AMSR-E RFI Update - Towards RFI Adaptive Algorithms 1.0

Slides:



Advertisements
Similar presentations
F. Wentz, T. Meissner, J. Scott and K. Hilburn Remote Sensing Systems 2014 Aquarius / SAC-D Science Team Meeting November ,
Advertisements

Atmospheric Correction Algorithm for the GOCI Jae Hyun Ahn* Joo-Hyung Ryu* Young Jae Park* Yu-Hwan Ahn* Im Sang Oh** Korea Ocean Research & Development.
1 © ACRI-ST, all rights reserved – 2012 TEC estimation Jean-Luc Vergely (ACRI-ST) Jacqueline Boutin (LOCEAN)
GCOM/AMSR2 status Earth Observation Research Center and GCOM Project Team Japan Aerospace Exploration Agency AMSR-E Joint Science Team Meeting Huntsville,
REMOTE SENSING OF SOUTHERN OCEAN AIR-SEA CO 2 FLUXES A.J. Vander Woude Pete Strutton and Burke Hales.
Aquarius Status Salinity Retrieval and Applications D. M. Le Vine NASA/GSFC, Greenbelt, MD E. P. Dinnat, G. Lagerloef, P. de Matthaeis, H. Kao, F.
The Aquarius Salinity Retrieval Algorithm Frank J. Wentz and Thomas Meissner, Remote Sensing Systems Gary S. Lagerloef, Earth and Space Research David.
Passive Measurements of Rain Rate in Hurricanes Ruba A.Amarin CFRSL December 10, 2005.
Maintaining and Improving the AMSR-E and WindSat Ocean Products Frank J. Wentz Remote Sensing Systems, Santa Rosa CA AMSR TIM Agenda 4-5 September 2013.
Sea water dielectric constant, temperature and remote sensing of Sea Surface Salinity E. P. Dinnat 1,2, D. M. Le Vine 1, J. Boutin 3, X. Yin 3, 1 Cryospheric.
NRL09/21/2004_Davis.1 GOES-R HES-CW Atmospheric Correction Curtiss O. Davis Code 7203 Naval Research Laboratory Washington, DC 20375
Aquarius/SAC-D Mission Mission Simulators - Gary Lagerloef 6 th Science Meeting; Seattle, WA, USA July 2010.
Analysis and Mitigation of Atmospheric Crosstalk Kyle Hilburn Remote Sensing Systems May 21, 2015.
Monthly Composites of Sea Surface Temperature and Ocean Chlorophyll Concentrations These maps were created by Jennifer Bosch by averaging all the data.
MWR Algorithms (Wentz): Provide and validate wind, rain and sea ice [TBD] retrieval algorithms for MWR data Between now and launch (April 2011) 1. In-orbit.
1 Improved Sea Surface Temperature (SST) Analyses for Climate NOAA’s National Climatic Data Center Asheville, NC Thomas M. Smith Richard W. Reynolds Kenneth.
Offline Assessment of NESDIS OSCAT data Li Bi 1 Sid Boukabara 2 1 RTI/STAR/JCSDA 2 STAR/JCSDA American Meteorological Society 94 th Annual Meeting 02/06/2014.
Recent activities on utilization of microwave imager data in the JMA NWP system - Preparation for AMSR2 data assimilation - Masahiro Kazumori Japan Meteorological.
MWR Roughness Correction Algorithm for the Aquarius SSS Retrieval W. Linwood Jones, Yazan Hejazin, Salem Al-Nimri Central Florida Remote Sensing Lab University.
Jason-1 QuikScat Principal Investigator Gary Lagerloef Earth and Space Research, Seattle NOAA/NESDIS Pilot Project: An Operational Data Center for Satellite-Derived.
September 4 -5, 2013Dawn Conway, AMSR-E / AMSR2 TLSCF Lead Software Engineer AMSR-E / AMSR2 Team Leader Science Computing Facility Current Science Software.
Current status of AMSR-E data utilization in JMA/NWP Masahiro KAZUMORI Numerical Prediction Division Japan Meteorological Agency July 2008 Joint.
Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA.
SCIENCE PROCESSING OVERVIEW David Le Vine Aquarius Deputy PI 07 July 2009.
25 June 2009 Dawn Conway, AMSR-E TLSCF Lead Software Engineer AMSR-E Team Leader Science Computing Facility.
SMOS L2 Ocean Salinity Level 2 Ocean Salinity L2OS planning 2 July 2014 ARGANS & SMOS L2OS ESL 1.
Optimization of L-band sea surface emissivity models deduced from SMOS data X. Yin (1), J. Boutin (1), N. Martin (1), P. Spurgeon (2) (1) LOCEAN, Paris,
ESTIMATION OF OCEAN CURRENT VELOCITY IN COASTAL AREA USING RADARSAT-1 SAR IMAGES AND HF-RADAR DATA Moon-Kyung Kang 1, Hoonyol Lee 2, Chan-Su Yang 3, Wang-Jung.
Applications of Satellite Derived
First Tropical Cyclone Overflights by the Hurricane Imaging Radiometer (HIRAD) Chris Ruf 1, Sayak Biswas 2, Mark James 3, Linwood Jones 2, Tim Miller 3.
USE OF AIRS/AMSU DATA FOR WEATHER AND CLIMATE RESEARCH Joel Susskind University of Maryland May 12, 2005.
The New Geophysical Model Function for QuikSCAT: Implementation and Validation Outline: GMF methodology GMF methodology New QSCAT wind speed and direction.
