JPH0733142Y2 - Atmospheric pressure determination device and weather prediction device using the device - Google Patents

Atmospheric pressure determination device and weather prediction device using the device

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Publication number
JPH0733142Y2
JPH0733142Y2 JP507691U JP507691U JPH0733142Y2 JP H0733142 Y2 JPH0733142 Y2 JP H0733142Y2 JP 507691 U JP507691 U JP 507691U JP 507691 U JP507691 U JP 507691U JP H0733142 Y2 JPH0733142 Y2 JP H0733142Y2
Authority
JP
Japan
Prior art keywords
atmospheric pressure
weather
determination
low
value
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
JP507691U
Other languages
Japanese (ja)
Other versions
JPH04102440U (en
Inventor
博三 大崎
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.)
Fujikura Ltd
Oki Electric Industry Co Ltd
Original Assignee
Fujikura Ltd
Oki Electric Industry 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 Fujikura Ltd, Oki Electric Industry Co Ltd filed Critical Fujikura Ltd
Priority to JP507691U priority Critical patent/JPH0733142Y2/en
Publication of JPH04102440U publication Critical patent/JPH04102440U/en
Application granted granted Critical
Publication of JPH0733142Y2 publication Critical patent/JPH0733142Y2/en
Anticipated expiration legal-status Critical
Expired - Lifetime legal-status Critical Current

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Description

【考案の詳細な説明】[Detailed description of the device]

【0001】[0001]

【産業上の利用分野】本考案は天候予測の一手法として
使用される気圧の高低判定装置及び該装置を使用した天
候予測装置に関するものである。
BACKGROUND OF THE INVENTION 1. Field of the Invention The present invention relates to an atmospheric pressure level determining device used as a weather forecasting method and a weather forecasting device using the device.

【0002】[0002]

【従来技術】ある地域を高気圧が覆えば天候が良く、低
気圧が近づけば天候が悪化することから、ある地点での
天候を簡易に予測するものとして、気圧の高低判定装置
がある。図2は、従来の気圧の高低判定装置の構成を示
すブロック図である。図2において、1は気圧を測定す
る気圧測定部、2は前記気圧測定部1で測定した測定気
圧値を記憶する気圧記憶部、3は現在高気圧か低気圧か
を判定し、気圧の変動状況から今後気圧と天候を予測す
る天候判定部である。
2. Description of the Related Art The weather is good if a high pressure covers a certain area, and the weather worsens if a low pressure approaches. Therefore, there is a high / low pressure determination device for simply predicting the weather at a certain point. FIG. 2 is a block diagram showing the structure of a conventional atmospheric pressure height determination device. In FIG. 2, reference numeral 1 is an atmospheric pressure measuring unit that measures atmospheric pressure, 2 is an atmospheric pressure storage unit that stores the measured atmospheric pressure value measured by the atmospheric pressure measuring unit 1, and 3 is a high atmospheric pressure or a low atmospheric pressure, and the atmospheric pressure fluctuation state Is a weather determination unit that predicts atmospheric pressure and weather from now on.

【0003】ここで、高気圧や低気圧とは、周囲の気圧
に比べて当該地域の気圧が高いか低いかという、相対的
な気圧の高低の現象である。言い替えれば、ある地点を
対象にした場合、その地点の平均的な気圧に対して現在
の気圧が高いか低いかを示すものといえる。
Here, the high pressure and the low pressure are phenomena in which the relative atmospheric pressure is high or low as to whether the atmospheric pressure in the area is higher or lower than the ambient pressure. In other words, when a certain point is targeted, it can be said that the present atmospheric pressure is higher or lower than the average atmospheric pressure at that point.

【0004】実際の天候は、この気圧の高低のみではな
く、その他の多くの要因を含めて決まるものであり、幾
つかの手法を併用して天候を予測する天候予測装置も多
いが、高気圧か低気圧かは天候予測において依然として
重要な要素であることには変わりがない。
The actual weather is determined not only by the high and low of this atmospheric pressure but also by many other factors, and there are many weather forecasting devices that forecast the weather by using some methods together. Low pressure is still an important factor in weather forecasting.

