CN115049754A - Method and device for generating infrared thermodynamic diagram on orbit based on satellite - Google Patents

Method and device for generating infrared thermodynamic diagram on orbit based on satellite Download PDF

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CN115049754A
CN115049754A CN202210977596.5A CN202210977596A CN115049754A CN 115049754 A CN115049754 A CN 115049754A CN 202210977596 A CN202210977596 A CN 202210977596A CN 115049754 A CN115049754 A CN 115049754A
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CN115049754B (en
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郭涛
赵宏杰
陆川
郭诗韵
张辉
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Chengdu Guoxing Aerospace Technology Co ltd
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Abstract

The embodiment of the application discloses a method and a device for generating an infrared thermodynamic diagram on orbit on a satellite. The method is applied to an in-orbit satellite, and comprises the following steps: acquiring a thermal infrared remote sensing image, wherein the infrared wavelength of the infrared remote sensing image is 3-14 mu m; converting the digital quantization DN value of each pixel in the thermal infrared remote sensing image into a radiance value of each pixel; calculating a brightness temperature value corresponding to the radiance value of each pixel; and generating a thermodynamic diagram of the thermal infrared remote sensing image according to the brightness temperature value corresponding to each pixel.

Description

Method and device for generating infrared thermodynamic diagram on orbit based on satellite
Technical Field
The embodiment of the application relates to the field of image processing, in particular to a method and a device for generating an infrared thermodynamic diagram on the basis of on-board satellite orbit.
Background
With the expansion and development of cities, the monitoring of urban thermal environment becomes a research hotspot in recent years. The urban thermodynamic diagram can reflect the thermal environment condition of the current city in time and space, and provides data support for monitoring urban pollution, researching urban heat island effect, urban planning development, intelligent management and the like. There are two main ways to monitor the urban thermal environment at present, one is: the method is based on an observation mode of a ground station, the data precision is high, but the global observation data is difficult to obtain due to the limited number of the ground observation stations, and a large-area cannot be covered; secondly, the following steps: when a satellite passes through a ground observation station, the satellite remote sensing image based on the satellite-borne thermal infrared sensor transmits a shot satellite image to the ground, a thermodynamic diagram is generated through a temperature inversion algorithm and is calculated and analyzed, and the whole city can be monitored through the method.
Because the satellite images have the characteristics of large coverage and strong timeliness, the generation of the thermal diagram currently mainly uses the satellite remote sensing images, and the inversion of the Surface Temperature (LST) is carried out by combining the atmospheric data observed by the ground station. The traditional thermodynamic diagram generation needs to go through the following steps: (1) a satellite obtains a remote sensing image and transmits data to the ground; (2) the DN value is converted into the radiance through the radiation correction; (3) performing geometric correction on the image; (4) calculating the brightness temperature according to the radiance value; (5) calculating the atmospheric transmittance according to the water vapor content of the atmosphere and the like, and performing atmospheric correction on the image; (6) inversion is performed on the LST in combination with the radiance to ground mass ratio. Finally, drawing a graph and analyzing the data.
The method has high inversion accuracy, but has complex ground procedures, large manual workload and low efficiency, and can not count and monitor the abnormal temperature of cities and surrounding areas in real time due to the large difficulty in acquiring the water vapor content in the atmosphere.
Disclosure of Invention
In order to solve any technical problem, the embodiment of the application provides a method and a device for generating an infrared thermodynamic diagram on the basis of on-board satellite orbit.
To achieve the purpose of the embodiments of the present application, the embodiments of the present application provide a method for generating an infrared thermodynamic diagram based on-satellite on-orbit, which is applied to an on-orbit satellite, and the method includes:
acquiring a thermal infrared remote sensing image of a target area, wherein the infrared wavelength of the infrared remote sensing image is 3-14 mu m;
converting the digital quantization DN value of each pixel in the thermal infrared remote sensing image into a radiance value of each pixel;
calculating a brightness temperature value corresponding to the radiance value of each pixel;
and generating a thermodynamic diagram of the thermal infrared remote sensing image according to the brightness temperature value corresponding to each pixel.
