C9 (the atmosphere) Flashcards
(54 cards)
describe the atmosphere of the Earth today:
- around 78% of the atmosphere is nitrogen
- around 21% is oxygen
- small proportions of other gases, such as carbon dioxide, water vapour, and noble gases (e.g. argon)
these gases have stayed pretty constant for around 200 million years.
why can scientists not be certain about the early atmosphere?
the Earth is around 4.6 billion years old, so it’s only a theory
what do scientists think about the first billion years of Earth?
- intense volcanic activity. these released the gases that formed the atmosphere (lots of carbon dioxide, water vapour)
- as the Earth cooled (couldn’t form oceans initially, as the temperatures were over 100 degrees celsius), the water vapour condensed to form the oceans
- Earth’s early atmosphere was mainly carbon dioxide, with very little oxygen (very much like the atmospheres of Mars and Venus today)
what gases did early volcanoes release, other than carbon dioxide and water vapour?
- nitrogen, which gradually built up in the atmosphere
- released small amounts of methane and ammonia
describe the overall early atmosphere of the Earth:
- mainly carbon dioxide
- small but increasing amounts of nitrogen
why have carbon dioxide levels decreased in the Earth’s atmosphere over time?
- the water vapour from volcanoes condensed to form oceans
- some of the carbon dioxide dissolved in the oceans to form a weak acid (carbonic acid)
- this reacted with minerals in the sea to form carbon precipitates, which over time formed sediments of carbonate rock on the sea bed
- plants and plankton photosynthesised, taking in CO2. animals then eat the plants, taking in the carbon. these die, get covered at the bottom of the ocean, and undergo huge pressures and heat, forming sedimentary rock, oil, and gas, trapping the carbon
how do we know what substance will be formed, depending on the type of organism being buried and the conditions involved?
- crude oil and natural gas: mainly from dead plankton
- coal: sedimentary rock from thick deposits of dead plant material
- limestone: sedimentary rock from the calcium carbonate from the shells and skeletons of marine organisms
where has oxygen come from since the Earth’s early atmosphere?
- around 2.7 billion years ago, photosynthetic algae first evolved in the oceans
- photosynthesis produced oxygen (and also absorbed more carbon dioxide) which entered the atmosphere
- over the following billion years, plants evolved, increasing the amount of oxygen in the atmosphere
- at some point the level of oxygen reached the point where animals could evolve
what was the first organism to produce oxygen?
cyanobacteria
describe fossil fuels:
- formed over millions of years
- non-renewable
- contain trapped carbon (part of the carbon dioxide taken in by photosynthesis)
how is coal formed?
FOSSIL FUEL
- from the remains of ferns and trees
- over time, the plant remains are covered with sediment and compressed
- high temperature and pressure creates coal
when may coal not be formed?
if the ferns/trees die in marshy wetlands. they don’t decompose, due to a lack of oxygen/acidic conditions, both preventing bacteria from carrying out decomposition.
how is crude oil formed?
FOSSIL FUEL
from plankton (tiny plants/animals found under the sea). when they die, they settle on the sea bed (apart from in anoxic conditions, when they’re unable to decompose). over time, they’re compressed by sediment, and heat and pressure convert them to crude oil.
what is natural gas?
FOSSIL FUEL
- mainly the hydrocarbon methane
- often found near deposits of oil, as it’s formed from plankton in a similar way to crude oil
describe the small proportions of the greenhouse gases in the modern day atmosphere:
water vapour: amount varies, changes depending on temperature
carbon dioxide: around 0.04%
methane: tiny amounts
what is the greenhouse effect?
the warming of the Earth caused by the greenhouse gases
describe the greenhouse effect:
- energy from the sun travels to Earth as short wavelength radiation (e.g. ultraviolet and visible light)
- some of the short wavelength radiation is absorbed and heats up the ground, but most of it is re-emitted/reflected back into the atmosphere, and into space, as longer wavelength radiation
- although some of this energy actually does reach space, most of it is absorbed by particles of gas in the atmosphere
- after a short delay, these re-emit the energy in random directions. some will be re-emitted towards space, and some towards the Earth
- most of the energy will collide with other gas particles before it leaves the atmosphere
- this process happens over and over again, meaning the heat energy stays close to Earth
describe the importance of the greenhouse effect:
keeps the temperature on Earth warm enough to support life.
why are the levels of carbon dioxide currently increasing?
- increasing as we burn fossil fuels (e.g. burning coal for electricity, petrol/diesel for cars, gas to heat our homes), which releases the locked up carbon as carbon dioxide
- rainforests are being destroyed through deforestation (usually burned) to provide land for grazing cattle, so they can’t absorb carbon dioxide through photosynthesis
- burning the forests also produces large amounts of carbon dioxide
why are the levels of methane currently increasing?
- released in agriculture (e.g. growing rice in flooded paddy fields, which generates methane emitting bacteria)
- released during farm animal (e.g. cows) digestion, which is then released into the atmosphere
- our release of waste releases methane as the waste is decomposed by microorganisms
what does it mean if the levels of methane and carbon dioxide in the atmosphere increase?
the temperature of the atmosphere is rising as more of the sun’s energy is being trapped by these greenhouse gases.
how is climate change measured?
by the changes in pattern of:
- temperature
- sunshine
- rainfall
- windspeed
how do we know that global warming is happening?
we have records going back hundreds of years, and we can see the steady increase
what are the some examples of climate change?
- climate change = the effect of global warming on the planet
- rising temperatures increases the melting of polar ice sheets and glaciers, increasing sea levels (water also expands at higher temperatures, volume increases)
- this could lead to more flooding of lowland areas, seasonal flooding, submersion of islands/coastal towns and coastal erosion
- climate change could lead to more severe weather (hurricanes)
- increasing temperatures could change the distribution of animals such as insects. may even change the distribution of insect-borne diseases (e.g. malaria)
- changes in amount, timing and distribution of rainfall (droughts)