JPH0460490A - Rain/snow discrimination - Google Patents

Rain/snow discrimination

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Publication number
JPH0460490A
JPH0460490A JP17159490A JP17159490A JPH0460490A JP H0460490 A JPH0460490 A JP H0460490A JP 17159490 A JP17159490 A JP 17159490A JP 17159490 A JP17159490 A JP 17159490A JP H0460490 A JPH0460490 A JP H0460490A
Authority
JP
Japan
Prior art keywords
rain
temperature
snow
value
difference
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.)
Granted
Application number
JP17159490A
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Japanese (ja)
Other versions
JP2907500B2 (en
Inventor
Masanao Anzai
安斎 正直
Tatsunosuke Takemoto
武本 達之助
Shigeo Yamazaki
茂雄 山崎
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Meisei Electric Co Ltd
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Meisei Electric Co Ltd
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Application filed by Meisei Electric Co Ltd filed Critical Meisei Electric Co Ltd
Priority to JP17159490A priority Critical patent/JP2907500B2/en
Publication of JPH0460490A publication Critical patent/JPH0460490A/en
Application granted granted Critical
Publication of JP2907500B2 publication Critical patent/JP2907500B2/en
Anticipated expiration legal-status Critical
Expired - Fee Related legal-status Critical Current

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Abstract

PURPOSE:To enable an en bloc treatment of kinds of meteorological observation data and rain/snow discrimination by comparing a judgement value defined by comparison of the maximum temperature variance of stored water surface periphery of a rain gauge during a certain time duration, to a precipitation amount during the same period, to a standard value. CONSTITUTION:A signal processing system is provided with two temperature measuring parts 10 and 11, a difference signal circuit 12 that outputs temperature difference data from the temperature difference measured by the temperature measuring parts 10 and 11, a signal processing part 13 that discriminates rain or snow based upon the temperature difference data from the circuit 12 and precipitation data from a over-turn measure 3, a recording part 14 that records the data processed by the processing part 13, and a judgment standard value setting part 15. The temperature measuring parts 10 and 11 output oscillation signal of corresponding frequency to the temperature which is measured by temperature sensors 6 and 7, and the like. The difference signal circuit 12 outputs signal of which frequency is equivalent to frequency difference between output signal frequencies of oscillation circuits 8 and 9 of the temperature measuring parts 10 and 11 and thereafter directly outputs the measured temperature difference data of the sensors 6 and 7. The signal processing part 13 is mainly constituted of a CPU, calculates the judgement value by a predetermined equation, compares the judgement value to a standard value, conducts rain/snow discrimination and finally outputs judgement result to the recording part 14.

Description

【発明の詳細な説明】 (産業上の利用分野) 本発明は降水があったとき、当該降水が雨であるか雪で
あるかを判定するための雨雪判別方法に関する。
DETAILED DESCRIPTION OF THE INVENTION (Industrial Application Field) The present invention relates to a rain/snow discrimination method for determining whether the precipitation is rain or snow when there is precipitation.

(先行する技術) 本件出願の比願人は、先に特願昭62−132832号
(特開昭64−485号)に於いて、例えば溢水式雨量
計(雨水貯留槽に一定しベルまで常時雨水を溜めておく
構造の雨量計)の貯留水面近傍に設けた温度センサによ
り測定した一定時間内の温度変化傾向又は当該貯留水面
近傍に設けた一対の温度センサにより測定した温度差傾
向により、雨雪判別を行なう方法を提案した。
(Prior Art) The applicant of the present application previously proposed in Japanese Patent Application No. 62-132832 (Japanese Unexamined Patent Publication No. 64-485) that, for example, an overflow rain gauge (a rainwater storage tank with a constant up to a bell) A rain gauge with a structure that collects rainwater) has a temperature change trend within a certain period of time measured by a temperature sensor installed near the stored water surface, or a temperature difference trend measured by a pair of temperature sensors installed near the stored water surface. We proposed a method for snow discrimination.

この方法に於いて、雨雪判別の最終判断は、温度変化又
は温度差をプロットしたアナログ的波形の経験的観察に
よっている。
In this method, the final judgment on rain/snow discrimination is based on empirical observation of analog waveforms plotting temperature changes or temperature differences.

