Earth System Science Data (Jun 2025)
Indicators of Global Climate Change 2024: annual update of key indicators of the state of the climate system and human influence
- P. M. Forster,
- C. Smith,
- C. Smith,
- T. Walsh,
- W. F. Lamb,
- W. F. Lamb,
- R. Lamboll,
- C. Cassou,
- C. Cassou,
- M. Hauser,
- Z. Hausfather,
- Z. Hausfather,
- J.-Y. Lee,
- J.-Y. Lee,
- M. D. Palmer,
- M. D. Palmer,
- K. von Schuckmann,
- A. B. A. Slangen,
- S. Szopa,
- B. Trewin,
- J. Yun,
- N. P. Gillett,
- S. Jenkins,
- H. D. Matthews,
- K. Raghavan,
- A. Ribes,
- J. Rogelj,
- J. Rogelj,
- J. Rogelj,
- D. Rosen,
- X. Zhang,
- M. Allen,
- M. Allen,
- L. Aleluia Reis,
- L. Aleluia Reis,
- R. M. Andrew,
- R. A. Betts,
- R. A. Betts,
- A. Borger,
- J. A. Broersma,
- S. N. Burgess,
- L. Cheng,
- P. Friedlingstein,
- P. Friedlingstein,
- C. M. Domingues,
- C. M. Domingues,
- M. Gambarini,
- M. Gambarini,
- T. Gasser,
- J. Gütschow,
- M. Ishii,
- C. Kadow,
- J. Kennedy,
- R. E. Killick,
- P. B. Krummel,
- A. Liné,
- A. Liné,
- A. Liné,
- D. P. Monselesan,
- C. Morice,
- J. Mühle,
- V. Naik,
- G. P. Peters,
- A. Pirani,
- J. Pongratz,
- J. Pongratz,
- J. C. Minx,
- J. C. Minx,
- M. Rigby,
- R. Rohde,
- A. Savita,
- A. Savita,
- S. I. Seneviratne,
- P. Thorne,
- C. Wells,
- L. M. Western,
- G. R. van der Werf,
- S. E. Wijffels,
- S. E. Wijffels,
- V. Masson-Delmotte,
- P. Zhai
Affiliations
- P. M. Forster
- Priestley Centre for Climate Futures, University of Leeds, Leeds, LS2 9JT, UK
- C. Smith
- Department of Water and Climate, Vrije Universiteit Brussel, Brussels, Belgium
- C. Smith
- International Institute for Applied Systems Analysis (IIASA), Vienna, Austria
- T. Walsh
- Environmental Change Institute, University of Oxford, Oxford, UK
- W. F. Lamb
- Priestley Centre for Climate Futures, University of Leeds, Leeds, LS2 9JT, UK
- W. F. Lamb
- Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, Potsdam, Germany
- R. Lamboll
- Centre for Environmental Policy, Imperial College London, London, UK
- C. Cassou
- Laboratoire de Météorologie Dynamique/Institut Pierre-Simon Laplace, CNRS, Ecole Normale Supérieure/Université PSL, Paris, France
- C. Cassou
- CECI, Université de Toulouse, CERFACS, CNRS, Toulouse, France
- M. Hauser
- Institute for Atmospheric and Climate Science, Department of Environmental Systems Science, ETH Zurich, Zurich, Switzerland
- Z. Hausfather
- Berkeley Earth, Berkeley, CA, USA
- Z. Hausfather
- Stripe Inc., South San Francisco, CA, USA
- J.-Y. Lee
- Research Center for Climate Sciences, Pusan National University, Busan, Republic of Korea
- J.-Y. Lee
- Center for Climate Physics, Institute for Basic Science, Busan, Republic of Korea
- M. D. Palmer
- Met Office Hadley Centre, Exeter, UK
- M. D. Palmer
- School of Earth Sciences, University of Bristol, Bristol, UK
- K. von Schuckmann
- Mercator Ocean international, Toulouse, France
- A. B. A. Slangen
- NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems, Yerseke, the Netherlands
- S. Szopa
- Institut Pierre Simon Laplace, Laboratoire des Sciences du Climat et de l'Environnement (UMR 8212 CEA-CNRS-UVSQ), Université Paris-Saclay, Gif-sur-Yvette, France
- B. Trewin
- Bureau of Meteorology, Melbourne, Australia
- J. Yun
- Research Center for Climate Sciences, Pusan National University, Busan, Republic of Korea
- N. P. Gillett
- Canadian Centre for Climate Modelling and Analysis, Environment and Climate Change Canada, Victoria, BC, Canada
- S. Jenkins
- Environmental Change Institute, University of Oxford, Oxford, UK
- H. D. Matthews
- Department of Geography, Planning and Environment, Concordia University, Montreal, Canada
- K. Raghavan
- Indian Institute of Tropical Meteorology, Pune, India
