Frank Wentz and Carl Mears Remote Sensing Systems, Santa Rosa CA, USA

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

Development and validation of a capability for wide-swath storm observations of ocean surface wind speed Timothy L. Miller 1 M.
Communicating Uncertainties for Microwave-Based ESDRs Frank J. Wentz, Carl A. Mears, and Deborah K. Smith Remote Sensing Systems, Santa Rosa CA Supported.
The Aquarius Salinity Retrieval Algorithm Frank J. Wentz and Thomas Meissner, Remote Sensing Systems Gary S. Lagerloef, Earth and Space Research David.
1 Analysis of Airborne Microwave Polarimetric Radiometer Measurements in the Presence of Dynamic Platform Attitude Errors Jean Yves Kabore Central Florida.
All-Weather Wind Vector Measurements from Intercalibrated Active and Passive Microwave Satellite Sensors Thomas Meissner Lucrezia Ricciardulli Frank Wentz.
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.
Cold Sky Calibration Aquarius: D. M. Le Vine MWR: J. C. Gallo.
Aquarius/SAC-D Mission Mission Simulators - Gary Lagerloef 6 th Science Meeting; Seattle, WA, USA July 2010.
Aquarius/SAC-D Mission Error Validation and Early Orbit Corrections Gary Lagerloef 6 th Science Meeting; Seattle, WA, USA July 2010.
This poster concerns the on-orbit validation of the antenna beam pointing and corresponding instantaneous field of view (IFOV) earth location for the CONAE.
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.
MWR Roughness Correction Algorithm for the Aquarius SSS Retrieval W. Linwood Jones, Yazan Hejazin, Salem Al-Nimri Central Florida Remote Sensing Lab University.
EECS 823 MACHARIA.  Four-frequency, linearly-polarized, passive microwave radiometric system which measures atmospheric, ocean and terrain microwave.
Jet Propulsion Laboratory California Institute of Technology QuikScat Retrieving Ocean Surface Wind Speeds from the Nonspinning QuikSCAT Scatterometer.
Thaddeus Johnson and Torie Hadel
Diagnosing Climate Change from Satellite Sounding Measurements – From Filter Radiometers to Spectrometers William L. Smith Sr 1,2., Elisabeth Weisz 1,
Yimin Ji - Page 1 October 5, 2010 Global Precipitation Measurement (GPM) mission Precipitation Processing System (PPS) Yimin Ji NASA/GSFC,
Evaluation of Microwave Scatterometers and Radiometers as Satellite Anemometers Frank J. Wentz, Thomas Meissner, and Deborah Smith Presented at: NOAA/NASA.
Calibration and Validation Studies for Aquarius Salinity Retrieval PI: Shannon Brown Co-Is: Shailen Desai and Anthony Scodary Jet Propulsion Laboratory,
SCIENCE PROCESSING OVERVIEW David Le Vine Aquarius Deputy PI 07 July 2009.
A NON-RAINING 1DVAR RETRIEVAL FOR GMI DAVID DUNCAN JCSDA COLLOQUIUM 7/30/15.
Also known as CMIS R. A. Brown 2005 LIDAR Sedona.
A New Satellite Wind Climatology from QuikSCAT, WindSat, AMSR-E and SSM/I Frank J. Wentz (presenting), Lucrezia Ricciardulli, Thomas Meissner, and Deborah.
Level 2 Algorithm. Definition of Product Levels LevelDescription Level 1 1A Reconstructed unprocessed instrument data 1B Geolocated, calibrated sensor.
Application of in situ Observations to Current Satellite-Derived Sea Surface Temperature Products Gary A. Wick NOAA Earth System Research Laboratory With.
Remote Sensing Systems Climate Satellite Program Frank J. Wentz and Carl Mears Remote Sensing Systems, Santa Rosa, CA Supported in part by : NASA’s Earth.
2011 IEEE International Geoscience And Remote Sensing Symposium IGARSS’11  July 24-29, 2011  Vancouver, C ANADA A synergy between SMOS & AQUARIUS: resampling.
The New Geophysical Model Function for QuikSCAT: Implementation and Validation Outline: GMF methodology GMF methodology New QSCAT wind speed and direction.
AIRS Radiance and Geophysical Products: Methodology and Validation Mitch Goldberg, Larry McMillin NOAA/NESDIS Walter Wolf, Lihang Zhou, Yanni Qu and M.
