Deprecated: The each() function is deprecated. This message will be suppressed on further calls in /home/zhenxiangba/zhenxiangba.com/public_html/phproxy-improved-master/index.php on line 456
JPH079469B2 - Snow depth measuring device - Google Patents
[go: Go Back, main page]

JPH079469B2 - Snow depth measuring device - Google Patents

Snow depth measuring device

Info

Publication number
JPH079469B2
JPH079469B2 JP62171159A JP17115987A JPH079469B2 JP H079469 B2 JPH079469 B2 JP H079469B2 JP 62171159 A JP62171159 A JP 62171159A JP 17115987 A JP17115987 A JP 17115987A JP H079469 B2 JPH079469 B2 JP H079469B2
Authority
JP
Japan
Prior art keywords
peak time
time
snow
value
predicted
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Expired - Lifetime
Application number
JP62171159A
Other languages
Japanese (ja)
Other versions
JPS6415692A (en
Inventor
正道 安藤
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
KI Holdings Co Ltd
Original Assignee
Koito Industries Ltd
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by Koito Industries Ltd filed Critical Koito Industries Ltd
Priority to JP62171159A priority Critical patent/JPH079469B2/en
Publication of JPS6415692A publication Critical patent/JPS6415692A/en
Publication of JPH079469B2 publication Critical patent/JPH079469B2/en
Anticipated expiration legal-status Critical
Expired - Lifetime legal-status Critical Current

Links

Landscapes

  • Measurement Of Levels Of Liquids Or Fluent Solid Materials (AREA)
  • Measurement Of Velocity Or Position Using Acoustic Or Ultrasonic Waves (AREA)

Description

【発明の詳細な説明】 〔産業上の利用分野〕 この発明は、気象観測等のため積雪量を測定する積雪深
測定装置に関するものである。
TECHNICAL FIELD The present invention relates to a snow depth measuring device for measuring the amount of snow for weather observation and the like.

〔従来の技術〕[Conventional technology]

従来、気象観測項目の中に積雪量の測定があり、これは
地面に設けた測定尺により目測で測定する方法と、超音
波の往復伝搬時間から求める方法があり、後者は自動測
定に適している。超音波による方法は、ある一定の受信
検出レベルを設け、雪面からの超音波反射波がこのレベ
ルを越えた時点を検出し、送信した時刻から受信した時
刻までの時間差により測定をする受信時刻検出方法と、
受信波形のピーク点を検出し、送信した時刻から受波ピ
ーク時刻までの時間差により測定するピーク時刻検出方
法とがある。
Conventionally, there is a measurement of the amount of snow in the meteorological observation items.There are a method of measuring by snow with a measuring scale installed on the ground and a method of obtaining from the round-trip propagation time of ultrasonic waves, the latter is suitable for automatic measurement. There is. The ultrasonic method provides a certain level of reception detection, detects the time when the reflected ultrasonic wave from the snow surface exceeds this level, and measures the time difference from the time of transmission to the time of reception. Detection method,
There is a peak time detection method in which the peak point of the received waveform is detected and measured by the time difference from the time of transmission to the time of the received peak.

〔発明が解決しようとする問題点〕[Problems to be solved by the invention]

しかしながら受信時刻検出方法は、積雪量が一定でも雪
質、風等によつて反射レベルが変化すると、受信検出レ
ベルを越える時刻が変化するため計測誤差が生じ、また
積雪面が柔らかい場合、超音波が雪に吸収され、表面か
らの反射波が非常に少なくなることでも計測誤差を生じ
る。一方、ピーク時刻検出方法は、柔かい積雪面を測定
するとき、送波した超音波は雪面内部にも入り込み、反
射波は表面だけでなく、その下層の固くなつた雪面から
も生じるので、その合成された信号を受信することにな
り、表面だけからの反射よりピーク時刻が遅れ、計測誤
差が生じるという問題がある。
However, the reception time detection method requires a measurement error when the reflection level changes due to snow quality, wind, etc. even if the amount of snowfall is constant, and the measurement error occurs when the snowfall surface is soft. It is also absorbed by snow and the reflected wave from the surface becomes very small, which causes a measurement error. On the other hand, the peak time detection method, when measuring a soft snow surface, the transmitted ultrasonic waves enter the inside of the snow surface, and the reflected wave is generated not only from the surface but also from the hard snow surface below it, Since the combined signal is received, there is a problem that the peak time is delayed from the reflection from only the surface and a measurement error occurs.

