CN108195558B - A kind of ascending air measurement method for weather modification aircraft - Google Patents

A kind of ascending air measurement method for weather modification aircraft Download PDF

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CN108195558B
CN108195558B CN201711280576.8A CN201711280576A CN108195558B CN 108195558 B CN108195558 B CN 108195558B CN 201711280576 A CN201711280576 A CN 201711280576A CN 108195558 B CN108195558 B CN 108195558B
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cos
sin
cosβ
ascending air
vtz
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CN108195558A (en
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孔宪书
李培仁
郝奎
高龙
孙鸿娉
李钰
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Shanxi Province Office Of Artificial Rainfall Hail
Taiyuan Aero Instruments Co Ltd
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Shanxi Province Office Of Artificial Rainfall Hail
Taiyuan Aero Instruments Co Ltd
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    • G01MEASURING; TESTING
    • G01MTESTING STATIC OR DYNAMIC BALANCE OF MACHINES OR STRUCTURES; TESTING OF STRUCTURES OR APPARATUS, NOT OTHERWISE PROVIDED FOR
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  • Fluid Mechanics (AREA)
  • General Physics & Mathematics (AREA)
  • Length Measuring Devices With Unspecified Measuring Means (AREA)
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Abstract

The invention belongs to aeronautical meteorology field, specifically a kind of ascending air measurement method for weather modification aircraft.Solve the problems, such as that conventional method ascending air can not be settled accounts, include the following steps, 101~obtain true air speed Vt, angle of attack and yaw angle β that fixed wing aircraft flies, 102~by vector VtSb=(VtX, VtY, VtZ) earth axes are transformed to by body coordinate system, 103~obtain the three-dimensional ground velocity VgXg of fixed wing aircraft flight, VgYg, VgZg, pitching angle theta, roll angle Φ and course angle Ψ;104~in ground coordinate system, three-dimensional ground velocity subtracts three-dimensional air speed and obtains ascending air.The present invention can accurately measure ascending air, and the measurement of ascending air can be used to judge cloud interior air-flow direction and size in the field of increasing rain artificially, and for the formulation of artificial rain operation scheme, improve catalytic efficiency.

