Difference between revisions of "Present global change"

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# [[Ocean Acidification|'''ocean acidification:''']] due to invasion of fossil fuel CO<sub>2</sub> into the ocean.
 
# [[Ocean Acidification|'''ocean acidification:''']] due to invasion of fossil fuel CO<sub>2</sub> into the ocean.
# [[Global warming|'''global warming:''']] how increasing the greenhouse effect interacts with other components of the Earth’s radiation balance and heat reservoirs.
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<!-- # [[Global warming|'''global warming:''']] how increasing the greenhouse effect interacts with other components of the Earth’s radiation balance and heat reservoirs. -->
# [[Global Dimming|'''global dimming:''']] the impact of sulphate aerosols in blocking the Sun's heat.
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<!-- # [[Global Dimming|'''global dimming:''']] the impact of sulphate aerosols in blocking the Sun's heat. -->
 
# [[Future Ocean Carbon Sink|'''future ocean C sink:''']] will any of the multiple ways in which the ocean is being changed make a large difference to how much CO<sub>2</sub> it absorbs?
 
# [[Future Ocean Carbon Sink|'''future ocean C sink:''']] will any of the multiple ways in which the ocean is being changed make a large difference to how much CO<sub>2</sub> it absorbs?
 
# [[Long-Term Legacy of Fossil Fuels|'''long-term CO<sub>2</sub>:''']] what legacy will our burning of fossil fuels leave behind for future generations, including our descendants living many thousands of years in the future?
 
# [[Long-Term Legacy of Fossil Fuels|'''long-term CO<sub>2</sub>:''']] what legacy will our burning of fossil fuels leave behind for future generations, including our descendants living many thousands of years in the future?

Latest revision as of 16:37, 24 August 2016

Human-caused rise in atmospheric CO2 (~100ppmv) set against the context of glacial-interglacial variations (~100 ppmv). This image is an original work created for Global Warming Art.
Rise in atmospheric CO2 as directly measured at Mauna Loa, Hawaii. This image is an original work created for Global Warming Art.

Response of the Earth System to Global Change

The JModels elucidate the natural cycling of nutrients and carbon in the oceans and the natural operation of the Earth’s radiation balance. They can also be used to examine some aspects of the operation of the perturbed Earth. Human activities are making large impacts on the ocean, and on the Earth’s radiation balance, and the carbon and radiation budget models in particular given an indication of the likely effects of some of these changes. Some of the changes that can be examined are:

  1. ocean acidification: due to invasion of fossil fuel CO2 into the ocean.
  2. future ocean C sink: will any of the multiple ways in which the ocean is being changed make a large difference to how much CO2 it absorbs?
  3. long-term CO2: what legacy will our burning of fossil fuels leave behind for future generations, including our descendants living many thousands of years in the future?