JPH0132959B2 - - Google Patents
Info
- Publication number
- JPH0132959B2 JPH0132959B2 JP9948381A JP9948381A JPH0132959B2 JP H0132959 B2 JPH0132959 B2 JP H0132959B2 JP 9948381 A JP9948381 A JP 9948381A JP 9948381 A JP9948381 A JP 9948381A JP H0132959 B2 JPH0132959 B2 JP H0132959B2
- Authority
- JP
- Japan
- Prior art keywords
- electric field
- ground electric
- value
- field value
- stage
- 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
Links
- 230000005684 electric field Effects 0.000 claims description 61
- 230000010354 integration Effects 0.000 claims description 11
- 238000000691 measurement method Methods 0.000 claims description 2
- 230000001186 cumulative effect Effects 0.000 claims 1
- 238000010586 diagram Methods 0.000 description 8
- 238000000034 method Methods 0.000 description 8
- 238000001514 detection method Methods 0.000 description 6
- 230000006698 induction Effects 0.000 description 3
- 239000013078 crystal Substances 0.000 description 2
- 230000005686 electrostatic field Effects 0.000 description 2
- 239000002245 particle Substances 0.000 description 2
- 230000004913 activation Effects 0.000 description 1
- 238000013459 approach Methods 0.000 description 1
- 230000015572 biosynthetic process Effects 0.000 description 1
- 230000007423 decrease Effects 0.000 description 1
- 238000013461 design Methods 0.000 description 1
- 238000011161 development Methods 0.000 description 1
- 238000007599 discharging Methods 0.000 description 1
- 238000002592 echocardiography Methods 0.000 description 1
- 230000000694 effects Effects 0.000 description 1
- 230000008014 freezing Effects 0.000 description 1
- 238000007710 freezing Methods 0.000 description 1
- 230000014509 gene expression Effects 0.000 description 1
- 230000005484 gravity Effects 0.000 description 1
- 239000005433 ionosphere Substances 0.000 description 1
- 238000010248 power generation Methods 0.000 description 1
- 238000001556 precipitation Methods 0.000 description 1
- 238000011160 research Methods 0.000 description 1
- 230000000630 rising effect Effects 0.000 description 1
- XLYOFNOQVPJJNP-UHFFFAOYSA-N water Substances O XLYOFNOQVPJJNP-UHFFFAOYSA-N 0.000 description 1
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01W—METEOROLOGY
- G01W1/00—Meteorology
- G01W1/16—Measuring atmospheric potential differences, e.g. due to electrical charges in clouds
Landscapes
- Environmental & Geological Engineering (AREA)
- Engineering & Computer Science (AREA)
- Life Sciences & Earth Sciences (AREA)
- Atmospheric Sciences (AREA)
- Biodiversity & Conservation Biology (AREA)
- Ecology (AREA)
- Environmental Sciences (AREA)
- Geophysics And Detection Of Objects (AREA)
- Emergency Alarm Devices (AREA)
- Radar Systems Or Details Thereof (AREA)
- Elimination Of Static Electricity (AREA)
Description
〔産業上の利用分野〕
本発明は高精度の襲雷警報装置に関するもので
ある。
〔従来の技術〕
従来襲雷警報装置としては、(1)レーダー式、(2)
電波式、(3)電界式などがある。
〔解決しようとする問題点〕
(1) レーダー式は、雷雲の大きさ、高さを比較的
精度よく測定でき、雷の発生を予想することに
充分利用出来るが、雷雲の電気的現象(雷雲の
電荷、放電など)を直接測定するものではない
という面と、実際上設備が大規模になり費用も
前記(2)電波式(3)電界式に比し数十倍以上要する
という問題がある。
(2) 電波式は妨害電波を受けやすく、例えば電離
層の反射等により、遠くにある雷雲を近くに感
応する傾向がある。
またその他に雷の終末期になり、主として雲
間放電だけになつても作動することがあるとい
う問題もあつた。
(3) 電界式においては、電界の強さは地表面付近
に蓄積された空間電荷に左右されるので電界強
度測定器単独では判断しにくい場合がある。
また電界値の瞬間的な急変化を一定時間積算
して、発生回数が設定値を超えた場合警報を出
す方式のものは、比較的近距離の雷をとらえる
が、放電開始以前の雷の感知に不向きであり、
設定値の調整がむずかしいなど、いずれも実用
上の欠点があつた。
〔問題点を解決するための手段〕
襲雷警報装置の終局の目的は『襲雷のおそれの
ない時は働かず、襲雷のおそれのあるときは必ず
働く』という姿に設計と調整の両面からつめてゆ
くことである。
本発明者は長年にわたり雷雨時に電界を測定し
た結果、電界式の欠点を克服して、
まず、地表電界値を測定し
電界値の瞬間的な急変化の発生回数を所定時
間積算し、その数が設定値を超えて増加した場
合を検知し、
さらに地表電界のうち緩慢に変化する成分即
ち低周波性の地表電界値の変動を別に検知し、
これらの情報の組合わせを以て作動の要因とな
す電界強度測定方式の高精度な襲雷警報装置を
提案するものである。
尚、本明細書では地表付近における電界を『地
表電界』と略記する。
まず、雷雲の進行に伴なう地表電界の変化およ
