Turn Down the Heat: State of the Climate (and Australia) February 2014 Damien Lockie.

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Turn Down the Heat: State of the Climate (and Australia) February 2014 Damien Lockie

State of the Climate ( AR5, WG1, Synthesis Report) AR5 IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, Impact – Observed changes in climate system “Warming of the climate system is unequivocal, and since the 1950s, many of the observed changes are unprecedented over decades to millennia. The atmosphere and ocean have warmed, the amounts of snow and ice have diminished, sea level has risen, and the concentrations of greenhouse gases have increased.” “Each of the last three decades has been successively warmer at the Earth’s surface than any preceding decade since 1850… In the Northern Hemisphere, 1983–2012 was likely the warmest 30-year period of the last 1400 years (medium confidence).” “The globally averaged combined land and ocean surface temperature data as calculated by a linear trend, show a warming of 0.85 [0.65 to 1.06] °C, over the period 1880 to 2012.”

Figure SPM.1

State of the Climate ( AR5, WG1, Synthesis Report) AR5 IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, Impact - Atmosphere “Changes in many extreme weather and climate events have been observed since about 1950… It is very likely that the number of cold days and nights has decreased and the number of warm days and nights has increased on the global scale. It is likely that the frequency of heat waves has increased in large parts of Europe, Asia and Australia. There are likely more land regions where the number of heavy precipitation events has increased than where it has decreased. The frequency or intensity of heavy precipitation events has likely increased in North America and Europe. In other continents, confidence in changes in heavy precipitation events is at most medium.”

State of the Climate ( AR5, WG1, Synthesis Report) AR5 IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, Impact – Ocean and Sea-level “Ocean warming dominates the increase in energy stored in the climate system, accounting for more than 90% of the energy accumulated between 1971 and 2010 (high confidence). It is virtually certain that the upper ocean (0−700 m) warmed from 1971 to 2010 … and it likely warmed between the 1870s and 1971.” “The rate of sea level rise since the mid-19th century has been larger than the mean rate during the previous two millennia (high confidence). Over the period 1901 to 2010, global mean sea level rose by 0.19 [0.17 to 0.21] m.” Impact - Cryosphere “Over the last two decades, the Greenland and Antarctic ice sheets have been losing mass, glaciers have continued to shrink almost worldwide, and Arctic sea ice and Northern Hemisphere spring snow cover have continued to decrease in extent (high confidence).”

State of the Climate ( AR5, WG1, Synthesis Report) AR5 IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, Impact – Greenhouse gases “The atmospheric concentrations of carbon dioxide, methane, and nitrous oxide have increased to levels unprecedented in at least the last 800,000 years. Carbon dioxide concentrations have increased by 40% since pre-industrial times, primarily from fossil fuel emissions and secondarily from net land use change emissions. The ocean has absorbed about 30% of the emitted anthropogenic carbon dioxide, causing ocean acidification.” “The atmospheric concentrations of the greenhouse gases carbon dioxide (CO 2 ), methane (CH 4 ), and nitrous oxide (N 2 O) have all increased since 1750 due to human activity. In 2011 the concentrations of these greenhouse gases were 391 ppm, 1803 ppb, and 324 ppb, and exceeded the pre-industrial levels by about 40%, 150%, and 20%, respectively.”

Figure SPM.4

State of the Climate ( AR5, WG1, Synthesis Report) AR5 IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, Impact – Detection and attribution of climate change “Human influence has been detected in warming of the atmosphere and the ocean, in changes in the global water cycle, in reductions in snow and ice, in global mean sea level rise, and in changes in some climate extremes... This evidence for human influence has grown since AR4. It is extremely likely that human influence has been the dominant cause of the observed warming since the mid-20th century.” “There has been further strengthening of the evidence for human influence on temperature extremes since the SREX. It is now very likely that human influence has contributed to observed global scale changes in the frequency and intensity of daily temperature extremes since the mid-20th century, and likely that human influence has more than doubled the probability of occurrence of heat waves in some locations.”

AUSTRALIA’S GHG PERFORMANCE 1990 GHG emissions = 546,327,620 t CO 2 -e 2000 GHG emissions = 552,680,480 t CO 2 -e 2007 GHG emissions = 597,156,550 t CO 2 -e 2008 GHG emissions = 553 Mt CO 2 -e 2012 GHG emissions = Mt CO 2 -e Estimated annual GHG emissions = ~ 566 Mt CO 2 -e TOTAL = 104% of 1990 emissions = 1.5% of global GHG AUSTRALIA’S AA = 2,990, AAUs Department of Climate Change Tracking to the Kyoto Target (2007) National Inventory Report 2007 (2009) Tracking to Kyoto and 2020 (2009) Department of the Environment Australian National Greenhouse Accounts: Quarterly Update of Australia’s National Greenhouse Gas Inventory, September Quarter 2013

State of the Climate ( AR5, WG1, Synthesis Report) AR5 IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, Projections “Continued emissions of greenhouse gases will cause further warming and changes in all components of the climate system. Limiting climate change will require substantial and sustained reductions of greenhouse gas emissions.” “Global surface temperature change for the end of the 21st century is likely to exceed 1.5°C relative to 1850 to 1900 for all RCP scenarios except RCP2.6. It is likely to exceed 2°C for RCP6.0 and RCP8.5, and more likely than not to exceed 2°C for RCP4.5… Warming will continue to exhibit interannual-to-decadal variability and will not be regionally uniform.” “ The global ocean will continue to warm during the 21st century. Heat will penetrate from the surface to the deep ocean and affect ocean circulation.” “Global mean sea level will continue to rise during the 21st century…”

Figure SPM.7

Figure SPM.9

State of the Climate ( AR5, WG1, Synthesis Report) AR5 IPCC, 2013: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, Projections, cont’d “Climate change will affect carbon cycle processes in a way that will exacerbate the increase of CO 2 in the atmosphere (high confidence). Further uptake of carbon by the ocean will increase ocean acidification.” “Ocean uptake of anthropogenic CO 2 will continue under all four RCPs through to 2100, with higher uptake for higher concentration pathways (very high confidence). The future evolution of the land carbon uptake is less certain.” “Cumulative emissions of CO 2 largely determine global mean surface warming by the late 21st century and beyond… Most aspects of climate change will persist for many centuries even if emissions of CO 2 are stopped. This represents a substantial multi- century climate change commitment created by past, present and future emissions of CO 2.”

Figure SPM.10

UN sources UN UNEP IPCC techange2013.org/ techange2013.org/ World Bank org org Climate- L.org Climate Change Gateway ent/site/climatechange /gateway ent/site/climatechange /gateway