JPH0543997B2 - - Google Patents

Info

Publication number
JPH0543997B2
JPH0543997B2 JP1120497A JP12049789A JPH0543997B2 JP H0543997 B2 JPH0543997 B2 JP H0543997B2 JP 1120497 A JP1120497 A JP 1120497A JP 12049789 A JP12049789 A JP 12049789A JP H0543997 B2 JPH0543997 B2 JP H0543997B2
Authority
JP
Japan
Prior art keywords
light
refracted
polarized
reflected
light beam
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 - Fee Related
Application number
JP1120497A
Other languages
Japanese (ja)
Other versions
JPH02300688A (en
Inventor
Shigetoshi Abe
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.)
Japan Radio Co Ltd
Original Assignee
Japan Radio Co 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 Japan Radio Co Ltd filed Critical Japan Radio Co Ltd
Priority to JP1120497A priority Critical patent/JPH02300688A/en
Publication of JPH02300688A publication Critical patent/JPH02300688A/en
Publication of JPH0543997B2 publication Critical patent/JPH0543997B2/ja
Granted legal-status Critical Current

Links

Classifications

    • YGENERAL TAGGING OF NEW TECHNOLOGICAL DEVELOPMENTS; GENERAL TAGGING OF CROSS-SECTIONAL TECHNOLOGIES SPANNING OVER SEVERAL SECTIONS OF THE IPC; TECHNICAL SUBJECTS COVERED BY FORMER USPC CROSS-REFERENCE ART COLLECTIONS [XRACs] AND DIGESTS
    • Y02TECHNOLOGIES OR APPLICATIONS FOR MITIGATION OR ADAPTATION AGAINST CLIMATE CHANGE
    • Y02ATECHNOLOGIES FOR ADAPTATION TO CLIMATE CHANGE
    • Y02A90/00Technologies having an indirect contribution to adaptation to climate change
    • Y02A90/10Information and communication technologies [ICT] supporting adaptation to climate change, e.g. for weather forecasting or climate simulation

Description

【発明の詳細な説明】 [産業上の利用分野] この発明は所望の空間位置における降雨、降雪
を検知し、降雨、降雪量を計測する気象用センサ
装置に関し、特に降雨であるか降雪であるかの判
定を行う降雨降雪測定装置に関するものである。
[Detailed Description of the Invention] [Industrial Application Field] The present invention relates to a weather sensor device that detects rainfall or snowfall at a desired spatial location and measures the amount of rainfall or snowfall, and particularly relates to a weather sensor device that detects rainfall or snowfall at a desired spatial location and measures the amount of rainfall or snowfall. This invention relates to a rainfall/snowfall measurement device that makes such determinations.

[従来の技術] 降雨であるか降雪であるかの判定を行う従来の
装置としては、投光器を用いて所望の空間位置に
自然光を投光し、雨滴や雪片などの反射物体から
反射してくる反射光を受光器で受光し、反射光強
度により降雨であるか降雪であるかを判定する装
置がある。
[Prior Art] A conventional device for determining whether it is raining or snowing uses a floodlight to project natural light onto a desired spatial position, and the light is reflected from reflective objects such as raindrops or snowflakes. There is a device that receives reflected light with a light receiver and determines whether it is raining or snowing based on the intensity of the reflected light.

即ち、降水量がほぼ同一の場合、雨滴からの反
射よりも雪片からの反射の方が反射光強度が強い
ので、この反射光強度の差を利用して雨か雪かの
判定を行つている。然しながらこの方法では、例
えば強い雨の場合の反射光強度と、弱い雪の場合
の反射光強度とが同一となり、雨か雪かの判定を
誤る場合がある。
In other words, when the amount of precipitation is almost the same, the intensity of reflected light from snowflakes is stronger than that from raindrops, so this difference in reflected light intensity is used to determine whether it is rain or snow. . However, with this method, for example, the intensity of reflected light in the case of heavy rain and the intensity of reflected light in the case of light snow may be the same, leading to errors in determining whether it is rain or snow.

このような場合、温度センサをを併設すること
で、低温のときは雪と判定する方法も考えられ
る。ただ0℃〜8℃の範囲においては、雨である
場合も雪である場合もあり、正確な判定を行うこ
とが困難である。
In such a case, it may be possible to install a temperature sensor to determine that it is snow when the temperature is low. However, in the range of 0°C to 8°C, it may be rain or snow, and it is difficult to make an accurate determination.

