ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 1 1. CO 2 Science and Sounder.

Slides:



Advertisements
Similar presentations
Environmental Application of Remote Sensing: CE 6900 Tennessee Technological University Department of Civil and Environmental Engineering Course Instructor:
Advertisements

LIDAR TECHNOLOGIES FOR EARTH OBSERVATION January 2008 Dr Kim Hampton Lidar Technologies Ltd.
(Program Director: George Komar)
Studying the Physical Properties of the Atmosphere using LIDAR technique Dinh Van Trung and Nguyen Thanh Binh, Nguyen Dai Hung, Dao Duy Thang, Bui Van.
Lecture 12 Content LIDAR 4/15/2017 GEM 3366.
Calibration Scenarios for PICASSO-CENA J. A. REAGAN, X. WANG, H. FANG University of Arizona, ECE Dept., Bldg. 104, Tucson, AZ MARY T. OSBORN SAIC,
Earth System Science Teachers of the Deaf Workshop, August 2004 S.O.A.R. High Earth Observing Satellites.
CO budget and variability over the U.S. using the WRF-Chem regional model Anne Boynard, Gabriele Pfister, David Edwards National Center for Atmospheric.
Doppler Wind and Temperature Sounder: A breakthrough technique GATS Proprietary Larry Gordley, GATS Inc. Dave Fritts, GATS Inc. Tom Marshall, GATS Inc.
The ICESat-2 Mission: Laser altimetry of ice, clouds and land elevation T. Markus, T. Neumann NASA Goddard Space Flight Center W. Abdalati Earth Science.
MR P.Durkee 5/20/2015 MR3522Winter 1999 MR Remote Sensing of the Atmosphere and Ocean - Winter 1999 Active Microwave Radar.
ICESat Overview H. Jay Zwally NASA Goddard Greenbelt, Maryland Bob E. Schutz The University of Texas at Austin Center for Space Research Laser Ranging.
Measured parameters: particle backscatter at 355 and 532 nm, particle extinction at 355 nm, lidar ratio at 355 nm, particle depolarization at 355 nm, atmospheric.
The Earth System Analyzer: Using all of the Data to Improve NOAA’s Mission Capabilities Alexander E. MacDonald NOAA Earth System Research Laboratory.
Observational Approaches for Climate Treaty Verification: Atmospheric observations provide the only source of independent information through which treaty.
Remote Sensing of Mesoscale Vortices in Hurricane Eyewalls Presented by: Chris Castellano Brian Cerruti Stephen Garbarino.
Combining satellite and surface observations to determine the radiative divergence across the atmosphere Tony Slingo Environmental Systems Science Centre.
HIRDLS High Resolution Dynamic Limb Sounder. Basics Set to fly on the Aura mission of NASA’s Earth Observation System Set to fly on the Aura mission of.
A-SCOPE Advanced Space Carbon and Climate Observation of Planet Earth MAG: F.M. Breon, H. Dolman, G. Ehret, P. Flamant, N. Gruber, S. Houweling, M. Scholze,
Code 912, Principle Investigator: Mr. Bruce Gentry NASA Academy Research Associate Jeremy Dobler.
Geostationary Imaging Fourier Transform Spectrometer An Update of the GIFTS Program Geostationary Imaging Fourier Transform Spectrometer An Update of the.
Spaceborne Weather Radar
Science Objectives for the ATHENA-OAWL Venture Tech Airborne Mission M. Hardesty CIRES University of Colorado/NOAA S. Tucker and C. Weimer Ball Aerospace.
G O D D A R D S P A C E F L I G H T C E N T E R Goddard Lidar Observatory for Winds (GLOW) Wind Profiling from the Howard University Beltsville Research.
OC3522Summer 2001 OC Remote Sensing of the Atmosphere and Ocean - Summer 2001 Active Microwave Radar.
B. Gentry/GSFCSLWG 06/29/05 Scaling Ground-Based Molecular Direct Detection Doppler Lidar Measurements to Space Using Wind Profile Measurements from GLOW.
An In-depth Look at ICESat and GLAS By: Vishana Ramdeen.
Space-Qualified Hardware for the CALIPSO Lidar
The Orbiting Carbon Observatory (OCO) Mission Watching Earth Breathe…Mapping Carbon Dioxide from Space Science Writers’ Workshop American Geophysical Union.
B.-M. Sinnhuber, Remote Sensing I, University of Bremen, Summer 2007 Remote Sensing I Active Remote Sensing Summer 2007 Björn-Martin Sinnhuber Room NW1.
Mike Newchurch 1, Shi Kuang 1, John Burris 2, Steve Johnson 3, Stephanie Long 1 1 University of Alabama in Huntsville, 2 NASA/Goddard Space Flight Center,
Scaling Surface and Aircraft Lidar Results for Space-Based Systems (and vice versa) Mike Hardesty, Barry Rye, Sara Tucker NOAA/ETL and CIRES Boulder, CO.