び地表電界値の瞬間的な急変化をみると、典型的
な雷雲を示す第2図のように、雷雲から遠い地点
では、電界の方向は下向き
[Industrial Field of Application] The present invention relates to a highly accurate lightning warning system. [Prior art] Conventional lightning warning systems include (1) radar type, (2)
There are radio wave type and (3) electric field type. [Problems to be solved] (1) The radar method can measure the size and height of thunderclouds with relatively high accuracy, and can be fully used to predict the occurrence of lightning. There are problems in that it does not directly measure electric charge, discharge, etc.), and in practice, the equipment is large-scale and costs several tens of times more than the (2) radio wave method and (3) electric field method. . (2) Radio-controlled systems are susceptible to interference, for example due to reflections from the ionosphere, which tends to make distant thunderclouds appear nearby. Another problem was that it could operate even in the final stage of lightning, when only intercloud discharge occurred. (3) In the electric field method, the strength of the electric field depends on the space charge accumulated near the ground surface, so it may be difficult to judge using an electric field strength measuring device alone. In addition, systems that integrate instantaneous sudden changes in the electric field value over a certain period of time and issue an alarm when the number of occurrences exceeds a set value catch lightning at a relatively short distance, but they detect lightning before it starts discharging. is unsuitable for
All of them had practical drawbacks, such as the difficulty of adjusting the setting values. [Means to solve the problem] The ultimate purpose of the lightning warning system is to ``do not work when there is no risk of a lightning strike, and always work when there is a risk of a lightning strike.'' Both design and adjustment are required. It is about tying things together. As a result of measuring electric fields during thunderstorms over many years, the present inventor overcame the shortcomings of the electric field method. First, the inventor measured the ground electric field value, accumulated the number of instantaneous sudden changes in the electric field value over a specified period of time, and calculated the number of instantaneous sudden changes in the electric field value. Detects when the ground electric field increases beyond a set value, and also separately detects fluctuations in the slowly changing component of the ground electric field, that is, low frequency ground electric field values,
This paper proposes a highly accurate lightning strike warning system that uses a combination of these pieces of information as the activation factor and uses an electric field strength measurement method. In this specification, the electric field near the earth's surface is abbreviated as "ground electric field." First, if we look at the changes in the ground electric field and the instantaneous sudden changes in the ground electric field value as the thundercloud advances, we can see that at points far from the thundercloud, the direction of the electric field changes as shown in Figure 2, which shows a typical thundercloud. downward
【式】である。
その値は晴天の場合(−100v/m位)よりか
なり大きいがそれほど強くない。
また雷雲の直下では上向きで10KV/m以上
となる。
従つて中間の点は電界は零となる。
雷雲が第2図中矢印の様に進行するとすれ
ば、点においては下向[Formula]. Although the value is considerably larger than that under clear skies (about -100v/m), it is not so strong. In addition, directly below the thundercloud, the upward direction is more than 10 KV/m. Therefore, the electric field becomes zero at the intermediate point. If the thundercloud moves as shown by the arrow in Figure 2, it will move downward at the point.
