water, carbon and life on earth Flashcards
role of water and carbon
- both w+c crucial in supporting life on earth
- in people carbon is stored in glucose and assists respiration
- in trees carbon content of woody matter is approx 50%
- through respiration and decomposition carbon is returned to the atmosphere in the form of co2
how do the water and carbon cycles interact in the atmosphere to influence climate
- atmosphere is an important store of both water and carbon
- all living organisms need water to survive
- carbon is essential for plant growth as well as an important greenhouse gas
what is an important link between the water and carbon cycle?
is the ability of water to absorb and transfer carbon dioxide
water and carbon mostly interact with eachother through rainwater and running water. what else?
- through el nino
- tropical rainforests
- weathering
how are water and carbon impacted upon by climate change?
increased co2 is warming the atmosphere this results in higher evaporation rates and a wetter atmosphere
what does co2 cause?
co2 causes around 20% of the earths greenhouse effect water vapour accounts for 50% and clouds 25% the rest is called be aerosoles
what happens when co2 concentrations rise?
air temperatures rise. the oceans warm up and more vapour evaporates into the atmosphere which amplifies greenhouse heating
what controls the temperature?
although co2 contributes less to the overall greenhouse effect than water vapour, scientists have found that it’s the co2 that controls the temp
what is there a lag time between?
there is a lag time between increased co2 and increased warming. for example the temp will increase by a further 0.6 because of the co2 in the atmosphere
how are the water and carbon cycles impacted upon by climate change.
- ice reflects radiation from sun so less heat absorbed by surface
- arctic sea ice is shrinking so less reflection and more absorption
- this warms water and further melts ice
- this affects the type and magnitude of water transfers between the land ocean and atmosphere
carbon cycle permafrost loop - negative feedback
higher temps have increased growing season for plants which means that more carbon can be absorbed from the atmosphere
phytoplankton
organisms which live in water
they release a chemical substance which may produce the formation of condensation and clouds over the ocean
marine phytoplankton positive feedback loop
less sunshine - reduction in phytoplankton - reducing cooling effect
marine phytoplankton negative feedback loop
warmer temps - increase in phytoplankton - increase in clouds - global cooling
political and economic implications of arctic sea ice
no arctic sea ice will affect trading routes, the exploitation of resources and the development of settlements