〔問題点を解決するための手段〕[Means for solving problems]

このような問題を解決するためにこの発明は、反射波の
受信時刻からのピーク時刻を予測し、この予測ピーク値
をもとに補正した値と、実測値のうち短かい方を検出値
とするものである。
In order to solve such a problem, the present invention predicts the peak time from the reception time of the reflected wave, corrects the value based on this predicted peak value, and the measured value, whichever is shorter, is the detected value. To do.

〔作用〕[Action]

受信レベルが平常値のときは受信レベルに応じてあらか
じめ決められている値を加えた値を予測ピーク時刻と
し、受信レベル値が路面反射より極端に小さいときは前
述のあらかじめ決められた値を加えたものに例えば、積
雪2cmに相当する120μsを引いた値を予測ピーク時刻と
し、予測ピーク時刻と実測ピーク時刻とのいずれか小さ
い方を最終的なピーク値とし、そのピーク時刻をもとに
積雪量を測定するものである。
When the reception level is a normal value, a value that is added in advance according to the reception level is used as the predicted peak time, and when the reception level value is extremely smaller than the road surface reflection, the above-mentioned predetermined value is added. For example, the value obtained by subtracting 120 μs corresponding to 2 cm of snow is used as the predicted peak time, and the smaller of the predicted peak time and the actually measured peak time is used as the final peak value, and the snow accumulation is based on that peak time. It is a measure of quantity.

〔実施例〕〔Example〕

第2図はこの方法を適用して構成した装置の一例であ
り、1は送受波器、2は送波駆動回路、3は送受波タイ
ミング発生回路、4はCPU、5は受波増幅回路、6は検
波回路、7a,7bはA/D変換回路、8は温度検出器、9は増
幅回路、10は出力回路、11はLED表示回路、12は水晶振
動子、13はRAM、14はROM、15は送受波器取付高さ設定ス
イッチである。なお出力回路は記号Aで示すアナログ出
力、記号Dで示すデイジタル出力、記号Tで示すテレメ
ータ出力を送出するようになつている。
FIG. 2 is an example of an apparatus configured by applying this method. 1 is a wave transmitter / receiver, 2 is a wave transmission drive circuit, 3 is a wave transmission / reception timing generation circuit, 4 is a CPU, 5 is a wave reception amplification circuit, 6 is a detection circuit, 7a and 7b are A / D conversion circuits, 8 is a temperature detector, 9 is an amplification circuit, 10 is an output circuit, 11 is an LED display circuit, 12 is a crystal oscillator, 13 is RAM, and 14 is ROM. , 15 are transducer height mounting switches. The output circuit outputs an analog output indicated by the symbol A, a digital output indicated by the symbol D, and a telemeter output indicated by the symbol T.

第3図は第1図に示す回路の各部波形図で、(A)〜
(E)は第1図に付したA〜Eの記号の部分の波形であ
る。
FIG. 3 is a waveform chart of each part of the circuit shown in FIG.
(E) is a waveform of the part of the symbols A to E attached to FIG.

このように構成された装置はCPU4の制御によつて第1図
に示す動作を行なう。先ず、S50に示すように超音波の
送波を行なうが、これは例えば周波数26kHz,パルス幅1m
s,繰返し周期100msの超音波を用い雪面に向けて送信す
る。送波された超音波は雪面で反射され、S51に示すよ
うに反射波が測定され、S52に示すように送波から受波
までの往復所要時間が測定される。S52の処理はS520〜S
526に詳細に示しているが、S520に示すように「受信タ
イミング開始?」において受信タイミングか否かの判定
が行なわれる。受信タイミングとは第4図(a)に示す
送信タイミングに対し、第4図(b)に示すように、例
えば送波後10ms後に40msだけ受信ゲートを開き、受信パ
ルスを取込むためのタイミングである。
The device thus constructed performs the operation shown in FIG. 1 under the control of the CPU 4. First, as shown in S50, ultrasonic waves are transmitted, which has a frequency of 26 kHz and a pulse width of 1 m, for example.
s, ultrasonic waves with a repetition period of 100 ms are transmitted toward the snow surface. The transmitted ultrasonic wave is reflected on the snow surface, the reflected wave is measured as shown in S51, and the round-trip time required from the transmitted wave to the received wave is measured as shown in S52. S520 processing is S520 ~ S
As shown in detail in 526, it is determined whether or not it is the reception timing in "reception timing start?", As shown in S520. As shown in FIG. 4 (b), the reception timing is, for example, the timing for opening the reception gate for 40 ms 10 ms after the transmission to take in the reception pulse with respect to the transmission timing shown in FIG. 4 (a). is there.

