Weather and Climate Flashcards
Define “Weather”.
The condition of the atmosphere at a particular place and time.
Define “Climate”.
The average condition of the atmosphere of a specific place over a long period of time, usually over 30 years.
Explain how latitude affects temperature.
Latitude is the distance of any point on the earth measured north or south from the equator.
At lower latitudes, the sun’s rays hit the earth’s surface at a higher angle of incidence, causing the heat to be concentrated on a small area, resulting in higher temperatures.
At higher latitudes, the sun’s rays hit the earth’s surface at a lower angle of incidence, causing the heat to be spread out over a larger area, resulting in lower temperatures.
Explain why places at higher altitudes have lower temperatures.
The atmosphere is mostly heated by the earth’s surface. The higher up you are, the further you are from the surface of the earth that is heated by the sun. Therefore, temperature decreases with increasing altitude
Longwave radiation that is emitted by the earth is absorbed by greenhouse gases such as Co2 in the atmosphere, trapping the heat and warming the earth.
Air is less dense at higher altitudes. Dense air is able to absorb more heat from longwave radiation from the earths surface , resulting in higher temperatures. Less dense air has less ability to absorb heat, causing these lower temperatures.
Explain the maritime effect.
Maritime effect is the effect that large ocean bodies have on the climate of coastal areas, resulting in a lower annual temperature range.
During summer, the air over the sea is cooler than the air over the land, as the land heats up faster than the sea. The cooler air over the sea helps to lower the temperature of the area, resulting in cooler summers.
During winter, the air over the sea is higher than the air over the land, as the land cools down faster than the sea. The warmer air over the sea helps increase the temperature of the area, resulting in warmer winters.
Explain why inland areas have a higher annual temperature range.
Inland areas have a higher annual temperature range due to the continental effect.
During summer, the land heats up quickly, while during winter, the land cools down quickly. As a result, inland areas experience hotter summers and colder winters, leading to a higher annual temperature range.
Explain why there is a larger daily temperature range in the desert.
Deserts lack cloud cover.
In the day, all of the sun’s energy is thus able to reach the earth’s surface, heating it up quickly and causing the temperature to increase.
At night, most of the heat radiated from the earth’s surface escapes into the atmosphere, causing temperatures to drop.
Explain why places with cloud cover have a lower daily temperature range.
In the day, the clouds reflect a large portion of the sun’s energy back to space, keeping the earth’s surface cool. At the same time, the clouds absorbs some of the heat radiated from the earth’s surface, lowering the temperature.
At night, the clouds absorbs some of the heat radiated from the earth’s surface, preventing them from escaping into space, keeping the earth warmer.
Explain the factors affecting relative humidity.
- Temperature.
Higher temperatures can hold more water vapour. Given the same amount of water vapour, places with higher temperature will therefore have a lower relative humidity compared to a place with lower temperature.
Higher temperatures result in more evaporation -> more water vapour -> higher relative humidity.
- Amount of water vapour
Coastal areas or places near water bodies have higher chances of evaporation -> more water vapour -> higher relative humidity.
More trees -> more transpiration -> higher relative humidity.
Explain how clouds form.
- Evaporation from water bodies and transpiration from trees , lead to water vapour in the atmosphere.
2, When the water vapour cools at dew point temperature, condensation takes place to form water droplets. - The water droplets merge and become larger to form clouds.
Explain the formation of relief rain.
- Warm, moist air from the sea is forced to rise due to the mountains.
- Air cools as it rises. When dew point temperature is reached, condensation occurs and cloud form. When the water droplets are large and heavy enough, rain falls on the windward side.
- By the time air moves to leeward side, the air is dry and there is no rain fall.
Explain the formation of convectional rain.
- Convectional rain occurs when the earth’s surface is heated intensely. As the sun’s energy heats up the earth’s surface, the warm surface heats the air around it.
- The air becomes unstable, causing it to expand and rise.
- As the air rises, its temperature begins to drop. When the rising air cools to dew point temperature, condensation occurs and clouds are formed.
- When the water droplets in the clouds become large and heavy enough, they fall to the ground as rain.
Define ‘air pressure’.
Air pressure is the force on an unit area of the earth’s surface by the weight of a column of air above it.
Explain how wind is formed.
When there is a difference in temperature and thus a difference in air pressure, the air moves from an area of high pressure to an area of low pressure, forming wind.
Explain the formation of land breeze.
- At night, the land cools down faster than the sea. This results in the land having a lower temperature than the sea.
- The land thus has a higher air pressure compared to the sea.
- As winds blow from an area of high pressure to low pressure, the winds blow from the land to the sea, forming land breeze.
Explain how the sea breeze helps moderate temperatures during the day.
- In the day, the land heats up faster than the sea. This results in the land having a higher temperature than the sea.
- The land thus has a lower air pressure compared to the sea.
- As winds blow from an area of high pressure to low pressure, the winds blow from the sea to the land, forming sea breeze and lowering the temperature of the coastal area.
Explain the coriolis effect.
The coriolis effect is the force produced by the earth’s rotation.
Winds deflect right in the northern hemisphere and left in the southern hemisphere.
The coriolis effect is strongest at the poles but is not felt at the equator.