Cross-Comparison Between China HJ1A-CCD and Landsat TM Data

Slides:



Advertisements
Similar presentations
Cross-Comparison Between China HJ1A-CCD and Landsat TM Data Guoqing Li, Xiaobing Li*, Hong Wang, Lihong Chen, Wanyu Wen State Key Laboratory of Earth Surface.
Advertisements

Evaluating Calibration of MODIS Thermal Emissive Bands Using Infrared Atmospheric Sounding Interferometer Measurements Yonghong Li a, Aisheng Wu a, Xiaoxiong.
Major Operations of Digital Image Processing (DIP) Image Quality Assessment Radiometric Correction Geometric Correction Image Classification Introduction.
Resolution Resolving power Measuring of the ability of a sensor to distinguish between signals that are spatially near or spectrally similar.
Some Basic Concepts of Remote Sensing
Resolution.
1. 2 Definition 1 – Remote sensing is the acquiring of information about an object or scene without touching it through using electromagnetic energy a.
Class 8: Radiometric Corrections
Study on applying MODIS image into drought indicator analysis in Taiwan Yuh-Lurng Chung, Chaur-Tzuhn Chen Chen-Ni Hsi, Shih-Ming Liu Yuh-Lurng.
Remote sensing in meteorology
Modeling Digital Remote Sensing Presented by Rob Snyder.
Remote Sensing of Our Environment Using Satellite Digital Images to Analyze the Earth’s Surface.
Remote Sensing What is Remote Sensing? What is Remote Sensing? Sample Images Sample Images What do you need for it to work? What do you need for it to.
January 20, 2006 Geog 258: Maps and GIS
Meteorological satellites – National Oceanographic and Atmospheric Administration (NOAA)-Polar Orbiting Environmental Satellite (POES) Orbital characteristics.
Hyperspectral Satellite Imaging Planning a Mission Victor Gardner University of Maryland 2007 AIAA Region 1 Mid-Atlantic Student Conference National Institute.
The Global Digital Elevation Model (GTOPO30) of Great Basin Location: latitude 38  15’ to 42  N, longitude 118  30’ to 115  30’ W Grid size: 925 m.
Fundamentals of Satellite Remote Sensing NASA ARSET- AQ Introduction to Remote Sensing and Air Quality Applications Winter 2014 Webinar Series ARSET -
Introduction to Digital Data and Imagery
Remote Sensing 2012 SUMMER INSTITUTE. Presented by: Mark A. Van Hecke National Science Olympiad Earth-Space Science Event Chair Roy Highberg North Carolina.
FEATURE EXTRACTION FOR JAVA CHARACTER RECOGNITION Rudy Adipranata, Liliana, Meiliana Indrawijaya, Gregorius Satia Budhi Informatics Department, Petra Christian.
HJ-1A/B CCD IMAGERY Geometric Distortions and Precise Geometric Correction Accuracy Analysis Changmiao Hu, Ping Tang
Satellites and Sensors
Regional Climate Modeling in the Source Region of Yellow River with complex topography using the RegCM3: Model validation Pinhong Hui, Jianping Tang School.
Geography 1010 Remote Sensing. Outline Last Lecture –Electromagnetic energy. –Spectral Signatures. Today’s Lecture –Spectral Signatures. –Satellite Remote.
Satellite Imagery and Remote Sensing NC Climate Fellows June 2012 DeeDee Whitaker SW Guilford High Earth/Environmental Science & Chemistry.
Introduction to Remote Sensing. Outline What is remote sensing? The electromagnetic spectrum (EMS) The four resolutions Image Classification Incorporation.
Spectral Characteristics
Remote Sensing Basics | August, Calibrated Landsat Digital Number (DN) to Top of Atmosphere (TOA) Reflectance Conversion Richard Irish - SSAI/GSFC.
Resolution A sensor's various resolutions are very important characteristics. These resolution categories include: spatial spectral temporal radiometric.
Guilford County SciVis V Applying Pixel Values to Digital Images.
