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The Available NCEP Reanalyses Wesley Ebisuzaki Climate Prediction Center National Centers for Environmental Prediction NWS/NOAA Maryland, USA wesley.ebisuzaki@noaa.gov.

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Presentation on theme: "The Available NCEP Reanalyses Wesley Ebisuzaki Climate Prediction Center National Centers for Environmental Prediction NWS/NOAA Maryland, USA wesley.ebisuzaki@noaa.gov."— Presentation transcript:

1 The Available NCEP Reanalyses Wesley Ebisuzaki Climate Prediction Center National Centers for Environmental Prediction NWS/NOAA Maryland, USA

2 Topics Introduction R1, R2, NARR, CFSR
Grib 1 and 2 and various utilities Getting the data by Nomads Will try to cover these topics from a user perspective. Some overlap with NOMADS and GrADS presentations.

3 Download links http://www. cpc. noaa. gov/products/ wesley/ams2010_sc
Download links wesley/ams2010_sc.html Documentation package includes a pdf version. The pdf has more details and covers more material.

4 Are Reanalyses Truth? Convenient Run through quality control programs
Consistent (ex. winds, temperature, heights) Almost every variable that you would ever want Better than interpolation of observations

5 But Need observations Some fields depend on the model physics
Some regions are poorly observed Some levels are poorly observed Some fields depend on the model physics Clear sky radiation is pretty good Clouds and other moist process are bad BL is somewhere in between

6 Reanalysis Errors Best for winds, temperature and heights Humidity
Observations, consistency relationships Near surface more dependent on BL physics Humidity Fewer observations, model physics important Other fields More model physics dependent

7 Not all observations are equal
Sondes and aircraft data are good quality Surface pressure is good quality Surface winds, temperatures, humidities Hard to assimilate, elevation, representativeness Satellite data Retrievals=old, Radiances=new Hard to get a consistent record with historical data A concern for trend analyses

8 Analysis Uncertainties Factors to Consider
Observation density Sensitivity to model parameterizations Dependent on lesser quality observations Model and data assimilation system

9 Are Observations Truth?
Data assimilation could fit the observations exactly but produce a worse forecast! Error by equipment manufacturer Representativeness error Observation in an air parcel is not the same as average value in the grid cell

10 Finally a plot spread from an ensemble of opn analyses and reanalyses simple way to get a error estimate

11 Averaged over a year

12 Monthly Means

13 Analysis Uncertainties
Not simple Uncertainty for a day: synoptic and data Averaged over a year: data Monthly/seasonal means have smaller uncertainties than daily field, biases

14 NCEP Reanalyses NCEP/NCAR Reanalysis (R1, CDAS)
Mid 1990s, 1947-present, 2.5 degree grid, global NCEP/DOE Reanalyses (R2) Late 1990s, 1979-present, 2.5 degree grid, global North American Regional Reanalysis (NARR) Early 2000's, 1979-present, 32 km grid Climate Forecast System Reanalysis (CFSR) 2010, 1979-present, 0.5 degree grid, global

15 Others Reanalyses ECMWF: ERA-15, ERA-40, ERA-interim
JMA, CRIEPI: JRA-25/JCDAS NASA/GSFC: MERRA ERSL (different approach) Check for robust signal

16 Support of NCEP Reanalyses
1) Journal articles (BAMS) 2) Web: NCEP, NCAR, ERSL, NCDC 3) Questions to provider of data 4) NCDC, NCAR, ERSL will forward tough questions to NCEP 5) At NCEP: R1, R2, NARR: CFSR: to be determined

17 Nuts and Bolts: data formats
grib1, grib2 grib is a WMO standard and national meteorological centers use WMO standards for day-to-day operations Reanalyses run at highest resolution possible Large portion of supercomputer, massive tape storage grib files are smaller than netcdf Netcdf NCAR and ERSL often translate into netcdf and redistribute the NCEP reanalyses

18 My grib1 toolbox wgrib: inventory, get values, database tool
GrADS: plots, some computations copygb: convert to different grid Calculations often easier on lat-lon grid Save space ggrib and lcgrib: subset of lat-lon, lambert- conformal grids, faster than copygb C/fortran programs: ieee -> grib

19 My grib2 tool box wgrib2: inventory, contents, database, encode
GrADS: plots and some computations copygb2: convert to a different grid, computations are often easier on lat-lon grid cnvgrib: convert between grib1 and grib2 ggrib and lcgrib functionality in wgrib2 wgrib2: ieee -> grib2

20 grib2 to grib1: cnvgrib grib2 is new, many people use cnvgrib to convert from grib2 to grib1 Long term solution? NO! NCO dropped support for cnvgrib (5 years) New variables in grib2 are not in grib1 grib2 files are compressed, easier to use New features in grib1 utilities?

