when air is heavy and is pressing down on the surface. Warm air rising causes LOW pressure. Cold air falling causes HIGH pressure. wind The Earth’s surface is warmed by the sun’s rays. AIR PRESSURE SYSTEMS
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Each of these systems brings different weather!
AIR PRESSURE SYSTEMS Low pressure systems (less than 1000mb) are called DEPRESSIONS. They spin in an anti- clockwise direction. High High pressure systems (more than 1000mb) are called ANTICYCLONES and they spin slowly in a clockwise direction. Low Each of these systems brings different weather!
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Passage of a Depression
This is a satellite photograph of a depression. Note the swirling pattern of white clouds. The dark is the sea below the system.
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LOW Pressure is also known as a DEPRESSION
Cold Sector Warm Sector Depressions are made up of different air masses. Where these air masses meet is known as a ‘front’.
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When depressions move, the weather changes.
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Describing and Explaining DEPRESSIONS
NOTE: Explaining weather in a depression is very difficult. The following sentence enders should help: …as warm air is forced to rise over cold air, condensing and forming clouds …as there is warm/cold air overhead …as the isobars are close together 36
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DESCRIBING and EXPLAINING DEPRESSIONS
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Passage of a Depression
COLD SECTOR AT THE COLD FRONT IN THE WARM SECTOR WARM FRONT WEATHER Temperature starts to decrease because there is cold air overhead. Air pressure starts to increase. Cumulonimbus clouds Heavy rain/ thunderstorms because warm air is forced to rise over cold air as it is less dense. Warm air starts to condense and form as clouds leading to rain. The rain here is heavier than the warm front due to the gradient between the two air masses. Wind speed starts to increase Stratus clouds Temperature starts to increase because there is warm air overhead. Rain showers Wind speed starts to increase because isobars are closer together Air pressure drops as warm air is rising. Cirrus clouds can be seen high in the sky Rain begins because warm air is forced to rise over cold air as it is less dense. Green Text = Describe Red Text = Explain
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HIGH Pressure is also known as an ANTICYCLONE
There are no ‘fronts’ in an Anticyclone – it is just one air mass.
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Differences between SUMMER and WINTER ANTICYCLONES
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HIGH PRESSURE LOW PRESSURE
Anticyclones Pressure increases towards the centre Isobars are widely spaced Light winds Winds move in a clockwise direction Little cloud Dry Depressions Lowest pressure in the centre Isobars are close together Strong winds Winds move in an anti-clockwise direction Warm and cold fronts Unsettled weather Rain at the fronts Cloudy skies
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How to Answer a popular weather question
SIMILAR TO NATIONAL 5 2014 EXAM QUESTION PAY ATTENTION TO THE STRUCTURE
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Synoptic Chart for the British Isles at 0700h on 31 August
A yacht race from Wick to Stornoway was due to start from Wick harbour at 8.00am on 31 August At 7.00am the Met Office advised the race organisers to cancel the race. With reference to the synoptic chart, explain why this advice was given. 5 marks
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What are the key words? use the information on the map
type of boat : think! place : see map A yacht race from Wick to Stornoway was due to start from Wick harbour at 8.00am on 31 August direction : see map time : compare with map At 7.00am the Met Office advised the race organisers to cancel the race. change of plan! use the information on the map With reference to the synoptic chart, explain why this advice was given. 5 marks number of points to make
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Link question to the map
31 August Where? Wick and Stornoway Direction? From Wick to Stornoway When? Race due to start at 0800h Map is for 0700h
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Study the map for information
Occluded front: broad belt of very heavy rain, low cloud and poor visibility Centre of low pressure : likely to bring stormy weather Cold mP air Tightly packed isobars : strong winds South westerly winds Warm mT air Associated weather is moving west to east
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Back to the question …. Why was the race cancelled?
Competitors would risk very strong winds and therefore high seas They would be sailing straight into the wind so it would be difficult to make progress Temperatures would be low There would be heavy rain There would be thick cloud and probably poor visibility But this is not enough. Why not?
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“Explain.. With reference to the map”
Strong winds – close isobars Head winds – wind direction SW Low temperatures – mP air mass Heavy rain – occluded front Low cloud and poor visibility – occluded front 5 marks
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2014 EXAM QUESTION
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QUESTION Give reasons for the differences in the weather conditions between Ballycastle and Lerwick? (5 marks)
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MARKING SCHEME ANSWER It is much windier at Ballycastle than Lerwick because the isobars are much closer together in Ireland (1); it is raining heavily at Ballycastle because it is next to the cold front whereas Lerwick is not close to any fronts (1); the wind direction is north west at Ballycastle and south east at Lerwick because the wind goes anticlockwise around the low pressure and the isobars show the approximate direction (1);
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the cloud cover is 8 oktas at Ballycastle because it is so close to the cold front where there is likely to be cumulonimbus cloud whereas Lerwick is not near any fronts so is less likely to have cloud (1); the temperature is warmer at Ballycastle as it is still in the warm sector whereas Lerwick is not (1); the weather is mostly worse in Ballycastle than Lerwick as it is closer to a depression (1). It is warmer in Ballycastle because the clouds trap the heat whereas it is colder in Lerwick because there are no clouds (1)
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LET’S TRY THE 2014 N5 EXAM PAPER
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