B. Gentry/GSFCGTWS 2/26/01 Doppler Wind Lidar Measurement Principles Bruce Gentry NASA / Goddard Space Flight Center based on a presentation made to the.
Measurement Example III Figure 6 presents the ozone and aerosol variations under a light-aerosol sky condition. The intensity and structure of aerosol.
GIFTS - The Precursor Geostationary Satellite Component of a Future Earth Observing System GIFTS - The Precursor Geostationary Satellite Component of a.
Field Methods of Monitoring Atmospheric Systems Remote Sensing Copyright © 2006 by DBS.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
Spaceborne 3D Imaging Lidar John J. Degnan Geoscience Technology Office, Code Code 900 Instrument and Mission Initiative Review March 13, 2002.
Page 1 The Passive A-band Wind Sounder (PAWS) for Measurement of Tropospheric Winds Brian R. Johnson (CO- I), Shane Roark (PI), Pei Huang, Grzegorz Miecznik,
Status of CFLOS study using CALIPSO data G. D. Emmitt, D. Winker and S. Greco WG SBLW Destin, FL January 27-30, 2009.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 Infrared Temperature and.
NASA ESTO ATIP Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations 12/12/01 NASA Goddard - Laser Remote Sensing Branch 1 James B. Abshire,
HOLOGRAPHIC SCANNING LIDAR TELESCOPES Geary K. Schwemmer Laboratory For Atmospheres NASA Goddard Space Flight Center
Geoscience Laser Altimeter System Aerosol and Cloud Observations by the GLAS Polar Orbiting Lidar Instrument NASA - Goddard Space Flight Center Launched.
Measurement Example III Figure 6 presents the ozone and aerosol variations under a light-aerosol sky condition. The intensity and structure of aerosol.
AIRS science team meeting Camp Springs, February 2003 Holger Vömel University of Colorado and NOAA/CMDL Upper tropospheric humidity validation measurements.
A new method for first-principles calibration
NASA Goddard - Laser Remote Sensing Branch 1/16/02 JBA 1 3/12/02 NASA/GSFC - Laser Remote Sensing Branch 1 Mars Orbital Lidar Small Orbital Planetary Lidar.
CO 2 an important driver for climate change. Currently only approximately half of the CO 2 produced by man can be accounted for in the atmosphere and oceans,
NASA Carbon Cycle & Ecosystems Joint Science Workshop 28 April - 2 May 2008 Berrien Moore III Climate Central Princeton, NJ & University of New Hampshire.
Ball Aerospace & Technologies Corporation -
1 Atmospheric Radiation – Lecture 13 PHY Lecture 13 Remote sensing using emitted IR radiation.
Spectrometer for Sky-Scanning, Sun-Tracking Atmospheric Research (4STAR) Earth Science Division - NASA Ames Research Center 2006 A concept for a sun-sky.
SCM x330 Ocean Discovery through Technology Area F GE.
NASA, CGMS-44, 7 June 2016 Coordination Group for Meteorological Satellites - CGMS SURFACE PRESSURE MEASUREMENTS FROM THE ORBITING CARBON OBSERVATORY-2.
Passive Microwave Remote Sensing
The Lodore Falls Hotel, Borrowdale
PADMA ALEKHYA V V L, SURAJ REDDY R, RAJASHEKAR G & JHA C S
Lidar winds from GEO: The Photons to Winds Conversion Efficiency
Pre-launch Characteristics and Calibration
G. Mevi1,2, G. Muscari1, P. P. Bertagnolio1, I. Fiorucci1
NASA/US Ocean Satellite Missions
Lidar winds from GEO: The Photons to Winds Conversion Efficiency
Surface Pressure Measurements from the NASA Orbiting Carbon Observatory-2 (OCO-2) Presented to CGMS-43 Working Group II, agenda item WGII/10 David Crisp.
Clouds, shear and the simulation of hybrid wind lidar
G. Mevi1,2, G. Muscari1, P. P. Bertagnolio1, I. Fiorucci1
NPOESS Airborne Sounder Testbed (NAST)
Instrument Considerations
By Narayan Adhikari Charles Woodman
Satellite Foundational Course for JPSS (SatFC-J)
Presentation transcript:

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC CO 2 Science and Sounder Overviews Jim Abshire

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 2 OCEANS LAND ATMOSPHERE + 3 Pg /yr 7 Pg /yr ~120 Pg /yr ~90 Pg /yr 1. The Global Carbon Cycle 1Pg C = g C  Only about 50% of the CO 2 emitted each year shows up in the atmosphere. The rest is absorbed by ocean or terrestrial “sinks”.  A detailed understanding of these sinks is needed to predict future atmospheric CO 2 levels.