【式】から零電位と なり、ついで上向From [Formula], zero potential and and then upward
次に本発明に係る襲雷警報装置の一実施例を図
面に基いて説明する。
第1図の実施例において、1は地表電界値を測
定する目的で使用される地表電界強度測定器であ
る。
これには回転型電界強度測定器(フイールドミ
ル)又はコロナ発生用針電極が用いられる。
2は急変化のセンサー、2′は急変化発生数積
算回路であり、センサー2は地表電界の急変化を
検知し、積算回路2′は変化値が所定値(巾)を
これたものについて所定時間内の発生回数を積算
するためのものである。
センサー2としては、静電誘導感知用静止板電
極などが用いられる。
3は、地表電界値が所定の値を越えたことを検
知する地表電界値検出回路。
4は、地表電界に低周波性の変動が0.3秒〜数
10秒程度の周期で繰り返し現れた場合の(低周波
変動を伴う場合)変動値が、センサーがフイール
ドミルでは10ミリボルト、コロナ電極では10マイ
クロアンペア以上(センサー部分で直接測定した
値)を超えたものの数を所定時間について積算す
る低周波変動数積算回路である。
5は、オワー回路であつて、地表電界値検出回
路3又は積算回路2′からの入力のいずれかが、
所定値を超えたことにより、注意警報発信器6を
作動させる。
7は、アンド回路であつて、前記地表電界値検
出回路3及び積算回路2′からの入力が、ともに
所定値を超えた場合に警戒警報発信器8を動作さ
せる。
9は第2オワー回路であつて地表電界値検出回
路3は低周波変動数積算回路4からの入力が所定
値を著るしく超えた場合、落雷警報発信器10を
動作させる。
注意警報、警戒警報、落雷警報の語句表現は落
雷確率に応じて複数段階の警報を発しうるという
意味での表現であり、例えば注意警報、退避警
報、非常警報という表現を用いても当然同じこと
である。
地表電界値の急変化を検出する検出器としては
増幅器を用い、センサーには静電界の変化分を検
出し得る静電誘導感知用静止板電極などが用いら
れる。
第6図に示す実施例は、より具体的な装置を示
すものである。
基本的に前記第1図実施例と同様の構成であ
り、コロナ発生用針電極1に雨切り型絶縁体30
を介して急変化センサーに該当する半球状電極板
2を設け、これを取付台に装着している。コロナ
発生用針電極1には、リレー接点付きのマイクロ
アンメーター90、継電器91が接続されてい
る。
このマイクロアンメーター90は、中心が零点
で両側に設定針をもており、コロナ電流が測定さ
れ、地表電界値の大きさおよび極性で、設定針に
より継電器91が作動して地表電界値の変動を検
知することができる。
つまり前記符号3の地表電界値検出回路、4の
低周波変動数積算回路の機能をなし、それぞれの
信号を得ることができる。
半球状電極板2には、急変化の積分器2′が接
続されている。
積分器2′は急変化発生数積分回路を有する。
しかして、この構成により、設定値を越える地
表電界値、急変化発生回数、低周波変動数の信号
を得ることができ、継電器11,12,13か
ら、弁別器70(オワー回路5,9、アンド回路
7を含む)を介して各段階の発信器6,8,10
からを所定の警報を発することになる。
なお第6図中符号14,15,16はタイマー
である。
なお前記実施例でも説明するように、地表電界
値の急変化を検出する検出器としては増幅器を用
い、センサーには静電界の変化分を検出し得る静
電誘導感知用静止板電極などが用いられる。
地表電界値の急変化とは、例えば0.001秒以下
の時間内で10ミルボルト以上の誘導電圧の変化幅
のものを指す。
一方、地表電界値の低周波性の変動を検出する
検出器には直流増幅器を用いかつ中心が零で両側
に設定針をもつたマイクロアンメーターなどを用
いる。
この場合のセンサーとしては同じく回転型電界
強度測定器またはコロナ発生用針電極など共用で
きる。
低周波性の電界値とは、上記センサーが直接感
知する値で、回転型電界強度測定器では10ミリボ
ルト以上、コロナ発生用針電極では10マイクロア
ンペア以上の電圧もしくは電流の値が、変化巾
0.3秒〜10数秒程度のゆるやかな変化があつた場
合を指す(第3図b)。
低周波性の電界変動が連続的かつ周期的に発生
する場合は特に活発な雷雲が接近している図中A
の部分に多い。
図中a−bのごとく地表電界値の急変化も混合
するがリレー接点付のマイクロアンメーター等で
検出するため変化巾0.3秒以下の変化はマイクロ
アンメーターの構造上検出されないので、容易に
両者を区別して襲雷判定の要素とすることができ
る。
かつて高名な気象学者バイヤーズの指導のもと
に、1940年代の末ごろ「雷雲計画」という詳細な
研究が行われた。
それによれば雷雲は第5図に示されるような3
段階の成長過程を経ることが教示されている。
雷雲の発生過程において、雲頂が氷結高度をこ
えると、レーダーにエコーがあらわれはじめる。
