CN116222550A - Underwater polarized sun calculation method with depth adaptability - Google Patents

Underwater polarized sun calculation method with depth adaptability Download PDF

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CN116222550A
CN116222550A CN202310504775.1A CN202310504775A CN116222550A CN 116222550 A CN116222550 A CN 116222550A CN 202310504775 A CN202310504775 A CN 202310504775A CN 116222550 A CN116222550 A CN 116222550A
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polarized light
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CN116222550B (en
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郭雷
赵谦
杨健
胡鹏伟
张腾
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Beihang University
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    • GPHYSICS
    • G01MEASURING; TESTING
    • G01CMEASURING DISTANCES, LEVELS OR BEARINGS; SURVEYING; NAVIGATION; GYROSCOPIC INSTRUMENTS; PHOTOGRAMMETRY OR VIDEOGRAMMETRY
    • G01C21/00Navigation; Navigational instruments not provided for in groups G01C1/00 - G01C19/00
    • G01C21/02Navigation; Navigational instruments not provided for in groups G01C1/00 - G01C19/00 by astronomical means
    • G01C21/025Navigation; Navigational instruments not provided for in groups G01C1/00 - G01C19/00 by astronomical means with the use of startrackers
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01CMEASURING DISTANCES, LEVELS OR BEARINGS; SURVEYING; NAVIGATION; GYROSCOPIC INSTRUMENTS; PHOTOGRAMMETRY OR VIDEOGRAMMETRY
    • G01C21/00Navigation; Navigational instruments not provided for in groups G01C1/00 - G01C19/00
    • G01C21/20Instruments for performing navigational calculations
    • G01C21/203Specially adapted for sailing ships
    • GPHYSICS
    • G06COMPUTING; CALCULATING OR COUNTING
    • G06TIMAGE DATA PROCESSING OR GENERATION, IN GENERAL
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    • G06T2207/00Indexing scheme for image analysis or image enhancement
    • G06T2207/20Special algorithmic details
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    • G06T2207/20061Hough transform
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Abstract

The invention relates to an underwater polarized sun calculation method with depth adaptability. Firstly, polarized light field information is acquired by using an image type underwater polarization sensor, and a reference sun position is obtained by carrying out Hough transformation on the polarized light intensity information; then, based on the Rayleigh scattering theory, the refraction law and the Fresnel theorem, obtaining the polarization azimuth angle of the atmospheric polarized light under water; further analyzing the polarization azimuth angle of the underwater scattered light by utilizing the Rayleigh scattering theory, and calculating the relative proportion parameter of the atmospheric polarized light and the underwater scattered light; and finally, establishing an equation set according to the relative proportion parameters, and calculating the sun position by using the underwater polarization information. The invention establishes an underwater polarized solar computing method with depth adaptability, which can be used for computing solar azimuth angle and altitude angle, realizes the depth self-adaption through the relative proportion parameters which are continuously updated, improves the environmental adaptability of the underwater polarized navigation method, and meets the autonomous navigation positioning requirement of the underwater vehicle.

Description

Underwater polarized sun calculation method with depth adaptability
Technical Field
The invention belongs to the field of underwater polarized light navigation, and particularly relates to an underwater polarized sun calculation method with depth adaptability.
Background
The underwater submarine has the advantages of strong autonomy, good concealment, high efficiency-cost ratio and the like, is a sharp tool for developing ocean resources, and plays an important role in the fields of underwater exploration, emergency rescue, reconnaissance monitoring and the like. The navigation system is an 'eye' and an 'ear' of the underwater vehicle, and is a precondition for the normal task execution and safe return. However, the characteristics of electromagnetic signal rejection, no mark point and less available navigation information exist in the underwater environment, so that the application of the traditional navigation methods such as satellite, inertia, vision and the like is limited. The mantis shrimp, rainbow trout and other organisms can navigate by utilizing underwater polarized light, so that a new thought is provided for solving the problem of underwater navigation, and a polarized navigation technology is formed.
