ASIC 3 May 16-18 2006 Broadband Breakout Group Recommendations Big 3 Crosscutting Earth Radiation Budget.

Slides:



Advertisements
Similar presentations
Learning from the IPCC AR4: Possible implications for GCOS Stephan Bojinski GCOS Secretariat, WMO.
Advertisements

Space-based Architecture for Climate Mary Kicza NOAA’s Assistant Administrator for Satellite and Information Services May 19, 2011.
Meteorological Observatory Lindenberg – Richard Assmann Observatory The GCOS Reference Upper Air Network.
TRUTHS (Traceable Radiometry Underpinning Terrestrial and Helio- Studies) Establishing an observational climate benchmark dataset. Paul Green & Nigel Fox.
Global Climate Observing System (GCOS) including GRUAN Greg Bodeker Bodeker Scientific, Alexandra, New Zealand Presented at the 9 th Ozone Research Managers.
Consistency between planetary heat balance and ocean heat storage Clivar research focus team: Karina von Schuckmann, Bernard Barnier, Carol Anne Clayson,
Pre-launch Characterization of the CERES Flight Model 5 (FM5) Instrument on NPP S. Thomas a, K. J. Priestley b, M. Shankar a, N. P. Smith a, M. G. Timcoe.
Working toward high accuracy and consistency of essential climate variables from multiple satellite ocean color missions …a joint CEOS/IOCCG initiative…
Global Warming and Climate Sensitivity Professor Dennis L. Hartmann Department of Atmospheric Sciences University of Washington Seattle, Washington.
Traceability to SI temperature standards: A prerequisite for Climate Data Records of SST Peter J Minnett Meteorology & Physical Oceanography Rosenstiel.
Climate Forcing and Physical Climate Responses Theory of Climate Climate Change (continued)
Calibration and Status of MOBY Dennis Clark, NOAA/NESDIS Carol Johnson, NIST Steve Brown, NIST Mark Yarbrough, MLML Stephanie Flora, MLML Mike Feinholz,
Langley Research Center / Atmospheric Sciences Directorate Climate Calibration Observatory Roadmap/Decadal Survey Mission Concept Bruce Wielicki, NASA.
Princeton University Global Evaluation of a MODIS based Evapotranspiration Product Eric Wood Hongbo Su Matthew McCabe.
Clouds and the Earth’s Radiant Energy System Langley Research Center / Science Directorate NASA Langley Research Center / Science Directorate State of.
ICESat dH/dt Thinning Thickening ICESat key findings.
Determining the accuracy of MODIS Sea- Surface Temperatures – an Essential Climate Variable Peter J. Minnett & Robert H. Evans Meteorology and Physical.
2010 CEOS Field Reflectance Intercomparisons Lessons Learned K. Thome 1, N. Fox 2 1 NASA/GSFC, 2 National Physical Laboratory.
CERES-GERB Joint Science Teams The Geostationary Earth Radiation Budget (GERB) experiment GERB Status Imperial College London J E Harries (GERB.
Meteorological Observatory Lindenberg – Richard Assmann Observatory The GCOS Reference Upper Air Network.
Data Matters from Sessions 8, 9 and 11 WOAP-4 Task Group 1 Contributors: H Cattle, E Kent, J Key, T Koike, C Kummerow, M Manton, K Taylor, C von Savigny,
Climate Change: Moonshine, Millions of Models, & Billions of Data New Ways to Sort Fact from Fiction Bruce Wielicki March 21, 2007 University of Miami.
Ocean Synthesis and Air-Sea flux evaluation Workshop Global Synthesis and Observations Panel (GSOP) Organized by Lisan Yu, Keith Haines, Tony Lee WHOI,
GOES-R Support to Future Climate Monitoring Needs Mitch Goldberg Chief, Satellite Meteorology and Climatology Division Office of Research and Applications.
15-18 October 2002 Greenville, North Carolina Global Terrestrial Observing System GTOS Jeff Tschirley Programme director.
2 - 1 Mission Concept Review 17Nov10 Bruce Wielicki, David Young, Marty Mlynczak, Rosemary Baize NASA Langley Roger Cooke Resources for the Future April.
The Earth’s surface is kept warm through one source: the Sun. It is the primary source for Earth’s energy. Some of the incoming sunlight and heat energy.
1 CERES Results Norman Loeb and the CERES Science Team NASA Langley Research Center, Hampton, VA Reception NASA GSFC, Greenbelt, MD.
Integrated Mission Review 28Jan108Jan10: N - 1 Use or disclosure of the data contained on this sheet is subject to the restrictions on the IMR cover page.
GOES Users’ Conference III May 10-13, 2004 Broomfield, CO Prepared by Integrated Work Strategies, LLC GOES USERS’ CONFERENCE III: Discussion Highlights.
