Wind Characteristics in Mountainous Valleys Obtained through Field Measurement
Abstract
:Featured Application
Abstract
1. Introduction
2. Materials and Methods
3. Results
3.1. Mean Characteristics
3.1.1. Wind Direction for Mean Wind Speed
3.1.2. Wind Profile
3.1.3. Wind Attack Angle at Mean Wind Speed
3.2. Turbulence Characteristics
3.2.1. Turbulence Intensity
3.2.2. Gust Factor
3.2.3. Correlation between Turbulence Intensity and Gust Factor
3.2.4. Wind Power Spectrum
3.2.5. Turbulence Integral Scale
4. Conclusions
- (1).
- The results indicate that the wind profile index α is about 0.21, and the measuring locations are near the gentle hilly terrain. According to the Chinese specifications, the surface roughness coefficient for this terrain is 0.22, which is close to the measured value of 0.21. However, due to the influence of the complex topography of the area, the wind profile index α cannot fully indicate the surface roughness of the area. As shown in Figure 5, the wind profile data were divided into six forms. This does not match the exponential law. The distribution of wind attack angle in the measured low-altitude range is discrete, even reaching 20°, which is much larger than the ±3° recommended by the specifications. The frequency of negative wind attack angle is greater than that of positive wind attack angle. As height increases, the tendency toward negative tapping angles becomes more obvious. There is a strong correlation between the wind speed profile and the wind direction angle in the observed area. The distribution of wind speed with height in the main wind direction (NW) is well in accordance with the exponential law, while the distribution of wind profile data in other directions is disorganized and irregular.
- (2).
- The downwind turbulence intensity degree Iu on both sides of the river channel is about 13%, slightly greater than the 12% recommended value in the norm. However, the ratio of crosswind and downwind turbulence intensity Iv/Iu is 0.46, only 52% of the recommended value of the specification (0.88). This may be due to the topography resulting in the main wind direction (NW and WNW), accounting for a larger component of the incoming wind direction, which in turn results in a reduced degree of crosswind pulsation. We found a strong linear correlation between the gust factor Gu and the turbulence Iu during the observation period, with Gu increasing with the increase in Iu. There is a high turbulent component in the incoming wind velocity in these areas. The high-frequency energy is relatively large, while the low-frequency energy is relatively small. The existing empirical spectra do not provide an accurate description of the measured spectrum. Therefore, the Von Karman spectrum was used to fit the spectrum expressions with good applicability to the wind characteristics.
- (3).
- The turbulence integral scale on both sides of the river is relatively close, with a statistical mean value of 90 m. Almost half of the sample values had an value between 50 and 100 m.
- (4).
- According to the above analysis results, it can also be seen that the study of the wind characteristics of particular terrain requires special analysis and discussion. The conclusions drawn can then guide the design of the bridges.
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Conflicts of Interest
References
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Observation Place | Measuring Point Location | Height of Measuring Point or Measuring Range | Instrument Model | Sampling Frequency or Transmitting Frequency |
---|---|---|---|---|
Bridge site | Measuring point 1 | 33 m | 2D ultrasonic anemometer | 4 Hz |
Measuring point 2 | 33 m | 2D ultrasonic anemometer | 4 Hz | |
Measuring point 3 | 30~200 m | 3D Doppler radar | 4504 Hz |
Wind Speed Range (m/s) | [4,6] | [6,8] | [8,10] | [10,12] | [12,14] | [14,16] | [16,18] | [18,20] |
---|---|---|---|---|---|---|---|---|
Iv/Iu interval on the northeast side | 0.22~0.60 | 0.22~0.86 | 0.25~1.09 | 0.30~0.92 | 0.31~0.85 | 0.38~0.86 | 0.40~0.82 | 0.78~0.78 |
Mean value of Iv/Iu on the northeast side | 0.36 | 0.48 | 0.5 | 0.52 | 0.53 | 0.55 | 0.61 | 0.78 |
Iv/Iu interval on the southwest side | --- | 0.27~0.91 | 0.29~1.00 | 0.25~0.79 | 0.30~0.67 | 0.29~0.50 | 0.3~0.48 | 0.29~0.42 |
Mean value of Iv/Iu on the southwest side | --- | 0.48 | 0.46 | 0.44 | 0.42 | 0.41 | 0.37 | 0.36 |
Integral Scale (m) | Northeast Side Frequency | Southwest Side Frequency | Integral Scale (m) | Northeast Side Frequency | Southwest Side Frequency |
---|---|---|---|---|---|
[0–50] | 36.99 | 33.26 | [400–450] | 0.56 | 0.65 |
[50–100] | 39.29 | 37.95 | [450–500] | 0.39 | 0.48 |
[100–150] | 10.78 | 14.33 | [500–550] | 0.17 | 0.22 |
[150–200] | 4.78 | 5.78 | [550–600] | 0.11 | 0.09 |
[200–250] | 2.96 | 3.00 | [600–650] | 0.11 | 0.13 |
[250–300] | 1.75 | 2.04 | [650–700] | 0.07 | 0.00 |
[300–350] | 1.03 | 1.04 | [700–750] | 0.05 | 0.09 |
[350–400] | 0.92 | 0.87 | [750–800] | 0.03 | 0.04 |
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Wang, F.; Chen, X.; He, R.; Liu, Y.; Hao, J.; Li, J. Wind Characteristics in Mountainous Valleys Obtained through Field Measurement. Appl. Sci. 2021, 11, 7717. https://doi.org/10.3390/app11167717
Wang F, Chen X, He R, Liu Y, Hao J, Li J. Wind Characteristics in Mountainous Valleys Obtained through Field Measurement. Applied Sciences. 2021; 11(16):7717. https://doi.org/10.3390/app11167717
Chicago/Turabian StyleWang, Feng, Xinming Chen, Rui He, Yan Liu, Jianming Hao, and Jiawu Li. 2021. "Wind Characteristics in Mountainous Valleys Obtained through Field Measurement" Applied Sciences 11, no. 16: 7717. https://doi.org/10.3390/app11167717
APA StyleWang, F., Chen, X., He, R., Liu, Y., Hao, J., & Li, J. (2021). Wind Characteristics in Mountainous Valleys Obtained through Field Measurement. Applied Sciences, 11(16), 7717. https://doi.org/10.3390/app11167717