Heating of Earth's climate continues in the 2000s based upon satellite data and ocean observations Richard P. Allan 1, N. Loeb 2, J. Lyman 3, G. Johnson.

Slides:



Advertisements
Similar presentations
University of Reading 2007www.nerc-essc.ac.uk/~rpa Monitoring satellite observations and model simulations of changes in the atmospheric.
Advertisements

© University of Reading 2009 EUMETSAT Monitoring changes in precipitation and radiative energy using satellite data and.
3) Empirical estimate of surface longwave radiation Use an empirical estimate of the clear-sky surface downward longwave radiation (SDLc) to estimate the.
Links Between Clear-sky Radiation, Water Vapour and the Hydrological Cycle Richard P. Allan 1, Viju O. John 2 1 Environmental Systems Science Centre, University.
Trends in Water Cycle meeting, Paris, November 2004 Cloud and water vapour variability: models, reanalyses and observations Richard P. Allan and Tony Slingo.
University of Reading 2007www.nerc-essc.ac.uk/~rpa Observed and simulated changes in water vapour, precipitation and the clear-sky.
Changes in Water Vapour, Clear-sky Radiative Cooling and Precipitation
1 Changes in low-latitude radiative energy budget - a missing mode of variability in climate models? Richard P. Allan, Tony Slingo Hadley Centre for Climate.
Earth’s Radiative Forcing Given the data: Can you close the energy budget? Alex, Elizabeth, & Tyreke.
Water Vapor and Cloud Feedbacks Dennis L. Hartmann in collaboration with Mark Zelinka Department of Atmospheric Sciences University of Washington PCC Summer.
Richard P. Allan 1 | Brian J. Soden 2 | Viju O. John 3 | Igor I. Zveryaev 4 Department of Meteorology Click to edit Master title style Water Vapour (%)
Reconciling net TOA flux/ocean heating in observations and models 5-yr running means (Smith et al. 2015)Smith et al Spurious ocean data? CERES ERBS/reconReanalysis/recon.
SHNHCEF EI ind c-5.3±0.24.5±0.1−0.8±0.1 EI dir c-5.4±0.24.8± ±0.2 E40 ind c−5.7±0.34.9±0.3−0.9±0.2 E40 dir c-4.9±0.64.7± ±0.2 FT08−4.9±0.25.1±0.5-
Use of CCSM3 and CAM3 Historical Runs: Estimation of Natural and Anthropogenic Climate Variability and Sensitivity Bruce T. Anderson, Boston University.
Radiation Group 3: Manabe and Wetherald (1975) and Trenberth and Fasullo (2009) – What is the energy balance of the climate system? How is it altered by.
On the Radiative and Dynamical Feedbacks over the Equatorial Pacific Cold Tongue De-Zheng Sun John Fasullo Tao Zhang Andres Roubicek J. Climate, 2003,
1 CERES Results Norman Loeb and the CERES Science Team NASA Langley Research Center, Hampton, VA Reception NASA GSFC, Greenbelt, MD.
3 May 2007 GIST May Professor John Harries, Professor John Harries, Space and Atmospheric Physics group, Blackett Laboratory, Imperial College,
Climate Forecasting Unit Attribution of the global temperature plateau Virginie Guemas, Francisco J. Doblas-Reyes, Isabel Andreu-Burillo and.
ISCCP at 30, April 2013 Backup Slides. ISCCP at 30, April 2013 NVAP-M Climate Monthly Average TPW Animation Less data before 1993.
© University of Reading Hadley Centre Workshop: Improving predictions of the large- scale hydrological cycle Agreement/discrepancies.
Interagency Ocean Observation Committee The Integrated Coastal & Ocean Observing System Act of 2009  Interagency Ocean Observing Committee  Lead Federal.
Satellite & Model Evidence for Global Warming Being Driven by the Pacific Decadal Oscillation Dr. Roy W. Spencer Principal Research Scientist The University.
LIMITLESS POTENTIAL | LIMITLESS OPPORTUNITIES | LIMITLESS IMPACT Copyright University of Reading AIR-SEA FLUXES FROM ATMOSPHERIC REANALYSES Richard Allan.
LIMITLESS POTENTIAL | LIMITLESS OPPORTUNITIES | LIMITLESS IMPACT Copyright University of Reading CHANGES IN EARTH’S ENERGY BALANCE AND IMPLICATIONS FOR.
1 Changes in global net radiative imbalance Richard P. Allan, Chunlei Liu (University of Reading/NCAS Climate); Norman Loeb (NASA Langley); Matt.
A Changing Character of Precipitation in a Warming World: Physical Drivers Richard Allan Department of Meteorology, University of Reading
Additional CLIVAR meeting slides Richard P. Allan – University of Reading.
DEEP-C: Diagnosing Earth’s Energy Pathways in the Climate system PIs : Richard Allan, Elaine McDonagh, Matt Palmer University of Reading, National Oceanography.
© University of Reading 2011www.reading.ac. uk Tracking Earth’s Energy since 2000 Richard Allan University of Reading/NCAS climate Collaborators: Norman.
LIMITLESS POTENTIAL | LIMITLESS OPPORTUNITIES | LIMITLESS IMPACT Copyright University of Reading CURRENT CHANGES IN EARTH’S ENERGY IMBALANCE
Current changes in precipitation and moisture Richard P. Allan, Chunlei Liu, Matthias Zahn Department of Meteorology, University of Reading Thanks to George.
Tracking Earth’s Net Energy Imbalance since 2000 Richard Allan University of Reading/NCAS climate.
The importance of upper tropospheric water and cloud for climate change Richard P. Allan Department of Meteorology/NCAS Climate, University of Reading.
CERES Update As for CERES status:
DEEPC: WP1 overview & rapid trawl through the literature…
Sensitivity of precipitation extremes to ENSO variability
Current and future changes in precipitation and its extremes
Current changes in Earth’s energy budget
Influence of climate variability and
Current Changes in Earth’s Energy Imbalance and the Global Water Cycle
Radiative biases in Met Office global NWP model
Introduction & WP1 update
Current changes in Earth’s ENERGY imbalance
changes in Earth’s ENERGY balance & implications for the water cycle
Introduction & WP1 update
Dust, vapour & cloud in greenhouse Earth
Global hydrological forcing: current understanding
Energy accumulation and surface warming
Monitoring current changes in precipitation and Earth’s radiative energy balance using satellite data, reanalyses and models Richard P. Allan1 | Viju.
Richard P.
Where has the warming gone?
Recent research updates for SMURPHS
Reconciling Ocean Heating and
Understanding Current Observed Changes in the Global Water Cycle
Changes in global net radiative imbalance
Current global and regional changes in atmospheric water vapour
Project Title: The Sensitivity of the Global Water and Energy Cycles:
New energy budget estimates at top of Earth’s atmosphere and surface
New energy budget estimates at top of Earth’s atmosphere and surface
How and why is rainfall changing across the globe?
Global energy and water cycle group
Environmental Systems Science Centre, University of Reading
Integrated Satellite Global Energy Data for Climate Studies
New energy budget estimates at top of Earth’s atmosphere and surface
Global to regional manifestation of Earth's energy imbalance
New energy budget estimates at top of Earth’s atmosphere and surface
TEMPERATURE anomaly (degC)
CURRENT Energy Budget Changes
New energy budget estimates at top of Earth’s atmosphere and surface
Presentation transcript:

Heating of Earth's climate continues in the 2000s based upon satellite data and ocean observations Richard P. Allan 1, N. Loeb 2, J. Lyman 3, G. Johnson 3 1 University of Reading (Department of Meteorology/NCAS Climate), 2 NASA Langley, 3 NOAA/PMEL Also thanks to Brian Soden, Graeme Stephens and CERES group

Decline in rate of surface warming? Global annual average temperature anomalies relative to 1951–1980 mean (shading denotes lower and upper 95% uncertainty range for HadCRUT4)

Radiative forcing or energy redistribution? Small, persistent volcanic forcing? –e.g. Solomon et al. (2011) ScienceSolomon et al. (2011) Science Sulphur emissions? –e.g. Kaufmann et al. (2011) PNASKaufmann et al. (2011) PNAS Stratospheric water vapour? –e.g. Solomon et al. (2010) ScienceSolomon et al. (2010) Science Cloud forcing/feedbacks & El Nino? Ocean circulation e.g. Modelling studies: Meehl et al. (2011) Nature Climate Change Meehl et al. (2011) Nature Climate Change, Palmer et al. (2010) GRL, Katsman and van Oldenborgh (2011) GRL Palmer et al. (2010) GRL Katsman and van Oldenborgh (2011) GRL

Missing energy? Trenberth and Fasullo (2010, Science) highlighted an apparent large discrepancy between net radiation and ocean heat content changesTrenberth and Fasullo (2010, Science) We undertook a reanalysis of the satellite and ocean record over the period …

Ocean Heat Content data Use weighted integral to account for changes in data coverage Ensures transition to ARGO era does not introduce spurious variability Integrate ocean heat content trend over time and divide by Earth’s surface area  Wm -2 Lyman & Johnson (2008) J Clim

Ocean heat content data uncertainty Accounting for considerable sampling/structural uncertainty we find no evidence for a robust decline in ocean heating rate since 2005 Loeb et al. (2012) Nat. Geosci.

Updated CERES satellite data Global Earth Radiation Balance Correction for degradation of shortwave filter Correction also improves physical consistency of trends in daytime longwave We use version CERES_EBAF-TOA_Ed2.6r

Trends in net radiation 8 Errors in satellite sensors and inappropriate use of satellite products explain much of large rise in net radiative flux shown by Trenberth and Fasullo (2010) global net radiation anomalies

Combining Earth Radiation Budget and Ocean Heat Content data Tie 10-year CERES record with SORCE TSI and ARGO- estimated heating rate Best estimates for additional storage terms Variability relating to ENSO reproduced by CERES and ERA Interim Estimate of decade long net energy imbalance of 0.54±0.43 Wm –2 Loeb et al. (2012) Nat. Geosci.

Combining Earth Radiation Budget and Ocean Heat Content data Replotted so that CERES and ERA Interim sample 6-months later than ARGO Is there a lag in the system? Where in ocean is energy accumulating? Mechanism?

Variation in net radiation since S-60N, after Allan (2011) Meteorol. AppsAllan (2011) Meteorol. Apps

Conclusions and Future work Previously highlighted “missing energy” explained by ocean heat content uncertainty combined with inappropriate net radiation satellite products Heating of Earth continues ( ~ 0.5 Wm -2 ) –Negative radiative forcing does not appear to strongly contribute Implications: –Energy continues to accumulate below the ocean surface –Strengthening of Walker circulation, e.g. Merrifield (2011) J Clim?Merrifield (2011) J Clim See also poster A203 (CL2.10), Hall A Friday AM (Matthias Zahn) –Implications for hydrological cycle, e.g. Simmons et al. (2010) JGR?Simmons et al. (2010) JGR See also poster A204 (CL2.10), Hall A Friday AM (Chunlei Liu)