そのころが雷雲の幼年期である。
それから10〜15分で直径5〜10Km、高さ7〜9
Kmくらいに発達する。
雲内の気流はすべて上昇気流で、中心付近が最
も強い。
気流は地表の収束気流だけでなく、雲の側面か
らも周囲の空気が引き込まれる。
飛行機で横断すると降水が観測されるが上昇気
流にささえられて雲底下には落下しない。
雷雲が発達をつづけ雲頂が一層高くなると上昇
気流内で生成される氷粒、水滴は大粒となり気流
で支えきれず地上に落下し始める。この時期が成
年期の始まりで、その雲形ははつきりした積乱雲
として観測出来る。
巨大な火花放電、雷放電を発生させる雷雲が電
荷をどのような形で分布しているかといえば、夏
の成熟期では雲の上層にプラスの電荷が広がつて
おり、マイナスの電荷は降水領域の中の−20℃〜
−30℃の範囲に比較的濃密に分布している。
これは上昇気流によつて運ばれてゆく細かい氷
晶にはプラス電荷が、重力で落ちてゆく大粒のあ
られ・ひようにマイナスの電荷が分離するような
かたちとなるためにそのような分布になる。
この電荷を分離・蓄積するためにはプラスとマ
イナスが引合う電気力に打ち勝つて両者を分離す
る力が必要であるが、その力は半径5mm以上の大
粒のあられ・ひようが大量に発生する雲のなかで
はじめて有効な力になる。つまり電荷分離−発電
作用という公式が成り立ち、雷が発生することに
なる。
上記の研究報告は本発明の襲雷警報装置が上昇
気流に影響される雷雲の発達とよく対応した適当
なものであることを示している。
〔効果〕
本発明の襲雷警報装置は、前記のような構成で
あり、地表電界値の瞬間的な急変化を積算する方
法と地表電界値の両方を要素としているため、山
地などの雷の発生場所(極く近雷の場所)でも有
効に使用できる。
しかも地表電界値の低周波の変動が雷雲の成長
過程とすこぶる関係の深いことに着目して、それ
らを警報要素の1つに取り入れたため『襲雷のお
それのない時は働らかず、襲雷のおそれのある時
は必ず働く』という精度の高い信頼性のある確実
なる警報が出せるものである。
その調整も一度各々の設定値をセツトすれば以
後は特に判断しなくとも自動的に注意警報や使用
目的に応じた警報(例えば避難指令)や落雷警報
を段階的に出すことができる。本発明の襲雷警報
装置は、信頼性が高くかつ経済的であり、あらゆ
る態様の雷に対処でき、落雷から貴重な財産や尊
い人命を守るため役立つ画期的な発明というべき
である。
Next, an embodiment of the lightning warning device according to the present invention will be described with reference to the drawings. In the embodiment shown in FIG. 1, reference numeral 1 denotes a surface electric field strength measuring instrument used for the purpose of measuring the surface electric field value. For this purpose, a rotating field strength measuring device (field mill) or a needle electrode for corona generation is used. 2 is a sudden change sensor, 2' is a sudden change occurrence number integration circuit, sensor 2 detects a sudden change in the ground electric field, and integration circuit 2' is a predetermined value when the change value exceeds a predetermined value (width). This is to add up the number of occurrences within a period of time. As the sensor 2, a stationary plate electrode for electrostatic induction sensing is used. 3 is a ground electric field value detection circuit that detects that the ground electric field value exceeds a predetermined value. 4 is a low-frequency fluctuation in the ground electric field of 0.3 seconds to several seconds.