A storage medium having a computer program stored therein, wherein the computer program is arranged to perform the method as described above when executed.
An apparatus for on-board on-satellite-based generation of an infrared thermodynamic diagram, comprising a memory having a computer program stored therein and a processor arranged to execute the computer program to perform the method as described above.
One of the above technical solutions has the following advantages or beneficial effects:
the brightness temperature is directly used to show the relative relation of temperature difference, the required calculated amount is smaller, the working efficiency is higher, the urban and surrounding temperature data information can be conveniently and quickly acquired, the purpose of generating the infrared thermodynamic diagram on orbit is achieved, the thermodynamic diagram can be quickly generated on orbit to monitor the urban temperature change, the working efficiency is improved, and compared with the prior art that satellite images are transmitted to a ground station for data processing, the problems of complex operation processing method, large manual workload and lower efficiency are solved.
The method and the device improve the accuracy of image processing based on cloud and fog discrimination and cloud mask extraction on the satellite; meanwhile, according to the obtained new sample image, the on-orbit continuous iteration updating model is realized; the method has the advantages that the target calibration coefficient of the on-orbit on the satellite is determined in real time by utilizing the two calibration coefficients and the shooting date, so that the accuracy of the target calibration coefficient is ensured, and meanwhile, the working efficiency is improved; in addition, the workload of the ground station can be effectively reduced by extracting the abnormal temperature area based on the thermodynamic diagram.
Additional features and advantages of the embodiments of the application will be set forth in the description which follows, and in part will be obvious from the description, or may be learned by the practice of the embodiments of the application. The objectives and other advantages of the embodiments of the application may be realized and attained by the structure particularly pointed out in the written description and claims hereof as well as the appended drawings.
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The accompanying drawings are included to provide a further understanding of the embodiments of the present application and are incorporated in and constitute a part of this specification, illustrate embodiments of the present application and together with the examples of the embodiments of the present application do not constitute a limitation of the embodiments of the present application.
Fig. 1 is a flowchart of a method for generating an infrared thermodynamic diagram based on-board satellite orbit provided by the present application;
FIG. 2 is another flow chart of a method for on-board on-satellite in-orbit generation of an infrared thermodynamic diagram as provided herein;
fig. 3 is a flowchart of a management method of a cloud and fog discrimination model based on deep learning according to an embodiment of the present application.
Detailed Description
In order to make the objects, technical solutions and advantages of the embodiments of the present application more apparent, the embodiments of the present application will be described in detail below with reference to the accompanying drawings. It should be noted that, in the embodiments of the present application, features in the embodiments and the examples may be arbitrarily combined with each other without conflict.
Fig. 1 is a flowchart of a method for generating an infrared thermodynamic diagram based on-board satellite provided by the present application. As shown in fig. 1, the method is applied to an in-orbit satellite, and comprises the following steps:
step 101, acquiring a thermal infrared remote sensing image;
in one exemplary embodiment, a satellite-borne thermal infrared sensor can be used to obtain a thermal infrared remote sensing image of a preset area, wherein the infrared wavelength can be 3-14 μm.
Step 102, converting a DN (Digital Number) value of each pixel in the thermal infrared remote sensing image into a radiance value of each pixel;
the method of converting the DN value into the radiance value in the related art is applicable to this step, and is not described herein again.
103, calculating a brightness temperature value corresponding to the radiance value of each pixel;
in the related technology, the image needs to be transmitted to a ground station, and the ground station performs inversion to obtain accurate ground surface temperature, so that the generation of a thermodynamic diagram is realized. In contrast, in the embodiment of the application, the brightness temperature value of the pixel is directly used to show the relative relationship of the temperature difference between different areas, so that the accurate earth surface temperature is obtained without inversion, the urban and ambient temperature data information is conveniently and rapidly acquired, the working efficiency is improved, and the problems of complex processing method, large manual workload and low efficiency in the related technology are solved.
104, generating a thermodynamic diagram of the thermal infrared remote sensing image according to the brightness temperature value corresponding to each pixel;
compared with the thermodynamic diagram generated by accurately representing the temperature in the related art, the temperature difference generation method and the temperature difference generation device have the advantages that the relative relation between the temperatures is represented by the brightness temperature value of the pixel, the temperature difference of different areas is represented by the relative relation between the temperatures, the required calculation amount is smaller, and the work efficiency is higher.
