CN109557333B - Method for inverting surface ocean current based on navigation buoy data - Google Patents

Method for inverting surface ocean current based on navigation buoy data Download PDF

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CN109557333B
CN109557333B CN201811209727.5A CN201811209727A CN109557333B CN 109557333 B CN109557333 B CN 109557333B CN 201811209727 A CN201811209727 A CN 201811209727A CN 109557333 B CN109557333 B CN 109557333B
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ocean current
parameters
ocean
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CN109557333A (en
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张安民
宁一伟
张豪
欧阳知雨
刘禹
刘帅
刘荣霞
侯泽北
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Tianjin University
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    • GPHYSICS
    • G01MEASURING; TESTING
    • G01PMEASURING LINEAR OR ANGULAR SPEED, ACCELERATION, DECELERATION, OR SHOCK; INDICATING PRESENCE, ABSENCE, OR DIRECTION, OF MOVEMENT
    • G01P5/00Measuring speed of fluids, e.g. of air stream; Measuring speed of bodies relative to fluids, e.g. of ship, of aircraft
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01PMEASURING LINEAR OR ANGULAR SPEED, ACCELERATION, DECELERATION, OR SHOCK; INDICATING PRESENCE, ABSENCE, OR DIRECTION, OF MOVEMENT
    • G01P13/00Indicating or recording presence, absence, or direction, of movement
    • G01P13/02Indicating direction only, e.g. by weather vane
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01SRADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
    • G01S19/00Satellite radio beacon positioning systems; Determining position, velocity or attitude using signals transmitted by such systems
    • G01S19/01Satellite radio beacon positioning systems transmitting time-stamped messages, e.g. GPS [Global Positioning System], GLONASS [Global Orbiting Navigation Satellite System] or GALILEO
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Abstract

The invention discloses a method for inverting surface ocean current based on navigation buoy data, which comprises the following steps: step one, arranging a navigation buoy in an observation sea area, and carrying a sea current data measuring system; collecting buoy position data according to an ocean current data measuring system, and correcting to obtain motion parameters of the buoy; thirdly, collecting buoy position data according to the ocean current data measurement system to establish a buoy stress model; analyzing the parameters of the ocean current resistance of the buoy in the buoy stress model through an ocean current inversion algorithm; calculating the movement parameters of the buoy in the step two and the ocean current resistance parameters of the buoy in the step three to obtain initial values of the flow velocity and the direction of the ocean current in the observation sea area; and step six, correcting the initial values of the flow velocity and the direction of the ocean current obtained in the step five to obtain a final ocean current flow velocity value. The invention realizes accurate measurement of the ocean current in a specific sea area through the navigation buoy, and overcomes the defects of the traditional measurement method.

Description

一种基于导航浮标数据反演表层海流的方法A method for inversion of surface currents based on navigation buoy data

技术领域technical field

本发明涉及海流观测技术领域,特别是涉及一种基于导航浮标数据反演表层海流的方法。The invention relates to the technical field of ocean current observation, in particular to a method for inverting surface ocean current based on navigation buoy data.

背景技术Background technique

海流对海洋中多种物理、化学、生物和地质作用和输送盐度、叶绿素和海洋热量过程,以及海洋上空的气候和天气的形成及变化,都有重要的影响和制约的作用,同时对于人类活动来说,海流对海洋开发、航海、军事、港口建设、海上捕鱼和防御海洋气象灾害,都具有重大的社会和经济意义。传统海流流速测量的方法主要是通过在海中固定海流计进行测量或者利用高度卫星数据进行反演,相比传统的测量方法,利用导航浮标反演海流既可减少购买仪器的成本也可避免海洋生物对仪器的表面附着造成的误差,并且能够实现定点测量海流。Ocean currents have important influences and constraints on various physical, chemical, biological and geological processes in the ocean and the processes of transporting salinity, chlorophyll and ocean heat, as well as the formation and changes of climate and weather over the ocean. In terms of activities, ocean currents are of great social and economic significance to ocean development, navigation, military, port construction, marine fishing and defense against marine meteorological disasters. The traditional method of current flow measurement is mainly through the measurement of fixed current meters in the sea or the use of altitude satellite data for inversion. Compared with traditional measurement methods, the use of navigation buoys to invert currents can not only reduce the cost of purchasing instruments, but also avoid marine life. The error caused by the surface attachment of the instrument, and can achieve fixed-point measurement of ocean currents.

