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S1 Weather and Climate Notes Weather and Climate Climate: the average weather conditions for an area Weather: the state of the atmosphere at any given time Factors Affecting Climate Altitude: temperature will decrease with increasing height. For every 100 metres climbed, temperature will drop by 0.6° C. Aspect: this is the direction a slope faces. A south facing slope will be warmer than a slope facing north. In the northern hemisphere, a south facing slope faces towards the sun. Distance from the Sea: sea breezes cool the land down in summer and warm it up in winter. Coastal areas tend to have slightly cooler summers and slightly warmer winters. In land areas are the opposite. Latitude: Latitude is the distance an area is from the equator ( 0° latitude.) The closer an area is to the equator, the warmer it is. As you move further away from the equator, it becomes cooler. Ocean Currents: cold ocean currents cool the sea and coastal area and warm ocean currents warm the sea and coastal areas. The Gulf Stream bathes Western Scotland with warmer water – palm trees grow on some of Scotland’s coastal towns e.g Plockton and Largs. Rainshadow: the west coast of Scotland receives more precipitation than the east coast. Moist air is carried by the SW prevailing winds and causes rain to fall on the west coast. The air is forced to rise over the mountains where it cools and produces more rain. The air then warmed as it descends in the east coast. Warmer air produces less rainfall Climate graphs Temperature: drawn as a line graph Precipitation: this includes all forms of moisture that fall (rain, snow, sleet and hail). Precipitation is always drawn as a drawn as a bar graph. Temperature range: the difference between the highest and lowest temperature of the year Annual rainfall: add all the rainfall readings for every month of the year together. This gives you the total amount of rain that has fallen over the year. World Climatic Patterns Brasilia: found at 16°S of equator and at approximately 1000m asl. It has warm temperatures all year round, low temperature range and high annual rainfall. La Paz: found at 16°S of the equator and at approximately 3800 m asl. La Paz has average monthly temperatures of about 10°C with a very low temperature range. Precipitation is less than Brasilia. It has lower temperatures because it is found at a higher altitude. Himalayas: climate very cold and treacherous. Mountains affect weather in surrounding areas Gobi Desert: found in NW China and Mongolia. Very dry as a result of Mt Everest. It is a rainshadow desert. The Gobi Desert is a cold desert. Bangladesh: experiences floods as a result of snow melt from the Himalayas Weather Elements and Instruments Anemometer – measures wind speed in knots/kmph/mph/beaufort scale. Anemometers are located in a high position so that accurate wind speed readings are recorded. Cloud Cover – measured by the eye. Sky is divided into eighths and the unit of measurement is oktas. Rain Gauge – measures the precipitation in mm. It is partially buried in the ground to prevent it being knocked over. Stevenson Screen – houses the max and min thermometers and the wet and dry bulb thermometers. It is painted white to reflect the sun, has a sloping roof, slatted sides to allow air to circulate, 1 m above the ground and made of wood (poor conductor of heat). Sunshine recorder – can also be called a heliograph. Records the hours of sunshine in one day Thermometers – the maximum thermometer measures the highest temperature of the day and contains mercury. The minimum thermometer contains alcohol and record the lowest temperature of the day. The unit of measurement is °C Wind Vane – measures the direction of the wind in compass points. A northerly wind blows from the north and brings colder temperatures. A southerly wind blows form the south and brings warmer temperatures. Prevailing Wind: the wind that blows most often. In the UK this comes from the SW. Pressure Systems Isobar: a line that joins areas of equal air pressure Synoptic Chart: a map that shows isobars and fronts Cold front: shown as triangles on a synoptic chart, this marks the head of warm air. Heavy rain will fall along a cold front Warm front: shown as semi-circles on a synoptic chart, this marks the head of warm air. Prolonged rain will fall along a warm front Low pressure: isobars tend to be close together and fronts will be found. It brings changeable weather and wind blow in an anticlockwise direction High pressure: isobars tend to be far apart and no fronts are found. It brings settled, dry, calm weather that can last for a few days. Winds blow in a clockwise direction. Weather Symbols and Forecasting Weather Forecasting: weather data is collected by satellites, radar, radiosonde balloons, aircraft and weather ships. The data is sent to the Met Office where it is analysed and synoptic charts are drawn. BBC Weather Symbols: all elements are represented by a weather symbol Weather and People: weather can affect people in many ways e,g snow can affect travel, cause school and busineses to close, cut-off remote settlements, increase accident and casualty figures, increase profits for energy providers and see an increase in sales of sledges and warm clothing.