Cal/Val Discussion. Summary No large errors in rain, freshening observed by Aquarius can be significant and real (up to about 3 hours on average after.
A New Inter-Comparison of Three Global Monthly SSM/I Precipitation Datasets Matt Sapiano, Phil Arkin and Tom Smith Earth Systems Science Interdisciplinary.
SMOS QWG-9, ESRIN October 2012 L2OS: Product performance summary v550 highlights 1 The SMOS L2 OS Team.
Finalizing the AMSR-E Rainfall Algorithm GPROF2010 AMSR-E Science Team Meeting Oxnard, CA 4-5 September, 2013 Dave Randel Colorado State University.
AMSR-E Ocean Rainfall Algorithm Status AMSR-E Science Team Meeting Asheville, NC June, 2011 C. Kummerow Colorado State University.
2006 IHC – Mobile, Alabama 20 – 24 March 2006 JHT Project: Operational SFMR- NAWIPS Airborne Processing and Data Distribution Products OUTLINE JHT Project.
An evaluation of a hybrid satellite and NWP- based turbulent fluxes with TAO buoys ChuanLi Jiang, Kathryn A. Kelly, and LuAnne Thompson University of Washington.
T. Meissner and F. Wentz Remote Sensing Systems 2014 Aquarius / SAC-D Science Team Meeting November , 2014 Seattle. Washington,
AMSR Bias Busting Find, Beat, Repeat, Report
Retrieval Algorithms The derivations for each satellite consist of two steps: 1) cloud detection using a Bayesian Probabilistic Cloud Mask; and 2) application.
Satellites Storm “Since the early 1960s, virtually all areas of the atmospheric sciences have been revolutionized by the development and application of.
Geophysical Ocean Products from AMSR-E & WindSAT Chelle L. Gentemann, Frank Wentz, Thomas Meissner, Kyle Hilburn, Deborah Smith, and Marty Brewer
A step toward operational use of AMSR-E horizontal polarized radiance in JMA global data assimilation system Masahiro Kazumori Numerical Prediction Division.
Social Studies Vocabulary Words August 30, th period 7/8 Subject: Maps.
SMOS Science Meeting September 2011 Arles, FR Simulating Aquarius by Resampling SMOS Gary Lagerloef, Yann Kerr & Eric Anterrieu and Initial Results.
Errors on SMOS retrieved SSS and their dependency to a priori wind speed X. Yin 1, J. Boutin 1, J. Vergely 2, P. Spurgeon 3, and F. Gaillard 4 1. LOCEAN.
September 11-12, 2012Dawn Conway, AMSR-E TLSCF Lead Software Engineer AMSR-E Team Leader Science Computing Facility New Browse Images Current Science Software.
Tests on V500 Sun On versus Sun Off 1)Tbmeas. –Tbmodel in the FOV X. Yin, J. Boutin Inputs from R. Balague, P. Spurgeon, A. Chuprin, M. Martin-Neira and.
AIRS Land Surface Temperature and Emissivity Validation Bob Knuteson Hank Revercomb, Dave Tobin, Ken Vinson, Chia Lee University of Wisconsin-Madison Space.
AMSR-E and WindSAT Version 7 Microwave SSTs C. Gentemann, F. Wentz, T. Meissner, & L.Riccardulli Remote Sensing Systems NASA SST ST October.
Satellite Derived Ocean Surface Vector Winds Joe Sienkiewicz, NOAA/NWS Ocean Prediction Center Zorana Jelenak, UCAR/NOAA NESDIS.
AQUA AMSR-E MODIS POES AVHRR TRMM TMI ENVISAT AATSR Multi-satellite, multi-sensor data fusion: global daily 9 km SSTs from MODIS, AMSR-E, and TMI
Year 6 Science EARTH, SUN and MOON.
A comparison of AMSR-E and AATSR SST time-series A preliminary investigation into the effects of using cloud-cleared SST data as opposed to all-sky SST.
Spaceborne Polarimetric Microwave Radiometer Brandon Ravenscroft
(2) Norut, Tromsø, Norway Improved measurement of sea surface velocity from synthetic aperture radar Morten Wergeland Hansen.
Blending multiple-source wind data including SMOS, SMAP and AMSR-2 new products Joe TENERELLI, Fabrice COLLARD OceanDataLab, Brest, France.
NASA’s Ocean Color Online Visualization and Analysis System
Passive Microwave Radiometer constellation for Sea Surface Temperature Prepared by CEOS Sea Surface Temperature Virtual Constellation (SST-VC) Presented.
NASA’s Ocean Color Online Visualization and Analysis System
Extreme Wind Speed Measurements from NASA’s SMAP L-Band Radiometer
Geostationary RFI in AMSR-E
Aquarius SSS space/time biases with respect to Argo data
‘Aquarius’ Maps Ocean Salinity Fine-scale Structure
AMSR-E Ocean Rainfall Algorithm Status
Soil Moisture Active Passive (SMAP) Satellite
Get final-look Atlas/Ardizzone wind product.
A Hydrologically-Consistent Multi-Satellite Climatology of Evaporation, Precipitation, and Water Vapor Transport Over the Oceans Project team: Frank Wentz.
Presentation transcript:

AMSR-E RFI Update - Towards RFI 2.0 - Adaptive Algorithms 1.0 Marty Brewer and Kyle Hilburn Frank, Carl, Chelle, et. al. Remote Sensing Systems AMSR Science Team Meeting Portland, Oregon, 2012.Sep.11-12

RFI Surface Based (~7GHz) GeoStationary Satellites (11GHz, 18GHz) Ascension Island, Hawaii, Netherlands, etc. GeoStationary Satellites (11GHz, 18GHz) “Space Based” “Ocean Reflected”

RFI RFI 1.0 RFI 2.0 We know where it’s coming from. We can filter it. We don’t really know where it’s coming from. We can retrieve around it.

Fishing for Geostationary RFI Data used: AMSR-E, March-September 2011 (7 months) RFI is very much a moving target Calculated the longitude and latitude where the reflection of the boresight vector from the surface crosses geostationary altitude (35,786 km) For this analysis: histograms of geostationary crossing longitude at 0.1 deg resolution maps of fraction of observations affected by RFI RFI defined as: SST or Wind diff > threshold 4 different thresholds (1, 3, 6, and 9 K or m/s) Required geostationary latitude to be within +/- 5 deg of equator Removed: land, ice, rain, sun glitter; used both asc/dsc passes

AMSR-E Ocean Products 6.9 10.65 18.7 23.8 36.5 SST Very Low X SST Low Res

AMSR-E Ocean Products 6.9 10.65 18.7 23.8 36.5 SST Very Low X SST Low Res Wind Low Res Wind Med Res

SST: LO-VL

SST LO-VL > 1 K (Weak RFI) Smooth Seas (wind speeds < 7 m/s) Glassy Seas (wind speeds < 3 m/s)

SST LO-VL > 3 K (Medium RFI) Smooth Seas (wind speeds < 7 m/s) Glassy Seas (wind speeds < 3 m/s)

SST LO-VL > 6 K (Strong RFI) Smooth Seas (wind speeds < 7 m/s) Glassy Seas (wind speeds < 3 m/s)

SST LO-VL > 9 K (V.Strong RFI) Smooth Seas (wind speeds < 7 m/s) Glassy Seas (wind speeds < 3 m/s)

Wind: MD-LO

Wind MD-LO > 1 m/s (Weak RFI) Smooth Seas (wind speeds < 7 m/s) Glassy Seas (wind speeds < 3 m/s)

Wind MD-LO > 3 m/s (Medium RFI) Smooth Seas (wind speeds < 7 m/s) Glassy Seas (wind speeds < 3 m/s)