NPOESS Conical Scanning Microwave Imager/ Sounder (CMIS) Overview
Design Features of a Boresighted GPM Core Radiometer Christopher S. Ruf Dept. of Atmospheric, Oceanic & Space Sciences University of Michigan, Ann Arbor,
Mission Operations Review February 8-10, 2010 Cordoba, ARGENTINA SECTION 16.x Aquarius Science Commissioning and Acceptance Draft 2 Prepared by: Gary Lagerloef,
Ocean Vector Wind Workshops and the Role of Cal/Val in Preparing for Future Satellite Wind Sensors Dudley Chelton Cooperative Institute for Oceanographic.
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
Challenge Volume: Over 100 satellite-years of observations Calibration Each sensor has its own unique set of Sensor Calibration Problems Precision: High.
AMSR-E Vapor and Cloud Validation Atmospheric Water Vapor –In Situ Data Radiosondes –Calibration differences between different radiosonde manufactures.
The Inter-Calibration of AMSR-E with WindSat, F13 SSM/I, and F17 SSM/IS Frank J. Wentz Remote Sensing Systems 1 Presented to the AMSR-E Science Team June.
Geophysical Ocean Products from AMSR-E & WindSAT Chelle L. Gentemann, Frank Wentz, Thomas Meissner, Kyle Hilburn, Deborah Smith, and Marty Brewer
Basis of GV for Japan’s Hydro-Meteorological Process Modelling Research GPM Workshop Sep. 27 to 30, Taipei, Taiwan Toshio Koike, Tobias Graf, Mirza Cyrus.
AVHRR Radiance Bias Correction Andy Harris, Jonathan Mittaz NOAA Cooperative Institute for Climate Studies University of Maryland Some concepts and some.
South Pole North Pole South Pole DD, K CONAE Microwave Radiometer (MWR) Counts to Tb Algorithm and On orbit Validation Zoubair Ghazi 1, Andrea Santos-Garcia.
SMOS Science Meeting September 2011 Arles, FR Simulating Aquarius by Resampling SMOS Gary Lagerloef, Yann Kerr & Eric Anterrieu and Initial Results.
A New Ocean Suite Algorithm for AMSR2 David I. Duncan September 16 th, 2015 AMSR Science Team Meeting Huntsville, AL.
AMSR-E and WindSAT Version 7 Microwave SSTs C. Gentemann, F. Wentz, T. Meissner, & L.Riccardulli Remote Sensing Systems NASA SST ST October.
Radiance Simulation System for OSSE  Objectives  To evaluate the impact of observing system data under the context of numerical weather analysis and.
EARWiG: SST retrieval issues for TWP Andy Harris Jonathan Mittaz Prabhat Koner NOAA-CICS University of Maryland Eileen Maturi NOAA/NESDIS, Camp Springs,
Passive Microwave Remote Sensing
Intercalibration of AMSR2 and PMW radiometers Takashi Maeda(JAXA/EORC), Arata Okuyama (JMA), Kazufumi Kobayashi (RESTEC), Mieko Seki (RESTEC), Keiji Imaoka.
T. Meissner, F. Wentz, J. Scott, K. Hilburn Remote Sensing Systems 2014 Aquarius / SAC-D Science Team Meeting November , 2014.
Spaceborne Polarimetric Microwave Radiometer Brandon Ravenscroft
Ocean Vector Winds in Storms from the SMAP L-Band Radiometer
EXTREME WINDS AND PRECIPITATION FROM SPACE
SOLab work description
Paper under review for JGR-Atmospheres …
Blending multiple-source wind data including SMOS, SMAP and AMSR-2 new products Joe TENERELLI, Fabrice COLLARD OceanDataLab, Brest, France.
In-orbit Microwave Reference Records
GPM Microwave Radiometer Vicarious Cold Calibration
Remote Sensing Systems
CoSMIR Performance during OLYMPEX
Calibration Activities of GCOM-W/AMSR2
Roughness Correction for Aquarius (AQ) Sea Surface Salinity (SSS) Algorithm using MicroWave Radiometer (MWR) W. Linwood Jones, Yazan Hejazin Central FL.
Extreme Wind Speed Measurements from NASA’s SMAP L-Band Radiometer
Validation of CYGNSS winds using microwave scatterometers/radiometers
An Update on the Activities of the Precipitation Measurement Missions (i.e. TRMM/GPM) XCAL Team PMM XCAL Team Wesley Berg, Rachael Kroodsma, Faisal Alquaeid,
Calibration, Validation and Status of OSI SAF ScatSat-1 products
Use of NWP+RTM as inter-calibration tool
Andrew Heidinger JPSS Cloud Team Lead
Presentation transcript:

Frank Wentz and Carl Mears Remote Sensing Systems, Santa Rosa CA, USA Evaluation of COWVR as a Cost-Effective Sensor for Ocean Vector Winds and Other Air-Sea Variables Frank Wentz and Carl Mears Remote Sensing Systems, Santa Rosa CA, USA

Outline What is COWVR What does RSS plan to do with it? The Basics Advantages Risks What does RSS plan to do with it? Adapt the WindSat Analysis Package to COWVR Evaluate COWVR wind vectors relative to WindSat, Scatterometers and moored buoys. Evaluate COWVR wind wpeed relative to conventional radiometers

COWVR (Compact Ocean Wind Vector Radiometer) PI – Shannon Brown, JPL Funder – US Air Force Fully Polarimetric Radiometer at 18.7, 23.8 and 33.9 GHz Single feed horn for all 3 frequencies Only the reflector rotates – the receiver is fixed to the spacecraft – No BAPTA – spinning angular momentum almost 50 times less than WindSat No External Calibration Loads -- Internally Calibrated Using PIN Diodes and correlated noise sources.

Implications of these features: 1. Polarizations are mixed as the reflector rotates But receiver is fully polarimetric, which allows the polarization state to be deduced even when basis is rotated. Technology has been demonstrated in the lab and for airborne radiometers. Requires a close match for the antenna patterns for the various components of the Stokes vector (or at least, a detailed understanding of the differences).

Implications of these features: 2. Lack of External Calibration Targets Allows for an Almost Uninterrupted 360 degree scan. Each location is observed twice at different azimuth angles. This is very good! WindSat had such “2-look” capability for part of the scan. RSS and others have shown that wind vectors are substantially improved by 2 looks.

Implications of these features: 3. Internal calibration sources can be tricky. Radiance may vary slowly over time due to changes in source or PIN diode switches. Need to use innovative cal-val methods to ensure that any such drifts are characterized and removed. Aquarius, SMAP and GMI* all use internal calibration sources. Aquarius had drifts issues, but SMAP is much improved. *GMI has traditional calibration targets too.

Launch + Launch Vehicle Launch was scheduled for July 2018 but is now delayed until ???? Original Launch Plan. “Commercial Rideshare” launch shared with numerous other, mostly smaller satellites COWVR project doesn’t get to choose the exact orbit or launch window, but…. The approach leads to substantial cost savings (25% to 50%) relative to a dedicated launch vehicle.

RSS Activities Related to COWVR Pre-launch Simulations Geolocation Footprint Resampling Calibration Vector Wind Algorithm Vapor, Cloud and Rain Algorithm

Prelaunch Simulation End-to-End Satellite Simulator Environmental Conditions for NWP output Wind, SST, Salinity, Profiles of Temperature, Vapor, Clouds and Rain + Total electron content in the ionosphere. RTM used to calculate top-of-the-atmosphere Tb TB converted to TA using antenna spill-over, cross-pol and geometrical polarization rotation. Noise is added to TA to account for receiver noise Simulated TA is then used to develop and test retrieval algorithms Results from retrievals can be compared to known conditions at the input to evaluate algorithm performance.

Geolocation and Resampling Satellite Location and Attitude used to compute footprint location on ground, as well as incidence angle, sun location, etc. For real COWVR data, the locations of coastlines and similar features can be used to evaluate. Often Antenna Boresights need to be adjusted by a few 10ths of a degree. This can depend on the polarization under study. Footprint Resampling to Common Footprint Optimum interpolation

The RSS Calibration and Retrieval System Validation EP Adjustments (i.e., clear sky bias, high vapor bias) Geophysical Retrievals Automatic Retrieval Algorithm Radiative Transfer Model Simulated Antenna Temperatures Sensor Adjustments Calibration RTM Adjustments Sensor Antenna Temperatures Start with Satellite Radiometer Counts Use same RTM for calibrating all satellites Use RTM-1 for same retrieval algorithm for all satellites

Radiometric Calibration Primary Method is comparison to GMI. GMI is absolutely calibrated (Wentz and Draper, 2016) GMI radiances converted to COWVR radiances using a RTM over the oceans. Receiver linearity can be investigated by adding comparisons over the Amazon rainforest. Needs to be monitored over entire mission to guard against drifts.

Wind Algorithm Adapt our WindSat Algorithm to COWVR Changes include Lack of low frequency channels De-rotating polarizations due to rotating antenna “back look” available for all swath positions – should lead to good direction retrievals Simplified footprint geometry – only one feed horn! Step 1 – Find wind speed using a multistep regression algorithm (The regression is trained using the simulated data) Step 2 – Find direction ambiguities by minimizing sum-of-squares for all channels Step 3– Choose direction ambiguity using median filter method (these are all proven methods for multi-look radiometers)

Wind Validation Compare to: Buoys NWP output CCMP Using binned wind speed differences, binned direction differences, Ebuchi plots, overall means and std. devs.

Vapor, Clouds and Rain Example from GMI These are retrieved simultaneously with wind speed by the multistep regression algorithm. Vapor can be validated via comparison with ground-based GPS results from small islands.

Conclusions We are excited about COWVR It could be a (relatively) low cost way to get ocean vector winds in the future (especially if future COWVR’s include 11 GHz). Low-cost satellites could make it possible to have more satellites operating at same time – better coverage, better assimilation into NWP, possible to study diurnal variability. Two-look capability should produce good direction retrievals than “classic” WindSat products.