The key point of the polarization navigation technology is that the sun position is inverted through polarization information, although a polarization sun calculation method has been primarily developed in an atmospheric environment, for example, a solar azimuth acquisition method based on an atmospheric polarization mode is proposed in chinese patent No. ZL201710027484.2, a solar vector calculation method based on an imitation compound eye multichannel polarization sensor is proposed in chinese patent application No. CN201810592616.0, but the method is only applicable to an atmospheric environment, and a plurality of problems still exist in an underwater environment to be solved: firstly, various light sources are mixed, and the underwater polarized light field has not only the part of the atmospheric polarized light entering the water, but also the underwater scattered light formed by the direct sunlight scattered by the water body, and the polarized light of different sources are mutually mixed and fused; and secondly, coupling various optical effects, wherein polarized light is subjected to the mixed influence of various optical effects such as atmospheric Rayleigh scattering, water surface refraction, underwater scattering and the like in the process of generating and transmitting. All of the above factors limit the environmental flexibility of the underwater polarized solar computing method.
In the aspect of underwater sun inversion, chinese patent ZL201911252040.4 proposes a solar vector calculation method based on an underwater polarization distribution mode, and the influence of water surface refraction on a polarization azimuth angle is considered; the Chinese patent ZL202011307244.6 proposes a solar altitude calculating method based on underwater refraction and scattering coupling polarization degree, considers the influence of water surface refraction and underwater scattering on atmospheric polarized light, and realizes the calculation of a solar altitude angle by utilizing the polarization degree.
However, the patent only considers the influence of the water environment on the refraction of the atmospheric polarized light, and does not consider the influence of the scattering of the direct sunlight under water on the polarized light field; and the model parameters are fixed, so that the self-adaptive adjustment of the polarization navigation model along with the water depth cannot be realized.
Disclosure of Invention
Aiming at the problem of poor environmental adaptability of the underwater polarized navigation method, various polarized light sources such as atmospheric polarized light, underwater scattered light and various optical effects such as atmospheric scattering, water surface refraction, underwater scattering and the like are considered, and relative proportion parameters capable of being adaptively adjusted along with depth are set.
According to the invention, polarized light field information is acquired by using an image type underwater polarization sensor, a reference sun position is obtained by carrying out Hough transformation on a polarized light intensity image, evaluation parameters are set, the relative proportion parameters of atmospheric polarized light polarization azimuth angle, underwater scattered light polarization azimuth angle and atmospheric polarized light and underwater scattered light entering the image type underwater polarization sensor are respectively inverted based on physical principles such as Rayleigh scattering theory, refraction law, fresnel theorem and the like, the sun position is inverted by using the polarized information based on the relative proportion parameters, and the depth self-adaptive adjustment of a polarized navigation model is realized by using the adjustable relative proportion parameters. In practical cases, the underwater polarized light field information not only comprises the part of atmospheric polarized light entering the water through refraction, but also comprises underwater scattered light formed by direct sunlight scattered by water; the problems of mixing various light sources and coupling various optical effects exist under the influence of atmospheric scattering and water surface refraction and underwater scattering. According to the method, by setting the relative proportion parameters of the atmospheric polarized light and the underwater scattered light and considering various optical sources and optical effects, the depth self-adaptive adjustment of the polarized navigation model can be realized, and the environmental adaptability of the polarized navigation method in an underwater complex environment is improved.