发明内容SUMMARY OF THE INVENTION

本发明的目的是为了克服现有技术中的不足,提出了一种基于导航浮标数据反演表层海流的方法,具体技术方案如下:The purpose of the present invention is to overcome the deficiencies in the prior art, and propose a method for inverting surface currents based on navigation buoy data, the specific technical scheme is as follows:

一种基于导航浮标数据反演表层海流的方法,包括以下步骤:A method for retrieving surface ocean currents based on navigation buoy data, comprising the following steps:

步骤一、在观察海域布设导航浮标,搭载海流数据测量系统;Step 1. Set up navigation buoys in the observation sea area and carry an ocean current data measurement system;

步骤二、根据海流数据测量系统收集浮标位置值和风速值进行修正获得其运动参数;同时,根据海流数据测量系统收集浮标的质量、入水深度和锚链长度的实际参数;Step 2: Collecting the position value and wind speed value of the buoy according to the ocean current data measurement system and correcting to obtain its motion parameters; at the same time, collecting the actual parameters of the buoy's mass, water entry depth and anchor chain length according to the ocean current data measurement system;

步骤三、根据浮标运动参数和实际参数建立浮标受力模型;Step 3: Establish a buoy force model according to the buoy motion parameters and actual parameters;

步骤四、通过海流反演算法分析浮标受力模型中浮标受到海流阻力参数;Step 4: Analyze the resistance parameters of the buoy received by the current in the force model of the buoy through the current inversion algorithm;

步骤五、将步骤二中浮标运动参数和步骤三中浮标受海流阻力参数进行运算获得观察海域海流流速大小和方向的初始值;Step 5: Calculating the motion parameters of the buoy in Step 2 and the resistance parameters of the buoy by the ocean current in Step 3 to obtain the initial value of the magnitude and direction of the current flow velocity in the observed sea area;

步骤六、对步骤五中获得的海流流速大小和方向的初始值进行修正获得最终海流流速数值。Step 6: Correct the initial values of the magnitude and direction of the current flow velocity obtained in the fifth step to obtain the final value of the current flow velocity.

所述海流数据测量系统包括导航浮标、GPS定位仪、风速仪、数据传输单元和锚链;所述浮标上部连接有风速仪,所述浮标内部重心位置分别设置有GPS定位仪和数据传输单元,所述浮标下部连接有锚链。The ocean current data measurement system includes a navigation buoy, a GPS locator, an anemometer, a data transmission unit and an anchor chain; an anemometer is connected to the upper part of the buoy, and a GPS locator and a data transmission unit are respectively set at the position of the inner center of gravity of the buoy, An anchor chain is connected to the lower part of the buoy.

步骤四中所述海流反演算法包括如下步骤:The ocean current inversion algorithm described in step 4 includes the following steps:

3.1、根据浮标受力模型中浮标位置值计算获得浮标的运动加速度;3.1. Calculate the motion acceleration of the buoy according to the buoy position value in the buoy force model;

3.2、根据浮标受力模型中浮标风速值按照公式(1)计算获得浮标的受风应力;3.2. According to the buoy wind speed value in the buoy force model, calculate the wind stress of the buoy according to formula (1);

R2=kqAd (1)R2=kqA d (1)

3.3、根据浮标受力模型中浮标锚链长度按照公式(2)计算浮标所受锚链拉力;3.3. According to the length of the buoy anchor chain in the buoy force model, calculate the anchor chain tension of the buoy according to formula (2);

Figure GDA0003356947540000021
Figure GDA0003356947540000021

3.4、根据浮标受力模型中浮标的质量计算浮标所受的重力;3.4. Calculate the gravity of the buoy according to the mass of the buoy in the buoy force model;

3.5、根据浮标受力模型中浮标的入水深度值计算浮标所受浮力;3.5. Calculate the buoyancy of the buoy according to the buoy's immersion depth value in the buoy force model;

3.6、根据步骤3.1~3.5生成的浮标已知的参数通过牛顿第二运动定律建立的浮标运动N-S控制方程获得浮标所受海流阻力参数R1;3.6. According to the known parameters of the buoy generated in steps 3.1 to 3.5, obtain the current resistance parameter R1 of the buoy through the N-S control equation of the buoy motion established by Newton's second law of motion;

3.7、根据已知的海流阻力参数R1按照公式(3)获得海流流速V。3.7. According to the known current resistance parameter R1, obtain the current velocity V according to the formula (3).

