Introduction to remote sensing

Release date:2021-12-15 Update date:2023-08-23 Editor:admin View counts:1972


Introduction to remote sensing

Remote Sensing (RS) is a science and technology that obtains its characteristic information and extracts, processes, expresses and applies it through a kind of sensor device without direct contact with the research object.

As a term, remote sensing appeared in 1962. The rapid development and wide use of remote sensing technology in the world came after the successful launch and acquisition of a large number of satellite images by the first Earth Resources Technology Satellite (LANDSAT-1) of the United States in 1972. In recent years, with the development of geographic information system technology, remote sensing technology and its close combination, the development is more rapid.

The basis of remote sensing technology is to interpret and analyze the targets and phenomena of the earth’s surface by observing electromagnetic waves. It utilizes the electromagnetic wave characteristics of the earth’s objects, that is, “all objects have the characteristics of reflecting or radiating electromagnetic waves of different wavelengths because of their different types and environmental conditions” (Fig. 12-1). So remote sensing can also be said to be a method of using objects to reflect or radiate electromagnetic waves. The inherent characteristics of the object, through the observation of electromagnetic waves, identify the object and the existence of environmental conditions of the object technology.


Figure 12-1: Electromagnetic reflection curves of several common ground objects (water, green vegetation, bare dryland)

In remote sensing technology, the devices receiving electromagnetic waves reflected or radiated from the target are called remote sensors, and the mobile objects carrying these remote sensors are called remote sensing platforms, including airplanes, satellites, and even ground observation vehicles belong to remote sensing platforms. Aerial Remote Sensing is commonly referred to as the airborne platform, while the spaceborne platform is called the space remote sensing.

According to the working principle of remote sensing, remote sensing can be divided into passive remote sensing and active remote sensing. Each mode can be divided into scanning mode and non-scanning mode. MSS (Multispectral Scanner) and TM (Thematic Mapper) used by land satellites belong to passive and scanning mode (Figure 12-2). SAR-Synthetic Aperture Radar (SAR-Synthetic Aperture Radar) is an active and scanning remote sensor.


Figure 12-2: schematic diagram of a multispectral scanner [Curran]

From the definition of remote sensing, we can see that, firstly, the remote sensor does not contact with the research object directly, that is to say, the “remote” here does not mean “remote”; secondly, the purpose of remote sensing is to obtain the characteristic information of the research object; finally, the data obtained through the sensor device will go through a processing process before being used. Figure 12-3 describes the process from acquiring remote sensing data to application.


Figure 12-3: Remote sensing data process

Processing of remote sensing data, usually in the form of images, mainly includes correction (including radiation correction and geometric correction), enhancement, transformation, filtering, classification and other functions. Its main purpose is to extract various thematic information, such as land construction, vegetation coverage, crop yield and water depth, etc. (Figure 12-4). Remote sensing image processing can adopt optical processing and digital processing. Digital image processing is widely used because of its good repeatability and easy integration with GIS. Following is a brief introduction to the main functions of digital image processing.


Figure 12-4: TM composite image near Donghu Lake, Wuhan City. Ships on the Yangtze River are clearly visible.

(Synthetic scheme: R = TM7, G = TM4, B = TM2, enhanced)

1) Image Correction

Image correction is a process of eliminating image distortion, including radiation correction and geometric correction. Radiation distortion is usually caused by solar position and atmospheric absorption and scattering. Geometric distortion (Figure 12-5) is caused by velocity, attitude change of remote sensing platform, sensor and topographic fluctuation. Geometric correction includes rough correction and precise correction. The former is corrected according to relevant parameters. The latter is constructed by collecting ground control points (GCPs, Ground Control Points). Correction polynomials are established and corrected.


Figure 12-5: Geometric distortion of remote sensing images [Lillesand and Kiefer]


The purpose of enhancement is to improve the visual effect of the image, without increasing the amount of information, including brightness, contrast change and histogram transformation.