According to the method provided by the embodiment of the application, the brightness temperature is directly used for showing the relative relation of the temperature difference, the city and surrounding temperature data information can be conveniently and quickly acquired, the purpose of generating the infrared thermodynamic diagram on the rail is achieved, the thermodynamic diagram can be quickly generated on the rail to monitor the temperature change of the city, and the working efficiency is improved.
Fig. 2 is another flowchart of a method for generating an infrared thermodynamic diagram based on-satellite orbit according to an embodiment of the present application. As shown in fig. 2, the method comprises the steps of:
step 201, acquiring a thermal infrared remote sensing image of a preset area by using a satellite-borne thermal infrared sensor;
step 202, carrying out cloud and fog discrimination on the obtained thermal infrared image and generating a mask;
specifically, cloud and fog recognition is carried out on the thermal infrared remote sensing image to obtain a target image with cloud and fog; and carrying out cloud and fog segmentation processing on the target image with the cloud and fog to generate a mask corresponding to the target image.
By generating a corresponding mask for the target image, interference of the highlighted DN value in the cloud area on subsequent DN value processing can be avoided.
Step 203, performing relative radiation correction on the masked thermal infrared remote sensing image;
and performing relative radiation correction on the region with cloud and fog in the thermal infrared remote sensing image by using the mask, so that the influence of the cloud and fog image on the thermal infrared remote sensing image in the processing process is reduced.
204, performing geometric correction on the target image after the relative radiation correction based on a global elevation model stored on the satellite;
the embodiments of geometric correction in the related art are all applicable to the present application and are not described herein again.
And step 205, converting the DN value of each pixel into the radiance value of each pixel according to the scaling coefficient.
And step 206, calculating a corresponding brightness temperature value according to the radiance value of each pixel element to generate a thermodynamic diagram.
Step 207, judging the area with abnormal temperature, and generating a binary image of the area with abnormal temperature;
wherein step 207 is an optional operation.
And step 208, transmitting the generated thermodynamic diagram and the image data of the temperature abnormal area to the ground station in the visible arc section of the ground station.
In the process of implementing task planning by the agile imaging satellite and the ground operation control system thereof, the visible arc segment of the target in a certain time period or a plurality of orbit circles needs to be calculated and forecasted according to target characteristic input provided by a user.
The method provided by the embodiment of the application realizes the on-orbit rapid processing of the thermal infrared remote sensing image by using on-satellite hardware resources, generates the urban thermodynamic diagram by using the bright temperature value obtained by on-orbit preprocessing and inversion, and simultaneously provides the method for rapidly downloading the temperature abnormal area information. The problem that ground processing timeliness of the current satellite-borne thermal infrared remote sensing image generated thermodynamic diagram is low is solved, and meanwhile abnormal temperature conditions of cities and surrounding areas can be rapidly counted and monitored.
The method is not only suitable for investigating the heat radiation characteristics of general objects on the earth surface (such as urban heat islands), but also suitable for other high-temperature target identification sensitive scenes (forest fires, active volcano identification and the like).
The method provided by the embodiments of the present application is explained as follows:
fig. 3 is a flowchart of a management method of a cloud and fog discrimination model based on deep learning according to an embodiment of the present application, and as shown in fig. 3, steps 301 to 307 are all on-satellite on-orbit real-time processing, and the specific steps are as follows:
step 301, cutting a large number of images into blocks, taking binary images marked as cloud and non-cloud as samples, and performing deep learning network model training to obtain an initial cloud and fog discrimination model;
302, performing cloud and mist distinguishing calculation based on an initial cloud and mist distinguishing model in real time on orbit on an image shot by a satellite, and outputting two classification calculation results based on cloud and non-cloud and mist;
step 303, extracting a cloud layer shielding region in the cloud image, wherein the extracting operation can be used for extracting a region meeting the condition based on a preset cloud segmentation algorithm;
step 304, generating a mask of a cloud layer shielding area;
the cloud and fog discrimination model obtained by deep learning algorithm training is transplanted to a satellite-borne hardware platform, cloud discrimination and cloud mask processing are performed on the obtained thermal infrared remote sensing image, new cloud samples can be injected to the satellite-borne hardware platform through a ground station for on-orbit learning, and algorithm precision is continuously improved. The satellite-borne hardware platform includes, but is not limited to, a GPU (graphics Processing Unit), an FPGA (Field Programmable Gate Array), and an NPU (Natural Processing Unit).