また反射光を用いる替わりに、透過光の減衰を
測定する方法もある。即ち、投光器から一定距離
に離した受光器に向けて自然光を投光し、その間
に雨滴や雪片が入ることによつて透過光の受ける
減衰を測定し、減衰の強さにより雨滴か雪片かを
判定する方法であるが、この方法の場合、光ビー
ムの方向に風が吹くと雪片がその方向に流れ、光
の減衰を低下させてしまう等、風向きや風速によ
つて誤つた判定がなされという問題がある。
Furthermore, instead of using reflected light, there is also a method of measuring attenuation of transmitted light. In other words, natural light is emitted from the emitter to a receiver placed a certain distance away, and when raindrops or snowflakes enter between them, the attenuation of the transmitted light is measured. Based on the strength of the attenuation, it is determined whether the light is a raindrop or a snowflake. However, with this method, if the wind blows in the direction of the light beam, snowflakes will flow in that direction, reducing the attenuation of the light. There's a problem.

さらに雨か雪かの判定は、テレビカメラで観察
することによつてもできるが、装置が高価にな
り、常に人間が監視しておく必要がある。
Furthermore, it is possible to determine whether it is raining or snowing by observing with a television camera, but the equipment is expensive and requires constant human monitoring.

[発明が解決しようとする課題] 上記のような従来の装置では以上のように、光
学式センサを用いる装置においては、センサの設
置した近傍に降雨または降雪があるか否かの検出
はできるが、雨であるか雪であるかの判定が困難
であり、またテレビカメラを用いる場合には、装
置が高価なものとなり、常に人間が監視しておく
必要がある等の問題点があつた。
[Problems to be Solved by the Invention] As described above, in the conventional device as described above, in the device using an optical sensor, it is possible to detect whether or not there is rain or snow in the vicinity where the sensor is installed. However, it is difficult to determine whether it is raining or snowing, and when a television camera is used, the equipment is expensive and requires constant human monitoring.

この発明は、従来の装置における上述の課題を
解決するためになされたもので、降雨であるか降
雪であるかを正確に判定することができる降雨降
雪測定装置を得ることを目的としている。
The present invention was made in order to solve the above-mentioned problems in conventional devices, and aims to provide a rainfall and snowfall measuring device that can accurately determine whether it is raining or snowing.

[課題を解決するための手段] この発明にかかる降雨降雪測定装置は、投光す
る光ビームを偏光した光ビームとし、雨滴は偏光
面を散乱させないが、雪片は結晶であるため偏光
面を散乱させるという性質を利用し、反射光の偏
光面の散乱を測定することにより雨か雪かを判定
することとした。
[Means for Solving the Problems] The rain and snowfall measuring device according to the present invention uses a polarized light beam as a projected light beam, and while raindrops do not scatter the polarized plane, snowflakes are crystals and therefore scatter the polarized plane. Taking advantage of this property, we decided to determine whether it is rain or snow by measuring the scattering of the polarization plane of reflected light.

[作用] 反射光を偏光分離器によつて垂直偏光成分と水
平偏光成分とに分離すると、投射光が垂直偏光成
分である場合に、水平偏光成分がある程度以上検
出されるときは雪からの反射波と判定すことがで
きる。
[Function] When the reflected light is separated into a vertically polarized component and a horizontally polarized component using a polarization separator, if the projected light is a vertically polarized component and a certain level of horizontally polarized component is detected, it is reflected from snow. It can be determined as a wave.

[実施例] 以下、この発明の実施例を図面を用いて説明す
る。第1図はこの発明の一実施例を示す構成図
で、図において1は投光器用電気回路、2は光
源、3は投光器用レンズ、4は偏光器、5は投光
された光ビーム、6は反射物体、7は反射光、8
は受光器用レンズ、9は偏光分離器、10は垂直
受光素子、11は水平受光素子、12は垂直受信
機、13は水平受信機、14は信号処理部であ
り、8〜13で受光器が構成されている。
[Examples] Examples of the present invention will be described below with reference to the drawings. FIG. 1 is a block diagram showing an embodiment of the present invention, in which 1 is an electric circuit for a projector, 2 is a light source, 3 is a lens for the projector, 4 is a polarizer, 5 is a projected light beam, and 6 is a reflective object, 7 is a reflected light, 8
9 is a light receiving lens, 9 is a polarization separator, 10 is a vertical light receiving element, 11 is a horizontal light receiving element, 12 is a vertical receiver, 13 is a horizontal receiver, 14 is a signal processing section, and 8 to 13 are the light receiving device. It is configured.

