Directions for SST estimation activities Chris Merchant.

Slides:



Advertisements
Similar presentations
Robin Hogan, Richard Allan, Nicky Chalmers, Thorwald Stein, Julien Delanoë University of Reading How accurate are the radiative properties of ice clouds.
Advertisements

Design of Experiments Lecture I
Pathfinder –> MODIS -> VIIRS Evolution of a CDR Robert Evans, Peter Minnett, Guillermo Podesta Kay Kilpatrick (retired), Sue Walsh, Vicki Halliwell, Liz.
ASII-NG: Developments and outlook NWCSAF 2015 Users Workshop.
An optimal estimation based retrieval method adapted to SEVIRI infra-red measurements M. Stengel (1), R. Bennartz (2), J. Schulz (3), A. Walther (2,4),
6-1 Introduction To Empirical Models 6-1 Introduction To Empirical Models.
Satellite SST Radiance Assimilation and SST Data Impacts James Cummings Naval Research Laboratory Monterey, CA Sea Surface Temperature Science.
Chapter 10 Simple Regression.
Xin Kong, Lizzie Noyes, Gary Corlett, John Remedios, Simon Good and David Llewellyn-Jones Earth Observation Science, Space Research Centre, University.
Retrieval Theory Mar 23, 2008 Vijay Natraj. The Inverse Modeling Problem Optimize values of an ensemble of variables (state vector x ) using observations:
GOES-13 Science Team Report SST Images and Analyses Eileen Maturi, STAR/SOCD, Camp Springs, MD Andy Harris, CICS, University of Maryland, MD Chris Merchant,
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 NOAA Operational Geostationary Sea Surface Temperature Products from NOAA.
1 NOAA’s National Climatic Data Center April 2005 Climate Observation Program Blended SST Analysis Changes and Implications for the Buoy Network 1.Plans.
Improved NCEP SST Analysis
NASA MODIS-VIIRS ST Meeting, May 18 – 22, A Deterministic Inverse Method for SST Retrieval from VIIRS: Early Results Andy Harris, Prabhat Koner.
Climate quality data and datasets from VOS and VOSClim Elizabeth Kent and David Berry National Oceanography Centre, Southampton.
Arctic SST retrieval in the CCI project Owen Embury Chris Merchant University of Reading.
EE513 Audio Signals and Systems Statistical Pattern Classification Kevin D. Donohue Electrical and Computer Engineering University of Kentucky.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 CLOUD MASK AND QUALITY CONTROL FOR SST WITHIN THE ADVANCED CLEAR SKY PROCESSOR.
Applications and Limitations of Satellite Data Professor Ming-Dah Chou January 3, 2005 Department of Atmospheric Sciences National Taiwan University.
1 Detection and Determination of Channel Frequency Shift in AMSU-A Observations Cheng-Zhi Zou and Wenhui Wang IGARSS 2011, Vancouver, Canada, July 24-28,
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 MAP (Maximum A Posteriori) x is reduced state vector [SST(x), TCWV(w)]
ECE 8443 – Pattern Recognition ECE 8423 – Adaptive Signal Processing Objectives: Deterministic vs. Random Maximum A Posteriori Maximum Likelihood Minimum.
A physical basis of GOES SST retrieval Prabhat Koner Andy Harris Jon Mittaz Eileen Maturi.
Rutherford Appleton Laboratory Requirements Consolidation of the Near-Infrared Channel of the GMES-Sentinel-5 UVNS Instrument: FP, 25 April 2014, ESTEC.
Satellite-derived Sea Surface Temperatures Corey Farley Remote Sensing May 8, 2002.
PROBABILITY AND STATISTICS FOR ENGINEERING Hossein Sameti Department of Computer Engineering Sharif University of Technology Principles of Parameter Estimation.
Introduction to CMUG assessments, SST and plans for phase 2 Roger Saunders 4 th Integration Meeting.
The Relation Between SST, Clouds, Precipitation and Wave Structures Across the Equatorial Pacific Anita D. Rapp and Chris Kummerow 14 July 2008 AMSR Science.
NASA MODIS-VIIRS ST Meeting, May 18 – 22, New physically based sea surface temperature retrievals for NPP VIIRS Andy Harris, Prabhat Koner CICS,
AIRS Radiance and Geophysical Products: Methodology and Validation Mitch Goldberg, Larry McMillin NOAA/NESDIS Walter Wolf, Lihang Zhou, Yanni Qu and M.
1 RTM/NWP-BASED SST ALGORITHMS FOR VIIRS USING MODIS AS A PROXY B. Petrenko 1,2, A. Ignatov 1, Y. Kihai 1,3, J. Stroup 1,4, X. Liang 1,5 1 NOAA/NESDIS/STAR,
BCS547 Neural Decoding.
