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Investigating the diurnal variations in a local wind field

Experiment using the Doppler SODAR 24

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SODAR PCS2000-24 (at front) and SODAR PCS2000-64 (at back)
  

SODAR PCS2000-24
(front)
SODAR PCS2000-64
(back)
 











   

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Samples of Mobile Phase Doppler SODAR 24

Measured by NCAR (Boulder/US)

Drainage Flow from Narrow Valley

pcs200024sm.jpg (4590 bytes)
 

General
The mobile SODAR 24 was operated by NCAR within an experiment near Salt Lake City which investigates diurnal variations in the local wind field within the vicinity of a narrow valley formation. The SODAR data was used to validate windprofiler data of the lowest hundreds of meter. The SODAR system was powered by an electric generator.

The samples show a striking variation for inflow/outflow periods, the nocturnal reorganisation of the wind field occurs more rapidly and takes less than a hour. Over one week this pattern develops nearly identically in time and intensity.

Data Retrieval
Simultaneously instantaneous and averaged data were calculated by the SODAR. In addition to the mean spectra derived data an off-line cluster algorithm was applied on the instantaneous data for wind speed and wind direction derivation.

 

Main Operation Parameters

Ave = 900 Averaging Interval 900 s
Trans = 1674 Acoustic Frequency 1674 Hz
Step = 25 Height Steps 25 m
Hmin = 37.5 Start of Sampling 37.5 m
Hmax = 400 End of Sampling 400 m

 

Shown Samples
A one week period and 3 consecutive days are shown in the following plots. Wind speed and wind direction are shown as wind vectors on-line derived from mean spectra.

ncar1sm.jpg (2951 bytes) 
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Plot with data for the week
ncar2sm.jpg (2884 bytes)
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Plot with data from Day 1
(8 m/s west wind)
ncar3sm.jpg (1591 bytes)
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Plot with data from Day 2
(8 m/s west wind)
ncar4sm.jpg (1602 bytes)
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Plot with data from Day 3
(8 m/s west wind)

 

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E&OE