GOES-8 thru GOES-15 NPP VIIRS MSG SEVIRI AVHRR GOES Sounder MTG FCI

Slides:

Advertisements

Similar presentations

Electromagnetic Radiation

Advertisements

1 Satellite Imagery Interpretation. 2 The SKY Biggest lab in the world. Available to everyone. We view from below. Satellite views from above.

Electromagnetic Radiation Electromagnetic Spectrum Radiation Laws Atmospheric Absorption Radiation Terminology.

CLOUD DETECTION WITH OPERATIONAL IMAGERS

SCIENCE NEWS Magnitude CENTRAL ITALY Magnitude CENTRAL ITALY.

ATS 351 Lecture 8 Satellites

CIRA & NOAA/NESDIS/RAMM GOES/POES Status, Orbits, and Products Dr. Bernie Connell CIRA/NOAA-RAMMT March 2005.

Steven Miller Cooperative Institute for Research in the Atmosphere (CIRA), Colorado State University, Ft. Collins, CO Jeremy Solbrig, Mindy Surratt, Kim.

Satellite Imagery Meteorology 101 Lab 9 December 1, 2009.

Image Interpretation for Weather Analysis Part 2 27 February 2008 Dr. Steve Decker.

GOES Advanced Baseline Imager (ABI) Color Product Development Don Hillger NOAA/NESDIS/StAR CoRP Third Annual.

Climate, Meteorology and Atmospheric Chemistry.

1 Remote Sensing of the Ocean and Atmosphere: John Wilkin Sea Surface Temperature IMCS Building Room 214C

The sun as a source of Energy Atmospheric Processes.

Visible Satellite Imagery Spring 2015 ARSET - AQ Applied Remote Sensing Education and Training – Air Quality A project of NASA Applied Sciences Week –

Introduction and Methodology Daniel T. Lindsey*, NOAA/NESDIS/STAR/RAMMB Louie Grasso, Cooperative Institute for Research in the Atmosphere

Remote Sensing Allie Marquardt Collow Met Analysis – December 3, 2012.

Spectral Band Selection for the Advanced Baseline Imager (ABI) Tim Schmit Paul Menzel September 1999 National Oceanic and Atmospheric Administration NESDIS/ORA.

What exactly is a budget? Do you or your parents have a budget? Definition: budg·et an estimate of income and expenditure for a set period of time.

Presentation April 26, 2007 at the NASA GSFC Earth Day celebrations Our Home Planet as Viewed from the Aqua Satellite Claire L. Parkinson/Aqua Project.

GOES-R highlights Bernie Connell Cooperative Institute for Research in the Atmosphere Colorado State University December 2013.

Green-1 9/17/2015 Green Band Discussion Satellite Instrument Synergy Working Group September 2003.

1 Met 10 Weather Processes Jeff Gawrych Temperature, Heat Transfer and Earth’s Energy Balance.

Applications and Limitations of Satellite Data Professor Ming-Dah Chou January 3, 2005 Department of Atmospheric Sciences National Taiwan University.

Spectral Characteristics

What are the four principal windows (by wavelength interval) open to effective remote sensing from above the atmosphere ? 1) Visible-Near IR ( );

Satellite-derived Sea Surface Temperatures Corey Farley Remote Sensing May 8, 2002.

SATELLITE METEOROLOGY BASICS satellite orbits EM spectrum

GOES-R ABI Synthetic Imagery at 3.9 and 2.25 µm 24Feb2015 Poster 2 Louie Grasso, Yoo-Jeong Noh CIRA/Colorado State University, Fort Collins, CO

Advanced Baseline Imager (ABI) will be flown on the next generation of NOAA Geostationary Operational Environmental Satellite (GOES)-R platform. The sensor.

Hank Revercomb, David C. Tobin, Robert O. Knuteson, Fred A. Best, Daniel D. LaPorte, Steven Dutcher, Scott D. Ellington, Mark W.Werner, Ralph G. Dedecker,

RGB Activities for the GOES-R Proving Ground Gary Jedlovec, NASA / MSFC / SPoRT Mark DeMaria NOAA / NESDIS / STAR Tim Schmit NOAA / NESDIS / CIMSS and.

Atmospheric turbulence identification to aid aviation safety USING MODIS.

Lessons on Satellite Meteorology Part I : General Introduction Short history Geo versus polar satellite Visible images Infrared images Water vapour images.

Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al Atmospheric Environment.

Bill Campbell, Brian Gockel, and Jim Heil (NOAA/NWS) Marge Ripley and Jean-Jacques Bedet (NOAA/NESDIS/GOES-R) Improved Temporal Resolution GOES-R Sectorized.