R1=C(ρV^2)Ω/2 (3)R1=C(ρV^2)Ω/2 (3)

有益效果beneficial effect

与现有技术相比,本发明的技术方案所带来的有益效果是:Compared with the prior art, the beneficial effects brought by the technical solution of the present invention are:

1、本发明采用的通过在导航浮标中安装GPS定位仪结合浮标受力模型得到的反演海流的方法与目前传统的通过海流计和卫星数据反演方法获得海流流速相比,很显然该方法能够大大降低获取海流流速的成本,且相比于卫星反演该方法算法简单需要用到的数据量小。1. Compared with the current traditional inversion method of current flow rate obtained by the current traditional current meter and satellite data inversion method, the method of inversion of ocean current obtained by installing a GPS locator in the navigation buoy combined with the force model of the buoy, it is obvious that this method It can greatly reduce the cost of obtaining the current flow velocity, and compared with the satellite inversion method, the simple algorithm needs to use a small amount of data.

2、本发明能有效解决由于生物附着等问题出现的测量误差。除此之外,浮标的锚定点可根据测量需要随时进行变更,从而实现随时随地地测量特定海域的海流大小和方向。2. The present invention can effectively solve the measurement error due to biological adhesion and other problems. In addition, the anchor point of the buoy can be changed at any time according to the measurement needs, so that the current size and direction of a specific sea area can be measured anytime, anywhere.

附图说明Description of drawings

图1为导航浮标测量系统仪器安装示意图;Figure 1 is a schematic diagram of the installation of the instrument of the navigation buoy measurement system;

图2为该海流反演算法的解算流程图。Fig. 2 is the solution flow chart of the current inversion algorithm.

附图标记:Reference number:

1-浮标 2-GPS定位仪 3-数据传输设备 4-风速仪 5-锚链1-buoy 2-GPS locator 3-data transmission equipment 4-anemometer 5-anchor chain

具体实施方式Detailed ways

下面结合具体实施方式对本专利的技术方案作进一步详细地说明。The technical solution of the present patent will be described in further detail below in conjunction with specific embodiments.

本发明介绍了一种基于导航浮标数据反演表层海流的方法,是指通过在海洋浮标上搭载高精度GPS定位仪获取数据并通过数据分析海流流速大小和方向的方法,具体过程如下:The present invention introduces a method for retrieving surface ocean currents based on navigation buoy data, which refers to a method for acquiring data by carrying a high-precision GPS locator on an ocean buoy and analyzing the magnitude and direction of the current flow rate through the data. The specific process is as follows:

步骤一、在观察海域布设导航浮标1,并用锚链5将其固定在锚点。其中浮标中搭载高精度GPS定位仪2、风速仪4以及数据传输设备3。所有仪器都与浮标1进行刚性连接,安装方式与位置,如图1所示。GPS定位仪2用于采集浮标的位置参数,包括浮标的经度、纬度和高程等信息;风速仪4用于测量浮标在海上受到的风力大小;数据传输设备3用于将数据传输到岸基。Step 1. Lay the navigation buoy 1 in the observation sea area and fix it at the anchor point with the anchor chain 5. The buoy is equipped with a high-precision GPS locator 2 , an anemometer 4 and a data transmission device 3 . All instruments are rigidly connected to buoy 1, and the installation method and location are shown in Figure 1. The GPS locator 2 is used to collect the position parameters of the buoy, including information such as longitude, latitude and elevation of the buoy; the anemometer 4 is used to measure the wind force received by the buoy at sea; the data transmission device 3 is used to transmit the data to the shore base.

步骤二、收集浮标位置数据。通过GPS定位仪2获取浮标的经纬度信息并修正浮标姿态后得到浮标运动轨迹,据此获得浮标的运动参数,如加速度等;进而建立浮标受力模型,其建立方法如下:Step 2: Collect buoy position data. Obtain the longitude and latitude information of the buoy through the GPS locator 2 and correct the attitude of the buoy to obtain the buoy motion trajectory, thereby obtaining the motion parameters of the buoy, such as acceleration, etc.; and then establish a buoy force model, and its establishment method is as follows:

在水中的浮标,主要受海流阻力、风荷载等因素的作用,除此之外,还受到系留缆索的拉力。The buoy in the water is mainly affected by the current resistance, wind load and other factors, in addition to the pulling force of the mooring cable.