The fluctuation value when it appears repeatedly with a period of about 10 seconds (with low frequency fluctuations) exceeds 10 millivolts when the sensor is a field mill, and 10 microamps or more when using a corona electrode (value measured directly at the sensor part). This is a low frequency fluctuation number integration circuit that integrates the number of objects over a predetermined period of time. Reference numeral 5 is an over circuit in which either the input from the ground electric field value detection circuit 3 or the integration circuit 2' is
When the predetermined value is exceeded, the caution alarm transmitter 6 is activated. Reference numeral 7 is an AND circuit which operates the warning alarm transmitter 8 when the inputs from the ground electric field value detection circuit 3 and the integration circuit 2' both exceed a predetermined value. 9 is a second power circuit, and the ground electric field value detection circuit 3 operates the lightning warning transmitter 10 when the input from the low frequency fluctuation number integration circuit 4 significantly exceeds a predetermined value. The phrases "cautionary warning", "cautionary warning", and "lightning warning" mean that multiple levels of warning can be issued depending on the probability of a lightning strike; for example, the expressions "cautionary warning,""evacuationwarning," and "emergency warning" also mean the same thing. It is. An amplifier is used as a detector to detect sudden changes in the ground electric field value, and a stationary plate electrode for electrostatic induction sensing that can detect changes in the electrostatic field is used as a sensor. The embodiment shown in FIG. 6 shows a more specific device. The structure is basically the same as that of the embodiment shown in FIG.
A hemispherical electrode plate 2 corresponding to the sudden change sensor is provided via the holder, and this is mounted on a mounting base. A microammeter 90 with a relay contact and a relay 91 are connected to the needle electrode 1 for corona generation. This microammeter 90 has a zero point at the center and setting needles on both sides.The corona current is measured, and depending on the magnitude and polarity of the ground electric field value, the setting needle operates a relay 91, causing fluctuations in the ground electric field value. can be detected. In other words, it functions as the ground electric field value detection circuit 3 and the low frequency fluctuation number integration circuit 4, and can obtain the respective signals. A rapidly changing integrator 2' is connected to the hemispherical electrode plate 2. The integrator 2' has a sudden change occurrence number integration circuit. With this configuration, it is possible to obtain signals of the ground electric field value exceeding the set value, the number of sudden changes, and the number of low frequency fluctuations. oscillators 6, 8, 10 of each stage via the AND circuit 7)
A predetermined alarm will be issued. Note that numerals 14, 15, and 16 in FIG. 6 are timers. As explained in the above embodiment, an amplifier is used as a detector to detect sudden changes in the ground electric field value, and a stationary plate electrode for electrostatic induction sensing that can detect changes in the electrostatic field is used as a sensor. It will be done. A sudden change in the ground electric field value refers to, for example, a change in induced voltage of 10 millivolts or more within a time of 0.001 seconds or less. On the other hand, the detector for detecting low-frequency fluctuations in the ground electric field value uses a DC amplifier and a microammeter with a zero point at the center and setting needles on both sides. In this case, the sensor may be a rotating electric field strength measuring device or a needle electrode for corona generation. The low frequency electric field value is the value that is directly sensed by the above sensor, and the voltage or current value is 10 millivolts or more for a rotating electric field strength measuring device, or 10 microamperes or more for a corona generation needle electrode.