In order to achieve the above purpose, the invention adopts the following technical scheme:
an underwater polarized sun calculating method with depth adaptability comprises the following implementation steps:
step (1), acquiring polarized light field information through an image type underwater polarization sensor, processing a polarized light intensity image by using Hough transformation, extracting a highlight region in the polarized light intensity image, and setting evaluation parameters
Figure SMS_1
And threshold->
Figure SMS_2
When (when)
Figure SMS_3
When the central position of the highlight area is taken as the reference sun position, the zenith angle of the reference sun is obtained according to the geometric model of the image type underwater polarization sensor>
Figure SMS_4
Reference sun azimuth->
Figure SMS_5
Step (2) of obtaining the reference solar zenith angle by using the step (1)
Figure SMS_6
Reference sun azimuth/>
Figure SMS_7
Based on Rayleigh scattering theory, refraction law and Fresnel law, calculating the polarization azimuth angle of atmospheric polarized light incident to the image underwater polarization sensor>
Figure SMS_8
Step (3) of obtaining the reference solar zenith angle by using the step (1)
Figure SMS_9
Reference sun azimuth->
Figure SMS_10
Based on Rayleigh scattering theory, calculating the polarization azimuth angle of underwater scattered light incident to the image type underwater polarization sensor>
Figure SMS_11
And the relative proportion parameter of the atmospheric scattered light and the underwater scattered light in the polarized light field is obtained>
Figure SMS_12
Wherein the relative proportion parameter->
Figure SMS_13
The method can correct and update in real time through the step (1), the step (2) and the step (3) under different depths, so that the depth adaptability adjustment of the polarized light field model is realized;
step (4) of utilizing the relative proportion parameter of the atmospheric polarized light and the underwater scattered light in the underwater polarized light field obtained in the step (3)
Figure SMS_16
In the polarized image measured by the image type underwater polarization sensor, the +.>
Figure SMS_20
Each pixel point has the observation zenith angle and azimuth angle of +.>
Figure SMS_21
,/>
Figure SMS_15
The measured azimuth angle of polarization under water is +.>
Figure SMS_17
, wherein
Figure SMS_18
Calculating a solar azimuth angle and a solar elevation angle; repeating the step (1), when ∈>
Figure SMS_19
When step (2), step (3) and step (4) are performed, when +.>
Figure SMS_14
And (3) directly executing the step (4). />
Further, the step (1) uses the image type underwater polarization sensor to obtain the zenith angle of the reference sun
Figure SMS_22
Reference sun azimuth->
Figure SMS_23
The specific requirements of (2) are as follows:
polarized light field information is acquired through an image type underwater polarization sensor, polarized light intensity images are processed through Hough transformation, highlight areas in the polarized light intensity images are extracted, and evaluation parameters are set
Figure SMS_24
Figure SMS_25
wherein ,
Figure SMS_26
for the area of the highlight region in the polarized light intensity image, is->
Figure SMS_27
Is the highlighting area perimeter.
Because polarized light intensity images are easily interfered by factors such as cloud layer shielding, wave refraction, lens distortion and the like, evaluation parameters are required to be set to distinguish the position accuracy of the sun extracted from polarized light intensity, and when
Figure SMS_28
When the polarized light intensity image is in a perfect circle, the sun position precision is highest; setting an evaluation parameter threshold +.>
Figure SMS_29
When->
Figure SMS_30
When the central position of the highlight area is taken as the reference sun position, the zenith angle of the reference sun is obtained according to the geometric model of the image type underwater polarization sensor>
Figure SMS_31
Reference sun azimuth->
Figure SMS_32
Further, the step (2) calculates the polarization azimuth angle of the atmospheric polarized light incident to the image type underwater polarization sensor based on the Rayleigh scattering theory, the refraction law and the Fresnel law
Figure SMS_33
The method is concretely realized as follows:
according to refraction law, observing solar zenith angle on water
Figure SMS_34
And the zenith angle of the reference sun->
Figure SMS_35
The relation of (2) is:
Figure SMS_36
wherein ,
Figure SMS_37
refractive index of water body>
Figure SMS_38
Is the refractive index of air.
The zenith angle in the image-taking type underwater polarization sensor is
Figure SMS_39
Azimuth angle is->
Figure SMS_40
According to Rayleigh scattering theory, the azimuth angle of polarization of atmospheric polarized light before being refracted by water surface +.>
Figure SMS_41
The method comprises the following steps:
Figure SMS_42
wherein ,
Figure SMS_43
for the angle of incidence of the observation direction in the atmosphere, +.>
Figure SMS_44
According to Fresnel's law, the polarization azimuth angle of atmospheric polarized light incident to the image type underwater polarization sensor after being refracted by the water surface can be obtained
Figure SMS_45
The method comprises the following steps:
Figure SMS_46
namely:
Figure SMS_47
wherein ,
Figure SMS_48
representation->
Figure SMS_49
And->
Figure SMS_50
A functional relationship between them.
