NCEP / NCAR Global Reanalysis Data

NCEP/NCAR Global Reanalysis Data Nodes:
Left = Nodes Covering Western Europe. Right = Nodes Covering France.

Data from the NCEP/NCAR reanalysis project is currently available to users of WindPRO as part of the on-line services from the EMD server. A connection to the internet is thus required. Users may download updated data from the present moment (typically the preceding month) back until 1948.

The sub-set of the NCEP/NCAR Global Reanalysis Data that we hold at EMD is updated on a monthly to bi-monthly update cycle.

Data Description

The NCEP/NCAR model dataset is immense, containing a very wide range of descriptive atmospheric model data. The actual measured climate data sources used in the global reanalysis model are:

• Upperair rawinsonde observations of temperature, horizontal wind, and specific humidity (i.e. weather balloons)
• Operational Television Infrared Observation Satellite (TIROS) Operational Vertical Sounder (TOVS) vertical temperature soundings from NOAA polar orbiters over ocean, with microwave retrievals excluded between 20°N and 20°S due to rain contamination
• TOVS temperature soundings over land only above 100 hPa
• Cloud-tracked winds from geostationary satellites
• Aircraft observations of wind and temperature
• Land surface reports of surface pressure
• Oceanic reports of surface pressure, temperature, horizontal wind, and specific humidity

These data are used as input into a frozen global assimilation system and processed by a spectral model in order to provide the model output of the variables in the grid.

NCEP/NCAR Global Reanalysis Dataset at EMD

Currently, two types of NCEP/NCAR modeled wind data are available from the EMD server. Both types of data are distributed through the NCAR_Basic dataset from the EMD server. The raw data are processed by EMD as the original data holds the vector components for the wind speeds only (U and V – winds). We convert the raw data into a format appropriate for use with wind turbine applications, i.e. wind speed and direction instead.

Table: Surface Data

Name	Description
Abbreviation	srf
External URL	http://www.cdc.noaa.gov/cdc/data.ncep.reanalysis.surface.html
Data valid at time	Instantaneous values at the reference time
Referred to as	“Wind" at level "sig995" under main title "Surface"
Level	99.5% of surface pressure (approximately 42m a.g.l. for standard atmosphere conditions)
Grid	2.5 degree latitude x 2.5 degree longitude global grid (144x73)
Coverage	Global
Columns in data-file	srf.dir.2 = Wind Direction at sigma level 0.995, i.e. 42 m a.g.l srf.wsp.2 = Wind Speed at sigma level 0.995, i.e. 42 m a.g.l gl.tmp.2 = Temperature at sigma level 0.995, i.e. at 42 m a.g.l

Table: 10 m Data

Name	Description
Abbreviation	u10
External URL	http://www.cdc.noaa.gov/cdc/data.ncep.reanalysis.surfaceflux.html
Data valid at time	Forecasts valid 6 hours after the reference time
Referred to as	"Wind at 10m" at level: "surface" under main title "Surface Fluxes"
Level	10 m above ground
Grid	T62 Gaussian grid with 192x94 points
Coverage	Global
Columns in data-file	u10.dir.10 = Forecast of Wind Direction at 10 m a.g.l u10.wsp.10 = Forecast of Wind Direction at 10 m a.g.l

You may learn more about these data by visiting the NCEP / NCAR web site holding the data at the URL http://www.cdc.noaa.gov or by reading the paper Kistler et al. (2001) published in Bulletin of the American Meteorological Society. The paper is available for free at: http://www.atmos.umd.edu/~ekalnay/Kistleretal.pdf).

Although the NCEP/NCAR data are simulations giving the “instantaneous values” every 6 hours, these are based on model simulation and there will be some “smoothening” compared to real measurements. We therefore recommend seeing the data as 10 min average values, although this is not specified as so in the documentation.

Converting Sigma Levels Coordinates into Physical Heights

Many of the NCEP / NCAR datasets are actually (internally) reported using sigma level coordinates. By definition, the sigma coordinate is the pressure at the current vertical level divided by the surface pressure level:

• EQUATION

Using the definition above, as well as the US standard atmosphere model - see the WindPRO manual on Air Density Adjustments) - it is possible to relate the sigma level coordinate to the physical height (by the assumption of the standard atmosphere parameters). This is shown in the figures below.

Figure: Transferring Sigma Levels into Physical Heights