Wind MD-LO > 6 m/s (Strong RFI) Smooth Seas (wind speeds < 7 m/s) Glassy Seas (wind speeds < 3 m/s)

Wind MD-LO > 9 m/s (V.Strong RFI) Smooth Seas (wind speeds < 7 m/s) Glassy Seas (wind speeds < 3 m/s)

Geostationary Fishing Results The analysis finds good agreement between geostationary longitude histogram peaks and the longitudes of: HotBird (13.0°) Astra (19.2°) Astra (28.2°) EutelsatW2A (10.0°) Presence of land can give peaks off the nominal longitudes AtlanticBird4 (352.8°) peak is 5-10° west of nominal longitude For 18.7 GHz RFI: DirectTV peaks are about 10° west and east of the nominal longitudes (257.2° and 260.8°)

Geostationary Fishing 2.0 Assume GeoStat Sats are equatiorial Look at latitudes as well as longitudes Geostationary Altitude Sky Maps

SST: LO-VL

SST LO-VL > 1 K (Weak RFI) Smooth Seas (wind speeds < 7 m/s)

SST LO-VL > 1 K (Weak RFI) Glassy Seas (wind speeds < 3 m/s)

SST LO-VL > 6 K (Strong RFI) Smooth Seas (wind speeds < 7 m/s)

SST LO-VL > 6 K (Strong RFI) Glassy Seas (wind speeds < 3 m/s)

SST LO-VL > 6 K (Strong RFI) Glassy Seas (wind speeds < 3 m/s)

SST LO-VL > 6 K (Strong RFI) All Seas (all wind speeds)

Wind: MD-LO

Wind MD-LO > 1 m/s (Weak RFI) Smooth Seas (wind speeds < 7 m/s)

Wind MD-LO > 1 m/s (Weak RFI) Glassy Seas (wind speeds < 3 m/s)

Wind MD-LO > 6 m/s (Strong RFI) Smooth Seas (wind speeds < 7 m/s)

Wind MD-LO > 6 m/s (Strong RFI) Glassy Seas (wind speeds < 3 m/s)

Wind MD-LO > 6 m/s (Strong RFI) Glassy Seas (wind speeds < 3 m/s)

Wind MD-LO > 6 m/s (Strong RFI) All Seas (all wind speeds)

Geostationary RFI 1.0 Implemented L2A Version B05 (August, 2005) Glint Angles computed to 13.0° E and 19.2° E (at geostationary altitude) L2A V10 (April, 2009) : 99.2° W and 102.8° W for data after July, 2007

Geostationary RFI 2.0 L2A Proposed New Swath Names: “Geostationary_Altitude_Reflection_Latitude” “Geostationary_Altitude_Reflection_Longitude”

Mitigating the Effect of 11 GHz RFI on AMSR-E SST Retrievals Towards: Adaptive Algorithms 1.0 Mitigating the Effect of 11 GHz RFI on AMSR-E SST Retrievals Kyle, Aug 2012

AMSR-E Ocean Products 6.9 10.65 18.7 23.8 36.5 SST Very Low X SST Low Res SST (-11GHz)

2011, Descending Passes, Standard Algorithm

2011, Descending Passes, 11 GHz RFI Mitigation

2002, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2003, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2004, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2005, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2006, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2007, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2008, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2009, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2010, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2011, Descending Passes Standard Algorithm 11 GHz RFI Mitigation Color = Standard Deviation of AMSR-E – Reynolds SST

2011, Ascending Passes Standard Algorithm 11 GHz RFI Mitigation 7GHz Ground-based RFI 7GHz Ground-based RFI Color = Standard Deviation of AMSR-E – Reynolds SST

2011, Descending Passes, Standard Algorithm

2011, Descending Passes, 11 GHz RFI Mitigation

Geostationary RFI 2.0 ~or~ L2A Proposed New Swath Names: “Geostationary_Reflection_Latitude” “Geostationary_Reflection_Longitude” ~or~ “Geostationary_Altitude_Reflection_Latitude” “Geostationary_Altitude_Reflection_Longitude”

Arigato Gozia Mas - Towards RFI 2.0 - Adaptive Algorithms 1.0 Marty Brewer and Kyle Hilburn Frank, Carl, Chelle, et. al. Remote Sensing Systems AMSR Science Team Meeting Portland, Oregon, 2012.Sep.11-12