Further, the step (3) calculates the azimuth angle of polarization of the underwater scattered light incident to the image-type underwater polarization sensor based on the Rayleigh scattering theory
Figure SMS_51
And the relative proportion parameter of the atmospheric scattered light and the underwater scattered light in the polarized light field is obtained>
Figure SMS_52
The method is concretely realized as follows:
the zenith angle in the image-taking type underwater polarization sensor is
Figure SMS_53
Azimuth angle is->
Figure SMS_54
According to Rayleigh scattering theory, the polarization azimuth angle of the underwater scattered light formed by the underwater scattering of the direct solar light is as follows:
Figure SMS_55
wherein ,
Figure SMS_56
representation->
Figure SMS_57
And->
Figure SMS_58
A functional relationship between them.
The polarization vector formed by superposition of atmospheric polarized light and underwater scattered light
Figure SMS_59
The method comprises the following steps:
Figure SMS_60
,/>
wherein ,
Figure SMS_61
polarization vector of light for atmospheric polarization,>
Figure SMS_62
is the polarization vector of the light of the underwater scattered light,
Figure SMS_63
the underwater polarization azimuth angle formed by superposition of the atmospheric polarized light and the underwater scattered light can be measured by an image type underwater polarization sensor, and can be obtained by the following steps:
Figure SMS_64
wherein the relative proportion parameter
Figure SMS_65
The method can correct and update in real time through the step (1), the step (2) and the step (3) under different depths, so that the depth adaptability adjustment of the polarized light field model is realized;
further, the step (4) uses the relative proportion parameter of the atmospheric polarized light and the underwater scattered light in the underwater polarized light field obtained in the step (3)
Figure SMS_66
In the polarized image measured by the image type underwater polarization sensor, the +.>
Figure SMS_67
Each pixel point, and the zenith angle and square of each pixel point are observedThe azimuth angles are respectively->
Figure SMS_68
,/>
Figure SMS_69
The measured underwater polarization azimuth angle is
Figure SMS_70
, wherein />
Figure SMS_71
The solar azimuth angle and the solar altitude angle are calculated, and the specific implementation is as follows:
according to the underwater polarization azimuth angle formed by superposition of the atmospheric polarized light and the underwater scattered light in the step (3)
Figure SMS_72
Is +.>
Figure SMS_73
Height angle->
Figure SMS_74
The relation between them can be found as follows:
Figure SMS_75
by using a nonlinear least square method, the optimal solution of the equation set can be obtained
Figure SMS_76
,/>
Figure SMS_77
The method comprises the steps of carrying out a first treatment on the surface of the Repeating the step (1), when ∈>
Figure SMS_78
When step (2), step (3) and step (4) are performed, when +.>
Figure SMS_79
When it is time, directly execute step (4)。
Compared with the prior art, the invention has the following advantages:
the existing underwater polarization navigation method has the defects that the considered light source and optical effect are single, and the underwater polarization navigation method is difficult to adapt to complex and changeable environments. The invention considers various polarized light sources such as atmospheric polarized light, underwater scattered light and various optical effects such as atmospheric scattering, water surface refraction, underwater scattering and the like, sets relative proportion parameters capable of being adaptively adjusted along with depth, and improves the environmental adaptability of the underwater polarized navigation method.
Drawings
FIG. 1 is a flow chart of an underwater polarized sun calculation method with depth adaptability of the present invention;
FIG. 2 is a schematic illustration of the propagation process of atmospheric polarized light and underwater scattered light;
fig. 3 is a schematic diagram of the superposition of polarized light.
Detailed Description
The technical solutions of the embodiments of the present invention will be clearly and completely described below with reference to the accompanying drawings in the embodiments of the present invention, and it is apparent that the described embodiments are only some embodiments of the present invention, but not all embodiments, and all other embodiments obtained by those skilled in the art without the inventive effort based on the embodiments of the present invention are within the scope of protection of the present invention.
