Basic Geography/Climate/Climate Elements
Temperature is the degree of hotness or coldness of the atmosphere on some chosen scale. It is commonly measured in Celsius or Fahrenheit. Temperature is a very important factor in determining the weather, because it influences other elements of the weather.
Temperature may be affected by:
- Sea Proximity and Temperature
- Ocean Currents
The amount of sunshine at a certain place can influence its temperature. The amount of sunshine can be measured in sunshine hours. That is worked out by the number of hours of daylight and how many of these are cloud free. Sunshine is variable due to daylight hours as during the night there is no sunshine as the Earth is pointing away from the sun at the given spot. Also due to the Earth's tilt some times of the year have more sunshine (summer) and some less (winter).
Latitude is the distance of a location from the equator. The hottest temperatures on Earth are found near the equator. This is because the sun shines directly on it for more hours during the year than anywhere else. As you move further away from the equator towards the poles, less sun is received during the year and the temperature become colder.
Altitude is the height you are above sea level. The higher up you are the lower the temperature will be. This is because air that is higher up is less dense than it is at lower altitudes and air temperature depends on its density. As a general rule for every 1,000m higher you go the temperature will drop by 6.5 °C.
Aspect is the direction in which you are facing. So if you are facing towards the equator then the temperature will be warmer than facing away. Therefore in the Northern Hemisphere if you wanted to lie in the sun on a hillside you would do so on the south facing slope (if you were in the Southern Hemisphere it would be the North Facing Slope).
Sea Proximity and Temperature
Sea temperature changes slower than land temperature. If the temperature on land drops then the area next to the sea will be kept warmer for longer than areas inland. Islands therefore have a less dramatic climate than continents. Different seas have different temperatures therefore allowing one side of an island to be a different temperature to the other side.
Currents are driven by the prevailing winds passing over the surface of the ocean. Therefore winds blowing from tropical areas bring warm currents and vice versa.
Humidity is the level of water in the air, the more water vapour in the air the higher the humidity. If the humidity level exceeds the amount of water air can hold condensation occurs forming dew if it's warm or frost if it's cold. When air is at a high altitude and has a high humidity then clouds start to form. Humidity varies with temperature. Warmer air can hold more moisture. Humidity is measured in percentages on the scale of air's ability to hold moisture. Therefore condensation occurs at 100% humidity for a given temperature thus reducing the humidity again.
Precipitation is the term given to moisture that falls from the air to the ground. Precipitation can be snow, hail, sleet, drizzle, fog, mist and rain. The water cycle drives the water from the oceans/seas on-shore where it falls as precipitation and then flows via rivers back in to the sea.
Types of Rainfall
- Convectional Rainfall
This is where a water surface is heated by the sun, e.g. the sea. The air above the sea then becomes heated making the air less dense so it rises and cools. As we know cooler air can not hold as much water vapour as warm air therefore when the rising air becomes too cold to hold the moisture the condensation occurs giving us clouds. Once there is too much water in the cloud for the air to support gravity forces the water to be released in what we know as rain.
- Frontal Rainfall
When two air masses meet where one is warmer than the other, the warmer air is forced to rise over the colder air. As this warm air rises it cools and forms clouds just like the air in convectional rainfall.
- Relief Rainfall
Wind bringing moist air from the seashore starts to rise up a hillside. As this air rises the air passes its Dew Point, the point at which condensation occurs, and the vapour forms clouds. The water vapour then falls as precipitation on top of the hill or on the other side.
Clouds are split into different groups depending on their height, shape and size. The most common terms are:
- Cirrus - Wispy, white clouds found at high altitudes
- Cumulus - Fluffy or heaped white clouds at relatively low altitudes
- Stratus - Low altitude layered cloud very rarely bringing precipitation
- Nimbus - Rain Clouds
- Cirro - High Altitude Clouds
- Alto - Medium Altitude cloud
The above terms are put together to form names of certain clouds:
- Cumulonimbus - Very large clouds bringing heavy rain, notice how the name comes from cumulus and nimbus above.
Air Pressure and Wind
Air pressure is simply the weight of the air above the Earth. Low Pressure is when air is warmer and therefore lighter. High pressure is colder air becoming heavier.
In meteorology pressure is charted on maps with isobars. The higher the number the higher the pressure.
Wind is simply the movement of air from high pressure to low pressure. The speed of the wind is determined by the difference between the high and low pressure. The greater the difference the faster the wind speed. Also the closer the isobars are on a weather chart the stronger the winds.
The wind brings with it the temperature of the area it is coming from, therefore a high pressure in a warm region will make the temperature in the low pressure area higher.
Wind-chill is the effect of the wind making it feel colder than it actually is. As the wind speed increases air is moving more quickly and therefore removes warm air therefore making it seem colder than the actual temperature.