ECMWF – 1© European Centre for Medium-Range Weather Forecasts Developments in the use of AMSU-A, ATMS and HIRS data at ECMWF Heather Lawrence, first-year.

Slides:



Advertisements
Similar presentations
GEO Energy Management Meeting WMO, August 2006 Earth Observations and Energy Management Expert Meeting Renate Hagedorn European Centre for Medium-Range.
Advertisements

ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course 1 to 4 July 2013.
Enza Di Tomaso* and Niels Bormann ECMWF *EUMETSAT fellow
© The Aerospace Corporation 2014 Observation Impact on WRF Model Forecast Accuracy over Southwest Asia Michael D. McAtee Environmental Satellite Systems.
Data Assimilation Andrew Collard. Overview Introduction to Atmospheric Data Assimilation Control Variables Observations Background Error Covariance Summary.
Validation of CrIMSS sounding products of Cloud contamination and angle dependency Zhenglong Li, Jun Li, and Yue Li University of Wisconsin -
Slide 1 IPWG, Beijing, October 2008 Slide 1 Assimilation of rain and cloud-affected microwave radiances at ECMWF Alan Geer, Peter Bauer, Philippe.
Satellite SST Radiance Assimilation and SST Data Impacts James Cummings Naval Research Laboratory Monterey, CA Sea Surface Temperature Science.
ECMWF CO 2 Data Assimilation at ECMWF Richard Engelen European Centre for Medium-Range Weather Forecasts Reading, United Kingdom Many thanks to Phil Watts,
1 ATOVS and SSM/I assimilation at the Met Office Stephen English, Dave Jones, Andrew Smith, Fiona Hilton and Keith Whyte.
Slide 1 Evaluation of observation impact and observation error covariance retuning Cristina Lupu, Carla Cardinali, Tony McNally ECMWF, Reading, UK WWOSC.
Sean P.F. Casey 1,2,3,4, Lars Peter Riishojgaard 2,3, Michiko Masutani 3,5, Jack Woollen 3,5, Tong Zhu 3,4 and Robert Atlas 6 1 Cooperative Institute for.
Data assimilation of polar orbiting satellites at ECMWF
GRAS SAF Workshop, 12 June 2003 Assimilation of satellite data at ECMWF Prospects for use of radio-occultation measurements Jean-Noël Thépaut ECMWF thanks.
NASA/GMAO Activities in Support of JCSDA S. Akella, A. da Silva, C. Draper, R. Errico, D. Holdaway, R. Mahajan, N. Prive, B. Putman, R. Riechle, M. Sienkiewicz,
Slide 1 Model Assimilation of Satellite Observations and Retrievals Andrew Collard
Kick-Off-Treffen SPP, Bonn October 2006 Improved Water Vapour and Wind Initialisation for Precipitation Forecasts: Impact Studies with the ECMWF.
Diagnosing Climate Change from Satellite Sounding Measurements – From Filter Radiometers to Spectrometers William L. Smith Sr 1,2., Elisabeth Weisz 1,
Five techniques for liquid water cloud detection and analysis using AMSU NameBrief description Data inputs Weng1= NESDIS day one method (Weng and Grody)
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.
On Improving GFS Forecast Skills in the Southern Hemisphere: Ideas and Preliminary Results Fanglin Yang Andrew Collard, Russ Treadon, John Derber NCEP-EMC.
Lessons on Satellite Meteorology Part VII: Metop Introduction to Metop Instruments The sounders with focus on IASI The GRAS instrument The ASCAT scatterometer.
Stephanie Guedj Florence Rabier Vincent Guidard Benjamin Ménétrier Observation error estimation in a convective-scale NWP system.
Research and development on satellite data assimilation at the Canadian Meteorological Center L. Garand, S. K. Dutta, S. Heilliette, M. Buehner, and S.
ECMWF WMO Workshop19-21 May 2008: ECMWF OSEs Slide 1 A summary of OSE and OSSE activities at ECMWF. Erik Andersson, Graeme Kelly, Jean-Noël Thépaut, Gabor.
© Crown copyright 2007 Optimal distribution of polar-orbiting sounding missions John EyreMet Office, UK CGMS-40; Lugano, Switzerland;5-9 Nov 2012.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 Infrared Temperature and.
1 Hyperspectral Infrared Water Vapor Radiance Assimilation James Jung Cooperative Institute for Meteorological Satellite Studies Lars Peter Riishojgaard.
1 Using water vapor measurements from hyperspectral advanced IR sounder (AIRS) for tropical cyclone forecast Jun Hui Liu #, Jinlong and Tim.
USE OF AIRS/AMSU DATA FOR WEATHER AND CLIMATE RESEARCH Joel Susskind University of Maryland May 12, 2005.
Status of improving the use of MODIS, AVHRR, and VIIRS polar winds in the GDAS/GFS David Santek, Brett Hoover, Sharon Nebuda, James Jung Cooperative Institute.
