M11 Saturation Assessment Chris Elvidge Earth Observation Group NOAA-NESDIS-NGDC June 3, 2014.

Slides:



Advertisements
Similar presentations
Summary of Changes for DATA 4.69 David Stevenson April 24, 2008.
Advertisements

NOAA National Geophysical Data Center
VIIRS Data Evaluation Over Thailand and Japan February 13, 2012 Chair, Chris Elvidge NOAA-NGDC 1.
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course
1 VIIRS McIDAS-V Colby, CA Fire January 17-20, 2014 William Straka III 1.
Boyles Law Experiment Starter If a cylinder with a piston is full air, how are the volume of the air and the air pressure related? In other words, as the.
Hercules 265 Natural Gas Platform Blaze Detected by VIIRS Nightfire July 24, 2013 NOAA-NGDC Earth Observation Group
FAFSA on the Web Preview Presentation December 2013.
MULTICULTURAL LITERACY February 10, INTRODUCTION  1. What is jazz music?  2. Can you name anyone involved in jazz music?  3. Can you name major.
DEELS workshop, ESRF, 12.– 13. May 2014 Friederike Ewald Difficulties to measure the absolute electron beam energy using spin depolarisation at the ESRF.
GOES-13 Scan Mirror E-W Emissivity Correction The four GOES-13 Imager infrared (IR) bands are characterized across the full scan width for space-view measurements:
Lightning Imager and its Level 2 products Jochen Grandell Remote Sensing and Products Division.
15 May 2009ACSPO v1.10 GAC1 ACSPO upgrade to v1.10 Effective Date: 04 March 2009 Sasha Ignatov, XingMing Liang, Yury Kihai, Boris Petrenko, John Stroup.
Improved Automated Cloud Classification and Cloud Property Continuity Studies for the Visible/Infrared Imager/Radiometer Suite (VIIRS) Michael J. Pavolonis.
VIIRS LST Uncertainty Estimation And Quality Assessment of Suomi NPP VIIRS Land Surface Temperature Product 1 CICS, University of Maryland, College Park;
VIIRS Low Light Imaging Applications
Request to trade M7 for M11 at night Christopher D. Elvidge, Ph.D. Earth Observation Group NOAA-NESDIS National Geophysical Data Center Boulder, Colorado.
RHESSI/GOES Observations of the Non-flaring Sun from 2002 to J. McTiernan SSL/UCB.
Using Impervious Surface as a spatially explicit Proxy Measure of CO 2 Emssions Dr. Paul C. Sutton Dr. Sharolyn Anderson Dr. Sharolyn Anderson Department.
GRAVITY Analysis & Interpretation GG 450 Feb 5, 2008.
Analysis of D Band Cloud Flag Jane Hurley Anu Dudhia Graham Ewen University of Oxford.
October 14, 2010Neural Networks Lecture 12: Backpropagation Examples 1 Example I: Predicting the Weather We decide (or experimentally determine) to use.
Determination of System Equivalency – TaskForce Audi, EA-52, V4.0 WLTP-10-33e.
Determining the Molar Heat of Combustion for Paraffin
Grocery Measure: LEDs for Reach-In Display Cases Regional Technical Forum July 21 st, 2015 Mohit Singh-Chhabra.
Elec471 Embedded Computer Systems Chapter 4, Probability and Statistics By Prof. Tim Johnson, PE Wentworth Institute of Technology Boston, MA Theory and.
VIIRS Nighttime Lights Algorithm Development 2015
Interannual and Regional Variability of Southern Ocean Snow on Sea Ice Thorsten Markus and Donald J. Cavalieri Goal: To investigate the regional and interannual.
Estimation of poverty rates based on satellite observed nighttime lights Chris Elvidge, NOAA National Geophysical Data Center (NGDC) Boulder, Colorado.
Prospects for Improved Global Mapping of Development Using VIIRS Data Chris Elvidge Earth Observation Group NOAA-NESDIS National Geophysical Data Center.
NPP VIIRS M6 Saturation Study Update
VIIRS Global DNB Product Status Chris Elvidge Earth Observation Group NOAA National Geophysical Data Center Kim Baugh, Feng-Chi Hsu, Mikhail Zhizhin CIRES,
Slide 1 EUMETSAT Fellow Day, 9 March 2015 Observation Errors for AMSU-A and a first look at the FY-3C MWHS-2 instrument Heather Lawrence, second-year EUMETSAT.
CHAPTER 1 LESSON 3 Math in Science.
03/05/03© 2003 University of Wisconsin Last Time Tone Reproduction If you don’t use perceptual info, some people call it contrast reduction.
Cathy Clerbaux, Geocape meeting, May 2011 The potential of MTG-IRS to detect high pollution events at urban and regional scales 1/ What do we see with.
Headwall Instrument Overview Laboratory Characterizations Geo-Location Field Characterization Data Product Description References.
This material is approved for public release. Distribution is limited by the Software Engineering Institute to attendees. Sponsored by the U.S. Department.
GERB-2 V999 Unfiltering Nicolas Clerbaux & RMIB GERB Team. GIST 24, Imperial College, London 15 december 2005.
NoRH Observations of Prominence Eruption Masumi Shimojo Nobeyama Solar Radio Observatory NAOJ/NINS 2004/10/28 Nobeyama Symposium SeiSenRyo.
AIRS Radiance and Geophysical Products: Methodology and Validation Mitch Goldberg, Larry McMillin NOAA/NESDIS Walter Wolf, Lihang Zhou, Yanni Qu and M.
Slide 1 NATO UNCLASSIFIEDMeeting title – Location - Date Satellite Inter-calibration of MODIS and VIIRS sensors Preliminary results A. Alvarez, G. Pennucci,
MODIS Collection 6 MCST Proposed Changes to L1B. Page 2 Introduction MODIS Collection History –Collection 5 – Feb present –Collection 4 – Jan.
STAR Algorithm and Data Products (ADP) Provisional Maturity Review Suomi NPP Surface Type EDR Products X. Zhan, C. Huang, R. Zhang, K. Song, M. Friedl,
Using MODIS and AIRS for cloud property characterization Jun W. Paul Menzel #, Steve Chian-Yi and Institute.
Satellites Storm “Since the early 1960s, virtually all areas of the atmospheric sciences have been revolutionized by the development and application of.
VIIRS Nighttime Lights Creating the Next Generation of Global Remotely-Sensed Nighttime Lights Products From VIIRS Day/Night Band (DNB) Data Chris Elvidge.
Global vs mesoscale ATOVS assimilation at the Met Office Global Large obs error (4 K) NESDIS 1B radiances NOAA-15 & 16 HIRS and AMSU thinned to 154 km.
Understanding and Improving Marine Air Temperatures David I. Berry and Elizabeth C. Kent National Oceanography Centre, Southampton
Aqua-MODIS and VIIRS DCC calibration
CCD Calibrations Eliminating noise and other sources of error.
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course
SNPP data access for agricultural monitoring
Weather Cloud Detection
Validation status overivew
NOAA VIIRS Team GIRO Implementation Updates
What Causes Day and Night?
Validation status overivew
MODIS SST Processing and Support for GHRSST at OBPG
ENGINEERING MEASUREMENTS
VIRTIS Operations at Lutetia
Using SCIAMACHY to calibrate GEO imagers
A “Field Guide” to WFPC2 HLA Image Anomalies
MODIS Characterization and Support Team Presented By Truman Wilson
AHI IR Tb bias variation diurnal & at low temperature
Using VIIRS I or M band as the calibration reference
Differential Emission Measure
What Causes Day and Night?
Signal Detection & Processing
What Causes Day and Night?
Presentation transcript:

M11 Saturation Assessment Chris Elvidge Earth Observation Group NOAA-NESDIS-NGDC June 3, 2014

CCR Request for M11 collection at night The VIIRS Nightfire (VNF) product relies on the detects and analyzes temperature, source size and heat release of combustion sources at night, with heavy reliance on M10 data collected at night. Adding M11 would resolve many ambiguous detections with weak signal and would aid in noise screening. To constrain data volume, M7 collection at night would be discontinued. The CCR has approval for further study.

How did VIIRS come to collect daytime data at night? Original Message Subject: Re: [NOTIFY] Does anyone use M7 nighttime data? Date: Mon, 10 Feb :57: From: Shawn W Miller To: Chris Elvidge Hi Chris, Way back in , I was the one who led the push to have the instrument folks turn these bands on at night, precisely to help with Active Fires (since we were unsuccessful in getting the saturation temperature raised as high as we wanted it in the thermal IR). During that analysis I determined that M11 would saturate for most fires that consumed more than 1% of the area of a pixel - that's the main reason the program doesn't currently have it turned on at night. That's not to say my analysis didn't have errors, or that it still wouldn't provide the value you're looking for, but just a heads-up that you might want to look at the dynamic range of that band if you haven't already. Shawn _________________________________________ Shawn W. Miller, Ph.D. Chief Architect, JPSS CGS Engineering Fellow, Raytheon IIS Office: Cell:

Determination of M11 Detection Limit and Saturation Radiance Detection limit set at the background noise average plus four standard deviations in nighttime M11 data collected in polar region W/m2.sr.um. Saturation radiance found in daytime data collected of extreme events W/m2.sr.um.

M11 Detection Limit and Saturation

M11 Saturation on May 20, 2014 Alaska Fire

M11 Saturation Summary M11 will saturate on small numbers of extreme events. Full saturation will be obvious. Inclusion of subpixel saturation in VNF Planck curve fitting would introduce errors in temperature, source size and heat release retrievals. Subpixel saturation also happens for M12. VNF detects M12 saturation based on the M13/M12 ratio. A similar approach would be implemented for detecting subpixel saturation in M11.