305, downloading a cloud and fog discrimination result on the satellite and a cloud mask to a ground station;
step 306, receiving a sample image fed back by the ground station;
the ground station can be used for judging cloud and fog identification precision by combining with a satellite remote sensing image, modifying an area with the judgment precision smaller than a preset threshold value, and taking a modification result as a sample image to be annotated with a satellite;
and 307, iteratively updating the cloud and fog discrimination model according to the received sample image.
Based on the process, the cloud and mist discrimination result obtained through the cloud and mist identification model on the satellite is downloaded to the ground station, the sample image is determined by screening the cloud and mist discrimination result through the ground station, the cloud and mist discrimination model stored on the satellite is updated based on the sample image, and the accuracy of the discrimination algorithm can be improved.
In an exemplary embodiment, the converting the digital quantized DN value of each pixel in the thermal infrared remote sensing image into a radiance value of each pixel includes:
acquiring a target gain value and a target offset value corresponding to the current date;
and multiplying the DN value of each pixel by the target gain value, and adding the DN value of each pixel with the target offset value to obtain the radiance value of each pixel.
The target gain value and the target offset value corresponding to the current date are obtained based on the gain value and the offset value determined by the two on-orbit calibrations, and the specific implementation mode is as follows:
step 401, determine a first date of an on-track scaling operation prior to a current date
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And a second date of the on-track calibration operation after the current date
Figure 595787DEST_PATH_IMAGE002
Step 402, determining a first date
Figure 546163DEST_PATH_IMAGE001
On-track calibration of operating gain values
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And an offset value
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And, a second date
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On-track calibration of operating gain values
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And an offset value
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The specific determination method is as follows:
and when the satellite passes through the border, synchronously acquiring the surface temperature of the water body, the surface radiation brightness of the water body and the meteorological parameters above the water body. And (4) calculating the radiance at the entrance pupil of the satellite according to the formula (1).
Figure 902899DEST_PATH_IMAGE008
;(1)
Wherein the content of the first and second substances,
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is a function of the wavelength of the light,
Figure 119434DEST_PATH_IMAGE010
is the radiance at the satellite entrance pupil; t is s Is the surface temperature;
Figure 528550DEST_PATH_IMAGE011
is a waveIs long as
Figure 488153DEST_PATH_IMAGE009
Surface emissivity of the earth;
Figure 590102DEST_PATH_IMAGE012
is a wavelength
Figure 769410DEST_PATH_IMAGE009
At temperature T of black body s The lower radiance can be calculated according to the Planck function;
Figure 841271DEST_PATH_IMAGE013
is a wavelength
Figure 156846DEST_PATH_IMAGE009
The atmospheric transmittance in the observation direction of the satellite sensor;
Figure 489800DEST_PATH_IMAGE014
and
Figure 890826DEST_PATH_IMAGE015
the radiation intensities of the atmosphere up and down, respectively.
Calculating to obtain satellite equivalent radiance by adopting an equation (2) according to the satellite entrance pupil radiance and the spectral response function, wherein the method comprises the following steps:
Figure 766378DEST_PATH_IMAGE016
; (2)
wherein the content of the first and second substances,
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is the equivalent radiance value of the satellite entrance pupil,
Figure 645789DEST_PATH_IMAGE018
as a function of the spectral response of the satellite.
And (4) obtaining a Gain value Gain and an offset value offset by the formula (3) according to the DN value of the water body pixel and the satellite equivalent radiance.
Figure 501487DEST_PATH_IMAGE019
; (3)
And step 403, obtaining a target gain value and a target offset value corresponding to the current date according to the gain value and the offset value corresponding to the on-track calibration operation of the first date and the second date.