S520が「NO」であればそのステップに止どまり、「YE
S」となつた時点でS521に示すような受信ゲートを通過
した信号のサンプリングが行なわれる。このサンプリン
グは例えば50μs毎に行なわれ、サンプリングされた信
号はA/D変換され、RAM13に供給される。この処理はS522
の「受信タイミング終了?」が「NO」の間行なわれ、S5
22が「YES」と判定されるとS523においてピーク時刻tp1
の検索が行なわれる。この検索はRAM13に格納したデー
タの中からピーク値を受信した時刻を見出すことによつ
て行なわれる。
If S520 is "NO", then stop at that step and select "YE
When "S" is reached, the signal passing through the reception gate is sampled as shown in S521. This sampling is performed, for example, every 50 μs, and the sampled signal is A / D converted and supplied to the RAM 13. This process is S522
“Reception timing end?” Is performed for “NO”, and S5
If 22 is determined to be "YES", the peak time tp 1 in S523.
Is searched. This search is performed by finding out the time when the peak value is received from the data stored in the RAM 13.

次にS524に示すように、予測ピーク時刻tp2の計算を行
なう。この計算は受信信号のピーク値に比例して決まる
次の値を受信信号の始まり時刻に加算する。
Next, as shown in S524, the predicted peak time tp 2 is calculated. This calculation adds the next value, which is proportional to the peak value of the received signal, to the start time of the received signal.

これは受信信号の大きさが0〜10Vの範囲であることお
よび、固い雪面の場合でも受信信号の大きさは伝搬路の
状態によつて第5図のように変化するが、ピーク値に達
するまでの受信信号の立上り時間tは受信信号の大きさ
にかかわらず略一定の1ms位である。一方、第6図に示
すようにスレシホールドレベルLを越える時刻、すなわ
ち受信信号の始まり時刻は受信信号の大きさによつて変
わり、受信信号の大きさが大きいときはスレシホールド
レベルを越えてからピークになるまでの時間は長く、小
さいときは短かい。このため、ピーク値の大きさに応じ
て、受信信号の始まり時刻に前述の値を加えれば、受信
ピーク時刻が予測できる。
This is because the magnitude of the received signal is in the range of 0 to 10V, and the magnitude of the received signal changes as shown in Fig. 5 depending on the state of the propagation path even on a hard snow surface. The rising time t of the received signal until reaching the time is approximately constant 1 ms regardless of the size of the received signal. On the other hand, as shown in FIG. 6, the time at which the threshold level L is exceeded, that is, the start time of the received signal changes depending on the size of the received signal. When the received signal is large, the threshold level is exceeded. It takes a long time to reach the peak from the beginning and a short time when it is small. Therefore, the reception peak time can be predicted by adding the above value to the start time of the reception signal according to the magnitude of the peak value.

受信ピーク時刻を予測するのは次のような理由による。
雪が何層にもわたり積つているときはそれぞれの層から
反射波が発生するので受信波形は第7図の点線で示すよ
うないくつものピークが発生し、これを検波すると実線
のような波形となる。図中、記号「ア」の時刻は雪の表
面からの受信時刻に略等しくなるが、記号「イ」の時刻
は雪面表面より数cm下部からの受信時刻になる。但し、
反射レベルが非常に小さいときは二点鎖線のような検波
波形となり「ア」の点が検出できず「ウ」の点しか観測
できず誤差が生ずる。このため反射波レベルが非常に小
さいときは予測ピーク時刻に補正を加えている。
The reason for predicting the peak reception time is as follows.
When snow is piled up over many layers, reflected waves are generated from each layer, so the received waveform has several peaks as shown by the dotted line in Fig. 7. When this is detected, the waveform looks like the solid line. Become. In the figure, the time indicated by the symbol "a" is approximately equal to the time received from the surface of the snow, while the time indicated by the symbol "a" is the time received from a few cm below the surface of the snow surface. However,
When the reflection level is very small, the detection waveform becomes like a chain double-dashed line, and the point "A" cannot be detected, and only the point "C" can be observed, resulting in an error. For this reason, when the reflected wave level is very small, the predicted peak time is corrected.

