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An Overview of the North American Regional Reanalysis

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Title: An Overview of the North American Regional Reanalysis


1
An Overview of the North American Regional
Reanalysis
  • W. Ebisuzaki, F. Mesinger, G. DiMego, E. Kalnay,
    K. Mitchell, M. Ek, R. Grumbine, D. Jovic, P.
    Shafran, and J. Woolen
  • http//wwwt.emc.ncep.noaa.gov/mmb/rreanl/inde
    x.html

2
Motivation for North American Regional
Reanalysis (NARR)
  • Create hi-resolution reanalysis for the North
    American domain
  • Address some of the weakness of the N/N
    Reanalysis, i.e., near surface temperature,
    winds
  • Hydrology in the North American domain
  • Make a more useful reanalysis (for people who
    want point values and live on the surface

  • Expectations
  • more applied meteorological applications
  • more uncertain about how non-meteorologists will
    use the data

3
High Lights of NARR
  • ETA model and assimilation system (EDAS)
  • 32 km resolution over the North and Central
    America
  • R-2 horizontal boundary conditions
  • new land surface model (NOAH)
  • precipitation assimilation
  • 8x daily analyses from October 1978 onwards
  • 5 TB for basic set of analyses and fluxes
  • Oct 1978-Nov 2002 done

4
NARR domain

5
180 km ( CDAS) vs 32 km (NARR) resolution
topography

6
ETA / NOAH LAND-SURFACE MODEL UPGRADES 24 Jul 01
- assimilation of hourly precipitation --
hourly 4-km radar/gage analysis (Stage IV) - cold
season processes(Koren et al 1999) -- patchy
snow cover -- frozen soil (new state variable)
-- snow density (new state variable) - bare
soil evaporation refinements -- parameterize
upper sfc crust cap on evap - soil heat flux --
new soil thermal conductivity (Peters-Lidard
et al 1998) -- under snowpack (Lunardini,
1981) -- vegetation reduction of thermal cond.
(Peters-Lidard et al 1997) - surface
characterization -- maximum snow albedo
database (Robinson Kukla 1985) -- dynamic
thermal roughness length refinements -
vegetation -- deeper rooting depth in forests
-- canopy resistance refinements
NOAH LSM tested in various land-model
intercomparison projects, e.g., GSWP, PILPS 2a,
2c, 2d, 2e, Rhone, and (near-future) DMIP.
7
January 1997 Precipitation Results
8
Precipitation
  • Several sources of precipitation
  • CONUS data with PRISM (Mountain Mapper) to
    improve orographic effects
  • Canada
  • Mexico
  • CMAP (combination of satellite and gauge data)
    over oceans CMAP is blocked
  • Near central areas of hurricanes (7.5 by 7.5 deg)
  • Observed precipitation gt 100 mm/day
  • A 15-degree 'blending belt' between 27.5 and 42.5
    N, with no CMAP north of 42.5 N

9
Comparison of N/N Reanalysis and NARRmodel
  • Global
  • Spectral
  • 250 km resolution
  • 28 sigma levels
  • Land sfc (Pan and Marht, 1987)
  • One soil type (sandy loam)
  • Two soil levels
  • Simplistic snow depth, fn(T)
  • 6 hour analyses time steps
  • N. Am. Sector
  • Grid point
  • 32 km resolution
  • 45 pressure levels
  • NOAH model (2002)
  • Realistic soil types
  • 4 soil layers
  • Snow depth, modeled/observed
  • 3 hour analyses time steps

10
Comparison of N/N Reanalysis and NARRinput
observations
  • Sondes, aircraft
  • TOVS temperature retrievals
  • Satellite winds
  • Land sfc prs
  • Ocean sfc prs, q, t, winds
  • Snow cover old is low res
  • Reynold's SST
  • Sea ice from R. Grumbine
  • Sondes, aircraft, profilers
  • Direct assimilation of radiances
  • Satellite winds
  • Land sfc prs, q, winds
  • Ocean sfc prs, q, t, winds
  • Precipitation
  • USAF snow depth (hi res)
  • Reynold's SST lakes
  • Sea ice from R. Grumbine lakes