And (5) determining a target scaling factor used by the current date by adopting the formula (4).
Figure 321676DEST_PATH_IMAGE020
; (4)
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; (5)
Wherein the content of the first and second substances,
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Figure 461167DEST_PATH_IMAGE022
and
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sequentially showing a first date, a second date and a current date,
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Figure 110214DEST_PATH_IMAGE025
Figure 707548DEST_PATH_IMAGE026
Sequentially showing a gain value corresponding to the first date, a gain value corresponding to the second date and a gain value corresponding to the current date;
Figure 603960DEST_PATH_IMAGE027
Figure 836096DEST_PATH_IMAGE028
Figure 58130DEST_PATH_IMAGE029
the offset value corresponding to the first date, the offset value corresponding to the second date, and the offset value corresponding to the current date are sequentially shown.
After the target scaling coefficient is obtained, the DN value is converted into an equivalent radiance value by adopting an equation (6), so that the equivalent radiance value is ensured:
Figure 267394DEST_PATH_IMAGE030
;(6)
the target calibration coefficient determined by the method is higher in accuracy, and the target calibration coefficient is used for calculating the equivalent radiance value, so that the accuracy of a calculation result is guaranteed.
How to calculate the brightness temperature value corresponding to the radiance value of each pixel is described below, which includes:
acquiring the sum of values corresponding to the spectral response function of the wavelength under different value-taking conditions;
obtaining a radiance value corresponding to the central wavelength of each pixel according to the sum of the values and the satellite equivalent radiance value of each pixel;
and calculating a brightness temperature value corresponding to the blackbody radiation brightness value of the central wavelength.
Because the central wavelength cannot accurately represent the whole thermal infrared wavelength range, values of the spectral response function under at least two wavelength values can be selected for calculation, so that the accuracy of the obtained radiance value is ensured.
Further, the radiance value is obtained by using the following formula (7):
Figure 967497DEST_PATH_IMAGE031
; (7)
wherein the content of the first and second substances,
Figure 821184DEST_PATH_IMAGE009
is the center wavelength of the light emitted by the light source,
Figure 184425DEST_PATH_IMAGE017
in order to radiate the brightness value of the light,
Figure 880986DEST_PATH_IMAGE032
is a value of the spectral response function,
Figure 119200DEST_PATH_IMAGE011
for the global emissivity map stored on the satellite,
Figure 358552DEST_PATH_IMAGE033
at a temperature T and a center wavelength of
Figure 391230DEST_PATH_IMAGE009
The value of the radiance at the time of the illumination,
Figure 948988DEST_PATH_IMAGE034
as wavelength in the spectral response function
Figure 115527DEST_PATH_IMAGE009
The minimum value of (a) is determined,
Figure 943806DEST_PATH_IMAGE035
as wavelength in the spectral response function
Figure 412964DEST_PATH_IMAGE009
Is measured.
The main purpose of the on-track thermodynamic diagram generation is to quickly monitor a temperature abnormal area, the surface temperature does not need to be accurately represented, and only the relative condition of the surface temperature needs to be reflected, so that the atmospheric effect can be ignored, and the Planck function simplified by the equation (1) is adopted to obtain the brightness temperature value.
Calculating a brightness temperature value by using a simplified Planck equation based on a global emissivity map stored on the satellite, and specifically referring to formula (8):
Figure 40965DEST_PATH_IMAGE037
;(8)
wherein, C 1 Is a first radiation constant, C 2 Is the second radiation constant.
Wherein, C 1 Can take the value of 1.191x10 -5 mW·sr -1 ·cm -4 ,C 2 The value of (A) may be 1.438833cm K.
The computational complexity for determining the brightness value based on the radiance value is significantly reduced due to the neglect of atmospheric effects.
