Wind
Wind parameters available through the POWER API and DAV include wind speeds and direction at various heights above the surface. The user community choice determines the exact height availability.
Mean Wind Speed and Wind Direction Parameters
The wind speed and wind direction parameters are to be used to determine the mean wind flow of a region rather than local area due to effects of buildings and local topography.
Corrected Wind Speed¶
In addition to the wind speed parameters available at set heights above surface, the POWER API allows the user to request a wind speed at a user defined height (between 10 and 300 m) for a particular surface type.
Equation: Corrected Wind Speed (Adjusted For Elevation)
surface | Definition | surface | Definition |
---|---|---|---|
vegtype_1 | 35-m broadleaf-evergreen trees (70% coverage) | vegtype_7 | 0.6-m perennial ground cover (100%) |
vegtype_2 | 20-m broadleaf-deciduous trees (75% coverage) | vegtype_8 | 0.5-m broadleaf shrubs (variable %) & ground cover |
vegtype_3 | 20-m broadleaf and needleleaf trees (75% coverage) | vegtype_9 | 0.5-m broadleaf shrubs (10%) with bare soil |
vegtype_4 | 17-m needleleaf-evergreen trees (75% coverage) | vegtype_10 | Tundra: 0.6-m trees/shrubs (variable %) & ground cover |
vegtype_5 | 14-m needleleaf-deciduous trees (50% coverage) | vegtype_11 | Rough bare soil |
vegtype_6 | Savanna:18-m broadleaf trees (30%) & ground cover | vegtype_12 | Crop: 20-m broadleaf-deciduous trees (10%) & wheat |
vegtype_20 | Rough glacial snow/ice | sea ice | Smooth sea ice |
openwater | Open water | airport ice | Airport: flat ice/snow |
airportgrass | Airport: flat rough grass |
Wind Speed Validation¶
In this section, MERRA-2 10-meter wind speed is compared to observations reported to the National Center for Environmental Information (NCEI – formerly National Climatic Data Center). Selected surface sites from the NCEI Integrated Surface Database (ISD) files are used for the hourly MERRA-2 comparisons. Global "Summary of the Day" (GSOD) files are used for the comparison to the daily mean MERRA-2 temperature.
Hourly¶
Hourly Wind Speed
Density plot of the 2-D histograms comparing MERRA-2 hourly 10-meter wind speed with station observations from the selected NCEI ISD files for the years 2001 - 2019. Darker reds indicate a higher number of matched pairs within the 2-D histogram.
Daily Average¶
Daily Average 10-meter Wind Speed
Density plot of the 2-D histograms comparing MERRA-2 daily wind speed with station observations from the NCEI GSOD files for 1981 – 2020. Darker reds indicate a higher number of matched pairs within the 2-D histogram.
Wind Direction¶
Wind Direction at a given height in degrees as the meteorological convention. The meteorological convention gives the direction from which the wind originates and wind direction is measured in degrees clockwise from due north.
The computation of wind direction from MERRA-2 u and v components is based upon the information from NCAR/UCAR/EOL's quick reference on wind direction. Verification of the equations is accomplished with the usage of MERRA-2 10 meter winds from July 11, 2015; shown in this table:
Latitude | Longitude | u (ms-1) | v (ms-1) | direction |
---|---|---|---|---|
38.0°N | 80.0°W | 1.14718 | 0.00922 | 270.46° |
37.0°N | 79.0°W | 1.53487 | -0.89496 | 300.25° |
37.0°N | 76.5°W | -1.53666 | 0.21723 | 81.95° |
35.0°N | 75.5°W | 1.85421 | 2.19976 | 220.13° |
39.0°N | 77.5°W | -0.09501 | 1.50678 | 3.61° |
These locations are shown as the red circles on the streamline map here.
Hourly Wind Direction Validation¶
Hourly 10-meter Wind Direction Contingency Chart
Diagram of the hourly wind direction contingency comparison (shown as percentage) between MERRA-2 10-meter wind direction and the selected NCEI ISD files for the years 2001 - 2019. Hourly wind directions for both are categorized into octads, then 2-D histograms relate the directions to each other.
Click to Expand - Python Code
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Reference
Chandler, William S., C.H. Whitlock, P.W. Stackhouse, Jr., 2005: Determining Wind Resources as a Function of Surface Roughness and Height from NASA Global Assimilation Analysis. Proceedings of the International Solar Energy Society 2005 Solar World Congress, August 6-12, Orlando, Florida