Description

A kind of ascending air measurement method for weather modification aircraft
Technical field
The invention belongs to aeronautical meteorology field, specifically a kind of ascending air measurement side for weather modification aircraft Method.
Background technique
Meteorological field mainly passes through the measurement that release balloon carries out upper-level winds at present, and the balloon that will ascend to heaven is as mobile with air-flow Particle, with ground installation tracking balloon track of ascending to heaven, read the elevation angle, azimuth, oblique distance of its time interval, determine its sky Between position coordinate values, the mean wind speed wind direction in the passed through height of balloon can be found out.This method be only capable of measuring horizontal wind speed and Horizontal wind direction cannot detect ascending air, and a detection time is not substantially less than 2h, and space-time is representative poor.
Some carry out upper air wind finding using fixed wing aircraft, when aircraft keeps horizontal flight posture, the speed of a ship or plane, air speed and The vector triangle relationship that wind speed is constituted calculates upper-level winds, is also only capable of resolving and obtains horizontal wind, is unable to get ascending air.
Summary of the invention
The present invention provides a kind of for weather modification to solve the problems, such as that conventional method ascending air can not be settled accounts The ascending air measurement method of aircraft.
The present invention takes following technical scheme: a kind of ascending air measurement method for weather modification aircraft, packet Include following steps,
101~true air speed Vt, angle of attack and yaw angle β that fixed wing aircraft flies are obtained, according to angle of attack, yaw angle β meter Three-dimensional component VtX, VtY, the VtZ of true air speed Vt in the body coordinate system are calculated, vector VtSb=(VtX, VtY, VtZ) is denoted as, Wherein: VtX=Vt*cos β * cos α, VtY=Vt*sin β, VtZ=Vt*cos β * sin α;
102~be denoted as vector VtSb=(VtX, VtY, VtZ) by the vector that body coordinate system transforms to earth axes VtSg=(VtXg, VtYg, VtZg);Transition matrix of the body coordinate system Sb to earth axes Sg are as follows:
VtSg=SθψФ× VtSb, wherein
VtYg=VtX*cos θ * sin ψ+VtY* (sin θ * sin ψ * sin φ+cos ψ * cos φ)+VtZ* (sin θ * sin ψ * cosφ-cosψ*sinφ)
VtZg=VtY*cos θ * sin φ+VtZ*cos θ * cos φ-VtX*sin θ;
VtX, VtY, VtZ are substituted into joint account in above-mentioned three formula to obtain:
VtXg=Vt* (cos α * cos β * cos θ * cos ψ+sin β * sin θ * cos ψ * sin φ-sin β * sin ψ * cos φ+ sinα*cosβ*sinθ*cosψ*cosφ+sinα*cosβ*sinψ*sinφ)
VtYg=Vt* (cos α * cos β * cos θ * sin ψ+sin β * sin θ * sin ψ * sin φ+sin β * cos ψ * cos φ+ sinα*cosβ*sinθ*sinψ*cosφ-sinα*cosβ*cosψ*sinφ)
103~obtain three-dimensional ground velocity VgXg, VgYg that fixed wing aircraft flies, VgZg, pitching angle theta, roll angle Φ and boat To angle Ψ;
104~in earth axes, three-dimensional ground velocity subtracts three-dimensional air speed and obtains ascending air.By three-dimensional ground velocity and three-dimensional space Speed vector subtraction in earth axes obtains three-dimensional velocity, relative to earth axes, i.e.,
VwXg=VgXg-VtXg
VwYg=VgYg-VtYg
VwZg=VgZg-VtZg
VwXg=VgXg-Vt (cos α * cos β * cos θ * cos ψ+sin β * sin θ * cos ψ * sin φ-sin β * sin ψ * cos φ+sinα*cosβ*sinθ*cosψ*cosφ+sinα*cosβ*sinψ*sinφ)
VwYg=VgYg-Vt (cos α * cos β * cos θ * sin ψ+sin β * sin θ * sin ψ * sin φ+sin β * cos ψ * cos φ+sinα*cosβ*sinθ*sinψ*cosφ-sinα*cosβ*cosψ*sinφ)
VwZg=VgZg-Vt (sin β * cos θ * sin φ+sin α * cos β * cos θ * cos φ-cos α * cos β * sin θ)
Wherein: VwXg is the east orientation wind that north orientation wind speed, the VwYg relative to earth axes are relative to earth axes Speed, VwZg are the ascending air relative to earth axes.
The measurement of ascending air is the important indicator increased rain artificially, and one side Yun Zhongyou ascending air proves that cloud is in development Stage, catalysis potentiality with higher prove that cloud is in the mature and extinction stage if Yun Zhongwei down current, catalysis potentiality compared with It is low.On the other hand there is the place of ascending air that can sow catalyst in cloud base, brought into entire cloud by ascending air, so that Catalyst distribution is more uniform.
Compared with prior art, the present invention can calculate rising by the atmospheric parameter and flight parameter of fixed wing aircraft Air-flow, the deficiency of ascending air cannot accurately be measured at present by solving meteorological field.The present invention can accurately measure ascending air, rise The measurement of air-flow can be used to judge cloud interior air-flow direction and size in the field of increasing rain artificially, for the formulation of artificial rain operation scheme, Improve catalytic efficiency.
Detailed description of the invention
Fig. 1 is flow chart of the present invention.
Specific embodiment
To keep the technical problem to be solved in the present invention, technical solution and advantage clearer, below in conjunction with attached drawing and tool Body embodiment is described in detail.
A kind of ascending air measurement method for weather modification aircraft, includes the following steps,
101~true air speed Vt, angle of attack and yaw angle β that fixed wing aircraft flies are obtained, according to angle of attack, yaw angle β meter Three-dimensional component VtX, VtY, the VtZ of true air speed Vt in the body coordinate system are calculated, vector VtSb=(VtX, VtY, VtZ) is denoted as, Wherein: VtX=Vt*cos β * cos α, VtY=Vt*sin β, VtZ=Vt*cos β * sin α;
102~be denoted as vector VtSb=(VtX, VtY, VtZ) by the vector that body coordinate system transforms to earth axes VtSg=(VtXg, VtYg, VtZg);Transition matrix of the body coordinate system Sb to earth axes Sg are as follows:
VtSg=sθψФ× VtSb, wherein
VtYg=VtX*cos θ * sin ψ+VtY* (sin θ * sin ψ * sin φ+cos ψ * cos φ)+VtZ* (sin θ * sin ψ * cosφ-cosψ*sinφ)
VtZg=VtY*cos θ * sin φ+VtZ*cos θ * cos φ-VtX*sin θ;
VtX, VtY, VtZ are substituted into joint account in above-mentioned three formula to obtain:
VtXg=Vt* (cos α * cos β * cos θ * cos ψ+sin β * sin θ * cos ψ * sin φ-sin β * sin ψ * cos φ+ sinα*cosβ*sinθ*cosψ*cosφ+sinα*cosβ*sinψ*sinφ)
VtYg=Vt* (cos α * cos β * cos θ * sin ψ+sin β * sin θ * sin ψ * sin φ+sin β * cos ψ * cos φ+ sinα*cosβ*sinθ*sinψ*cosφ-sinα*cosβ*cosψ*sinφ)
103~obtain three-dimensional ground velocity VgXg, VgYg that fixed wing aircraft flies, VgZg, pitching angle theta, roll angle Φ and boat To angle Ψ;
104~in earth axes, three-dimensional ground velocity subtracts three-dimensional air speed and obtains ascending air.By three-dimensional ground velocity and three-dimensional space Speed vector subtraction in ground coordinate system obtains three-dimensional velocity, relative to earth axes, i.e.,
VwXg=VgXg-VtXg
VwYg=VgYg-VtYg
VwZg=VgZg-VtZg
VwXg=VgXg-Vt (cos α * cos β * cos θ * cos ψ+sin β * sin θ * cos ψ * sin φ-sin β * sin ψ * cos φ+sinα*cosβ*sinθ*cosψ*cosφ+sinα*cosβ*sinψ*sinφ)
VwYg=VgYg-Vt (cos α * cos β * cos θ * sin ψ+sin β * sin θ * sin ψ * sin φ+sin β * cos ψ * cos φ+sinα*cosβ*sinθ*sinψ*cosφ-sinα*cosβ*cosψ*sinφ)
VwZg=VgZg-Vt (sin β * cos θ * sin φ+sin α * cos β * cos θ * cos φ-cos α * cos β * sin θ)
Wherein: VwXg is the east orientation wind that north orientation wind speed, the VwYg relative to earth axes are relative to earth axes Speed, VwZg are the ascending air relative to earth axes.
The above is a preferred embodiment of the present invention, it is noted that for those skilled in the art For, without departing from the principles of the present invention, several improvements and modifications can also be made, these improvements and modifications It should be regarded as protection scope of the present invention.