目前,计算海流摩擦阻力的公式较多,我国常用的是基于平板试验和理论分析所得到的阻力计算公式,其表达式为:At present, there are many formulas for calculating the frictional resistance of the ocean current. The commonly used resistance calculation formula in my country is based on the plate test and theoretical analysis. Its expression is:

R1=C(ρV^2)Ω/2 (3)R1=C(ρV^2)Ω/2 (3)

其中,V为海水流速。where V is the seawater velocity.

作用于浮标标体上的风压力可由《港口工程计算规范》所给出的计算公式确定:The wind pressure acting on the buoy body can be determined by the calculation formula given in the "Code for Calculation of Port Engineering":

R2=kqAd (1)R2=kqA d (1)

根据H.0.贝托和岩井聪对浮标受力的平衡分析,缆索呈悬链曲线形状,且其长度和受力可由以下计算式确定:According to the balance analysis of H.0. Beto and Satoshi Iwai on the force of the buoy, the cable is in the shape of a catenary curve, and its length and force can be determined by the following formulas:

Figure GDA0003356947540000031
Figure GDA0003356947540000031

通过对浮标的受力分析可知,浮标受到的水流力与海流流速有一定的相关关系,可以根据其他已知的受力通过浮标运动方程求出水流力,然后参照经验公式得到海流流速的大小并用实验数据进行修正。流速的方向也可由浮标的运动轨迹方向确定。方法的核心思想就是通过锚定浮标的运动轨迹反演海流的流速。Through the force analysis of the buoy, it can be seen that the water flow force on the buoy has a certain correlation with the current flow rate. The water flow force can be obtained through the buoy motion equation according to other known forces, and then the magnitude of the ocean current flow rate can be obtained by referring to the empirical formula and used The experimental data are corrected. The direction of the flow velocity can also be determined by the direction of the movement trajectory of the buoy. The core idea of the method is to invert the velocity of the ocean current through the motion trajectory of the anchored buoy.

步骤四、结合步骤二中标运动参数和步骤三中浮标受海流阻力参数推算海流的算法得出该海域海流流速大小和方向的初始值;如图2流程图所示,首先通过浮标采集到的数据和浮标姿态修正后得到浮标的运动轨迹,该运动轨迹是浮标所受到的所有力的体现;然后再结合受力分析得到的已知力有浮标受到的浮力、风力、和锚链约束力、重力、浮力,根据牛顿运动定律和运动N-S控制方程可以解算得出浮标受到的海流阻力,最后依据海流阻力与海流大小的经验公式R1=C(ρV^2)/2Ω得到海流流速。具体方法如下:Step 4: Combining the motion parameters of the winning bid in Step 2 and the algorithm of the current resistance parameter of the buoy in Step 3 to estimate the ocean current, the initial value of the current flow velocity and direction in the sea area is obtained; as shown in the flowchart in Figure 2, the data collected by the buoy first After correcting the attitude of the buoy and the buoy, the movement trajectory of the buoy is obtained, which is the embodiment of all the forces on the buoy; and then combined with the force analysis, the known forces obtained include the buoyancy, wind, and anchor chain binding force, gravity, For buoyancy, the current resistance to the buoy can be calculated according to Newton's law of motion and the N-S control equation of motion. Finally, the current flow rate can be obtained according to the empirical formula R1=C(ρV^2)/2Ω of the current resistance and the size of the current. The specific method is as follows:

a.用GPS定位仪获得浮标的位置值,用风速仪获得浮标所受风速值。根据实际测量获得浮标的质量、入水深度、锚链长度等数值。a. Use the GPS locator to obtain the position value of the buoy, and use the anemometer to obtain the wind speed value of the buoy. According to the actual measurement, the quality of the buoy, the depth of water entry, and the length of the anchor chain are obtained.

b.用位置值求得浮标的运动加速度,用风速值根据风压力公式R2=kqAd求得浮标所受风应力,用浮标的锚链长度根据H.0.贝托和岩井聪给出的锚链拉力公式

Figure GDA0003356947540000041
计算浮标所受锚链拉力,用浮标的质量计算浮标所受的重力,用入水深度计算浮标所受浮力;b. Use the position value to obtain the motion acceleration of the buoy, use the wind speed value to obtain the wind stress on the buoy according to the wind pressure formula R2=kqAd, and use the anchor chain length of the buoy according to the anchor given by H.0. Beto and Iwai Satoshi chain tension formula
Figure GDA0003356947540000041
Calculate the anchor chain tension of the buoy, calculate the gravity of the buoy with the mass of the buoy, and calculate the buoyancy of the buoy with the depth of water entry;

c.根据牛顿第二运动定律建立浮标运动N-S控制方程,根据已知的加速度、风应力、锚链拉力、重力、浮力通过求解N-S控制方程,求得浮标所受水流拉力R1。c. Establish the N-S control equation of buoy motion according to Newton's second law of motion, and obtain the current pulling force R1 on the buoy by solving the N-S control equation according to the known acceleration, wind stress, anchor chain tension, gravity, and buoyancy.