Overview of the “Geostationary Earth Radiation Budget (GERB)” Experience. Nicolas Clerbaux Royal Meteorological Institute of Belgium (RMIB) In collaboration.
2008 US CLIVAR Summit Phenomena Observations and Synthesis.
NRC April 23, NPOESS EDRs vs. Climate Data Records (CDRs) John J. Bates, Chief Remote Sensing Applications Division NOAA’s National Climatic Data.
Diane E. Wickland NPP Program Scientist NPP Science: HQ Perspective on VIIRS May 18, 2011.
Climate data past and future: Can we more effectively monitor and understand our changing climate? Peter Thorne.
1 NOAA’s Science Data Stewardship Project: Background, Concepts, and Examples of Climate Data and Information Records (CDRs and CIRs) National Climatic.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 The Influences of Changes.
Climate Absolute Radiance and Refractivity Observatory (CLARREO) The Story so Far… David F. Young NASA Langley Research Center CLARREO Mission Study Lead.
IOCCG Standing Working Group on Satellite Ocean Colour Radiometry Essential Climate Variable (ECV) Assessment (Coming to a city near you in 2012)
Meteorological Observatory Lindenberg Results of the Measurement Strategy of the GCOS Reference Upper Air Network (GRUAN) Holger Vömel, GRUAN.
ISCCP Calibration 25 th Anniversary Symposium July 23, 2008 NASA GISS Christopher L. Bishop Columbia University New York, New York.
VIIRS Product Evaluation at the Ocean PEATE Frederick S. Patt Gene C. Feldman IGARSS 2010 July 27, 2010.
Meteorological Observatory Lindenberg – Richard Assmann Observatory (2010) GCOS Reference Upper Air Network Holger Vömel Meteorological Observatory Lindenberg.
RMIB involvement in the Geostationary Earth Radiation Budget (GERB) and Climate Monitoring SAF projects Nicolas Clerbaux Remote sensing from Space Division.
ISCCP SO FAR (at 30) GOALS ►Facilitate "climate" research ►Determine cloud effects on radiation exchanges ►Determine cloud role in global water cycle ▬
1 Climate Absolute Radiance and Refractivity Observatory (CLARREO) Welcome David Young Project Scientist CLARREO Mission Formulation Team NASA Langley.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 Closing the Global Sea Level.
Estimation of Potential Evapotranspiration from Merged CERES and MODIS Observations Anand Inamdar & A. French Arid Land Agricultural Research Center (ALARC/ARS/USDA)
CLARREO Science Briefing 11/14/08 1 Reflected Solar Accuracy Science Requirements Bruce Wielicki, Dave Young, Constantine Lukashin, Langley Zhonghai Jin,
Use of the Moon as a calibration reference for NPP VIIRS Frederick S. Patt, Robert E. Eplee, Robert A. Barnes, Gerhard Meister(*) and James J. Butler NASA.
CIOSS Ocean Optics Aug 2005 Ocean Optics, Cal/Val Plans, CDR Records for Ocean Color Ricardo M Letelier Oregon State University Outline - Defining Ocean.
October 2, 2002National Climatic Data Center GOES USERS CONFERENCE October 2,
Overview of Climate Observational Requirements for GOES-R Herbert Jacobowitz Short & Associates, Inc.
- 1 CLARREO Science Meeting CLARREO Science Meeting July 6, 2010 July 6, 2010 Bruce Wielicki.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Double Differences of BTs in AVHRR Ch4 from MICROS Climate Quality Calibration.
NASA Langley Research Center / Atmospheric Sciences CERES Instantaneous Clear-sky and Monthly Averaged Radiance and Flux Product Overview David Young NASA.
1 Changes in global net radiative imbalance Richard P. Allan, Chunlei Liu (University of Reading/NCAS Climate); Norman Loeb (NASA Langley); Matt.
© University of Reading 2011www.reading.ac. uk Tracking Earth’s Energy since 2000 Richard Allan University of Reading/NCAS climate Collaborators: Norman.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 STAR Enterprise Synthesis.
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.
CLARREO Pathfinder - Overview
Validation status overivew
Validation status overivew
VIS/NIR reference instrument requirements
Update on Advancing Development of the ROLO Lunar Calibration System
M. J. Burgdorf, S. A. Buehler, I. Hans
Reconciling Ocean Heating and
Recent activities of OCR-VC
Earth Radiation Budget: Insights from GERB and future perspectives
Integrated Satellite Global Energy Data for Climate Studies
Presentation transcript:

ASIC 3 May Broadband Breakout Group Recommendations Big 3 Crosscutting Earth Radiation Budget

ASIC 3 May Achieving Satellite Instrument Calibration for Climate Change Roughly 100 attendees, mostly NOAA, NASA, with some international from key programs (GCOS) or satellite calibration concepts

Big 3 Recommendations Continuous Overlapped Satellite Altimeter Sea Level Data: key climate riskContinuous Overlapped Satellite Altimeter Sea Level Data: key climate risk Continuous Overlapped Broadband Earth Radiation Budget Data: key IPCC climate feedback and forcing uncertaintyContinuous Overlapped Broadband Earth Radiation Budget Data: key IPCC climate feedback and forcing uncertainty Calibration Benchmark Mission: 0.2 to 100  m. Spectrally resolved plus broadband. Crosscuts calibration of many climate variables.Calibration Benchmark Mission: 0.2 to 100  m. Spectrally resolved plus broadband. Crosscuts calibration of many climate variables.

Crosscutting Recommendations Calibration Standards activity unified across GEO, GCOS, IEEE effortsCalibration Standards activity unified across GEO, GCOS, IEEE efforts SI traceable is a goal, absolute accuracy and long term stability should both be designed into the system to assure success. SI may not be sufficient if sampling or analysis algorithms are inadequate. (e.g. perfect single surface pyranometer) or SI standard does not meet climate rqmt.SI traceable is a goal, absolute accuracy and long term stability should both be designed into the system to assure success. SI may not be sufficient if sampling or analysis algorithms are inadequate. (e.g. perfect single surface pyranometer) or SI standard does not meet climate rqmt. Joint Center for Satellite IntercalibrationJoint Center for Satellite Intercalibration –Very useful for NOAA, Enhances connections of instrument calibration to NIST, NASA science team climate missions already doing this as part of science team activities. –Maintain responsibility in climate data record science teams Two additional Climate Observing Principles : independent observations and independent scientific analysis.Two additional Climate Observing Principles : independent observations and independent scientific analysis. Reprocessing of CDRs, including Level1b radiances to resolve errors is fundamentalReprocessing of CDRs, including Level1b radiances to resolve errors is fundamental

Crosscutting Recommendations Science team involvement in climate data records must be continual to reach climate accuracy.Science team involvement in climate data records must be continual to reach climate accuracy. –Transition NASA science team approach to NOAA climate programs: responsibility for calibration, algorithms, and validation and reprocessing.

Broadband Recommendations Earth Reflected and Emitted Broadband FluxesEarth Reflected and Emitted Broadband Fluxes –Do Earth Radiation Budget measurements on NPP (2009) to eliminate current 20% gap risk –To meet stability requirments, improve characterization of CERES FM-5 (silver mirror spectral char, MAM coatings, lamps/monitors) –Pre-launch round robin calibrations (e.g. GERB, CERES radiometric test model, CERBE?) with NIST –Put past broadband radiometers on common radiometric scale –Global Net Earth Radiation Error Budget and define current best consistency with ocean heat storage –Quantify accuracy of contamination/uv exposure of broadband instruments. –Reprocess broadband record from 1980 to 2000 consistently on common radiometric scale and analysis algorithms. –Work with GEWEX Radiative Flux Assessment to improve use of narrowband AVHRR/geostationary/AVHRR estimates of past radiation budget and constrain to broadband radiometry scale

Broadband Recommendations Change SW, LW stability goal from 0.3 Wm -2 to 0.15 Wm -2 per decade. Purpose is to constrain climate sensitivity to +/- 25% (I.e. 1/4 of anthropogenic forcing of 0.6 Wm -2 per decade). Accuracy goal remains 1 Wm -2.Change SW, LW stability goal from 0.3 Wm -2 to 0.15 Wm -2 per decade. Purpose is to constrain climate sensitivity to +/- 25% (I.e. 1/4 of anthropogenic forcing of 0.6 Wm -2 per decade). Accuracy goal remains 1 Wm -2. Extend studies of deep convection and lunar viewing for broadband indepenent consistency/stability checks.Extend studies of deep convection and lunar viewing for broadband indepenent consistency/stability checks.