- A. Ribes
- CNRM, Université de Toulouse, Météo France, CNRS, Toulouse, France
- J. Rogelj
- International Institute for Applied Systems Analysis (IIASA), Vienna, Austria
- J. Rogelj
- Centre for Environmental Policy, Imperial College London, London, UK
- J. Rogelj
- Grantham Institute for Climate Change and Environment, Imperial College London, United Kingdom
- D. Rosen
- Priestley Centre for Climate Futures, University of Leeds, Leeds, LS2 9JT, UK
- X. Zhang
- Pacific Climate Impacts Consortium, University of Victoria, Victoria, Canada
- M. Allen
- Environmental Change Institute, University of Oxford, Oxford, UK
- M. Allen
- Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, Oxford, UK
- L. Aleluia Reis
- CMCC Foundation, Euro-Mediterranean Center on Climate Change, Lecce, Italy
- L. Aleluia Reis
- RFF-CMCC, European Institute on Economics and the Environment, Milan, Italy
- R. M. Andrew
- CICERO Center for International Climate Research, Oslo, Norway
- R. A. Betts
- Met Office Hadley Centre, Exeter, UK
- R. A. Betts
- Global Systems Institute, Science and Economy, University of Exeter, Exeter, UK
- A. Borger
- Climate Change Tracker, Data for Action Foundation, Amsterdam, the Netherlands
- J. A. Broersma
- Climate Change Tracker, Data for Action Foundation, Amsterdam, the Netherlands
- S. N. Burgess
- European Centre for Medium-Range Weather Forecasts, ECWMF, Reading, United Kingdom
- L. Cheng
- State Key Laboratory of Earth System Numerical Modeling and Application, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
- P. Friedlingstein
- Laboratoire de Météorologie Dynamique/Institut Pierre-Simon Laplace, CNRS, Ecole Normale Supérieure/Université PSL, Paris, France
- P. Friedlingstein
- Global Systems Institute, Science and Economy, University of Exeter, Exeter, UK
- C. M. Domingues
- Marine Physics and Ocean Climate, National Oceanography Centre, Southampton, UK
- C. M. Domingues
- Environmental Business Unit, CSIRO, Hobart, Tasmania, Australia
- M. Gambarini
- CMCC Foundation, Euro-Mediterranean Center on Climate Change, Lecce, Italy
- M. Gambarini
- RFF-CMCC, European Institute on Economics and the Environment, Milan, Italy
- T. Gasser
- International Institute for Applied Systems Analysis (IIASA), Vienna, Austria
- J. Gütschow
- Climate Resource, Melbourne, Australia
- M. Ishii
- Meteorological Research Institute, Tsukuba, Japan
- C. Kadow
- German Climate Computing Center (DKRZ), Hamburg, Germany
- J. Kennedy
- independent researcher: Verdun, France
- R. E. Killick
- Met Office Hadley Centre, Exeter, UK
- P. B. Krummel
- CSIRO Environment, Aspendale, Australia
- A. Liné
- CECI, Université de Toulouse, CERFACS, CNRS, Toulouse, France
- A. Liné
- Mercator Ocean international, Toulouse, France
- A. Liné
- Institut de Mécanique des Fluides de Toulouse, Université de Toulouse, INP, CNRS, Toulouse, France
- D. P. Monselesan
- CSIRO, Environment Research Unit, Climate intelligence, climate variability and hazards, Hobart, Tasmania, Australia
- C. Morice
- Met Office Hadley Centre, Exeter, UK
- J. Mühle
- Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA
- V. Naik
- NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA
- G. P. Peters
- CICERO Center for International Climate Research, Oslo, Norway
- A. Pirani
- Euro-Mediterranean Center on Climate Change (CMCC), Venice, Italy
- J. Pongratz
- Ludwig-Maximilians-Universität München, Munich, Germany
- J. Pongratz
- Max Planck Institute for Meteorology, Hamburg, Germany
- J. C. Minx
- Priestley Centre for Climate Futures, University of Leeds, Leeds, LS2 9JT, UK
- J. C. Minx
- Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, Potsdam, Germany