d.根据求得的水流拉力R1利用基于平板试验和理论分析所得到的海流阻力计算公式R1=C(ρV^2)Ω/2求解海流流速V。由此得到海流流速的大小和方向的初始值。d. According to the obtained water current pulling force R1, use the current resistance calculation formula R1=C(ρV^2)Ω/2 based on the flat plate test and theoretical analysis to solve the current flow velocity V. From this, the initial value of the magnitude and direction of the current velocity is obtained.

步骤五、对步骤四中获得的海流流速大小和方向的初始值进行修正,得到最后的结果。由于步骤四中得到的结果是由经验公式得到的,因此有必要重复进行实验对相关参数进行校正以获得更准确的结果。Step 5: Correct the initial values of the magnitude and direction of the current flow velocity obtained in the fourth step to obtain the final result. Since the results obtained in step 4 are obtained by empirical formulas, it is necessary to repeat the experiment to correct the relevant parameters to obtain more accurate results.

以上所述仅是本发明的优选实施方式,应当指出,对于本技术领域的普通技术人员来说,在不脱离本发明原理的前提下,还可以做出若干改进和变化,这些改进和变化也应视为发明的保护范围。The above are only the preferred embodiments of the present invention. It should be pointed out that for those skilled in the art, several improvements and changes can be made without departing from the principles of the present invention. These improvements and changes also It should be regarded as the scope of protection of the invention.

Claims (2)

1. A method for inverting surface ocean currents based on navigation buoy data comprises the following steps:
step one, arranging a navigation buoy in an observation sea area, and carrying a sea current data measuring system;
step two, collecting a buoy position value and a wind speed value according to the ocean current data measurement system, and correcting to obtain a motion parameter of the buoy; meanwhile, collecting actual parameters of the quality, the underwater depth and the anchor chain length of the buoy according to an ocean current data measuring system;
step three, establishing a buoy stress model according to the buoy motion parameters and the actual parameters;
analyzing the parameters of the ocean current resistance borne by the buoy in the buoy stress model through an ocean current inversion algorithm;
the ocean current inversion algorithm in the fourth step comprises the following steps:
3.1, calculating to obtain the movement acceleration of the buoy according to the buoy position value in the buoy stress model;
3.2, calculating according to the buoy wind speed value in the buoy stress model and the formula (1) to obtain the buoy wind stress;
R2=kqAd (1)
3.3, calculating the anchor chain tension borne by the buoy according to the length of the anchor chain of the buoy in the buoy stress model and a formula (2);
Figure FDA0003356947530000011
3.4, calculating the gravity borne by the buoy according to the mass of the buoy in the buoy stress model;
3.5, calculating buoyancy borne by the buoy according to the water entry depth of the buoy in the buoy stress model;
3.6, obtaining an ocean current resistance parameter R1 borne by the buoy according to the known parameters of the buoy generated in the step 3.1 to 3.5 through a buoy motion N-S control equation established by a Newton second motion law;
3.7 obtaining the current flow velocity V according to the formula (3) according to the known current resistance parameter R1:
R1=C(ρV^2)Ω/2 (3)
step five, calculating the movement parameters of the buoy in the step two and the ocean current resistance parameters borne by the buoy in the step four to obtain initial values of the flow velocity and the direction of the ocean current in the observation sea area;
and step six, correcting the initial values of the flow velocity and the direction of the ocean current obtained in the step five to obtain a final ocean current flow velocity value.
2. The method for inverting surface ocean currents based on navigation buoy data according to claim 1, wherein the ocean current data measuring system comprises a navigation buoy, a GPS locator, an anemometer, a data transmission unit and an anchor chain; the upper portion of the buoy is connected with an anemoscope, the gravity center position inside the buoy is provided with a GPS locator and a data transmission unit respectively, and the lower portion of the buoy is connected with an anchor chain.
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