偏光された光ビーム5が投射され、反射物体6
からの反射光7が受光器で受光され、偏光分離器
9で垂直偏光成分と水平偏光成分とに分離され、
垂直偏光成分は垂直受光素子10で電気信号に変
換され、水平偏光成分は水平受光素子11で電気
信号に変換される。
A polarized light beam 5 is projected onto a reflecting object 6
The reflected light 7 from
The vertically polarized light component is converted into an electrical signal by the vertical light receiving element 10, and the horizontally polarized light component is converted into an electrical signal by the horizontal light receiving element 11.

垂直受光素子10と水平受光素子11との出力
は、それぞれ垂直受信機12と水平受信機13と
で増幅され、信号処理部14に入力される。信号
処理部14では垂直受信機12の出力と水平受信
機13の出力とを処理することによつて、反射物
体の性質を判断する。
The outputs of the vertical light receiving element 10 and the horizontal light receiving element 11 are amplified by a vertical receiver 12 and a horizontal receiver 13, respectively, and input to a signal processing section 14. The signal processing section 14 processes the output of the vertical receiver 12 and the output of the horizontal receiver 13 to determine the nature of the reflecting object.

例えば水平受信機13の出力が垂直受信機12
の出力に比し充分に小さい時は、反射物体6にお
いて偏光面の散乱が生じてないことを意味し、従
つてその反射物体6は雪でないと判定する。
For example, the output of the horizontal receiver 13 is the output of the vertical receiver 12.
When the output is sufficiently small compared to the output of , it means that no scattering of the plane of polarization occurs in the reflecting object 6, and therefore, it is determined that the reflecting object 6 is not snow.

第2図〜第5図は、この発明における原理を説
明するための図であつて、これらの図において第
1図と同一符号は同一または相当部分を示し、1
5は雨滴、24は氷粒、33は雪片、16,19
はそれぞれ入射光{光ビーム5であるが、ここで
は反射物体に対する入射光となる}。17,30
はそれぞれ反射光、18,20,21,25,2
6,31,32はそれぞれ屈折光、22,27,
28,34はそれぞれ偏光波面を表す。
2 to 5 are diagrams for explaining the principle of this invention, and in these figures, the same reference numerals as in FIG. 1 indicate the same or corresponding parts, and 1
5 is raindrop, 24 is ice grain, 33 is snowflake, 16, 19
are incident light (light beam 5, here, incident light on a reflective object), respectively. 17,30
are reflected light, 18, 20, 21, 25, 2, respectively.
6, 31, 32 are refracted lights, 22, 27,
28 and 34 each represent a polarized wavefront.

第2図に示すように、雨滴15のA点に入射し
た偏光波面22を有する入射光16は、入射角に
対応した反射光17となるが、この反射光17の
偏光波面は入射光16の偏光波面22と同じであ
る。
As shown in FIG. 2, the incident light 16 having the polarized wavefront 22 that is incident on the point A of the raindrop 15 becomes reflected light 17 corresponding to the angle of incidence. This is the same as the polarization wavefront 22.

A点で雨滴15内に屈折し、B点において屈折
して雨滴15から出射する屈折光18の偏光波面
も、雨滴15が水であり、等方性物質であるた
め、入射光16と同じ偏光波面22を持つ。
The polarized wavefront of the refracted light 18 that is refracted into the raindrop 15 at point A, refracted at point B, and exits from the raindrop 15 is also the same polarized light as the incident light 16 because the raindrop 15 is water and is an isotropic substance. It has a wave front 22.

入射光19はC点、D点で屈折された屈折光2
0となり、またD点で反射されE点で屈折されて
出射する屈折光21となるが、これらの屈折光2
0,21の偏光波面も、上述のように水が等方性
物質であるため、入射光19の偏光波面22と同
様である。
Incident light 19 is refracted light 2 refracted at point C and point D.
0, and becomes refracted light 21 that is reflected at point D, refracted at point E, and emitted, but these refracted lights 2
The polarization wavefronts of 0 and 21 are also similar to the polarization wavefront 22 of the incident light 19 because water is an isotropic substance as described above.

以上のように、反射物体が雨滴15である場合
には、入射光が垂直偏光成分である場合、反射屈
折光に水平偏光成分が含まれることはない。
As described above, when the reflective object is a raindrop 15 and the incident light has a vertically polarized component, the catadioptric light does not include a horizontally polarized component.