Slide 1 VAISALA Award Lecture Characterising the FY-3A Microwave Temperature Sounder Using the ECMWF Model Qifeng Lu, William Bell, Peter Bauer, Niels.
MODIS Polar Winds in ECMWF’s Data Assimilation System: Long-term Performance and Recent Case Studies Lueder von Bremen, Niels Bormann and Jean-Noël Thépaut.
AIRS, HIRS and CSBT Experiments Plus Other FY05/06 Results by James A. Jung Tom H. Zapotocny and John Le Marshall Cooperative Institute for Meteorological.
25 th EWGLAM/10 th SRNWP Lisbon, Portugal 6-9 October 2003 Use of satellite data at Météo-France Élisabeth Gérard Météo-France/CNRM/GMAP/OBS, Toulouse,
ECMWF reanalysis using GPS RO data Sean Healy Shinya Kobayashi, Saki Uppala, Mark Ringer and Mike Rennie.
Preliminary results from assimilation of GPS radio occultation data in WRF using an ensemble filter H. Liu, J. Anderson, B. Kuo, C. Snyder, A. Caya IMAGe.
Layered Water Vapor Quick Guide by NASA / SPoRT and CIRA Why is the Layered Water Vapor Product important? Water vapor is essential for creating clouds,
Concordiasi Satellite data assimilation at high latitudes F. Rabier, A. Bouchard, F. Karbou, V. Guidard, S. Guedj, A. Doerenbecher, E. Brun, D. Puech +
CO 2 retrievals from IR sounding measurements and its influence on temperature retrievals By Graeme L Stephens and Richard Engelen Pose two questions:
ITSC-1227 February-5 March 2002 Use of advanced infrared sounders in cloudy conditions Nadia Fourrié and Florence Rabier Météo France Acknowledgement G.
A step toward operational use of AMSR-E horizontal polarized radiance in JMA global data assimilation system Masahiro Kazumori Numerical Prediction Division.
MODIS Winds Assimilation Impact Study with the CMC Operational Forecast System Réal Sarrazin Data Assimilation and Quality Control Canadian Meteorological.
Rutherford Appleton Laboratory Requirements Consolidation of the Near-Infrared Channel of the GMES-Sentinel-5 UVNS Instrument: H 2 O retrieval from IASI.
1 3D-Var assimilation of CHAMP measurements at the Met Office Sean Healy, Adrian Jupp and Christian Marquardt.
ITSC-12 Cloud processing in IASI context Lydie Lavanant Météo-France, Centre de Météorologie Spatiale, BP 147, Lannion Cedex France Purpose: Retrieval.
© 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.
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.
Status on Cloudy Radiance Data Assimilation in NCEP GSI 1 Min-Jeong Kim JCSDA 9th Workshop on Satellite Data Assimilation, May 24-25, 2011, M-J. Kim 2.
Methane Retrievals in the Thermal Infrared from IASI AGU Fall Meeting, 14 th -18 th December, San Francisco, USA. Diane.
Workshop on Soundings from High Spectral Resolution Infrared Observations May 6-8, 2003 University of Wisconsin-Madison.
© Crown copyright Met Office Assimilating infra-red sounder data over land John Eyre for Ed Pavelin Met Office, UK Acknowledgements: Brett Candy DAOS-WG,
Indirect impact of ozone assimilation using Gridpoint Statistical Interpolation (GSI) data assimilation system for regional applications Kathryn Newman1,2,
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course
Surface Pressure Measurements from the NASA Orbiting Carbon Observatory-2 (OCO-2) Presented to CGMS-43 Working Group II, agenda item WGII/10 David Crisp.
European Centre for Medium-Range Weather Forecasts
Cristina Lupu, Niels Bormann, Reima Eresmaa
Assimilation of MWHS on FY-3B over Land
PGE06 TPW Total Precipitable Water
Impact of hyperspectral IR radiances on wind analyses
GOES-16 AMV data evaluation and algorithm assessment
Assimilation of Cloudy AMSU-A Microwave Radiances in 4D-Var
FSOI adapted for used with 4D-EnVar
Exploring Application of Radio Occultation Data in Improving Analyses of T and Q in Radiosonde Sparse Regions Using WRF Ensemble Data Assimilation System.
Item Taking into account radiosonde position in verification
Assimilation of Global Positioning System Radio Occultation Observations Using an Ensemble Filter in Atmospheric Prediction Models Hui Liu, Jefferey Anderson,
Satellite Foundational Course for JPSS (SatFC-J)
Current and future use of microwave imager radiances in NWP models
Session 1 – summary (1) Several new satellite data types have started to be assimilated in the last 4 years, all with positive impacts, including Metop-B.
Presentation transcript:

ECMWF – 1© European Centre for Medium-Range Weather Forecasts Developments in the use of AMSU-A, ATMS and HIRS data at ECMWF Heather Lawrence, first-year EUMETSAT fellow, ECMWF Supervised by: Niels Bormann & Stephen English

ECMWF – 2© European Centre for Medium-Range Weather Forecasts Outline 1. Investigating the value of HIRS 2. Introducing ATMS data over land and sea-ice 3. Situation-dependent observation errors for AMSU-A channels PARTS:

ECMWF – 3© European Centre for Medium-Range Weather Forecasts 1. Investigating the value of HIRS

ECMWF – 4© European Centre for Medium-Range Weather Forecasts 1. HIRS: The Instrument IR sounder with Temperature sounding CO 2, CO 2 /N 2 O channels Water vapour channels 9 channels used… Coverage: MetOp-A, NOAA-19 …over ocean & sea-ice … and land for channel 12 HIRS 19 Channels

ECMWF – 5© European Centre for Medium-Range Weather Forecasts 1. HIRS: Aim & Motivation HIRS is an older instrument whose value in the ECMWF system has not been tested recently New hyper-spectral IR sounders (AIRS, IASI) may have made HIRS redundant AIM: Investigate the value of HIRS in the ECMWF forecasting system WHY?

ECMWF – 6© European Centre for Medium-Range Weather Forecasts Perform 2 sets of experiments: 2 x 2 months summer and winter, T511, 38R2: Control: 38R2 version of ECMWF model (IR, MW sounders, scatterometers, radiosondes, etc.) HIRS denial experiments: as control but take HIRS (MetOp-A and NOAA-19) out 1. HIRS: Method

ECMWF – 7© European Centre for Medium-Range Weather Forecasts 1. HIRS: Results DEPARTURE STATISTICS: observation – 12h forecast MHS MW humidity sounder Improved fit of MHS, IASI, AIRS to 12h humidity & temperature forecast IASI IR temperature sounder AIRS IR temperature sounder 0.5 – 1% improvement 2% improvement 0.4% improvement

ECMWF – 8© European Centre for Medium-Range Weather Forecasts 1. HIRS: results FORECAST SCORES : 1 – 10 day T, Z, R, VW forecast minus analysis Degraded forecast Improved forecast Lots of blue = HIRS improves (short-range) forecasts Day 2 500hPa Day 3 500hPa neutral to positive: e.g. 500hPa Geopotential

ECMWF – 9© European Centre for Medium-Range Weather Forecasts 1. HIRS: Conclusions and future developments HIRS improves short-range forecasts of temperature, humidity, geopotential Future Developments: MetOp-B HIRS Trials are underway to test the introduction of MetOp-B HIRS So far results look promising Improved AIRS departures

ECMWF – 10© European Centre for Medium-Range Weather Forecasts 2. Introducing ATMS over land and sea-ice

ECMWF – 11© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: The ATMS instrument Microwave Temperature/Humidity sounder (AMSU-A & MHS combination) 10 temperature sounding channels5 humidity sounding channels Temperature sounding: Humidity sounding:

ECMWF – 12© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: The ATMS instrument 2011: Suomi-NPP satellite launched with ATMS on board 2012: Some ATMS data assimilated operationally at ECMWF Land, sea-ice, ocean Channel 9 coverage (2 cycles) Channel 6 coverage (2 cycles) Ocean only

ECMWF – 13© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: Aim & Motivation AIM: Add channels over land and sea-ice Intoducing more AMSU-A data improves forecasts Microwave data less affected by cloud than IR: has value over land/sea-ice Add data: Humidity sounding channels Surface-sensitive temperature channels MOTIVATION:

ECMWF – 14© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: Method How can we obtain skin temperature and emissivity? Treat ATMS like AMSU-A and MHS: Emissivity retrieved from window channel prior to assimilation Skin temperature retrieved during assimilation as a ‘sink variable’ Desired values retrieved in analysis We need emissivity and skin temperature inputs Karbou et al, Di Tomaso et al (2013)

ECMWF – 15© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: Assimilation experiments 3 experiments, months, 39R1 137 vertical levels Control: Same as operational 39R1 at lower resolution T511 (~40km) ATMS Land: Control + ATMS over land ATMS Land Sea-ice: Control + ATMS over land + ATMS over sea-ice