(発明が解決しようとする課題) 上記先行技術では、雨雪判別の最終的判断は、処理装置
から出力される観測波形の観察によっているため雨雪判
別速度が遅くなり、かつ雨g判別のコンピュータによる
自動処理、自動記録等が困難であるという問題点がある
(Problems to be Solved by the Invention) In the above-mentioned prior art, the final judgment of rain and snow discrimination is based on observation of the observed waveform output from the processing device, so the speed of rain and snow discrimination is slow, and the rain g discrimination There is a problem that automatic processing, automatic recording, etc. are difficult.

本発明は以上の問題点を解決すへく提案するものてあり
、コンピュータによる雨雪判別の自動化を可能とする雨
雪判別方法を得ることを課題とするものである。
The present invention has been proposed to solve the above-mentioned problems, and an object of the present invention is to provide a rain/snow discrimination method that enables automation of rain/snow discrimination using a computer.

(発明の開示) 本発明の発明者は、雨水貯留槽の貯留水面近傍の比較的
近距離にある2点の測定点間の一定時間内に於ける最大
温度差変化(温度差の最大値と最小値の差)、又は当該
貯留水面近傍の1測定点の一定時間内での最大温度変化
(測定温度の最大値と最小値の差)と、そのとぎの降水
量とを、降雨時及び降雪時に多数測定し、測定結果を分
析した結果、上記最大温度差変化又は最大温度変化は降
雨又は降雪の違いと相関することはもとより、降水量と
も相関関係を持ち、かつ上記最大温度差変化又は最大温
度変化と降雨量との比が、降雨時と降雪時とでは、高い
精度で区分し得ることを見出した。
(Disclosure of the Invention) The inventor of the present invention has discovered that the maximum temperature difference change (maximum value of temperature difference and (difference between the minimum value) or the maximum temperature change (difference between the maximum and minimum measured temperature) at one measurement point near the reservoir water surface within a certain period of time, and the amount of precipitation at that time. As a result of taking multiple measurements and analyzing the measurement results, we found that the above maximum temperature difference change or maximum temperature change not only correlates with the difference in rainfall or snowfall, but also has a correlation with the amount of precipitation. We found that the ratio between temperature change and rainfall amount can be classified with high accuracy between rainy and snowy periods.

すなわち、上記最大温度差変化又は最大温度変化をΔT
とし、一定時間内の降水量をRとしたとき、次式 %式%(1) て定義される判定値Sと、降雨又は降雪か観察された回
数との関係をグラフに示すと第1図のようになり(但し
、第1図はΔTとして一対の温度センサによって測定さ
れた最大温度差変化を使用して判定値Sを求めたもので
ある。)、この第1図で明らかなように、判定値Sが約
1.0のとき降雨と降雪の観測回数がほぼ等しく、判定
値が約1.0以下となると降雨の観測回数が多くなり、
約1.0以上になると降雪の観測回数が多くなる如く、
観測回数の分布が降雨時と降雪時とで明確に区別し得る
。このことから判定値Sについて基準値S0を定め、降
水時の判定値Sと上ご己基準値S0との比較により雨雪
判別が可能となる。
In other words, the maximum temperature difference change or maximum temperature change is ΔT
When the amount of precipitation within a certain period of time is R, the relationship between the judgment value S defined by the following formula % formula % (1) and the number of times rain or snowfall is observed is shown in a graph as shown in Figure 1. (However, in Figure 1, the judgment value S is determined using the maximum temperature difference change measured by a pair of temperature sensors as ΔT.) As is clear from Figure 1, , when the judgment value S is about 1.0, the number of observations of rain and snowfall is almost equal, and when the judgment value is about 1.0 or less, the number of observations of rain increases,
When it is about 1.0 or more, the number of snowfall observations increases.
The distribution of the number of observations can be clearly distinguished between rain and snow. Based on this, a reference value S0 is determined for the determination value S, and by comparing the determination value S during rain with the personal reference value S0, it becomes possible to distinguish between rain and snow.

また、降水量Rか多くなると前記最大温度差変化又は最
大温度変化と降水量Rとの相関関係が薄れてくるので(
雨水貯留水面に降り注ぐ降雨又は降雪が激しくなると、
当該貯留水面の温度変化中は小さくなる。降水量Rが一
定値R0を超えたときには、前記(1)式の判定値Sを
求める際に降水量Rとして当該一定値R0を用いる。
Furthermore, as the amount of precipitation R increases, the correlation between the maximum temperature difference change or the maximum temperature change and the amount of precipitation R weakens (
When the rainfall or snowfall that falls on the rainwater storage water surface becomes heavy,
It becomes smaller while the temperature of the reservoir water surface changes. When the amount of precipitation R exceeds the constant value R0, the constant value R0 is used as the amount of precipitation R when determining the determination value S of the equation (1).