Resolution Resolution. Landsat ETM+ image Learning Objectives Be able to name and define the four types of data resolution. Be able to calculate the.
Fuzzy Entropy based feature selection for classification of hyperspectral data Mahesh Pal Department of Civil Engineering National Institute of Technology.
Chapter 5 Remote Sensing Crop Science 6 Fall 2004 October 22, 2004.
West Hills College Farm of the Future. West Hills College Farm of the Future Precision Agriculture – Lesson 4 Remote Sensing A group of techniques for.
The ALTA Spectrometer Introduction to Remote Sensing Adapted from Fundementals of Remote Sensing
Remote Sensing. Vulnerability is the degree to which a system is susceptible to, or unable to cope with, adverse effects of climate change, including.
Remote Sensing Introduction to light and color. What is remote sensing? Introduction to satellite imagery. 5 resolutions of satellite imagery. Satellite.
The Semivariogram in Remote Sensing: An Introduction P. J. Curran, Remote Sensing of Environment 24: (1988). Presented by Dahl Winters Geog 577,
Remote Sensing Data Acquisition. 1. Major Remote Sensing Systems.
Satellite Imagery and Remote Sensing DeeDee Whitaker SW Guilford High EES & Chemistry
Chapter 8 Remote Sensing & GIS Integration. Basics EM spectrum: fig p. 268 reflected emitted detection film sensor atmospheric attenuation.
Remotely sensed land cover heterogeneity
14 ARM Science Team Meeting, Albuquerque, NM, March 21-26, 2004 Canada Centre for Remote Sensing - Centre canadien de télédétection Geomatics Canada Natural.
Assessment of Atmospheric Correction Methods for Landsat TM Data Applicable to Amazon Basin Research Dengsheng Lu, Paul Mausel (Department of Geography,
ERDAS 1: INTRODUCTION TO ERDAS IMAGINE
Data Models, Pixels, and Satellite Bands. Understand the differences between raster and vector data. What are digital numbers (DNs) and what do they.
Satellites Storm “Since the early 1960s, virtually all areas of the atmospheric sciences have been revolutionized by the development and application of.
Progress of in-flight Calibration of HJ-1A/HSI Li Chuanrong Invited expert of NRSCC Professor and Vice President Academy of Opto-Electronics,CAS Phuket,
SATELLITE ORBITS The monitoring capabilities of the sensor are, to a large extent, governed by the parameters of the satellite orbit. Different types of.
Interactions of EMR with the Earth’s Surface
Spatial Analysis Variogram
Remote sensing: the collection of information about an object without being in direct physical contact with the object. the collection of information about.
Orbits and Sensors Multispectral Sensors. Satellite Orbits Orbital parameters can be tuned to produce particular, useful orbits Geostationary Sun synchronous.
Remote sensing of snow in visible and near-infrared wavelengths
Using vegetation indices (NDVI) to study vegetation
Basic Concepts of Remote Sensing
GEOGRAPHIC INFORMATION SYSTEMS & RS INTERVIEW QUESTIONS ANSWERS
Digital Data Format and Storage
Remote Sensing What is Remote Sensing? Sample Images
Toru Kouyama Supported by SELENE/SP Team HISUI calibration WG
Digital Numbers The Remote Sensing world calls cell values are also called a digital number or DN. In most of the imagery we work with the DN represents.
Lunar reflectance model based on SELENE/SP data
Satellite Sensors – Historical Perspectives
REMOTE SENSING Multispectral Image Classification
Image Information Extraction
Planning a Remote Sensing Project
REMOTE SENSING.
Spectral Transformation
Remote sensing in meteorology
Presentation transcript:

Cross-Comparison Between China HJ1A-CCD and Landsat TM Data Guoqing Li, Xiaobing Li*, Hong Wang, Lihong Chen, Wanyu Wen   State Key Laboratory of Earth Surface Processes and Resource Ecology, College of Resources Science and Technology, Beijing Normal University, Beijing, China, 100875

1. Introduction 2. Selection of Image Test Zone 3. Methodology 4. Results and Discussion

1. Introduction With the increasing service life of Landsat 5, the stability of over-life operation of sensor is facing important challenges. In addition, many currently used data outcomes directly or indirectly come from TM or ETM+ data. It is especially necessary to choose a remote sensing data source similar to Landsat TM data which can replace TM in a certain degree. Considering there is great similarity between the wave–band design and spatial resolution of the China HJ1A/1B satellite CCD Camera and Landsat TM data, this paper plans to conduct comparison and analysis to the data mentioned above from the aspects of track parameter, spectral response characteristics and imaging quality.

The HJ-1 satellite was launched successfully in 2008, and carried two satellites: HJ-1A and HJ-1B. HJ-1A carries two CCD sensors with 30 m spatial resolution and a hyper-spectral sensor with 100 m spatial resolution. HJ-1B carries two identical CCD sensors and an infrared sensor with two kinds of spatial resolution (150 m at near, short-wave and middle-infrared band scope and 300 m at far-infrared band). The return period of the HJ-1 satellite is two days, with synergistic operation of HJ-1A and HJ-1B. The scan width exceeds 700 km with the two satellite CCD sensors working together. This enables HJ-1 CCD remote sensing images covering all lands of China to be captured every two to three days.

Tab1. Orbital characteristics of Landsat5 and HJ satellites Altitude(km) Inclination(°) Repetition cycle(d) Cycles/d HJ1A、1B 649.09 97.996 31 14+23/31 Landsat5 705 98.2 16 14.5 Tab2 Contrasting between HJ-CCD and Landsat TM imaging parameters Particular HJ1A、1B-CCD/ Landsat TM Spatial resolution /m 30/30 Swath width(km) 360/185 Bands no. 4/7 HJ CCD band(1-4)/μm 0.43-0.52 0.52-0.60 0.63-0.69 0.76-0.9 LandsatTM band (1-7)/μm 0.45-0.52 5-7(Omission) 可以较为详细的介绍tab2 The sensor of HJ1A and 1B satellite CCD cameras does not have shortwave infrared (SWIR) waveband, and its infrared imaging is completed by the infrared camera of HJ1B satellite. Of the 1~4 wavebands of the CCD camera, except there is a difference of 0.02μm between the first waveband and the TM data, the range of the other three wavebands is consistent (Table2). This has provided a consistent data foundation to conduct comparative research of image qualities of the two sensors.

Figure1. Spectral response profiles of Landsat TM From Figure 1 we can see that in the range of the 1~4 (blue, green, red and near-infrared) wavebands, these two sensors have similar spectral response characteristics, thus having obvious consistent comparability from the spectral perspective. Figure1. Spectral response profiles of Landsat TM and HJ1A-CCD1 in corresponding 1st to 4th wavelength region

2. Selection of Image Test Zone In order to comparatively analyze images in the research zone, selection of image pair should consider similar viewing angles of sensors and cloudlessness, and the imaging time should also be close to obtain images with similar solar altitudes and solar azimuths to compare two different sensor images. In addition, in order to objectively analyze the relation of two different remote sensing images in the spectral range of the whole design, the research zone should have rich surface features; there should be highly reflective areas and there should also be lowly reflective areas, which should to a great extent be averagely distributed in the whole grayscale range of the remote sensing images (Figure2). Figure2. Overlaid area of TM and HJ1A-CCD1 synchronization scenes within China Satellite Sensor Scene_Center_Scan_Time (GMT) Sun Elevation (°) Sun Azimuth (°) Earth-Sun distance in astronomical units HJ1-CCD1 2010-9-9 3:15 45.55 164.15 1.00733 Landsat-TM 2010-9-9 2:41 43.53 152.96

HJ1A-CCD1 4(R) 3(G)2(B) Landsat-TM 4(R) 3(G)2(B)

3. Methodology 3.1 Radiation Precision Analysis Radiation precision is the index which reflects the information richness of the image. Many scholars have adopted grayscale mean-value and grayscale variance to evaluate radiation precision, and they believe that for different images of the area, the bigger is the distribution range of grayscale, the bigger the variance, and the richer the image information (Franke2006,LI Shi-hua 2009). But the physical significance of the image’s grayscale is not determined, which is closely related to the calibration parameter. This paper has adopted maximum, minimum, mean value (Formula1) and variance of radiances of different wavebands to measure the radiation precision (Formula2).