Claims (3)

1. a kind of ascending air measurement method for weather modification aircraft, it is characterised in that:
Include the following steps,
101~true air speed Vt, angle of attack and yaw angle β that fixed wing aircraft flies are obtained, according to angle of attack, yaw angle β is calculated Three-dimensional component VtX, VtY, the VtZ of true air speed Vt in the body coordinate system, are denoted as vector VtSb=(VtX, VtY, VtZ), in which: VtX=Vt*cos β * cos α, VtY=Vt*sin β, VtZ=Vt*cos β * sin α;
102~vector VtSb=(VtX, VtY, VtZ) is denoted as VtSg by the vector that body coordinate system transforms to earth axes =(VtXg, VtYg, VtZg);
103~obtain three-dimensional ground velocity VgXg, VgYg that fixed wing aircraft flies, VgZg, pitching angle theta, roll angle Φ and course angle Ψ;
104~in earth axes, three-dimensional ground velocity subtracts three-dimensional air speed and obtains ascending air.
2. the ascending air measurement method according to claim 1 for weather modification aircraft, it is characterised in that: institute It states in step 102, transition matrix of the body coordinate system Sb to earth axes Sg are as follows:
VtSg=SθψФ× VtSb, wherein
VtYg=VtX*cos θ * sin ψ+VtY* (sin θ * sin ψ * sin φ+cos ψ * cos φ)+VtZ* (sin θ * sin ψ * cos φ-cosψ*sinφ)
VtZg=VtY*cos θ * sin φ+VtZ*cos θ * cos φ-VtX*sin θ;
VtX, VtY, VtZ are substituted into joint account in above-mentioned three formula to obtain:
VtXg=Vt* (cos α * cos β * cos θ * cos ψ+sin β * sin θ * cos ψ * sin φ-sin β * sin ψ * cos φ+sin α * cosβ*sinθ*cosψ*cosφ+sinα*cosβ*sinψ*sinφ)
VtYg=Vt* (cos α * cos β * cos θ * sin ψ+sin β * sin θ * sin ψ * sin φ+sin β * cos ψ * cos φ+sin α * cosβ*sinθ*sinψ*cosφ-sinα*cosβ*cosψ*sinφ)
3. the ascending air measurement method according to claim 2 for weather modification aircraft, it is characterised in that: institute It states in step 104, three-dimensional ground velocity and three-dimensional air speed vector subtraction in earth axes is obtained into three-dimensional velocity, relative to ground Coordinate system, i.e.,
VwXg=VgXg-VtXg
VwYg=VgYg-VtYg
VwZg=VgZg-VtZg
VwXg=VgXg-Vt (cos α * cos β * cos θ * cos ψ+sin β * sin θ * cos ψ * sin φ-sin β * sin ψ * cos φ+ sinα*cosβ*sinθ*cosψ*cosφ+sinα*cosβ*sinψ*sinφ)
VwYg=VgYg-Vt (cos α * cos β * cos θ * sin ψ+sin β * sin θ * sin ψ * sin φ+sin β * cos ψ * cos φ+ sinα*cosβ*sinθ*sinψ*cosφ-sinα*cosβ*cosψ*sinφ)
VwZg=VgZg-Vt (sin β * cos θ * sin φ+sin α * cos β * cos θ * cos φ-cos α * cos β * sin θ)
Wherein: VwXg is the east orientation wind speed that north orientation wind speed, the VwYg relative to earth axes are relative to earth axes, VwZg is the ascending air relative to earth axes.
CN201711280576.8A 2017-12-06 2017-12-06 A kind of ascending air measurement method for weather modification aircraft Active CN108195558B (en)

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CN109710961B (en) * 2018-10-26 2023-01-13 中国飞行试验研究院 High-altitude unmanned aerial vehicle limit rising data processing method based on GPS data
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CN111222082B (en) * 2020-01-15 2022-01-04 南京航空航天大学 Method for identifying position and speed of ascending airflow suitable for unmanned aerial vehicle
CN115438293B (en) * 2022-09-09 2023-06-06 青海省人工影响天气办公室 Ground smoke furnace artificial precipitation operation condition identification method

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