Filtering is divided into low-pass filtering, high-pass filtering and band-pass filtering. Low-pass filtering can remove noise in images, while high-pass filtering is used to extract some linear information, such as roads, regional boundaries and so on. The filtering can be operated by filtering template in spatial domain or directly in frequency domain.


It includes Principal Component Analysis (PCA), chromaticity transformation and Fourier transform. It also includes some specific transformations for remote sensing images, such as hat transformation.


The main purpose of using remote sensing images is to extract various kinds of information. Some specific transformations can be used to extract information, but the main method is to classify remote sensing images. The basic principle of computer classification is to calculate the gray level characteristics of each pixel in the image and classify them according to different criteria. There are two classifications for remote sensing image classification: Supervised Classification and Unsupervised Classification. The former needs to determine each class and its training area beforehand, calculate the gray level statistical characteristics of training area pixels, and then merge other pixels into different classes. The latter is based on the similarity and similarity between gray level features of pixels directly. Different degrees of merger and differentiation, forming different categories. Typical supervised classification algorithms include minimum distance method, maximum likelihood method, parallel hexahedron method, etc. K-means clustering belongs to unsupervised classification. Applying ANN (Artificial Neural Network) to remote sensing classification can achieve better classification results in some cases.

The emergence of remote sensing has expanded human’s ability to understand their living environment. Compared with the data obtained from traditional field surveys and field observations, remote sensing technology has the following advantages:

  • The observation range is enlarged.

  • It can provide a wide range of instantaneous static images for monitoring dynamic changes.

  • It can carry out large-scale repetitive observation, even in remote areas which are difficult for human beings to reach.

  • The spectrum range that the human eye can observe is greatly broadened, and the electromagnetic wave band used in remote sensing is far beyond the visible light range from X-ray to microwave, while radar remote sensing can observe all-weather without restriction of day and night and weather change due to the use of microwave.

  • With high spatial detail, the spatial resolution of aerial photographs can be as high as centimeter level or even millimeter level.

Compared with aerial remote sensing, aerospace remote sensing can perform continuous, all-weather work, provide a larger range of data, and its cost is lower, which is the main way to obtain remote sensing data; while aerial remote sensing is mainly used in temporary and urgent observation tasks to obtain high-precision data. At present, many countries in the world have launched various remote sensing satellites for different purposes, and the spatial and spectral resolution of their remote sensors are also different, forming a series of ground observation data sources from coarse to fine, which can be used to monitor information and its dynamic changes from land use, crop growth, vegetation cover to floods, forest fires, pollution and other phenomena. 。

In a word, remote sensing technology can monitor environmental information more quickly and objectively. At the same time, because of the spatial distribution characteristics of remote sensing data, it can be used as an important data source of Geographic Information System to update the spatial database in real time.

Table 12-1: Several commonly used remote sensing satellites and their remote sensor parameters

Satellite sensor

Band (μ m)

Spatial resolution

Coverage area


Main use

Landsat TM








30m (1-5pm 7 band)

185km ×


16 days

Water depth, water color

Water color, vegetation

Chlorophyll, residential area

Plant growth

Soil and plant moisture

Cloud and surface temperature

Rock type










60km ×


26 days

Water color, plant condition

Chlorophyll, residential area

Plant growth













Plants, clouds, ice and snow

Plants and the boundary between water and land

Hot spots, night clouds

Cloud and surface temperature

Atmospheric and surface temperature












11km ×


14 days

  • 1. Geographical Cognition of the Real World
  • 2. The abstraction of the real world
  • 3. Bit world
  • 1. Data meaning and data type
  • 2. Measurement scale of data
  • 3. GIS data quality
  • 1. Map digitization
  • 2. Processing of spatial data entry
  • 1. Computer network technology
  • 2. Distributed geographic information system
  • 3. WebGIS - World Wide Web Geographic Information System
  • 1. Socialization of GIS
  • 2. Other problems of GIS socialization
  • 3. The impact of society on the development of GIS

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