Weather Hazards and Climate Change Flashcards
What are the features of global atmospheric circulation?
-The transfer of heat from the Equator to the poles.
-There are there circulation cells - Hadley, Ferrel and Polar
-Jet streams impact on the movement of heat energy
-The spin of the Earth creates the Coriolis effect.
What is global atmospheric circulation?
The worldwide movement of air which transports heat from tropical to polar latitudes.
What is a hemisphere?
A half of the earth. The northern hemisphere is above the equator, th southern hemisphere is below it.
What is latitude?
The distance, north or south from the equator measured from 0 to 90 degrees North or South.
What is the troposphere?
The lowest layer of the atmosphere. It is thicker at the equator (~20km) than at the poles (~10km) in height.
What is a depression (in Geographical terms)?
A low pressure system that produces clouds, wind and rain.
What is an ocean current?
A continous directed movement of ocean water. The currents are made from forces acting on the water such as the wind, different temperatures and the Earthβs rotation.
What is the ITCZ?
The Inter Tropical Convergence Zone, where the two hemispheresβ Hadley cells meet.
What are trade winds?
A wind that blows steadily from the tropics towards the equator. In the northern hemisphere it is from the northeast and in the southern hemisphere it is from the southeast.
What are the characteristics of Hadley cells?
-They stretch from the equator to 30 degrees north and south.
-Warm trade winds blow towards the equator.
-At the equator, trade winds from each hemisphere meet. The warm air rises rapidly causing thunderstorms. An area of low pressure is formed in the ITCZ.
-The air at the top of the troposphere moves away from the equator where it becomes cooler and sinks. It warms and any moisture is evaporated around 30 degress north and south. This creates high pressure areas, with cloudless skies.
-On returning to the ground some of the air returns to the equatorial areas as trade winds, completing the circle.
What are the characteristics of Ferrel cells?
-Ferrel cells stretch from 30 degrees north and south to 60 degrees north and south.
-These winds collect moisture as they blow over oceans on the Earthβs surface.
-At about 60 degrees north and south they meet cold air from the poles.
-The warm air rises over the cold air as it is less dense. This produces low pressure at the surface causing depressions.
-Some of the air returns to the tropics and some is diverted to the poles as part of the polar cells.
-The cell has a motion to the right in the northern hemisphere and to the left in the southern hemisphere due to the spin of the Earth. This is called the Coriolis effect.
What are the characteristics of the polar cells?
Polar cells stretch from latitudes 60 degrees north and south to the poles. They:
-Have air that sinks over the poles producing high pressure.
-Have air that flows towards low pressure in the mid-latitudes, meeting air from the Ferrel cells.
What are jet streams?
In the upper atmosphere, winds blow around the Earth in a westerly direction. Within these winds there are bands of extremely fast-moving air known as jet streams. These jet streams can be hundreds of kilometres in width, but only 1000-2000 metres high. They are found at altitudes of about 10000 metres. The jet streams can be found in:
-The polar stream, going from 40 degrees to 60 degrees, in a westerly direction.
-The subtropical jet stream between 25 to 35 degrees in a westerly direction.
What are Milankovitch cycles?
The amount of heat the Earth receives from the sun is affected by orbit. Three cycles affect this - eccentricity, axial tilt and precession.
What is precession?
The Earthβs axis wobbles like a spinning top, taking around 26,000 years to complete a cycle. The motion is caused by the gravitational action of the sun and moon. This cycle can affect seasonality.
What is eccentricity?
The path of the Earth around the sun is eliptical. This shape can change to a circle. This is caused by the gravitational pull of other celestial bodies. One complete cycle lasts for about 100,000 years. It appears colder periods are when the orbit is more circular and warmer periods are when it is more eliptical.
What is axial tilt?
The earth is spinning on its own axis. The axis is not upright and takes an angle of between 22.1 degrees and 24.5 degrees. A complete cycle for this tilt takes about 41,000 years. A greater degree of tilt is associated with the world having a higher average temperature.
What is solar variation?
This is a change in the amount of heat energy coming from the sun. Sunspots on the surface of the sun can have an impact. Between 1645 and 1715 the Little Ice Age occured perhaps due to lower sunspot activity.
What is volcanism?
Large volcanic eruptions release ash and sulphur dioxide into the atmosphere, causing less solar rays to enter the Earthβs atmosphere, cooling the Earth. Sulphur dioxide reacts with water to make Sulphuric acid, which causes acid rain, damaging the environment.
How do ice cores prove climate change?
The polar regions have ice frozen for millions of years. Cores can be drilled into to measure the amount of CO2 in the atmosphere at the time it was formed. It can show how CO2 levels have changed.
How do pollen records prove climate change?
Pollen analysis shows which plants were dominant at a particular time due to climate. Each species has specific climatic requirements that influence their geographic distribution. Changes in the pollne found in levels of peat bog shows how climate changes over time.
How do tree rings prove climate change?
Trees develop rings each year, if the ring is narrow it shows a cooler, drier year, and thicker rings show hotter and more humid years.
How do historical sources prove climate change?
Cave paintings, diaires and documentary evidence can be used. For example, the fairs held on the river Thames when it froze. Since 1873, daily weather reports have been held. Parish records are a good source of climate data too.
How does the greenhouse effect work?
When fossil fuels are burned, greenhouse gases are released into the atmosphere, thickening it.
Heat energy from the sun beams down onto Earth, some of it passing through a blanket of gases in our atmosphere.
Some of the heat energy escapes back into space.
Greenhouse gases form a blanket around the Earth which traps heat energy in the atmosphere.
The energy which does not escape into space is reflected back into Earth.
The main greenhouse gases are carbon dioxide, methane and nitrous oxide.