Weather, climate and natural vegetation revision Flashcards
(41 cards)
Weather
The current conditions of the atmosphere
Climate
The average weather conditions
Anemometer
(wind speed)
An anemometer is used to measure wind speed.
* When there is wind the cups rotate, The stronger the wind the faster the rotation.
* The number of rotations is recorded on a meter to give the speed in kmph.
* An anemometer should be placed well away from buildings or trees that may interfere with the free movement of air – buildings may channel air through narrow passages between two buildings or decrease the flow of air by blocking its path.
* Winds are shown by arrows on a weather map – the shaft of the arrow shows wind direction and the feathers on the arrow indicate wind speed.
Wind vane
(wind direction)
- A wind vane is used to measure wind direction.
- A wind vane has the points of the compass (i.e. NESW) fixed and sited so that they point in the correct directions.
- Winds are shown by arrows on a weather map – the shaft of the arrow shows wind direction and the feathers on the arrow indicate wind speed.
Barometer (air
pressure)
- Pressure is the amount of air pressing down on the earth’s surface.
- The unit of measurement for air pressure is millibars (MB)
- The mean average pressure at sea level is said to be 1013 mb, so pressures below these are usually said to be low and pressures above this high.
- Low air pressure is associated with unsettled conditions (as warm air is rising off the surface of the earth – which later cools and condenses forming clouds and potentially rain).
- High pressure is associated with settled/clear conditions as cool air is descending and warming up.
Lines are drawn through points where pressure is the same – these lines are called isobars.
Wet-dry
thermometer
/hygrometer
(relative
humidity)
Humidity is the amount of water vapour in a given volume of air.
* Water vapour is an invisible gas. The amount of water vapour that any air can hold depends on the temperature – warm air can hold more water vapour than cold air.
When air is cooled the amount of water vapour that it can hold reduces. If the air is cool sufficiently it reaches the maximum amount of moisture that is can hold – this is called dew point. Any further cooling will result in condensation – a process by which excess water vapour turns into water droplets or ice depending on the temperature of the air.
The relative humidity of the air is expressed as a percentage. When air is saturated the relative humidity is 100%.
If the air is not saturated water will evaporate from the muslin.
* Evaporation causes cooling of the bulb which causes the mercury to contract and register a lower temperature.
* The temperature of the wet bulb minus the temperature of the dry bulb temperature gives the depression of the wet bulb. The larger this is, the lower the relative humidity will be.
Maximum-
minimum thermometer
(temperature)
Show the highest and lowest temperatures reached.
The instrument is read at eye level from the lower end of each index.
* It is reset by using a magnet to draw each index back to the mercury.
* Lines can be drawn on a map connecting areas of equal temperature – these lines are called isotherms.
Rain gauge
(precipitation)
- Amounts of precipitation e.g. rain, snow, sleet or hail are measured using a range gauge.
*The gauge is sunk into the ground so that the top of the funnel is about 30cm above ground level. This is to prevent water splashing on the ground and then entering the funnel. - Rainfall collects in the jar and this is usually emptied every 24
hours.
Sunshine
recorder
(sunshine)
The number of hours and minutes of sunshine received at a place can be measured on a sunshine recorder.
* A strip of special card, divided into hours and minutes is placed below the sphere.
* When the sun shines, the sphere focuses the sun’s rays on the card.
* As the sun moves, the rays burn a trace on the card. At the end of the day the card is removed and replaced.
* The length of the trace represents the amount of sunshine the area received.
The main clouds that you need to be aware of are:
Stratus: These are layered clouds that are low, grey and shapeless and usually are like a blanket of cloud over an area. They can bring some drizzle and rain.
Cumulus: These are clouds that move quite quickly. They are white and fluffy and look like cotton wool. They can bring rain showers – especially when the base is grey.
Cumulonimbus: These are much deeper clouds that climb high into the atmosphere. They often contain a lot of heavy rain and are associated with thunder and lightning storms.
Cirrus: These are very high clouds that are wispy and made up from ice crystals.
Stevenson screen adaptation
Made of wood. It is a bad conductor of heat.
Painted white. To reflect sun rays.
Has slates/louvres. To allow free circulation of air.
Has a double roof. For insulation.
Placed 1.21m above the ground too avoid flooding
The door of the screen faces South in the Southern hemisphere and North in the Northern hemisphere.
In a fenced area to avoid human contact
On grass so that the ground absorbs heat
Cloud cover
Cloud cover is observed (not measured) in units called oktas. Each okta represents one-eighth of the sky covered by clouds.
Synoptic chart
A map that summarises atmospheric conditions
Factors influencing climate
Latitude
Prevailing wind
Distance from sea
Relief
Ocean currents
Presenting climate data
Bars: Rainfall
Line: Temperature
Relief rainfall
- Relief rainfall occurs when air has been blown over the sea and is then forced up over an area
of high land. - This causes the air to cool and the moisture in the air condenses and rain falls.
Frontal rainfall
- Frontal rainfall occurs when warm air is forced to rise over cold air.
- The moisture in the warm air condenses as it cools which causes clouds and rain.
Convectional rainforests
- Occurs mostly in tropics where it is hot.
- When air is hot is rises and cools and condenses forming rain.
- If the air is hot enough, it rises very quickly and can cause thunderstorms.
Tropical rainforest: Location:
- Along the equator and between the tropics
- Main areas are northern South America (e.g. Amazon), Central Africa (e.g. Congo) and South
East Asia.
Tropical rainforest climate:
- Consistently high temperatures throughout the year – an average of about 25°C
- Annual temperature range: less than 5°C
Rainfall – amount exceeds 2000mm - Rainfall– seasonal distribution: fairly evenly distributed throughout the year
- Wind: low
Cloud: heavy
Humidity: high - Pressure: low
- Little seasonal variation
Rainforests typically receive convectional rainfall:
Stage 1.
The sun heats the ground, and warm air rises.
Stage 2.
As the air rises, it cools, and water vapour condenses to form clouds.
Stage 3.
When the condensation point is reached, large cumulonimbus clouds are formed.
Stage 4.
Heavy rainstorms occur. These usually include thunder and lightning due to the electrical charge created by unstable conditions.
Convectional rainfall is widespread in areas where the ground is heated by the hot sun,
such as the Tropics. This is why areas, such as the Amazon Rainforest, experience heavy
rainfall most afternoons.
Layers of rainforest
Emergent trees
Canopy
Under canopy
Shrub layer/ Forest floor
Nutrients cycle
Nutrients are the goodness that plants need to grow.
Most nutrients in rainforests are not held in the soil, but instead in the biomass.
When plants and animals die they decompose on the forest floor.
The mixing of dead organic material and weathered rock in the soil leads to the development of nutrients.
Nutrients are then taken up by shallow plant roots, providing plants with the goodness they need to grow.
Plant adaptations of rainforest
*Lianas - these are woody vines that have roots in the ground but climb up the trees to reach the sunlight. Their leaves and flowers grow in the canopy.
*Tree trunks - these are tall and thin to allow trees to reach the sunlight. The bark on these trees is smooth to allow water to flow down to the roots easily.
*Drip tips - plants have leaves with pointy tips. This allows water to run off the leaves quickly without damaging or breaking them.
*Buttress roots - large roots have ridges which create a large surface area that help to support large trees.
*Epiphytes - these are plants which live on the branches of trees high up in the canopy. They get their nutrients from the air and water, not from the soil.