Optionally, after obtaining the thermodynamic diagram, determining a target region indicating that the temperature is abnormal in the thermodynamic diagram, where the specific implementation manner is as follows:
performing image segmentation on the thermodynamic diagram to obtain at least two image fragments;
performing the following operations for each image slice, including:
calculating pixel values corresponding to all pixels in the image fragment to obtain the maximum value and the average value of the pixels of the image fragment;
if the maximum value of the image elements in the image fragment is at least two times higher than the average value, marking the image elements, and determining the area where the marked image elements are located as a temperature abnormal area only when the marked image elements are connected and the number of the marked image elements is larger than a preset number threshold;
recording the central coordinates of the temperature abnormal area;
cutting according to a preset range by taking the central coordinate as a center to obtain a target area;
and carrying out binarization processing on the cut target area according to abnormity and non-abnormity to obtain the coordinate information of the central point of the temperature abnormal area.
Specifically, performing N × N windowing calculation on the generated thermodynamic diagram, wherein N is an integer; counting the maximum value and the average value in the window; when the maximum value in the window is more than 3 times higher than the average value, marking the pixel, and only when the marked pixels are connected and the number of the pixels is more than N/2, considering the pixels as a temperature abnormal area, recording the central coordinate of the area, and cutting the pixels according to a certain rectangular range by taking the central coordinate as the center to obtain a target area; and carrying out binarization processing on the cut target area according to abnormity and non-abnormity to obtain the coordinate information of the central point of the abnormal temperature area.
In summary, the embodiment of the present application provides a scheme for generating a thermodynamic diagram on a satellite, where the scheme uses a brightness temperature value of a pixel to represent a relative relationship of surface temperatures, so as to effectively reduce ground procedures and manual workload, and improve monitoring timeliness and frequency.
In addition, the accuracy of image processing is improved based on cloud and mist discrimination and cloud mask extraction on the satellite; meanwhile, according to the obtained new sample image, the on-orbit continuous iteration updating model is realized; the method has the advantages that the target calibration coefficient of the on-orbit on the satellite is determined in real time by utilizing the two calibration coefficients and the shooting date, so that the accuracy of the target calibration coefficient is ensured, and meanwhile, the working efficiency is improved; in addition, the workload of the ground station can be effectively reduced by extracting the abnormal temperature area based on the thermodynamic diagram.
The method is not only suitable for investigating the heat radiation characteristics of general objects on the ground (such as urban heat islands), but also suitable for other high-temperature target recognition sensitive scenes (forest fires, live volcano recognition and the like).
An embodiment of the present application provides a storage medium, in which a computer program is stored, wherein the computer program is configured to perform the method described in any one of the above when the computer program runs.
The present application provides an apparatus for generating an infrared thermodynamic diagram on orbit on a satellite, including a memory and a processor, where the memory stores a computer program, and the processor is configured to execute the computer program to perform the method described in any one of the above.
It will be understood by those of ordinary skill in the art that all or some of the steps of the methods, systems, functional modules/units in the devices disclosed above may be implemented as software, firmware, hardware, or suitable combinations thereof. In a hardware implementation, the division between functional modules/units mentioned in the above description does not necessarily correspond to the division of physical components; for example, one physical component may have multiple functions, or one function or step may be performed by several physical components in cooperation. Some or all of the components may be implemented as software executed by a processor, such as a digital signal processor or microprocessor, or as hardware, or as an integrated circuit, such as an application specific integrated circuit. Such software may be distributed on computer readable media, which may include computer storage media (or non-transitory media) and communication media (or transitory media). The term computer storage media includes volatile and nonvolatile, removable and non-removable media implemented in any method or technology for storage of information such as computer readable instructions, data structures, program modules or other data, as is well known to those of ordinary skill in the art. Computer storage media includes, but is not limited to, RAM (Random Access Memory), ROM (Read-Only Memory), EEPROM (Electrically Erasable Programmable Read-Only Memory), flash Memory or other Memory technology, CD-ROM (Compact Disc Read-Only Memory), Digital Versatile Discs (DVD) or other optical Disc storage, magnetic cassettes, magnetic tape, magnetic disk storage or other magnetic storage devices, or any other medium which can be used to store the desired information and which can be accessed by a computer. In addition, communication media typically embodies computer readable instructions, data structures, program modules or other data in a modulated data signal such as a carrier wave or other transport mechanism and includes any information delivery media as known to those skilled in the art.