According to one embodiment of the present invention, as shown in fig. 1, the method for calculating the underwater polarized sun with depth adaptability specifically comprises the following steps:
step (1), acquiring polarized light field information through an image type underwater polarization sensor, processing a polarized light intensity image by using Hough transformation, extracting a highlight region in the polarized light intensity image, and setting evaluation parameters
Figure SMS_80
Figure SMS_81
wherein ,
Figure SMS_82
for the area of the highlight region in the polarized light intensity image,/->
Figure SMS_83
Is the highlighting area perimeter.
Because polarized light intensity images are easily interfered by factors such as cloud layer shielding, wave refraction, lens distortion and the like, evaluation parameters are required to be set to distinguish the position accuracy of the sun extracted from polarized light intensity, and when
Figure SMS_84
When the polarized light intensity image is in a perfect circle, the sun position precision is highest; setting an evaluation parameter threshold +.>
Figure SMS_85
When->
Figure SMS_86
When the central position of the highlight area is taken as the reference sun position, the zenith angle of the reference sun is obtained according to the geometric model of the image type underwater polarization sensor>
Figure SMS_87
Reference sun azimuth->
Figure SMS_88
Step (2) of obtaining the reference solar zenith angle by using the step (1)
Figure SMS_89
Reference sun azimuth->
Figure SMS_90
Based on Rayleigh scattering theory, refraction law and Fresnel law, calculating the polarization azimuth angle of atmospheric polarized light incident to the image underwater polarization sensor>
Figure SMS_91
The light propagation diagram is shown in figure 2, and the zenith angle of the sun is observed on water according to the law of refraction
Figure SMS_92
And the zenith angle of the reference sun->
Figure SMS_93
The relation of (2) is:
Figure SMS_94
,/>
wherein ,
Figure SMS_95
refractive index of water body>
Figure SMS_96
Is the refractive index of air.
The method can be characterized by comprising the following steps:
Figure SMS_97
the zenith angle in the image-taking type underwater polarization sensor is
Figure SMS_98
Azimuth angle is->
Figure SMS_99
According to Rayleigh scattering theory, the azimuth angle of polarization of atmospheric polarized light before being refracted by water surface +.>
Figure SMS_100
The method comprises the following steps:
Figure SMS_101
wherein ,
Figure SMS_102
in the atmosphere for the direction of observationIncident angle of>
Figure SMS_103
Polarized light amplitude parallel to the refractive surface before and after refraction according to fresnel's law
Figure SMS_104
The following relationship exists:
Figure SMS_105
amplitude of polarized light perpendicular to the plane of refraction
Figure SMS_106
The following relationship exists:
Figure SMS_107
definition of polarization azimuth angle:
Figure SMS_108
,/>
Figure SMS_109
the change of the polarization azimuth before and after the refraction on the water surface can be obtained as follows:
Figure SMS_110
Figure SMS_111
wherein ,
Figure SMS_112
the atmospheric polarized light is incident to the image type underwater polarization sensor after being refracted by the water surface. The simultaneous preparation method comprises the following steps:
Figure SMS_113
wherein ,
Figure SMS_114
representation->
Figure SMS_115
And->
Figure SMS_116
A functional relationship between them.
Step (3) of obtaining the reference solar zenith angle by using the step (1)
Figure SMS_117
Reference sun azimuth->
Figure SMS_118
Based on Rayleigh scattering theory, calculating the polarization azimuth angle of underwater scattered light incident to the image type underwater polarization sensor>
Figure SMS_119
And the relative proportion parameter of the atmospheric scattered light and the underwater scattered light in the polarized light field is obtained>
Figure SMS_120
The zenith angle in the image-taking type underwater polarization sensor is
Figure SMS_121
Azimuth angle is->
Figure SMS_122
According to Rayleigh scattering theory, the polarization azimuth angle of the underwater scattered light formed by the underwater scattering of the direct solar light is as follows:
Figure SMS_123
wherein ,
Figure SMS_124
representation->
Figure SMS_125
And->
Figure SMS_126
A functional relationship between them.