次に、上記基準値Soを定めるに当り、第1図から判定
値Sと、降雨又は降雪か観測された確率との関係を求め
ると第2図に示す通りとなり、この第2図から明らかな
ように、基準値S。
Next, in determining the above reference value So, the relationship between the judgment value S and the observed probability of rain or snowfall is determined from Figure 1, as shown in Figure 2, and it is clear from Figure 2. So, the standard value S.

を約0.65としたときには、降雨である確率及び降雪
である確率か共に約93%の精度で雨雪判別が可能であ
る。また、降雨判別に重点をおく場合には、基準値S。
When is set to about 0.65, it is possible to distinguish between rain and snow with an accuracy of about 93% for both the probability of rain and the probability of snow. In addition, when placing emphasis on rainfall discrimination, the standard value S is used.

の値を上記0.65より高い値としく例えばS。=0.
8としたときの降雨判定精度は95%、降雪判定精度は
88%)、降雪判定に重点をおく場合には、基準値S0
の値を上記0.65より低い値とする(例えば5o=0
.5 としたときの降雪判定精度は95%、降雨判定精
度は88%)。
For example, set the value of S to a value higher than the above 0.65. =0.
8, the rainfall determination accuracy is 95% and the snowfall determination accuracy is 88%), when placing emphasis on snowfall determination, the standard value S0
Set the value to be lower than the above 0.65 (for example, 5o=0
.. 5, the snowfall determination accuracy is 95% and the rainfall determination accuracy is 88%).

(実 施 例) 第3−及び第4図に、本発明の実施に際して使用する溢
水式雨量計の構造と、信号処理系のブロック図を示す。
(Embodiment) Figures 3 and 4 show the structure of a flood gauge and a block diagram of a signal processing system used in implementing the present invention.

溢水式雨量計は、第3図に示すように、円筒形状の受水
筒1は有底て降水を貯留するように構成され、その中央
には溢水パイプ21を含む溢水構体2か取付けられてい
る。溢水バイブ21の下端211は貯留部11に開口し
、上端212は溢水構体2の中央上方に開口しており、
貯留部11には、当該溢水パイプ21の上端212のレ
ベルまで雨水が貯留されている。
As shown in Fig. 3, the overflow type rain gauge has a cylindrical water receiving tube 1 with a bottom to store precipitation, and an overflow structure 2 including an overflow pipe 21 is attached to the center of the cylinder. . The lower end 211 of the overflow vibrator 21 opens into the storage section 11, and the upper end 212 opens above the center of the overflow structure 2.
Rainwater is stored in the storage section 11 up to the level of the upper end 212 of the overflow pipe 21 .

また、溢水構体2の下端には溢水パイプ21から溢れた
雨水を放出する放出口22が設けられ、その下方には放
出された雨水量を計測するために例えは転倒升3が設け
られている。
Further, a discharge port 22 is provided at the lower end of the overflow structure 2 to discharge rainwater overflowing from the overflow pipe 21, and a tipping box 3, for example, is provided below the discharge port 22 to measure the amount of rainwater discharged. .

貯留部11の底面には、融雪用ヒーター4が設けられて
おり、降雪時の融雪のため貯留部11の雨水の水温は常
時4〜5℃に保たれている。
A snow melting heater 4 is provided at the bottom of the storage section 11, and the temperature of rainwater in the storage section 11 is always maintained at 4 to 5 degrees Celsius for snow melting during snowfall.

また、貯留部11の水面a上には、雨水の蒸発を防止す
るための油5が水面全体に張られている。
Furthermore, oil 5 is spread over the entire water surface a of the storage section 11 to prevent rainwater from evaporating.

以上の構成は、溢水式雨量計の一般的な構造であるが、
本発明の実施のために、貯留部11の貯留水面aの近傍
に一対の温度センサ6.7が設けられている。この温度
センサ6.7の取付位置は降雪時に於いて雪か油5中を
下降し、略融は終る程度の踏動を目安にして決め、また
相互間の間隔は略10mm程度の間隔に設定しである。
The above configuration is a general structure of a flood gauge, but
In order to implement the present invention, a pair of temperature sensors 6.7 are provided near the reservoir water surface a of the reservoir 11. The installation positions of the temperature sensors 6 and 7 are determined based on the stepping motion that will descend through the snow or oil 5 during snowfall and will almost completely melt, and the intervals between them are set to approximately 10 mm. It is.

