1.1 Hazardous Earth Flashcards
how does the world’s climate system function, why does it change and how can this be hazardous for people?
how does climate vary with latitude?
with distance from the equator:
temps decrease
range of temps increase
precipitation fluctuates
why does temp decrease w distance from the equator?
in areas closer to the poles, incoming solar radiation has a thicker atmosphere to travel through due to the curvature of the Earth. the sun is also at a lower angle in the sky, so solar radiation is spread across a larger area.
name the three global circulatory cells.
hadley cell; ferrel cell; polar cell
describe how the global circulation system works
warm air at Equator rises and moves away; as it cools, it descends at the tropics, creating the hadley cell
cold air at the poles descends; then moves away towards the mid latitudes, creating the polar cell
cold air from poles meets warm air from tropics in the mid latitudes, creating the ferrel cell
what is atmospheric pressure
the weight of the air and the force it exerts on the ground
why do areas of high pressure have low precipitation?
cooled air descends, exerting more pressure on ground and resulting in dry, stable conditions
why do areas of low pressure have high precipitation?
warmed air is unstable and rises, exerting less pressure on ground; as air rises, it cools and cannot hold as much water vapour, resulting in condensation, cloud formation, and precipitation
explain how ocean currents redistribute heat.
surface ocean currents are driven by wind across the top of the water, whereas deep ocean currents are driven by water sinking and rising bc of temp changes
(extra e.g. : cold water from arctic sinks, drawing in warmer water from south)
describe how volcanic activity can affect climate.
they produce ash and sulphur dioxide gas; if these rise high enough, they’ll spread around the Earth’s stratosphere; this blanket will stop some sunlight reaching the Earth’s surface and instead will reflect it back into space; this cools the planet and the average temperature
e.g.1815 eruption of Tambura - in 1816, temps were so cold that 200,000 people died in Europe dur to harvest fail
describe how variation in solar output can affect climate.
black spots on the surface of the sun called sunspots disappear and reappear at different times; lots of sunspots mean more solar energy is being fired out, causing temp increases; less cause temp decreases
e.g. the cooler period known as the Little Ice Age may have been caused by sunspot activity
describe how orbital changes (milankovitch cycles) can affect climate.
over very long periods of time, the Earth’s orbit changes (known as Milankovitch cycles): it is sometime is more circular or more elliptic; sometimes the axis is more upright, or more on the side; sometimes the axis wobbles. these alter the amount of sunlight the Earth receives and where sunlight falls
e.g. these changes over tens of thousands of years would be enough to start or end an ice age
describe how asteroid collisions can affect climate.
every once in a while, an asteroid comes in contact w Earth; these can release huge quantities of vaporised material into the atmosphere, blocking the sun and causing a potential temp. drop of 5-6 degrees - initial ‘impact winter’; can also cause forest fires due to large amounts of CO2 released
e.g. asteroid collision theory considered to account for the extinction of the dinosaurs 65 million years ago.
how can historical sources be used for evidence for natural climate change?
personal diaries e.g. Anglo Saxon chronicles record years of droughts and heavy rainfall
paintings e.g. Painting of River Thames, 1963, during the Little Ice Age
religious records
how can tree rings be used for evidence for natural climate change?
every ring represents a year of growth; wider rings suggest the year was wetter and/or warmer; thinner rings suggest the opposite; black marks = scars from forest fires - suggest year was warmer and/or drier
how can ice cores be used for evidence for natural climate change?
a drill extracts an ice core; bubbles in ice trap ancient atmosphere - ghg content can be measured for particular years, allowing us to model past climate