21 Short Grib1 Inventories
-sh-3.00$ wgrib -s narr.t09z.awip32.merged 1:0:d= :MSLET:MSL:anl:NAve=0 2:166602:d= :PRMSL:MSL:anl:NAve=0 3:333204:d= :PRES:hybrid lev 1:anl:NAve=0 .. -s is the short inventory column 1 = message (record) number column 2 = byte location starting from 0 column 3 = analysis time or initial time of the forecast column 4 = variable name column 5 = level/layer column 6 = timing information, anl=analysis, acc=accumulation, ave=average column 7 = number of fields used to make an ave/acc

22 Short Grib2 Inventories
--sh-3.00$ wgrib2 pgblnl.gdas grb2 -s 1:4:d= :HGT:1 mb:anl: 2:16552:d= :TMP:1 mb:anl: 3:22064:d= :RH:1 mb:anl: .. column 1: message or message.submessage number column 2: the byte location of the grib message column 3: the analysis or start of forecast time, use -T to see the minutes and seconds column 4: variable name column 5: level column 6 = timing information, anl=analysis, acc=accumulation, ave=average, fcst = forecast

23 Names HGT = geopotential height (m) TMP = temperature (K)
UGRD = zonal wind (m/s) VGRD = meridional wind (m/s) see NCEP tables on web (see pdf file) or use -v option in wgrib/wgrib2

24 Grid information: grib
grib1/grib2 support many different grids internally grib stores data in different orders, 8 in grib1, 16 in grib2 up to software to figure it out wgrib -V wgrib2 -grid

25 Values at specified locations
Grib1: understand the grid R1, R2: WE:NS storage NARR: WE:SN storage Global – easy to figure out the lat-lon of points NARR – need file with the lat-lon of the points rr-fixed.grb is with other course files On your own

26 Values at specified locations
Grib2: harder to understand and easier to use 16 storage orders (3 in common use) wgrib2 convert data to WE:SN order by default Can use old way to pick up data (i.e. get n-th point) Can use wgrib2 to get the data (-lon option) See documentation for wgrib2 examples

27 Winds and other vectors
Winds have two orientations North can point to the north pole (earth relative) North can point to the north grid point (grid relative) Non-staggered grid: (ix,iy) -> (ix,iy+1)

28 NARR Output Grid

29 Winds and other vectors
NCEP convention is grid relative Lat-lon, Gaussian, Mercator is not an issue Lambert-conformal, polar stereographic an issue NARR is earth relative (anti-NCEP convention) Good for new users Bad for users of other NCEP regional products

30 GrADS and grib Widely used, open source, visualization + more
Data model GrADS x,y,z,t and ensemble Grib time is more complicated forecast verification time Start of forecast time (or analysis time) average from 6-12 hours into the forecast Monthly average of one of the above Need to map grib times into GrADS time

31 Making plots with GrADS: grib1
Analyses grib2ctl.pl grib_file >ctl_file gribmap -0 -i ctl_file (run grads) Forecasts grib2ctl.pl -verf grib_file >ctl_file gribmap -i ctl_file

32 Making plots with GrADS: grib2
Analyses g2ctl.pl -0 grib_file >ctl_file gribmap -0 -i ctl_file (run grads) Forecasts g2ctl.pl grib_file >ctl_file gribmap -i ctl_file Unified options, -b option is working

33 See Jennifer's presentations
More GrADS See Jennifer's presentations

34 Getting data the Nomads way
On-line is easiest way – if downloading time ok Big jobs: spend more time optimizing the transfer and reduce the amount of data transferred Small jobs: ease of use is important, ex. plots, OpeNDAP (lat-lon grid, text output).

35 Downloading Methods Partial http downloading:
download the fields that you want select by field/time/level data is compressed (grib2) or packed (grib1) efficient for the server (support many clients) easy to script (not point and click) example in the documentation package good for large downloads

36 Downloading Methods g2subset (grib-filter):
download the fields that you want select by field/time/level select an optional regional subset grib2 only point and click to learn or a few files moderately easy to script example in the documentation package more server resources, less data transferred

37 Downloading Methods OPeNDAP: standard protocol (text based)
select field/time/level/region data is read by the server interpolated to a lat-lon grid if needed sent to the client by a standard protocol advantages: supported by software easy to use .. can even use a browser disadvantages: server overhead data may not be compressed

38 Downloading Methods Plots: Part of the development nomads at NCEP
Point and click Designed for casual use of the data Not designed to do everything Research: download and do own plots For some people, this all that they need

39 Downloading Methods Full File:
Can use browser, etc to download full file from http server, get the directory listing and right click. Easy Good to get a sample file to help plan the download.

40 Typical Nomads front page

41 Summary Reanalyses are not truth Observations are not truth
Tools for grib1 and grib2 Introduction to Nomads Save time in downloading data Select fields that you will need Can alway get other fields later Select access method


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