この温度センサ6.7は受水筒1の開口部12に降り込
んた雨滴又は雪片か貯留水面aに到達したときの極めて
瞬間的でかつ微少な温度変化を計測する必要があること
から、高感度で応答速度の速い温度センサ、例えば水晶
温度センサ又は小型サーミスタ等が使用される。
This temperature sensor 6.7 has high sensitivity because it is necessary to measure extremely instantaneous and minute temperature changes when raindrops or snowflakes that have fallen into the opening 12 of the water tank 1 reach the stored water surface a. For example, a temperature sensor with a fast response speed, such as a crystal temperature sensor or a small thermistor, is used.

受水筒1の開口部12に降下した雨又は雪は油5を通り
、やがて貯留部11の貯留水に加わる。
Rain or snow that has fallen into the opening 12 of the water tank 1 passes through the oil 5 and eventually joins the water stored in the storage section 11.

降雪の場合には、ヒーター4により貯留水温度が4〜5
℃に保たれていることにより融けて貯留水に加わる。以
上により貯留水が多くなると溢水パイプ21から貯留水
が溢れ、溢れた水は放出口22から放出され、この放出
された水の量が転倒升3で計測され降水量が測定される
In the case of snowfall, the temperature of the stored water is set to 4 to 5 by the heater 4.
Because it is kept at ℃, it melts and joins the stored water. When the amount of stored water increases as described above, the stored water overflows from the overflow pipe 21, the overflowing water is discharged from the discharge port 22, and the amount of discharged water is measured by the tipping box 3 to measure the amount of precipitation.

方、降水時の貯留水面a近傍の2点の温度が一対の温度
センサ6.7で計測され、当該2地間の温度差が測定さ
れる。
On the other hand, the temperature at two points near the reservoir water surface a during precipitation is measured by a pair of temperature sensors 6.7, and the temperature difference between the two locations is measured.

以上のように、一対の温度センサ6.7を使用する場合
は、貯留水面aの場所的な温度差を雨雪判別の基礎デー
タとするものであるが、この他に、一定時間間隔で温度
を測定し、その間の最高温度と最低温度の差、すなわち
時間的な温度差を雨雪判別の基礎データとすることもで
き、この場合には貯留水面aの近傍に設ける温度センサ
は1つ(温度センサ6.7の一方)でよい。
As described above, when using a pair of temperature sensors 6.7, the local temperature difference of the stored water surface a is used as basic data for rain/snow discrimination. The difference between the highest and lowest temperatures, that is, the temporal temperature difference, can be used as basic data for rain/snow discrimination. In this case, only one temperature sensor is installed near the reservoir water surface a ( Temperature sensor 6.7) may be used.

次に第4図により信号処理系とその動作を説明する。Next, the signal processing system and its operation will be explained with reference to FIG.

信号処理系には、2つの測温部10,11 、該測温部
10.11で計測した温度の差をとって温度差データを
出力する差信号回路12、該差信号回路12からの温度
差データ及び転倒升3からの降水データに基いて雨雪判
別を行なう信号処理部13、該信号処理部13によりて
処理したデータ(雨雪判別データ等)を記録する記録部
14、前記判定基準S。を設定するための判定基準値設
定部15を含む。
The signal processing system includes two temperature measurement units 10 and 11, a difference signal circuit 12 that calculates the difference between the temperatures measured by the temperature measurement units 10 and 11 and outputs temperature difference data, and a temperature signal from the difference signal circuit 12. A signal processing unit 13 that performs rain/snow discrimination based on the difference data and precipitation data from the overturned square 3, a recording unit 14 that records data processed by the signal processing unit 13 (rain/snow discrimination data, etc.), and the determination criteria. S. It includes a determination reference value setting section 15 for setting.

測温部10.11は、例えば水晶振動子を使用した温度
センサ6.7と、該温度センサ6.7を発振素子とする
発振回路8,9て構成され、それぞれ温度センサ6.7
で測定した温度に対応する周波数の発振信号を出力する
The temperature measuring section 10.11 is composed of a temperature sensor 6.7 using, for example, a crystal oscillator, and oscillation circuits 8 and 9 using the temperature sensor 6.7 as an oscillation element.
Outputs an oscillation signal with a frequency corresponding to the temperature measured.