Claims (10)

1. A method for generating an infrared thermodynamic diagram based on-orbit satellite on a satellite, which is applied to real-time processing on in-orbit satellite hardware to generate the infrared thermodynamic diagram, and comprises the following steps:
acquiring a thermal infrared remote sensing image of a target area, wherein the infrared wavelength of the infrared remote sensing image is 3-14 mu m;
converting the digital quantization DN value of each pixel in the thermal infrared remote sensing image into a radiance value of each pixel;
calculating a brightness temperature value corresponding to the radiance value of each pixel;
and generating a thermodynamic diagram of the thermal infrared remote sensing image according to the brightness temperature value corresponding to each pixel.
2. The method of claim 1, wherein prior to converting the digitally quantized DN value for each pixel in the thermal infrared remote sensing image to a radiance value for each pixel, the method further comprises:
carrying out cloud and fog recognition on the thermal infrared remote sensing image to obtain a target image with cloud and fog;
carrying out cloud and fog segmentation processing on the target image with cloud and fog to generate a mask corresponding to the target image;
performing relative radiation correction on the target image by using the mask;
performing geometric correction on the target image after the relative radiation correction based on a global elevation model stored on the satellite;
and after the relative radiation correction and the geometric correction are finished, converting the digital quantization DN value into a radiation brightness value.
3. The method of claim 2, wherein:
carrying out cloud and fog recognition on the thermal infrared remote sensing image by utilizing a cloud and fog discrimination model prestored on the satellite, wherein the cloud and fog discrimination model is obtained by training according to a sample image sent by a ground station;
after the mask corresponding to the target image is generated, the method further includes:
downloading the processing result of the cloud and fog discrimination model on the satellite and the cloud mask to the ground station;
receiving a sample image fed back by a ground station, wherein the ground station can be combined with a satellite remote sensing image to judge cloud and fog identification precision, modify an area with the judgment precision smaller than a preset threshold value, and annotate a satellite on the modified result serving as the sample image;
and according to the received sample image, carrying out iterative update on the cloud and fog discrimination model.
4. The method of claim 1, wherein converting the digitally quantized DN value of each pixel in the thermal infrared remote sensing image into a radiance value of each pixel comprises:
acquiring a target gain value and a target offset value corresponding to the current date;
and multiplying the DN value of each pixel by the target gain value, and adding the DN value of each pixel with the target offset value to obtain the radiance value of each pixel.
5. The method of claim 4, wherein obtaining the target gain value and the target offset value corresponding to the current date comprises:
determining a first date of an on-track scaling operation prior to a current date
Figure 950207DEST_PATH_IMAGE001
And a second date of the on-track calibration operation after the current date
Figure 929664DEST_PATH_IMAGE002
Determining a first date
Figure 443822DEST_PATH_IMAGE001
On-track calibration of operating gain values
Figure 635769DEST_PATH_IMAGE003
And offset value
Figure 309196DEST_PATH_IMAGE004
And, a second date
Figure 928396DEST_PATH_IMAGE002
On-track calibration of operating gain values
Figure 929850DEST_PATH_IMAGE005
And an offset value
Figure 925488DEST_PATH_IMAGE006
Obtaining a target gain value and a target offset value corresponding to the current date according to the gain value and the offset value corresponding to the on-orbit scaling operation of the first date and the second date;
wherein, gain value and offset value corresponding to each on-orbit calibration operation are obtained by the following method, including:
calculating equivalent radiance of satellite
Figure 456351DEST_PATH_IMAGE007
The method comprises the following steps:
Figure 512032DEST_PATH_IMAGE008
wherein the content of the first and second substances,
Figure DEST_PATH_IMAGE010A
is the radiance at the satellite entrance pupil;
according to DN value of water body pixel and satellite equivalent radiance
Figure 718891DEST_PATH_IMAGE007
Calculating Gain and offset;
Figure 518220DEST_PATH_IMAGE011
wherein the content of the first and second substances,
Figure 900660DEST_PATH_IMAGE007
is the equivalent radiance value of the satellite entrance pupil,
Figure 395750DEST_PATH_IMAGE012
as a function of the spectral response of the satellite.