This refers to a case where there is a gradual change of about 0.3 seconds to 10-odd seconds (Figure 3 b). When low-frequency electric field fluctuations occur continuously and periodically, especially active thunderclouds are approaching A in the diagram.
There are many cases in this area. Sudden changes in the ground electric field value, as shown in a and b in the figure, are also mixed, but since they are detected by a microammeter with a relay contact, changes with a width of less than 0.3 seconds cannot be detected due to the structure of the microammeter, so it is easy to detect both. can be distinguished and used as an element for lightning strike determination. A detailed study called the "Thundercloud Project" was conducted in the late 1940s under the direction of the famous meteorologist Byers. According to this, thunderclouds are formed by three clouds as shown in Figure 5.
They are taught to go through a stage of growth. During the process of thundercloud formation, when the cloud top exceeds the freezing altitude, echoes begin to appear on radar. That was the childhood of thunderclouds. After that, in 10-15 minutes, the diameter was 5-10km, the height was 7-9.
It develops to about Km. All air currents within a cloud are updrafts, and are strongest near the center. Air currents are not limited to converging air currents on the ground, but surrounding air is also drawn in from the sides of the cloud. When you cross it by plane, precipitation is observed, but it is supported by rising air currents and does not fall below the cloud base. As the thundercloud continues to develop and the cloud top becomes higher, the ice particles and water droplets generated in the updraft become large and cannot be supported by the air current and begin to fall to the ground. This period marks the beginning of the adult phase, and the cloud shape can be observed as a sharp cumulonimbus cloud. The way electrical charges are distributed in thunderclouds, which generate huge spark discharges and lightning discharges, is that during the mature stage of summer, positive charges spread to the upper layer of the cloud, and negative charges spread to the upper layer of the cloud. -20℃~
It is relatively densely distributed in the -30℃ range. This is because the fine ice crystals that are carried by the updraft have a positive charge, and the large ice crystals that fall due to gravity have a negative charge that separates. Become. In order to separate and accumulate this charge, a force is needed to overcome the electric force that attracts the positive and negative and separate them, but this force generates a large amount of large hail particles with a radius of 5 mm or more. It becomes an effective force only in the clouds. In other words, the formula of charge separation-power generation is established, and lightning occurs. The above research report shows that the lightning warning system of the present invention is suitable and corresponds well to the development of thunderclouds affected by updrafts. [Effects] The lightning warning device of the present invention has the above-described configuration, and uses both the method of integrating instantaneous sudden changes in the ground electric field value and the ground electric field value, so it can detect lightning strikes in mountainous areas, etc. It can be used effectively even in places where lightning occurs (places where lightning is extremely close). Furthermore, we focused on the fact that low-frequency fluctuations in the ground electric field value are closely related to the growth process of thunderclouds, and incorporated them into one of the warning elements. It is possible to issue a highly accurate, reliable, and reliable warning that is always activated when there is a risk of danger. As for the adjustment, once each set value is set, caution warnings, warnings depending on the purpose of use (for example, evacuation orders), and lightning warnings can be automatically issued step by step without any particular judgment. The lightning warning device of the present invention is highly reliable and economical, can deal with all types of lightning, and can be called an epoch-making invention useful for protecting valuable property and precious human lives from lightning strikes.