一方、雪面が柔らかな場合、表面からの反射波はほとん
どないため、反射波は内部からのものとなり、一般に前
述の方法で予測した予測ピーク時刻から求めた積雪は真
値より数cm低く計測される。このとき、反射波のレベル
に着目すると路面に雪がないときの反射波に比べ数10分
の1以下になつていることが多い。このように、反射波
のレベルが雪のないときの路面反射波に比べ例えば1/30
以下の時は、計測値が真値より2cm程度低くなることが
予測されるため、積雪2cmに相当する時間120μsを前述
の予測ピーク時刻から引いた値を予測ピーク時刻とす
る。
On the other hand, when the snow surface is soft, there is almost no reflected wave from the surface, so the reflected wave comes from the inside, and the snowfall obtained from the predicted peak time predicted by the above method is generally measured several cm lower than the true value. To be done. At this time, focusing on the level of the reflected wave, it is often several tenths or less that of the reflected wave when there is no snow on the road surface. In this way, the level of the reflected wave is, for example, 1/30 of that of the road surface reflected wave when there is no snow.
In the following cases, the measured value is predicted to be about 2 cm lower than the true value, so the value obtained by subtracting 120 μs, which corresponds to 2 cm of snow from the predicted peak time, is the predicted peak time.

S523,S524によつてピーク時刻が求められたら、S525に
よつてピーク時刻tp1と予測ピーク時刻tp2を比較する。
ここで、積雪は通常、真値より低目に計測されることが
あつても、高目に計測されることはないので、S525にお
いては短かい方の値をここで用いるピーク時刻として決
定する。
When the peak time is obtained by S523 and S524, the peak time tp 1 and the predicted peak time tp 2 are compared by S525.
Here, snowfall is usually measured lower than the true value but not higher, so in S525, the shorter value is determined as the peak time used here. .

ピーク時刻が決定したらこのデータと、S526において求
められた気温をもとに、S53において積雪計算処理を行
なう。これは送受波器取付高さ設定スイツチのデータを
H、送波から受波までの時間をtp、送受波器から雪面ま
での距離をl、音速をV、積雪をD気温をTとすると、
次の処理で求められる。
When the peak time is determined, snow cover calculation processing is performed in S53 based on this data and the temperature obtained in S526. This is, assuming that the data of the transducer mounting height setting switch is H, the time from transmission to reception is tp, the distance from the transducer to the snow surface is 1, the speed of sound is V, and the snowfall is D, the temperature is T. ,
It is calculated by the following process.

l=V×Tp/2 D=H−l V=331.45+0.61T この処理が終了するとS54に示すように有効・無効デー
タ判定処理が行なわれる。これは外乱雑音による誤計測
を避けるためで、具体的にはS540において次式によつて
有効データかどうか判定している。
l = V * Tp / 2 D = H-1 V = 331.45 + 0.61T When this process is completed, the valid / invalid data determination process is performed as shown in S54. This is to avoid erroneous measurement due to disturbance noise. Specifically, in S540, it is determined by the following equation whether the data is valid data.

x−D<y<x+D これは現在出力している過去N個の平均データx(cm)
に対して新たに計測した積雪y(cm)が上下限範囲内に
あるか否かを判定するもので、Dは1〜99(cm)の範囲
で任意に設定できる値であり、上下限範囲外のデータを
無効データとする。
x−D <y <x + D This is the past N average data x (cm) that is currently output.
Is to determine whether or not the newly measured snowy y (cm) is within the upper and lower limit range, and D is a value that can be arbitrarily set in the range of 1 to 99 (cm). The outside data is invalid data.

