Title: An Overview of the North American Regional Reanalysis
1An 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
2Motivation 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
3High 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
4NARR domain
5180 km ( CDAS) vs 32 km (NARR) resolution
topography
6ETA / 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.
7January 1997 Precipitation Results
8Precipitation
- 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
9Comparison 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
10Comparison 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
11Comparison of N/N Reanalysis and NARRdates
- Software 1994
- Analyses 1948-present
- Software 2002
- Analyses Oct 1978-Nov 2002
- Nov 2002 in development
12Operational 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
13Operational 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
-
14Why 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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30Principal 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.
31Data Distribution
- NCAR
- SDSC (San Diego Super Computing Center, UCSD)
- U. of Maryland
- NCDC-NOMADS (NOAA Operational Model Archive
Distribution System)
32NOMADS
- 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
33I 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
34Summary
- 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