3.1 Radiation Precision Analysis (m, n are the height and width of the image; f(i, j) is the radiances of the image; v is the mean value of radiance.)

3.2 Calculation of Texture and Definition Information entropy is a measurement of the information amount that the image possesses. The higher complexity the texture has, the bigger the image information amount is, and the bigger its information entropy is. This paper adopts the normalized Gray-level Co-occurrence Matrix to calculate the entropy (Formula3); the improved Point Sharpness Method is used to evaluate definition of the image (Formula4).

is the probability of pixel gray value of “ i ”, MAX is the max valve of grayscale. ( m, n are the height and width of the image; df is the amplitude of the image grayscale; dx is the distance increments between pixels; “a” is the number of pixels around pixel “i”.)

4. Results and Discussion Table3.Landsat TM and HJ1A-CCD1 mean value and variance of radiance TM/HJ1A-CCD1 Min Max Mean Variance Band1(B) 40.99/ 9.32 254.97/ 373.71 59.97/ 6.11 107.16/ 83.11 Band2(G) 33.92/ 9.18 618.17/ 454.65 76.56/ 1.50 401.48/ 138.32 Band3(R) 14.99/ 7.51 347.67/ 369.46 49.31/ 48.53 333.21/ 177.11 Band4(N-I) 21.01/ 4.15 670.38/ 314.87 192.52/ 85.91 1579.84/ 189.06 Radiation precision evaluation results show that in the 4 wavebands of blue, green, red and near-infrared, HJ1A-CCD1 is more sensitive to low radiance, and has a stronger capability to receive low radiance value than TM; in the blue and red wavebands, it also has a stronger capability to receive high radiance value than TM, from which we can conclude that HJ1A-CCD1 has a wider threshold value range than TM in the blue and red wavebands; it has a weaker capability to receive high radiance than TM in the green and near-infrared wavebands; from the aspects of radiance mean value and variance we can see that the radiance level of HJ1A-CCD1 is not as high as that of TM(Table3.). In particular, the fourth waveband of HJ has a much lower radiance mean value and variance than TM, which is closely related to the spectral response characteristics of the fourth waveband of HJ1A-CCD1; HJ1A-CCD1 presents an obvious decrease after the wave length of 0.83μm, which indicates that under the same solar radiation, after the wave length exceeds 0.83μm, HJ1A-CCD1’s capability to receive radiation energy will rapidly decrease (Figure2)

Table4.The correlation matrix of Landsat TM and HJ1A-CCD1 spectrum statistics TM \ HJ1A-CCD1 Band1 Band2 Band3 Band4 1.00 0.93 0.88 0.13 0.96 0.141 0.92 -0.01 0.22 0.26 Coefficient of correlation between wavebands also indicates that image data of various wavebands of HJ1A-CCD1 have a higher independence than Landsat TM, and also a smaller information redundancy. (Table4.)

Table5.The Definition and texture statistic Satellite sensor Definition Information Entropy HJ-1A-CCD1 Landsat-TM Band1 526.589 668.758 1.388 1.407 Band2 603.205 654.228 1.402 1.404 Band3 642.992 703.751 1.416 1.422 Band4 685.085 738.209 1.420 1.428 Texture and definition evaluation results show that both HJ1A-CCD1 and Landsat TM data are of the spatial resolution of 30m (actual sub-stellar point resolution of TM is 28.5m); however, from the perspective of imaging effect, the information amount, texture feature and definition of various wavebands of HJ1A-CCD1 data are not as good as Landsat TM data(Table5.),so when conducting discrimination and classification based on image texture and definition, the application effect of HJ1A-CCD1 data needs further analysis.

Thank you! O(∩_∩)O