差信号回路12は、測温部10.11の発振回路8.9
の出力信号周波数の差の周波数の信号を出力することに
より、温度センサ6.7の測定温度差データを直接出力
する。尚、前記時間的温度差を基礎データとする場合に
は、測温部10.11はいずれか1つでよく、かつ差信
号回路12も必要とせず、測温部10(又は11)の測
温データ(発振回路8又は9の出力信号)を直接信号処
理部13に人力し、信号処理部13の処理によって一定
時間内での最高、最低温度差(最大温度変化)を算出す
る。
The difference signal circuit 12 is an oscillation circuit 8.9 of the temperature measuring section 10.11.
By outputting a signal with a frequency corresponding to the difference between the output signal frequencies of , the temperature difference data measured by the temperature sensor 6.7 is directly output. In addition, when the temporal temperature difference is used as the basic data, only one of the temperature measurement sections 10 and 11 is required, and the difference signal circuit 12 is not required, and the measurement of the temperature measurement section 10 (or 11) The temperature data (output signal of the oscillation circuit 8 or 9) is directly inputted to the signal processing section 13, and the maximum and minimum temperature difference (maximum temperature change) within a certain period of time is calculated by the processing of the signal processing section 13.

信号処理1113はマイクロプロセッサ(CPII)を
主体に構成されており、前記(1)式によって判定値S
を演算し、当該判定値Sと、判定基準値設定部15で設
定された基準値S。と比較し、雨雪判別を行なう。すな
わち、S≧S0のとぎは降雪であるものと判断し、S<
S。のときは降雨であると判断し、この判断結果を記録
部14に出力し、記録する。
The signal processing 1113 is mainly composed of a microprocessor (CPII), and the judgment value S is determined by the above equation (1).
The judgment value S and the reference value S set by the judgment reference value setting section 15 are calculated. Rain/snow discrimination is performed by comparing with In other words, it is determined that S≧S0 is snowfall, and S<
S. When this happens, it is determined that it is raining, and this determination result is output to the recording section 14 and recorded.

(発明の効果) 以上説明したように、本発明は、常時一定レベルまで雨
水を溜めておく構造の雨量計の貯留水面近傍の一定時間
内に於ける最大温度変化又は当該貯留水面近傍2点間の
一定時間内に於ける最大温度差変化と、そのときの降水
量との比で定義した判定値を基準値と比較することによ
って雨雪判別を行なうようにしたものであり、雨雪判別
がコンピュータ処理によって高精度で自動化でき、気象
観測における各種データと雨雪判別との一括処理が可能
となる。
(Effects of the Invention) As explained above, the present invention is capable of measuring the maximum temperature change within a certain period of time near the water surface of a rain gauge having a structure in which rainwater is always stored up to a certain level, or between two points near the water surface. Rain and snow discrimination is performed by comparing a judgment value defined as the ratio of the maximum temperature difference change within a certain period of time to the precipitation amount at that time with a reference value. It can be automated with high precision through computer processing, and batch processing of various weather observation data and rain/snow detection is possible.

また、例えば溢水式雨量計のように雨水を常時溜めてお
く構造の雨量計に温度センサを取付けることによって雨
雪判別が可能であるため、雨雪判別センサを独立した気
象観測機器として必要とせず、観測設備費用及びその運
用費用等の低減が図れる。
In addition, it is possible to distinguish between rain and snow by attaching a temperature sensor to a rain gauge that constantly collects rainwater, such as an overflow rain gauge, so there is no need for a rain or snow discrimination sensor as an independent weather observation device. , the cost of observation equipment and its operation cost can be reduced.