- M. Rigby
- School of Chemistry, University of Bristol, Bristol, United Kingdom
- R. Rohde
- Berkeley Earth, Berkeley, CA, USA
- A. Savita
- Centre for Atmospheric Sciences, Indian Institute of Technology Delhi, Delhi, India
- A. Savita
- Department of Atmospheric Sciences, Rosenstiel School of Marine, Atmospheric and Earth Science, Miami, FL, USA
- S. I. Seneviratne
- Institute for Atmospheric and Climate Science, Department of Environmental Systems Science, ETH Zurich, Zurich, Switzerland
- P. Thorne
- ICARUS Climate Research Centre, Maynooth University, Maynooth, Ireland
- C. Wells
- Priestley Centre for Climate Futures, University of Leeds, Leeds, LS2 9JT, UK
- L. M. Western
- School of Chemistry, University of Bristol, Bristol, United Kingdom
- G. R. van der Werf
- Wageningen University and Research, Wageningen, the Netherlands
- S. E. Wijffels
- CSIRO, Environment Research Unit, Climate intelligence, climate variability and hazards, Hobart, Tasmania, Australia
- S. E. Wijffels
- Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, MA, USA
- V. Masson-Delmotte
- Institut Pierre Simon Laplace, Laboratoire des Sciences du Climat et de l'Environnement (UMR 8212 CEA-CNRS-UVSQ), Université Paris-Saclay, Gif-sur-Yvette, France
- P. Zhai
- Chinese Academy of Meteorological Sciences, Beijing, China
- DOI
- https://doi.org/10.5194/essd-17-2641-2025
- Journal volume & issue
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Vol. 17
pp. 2641 – 2680
Abstract
In a rapidly changing climate, evidence-based decision-making benefits from up-to-date and timely information. Here we compile monitoring datasets (published at https://doi.org/10.5281/zenodo.15639576; Smith et al., 2025a) to produce updated estimates for key indicators of the state of the climate system: net emissions of greenhouse gases and short-lived climate forcers, greenhouse gas concentrations, radiative forcing, the Earth's energy imbalance, surface temperature changes, warming attributed to human activities, the remaining carbon budget, and estimates of global temperature extremes. This year, we additionally include indicators for sea-level rise and land precipitation change. We follow methods as closely as possible to those used in the IPCC Sixth Assessment Report (AR6) Working Group One report. The indicators show that human activities are increasing the Earth's energy imbalance and driving faster sea-level rise compared to the AR6 assessment. For the 2015–2024 decade average, observed warming relative to 1850–1900 was 1.24 [1.11 to 1.35] °C, of which 1.22 [1.0 to 1.5] °C was human-induced. The 2024-observed best estimate of global surface temperature (1.52 °C) is well above the best estimate of human-caused warming (1.36 °C). However, the 2024 observed warming can still be regarded as a typical year, considering the human-induced warming level and the state of internal variability associated with the phase of El Niño and Atlantic variability. Human-induced warming has been increasing at a rate that is unprecedented in the instrumental record, reaching 0.27 [0.2–0.4] °C per decade over 2015–2024. This high rate of warming is caused by a combination of greenhouse gas emissions being at an all-time high of 53.6±5.2 Gt CO2e yr−1 over the last decade (2014–2023), as well as reductions in the strength of aerosol cooling. Despite this, there is evidence that the rate of increase in CO2 emissions over the last decade has slowed compared to the 2000s, and depending on societal choices, a continued series of these annual updates over the critical 2020s decade could track decreases or increases in the rate of the climatic changes presented here.