次に第3図に示すように、偏光波面27を有す
る光ビーム5が氷粒24のF点に入射したとす
る。氷粒24は六方晶系の結晶体であり、入射し
た光は複屈折をおこす。即ち、入射光と同一偏光
波面を保ちながら屈折する光に対する屈折率、即
ち常光線の屈折率は1.309であり、入射光と偏光
波面が異なる状態で屈折する光に対する屈折率、
即ち異常光線の屈折率は1.313{但し、氷粒24の
温度を0℃とした場合}であるので、偏光波面2
7を持つ屈折光25と、偏光波面28を持つ屈折
光26とは、進行方向が異なる。
Next, as shown in FIG. 3, it is assumed that the light beam 5 having the polarized wavefront 27 is incident on the point F of the ice grain 24. The ice grains 24 are hexagonal crystals, and incident light causes birefringence. In other words, the refractive index for light that is refracted while maintaining the same polarized wavefront as the incident light, that is, the refractive index of ordinary rays, is 1.309, and the refractive index for light that is refracted with a polarized wavefront that is different from the incident light,
In other words, the refractive index of the extraordinary ray is 1.313 (when the temperature of the ice grains 24 is 0°C), so the polarization wavefront 2
7 and the refracted light 26 having a polarization wavefront 28 have different traveling directions.

従つて第4図に示すように、氷粒24のF点で
反射される反射光30は、入射光5と同一偏光波
面に保たれ、F点で常光線として屈折される屈折
光32はH点で屈折されて氷粒24から出射され
るが、この屈折光32は入射光5と同一の偏光波
面を持つ。然しながらF点で異常光線として屈折
される屈折光31はG点で屈折されて氷粒24か
ら出射されるが、この屈折光31の偏光波面は入
射光5の偏光波面とは異なるものになる。
Therefore, as shown in FIG. 4, the reflected light 30 reflected at point F of the ice grain 24 is kept at the same polarization wavefront as the incident light 5, and the refracted light 32 refracted as an ordinary ray at point F is H Although the refracted light 32 is refracted at a point and emitted from the ice grain 24, this refracted light 32 has the same polarization wavefront as the incident light 5. However, although the refracted light 31 refracted as an extraordinary ray at point F is refracted at point G and exits from the ice grain 24, the polarized wavefront of this refracted light 31 is different from the polarized wavefront of the incident light 5.

また第5図に示すように、雪片33は氷粒24
が無数に結合して出来た氷粒24の集合体であ
り、偏光波面27を持つ入射光は、雪片33の中
で多数回の反射屈折が繰り返され、第1図に示す
受光器用レンズ8に入る反射光7の偏光波面は、
第5図の34に示すように、ほぼランダムなもの
となる。
Furthermore, as shown in FIG. 5, the snowflake 33 is
The incident light having a polarized wavefront 27 is reflected and refracted many times in the snowflake 33, and is reflected by the light receiving lens 8 shown in FIG. The polarization wavefront of the reflected light 7 that enters is
As shown at 34 in FIG. 5, it becomes almost random.

このようなランダムな偏光波面34の反射光7
は、垂直偏光成分と水平偏光成分とに分離するこ
とができ、従つて投射する光ビーム5を垂直偏光
成分としておけば、反射光7に水平偏光成分が含
まれていないときは雨、水平偏光成分がある程以
上含まれているときは雪と判定することができ
る。
Reflected light 7 of such a random polarized wavefront 34
can be separated into a vertically polarized component and a horizontally polarized component. Therefore, if the projected light beam 5 is set as a vertically polarized component, if the reflected light 7 does not include a horizontally polarized component, it is rain, and horizontally polarized light is detected. When it contains more than a certain amount of ingredients, it can be determined as snow.

また反射光7に含まれる水平偏光成分の強さに
従つて、みぞれ、湿り雪、乾き雪などの判定も行
うことができる。
Further, depending on the strength of the horizontally polarized component included in the reflected light 7, it is possible to determine whether it is sleet, wet snow, dry snow, or the like.

[発明の効果] この発明は以上説明したように、投光する光ビ
ームを偏光した光ビームとし、反射光の偏光面の
散乱を測定することとしたので、雨か雪かの判定
を正確に行うことができ、且つ、みぞれ、湿り
雪、乾き雪などの判定も行うことができるという
効果がある。
[Effects of the Invention] As explained above, in this invention, the projected light beam is a polarized light beam and the scattering of the polarization plane of the reflected light is measured, so it is possible to accurately determine whether it is rain or snow. This method has the advantage of being able to determine whether it is sleet, wet snow, dry snow, etc.