【0005】[0005]

【考案が解決しようとする課題】図3は気圧の高低によ
り天候を判定する方法例を示す図である。図3において
は、天候判定の一例として標準大気圧である1013ミ
リバールを基準値として、気圧の高低を判定し、高い気
圧範囲(T1)にある場合を晴れ、低い気圧範囲(T
3)にある場合を雨、中間の気圧範囲(T2)にある場
合を曇りと分ける例を示している。
FIG. 3 is a diagram showing an example of a method for judging the weather based on whether the atmospheric pressure is high or low. In FIG. 3, as an example of weather determination, a standard atmospheric pressure of 1013 mbar is used as a reference value to determine whether the atmospheric pressure is high or low, and a high atmospheric pressure range (T1) is clear, and a low atmospheric pressure range (T1).
An example is shown in which the case 3) is divided into rain and the case in the middle pressure range (T2) is divided into cloudy.

【0006】しかしながら、気圧の絶対値は気圧を測定
する測定点の海抜の高さ(海抜高度)によって異なるの
で、気圧の測定値から気圧の高低を判定するためには、
上記基準値をその場所によってそれぞれ定める必要があ
る。
However, since the absolute value of the atmospheric pressure differs depending on the altitude (altitude above sea level) of the measuring point for measuring the atmospheric pressure, in order to determine the level of the atmospheric pressure from the measured value of the atmospheric pressure,
It is necessary to determine the above-mentioned standard values depending on the location.

【0007】従来は、図2に示すように、高度補正部5
を設け、その地点の海抜高度によって基準値の補正をお
こなっている。しかしながら、測定場所の海抜高度は正
確にわからないことが多く、また気圧測定をビル内で行
う場合は測定場所の階数によっても海抜高度が変わる
等、上記基準値の変更には困難がつきまとうという問題
がある。
Conventionally, as shown in FIG. 2, the altitude correction unit 5
Is provided and the standard value is corrected according to the altitude above sea level. However, the altitude above sea level at the measurement location is often unknown, and when the barometric pressure is measured inside the building, the altitude above sea level also changes depending on the number of floors at the measurement site, which makes it difficult to change the above reference values. is there.

【0008】特に、装置を動作させた初期には、過去の
測定値がなく変動状況の要素が判断に寄与しないため高
度補正が正しく行われないと、気圧の判定が現状と全く
異なる判定となるという問題がある。
Particularly, in the initial stage of operating the apparatus, there is no past measured value, and the factors of the fluctuation situation do not contribute to the determination. Therefore, if the altitude correction is not performed correctly, the determination of the atmospheric pressure becomes a determination different from the current state. There is a problem.

【0009】本考案は上述の点に鑑みてなされたもの
で、上記問題点、即ち気圧の高低を判定するとき、気圧
測定点の海抜高度による判定基準値の補正を必要とする
という問題点を簡易に解決できる気圧の高低判定装置及
び該装置を用いた天候予測装置を提供することを目的と
する。
The present invention has been made in view of the above points, and has the above-mentioned problem, that is, when determining the level of atmospheric pressure, it is necessary to correct the determination reference value according to the altitude above sea level of the atmospheric pressure measurement point. It is an object of the present invention to provide an atmospheric pressure level determination device that can be easily solved, and a weather prediction device using the device.