Global Modeling and Assimilation Office Goddard Space Flight Center National Aeronautics and Space Administration Recent Advances towards the Assimilation.
REANALYSIS OF SEA ICE CONCENTRATION FROM THE SMMR AND SSM/I RECORDS Søren Andersen, Lars-Anders Breivik, Mary J. Brodzik, Craig Donlon, Steinar Eastwood,
An Introduction to Optimal Estimation Theory Chris O´Dell AT652 Fall 2013.
Estimation of Random Variables Two types of estimation: 1) Estimating parameters/statistics of a random variable (or several) from data. 2)Estimating the.
Retrieval Algorithms The derivations for each satellite consist of two steps: 1) cloud detection using a Bayesian Probabilistic Cloud Mask; and 2) application.
Physical retrieval (for MODIS) Andy Harris Jonathan Mittaz Prabhat Koner (Chris Merchant, Pierre LeBorgne)
A step toward operational use of AMSR-E horizontal polarized radiance in JMA global data assimilation system Masahiro Kazumori Numerical Prediction Division.
Infrared and Microwave Remote Sensing of Sea Surface Temperature Gary A. Wick NOAA Environmental Technology Laboratory January 14, 2004.
NOAA Environmental Technology Laboratory Gary A. Wick Observed Differences Between Infrared and Microwave Products Detailed comparisons between infrared.
ESTIMATION METHODS We know how to calculate confidence intervals for estimates of  and  2 Now, we need procedures to calculate  and  2, themselves.
AVHRR Radiance Bias Correction Andy Harris, Jonathan Mittaz NOAA Cooperative Institute for Climate Studies University of Maryland Some concepts and some.
November 28, 2006 Derivation and Evaluation of Multi- Sensor SST Error Characteristics Gary Wick 1 and Sandra Castro 2 1 NOAA Earth System Research Laboratory.
One-dimensional assimilation method for the humidity estimation with the wind profiling radar data using the MSM forecast as the first guess Jun-ichi Furumoto,
A New Ocean Suite Algorithm for AMSR2 David I. Duncan September 16 th, 2015 AMSR Science Team Meeting Huntsville, AL.
Digital Communications I: Modulation and Coding Course Spring Jeffrey N. Denenberg Lecture 3c: Signal Detection in AWGN.
© 2014 RAL Space Study for the joint use of IASI, AMSU and MHS for OEM retrievals of temperature, humidity and ozone D. Gerber 1, R. Siddans 1, T. Hultberg.
International GHRSST User Symposium Santa Rosa, California, USA 28-29th May 2009 MODIS Sea-Surface Temperatures Peter J Minnett & Robert H. Evans With.
EARWiG: SST retrieval issues for High Latitudes Andy Harris Jonathan Mittaz NOAA-CICS University of Maryland Chris Merchant U Edinburgh.
EARWiG: SST retrieval issues for TWP Andy Harris Jonathan Mittaz Prabhat Koner NOAA-CICS University of Maryland Eileen Maturi NOAA/NESDIS, Camp Springs,
Uncertainty estimation from first principles: The future of SSES? Gary Corlett (University of Leicester) Chris Merchant (University of Edinburgh)
Alternative forms of the atmospheric correction algorithms (at high latitudes) GHRSST Workshop University of Colorado Feb 28-March 2, 2011 Peter J Minnett.
Recommendations to GSICS from international working groups GSICS meeting, March 2015, New Delhi, India Rob Roebeling.
New Australian High Resolution AVHRR SST Products from the Integrated Marine Observing System Presented at the GHRSST Users Symposium, Santa Rosa, USA,
June 20, 2005Workshop on Chemical data assimilation and data needs Data Assimilation Methods Experience from operational meteorological assimilation John.
ATSR Re-analysis for Climate (ARC) Chris Merchant The University of Edinburgh.
ESTIMATION METHODS We know how to calculate confidence intervals for estimates of  and 2 Now, we need procedures to calculate  and 2 , themselves.
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course
SPLIT-WINDOW TECHNIQUE
Joint GRWG and GDWG Meeting February 2010, Toulouse, France
Probability Theory and Parameter Estimation I
Ch3: Model Building through Regression
M. J. Burgdorf, S. A. Buehler, I. Hans
The SST CCI: Scientific Approaches
Sea Surface Temperature, Forward Modeling,
EE513 Audio Signals and Systems
ESTIMATION METHODS We know how to calculate confidence intervals for estimates of  and 2 Now, we need procedures to calculate  and 2 , themselves.
Probabilistic Surrogate Models
Presentation transcript:

Directions for SST estimation activities Chris Merchant

A typology of estimation techniques Empirical regression to buoys Optimal estimation of SST & atmosph. Regression to RT modelling Joint estimation of SST-WV- cloud-aerosol? Empirical screening thresholds Probabilistic / dynamic RT RT-based screening thresholds Retrieval Cloud detection

Need to make progress Current coefficient-based retrievals have “features” that are not widely appreciated (NLSST)

NLSST 3 channel Same observations, two different retrievals

Optimal estimation Calculation local coefficients “on the fly” Based on –Local atmospheric state –Physics of radiative transfer What should OE give us? –Minimized random retrieval error –No regional biases related to coefficients –Reduced sensitivity to water vapour –New and powerful metric of retrieval quality But, potentially can introduce different biases

Potential of optimal estimation techniques: Metop-A study Showed that potential benefits of OE can largely be obtained in practice

Two main estimators Maximum a posteriori – MAP –Minimizes SST error variance –Explicitly embeds prior information in result –But may attenuate frontal gradients etc –Probably appropriate for NWP, oceanography Maximum likelihood – ML –Minimizes BT residuals, SST is noisier –“Zero” prior influence in result –Preserves frontal gradients, diurnal variability etc –The only type of SST that should be used in climate re-analyses (if you are a purist) or frontal studies

Reduced SST single-pixel error Operational NLSST Error= 0.47 K MAP split window Error= 0.39 K

Cost: powerful quality indicator MAP errors by confidence level CL 5 (44%) / CL 4 (36%) / CL 3 (19%) / MAP errors by cost Lowest 44% / Next 36% / Poorest 19% /- 0.53

Satellite Radiances Satellite Radiances Satellite Radiances SSTs Operational analysis Re-analysis Value-added service Users Exploiting system of sensors: referencing, bias adjustment

Retrieved SST in some region Biasing factor System-adjusted SST Use differential sensitivity and or auxiliary observations to detect & do mutual correction SSTs of three different sensors Exploiting the system of sensors to reduce biases at source: (1) Learn better how to exploit “reference” sensors (2) Move beyond privileging one reference, mutual correction

Conclusion There is plenty for an Estimation WG to do, some at a pretty fundamental level –Didn’t mention Marginal Ice Zone, MW-IR differences, cloud-related biases, aerosols … –Open questions on OE: spatial correlations of water vapour, state vector elements, forward model errors … Exploiting the system is a big new challenge