Preparing for GOES-R: old tools with new perspectives Bernadette Connell, CIRA CSU, Fort Collins, Colorado, USA ABSTRACT Creating.

Spectral Band Selection for the Advanced Baseline Imager (ABI)

Real-time Display of Simulated GOES-R (ABI) Experimental Products Donald W. Hillger NOAA/NESDIS, SaTellite Applications and Research (STAR) Regional And.

Satellites Storm “Since the early 1960s, virtually all areas of the atmospheric sciences have been revolutionized by the development and application of.

SANDY SUPPLEMENTAL PROJECT: NEW AWIPS DATA FOR ALASKA Carl Dierking, Tom Heinrichs, Gwen Bryson, Jay Cable, Scott Macfarlane, Jessie Cherry, Eric Stevens.

1 GLIMPSING THE FIRST PRODUCTS FROM VIIRS Dr. Wayne Esaias NASA GSFC Thomas F. Lee Jeffrey Hawkins Arunas Kuciauskas Kim Richardson Jeremy Solbrig Naval.

Matthew Lagor Remote Sensing Stability Indices and Derived Product Imagery from the GOES Sounder

GOES-R ABI AS A WARNING AID Louie Grasso, Renate Brummer, and Robert DeMaria CIRA, Fort Collins, CO Dan Lindsey, Don Hillger, NOAA/NESDIS/RAMMB, Fort Collins,

Satellite Imagery. Geostationary Satellites (GOES) Geostationary satellites orbit high (approximately 36,000 km) above the equator and orbit around the.

Remote sensing of snow in visible and near-infrared wavelengths

GOES-R ABI and Himawari-8 AHI Training using SIFT

True-Color Imagery for GOES-R: Creating a Green Band for ABI

GOES-R ABI and Himawari-8 AHI Training using SIFT

VIIRS and the Fort McMurray Fire VISIT Satellite Chat (18 May 2016)

AmeriGEOSS Week. GEONETCast. Americas and

Who We Are SSEC (Space Science and Engineering Center) is part of the Graduate School of the University of Wisconsin-Madison (UW). SSEC hosts CIMSS (Cooperative.

ABI Visible/Near-IR Bands

Sea Surface Temperature

Geostationary Sounders

TIROS-1: The First Weather Satellite

Suomi NPP VIIRS Day Night Band (DNB)

DNB provides more low cloud structure City Lights

ELECTROMAGNETIC RADIATION

devised by: D. Rosenfeld

Objective Overshooting Top and Cold V Detection

Generation of Cloud Products from NOAA’s Operational Satellite Imagers

GOES -12 Imager April 4, 2002 GOES-12 Imager - pre-launch info - radiances - products Timothy J. Schmit et al.

Image Interpretation for Weather Analysis

Mark Schoeberl NASA/GSFC

Front page of the realtime GOES-12 site, showing all of the latest Sounder spectral bands (18 infrared and 1 visible) over the central and Eastern US All.

Convectively Induced Turbulence

Representing Climate Data II

ELECTROMAGNETIC RADIATION

Presentation transcript:

GOES-8 thru GOES-15 NPP VIIRS MSG SEVIRI AVHRR GOES Sounder MTG FCI Imager Band Central Wavelength (μm) Wavelength Range Band Explanation Spatial Resolution (km) @ nadir 1 0.65 0.55 - 0.75 Visible 2 3.9 3.8 - 4.0 Shortwave IR window 4 3 6.75 (GOES-8/11) 6.5 - 7.0 Water vapor 8 6.48 (GOES-12/15) 5.8 - 7.3 10.7 10.2 - 11.2 Longwave IR window 5 12.0 (GOES-8/11) 11.5 - 12.5 Split-window 6 13.3 (GOES-12/13) 12.9 - 13.7 Longwave IR 13.3 (GOES-14/15) VIIRS Band Central Wavelength (μm) Wavelength Range Band Explanation Spatial Resolution (m) @ nadir M1 0.412 0.402 - 0.422 Visible/ Reflective 750 m M2 0.445 0.436 - 0.454 M3 0.488 0.478 - 0.488 M4 0.555 0.545 - 0.565 M5 (B) 0.672 0.662 - 0.682 M6 0.746 0.739 - 0.754 Near IR M7 (G) 0.865 0.846 - 0.885 M8 1.240 1.23 - 1.25 Shortwave IR M9 1.378 1.371 - 1.386 M10 (R) 1.61 1.58 - 1.64 M11 2.25 2.23 - 2.28 M12 3.7 3.61 - 3.79 Medium-wave IR M13 4.05 3.97 - 4.13 M14 8.55 8.4 - 8.7 Longwave IR M15 10.763 10.26 - 11.26 M16 12.013 11.54 - 12.49 DNB 0.7 0.5 - 0.9 750 m across full scan I1 (B) 0.64 0.6 - 0.68 375 m I2 (G) 0.85 - 0.88 I3 (R) I4 3.74 3.55 - 3.93 I5 11.45 10.5 - 12.4 MSG Band Central Wavelength (μm) Wavelength Range Band Explanation Spatial Resolution (km) @ nadir 1 (B) 0.635 0.56 – 0.71 Visible 3 2 (G) 0.81 0.74 – 0.88 3 (R) 1.64 1.50 – 1.78 Ice/water 4 3.92 3.48 – 4.36 Shortwave IR 5 6.25 5.35 – 7.15 Water vapor 6 7.35 6.85 – 7.85 7 8.7 8.3 – 9.1 8 9.66 9.38 – 9.94 Ozone 9 10.8 9.8 – 11.8 Longwave IR 10 12.0 11.0 – 13.0 11 13.4 12.4 – 14.4 CO2 12 0.75 0.5 – 0.9 Broadband visible 1 AVHRR (1.1 km spatial resolution @ nadir) AVHRR Band Central Wavelength (μm) Wavelength Range Band Explanation 1 0.63 0.58 - 0.68 Visible 2 0.86 0.73 - 1.00 3 (3B) 3.74 3.55 - 3.93 Shortwave window 4 10.8 10.3 - 11.3 Longwave IR window 5 12.0 11.5 - 12.5 Split-window 6 (3A) 1.61 1.58 - 1.64 Reflective snow/ice Red component band is highlighted in red color. GOES Sounder (10 km spatial resolution @ nadir) Red component band is highlighted in red color. Natural-color component bands are noted with R, G, and B GOES Sounder Band Central Wavelength (μm) Wavelength Range Band Explanation 1 14.71 14.6 - 14.8 Longwave IR 2 14.37 14.2 - 14.5 3 14.06 13.9 - 14.2 4 13.64 13.5 - 13.8 5 13.37 13.3 - 13.5 6 12.66 12.4 - 12.9 7 12.02 11.7 - 12.4 Split-window 8 11.03 10.7 - 11.3 Longwave IR window 9 9.71 9.59 - 9.83 Ozone 10 7.43 7.32 - 7.61 Water vapor 11 7.02 6.83 - 7.24 12 6.51 6.40 - 6.63 13 4.57 4.55 - 4.60 Shortwave IR 14 4.52 4.51 - 4.55 15 4.46 4.43 - 4.47 16 4.13 4.16 - 4.10 17 3.98 3.95 - 4.02 Shortwave window 18 3.74 3.68 - 3.82 19 0.70 0.68 - 0.72 Visible Red component band is highlighted in red color. MTG FCI FCI Band Central Wavelength (μm) Bandwidth Band Explanation Spatial Resolution (km) @ nadir 1 0.44 0.06 Visible/reflective 2 0.51 0.04 3 (B) 0.64 0.05 1 / 0.51 4 (G) 0.865 Reflective 5 0.914 0.02 6 1.38 0.03 Cirrus 7 (R) 1.61 Snow/ice 8 2.25 Particle size 9 3.8 0.4 Shortwave IR window 2 / 11 10 6.3 1.0 Water vapor 11 7.35 0.5 12 8.7 Water vapor, SO2 13 9.66 0.3 Ozone 14 10.5 0.7 Longwave IR window 15 12.3 Longwave IR 16 13.3 0.6 MODIS (1 km spatial resolution @ nadir, unless otherwise specified) MODIS Band Central Wavelength (μm) Wavelength Range Band Explanation 1 (B) 0.645 0.620 - 0.670 Land/Cloud Boundaries (0.25 km @ nadir) 2 (G) 0.858 0.841 - 0.876 3 0.469 0.459 - 0.479 Land/Cloud Properties (0.5 km @ nadir) 4 0.555 0.545 - 0.565 5 1.240 1.230 - 1.250 6 (R) 1.640 1.628 - 1.652 7 2.130 2.105 - 2.155 8 0.412 0.405 - 0.420 Ocean Color / Phytoplankton / Biogeochemistry (13A and 14A are