【0010】[0010]

【課題を解決するため手段】上記課題を解決するため本
考案は、天候予測のため気圧を測定し、該測定値と所定
の判定基準値とを比較し、該測定値の高低を判定する気
圧の高低判定装置であって、装置起動時に判定基準を変
更することにより、測定値の高低判定結果を強制的に変
化させ、該高低の判定結果を現状の天候状態に合わせる
初期校正部を設けたことを特徴とする。
In order to solve the above problems, the present invention measures the atmospheric pressure for weather prediction, compares the measured value with a predetermined judgment reference value, and judges the high or low of the measured value. The device for determining whether the height is high or low, forcibly changing the high or low determination result of the measurement value by changing the determination standard at the time of starting the device, and providing an initial calibration unit for adjusting the high or low determination result to the current weather condition. It is characterized by

【0011】また、天候予測のために幾つかの手法を使
用して天候を総合的に判定する天候予測装置のこの幾つ
かの手法の一つとして上記気圧の高低判定装置を使用す
ることを特徴とする。
Further, as one of the several methods of the weather forecasting apparatus for comprehensively judging the weather by using some methods for forecasting the weather, the above-mentioned atmospheric pressure level determining apparatus is used. And

【0012】[0012]

【作用】気圧判定装置を上記のように構成することによ
り、初期校正部は、起動時に測定気圧値の高低の判定結
果を現在の天候に合わせることで逆に判定基準値を補正
し、以後の高低の判定にこの判定基準値を利用する。こ
れにより、以後の天候予測が正確となり、且つ起動後比
較的早く天候の予測が可能となる。
By configuring the atmospheric pressure determination device as described above, the initial calibration unit reversely corrects the determination reference value by matching the determination result of whether the measured atmospheric pressure value is high or low at the time of startup, and This judgment reference value is used for judgment of high and low. This makes it possible to accurately predict the weather thereafter, and to predict the weather relatively early after the start.

【0013】[0013]

【実施例】以下、本考案の一実施例を図面に基づいて説
明する。図1は、本考案の一実施例である気圧の高低判
定装置の構成を示すブロック図である。
DETAILED DESCRIPTION OF THE PREFERRED EMBODIMENTS An embodiment of the present invention will be described below with reference to the drawings. FIG. 1 is a block diagram showing the configuration of an atmospheric pressure level determining apparatus according to an embodiment of the present invention.

【0014】本気圧の高低判定装置は、図2の装置と同
様、気圧測定部1、気圧記憶部2及び天候判定部3を具
備する。天候判定部3は図2の天候判定部3と同様、気
圧の高低による天候判定を図3で示す判定方法で行う。
4は初期校正部であり、該初期校正部4は、装置が動作
を始めたとき過去の測定値を全て現在の測定値に書換え
る作用をする記憶書換部4−1とスイッチ4−3からの
指示で判定基準値を順次変える判定変更部4−2とで構
成される。
The apparatus for determining the level of this atmospheric pressure comprises an atmospheric pressure measuring section 1, an atmospheric pressure storage section 2 and a weather determining section 3 as in the apparatus of FIG. The weather determination unit 3 performs the weather determination based on the level of atmospheric pressure by the determination method shown in FIG. 3, similarly to the weather determination unit 3 in FIG.
Reference numeral 4 denotes an initial calibrating unit, and the initial calibrating unit 4 includes a memory rewriting unit 4-1 and a switch 4-3 which operate to rewrite all past measured values to the present measured values when the apparatus starts operating. The determination change unit 4-2 sequentially changes the determination reference value in response to the instruction.

【0015】図4は上記構成の気圧高低判定装置の判定
動作を示した図である。以下、図4に基づいて判定動作
を説明する。仮に装置起動時の気圧測定値が1000ミ
リバールで、実際の天候が曇りであったとする。初期校
正部4の記憶書換部4−1は気圧記憶部2の記憶値をこ
の測定値1000ミリバールに書き替える。これによっ
て過去に気圧の変化はなかった事になり天候判定部3の
予測する今後の天候は現在と同一になる。
FIG. 4 is a diagram showing a judgment operation of the atmospheric pressure high / low judgment device having the above structure. The determination operation will be described below with reference to FIG. It is assumed that the measured atmospheric pressure at the time of starting the device is 1000 mbar and the actual weather is cloudy. The memory rewriting unit 4-1 of the initial calibration unit 4 rewrites the stored value of the atmospheric pressure storage unit 2 into the measured value of 1000 mbar. As a result, the atmospheric pressure has not changed in the past, and the future weather predicted by the weather determination unit 3 becomes the same as the present.

