Global reanalysis: Some lessons learned and future plans
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1 Global reanalysis: Some lessons learned and future plans Adrian Simmons and Sakari Uppala European Centre for Medium-Range Weather Forecasts With thanks to Per Kållberg and many other colleagues from ECMWF and Partners in ERA-40 1 Reanalysis Data assimilation has been developed primarily to provide initial conditions, analyses, for operational numerical weather forecasts Quality of operational analyses varies over time largely because of changes in data assimilation systems Reanalysis: - applies a fixed, modern data assimilation system to multidecadal sets of observations - generates a sequence of atmospheric and land/ocean/ice surface conditions every few hours throughout the period - provides complete, gridded data sets for use in a wide variety of applications 2
2 Data assimilation combines information from - Current observations - A short-range background forecast that carries forward T Background forecast the information extracted from prior observations - Statistics Analysis 12UTC 18UTC - Dynamical and physical relationships Analysis Analysis Analysis 00UTC 06UTC 12UTC t Six-hourly 3D analysis to produce the most probable estimate of the atmospheric state (and some estimate of uncertainty) 3 The quality of reanalyses is affected by: The quality of the assimilation system - The assimilating model (atmosphere, ocean waves, land state) - The analysis system The characteristics of the observing system - The type, accuracy and coverage of observations, changes over time in particular The prescribed boundary conditions - Sea-surface temperature and sea-ice distribution - Land-surface state (vegetation, lakes, ) The specified atmospheric composition - Greenhouse gases, aerosols, 4
3 Primary global reanalyses NCEP/NCAR present by NCEP with NCAR data supply ERA by ECMWF NCEP/DOE (Reanalysis-2) present by NCEP with DOE funding ERA by ECMWF and partners (including NCAR) JRA by JMA (including observations from ERA-40) 5 Changes to the observing system 1940s: Establishment of network of Atlantic and Pacific Weather Ships 1957: Radiosonde network enhanced in Southern Hemisphere for International Geophysical Year 1973: NOAA-2 First operational sounding of temperature and humidity from polarorbiting satellite 1979: Improved sounding from polar orbiters Winds from geostationary orbit More data from commercial aircraft Drifting buoys Ship Alpha NOAA-2 15 Oct 1972 Today: Additional satellite, aircraft and buoy data Poorer radiosonde coverage (but better quality data) 6
4 00UTC 1 February 1953 The Netherlands gift to ECMWF 7 00UTC 1 February m wind 25ms -1 Significant wave height (m) 8
5 Re-analyses for time of Windscale nuclear reactor fire 12UTC 11 October UTC 12 October 1957 Iodine-131 measurements 24h from 9UTC 11 Oct Crabtree(1959) Quarterly Journal Royal Met Soc 48h from 9UTC 12 Oct O data supplied by public server (to Dec 2003) 7000 Number of fields supplied for each day of the reanalysis
6 Accuracy of forecasts from ERA-40 and ECMWF operations Anomaly correlation (%) of 500hPa height field 11 Non-satellite data supplied by NCAR/NCEP for ERA-40 Radiosonde and pilot China Raobs Countries, US Control, France, Misc Russia TD52 TD53 TD54 ON20 US Navy GATE/TWERLE USAF, ON29 Surface TD13, TD14, USSR USAF ON124 COADS USSR snow depth Automatic Antarctic Aircraft Australian US Navy ON20 Sadler Rean-1 Cloud Motion Winds ON20 Rean
7 NCAR s current upper-air datasets (J. Comeaux) DESCRIPTION C-CARDS Raobs CARDS 542 China R & P Countries R & P PERIOD ERA French R & P GATE R & P 1974 Line Island 1967 MIT Raobs Navy Kunia Navy Spot Soundings NCEP ADP 1973-Cont NCEP B Permanent Ship NCAR s current upper-air datasets (J. Comeaux) DESCRIPTION Ptarmigan Drops Russian NP Russian Ship Russian Upper Air PERIOD ERA Scherhag Raobs South African TD390 Raobs TD52 Pibals TD53 Pibals TD54 Raobs TWERLE US Control 1946-Cont USAF Upper Air
8 NCDC s Integrated Global Radiosonde Archive 15 Radiosonde coverage 1958 Average number of soundings per day: Average number of soundings per day:
9 ERA-40 SYNOP and SHIP coverage 9-15UTC 1 July ERA-40 SYNOP and SHIP coverage 9-15UTC 1 July
10 SYNOP sources for NCEP/NCAR reanalysis (J.Woollen, NCEP) 19 Snow-depth data available for ERA
11 Trend and variability in two-metre temperature ERA-40 CRUTEM2v (Jones & Moberg, 2003) 21 Identification of data problems: a land example Surface air temperature anomaly ( o C) with respect to ERA-40 CRUTEM2v Europe Inadequate ERA-40 data coverage Erroneous station climate data 22
12 EUMETSAT s reprocessed METEOSAT-2 winds EUMETSAT is reprocessing data from later METEOSATs 23 Radiosonde bias correction using ERA-40 feedback (Haimberger, 2005) ST PETERSBURG 12UTC 50hPa temperature (Background Observation) Correction 24
13 69 (Obs- background) for UK radiosonde temperatures at 100hPa as a function of solar angle hPa specific humidity differences Background - sonde Analysis - sonde 26
14 Precipitation over the Baltic catchment area ( ) OBS ERA-40 (Ulf Andrae) 27 Stratospheric age of air simulations with a chemical transport model (Beatriz Monge Sanz, Martyn Chipperfield) From CO 2 and SF 6 measurements New reanalysis ERA-40 28
15 Plans for global reanalysis ECMWF An interim global reanalysis - will cover , starting soon - will have higher horizontal and vertical resolution than ERA-40 - will use 4D-Var and latest version of forecasting system - will address several problems in ERA-40 analyses - will provide baseline for further developments, including constituent analysis A new extended global reanalysis - ERA-65/75 (1938/ ) to begin in experimentation for pre-1989 periods will be done with interim system - preparatory work on observational database is a major task - subject to funding 29 Plans for global reanalysis Japan Meteorological Agency JCDAS (JMA CDAS) - JRA-25 ( ) will be continued in near real time 2nd Japanese reanalysis (JRA-50) - will cover and be completed by 2012 USA NOAA CDC - Reanalysing using only surface-pressure obs NASA GMAO - MERRA will cover ; 1970s will also be studied New NOAA (NCEP/CDC/NCDC) programme - ~
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