low-polarization) 9 0.443 0.438 - 0.448 10 0.488 0.483 - 0.493 11 0.531 0.526 - 0.536 12 0.551 0.546 - 0.556 13 (13A) 0.667 0.662 - 0.672 14 (14A) 0.678 0.673 - 0.683 15 0.748 0.743 - 0.753 16 0.870 0.862 - 0.877 17 0.905 0.890 - 0.920 Atmospheric Water Vapor 18 0.936 0.931 - 0.941 19 0.940 0.915 - 0.965 20 3.75 3.66 - 3.84 Surface/Cloud Temperature (shortwave CO2) 21 (high-temp) 3.959 3.929 - 3.989 22 23 4.05 4.02 - 4.08 24 4.466 4.433 - 4.498 Atmospheric Temperature (shortwave CO2) 25 4.516 4.482 - 4.549 26 1.375 1.36 - 1.39 Cirrus Clouds 27 6.715 6.535 - 6.895 Water Vapor 28 7.325 7.175 - 7.475 29 8.55 8.4 - 8.7 30 9.73 9.58 - 9.88 Ozone (O3) 31 11.03 10.78 - 11.28 Surface/Cloud Temperature 32 12.02 11.77 - 12.27 33 13.335 13.185 - 13.485 Cloud Top Altitude (longwave CO2) 34 13.635 13.485 - 13.785 35 13.935 13.785 - 14.085 36 14.235 14.085 - 14.385 37 (13B) High-polarization Ocean Color / Phytoplankton / Biogeochemistry 38 (14B) M = Moderate (750 m) resolution bands I = Imagery (375 m) resolution bands DNB = Day-Night Band (or Near Constant Contrast (NCC) band) True-color component bands are highlighted in red, green, and blue. Natural-color component bands are noted with R, G, and B. True-color component bands are highlighted in red, green, and blue. Natural-color component bands are noted with R, G, and B. 1Resolution depends on imaging mode. Red component band is highlighted in red color. GOES-R ABI Geo-KOMPSAT-2A ‘ABI’ MTSAT/Himawari-8/9 AHI ABI Band Central Wavelength (μm) Wavelength Range Band Explanation Spatial Resolution (km) @ nadir 1 0.47 0.45 - 0.49 Visible/reflective X1 0.55 synthetic 2 (B) 0.64 0.59 - 0.69 0.5 3 (G) 0.865 0.846 - 0.885 Reflective 4 1.378 1.371 - 1.386 Cirrus 2 5 (R) 1.61 1.58 - 1.64 Snow/ice 6 2.25 2.225 - 2.275 Particle size 7 3.90 3.80 - 4.00 Shortwave IR window 8 6.19 5.77 - 6.6 Water vapor 9 6.95 6.75 - 7.15 10 7.34 7.24 - 7.44 11 8.5 8.3 - 8.7 Water vapor, SO2 12 9.61 9.42 - 9.8 Ozone 13 10.35 10.1 - 10.6 Longwave IR window 14 11.2 10.8 - 11.6 15 12.3 11.8 - 12.8 Longwave IR 16 13.3 13.0 - 13.6 AHI Band Central Wavelength (μm) Band Explanation Spatial Resolution (km) @ nadir 1 0.46 Visible/reflective 2 0.51 3 (B) 0.64 0.5 4 (G) 0.86 Reflective 5 (R) 1.6 Snow/ice 6 2.3 Particle size 7 3.9 Shortwave IR window 8 6.2 Water vapor 9 7.0 10 7.3 11 8.6 Water vapor, SO2 12 9.6 Ozone 13 10.4 Longwave IR window 14 11.2 15 12.3 Longwave IR 16 13.3 ‘ABI’ Band Central Wavelength (μm) Wavelength Range Band Explanation Spatial Resolution (km) @ nadir 1 0.46 0.431 – 0.479 Visible/reflective 2 0.51 0.5025 – 0.5175 3 (B) 0.64 0.625 – 0.66 0.5 4 (G) 0.86 0.8495 – 0.8705 Reflective 5 1.38 1.373 – 1.383 Cirrus 6 (R) 1.61 1.601 – 1.619 Snow/ice 7 3.85 3.74 – 3.96 Shortwave IR window 8 6.24 6.061 – 6.425 Water vapor 9 6.95 6.89 – 7.01 10 7.35 7.258 – 7.433 11 8.6 8.44 – 8.76 Water vapor, SO2 12 9.63 9.543 – 9.717 Ozone 13 10.43 10.25 – 10.61 Longwave IR window 14 11.2 11.06 – 11.32 15 12.3 12.15 – 12.45 Longwave IR 16 13.3 13.21 – 13.39 True-color component bands are highlighted in red, green, and blue. Natural-color component bands are noted with R, G, and B. 1The X (green) band needs to be synthesized from the other ABI bands. True-color component bands are highlighted in red, green, and blue. Natural-color component bands are noted with R, G, and B True-color component bands are highlighted in red, green, and blue. Natural-color component bands are noted with R, G, and B. True-color component bands are highlighted in red, green, and blue. Natural-color component bands are noted with R, G, and B.