【0016】上記測定値1000ミリバールを標準的気
圧である1013ミリバールを基準値として、天候判定
部3において気圧の高低の判定を行った場合、天候は雨
と予測される(図3参照)。そこでここでは、実際の天
候が曇りであることから、初期校正部4のスイッチ4−
3を操作し、判定の基準となる判定基準値を所定量だけ
下方に下げる操作を行い、判定変更部4−2を介して判
定基準値の補正を行う。そしてこの補正された基準値に
基づいて気圧の高低を判定し、該判定結果から天候の予
測を行う。この天候の予測が雨であった場合は、さらに
判定基準値を下げ、気圧の高低を判定し、この判定から
天候の予測を行う。そしてこの天候の予測値が現在の天
候、即ち曇りになるまで行う。
When the measured pressure value of 1000 mbar is used as a standard value of 1013 mbar, which is a standard atmospheric pressure, when the weather determination unit 3 determines whether the atmospheric pressure is high or low, the weather is predicted to be rain (see FIG. 3). Therefore, here, since the actual weather is cloudy, the switch 4-
3 is operated to lower the judgment reference value serving as a judgment reference downward by a predetermined amount, and the judgment reference value is corrected via the judgment changing unit 4-2. Then, the level of the atmospheric pressure is determined based on the corrected reference value, and the weather is predicted from the determination result. If the weather is predicted to be rain, the judgment reference value is further lowered to judge whether the atmospheric pressure is high or low, and the weather is predicted from this judgment. Then, the process is performed until the predicted value of the weather becomes the present weather, that is, cloudy.

【0017】本実施例では、予測天候は晴れ、曇り、雨
の3種であり、スイッチ4−3を操作したとき、何回か
は同一出力となるが、操作を繰り返すことによって現在
の天候に一致させることができる。また、例えば、現在
の天候が雨よりの曇りであるときは、図4に示すように
現在の気圧1000ミリバールを曇りと判断する気圧範
囲(T2)の雨と判断する気圧範囲(T3)に寄せて設
定すればよい。
In the present embodiment, there are three types of forecast weather: sunny, cloudy, and rain. When the switch 4-3 is operated, the same output is obtained several times, but by repeating the operation, the current weather can be obtained. Can be matched. Further, for example, when the present weather is cloudy rather than rain, as shown in FIG. 4, the present atmospheric pressure of 1000 mbar is moved to the atmospheric pressure range (T3) which is judged to be rain in the atmospheric pressure range (T2) which is judged to be cloudy. And set it.

【0018】上記気圧の高低の判定は、測定気圧値と判
定基準値との差で行うから、使用した判定基準値、例え
ば1013ミリバールをそれより下方に下げることと、
測定気圧値を補正して上げることは同じことであり、測
定気圧値を補正する方法も可能である。
Since the above-mentioned judgment of the atmospheric pressure is made by the difference between the measured atmospheric pressure value and the judgment reference value, the judgment reference value used, for example, 1013 mbar is lowered below that.
Correcting and increasing the measured atmospheric pressure value is the same, and a method of correcting the measured atmospheric pressure value is also possible.

【0019】以後この補正値を記憶して判定基準値や測
定値を校正して使用すればよい。
Thereafter, the correction value may be stored and the judgment reference value and the measured value may be calibrated before use.

【0020】[0020]

【考案の効果】以上説明したように本考案によれば、簡
易な初期校正部を設け、起動時に操作することにより、
実行を怠りがちである海抜高度による補正に代えること
ができ、高気圧・低気圧の判定がより正確になると共
に、初期特性の向上も期待できる。
As described above, according to the present invention, by providing a simple initial calibration unit and operating it at startup,
It is possible to substitute the correction based on the altitude above sea level, which is apt to be neglected, so that the determination of high pressure / low pressure becomes more accurate, and the initial characteristics can be expected to improve.