有効データのときはS55において積雪値統計処理が行な
われるが、これは計測値が風その他の外乱等によつて刻
々と細かく変動することを防ぐもので、有効と判定した
過去N個のデータのうち、一番古い計測値と最新の計測
値を入換え、平均を求める。この平均値を最終の計測値
とし、平均値算出方法は移動平均値法とする。
In the case of valid data, the snow value statistical processing is performed in S55, but this prevents the measured values from fluctuating minutely due to wind and other disturbances. Among them, replace the oldest measured value with the latest measured value and calculate the average. This average value is used as the final measurement value, and the average value calculation method is the moving average value method.

無効データのときはS56において無効データ統計処理が
行なわれるが、これは無効性のチエツクのためのもの
で、無効と判定したデータが連続してN個に達したと
き、その分散を求めることによつて行なう。そして、無
効データの分散と、有効データの分散を比較し、無効デ
ータの分散がより小さい場合、無効データと有効データ
の入換を行なう。
In case of invalid data, the invalid data statistical processing is carried out in S56, but this is for checking the invalidity, and when the number of data judged to be invalid reaches N consecutive times, the variance is calculated. I will do it. Then, the variance of invalid data and the variance of valid data are compared. If the variance of invalid data is smaller, the invalid data and valid data are exchanged.

以上の処理が終了すると、S57に示す出力処理が行なわ
れ、表示出力信号、アナログ出力信号、デイジタル出力
信号が送出される。
When the above process ends, the output process shown in S57 is performed, and the display output signal, the analog output signal, and the digital output signal are sent out.

なお、本発明は積雪量測定の場合について述べたが、以
上の説明から、明らかなように反射面が雪でなく、粉体
のように柔らかく超音波の一部を吸収するような物のレ
ベルを測定する場合にも有効である。
Although the present invention has been described for the case of measuring the amount of snow, from the above description, it is clear that the reflecting surface is not snow, but the level of an object that is soft like powder and absorbs a part of ultrasonic waves. It is also effective when measuring.

〔発明の効果〕〔The invention's effect〕

以上説明したようにこの発明は、実測したピーク時刻
か、予測ピーク時刻のいずれか短い方の値によつて測定
を行なうようにしたので、従来のように雪面が柔らかい
ときの測定誤差がなくなるという効果を有する。
As described above, according to the present invention, the measurement is performed using the measured peak time or the predicted peak time, whichever is shorter. Therefore, there is no measurement error when the snow surface is soft as in the conventional case. Has the effect.

【図面の簡単な説明】[Brief description of drawings]

第1図はこの発明の一実施例を示すフローチャート、第
2図はこの発明を適用して構成した装置の一例を示すブ
ロツク図、第3図は各部波形図、第4図は送信タイミン
グと受信タイミングの関係を示す図、第5図は信号レベ
ルとピーク時刻との関係を示す図、第6図は信号レベル
とスレシホールドレベルとの関係を示す図、第7図は受
信波形を示す図である。 1……送受波器、3……送受波タイミング発生回路、4
……CPU、5……受波増幅回路。
FIG. 1 is a flow chart showing an embodiment of the present invention, FIG. 2 is a block diagram showing an example of an apparatus configured by applying the present invention, FIG. 3 is a waveform chart of each part, FIG. 4 is transmission timing and reception. FIG. 5 is a diagram showing the relationship between timings, FIG. 5 is a diagram showing the relationship between signal levels and peak times, FIG. 6 is a diagram showing relationships between signal levels and threshold levels, and FIG. 7 is a diagram showing received waveforms. Is. 1 ... Transceiver, 3 ... Transmit / receive timing generation circuit, 4
…… CPU, 5 …… Received amplifier circuit.

