The NCEP and NCAR are cooperating in a project (denoted ''reanalysis''
) to produce a 40-year record of global analyses of atmospheric fields
in support of the needs of the research and climate monitoring commun
ities. This effort involves the recovery of land surface, ship, rawins
onde, pibal, aircraft, satellite, and other data; quality controlling
and assimilating these data with a data assimilation system that is ke
pt unchanged over the reanalysis period 1957-96. This eliminates perce
ived climate jumps associated with changes in the data assimilation sy
stem. The NCEP/NCAR 40-yr reanalysis uses a frozen state-of-the-art gl
obal data assimilation system and a database as complete as possible.
The data assimilation and the model used are identical to the global s
ystem implemented operationally at the NCEP on 11 January 1995, except
that the horizontal resolution is T62 (about 210 km). The database ha
s been enhanced with many sources of observations not available in rea
l time for operations, provided by different countries and organizatio
ns. The system has been designed with advanced quality control and mon
itoring components, and can produce 1 mon of reanalysis per day on a G
ray YMP/8 supercomputer. Different types of output archives are being
created to satisfy different user needs, including a ''quick look'' CD
-ROM (one per year) with six tropospheric and stratospheric fields ava
ilable twice daily, as well as surface, top-of-the atmosphere, and ise
ntropic fields. Reanalysis information and selected output is also ava
ilable on-line via the Internet (http//:nic.fb4.noaa.gov:8000). A spec
ial CDROM, containing 13 years of selected observed, daily, monthly, a
nd climatological data from the NCEP/NCAR Reanalysis, is included with
this issue. Output variables are classified into four classes, depend
ing on the degree to which they are influenced by the observations and
/or the model. For example, ''C'' variables (such as precipitation and
surface fluxes) are completely determined by the model during the dat
a assimilation and should be used with caution. Nevertheless, a compar
ison of these variables with observations and with several climatologi
es shows that they generally contain considerable useful information.
Eight-day forecasts, produced every 5 days, should be useful for predi
ctability studies and for monitoring the quality of the observing syst
ems. The 40 years of reanalysis (1957-96) should be completed in early
1997. A continuation into the future through an identical Climate Dat
a Assimilation System will allow researchers to reliably compare recen
t anomalies with those in earlier decades. Since changes in the observ
ing systems will inevitably produce perceived changes in the climate,
parallel reanalyses (at least 1 year long) will be generated for the p
eriods immediately after the introduction of new observing systems, su
ch as new types of satellite data. NCEP plans currently call for an up
dated reanalysis using a state-of-the-art system every five years or s
o. The successive reanalyses will be greatly facilitated by the genera
tion of the comprehensive database in the present reanalysis.