A schematic diagram of superposition of atmospheric polarized light and underwater scattered light under water is shown in FIG. 3, wherein the polarization vector of the atmospheric polarized light is
Figure SMS_127
The polarization vector of the underwater scattered light is +.>
Figure SMS_128
The definition is as follows:
Figure SMS_129
Figure SMS_130
,/>
the polarization vector formed by superposition of atmospheric polarized light and underwater scattered light
Figure SMS_131
The method comprises the following steps:
Figure SMS_132
wherein ,
Figure SMS_133
the underwater polarization azimuth angle formed by superposition of the atmospheric polarized light and the underwater scattered light can be measured by an image type underwater polarization sensor, and can be obtained by the following steps:
Figure SMS_134
Figure SMS_135
wherein the relative proportion parameter
Figure SMS_136
And (3) carrying out real-time correction and updating through the step (1), the step (2) and the step (3) under different depths, so as to realize the depth adaptive adjustment of the polarized light field model.
Step (4) of utilizing the relative proportion parameter of the atmospheric polarized light and the underwater scattered light in the underwater polarized light field obtained in the step (3)
Figure SMS_137
In the polarized image measured by the image type underwater polarization sensor, the +.>
Figure SMS_138
Each pixel point has the observation zenith angle and azimuth angle of +.>
Figure SMS_139
,/>
Figure SMS_140
The measured polarization azimuth angle is +.>
Figure SMS_141
, wherein
Figure SMS_142
And calculating the solar azimuth angle and the solar altitude angle.
According to the underwater polarization azimuth angle formed by superposition of the atmospheric polarized light and the underwater scattered light in the step (3)
Figure SMS_143
Is +.>
Figure SMS_144
Height angle->
Figure SMS_145
The relation between them can be obtained:
Figure SMS_146
the following set of equations can be obtained:
Figure SMS_147
by using a nonlinear least square method, the optimal solution of the equation set can be obtained
Figure SMS_148
,/>
Figure SMS_149
The method comprises the steps of carrying out a first treatment on the surface of the Repeating the step (1), when ∈>
Figure SMS_150
When step (2), step (3) and step (4) are performed, when +.>
Figure SMS_151
And (3) directly executing the step (4).
While the foregoing has been described in relation to illustrative embodiments thereof, so as to facilitate the understanding of the present invention by those skilled in the art, it should be understood that the present invention is not limited to the scope of the embodiments, but is to be construed as limited to the spirit and scope of the invention as defined and defined by the appended claims, as long as various changes are apparent to those skilled in the art, all within the scope of which the invention is defined by the appended claims.

Claims (5)

1. The underwater polarized sun calculating method with the depth adaptability is characterized by comprising the following steps of:
step (1), acquiring polarized light field information through an image type underwater polarization sensor, processing a polarized light intensity image by using Hough transformation, extracting a highlight region in the polarized light intensity image, and setting evaluation parameters
Figure QLYQS_1
And threshold->
Figure QLYQS_2
When->
Figure QLYQS_3
When the central position of the highlight area is taken as the reference sun position, the zenith angle of the reference sun is obtained according to the geometric model of the image type underwater polarization sensor>
Figure QLYQS_4
Reference sun azimuth->
Figure QLYQS_5
Step (2) of obtaining the reference solar zenith angle by using the step (1)
Figure QLYQS_6
Reference sun azimuth->
Figure QLYQS_7
Based on Rayleigh scattering theory, refraction law and Fresnel law, calculating the polarization azimuth angle of atmospheric scattered light incident to the image underwater polarization sensor>
Figure QLYQS_8
Step (3) of obtaining the reference solar zenith angle by using the step (1)
Figure QLYQS_9
Reference sun azimuth->
Figure QLYQS_10
Based on Rayleigh scattering theory, calculating the polarization azimuth angle of underwater scattered light incident to the image type underwater polarization sensor>
Figure QLYQS_11
And the relative proportion parameter of the atmospheric scattered light and the underwater scattered light in the polarized light field is obtained>
Figure QLYQS_12
Wherein the relative proportion parameter->
Figure QLYQS_13
Carrying out real-time correction and updating through the step (1), the step (2) and the step (3) under different depths, and realizing the depth adaptability adjustment of the polarized light field model;
step (4) of utilizing the relative proportion parameter of the atmospheric polarized light and the underwater scattered light in the underwater polarized light field obtained in the step (3)
Figure QLYQS_16
In the polarized image measured by the image type underwater polarization sensor, the +.>
Figure QLYQS_18
Each pixel point has the observation zenith angle and azimuth angle of +.>
Figure QLYQS_20
,/>
Figure QLYQS_15
The measured azimuth angle of polarization under water is +.>
Figure QLYQS_17
, wherein />
Figure QLYQS_19
Calculating a solar azimuth angle and a solar elevation angle; repeating the step (1), when ∈>
Figure QLYQS_21
When step (2), step (3) and step (4) are performed, when +.>
Figure QLYQS_14
And (3) directly executing the step (4).