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

第1図はこの発明の一実施例を示す構成図、第
2図〜第5図はこの発明における原理を説明する
ための図。 1……投光器用電気回路、2……光源、3……
投光器用レンズ、4……偏光器、5……光ビーム
(入射光)、6……反射物体、7……反射光、8…
…受光器用レンズ、9……偏光分離器、10……
垂直受光素子、11……水平受光素子、12…垂
直受信機、13……水平受信機、14……信号処
理部。なお、各図中同一符号は同一または相当部
分を示すものとする。
FIG. 1 is a block diagram showing one embodiment of the invention, and FIGS. 2 to 5 are diagrams for explaining the principle of the invention. 1... Electric circuit for floodlight, 2... Light source, 3...
Lens for projector, 4...Polarizer, 5...Light beam (incident light), 6...Reflecting object, 7...Reflected light, 8...
...Receiver lens, 9...Polarization separator, 10...
Vertical light receiving element, 11... Horizontal light receiving element, 12... Vertical receiver, 13... Horizontal receiver, 14... Signal processing section. Note that the same reference numerals in each figure indicate the same or corresponding parts.

Claims (1)

【特許請求の範囲】 1 所定の偏光波面に偏光された光ビームを空中
に投光する投光器。 この投光器から投光された光ビームが当該光ビ
ーム内に存在する雨滴、雪片等の反射物体で反射
された反射光を受光する受光器、 この受光器に設けられ、受光器が受光する反射
光を垂直偏光成分と、水平偏光成分とに分離する
偏光分離器、 この偏光分離器により分離された垂直偏光成分
の強さに依存する電気信号を出力する第1の受光
素子、 上記偏光分離器により分離された水平偏光成分
の強さに依存する電気信号を出力する第2の受光
素子、 上記第1の受光素子と第2の受光素子とから出
力される電気信号を入力し、両電気信号の差異に
より上記反射物体の種類を判定する信号処理部、 を備えた降雨降雪測定装置。
[Claims] 1. A light projector that projects a light beam polarized to a predetermined polarization wavefront into the air. A light receiver that receives reflected light from a light beam projected from this light beam reflected by reflective objects such as raindrops and snowflakes present in the light beam; a polarization separator that separates the light into a vertically polarized component and a horizontally polarized component; a first light-receiving element that outputs an electrical signal that depends on the strength of the vertically polarized component separated by the polarization separator; a second light-receiving element that outputs an electrical signal that depends on the strength of the separated horizontally polarized light component; A rainfall and snowfall measurement device comprising: a signal processing unit that determines the type of the reflecting object based on the difference.
JP1120497A 1989-05-16 1989-05-16 Rainfall and snowfall measuring instrument Granted JPH02300688A (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
JP1120497A JPH02300688A (en) 1989-05-16 1989-05-16 Rainfall and snowfall measuring instrument

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP1120497A JPH02300688A (en) 1989-05-16 1989-05-16 Rainfall and snowfall measuring instrument

Publications (2)

Publication Number Publication Date
JPH02300688A JPH02300688A (en) 1990-12-12
JPH0543997B2 true JPH0543997B2 (en) 1993-07-05

Family

ID=14787665

Family Applications (1)

Application Number Title Priority Date Filing Date
JP1120497A Granted JPH02300688A (en) 1989-05-16 1989-05-16 Rainfall and snowfall measuring instrument

Country Status (1)

Country Link
JP (1) JPH02300688A (en)

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Publication number Priority date Publication date Assignee Title
FI90596C (en) * 1991-04-22 1994-02-25 Vaisala Oy Method and apparatus for measuring the meteorological visibility of the prevailing weather
US5298750A (en) * 1992-01-15 1994-03-29 Rericha Frank M Laser precipitation sensor
FR2768122B1 (en) * 1997-09-09 1999-11-19 Sextant Avionique OPTICAL DEVICE FOR DETECTION OF ICING CONDITIONS ON AIRCRAFT

Citations (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPS61175550A (en) * 1985-01-31 1986-08-07 Meisei Electric Co Ltd Optical measuring method and apparatus for intensity of rain and snow falling

Patent Citations (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPS61175550A (en) * 1985-01-31 1986-08-07 Meisei Electric Co Ltd Optical measuring method and apparatus for intensity of rain and snow falling

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JPH02300688A (en) 1990-12-12

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