The main requirement is that the measurements are representative for an area or an air volume covered by the foreseen devices for power generation. For instance, wind measurements often have to be performed at exposed sites, such as hilltops.
Users of wind speed measurement data for the assessment of available wind energy often request a rather high accuracy in the order of 1%, because wind energy depends on the third power of the wind speed (51.1). A 1%-error in wind speed thus means up to 3% error in wind energy.
Irradiance is given in units of W m −2 within a ±25 W m −2 interval. Courtesy of Birk Kraas, CSPS Services, Stefan Wilbert, DLR Measurement techniques for atmospheric parameters at hub height of wind turbines and over the area swept by their rotors have changed. In-situ measurements by cup and sonic anemometers are no longer fully sufficient.
Please note, that wind data from remote sensing and in-situ measurements are not fully comparable due to the different measurement principles (cup anemometers are in-situ instruments; sodars and wind lidars are volume-averaging instruments). Specifications of solar energy related instruments are also included in Table 51.3.
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