ECMWF – 16© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: Results Departures: 12h forecast – observation 0.5% improvement 1% improvement: sea-ice AMSU-A global standard deviation(o-b) 2x2 months Channel number MHS global MHS Nhem winter standard deviation(o-b) 2 months Improved temperature and humidity 12h forecasts fit to observations 0.05% improvement

ECMWF – 17© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: Results Forecast scores: 1 – 10 day forecast minus own analysis Degraded Forecast Improved Forecast ATMS Land + Sea-ice

ECMWF – 18© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: Results COLD SEA ATMS data appear to have a negative impact on TEMPERATURE Could be because adding data makes analysis more variable? Day 1 Temperature 1000hPa

ECMWF – 19© European Centre for Medium-Range Weather Forecasts 2. ATMS over land and sea-ice: Conclusions ATMS temperature and humidity sounding data was introduced over land and sea-ice Departure statistics were improved for AMSU-A and MHS Forecast scores were neutral to positive for ATMS over land data Geopotential Forecast scores were neutral for ATMS over sea-ice Short-range Temperature forecasts appeared degraded over Southern Ocean when sea-ice data introduced

ECMWF – 20© European Centre for Medium-Range Weather Forecasts 3. AMSU-A Observation Errors

ECMWF – 21© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: The Instrument 10 Temperature sounding channels 7 satellites: good global coverage Microwave Temperature Sounder

ECMWF – 22© European Centre for Medium-Range Weather Forecasts Tropospheric channels 5 – 7: Important for NWP But cloud contamination/surface sensitive 3. AMSU-A observation errors: The Instrument

ECMWF – 23© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Aim & Motivation Channels 5 – 7 observation errors should contain: AIM: Develop situation- dependent observation errors Observation error = surface term + cloud term + noise Situation-dependent constant stdev(o-b) MetOp-A AMSU-A channel 5: ALL DATA NOT CONSTANT

ECMWF – 24© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Surface term Do not include skin temperature term: skin temperature retrieved as sink variable in analysis Include emissivity term Surface type Sea0.015 Sea-ice0.050 Snow-free land0.022 Snow-covered land0.050 (S. English 2008)

ECMWF – 25© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Liquid water path term Channel 5: Channel 6: Channel 7: LWP (kg/m 2 ) Data screened for cloud but may still have some contamination…

ECMWF – 26© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Noise term LWP (kg/m 2 ) Channel 5: 0.25 K Channel 6 – 7: 0.20 K

ECMWF – 27© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: New Observation Errors Metop-B AMSU-A channel 5 observation errors: used data Nadir angles have higher values High lwp = higher value

ECMWF – 28© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Assimilation Trials Situation- dependent observation errors: Weight data differently Allows the introduction of more data in ‘difficult’ areas: cloudy, high orography Assimilation trials (2 months): Control: version 40R1 with some 40R2 contributions at T511 (40km) resolution, 137 vertical levels New observation errors: Control + new observation errors Extended coverage over cloud: Control + new observation errors + relaxed cloud screening Extended coverage over high orography: control + new observation errors + relaxed orography screening

ECMWF – 29© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Extended coverage Add cloud-screened data Metop-B AMSU-A channel 5 Add data over high orography

ECMWF – 30© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Results Control vs Observation errors experiment Neutral Impact on forecast accuracy degradation Temperature 850hPa Geopotential 500hPa improvement

ECMWF – 31© European Centre for Medium-Range Weather Forecasts Ctrl – obs error Ctrl – ext. cloud 3. AMSU-A observation errors: Results Control vs Extended coverage in cloudy regions ATMS over sea Observation - 12h forecast 0.4% improvement Improved fit to ATMS, neutral forecast scores: results encouraging degradation improvement Ctrl – obs error Ctrl – ext. cloud

ECMWF – 32© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Results Control vs Extended coverage in high topography 3 day geopotential fc - an 3 day temperature fc - an Blue= Improved forecast Red/green= degraded forecast Positive impact in northern hemisphere Mixed positive/negative Over Antarctica Mixed positive/negative results

ECMWF – 33© European Centre for Medium-Range Weather Forecasts 3. AMSU-A observation errors: Conclusions Situation-dependent observation errors were derived for AMSU-A channels 5 -7 This gave neutral results with screening as-is Introducing data previously screened for clouds improved fit to ATMS instrument Introducing data over high orography had mixed positive/negative results Work is ongoing

ECMWF – 34© European Centre for Medium-Range Weather Forecasts Summary of Findings The HIRS instrument has a small positive impact on short-term T, Z, R forecasts Introduction of ATMS data over land improves temperature/humidity forecast accuracy Introduction of ATMS data over sea-ice has mixed results – further investigation needed Situation-dependent observation errors for AMSU-A channels 5 – 7 have the potential to improve forecasts by introducing more data (work ongoing)