2. The method for calculating the underwater polarized sun with depth adaptability according to claim 1, wherein the method comprises the following steps:
in the step (1), the evaluation parameter
Figure QLYQS_22
The method comprises the following steps:
Figure QLYQS_23
wherein ,
Figure QLYQS_24
for the area of the highlight region in the polarized light intensity image, is->
Figure QLYQS_25
Is the highlighting area perimeter.
3. The method for calculating the underwater polarized sun with depth adaptability according to claim 2, wherein the method comprises the following steps:
the specific implementation of the step (2) is as follows:
according to refraction law, observing solar zenith angle on water
Figure QLYQS_26
And the zenith angle of the reference sun->
Figure QLYQS_27
The relation of (2) is:
Figure QLYQS_28
wherein ,
Figure QLYQS_29
refractive index of water body>
Figure QLYQS_30
Is the refractive index of air;
the zenith angle in the image-taking type underwater polarization sensor is
Figure QLYQS_31
Azimuth angle is->
Figure QLYQS_32
According to Rayleigh scattering theory, the azimuth angle of polarization of atmospheric polarized light before being refracted by water surface +.>
Figure QLYQS_33
The method comprises the following steps:
Figure QLYQS_34
wherein ,
Figure QLYQS_35
for the angle of incidence of the observation direction in the atmosphere, +.>
Figure QLYQS_36
According to Fresnel's law, the polarization azimuth angle of atmospheric polarized light incident to the image type underwater polarization sensor after being refracted by the water surface is obtained
Figure QLYQS_37
The method comprises the following steps:
Figure QLYQS_38
namely:
Figure QLYQS_39
wherein ,
Figure QLYQS_40
representation->
Figure QLYQS_41
And->
Figure QLYQS_42
A functional relationship between them.
4. A method for computing underwater polarized sun with depth adaptability according to claim 3, wherein:
the specific implementation of the step (3) is as follows:
the zenith angle in the image-taking type underwater polarization sensor is
Figure QLYQS_43
Azimuth angle is->
Figure QLYQS_44
According to Rayleigh scattering theory, the polarization azimuth angle of the underwater scattered light formed by the underwater scattering of the direct solar light is as follows:
Figure QLYQS_45
wherein ,
Figure QLYQS_46
representation->
Figure QLYQS_47
And->
Figure QLYQS_48
A functional relationship between;
then the atmospheric polarized light and the underwater scattered light are overlapped to formPolarization vector
Figure QLYQS_49
The method comprises the following steps:
Figure QLYQS_50
wherein ,
Figure QLYQS_51
polarization vector of light for atmospheric polarization,>
Figure QLYQS_52
is the polarization vector of the underwater scattered light, ">
Figure QLYQS_53
The underwater polarization azimuth angle formed by superposition of the atmospheric polarized light and the underwater scattered light is measured by an image type underwater polarization sensor, and is obtained by the following steps:
Figure QLYQS_54
5. the method for calculating the underwater polarized sun with depth adaptability according to claim 4, wherein the method comprises the following steps: the specific implementation of the step (4) is as follows:
according to the underwater polarization azimuth angle formed by superposition of the atmospheric polarized light and the underwater scattered light in the step (3)
Figure QLYQS_55
Is +.>
Figure QLYQS_56
Height angle->
Figure QLYQS_57
The relation between the two is obtained as follows: />
Figure QLYQS_58
Using nonlinear least square method to obtain solar azimuth angle in the above equation set
Figure QLYQS_59
Height angle->
Figure QLYQS_60
Is a solution to the optimization of (3). />
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