CERES Update As for CERES status:

Slides:



Advertisements
Similar presentations
TOA radiative flux diurnal cycle variability Patrick Taylor NASA Langley Research Center Climate Science Branch NEWS PI Meeting.
Advertisements

Ocean Heat Uptake Gregory C. Johnson 1,2, John M. Lyman 3,1, & Sarah G. Purkey 2,1 1 NOAA/Pacific Marine Environmental Laboratory, 2 University of Washington.
1. weather or climate ? Annual mean temperature (red is warm, blue cold)
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.
TEMPLATE DESIGN © Total Amount Altitude Optical Depth Longwave High Clouds Shortwave High Clouds Shortwave Low Clouds.
Surface Atmospheric Radiation Budget (SARB) working group update Seiji Kato 1, Fred Rose 2, David Rutan 2, Alexander Radkevich 2, Tom Caldwell 2, David.
Climate Change: Moonshine, Millions of Models, & Billions of Data New Ways to Sort Fact from Fiction Bruce Wielicki March 21, 2007 University of Miami.
Global Interannual Upper Ocean Heat Content Variability Gregory C. Johnson (NOAA/PMEL), John M. Lyman (UH/JIMA & NOAA/PMEL), Josh K. Willis (NASA/JPL),
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.
1 CERES Results Norman Loeb and the CERES Science Team NASA Langley Research Center, Hampton, VA Reception NASA GSFC, Greenbelt, MD.
Global Scale Energy Fluxes: Comparison of Observational Estimates and Model Simulations Aaron Donohoe -- MIT David Battisti -- UW CERES Science Team Meeting.
NASA Langley Research Center / Science Directorate CERES SW channel spectral darkening: Rev1 adjustments and beyond Contributors: Norman Loeb, Jennifer.
ISCCP at its 30 th (New York, 22 – 25 April, 2013) Congratulations to the “Core Team” and to “Patient Outside-Supporters”: Our best wishes for a perspective.
ISCCP at 30, April 2013 Backup Slides. ISCCP at 30, April 2013 NVAP-M Climate Monthly Average TPW Animation Less data before 1993.
A Preliminary Evaluation of the Global Water and Energy Budgets in an Upcoming NASA Reanalysis Junye Chen (1,2) and Michael G. Bosilovich (2) 1 ESSIC,
National Aeronautics and Space Administration Energy and the Atmosphere Dr. Lin H. Chambers, NASA Langley Research Center, Hampton, VA New.
 We also investigated the vertical cross section of the vertical pressure velocity (dP/dt) across 70°W to 10°E averaged over 20°S-5°S from December to.
1 J. Ranson NASA’s Earth Observing System Terra Mission Update Jon Ranson, Terra Project Scientist Si-Chee Tsay, Terra Deputy Project Scientist NASA’s.
Consistent Earth System Data Records for Climate Research: Focus on Shortwave and Longwave Radiative Fluxes Rachel T. Pinker, Yingtao Ma and Eric Nussbaumer.
Variability of CO 2 From Satellite Retrievals and Model Simulations Xun Jiang 1, David Crisp 2, Edward T. Olsen 2, Susan S. Kulawik 2, Charles E. Miller.
LIMITLESS POTENTIAL | LIMITLESS OPPORTUNITIES | LIMITLESS IMPACT Copyright University of Reading AIR-SEA FLUXES FROM ATMOSPHERIC REANALYSES Richard Allan.
NASA Langley Research Center / Atmospheric Sciences CERES Instantaneous Clear-sky and Monthly Averaged Radiance and Flux Product Overview David Young NASA.
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.
1 Changes in global net radiative imbalance Richard P. Allan, Chunlei Liu (University of Reading/NCAS Climate); Norman Loeb (NASA Langley); Matt.
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
Understanding and Improving Marine Air Temperatures David I. Berry and Elizabeth C. Kent National Oceanography Centre, Southampton
Tracking Earth’s Net Energy Imbalance since 2000 Richard Allan University of Reading/NCAS climate.
A New Climatology of Surface Energy Budget for the Detection and Modeling of Water and Energy Cycle Change across Sub-seasonal to Decadal Timescales Jingfeng.
The importance of upper tropospheric water and cloud for climate change Richard P. Allan Department of Meteorology/NCAS Climate, University of Reading.
DEEPC: WP1 overview & rapid trawl through the literature…
Yinghui Liu1, Jeff Key2, and Xuanji Wang1
Mid Term II Review.
Insights into Earth’s energy imbalance from multiple sources
Sensitivity of precipitation extremes to ENSO variability
Xiquan Dong, Baike Xi, Erica Dolinar, and Ryan Stanfield
Current changes in Earth’s energy budget
Influence of climate variability and
Instrumental Surface Temperature Record
Reanalyzed Clouds, Precipitation, TOA and Surface Radiation Budgets: A Global Satellite Comparison and a Regional Study at Two ARM Locations Erica Dolinar,
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
The absorption of solar radiation in the climate system
changes in Earth’s ENERGY balance & implications for the water cycle
Energy accumulation and surface warming
Variability of CO2 From Satellite Retrievals and Model Simulations
Monitoring current changes in precipitation and Earth’s radiative energy balance using satellite data, reanalyses and models Richard P. Allan1 | Viju.
Richard P.
Components of the yield trend.
Instrumental Surface Temperature Record
Where has the warming gone?
Variability of CO2 From Satellite Retrievals and Model Simulations
Reconciling Ocean Heating and
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 will precipitation change under global warming?
Global mean temperatures are rising faster with time Warmest 12 years:
Surface Fluxes and Model Error An introduction
Global energy and water cycle group
Instrumental Surface Temperature Record
Integrated Satellite Global Energy Data for Climate Studies
TEMPERATURE anomaly (degC)
CURRENT Energy Budget Changes
Presentation transcript:

CERES Update As for CERES status: CERES instruments on Terra and Aqua performing nominally (except for SW channel on FM4 which failed in March 2005) Release of SSF1deg, SYN1deg and EBAF Ed2.6 on new CERES subsetter/visualization/ordering tool: http://ceres.larc.nasa.gov/order_data.php Merged CERES Terra and Aqua data code has been delivered to ASDC. In testing. Latest Edition of CERES cloud code delivered (Edition4) to ASDC. Production to start in September. Upcoming events: - Next CERES science team meeting October 4-6, 2011 at Lawrence Livermore National Laboratory. - CERES FM5 on NPP launch date October 25, 2011. - Special Aqua@10 Union session at Fall AGU in December. Science Results: - Paper refuting Trenberth's "Missing Energy" Science Perspectives paper.   The paper has been submitted to Nature Geosciences.

Paper to Nature Geosciences Heating of Earth's Climate System Continues Despite Lack of Surface Warming in Past Decade Norman G. Loeb1*, John M. Lyman2,3, Gregory C. Johnson3, Richard P. Allan4, David R. Doelling1, Takmeng Wong1, Brian J. Soden5 and Graeme L. Stephens6

Paper to Nature Geosciences Figure 1 | Global surface temperature anomalies during the past 30 years. Global annual average temperature anomalies from the 1981–2010 mean (black dots with 95% confidence limits) from the HadCRUT3 dataset10. The trend for the entire period (dashed line) is 0.016±0.002 °C/yr. For 2001–2010 the trend (red line) is 0.00±0.01 °C/yr. Figure 4 | Comparison of net TOA flux and upper ocean heating rates. (a) Global annual average net TOA flux from CERES observations (based upon the EBAFTOA_ Ed2.6 product) and (b) ERA Interim reanalysis25 are anchored to an estimate of Earth’s heating rate for 2006–2010 (see methods). The Pacific Marine Environmental Laboratory/Jet Propulsion Laboratory/Joint Institute for Marine and Atmospheric Research (PMEL/JPL/JIMAR) ocean heating rate estimates17 (a) use data from Argo and World Ocean Database 200918; Uncertainties for upper ocean heating rates are given at one-standard error derived from OHCA uncertainties3. See methods for a description of CERES uncertainties. The gray bar (b) corresponds to one standard deviation about the 2001–2010 average net TOA flux of 15 CMIP3 models.