guest post by Steve Easterbrook
(4) Most of the heat is going into the oceans
The oceans have a huge thermal mass compared to the atmosphere and land surface. They act as the planet’s heat storage and transportation system, as the ocean currents redistribute the heat. This is important because if we look at the global surface temperature as an indication of warming, we’re only getting some of the picture. The oceans act as a huge storage heater, and will continue to warm up the lower atmosphere (no matter what changes we make to the atmosphere in the future).
Note the relationship between this figure (which shows where the heat goes) and the figure from Part 2 that showed change in cumulative energy budget from different sources:
Both graphs show zettajoules accumulating over about the same period (1970-2011). But the graph from Part 1 has a cumulative total just short of 800 zettajoules by the end of the period, while today’s new graph shows the earth storing “only” about 300 zettajoules of this. Where did the remaining energy go? Because the earth’s temperature rose during this period, it also lost increasingly more energy back into space. When greenhouse gases trap heat, the earth’s temperature keeps rising until outgoing energy and incoming energy are in balance again.
You can download all of Climate Change 2013: The Physical Science Basis here. Click below to read any part of this series:
- The warming is unequivocal.
- Humans caused the majority of it.
- The warming is largely irreversible.
- Most of the heat is going into the oceans.
- Current rates of ocean acidification are unprecedented.
- We have to choose which future we want very soon.
- To stay below 2°C of warming, the world must become carbon negative.
- To stay below 2°C of warming, most fossil fuels must stay buried in the ground.
Climate Change 2013: The Physical Science Basis is also available chapter by chapter here:
- Observations: Atmosphere and Surface
- Observations: Ocean
- Observations: Cryosphere
- Information from Paleoclimate Archives
- Carbon and Other Biogeochemical Cycles
- Clouds and Aerosols
- Anthropogenic and Natural Radiative Forcing
- Evaluation of Climate Models
- Detection and Attribution of Climate Change: from Global to Regional
- Near-term Climate Change: Projections and Predictability
- Long-term Climate Change: Projections, Commitments and Irreversibility
- Sea Level Change
- Climate Phenomena and their Relevance for Future Regional Climate Change
- Annex I: Atlas of Global and Regional Climate Projections
- Annex II: Climate System Scenario Tables
- Annex III: Glossary
- Annex IV: Acronyms
- Annex V: Contributors to the WGI Fifth Assessment Report
- Annex VI: Expert Reviewers of the WGI Fifth Assessment Report