第1図は、本発明に係る襲雷警報装置の基本的
な一実施例を示す結線図。第2図〜第5図は雷雲
に関する説明図であつて、第2図は、典型的な雷
雲による地上の電界分布を示す観測図。第3図
は、第2図の点において観測した場合に、地表
電界値の変化を示す模式図であつて、第3図a
は、雷雲接近による全体的な地表電界値の変化と
急変化の発生を示し、第3図bは、第3図a図中
Aで示す範囲あたりに低周波成分が顕著に現れる
場合を示すものである。第4図は、成年期の雷雲
内における電荷分布の模式図。第5図は、幼年
期・成年期・衰弱期の単細胞雷雲の模式図。第6
図は本発明の他の実施例を示す結線図である。
符号の簡単な説明 1…地表電界値測定用セン
サー(コロナ発生用針電極)、2…地表電界値急
変化検知用センサー(半球状電極板)、2′…急変
化発生数積算回路(急変化の積分器)、3…地表
電界値検出回路、4…低周波変動数積算回路、5
…オワー回路、6…注意警報発信器、7…アンド
回路、8…警戒警報発信器、9…第2のオワー回
路、10…落雷警報発信器。
FIG. 1 is a wiring diagram showing a basic embodiment of a lightning warning device according to the present invention. FIGS. 2 to 5 are explanatory diagrams regarding thunderclouds, and FIG. 2 is an observation diagram showing the electric field distribution on the ground due to a typical thundercloud. Figure 3 is a schematic diagram showing changes in the ground electric field value when observed at the points in Figure 2;
Figure 3b shows the occurrence of overall changes and sudden changes in the ground electric field value due to the approach of thunderclouds, and Figure 3b shows the case where low frequency components appear prominently around the range indicated by A in Figure 3a. It is. Figure 4 is a schematic diagram of the charge distribution within an adult thundercloud. Figure 5 is a schematic diagram of a single-cell thundercloud in its childhood, adulthood, and decline stages. 6th
The figure is a wiring diagram showing another embodiment of the present invention. Brief explanation of the symbols 1...Sensor for measuring ground electric field value (needle electrode for corona generation), 2...Sensor for detecting sudden changes in ground electric field value (hemispherical electrode plate), 2'...Sudden change occurrence number integration circuit (sudden change (integrator), 3... Ground electric field value detection circuit, 4... Low frequency fluctuation number integration circuit, 5
...Ower circuit, 6...Caution alarm transmitter, 7...AND circuit, 8...Warning alarm transmitter, 9...Second Ower circuit, 10...Lightning warning transmitter.
Claims (1)
次のを備え、地表電界値と所定時間内の地
表電界値の急変化の発生回数を積算した数値のう
ちそのいづれかが設定値を越えた段階、その両方
共設定値を越えた段階、さらに前記地表電界値が
著しく大となつた段階あるいは前記急変化とは異
なる低周波性の地表電界値の変動が発生した段階
と、複数段階の警報を発し得ることを特徴とする
襲雷警報装置。 地表電界値を測定する回転型電界強度測定器
(フイールドミル)又はコロナ発生用針電極な
どのセンサー。 地表電界値の急変化を検知するセンサーおよ
び所定時間内の所定値以上の急変化の発生回数
を積算する急変化発生数積算回路。 地表電界値の低周波性の変動を検知する回
路。[Claims] 1. In a lightning warning device using electric field strength measurement method,
A stage in which one of the ground electric field value and the cumulative number of occurrences of sudden changes in the ground electric field value within a predetermined time exceeds a set value, a stage in which both exceed the set value, and a stage in which the above-mentioned A lightning strike warning device capable of issuing a warning in multiple stages, including a stage when the ground electric field value becomes extremely large or a stage when a low-frequency fluctuation in the ground electric field value different from the sudden change occurs. Sensors such as a rotating electric field strength meter (field mill) that measures the ground electric field value or a needle electrode for corona generation. A sensor that detects sudden changes in the ground electric field value and a sudden change occurrence count integration circuit that adds up the number of sudden changes that are greater than or equal to a predetermined value within a predetermined time. A circuit that detects low-frequency fluctuations in ground electric field values.
