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ds082.1 MORE SUMMARYGo to Dataset: 
 

PAGE 2

Please see this information for ds082.0, the source of this dataset. The first few paragraphs describe the model.


TYPES:

Operational
Gridded analyses
Synoptic
Surface analyses
Sea analyses
Oceanographic


COVERAGE:

Global coverage
Latitude / longitude grid
Northern hemisphere and Southern hemisphere are in separate grids. Information about the grid orientation is here.


UPDATES:

None

See DS083.1 for later analyses.


TIMES:

daily 12-hrly
at 00Z and 12Z


VARIABLES:

About 1991, NCEP acknowledged that the temperature is actually virtual temperature.

A humidity field problem is described here.

Some wind field problems are described here.

Sea surface temperatures, based on Navy analyses, begin 1979May16. For earlier analyses, see DS240.0.

Snow depth analyses begin 1979Jul25 and appear just once a week or so.

Surface elevation field from DS757.0.


VARIABLE / LEVEL TABLES:

Table of Levels and Variables
(in 1993: 14 grids max per hemisphere per analysis time)

    bound  theta u v rh
     1000  z t u v rh
      msl  slp
      sfc  sfcp sfct sst snow(weekly)


FORMAT:

Be aware of these processing issues.

MM5, WRF and RAMS users click here.

A little advice is available for: GRIB and GrADs (display) software


VOLUME:

0.5MB/day, 33MB/VSN (MSS), 3.2GB total through 1994


COST:

Users with NCAR computing accounts have free access from the NCAR MSS through clicking the tab in the navigation bar.

For all others, costs depend on the amount requested, and the DSS standard charging rate applies unless their order qualifies for a substantially reduced charging rate, aka "direct copy rate" as shown on the service charges page.

We can extract a limited variety of subsets from the NCAR MSS files, such as whole grids or whole observations. This may greatly reduce our output charges, but not our input charges. Please inquire, but note that internal logical record reformatting or subsetting is usually not supported.

To send a data request to a staff member, please use this form.



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