【0021】また、気圧の測定には、正確な校正が必要
であるが、本考案では使用時に補正するので必ずしも正
確な絶対値の校正は必要でなく、天候予測のみが目的で
あれば装置の簡略化が可能になる。
In addition, although accurate calibration is necessary for measuring the atmospheric pressure, since the present invention corrects it at the time of use, accurate calibration of the absolute value is not always necessary. Simplification is possible.

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

【図1】本考案の気圧の高低判定装置の構成を示すブロ
ック図である。
FIG. 1 is a block diagram showing the configuration of a device for determining the level of atmospheric pressure according to the present invention.

【図2】従来の気圧の高低判定装置の構成を示すブロッ
ク図である。
FIG. 2 is a block diagram showing a configuration of a conventional atmospheric pressure height determination device.

【図3】気圧による天候判定例を説明するための図であ
る。
FIG. 3 is a diagram for explaining an example of weather determination based on atmospheric pressure.

【図4】本考案の気圧高低判定装置の判定動作を説明す
るための図である。
FIG. 4 is a diagram for explaining a determination operation of the atmospheric pressure height determination device of the present invention.

【符号の説明】[Explanation of symbols]

1 気圧測定部 2 気圧記憶部 3 天候判定部 4 初期校正部 4−1 記憶書換部 4−2 判定変更部 4−3 スイッチ 1 Atmospheric pressure measurement unit 2 Atmospheric pressure storage unit 3 Weather determination unit 4 Initial calibration unit 4-1 Memory rewriting unit 4-2 Determination change unit 4-3 Switch

Claims (2)

【実用新案登録請求の範囲】[Scope of utility model registration request] 【請求項1】天候予測のため気圧を測定し、該測定値と
所定の判定基準値とを比較し、該測定値の高低を判定す
る気圧の高低判定装置であって、装置起動時に前記判定
基準を変更することにより、測定値の高低判定結果を強
制的に変化させ、該高低の判定結果を現状の天候状態に
合わせる初期校正部を設けたことを特徴とする気圧の高
低判定装置。
1. An atmospheric pressure level determination device for determining atmospheric pressure for weather prediction, comparing the measured value with a predetermined determination reference value, and determining whether the measured value is high or low. An apparatus for determining whether the atmospheric pressure is high or low, in which an initial calibration unit for forcibly changing the determination result of the measured value by changing the reference and matching the determination result of the height with the current weather condition is provided.
【請求項2】天候予測のために幾つかの手法を使用して
天候を総合的に判定する天候予測装置であって、前記天
候予測の手法の一つとして請求項1記載の気圧の高低判
定装置を使用することを特徴とする天候予測装置。
2. A weather forecasting apparatus that comprehensively determines the weather by using several methods for weather forecasting, wherein the atmospheric pressure level determination according to claim 1 is one of the weather forecasting methods. A weather forecasting device characterized by using the device.
JP507691U 1991-01-18 1991-01-18 Atmospheric pressure determination device and weather prediction device using the device Expired - Lifetime JPH0733142Y2 (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
JP507691U JPH0733142Y2 (en) 1991-01-18 1991-01-18 Atmospheric pressure determination device and weather prediction device using the device

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP507691U JPH0733142Y2 (en) 1991-01-18 1991-01-18 Atmospheric pressure determination device and weather prediction device using the device

Publications (2)

Publication Number Publication Date
JPH04102440U JPH04102440U (en) 1992-09-03
JPH0733142Y2 true JPH0733142Y2 (en) 1995-07-31

Family

ID=31735356

Family Applications (1)

Application Number Title Priority Date Filing Date
JP507691U Expired - Lifetime JPH0733142Y2 (en) 1991-01-18 1991-01-18 Atmospheric pressure determination device and weather prediction device using the device

Country Status (1)

Country Link
JP (1) JPH0733142Y2 (en)

Also Published As

Publication number Publication date
JPH04102440U (en) 1992-09-03

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