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 3 Possible consequences of inaccurate or too late predictions:

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 4 CO 2 Sounder Concept

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 5 Current capability for measuring CO 2 is primarily the NOAA/CMDL surface air sampling network: Lidar on satellites can give the needed global coverage and the needed dawn-dusk measurement times. Significant limitations:  Flask samples are obtained only biweekly at most sites.  Samples are infrequent  Too coarse in spatial coverage to capture the CO2 signal Sun-synchronous Orbit – 1 month 600 km 550 km Why measure CO 2 with Lidar from orbit ?

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 6 CO2 1570nm Absorption Band Single CO2 Absorption Line & Background CO2 1570nm Absorption Band

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 7 Relative Absorptivity Pressure Altitude (km) LINE CENTER 90% 75% 50% 25% COLUMN Relative Frequency (wavenumbers) Transmittance The absorption lines are pressure broadened Measuring on side of absorption line permits weighting of tropospheric CO 2 Sounder technique permits selecting the on-line locking point to optimize the weighting function Using Pressure broadening permits weighting to troposphere

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 8 ICESat/GLAS Measurements Surface Altimetry: Range to ice, land, water, clouds Time of flight: 1064 nm laser pulse Digitizes transmitted & received 1064-nm pulse waveforms Laser-beam attitude from star- trackers, laser camera & gyro Atmospheric Lidar: Laser backscatter profiles from clouds & aerosols 1064 nm & 532 nm laser pulses Profiles; 75 m vertical resolution Analog; photon counting detection Simultaneous, co-located measurements with altimeter ICESat & GLAS provide needed data and Heritage

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC 1- 9 Day of 2003 CO 2 (ppmv) Licor In-Situ Co2 Sampler - Update Licor now operating continuously, 24 hours per day with automatic calibrations. Repaired Building 33 weather station—provides meteorological context (e.g., wind speed, direction) needed to compare Licor data with laser sounder. Morning Rush Hour: 6-9am Evening Rush Hour: 4-7pm

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC ICESat I GLAS is now in space & operational Our CO 2 Sounder team had leadership roles in it In terms of the CO 2 Sounder, GLAS has: Demonstrated some key measurements Demonstrated some key lidar technologies Shown complexity of the real atmosphere & the actual CO 2 measurement environment Our CO 2 measurement approach is best suited to leverage from GLAS & measure in actual atmospheric conditions 2. GLAS Instrument on the ICESat mission

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC GLAS during integration with ICESat in June 2002 at Ball Aerospace in Boulder, Colorado GLAs Instrument during Testing Primary involvements: Science measurement approach & specification, technology trades, laser technology tradeoffs, detector and filter development, pre-& post- launch testing, calibration

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC GLAS Instrument Graphics courtesy of GLAS Instrument Team (not to same scale) Emitted Laser Pulse (532 nm) Reflected Laser Pulse (532 nm) Altimeter Detectors (2) Lidar Detectors (8) Lasers (3) Telescope Sun Shade Main Mirror (1m) Secondary Mirror IST and LRS

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC New Space Lidar Technology developed by GLAS Team for ICESat GLAS instrument components now available for use on future lidar missions: 100 cm diameter telescope; laser flight unit which delivers 75 mJ at 1064 nm & 35 mJ at 532 nm; thermally tuned solid etalon with 42% peak transmission and a 26 pm bandwidth; (d) Perkin Elmer SPCM photon counting detector with 70% counting efficiency at 770 nm. a) d)

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC Glas Surface Topography Measurements GLAS Science Team

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC Glas Surface Topography Measurements GLAS Science Team

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC Open Path CO2 measurements - test range Test Range (laser path highlighted)

ESTO Advanced Component Technology 11/17/03 Laser Sounder for Remotely Measuring Atmospheric CO 2 Concentrations GSFC Measurement validation Comparison of CO2 Sounder Prototype with Licor  Comparison Approach:  Sounder raw data offset & scaled  Sounder referenced to Licor at single point  Best results were Excellent:  Agreement (correlation) was ±1 ppm over 6 hours.  Measurement precision < 1 ppm