超聲波傳感器雪深測量與人工觀測對比試驗分析
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Comparison and Analysis of Snow Depth Records Obtained by Manual Observation and Ultrasonic Sensor in Different Weather Conditions
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    摘要:

    通過對2010年2、3月佳木斯國家基準氣候觀測站人工觀測與超聲波雪深傳感器測量獲取數據對比、分析不同天氣條件下(高風速、低風速、低溫度)兩種方法獲得的數據差值的變化情況。結果表明:觀測結果差異的大小主要受溫度和風速兩個因素的影響。低溫環境下溫度會影響超聲波的行程時間使得超聲波傳感器的測量精度受到影響,通過溫度補償的方法對雪深進行訂正可以提高超聲波傳感器的測量精度,兩者的差值較小,且觀測資料有較好的可比性;高風速時,風速會影響超聲波脈沖,使其偏離傳感器的下方,同時超聲波的速度也會受到影響,從而影響測量結果,使得兩者的差值較大。

    Abstract:

    An introduction is made to the principles and measuring method of the ultrasonic snow depth sensor. Based on the snow depth data observed by the two methods, ultrasonic sensor and manual observation in the Jiamusi national reference climatological station,comparison and analysis are made in different weather conditions (high wind velocity, low wind velocity, low temperature). The results show that the differences are mainly influenced by wind velocity and temperature. At high wind velocity, the ultrasonic pulses are greatly affected by wind speed, leading to the departure of the ultrasonic pulses from the bottom of the ultrasonic sensor; meanwhile, the speed of ultrasound pulses is also affected, and thus, the measurement results are affected. The travel time of ultrasonic pulses is affected by the temperature, so when the temperature was extremely low, the performance of ultrasonic sensors is obviously affected.

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梁延偉,梁海河,王柏林.超聲波傳感器雪深測量與人工觀測對比試驗分析[J].氣象科技,2012,40(2):198~202

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  • 收稿日期:2010-09-09
  • 定稿日期:2011-03-16
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  • 在線發布日期: 2012-04-23
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