【図面の簡単な説明】[Brief explanation of the drawing]

第1図及び第2図は、本発明かなされるに至ったデータ
の分析結果を表わしたグラフで、第1図は判定値Sと降
雨又は降雪の観測回数の関係を示すもの、第2図は判定
基準値S。と降雨又は降雪の確率の関係を示すものであ
り、第3図は本発明の実施に際して使用する溢水式雨量
計の構造図、第4図は信号処理系のブロック図である。 (主な記号) 3・・・転倒弁      6.7・・・温度センサ1
0.11・・・測温部    13・・・信号処理部1
5・・・判定基準値設定部 化4名 第1図 第2図 判定値(S)
Figures 1 and 2 are graphs showing the results of the data analysis that led to the present invention, with Figure 1 showing the relationship between the judgment value S and the number of observations of rain or snowfall, and Figure 2. is the judgment reference value S. Fig. 3 is a structural diagram of the overflow type rain gauge used in carrying out the present invention, and Fig. 4 is a block diagram of the signal processing system. (Main symbols) 3... Overturning valve 6.7... Temperature sensor 1
0.11...Temperature measurement section 13...Signal processing section 1
5... Judgment standard value setting department 4 people Figure 1 Figure 2 Judgment value (S)

Claims (1)

【特許請求の範囲】 1 常時一定レベルまで雨水を溜めておく手段を有する
雨量計の貯留水中で水面近傍に温度センサを設け、降雨
時又は降雪時に上記温度センサで検出された温度の一定
時間内に於ける最大値と最小値の差をΔT、上記一定時
間内の降水量をRとしたとき、次式 S=ΔT/R で定義される判定値Sが、当該判定値Sについて定めた
判定基準値S_0を超えない場合には降雨であるものと
、超えた場合には降雪であるものと、それぞれ判断する
ようにした雨雪判別方法。 2 請求項1に記載の雨雪判別方式に於いて、温度セン
サを一対(2個)とし、ΔTを当該一対の温度センサで
それぞれ検出した温度の差の一定時間内に於ける最大値
と最小値の差とした雨雪判別方法。 3 請求項1又は2に記載の雨雪判別方式に於いて、降
水量Rが一定値R_0を超えたときには、降水量Rとし
て当該一定値R_0を用いて判定値Sを求めるようにし
た雨雪判別方法。 4 請求項1又は2に記載の雨雪判別方式に於いて、判
定基準値S_0を、降雨判定確率と降雪判定確率とが等
しくなるような値に設定した雨雪判別方法。 5 請求項1又は2に記載の雨雪判別方式に於いて、雨
雪判別を、降雨判別に重点をおくか又は降雪判別に重点
をおくかによって判定基準値S_0を変えるようにした
雨雪判別方法。
[Claims] 1. A temperature sensor is provided near the water surface in the stored water of a rain gauge that has means for constantly storing rainwater up to a certain level, and the temperature detected by the temperature sensor during rain or snow falls within a certain period of time. When ΔT is the difference between the maximum value and the minimum value in A rain/snow discrimination method in which it is determined that it is rain if the standard value S_0 is not exceeded, and that it is snowfall if it is exceeded. 2 In the rain/snow discrimination method according to claim 1, a pair (two) of temperature sensors is used, and ΔT is defined as the maximum value and minimum value of the temperature difference detected by the pair of temperature sensors within a certain period of time. A rain/snow discrimination method based on the difference in values. 3. In the rain/snow discrimination method according to claim 1 or 2, when the amount of precipitation R exceeds a certain value R_0, the certain value R_0 is used as the amount of precipitation R to determine the determination value S. Discrimination method. 4. The rain and snow discrimination method according to claim 1 or 2, wherein the determination reference value S_0 is set to a value such that the rain determination probability and the snowfall determination probability are equal. 5. In the rain/snow discrimination method according to claim 1 or 2, the rain/snow discrimination is configured such that the determination reference value S_0 is changed depending on whether emphasis is placed on rain/snow discrimination or on snowfall discrimination. Method.
JP17159490A 1990-06-29 1990-06-29 Rain and snow determination method Expired - Fee Related JP2907500B2 (en)

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JP17159490A JP2907500B2 (en) 1990-06-29 1990-06-29 Rain and snow determination method

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP17159490A JP2907500B2 (en) 1990-06-29 1990-06-29 Rain and snow determination method

Publications (2)

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JPH0460490A true JPH0460490A (en) 1992-02-26
JP2907500B2 JP2907500B2 (en) 1999-06-21

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JP17159490A Expired - Fee Related JP2907500B2 (en) 1990-06-29 1990-06-29 Rain and snow determination method

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Country Link
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Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN106547038A (en) * 2017-01-17 2017-03-29 水利部交通运输部国家能源局南京水利科学研究院 A kind of snow melt mountain torrent monitoring experimental rig and method

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN106547038A (en) * 2017-01-17 2017-03-29 水利部交通运输部国家能源局南京水利科学研究院 A kind of snow melt mountain torrent monitoring experimental rig and method

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