paper 2 - the atmosphere Flashcards
atmosphere of earth today
78% nitrogen
21% oxygen
1% other gases
early earth and how carbon dioxide levels decreased
volcanoes released natural gases such as carbon dioxide. methane, ammonia and water vapour which formed the atmosphere
earth cooled and water vapour condensed forming the oceans
some of the carbon dioxide dissolved in the oceans to form a weak acid. this reacted with minerals in the sea to form precipitates. over time this formed sediments of carbonate rock on the sea bed
some of the carbon dioxide was used to make shells. when these died they formed the sedimentary rock limestone which also removed carbon dioxide from the atmosphere
early earth atmosphere
98% carbon dioxide
how oxygen levels increased
photosynthetic algae evolved
photosynthesis produced oxygen which entered the atmosphere
over the following billion years plants evolved. this increased the amount of oxygen in the atmosphere .
at some point the level of oxygen reached the point where animals could evolve
fossil fuels
formed over millions of years
non renewable so they will eventually run out
all contain trapped carbon
coal
is formed from the remains of trees
if these die in marshy wetlands then they dont decompose
this can be due to a lack of oxygen or acidic conditions
these both prevent bacteria from carrying out decomposition
over time the plant remains are covered with sediment and compressed
high temp and pressure creates coal
crude oil
formed from plankton
when these die they settle in mud on the sea bed
if oxygen is not present they do not decompose
over time they are compressed by sediment
heat and pressure convert them into crude oil
natural gas
mainly methane
often found near deposits of oil as it is formed by plankton similarly to oil
types of greenhouse gases
water vapour
carbon dioxide
methane
what greenhouse gases do in the atmosphere
energy from the sun travels to the earth as short wavelengths radiation
some of the shortlength radiation simply reflects back into space but most of it passes easily through the atmosphere
that is because short wavelength radiation doesnt interact strongly with the gas molecules in the atmosphere
the energy of the radiation is now absorbed when it reaches the surface of the earth
the surface of the earth now radiates the energy as long wave radiation
some of the long wave radiation interacts with the greenhouse gas molecules in the atmosphere - the energy is absorbed
because the energy is trapped in the atmosphere, this causes the temperature of the atmosphere to increase
how levels of carbon dioxide are increasing
burning fossil fuels
normally carbon dioxide is absorbed by trees however because of deforestation and the burning of trees , more carbon dioxide is being released than absorbed
how methane levels are increasing
released in agriculture
released when cattle pass wind
how rising temperatures effect earth
increases melting of the polar ice caps which will increase sea levels
high sea levels leads to flooding in low land
more severe weather
change the distribution of animals and insect borne diseases
carbon foot
the total amount of carbon dioxide and other greenhouse gases emitted over the full life cycle of a product, service or an event
ways to reduce carbon dioxide emissions
insulating homes or turning down heating
using public transport as they release less carbon dioxide per passenger
switch to renewable sources of electricity
reduce electricity use at home