Priority Applications (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP9948381A JPS58789A (en) | 1981-06-26 | 1981-06-26 | Alarm device for visitation of thunder |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP9948381A JPS58789A (en) | 1981-06-26 | 1981-06-26 | Alarm device for visitation of thunder |
Publications (2)
| Publication Number | Publication Date |
|---|---|
| JPS58789A JPS58789A (en) | 1983-01-05 |
| JPH0132959B2 true JPH0132959B2 (en) | 1989-07-11 |
Family
ID=14248550
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP9948381A Granted JPS58789A (en) | 1981-06-26 | 1981-06-26 | Alarm device for visitation of thunder |
Country Status (1)
| Country | Link |
|---|---|
| JP (1) | JPS58789A (en) |
Families Citing this family (5)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| FR2602342B1 (en) * | 1986-07-31 | 1989-06-02 | Onera (Off Nat Aerospatiale) | METHOD AND APPARATUS FOR DETECTING THE APPEARANCE AND DISAPPEARANCE OF ATMOSPHERIC ELECTRICAL PHENOMENES LINKED TO A THUNDERSTORM |
| FR2602343B1 (en) * | 1986-07-31 | 1989-05-05 | Onera (Off Nat Aerospatiale) | METHOD AND INSTALLATION FOR PREDICTING THE EVOLUTION OF ATMOSPHERIC ELECTRICAL PHENOMENES LINKED TO A THUNDERSTORM |
| JPH0627876B2 (en) * | 1990-04-27 | 1994-04-13 | 儀一郎 加藤 | Multi-function lightning alarm |
| CA2015774C (en) * | 1990-04-30 | 1995-07-25 | Giichiro Kato | Apparatus for detection the onset of thunderstorms and the occurrence of nearby lightning |
| JP6937874B1 (en) * | 2020-07-15 | 2021-09-22 | 株式会社昭電 | Lightning strike alarm device |
-
1981
- 1981-06-26 JP JP9948381A patent/JPS58789A/en active Granted
Also Published As
| Publication number | Publication date |
|---|---|
| JPS58789A (en) | 1983-01-05 |
Similar Documents
| Publication | Publication Date | Title |
|---|---|---|
| US5771020A (en) | Lightning locating system | |
| Winn et al. | Electric field growth in thunderclouds | |
| Takahashi | Measurement of electric charge of cloud droplets, drizzle, and raindrops | |
| Yang et al. | Near-surface sand-dust horizontal flux in Tazhong—the hinterland of the Taklimakan Desert | |
| Chauzy et al. | Multilevel measurement of the electric field underneath a thundercloud: 1. A new system and the associated data processing | |
| CN104048640A (en) | Intelligent landslide catastrophe monitoring method based on L-type liquid metal antennas | |
| Latham et al. | Airborne studies of the electrical properties of large convective clouds | |
| JPH0132959B2 (en) | ||
| Ramamurthy et al. | Evidence of very-large-amplitude solitary waves in the atmosphere | |
| CN109035709A (en) | A kind of method for early warning, the apparatus and system of mountain torrents mud-rock flow | |
| Opachat et al. | Smart lightning warning system based on electric field sensor | |
| JPH049792A (en) | Multifunctional type thunder alarm | |
| Mikhailovsky et al. | The features of thunderstorm activity control by different radiophysical measuring instruments (radar, lightning detection systems, ground-based fluxmeters) | |
| Jones et al. | Plumes of electric space charge in the lower atmosphere | |
| Winn et al. | Electric field at the ground in a large tornado | |
| Kwon et al. | Airborne sodium lidar measurements of gravity wave intrinsic parameters | |
| Dye et al. | Final report on the Airborne Field Mill Project (ABFM) 2000-2001 field campaign | |
| Rust et al. | Microwave radiometric detection of corona from chaff within thunderstorms | |
| CN110927725B (en) | Lightning early warning and monitoring method based on meteorological radar | |
| Delannoy et al. | Airborne Measurements of the Charge of Precipitating Particles Related to Radar Reflectivity and Temperature within two Different Convective Clouds. | |
| NARITA | Aoba, Aramaki, Aoba-ku, Sendai, 980, JAPAN | |
| KRAUS et al. | Severe thunderstorm and tornado warning in real time by color display of Doppler velocities[Interim Report] | |
| Johnson et al. | A study of the comparative performance of six lightning warning systems | |
| Lerfald | Feasibility of monitoring aerosol concentrations by 10. 6-micrometer backscatter lidar | |
| Chmielewski | Variations of the vertical electric field and wind speed on days with airborne dust in Lubbock, Texas |