Claims (1)

【特許請求の範囲】[Claims] 【請求項1】超音波反射波のピーク時刻から積雪量を測
定する積雪深測定装置において、受信信号がスレシホー
ルドレベルを越えた時刻に対し受信信号のピークレベル
に比例して決まる所定時間を計測する第1の予測ピーク
時刻計測手段と、第1の予測ピーク時刻に補正値を加え
た値を演算する第2の予測ピーク時刻計測手段と、受信
信号のレベルが所定値以上のときは第1の予測ピーク時
刻を予測ピーク時刻とし,受信信号のレベルが所定値未
満のときは第2の予測ピーク時刻を予測ピーク時刻と
し,予測ピーク時刻と実測したピーク時刻のうち短かい
方の値をピーク時刻として採用する予想ピーク時刻決定
手段とを備えたことを特徴とする積雪深測定装置。
1. In a snow depth measuring device for measuring the amount of snow from the peak time of an ultrasonic reflected wave, a predetermined time is determined in proportion to the peak level of the received signal with respect to the time when the received signal exceeds a threshold level. A first predicted peak time measuring means for measuring, a second predicted peak time measuring means for calculating a value obtained by adding a correction value to the first predicted peak time, and a first predicted peak time measuring means when the level of the received signal is equal to or higher than a predetermined value. The predicted peak time of 1 is set as the predicted peak time, and when the level of the received signal is less than the predetermined value, the second predicted peak time is set as the predicted peak time, and the shorter of the predicted peak time and the measured peak time is set. A snow depth measuring device, comprising: an expected peak time determining means to be used as a peak time.
JP62171159A 1987-07-10 1987-07-10 Snow depth measuring device Expired - Lifetime JPH079469B2 (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
JP62171159A JPH079469B2 (en) 1987-07-10 1987-07-10 Snow depth measuring device

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP62171159A JPH079469B2 (en) 1987-07-10 1987-07-10 Snow depth measuring device

Publications (2)

Publication Number Publication Date
JPS6415692A JPS6415692A (en) 1989-01-19
JPH079469B2 true JPH079469B2 (en) 1995-02-01

Family

ID=15918082

Family Applications (1)

Application Number Title Priority Date Filing Date
JP62171159A Expired - Lifetime JPH079469B2 (en) 1987-07-10 1987-07-10 Snow depth measuring device

Country Status (1)

Country Link
JP (1) JPH079469B2 (en)

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH11211846A (en) * 1998-01-22 1999-08-06 Yokogawa Electric Corp Snow depth gauge

Families Citing this family (2)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JP6986076B2 (en) * 2016-09-22 2021-12-22 シグニファイ ホールディング ビー ヴィSignify Holding B.V. Flood location and notification via intelligent lighting
JP7604003B2 (en) 2022-06-14 2024-12-23 株式会社Blossom Energy Nuclear Reactor Systems

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH11211846A (en) * 1998-01-22 1999-08-06 Yokogawa Electric Corp Snow depth gauge

Also Published As

Publication number Publication date
JPS6415692A (en) 1989-01-19

Similar Documents

Publication Publication Date Title
CA1238110A (en) Method and arrangement for signal transmission in ultrasonic echo sounding systems
EP1770409B1 (en) Time-of-flight-ranging system and method for calibrating such a system
JP2859514B2 (en) Doppler shift correction pulse type fishing net depth gauge
JPH0568668B2 (en)
KR20000057568A (en) Method and device for ultrasonic ranging
EP0142733A2 (en) Ultrasonic rangefinder
JPH079469B2 (en) Snow depth measuring device
RU2123191C1 (en) Echo sounder
RU2002133946A (en) METHOD OF DISTANCE MEASUREMENT (OPTIONS)
JPH0760187B2 (en) Road area snow depth meter
JPH08201514A (en) Ultrasonic distance measuring device
RU2032154C1 (en) Ultrasonic level meter
JPH09218033A (en) Snow depth measuring device
JP3709751B2 (en) Ultrasonic level meter
JP3296985B2 (en) Ultrasonic snow gauge
JPS59111074A (en) Apparatus for sensing moving matter
JPH03180794A (en) Method and instrument for ultrasonic distance measurement
JP2856042B2 (en) Radar equipment for vehicles
JPS6239337Y2 (en)
JP2801997B2 (en) Tidal current measurement method
JPH0534193A (en) Ultrasonic transmitter-receiver
JP3044146B2 (en) Distance measuring device
JPH1164516A (en) Ultrasonic snow depth gauge
JP2546716Y2 (en) Ultrasonic radar
JPH0882673A (en) Ultrasonic distance-measuring apparatus

Legal Events

Date Code Title Description
EXPY Cancellation because of completion of term
FPAY Renewal fee payment (event date is renewal date of database)

Free format text: PAYMENT UNTIL: 20080201

Year of fee payment: 13