Diurnal Variability Analysis for GHRSST products Chris Merchant and DVWG.

Slides:



Advertisements
Similar presentations
Sst_cci Chris Merchant The University of Edinburgh.
Advertisements

Land Surface Evaporation 1. Key research issues 2. What we learnt from OASIS 3. Land surface evaporation using remote sensing 4. Data requirements Helen.
L4 SST analysis of Diurnal cycle J. Tournadre, J.F. Piollé, E. Autret IFREMER, Laboratoire d’Océanographie Spatiale.
WMOIOC 1 OOPC-XII, Paris, 2-5 May 2007 DBCP issues for OOPC Boram Lee IOC Secretariat for JCOMM.
1 st Joint GOSUD/SAMOS Workshop The Florida State University 1 Sensitivity of Surface Turbulent Fluxes to Observational Errors  or.
GIST 24/10/06 Jeff Settle, ESSC Reconciling Point and Area Data for RADAGAST GIST 24 October 2006.
1988. Station ALOHA (~4750m deep) Hawaii Ocean Time-series (HOT) October present (260 cruises; ~10/yr) 25 years of HOT.
Initialization Issues of Coupled Ocean-atmosphere Prediction System Climate and Environment System Research Center Seoul National University, Korea In-Sik.
Air-sea heat fluxes in the stratocumulus deck / cold tongue / ITCZ complex of the eastern tropical Pacific Meghan F. Cronin (NOAA PMEL) Chris Fairall (NOAA.
THE PHYSICAL BASIS OF SST MEASUREMENTS Diurnal Warming 1.Continue/expand research into development of diurnal warming models and analysis of satellite.
1 Variability of sea surface temperature diurnal warming Carol Anne Clayson Florida State University Geophysical Fluid Dynamics Institute SSTST Meeting.
Aquarius/SAC-D Mission Validation Working Group Summary Gary Lagerloef 6 th Science Meeting; Seattle, WA, USA July 2010.
Statistics, data, and deterministic models NRCSE.
November 9, 2010 Diurnal Warming and Associated Uncertainties Gary A. Wick NOAA ESRL/PSD New Chair, GHRSST DVWG.
Statistics, data, and deterministic models NRCSE.
Observational study of the transition from unbroken marine boundary layer stratocumulus to the shallow cumulus regime Irina Sandu and Bjorn Stevens Max-Planck-Institut.
© Imperial College LondonPage 1 Quantifying the direct radiative effect of Saharan dust aerosol over north-west Africa and the tropical Atlantic Richard.
Exploring strategies for coupled 4D-Var data assimilation using an idealised atmosphere-ocean model Polly Smith, Alison Fowler & Amos Lawless School of.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 NOAA Operational Geostationary Sea Surface Temperature Products from NOAA.
Improved NCEP SST Analysis
NATS 101 Lecture 25 Weather Forecasting I. Review: ET Cyclones Ingredients for Intensification Strong Temperature Contrast Jet Stream Overhead S/W Trough.
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.
Coupled Data Assimilation Keith Haines: NCEO Work Meeting Feb19th 2013 Aim: To establish coupled Atmosphere-Ocean assimilation system at ECMWF and demonstrate.
SST Diurnal Cycle over the Western Hemisphere: Preliminary Results from the New High-Resolution MPM Analysis Wanqiu Wang, Pingping Xie, and Chenjie Huang.
Assessment of one year of Medspiration L4 fields J. Tournadre, J.F. Piollé and E. Autret.
Satellite SST in Coupled Data Assimilation Chris Old and Chris Merchant School of GeoSciences, The University of Edinburgh ESA Data Assimilation Projects,
ECMWF Summer Seminars September Task 3: Management Activities Orial Kryeziu recruited started June 18 th September coupled DA workshop Chris Old.
The Activities of Andrea Kaiser-Weiss GHRSST Project Officer, based at NCEO, University of Reading, UK.
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)]
Dataset Development within the Surface Processes Group David I. Berry and Elizabeth C. Kent.
Analyzed Data Products Available from NCAR that Support Marine Climate Research JCOMM ETMC-III 9-12 February 2010 Steven Worley Doug Schuster.
Ocean Surface Winds Research Summary: Meteorological Applications Mark DeMaria, NOAA/NESDIS, Fort Collins, CO Ocean Surface Winds Workshop NCEP/Tropical.
Ocean Surface heat fluxes Lisan Yu and Robert Weller
Chelle L. Gentemann & Peter J. Minnett Introduction to the upper ocean thermal structure Diurnal models M-AERI data Examples of diurnal warming Conclusions.
ICDC7, Boulder September 2005 Estimation of atmospheric CO 2 from AIRS infrared satellite radiances in the ECMWF data assimilation system Richard.
Ocean Surface heat fluxes
Eileen Maturi 1, Jo Murray 2, Andy Harris 3, Paul Fieguth 4, John Sapper 1 1 NOAA/NESDIS, U.S.A., 2 Rutherford Appleton Laboratory, U.K., 3 University.
AQUA AMSR-E MODIS POES AVHRR TRMM TMI ENVISAT AATSR GOES Imager Multi-sensor Improved SST (MISST) for GODAE Part I: Chelle Gentemann, Gary Wick Part II:
Infrared and Microwave Remote Sensing of Sea Surface Temperature Gary A. Wick NOAA Environmental Technology Laboratory January 14, 2004.
SPURS Synthesis Research Objectives: Budget calculations Resolve important terms of the freshwater and heat budgets of the upper 1000 m on temporal scales.
AQUA AMSR-E MODIS POES AVHRR TRMM TMI ENVISAT AATSR GOES Imager Multi-sensor Improved SST (MISST) for GODAE Part I: Chelle Gentemann, Gary Wick Part II:
Report from the Australian Regional Data Assembly Centre Helen Beggs 1, Leon Majewski 2 and Justin Freeman 1 1 Centre for Australian Weather and Climate.
Chelle L. Gentemann Peter J. Minnett Brian Ward Refinement of bulk model M-AERI data Observed diurnal warming Conclusions Profile of Ocean Surface Heating:
Testing of the Zeng and Beljaars scheme in the TWP Michael Brunke and Xubin Zeng Department of Atmospheric Sciences The University of Arizona Tucson, Arizona.
Diurnal Variability Working Group: GHRSST-10 Breakout Session Report Chris Merchant Gary Wick.
Multi-sensor Improved SST (MISST) for GODAE : A US contribution to GHRSST-PP Research, Data, and Impacts.
Use of high resolution global SST data in operational analysis and assimilation systems at the UK Met Office. Matt Martin, John Stark,
Towards the utilization of GHRSST data for improving estimates of the global ocean circulation Dimitris Menemenlis 1, Hong Zhang 1, Gael Forget 2, Patrick.
New Australian High Resolution AVHRR SST Products from the Integrated Marine Observing System Presented at the GHRSST Users Symposium, Santa Rosa, USA,
L3 PLB May L2 Pre-ProcessedL3 Pre processedL3 (collated)Analysed SST AcronymL2PL3PL3L4 DescriptionNative SST data streams reformatted into netCDF.
Summary of the GHRSST Joint Workshop Melbourne discussion on the Argo near- surface temperature measurements Andrea Kaiser-Weiss, Gary Wick, Carol-Anne.
GHRSST 10: Report from Diurnal Variability Working Group Report on activities of the Diurnal Variability Working Group Chris Merchant University of Edinburgh.
May 28-29, 2009GHRSST 2009 International Users Symposium National Oceanic and Atmospheric Administration Group for High Resolution Sea Surface Temperature.
Validation of MTSAT-1R SST for the TWP+ Experiment Leon Majewski 1, Jon Mittaz 2, George Kruger 1,3, Helen Beggs 3, Andy Harris 2, Sandra Castro 4 1 Observations.
Calculation of Sea Surface Temperature Forward Radiative Transfer Model Approach Alec Bogdanoff, Florida State University Carol Anne Clayson and Brent.
The development of the NSST within the NCEP GFS/CFS
EXTREME WINDS AND PRECIPITATION FROM SPACE
The impact of Argo data on ocean and climate forecasting
ENSO Frequency Cascade and Implications for Predictability
A Comparison of Profiling Float and XBT Representations of Upper Layer Temperature Structure of the Northwestern Subtropical North Atlantic Robert L.
GlobColour: New/Future products
Coastal CO2 fluxes from satellite ocean color, SST and winds
Panel: Bill Large, Bob Weller, Tim Liu, Huug Van den Dool, Glenn White
Rob Wood, University of Washington POST Meeting, February, 2009
Nicolas Reul1, Joseph Tenerelli2
Precipitation variability over Arizona and
D1 D2 D3 D4 Figure 2 Initial sea-surface temperature (SST, color) and ocean heat content (OHC, contour) fields for the coupled model simulation of Hurricane.
Rob Wood, University of Washington POST Meeting, February, 2009
Integrated Satellite Global Energy Data for Climate Studies
Presentation transcript:

Diurnal Variability Analysis for GHRSST products Chris Merchant and DVWG

Mean ocean diurnal-warming cycles

Importance of diurnal cycle in SST Diurnal cycle in air-sea interaction Affects the mean air-sea interaction Source of variability in satellite skin SSTs “Error” in satellite SSTs as estimates of SST depth –Deleterious to SST analyses –Complicates inter-sensor comparison, validation –Affects climate analysis of SST Need a DSST & eDSST estimate in L2P

Diurnal Variability Working Group

DV analysis: Spatially complete blend of diurnal warming estimated from temporal evolution of observed SST from model-based knowledge appropriately combined to give estimated subdaily time evolution of skin/subskin/buoy-depth SST

Experimental DVAs Data driven (SST differences, day-night) Analyses differences (skin-foundation) Blending of NWP-driven model and data

Based on SEVIRI SSTs + data driven analysis Cloudy areas set to zero diurnal warming 1 May 2006

Empirical model (Mark Filipiak poster in GHRSST10) Driven by NWP fluxes and winds (ECMWF)

Blending experiment Blend obs and model at 1400h LT (only) Blending done by adjusting the NWP fields to bring model DSST towards observed where available Then use model to propagate observations in time – validate

Blending Maximum wind since t 0, w max Integrated surface heating since t 0,, Qint DSST contours at 14h 1 K 2 K Example: Observed DSST = 2 K +/- 0.5 K Model DSST = 1 K Estimated errors in Qint and w max

Propagating in space and time At 1400h, the NWP increments are propagated into unobserved areas using assumed length scales For hours before and after 1400h, the NWP is also incremented to be consistent

Estimates of DSST field before and after observation time

Statistical improvement cf. SEVIRI data-driven analysis. Obs. from 14h only are used in blending SD(M-O) / KCorrelation HourModelBlendedModelBlended

Summary and feedback DVWG pursuing experiments in DVA Aim: “DVACs” providing NRT time- resolved (~hourly) analysis/forecast of diurnal warming for L2P providers Comments on this aim?