TFE.4, Figure 1 - The Earth’s energy budget from 1970 through 2011

TFE.4, Figure 1- The Earth’s energy budget from 1970 through 2011. (a) The cumulative energy inflow into the Earth system from changes in well-mixed and shortlived greenhouse gases, solar forcing, tropospheric aerosol forcing, volcanic forcing and changes in surface albedo due to land use change (all relative to 1860–1879) are shown by the coloured lines; these contributions are added to give the total energy inflow (black; contributions from black carbon on snow and contrails as well as contrail-induced cirrus are included but not shown separately). (b) The cumulative total energy inflow from (a, black) is balanced by the sum of the energy uptake of the Earth system (blue; energy absorbed in warming the ocean, the atmosphere and the land, as well as in the melting of ice) and an increase in outgoing radiation inferred from changes in the global mean surface temperature. The sum of these two terms is given for a climate feedback parameter α of 2.47, 1.23 and 0.82 W m–2 °C–1, corresponding to an equilibrium climate sensitivity of 1.5°C, 3.0°C and 4.5°C, respectively; 1.5°C to 4.5°C is assessed to be the likely range of equilibrium climate sensitivity. The energy budget would be closed for a particular value of a if the corresponding line coincided with the total energy inflow. For clarity, all uncertainties (shading) shown are likely ranges. {Box 12.2; Box 13.1, Figure 1}

Source: IPCC  Climate Change 2013: Technical Summary, p.67

Climate Change: 2013 IPCC Update

Box TS.1 - Treatment of Uncertainty

Figure TS.1 - Multiple complementary indicators of a changing global climate

Figure TS.2 - Change in surface temperature over 1901–2012

Figure TS.3 - Ice loss in Greenland and Antarctica

TFE.1, Figure 1 - Changes in sea surface salinity

TFE.1, Figure 2 - Changes in precipitation over 20th century

TFE.1, Figure 3 - Projected changes in precipitation, 21st century

TFE.2, Figure 1 - Comparison of observed trends with previous projections.

TFE.2, Figure 2 - Compilation of paleo sea level data

Figure TS.4 - Annual anthropogenic CO2 emissions

Figure TS.5 - Atmospheric composition.

Figure TS.6 - Radiative forcing and Effective radiative forcing of climate change during the Industrial Era

Figure TS.7 - Radiative forcing of climate change during the Industrial Era shown by emitted components from 1750 to 2011

Figure TS.8 - (Upper) Global anthropogenic present-day emissions weighted by the Global Warming Potential and the Global Temperature change Potential

Figure TS.9 - Global temperatures with and without anthropogenic forcing

Box TS.3, Figure 1 - Trends in temperature changes for the last few decades.

TFE.3, Figure 1 - Observed globally and annually averaged CO2 concentrations in parts per million since 1950 compared with projections from the previous IPCC assessments. Observed global annual CO2 concentrations are shown in dark blue.

Figure TS.10 - Likely ranges of warming trends.

TFE.4, Figure 1 - The Earth’s energy budget from 1970 through 2011

TFE.5, Figure 1 - Atlantic Meridional Overturning Circulation

Figure TS.11 - Simulated and observed 1951–2011 trends in the Southern Annular Mode index by season

Figure TS.12 - Comparison of observed and simulated change in the climate system, at regional scales and global scales

Box TS.4, Figure 1 - Summary of how well the current-generation climate models simulate important features of the climate of the 20th century

Box TS.5, Figure 1 - Simulations and reconstructions of the climate of the last millennium.

Box TS.6, Figure 1 - Modeled patterns of temperature and precipitation changes.

TFE.6, Figure 1 - Climate sensitivity

TFE.6, Figure 2 - Climate response

Figure TS.13 - Decadal prediction forecast quality of several climate indices.

Figure TS.14 - Synthesis of near-term projections of global mean surface air temperature

Figure TS.15 - Annual mean temperature change

Figure TS.16 - Maps of multi-model results for the scenarios in 2081–2100 of average percent change in mean precipitation

Figure TS.17 - Northern Hemisphere sea ice extent in September over the late 20th century and the whole 21st century for the scenarios

Figure TS.18 - Northern hemisphere snow cover and permafrost area over the 21st century

Figure TS.19 - Compatible fossil fuel emissions simulated by the CMIP5 models for the four RCP scenarios

Figure TS.20 - Time series (model averages and minimum to maximum ranges) and maps of multi-model surface ocean pH

TFE.7, Figure 1 - Percentage of CO2 pulse remaining in the atmosphere after a number of years

TFE.7, Figure 2 - Comparison of carbon cycle feedback metrics between the ensemble of seven General Circulation Models

Figure TS.21 - Projections of global mean sea level

Figure TS.22 - Projections from process-based models of global mean sea level

Figure TS.23 - Sea level rise in different scenarios

TFE.8, Figure 1 - Temperature increases in different scenarios

Figure TS.24 - Future change in monsoon statistics between the present-day (1986–2005) and the future (2080–2099)

Figure TS.25 - Standard deviation in CMIP5 multi-model ensembles of sea surface temperature variability over the eastern equatorial Pacific Ocean

Figure TS.26 - Projected changes in tropical cyclone statistics.

TFE.9, Figure 1 - Global projections of the occurrence of extreme events

Table TS.1 - Projected change in global mean surface air temperature and global mean sea level rise for the mid- and late 21st century relative to the reference period of 1986–2005.

Table TS.2 - Overview of projected regional changes and their relation to major climate phenomena.

TFE.9, Table 1 - Extreme weather and climate events: Global-scale assessment of recent observed changes, human contribution to the changes and projected further changes for the early (2016–2035) and late (2081–2100) 21st century