11
Comparison of N/N Reanalysis and NARRdates
  • Software 1994
  • Analyses 1948-present
  • Software 2002
  • Analyses Oct 1978-Nov 2002
  • Nov 2002 in development

12
Operational ETA vs NARR
  • 32 km
  • 45 levels
  • Frozen physics
  • Better precip obs
  • Better lake obs
  • 12 km
  • 60 levels
  • Evolving physics
  • Precip assim for CONSUS
  • Lakes SST, ice-real time

13
Operational ETA vs NARRUser Output RR is more
friendly
  • RR 1 grib table vs 3 grib tables for OPN
  • (some software cannot handle multiple
    tables)
  • RR Winds are N/S vs grid-relative winds in OPN
  • (some software cannot handle grid-relative
    winds)
  • RR new variables moisture fluxes, etc
  • RR redundant variables removed ex dew pt, rel
    q, specific q
  • RR added new BL levels, removed others
  • RR BUFR files have QC and increments
  • RR many monitoring plots

14
Why NARR should have better surface values
  • 1) higher horizontal orography 32 km vs 250 km
  • need to resolve orography
  • 2) better land surface model
  • to get 2m temp and q .. need better sfc
    fluxes
  • 3) assimilated precipitation
  • better model precipitation .. clouds,
    radiative flux
  • better soil moisture .. latent and sensible
    heat flux
  • 4) gridded snow depth is similar to NARR
    resolution
  • a problem with NCEP's global reanalyses
  • 5) assimilate more near surface data (winds, q)
  • 6) 3 hour assim cycle, better resolve diurnal
    cycle

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30
Principal Output Datasets
  • Observations with QC marks, increments (BUFR)
  • plots obs locations, fit to sondes, fit to sfc
    obs,
  • fit to global reanalysis, various NARR fields
  • binary restart files (to rerun model, high
    resolution), very big, small usage
  • GRIB analyses and first guess on model grid big,
    no interpolation errors
  • GRIB analyses and first guess on Lambert
    conformal 32-km grid, big, easier to use,
    interpolation error
  • Merged GRIB analyses and averaged/accumulated
    flux/precip and some 1st guess fields for water
    budgets, Lambert Conformal grid (AWIP 221), 5 TB
    for 8x daily for entire period. This will be
    work-horse data set.

31
Data Distribution
  • NCAR
  • SDSC (San Diego Super Computing Center, UCSD)
  • U. of Maryland
  • NCDC-NOMADS (NOAA Operational Model Archive
    Distribution System)

32
NOMADS
  • Partnership of many organizations including core
    collaborators CDC, COLA, FSL, GFDL, LLNL, NCAR,
    NCDC, NCEP, PMEL, UNIDATA
  • On-line access to the merged RR data set
    (analyses fluxessome first guess)
  • NCDC 7 TB on-line storage, web servers, x-TB
    tape storage
  • NCEP ¾ TB on-line, web servers, software
    upgrades
  • Software
  • on-line plotting package
  • on-line slice-and-dice of GRIB files
  • GrADS-DODS
  • Status
  • plotting package will be enhanced by NCEP
  • downloading of GRIB files will be enhanced by
    NCEP
  • GrADS-DODS needs enhancements
  • NOMADS-NCDC has experience running software

33
I can't download the 5 TB merged data set!
  • Download what you want
  • Select
  • 1) variables
  • 2) levels
  • 3) times
  • 4) domain
  • 5) resolution 32 km, 64 km, 96 km
  • Downloading can be scripted

34
Summary
  • Oct 4, 2003 Finished Oct 1978 to mid-Nov 2002
  • no more inland lake data
  • no 2003 Canadian precip
  • currently planning the real-time NARR
  • will use different datasets as some
  • precip/lake data are not available in
    real time
  • currently planning subsets and archive
  • Dec 2003 internet-2 will be available at NCDC and
  • distribution to archive sites can start
  • Until NARR appears at archive sites, you can look
    at
  • 1 year of merged data at NCEP.
  • http//wwwt.emc.ncep.noaa.gov/mmb/rreanl/inde
    x.html
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