6. The method of claim 5, wherein the target gain value and the target offset value corresponding to the current date are obtained according to the gain value and the offset value corresponding to the on-track scaling operation of the first date and the second date, and the calculation expression is as follows:
Figure 434114DEST_PATH_IMAGE013
Figure 443658DEST_PATH_IMAGE014
wherein the content of the first and second substances,
Figure 149446DEST_PATH_IMAGE015
Figure 281350DEST_PATH_IMAGE016
and
Figure 338167DEST_PATH_IMAGE017
sequentially showing a first date, a second date and a current date,
Figure 479299DEST_PATH_IMAGE018
Figure 39593DEST_PATH_IMAGE019
Figure 607978DEST_PATH_IMAGE020
Sequentially showing a gain value corresponding to the first date, a gain value corresponding to the second date and a target gain value corresponding to the current date;
Figure 635582DEST_PATH_IMAGE021
Figure 580404DEST_PATH_IMAGE022
Figure 995205DEST_PATH_IMAGE023
the offset value corresponding to the first date, the offset value corresponding to the second date, and the target offset value corresponding to the current date are sequentially expressed.
7. The method of claim 1, wherein calculating a brightness temperature value corresponding to a radiance value of each pixel element comprises:
acquiring the sum of values corresponding to the spectral response function of the wavelength under different value-taking conditions;
obtaining a blackbody radiation brightness value corresponding to the central wavelength of each pixel according to the sum of the values and the satellite equivalent radiation brightness value of each pixel;
calculating a brightness temperature value corresponding to the blackbody radiation brightness value of the central wavelength;
wherein, the calculation expression of the blackbody radiation brightness value is as follows:
Figure 70DEST_PATH_IMAGE024
wherein the content of the first and second substances,
Figure 297059DEST_PATH_IMAGE025
is the center wavelength of the light emitted by the light source,
Figure 779993DEST_PATH_IMAGE026
is the radiance value of the satellite's entrance pupil,
Figure 314879DEST_PATH_IMAGE027
is the value of the spectral response function,
Figure 490646DEST_PATH_IMAGE028
for the global emissivity map stored on the satellite,
Figure 215544DEST_PATH_IMAGE029
at a temperature T and a center wavelength of
Figure 174273DEST_PATH_IMAGE025
The value of the black body radiation luminance at the time,
Figure 298086DEST_PATH_IMAGE030
as wavelength in the spectral response function
Figure 379175DEST_PATH_IMAGE025
The minimum value of (a) is determined,
Figure 650756DEST_PATH_IMAGE031
as wavelength in the spectral response function
Figure 475493DEST_PATH_IMAGE025
Is measured.
8. The method according to claim 1, wherein calculating the brightness temperature value corresponding to the blackbody radiation brightness value of the center wavelength using the following computational expression comprises:
Figure DEST_PATH_IMAGE033
wherein, C 1 Is a first radiation constant, C 2 Is the second radiation constant.
9. The method of claim 1, wherein after generating the thermodynamic diagram of the thermal infrared remote sensing image according to the brightness temperature value corresponding to each pixel, the method further comprises:
judging the area indicating the temperature abnormality in the thermodynamic diagram, comprising:
performing image segmentation on the thermodynamic diagram to obtain at least two image fragments;
performing the following operations for each image slice, including:
calculating pixel values corresponding to all pixels in the image fragment to obtain the maximum value and the average value of the pixels of the image fragment;
if the maximum value of the image elements in the image fragment is at least two times higher than the average value, marking the image elements, and determining the area where the marked image elements are located as a temperature abnormal area only when the marked image elements are connected and the number of the marked image elements is larger than a preset number threshold;
recording the central coordinates of the temperature abnormal area;
cutting according to a preset range by taking the central coordinate as a center to obtain a target area;
and carrying out binarization processing on the cut target area according to abnormity and non-abnormity to obtain the coordinate information of the central point of the temperature abnormal area.
10. An apparatus for on-board on-satellite in-orbit generation of an infrared thermodynamic diagram, comprising a memory and a processor, wherein the memory has stored therein a computer program, the processor being arranged to execute the computer program to perform the method of any one of claims 1 to 9.
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