CHARACTERISTICS OF REMOTELY SENSED IMAGERY. Radiometric Resolution

Similar documents
remote sensing? What are the remote sensing principles behind these Definition

An Introduction to Geomatics. Prepared by: Dr. Maher A. El-Hallaq خاص بطلبة مساق مقدمة في علم. Associate Professor of Surveying IUG

Introduction of Satellite Remote Sensing

COMPARISON OF INFORMATION CONTENTS OF HIGH RESOLUTION SPACE IMAGES

Remote Sensing and GIS

CHARACTERISTICS OF REMOTELY SENSED IMAGERY. Spatial Resolution

Introduction to Remote Sensing

Some Basic Concepts of Remote Sensing. Lecture 2 August 31, 2005

Lecture 6: Multispectral Earth Resource Satellites. The University at Albany Fall 2018 Geography and Planning

Remote Sensing Platforms

Remote Sensing Platforms

Remote Sensing 1 Principles of visible and radar remote sensing & sensors

9/12/2011. Training Course Remote Sensing Basic Theory & Image Processing Methods September 2011

NORMALIZING ASTER DATA USING MODIS PRODUCTS FOR LAND COVER CLASSIFICATION

746A27 Remote Sensing and GIS

Remote Sensing for Rangeland Applications

Spectral Signatures. Vegetation. 40 Soil. Water WAVELENGTH (microns)

The studies began when the Tiros satellites (1960) provided man s first synoptic view of the Earth s weather systems.

An Introduction to Remote Sensing & GIS. Introduction

Blacksburg, VA July 24 th 30 th, 2010 Remote Sensing Page 1. A condensed overview. For our purposes

Introduction to Remote Sensing Fundamentals of Satellite Remote Sensing. Mads Olander Rasmussen

RGB colours: Display onscreen = RGB

Atmospheric interactions; Aerial Photography; Imaging systems; Intro to Spectroscopy Week #3: September 12, 2018

Introduction to Remote Sensing

On the use of water color missions for lakes in 2021

Remote Sensing Exam 2 Study Guide

Introduction. Introduction. Introduction. Introduction. Introduction

Preparing Remote Sensing Data for Natural Resources Mapping (image enhancement, rectifications )

1. Theory of remote sensing and spectrum

Introduction to Remote Sensing

FOR 353: Air Photo Interpretation and Photogrammetry. Lecture 2. Electromagnetic Energy/Camera and Film characteristics

Satellite Imagery and Remote Sensing. DeeDee Whitaker SW Guilford High EES & Chemistry

John P. Stevens HS: Remote Sensing Test

Introduction to Remote Sensing Part 1

Geo/SAT 2 INTRODUCTION TO REMOTE SENSING

GIS Data Collection. Remote Sensing

Global hot spot monitoring with Landsat 8 and Sentinel-2. Soushi Kato Atsushi Oda Ryosuke Nakamura (AIST)

Ge111A Remote Sensing and GIS Lecture

The studies began when the Tiros satellites (1960) provided man s first synoptic view of the Earth s weather systems.

Govt. Engineering College Jhalawar Model Question Paper Subject- Remote Sensing & GIS

Interpreting land surface features. SWAC module 3

HYPERSPECTRAL IMAGERY FOR SAFEGUARDS APPLICATIONS. International Atomic Energy Agency, Vienna, Austria

Lecture Notes Prepared by Prof. J. Francis Spring Remote Sensing Instruments

Overview of how remote sensing is used by the wildland fire community.

Image interpretation I and II

Mod. 2 p. 1. Prof. Dr. Christoph Kleinn Institut für Waldinventur und Waldwachstum Arbeitsbereich Fernerkundung und Waldinventur

Lecture 2. Electromagnetic radiation principles. Units, image resolutions.

University of Texas at San Antonio EES 5053 Term Project CORRELATION BETWEEN NDVI AND SURFACE TEMPERATURES USING LANDSAT ETM + IMAGERY NEWFEL MAZARI

NON-PHOTOGRAPHIC SYSTEMS: Multispectral Scanners Medium and coarse resolution sensor comparisons: Landsat, SPOT, AVHRR and MODIS

Int n r t o r d o u d c u ti t on o n to t o Remote Sensing

Remote Sensing of Environment (RSE)

Lecture 13: Remotely Sensed Geospatial Data

Multi-Resolution Analysis of MODIS and ASTER Satellite Data for Water Classification

Digitization and fundamental techniques

Remote sensing in archaeology from optical to lidar. Krištof Oštir ModeLTER Scientific Research Centre of the Slovenian Academy of Sciences and Arts

Digital Imaging Rochester Institute of Technology

Textbook, Chapter 15 Textbook, Chapter 10 (only 10.6)

Hyperspectral Remote Sensing

Ge111A Remote Sensing and GIS Lecture

Introduction to Remote Sensing. Electromagnetic Energy. Data From Wave Phenomena. Electromagnetic Radiation (EMR) Electromagnetic Energy

(Refer Slide Time: 1:28)

Image interpretation. Aliens create Indian Head with an ipod? Badlands Guardian (CBC) This feature can be found 300 KMs SE of Calgary.

Basic Hyperspectral Analysis Tutorial

Chapter 8. Remote sensing

Remote Sensing. Measuring an object from a distance. For GIS, that means using photographic or satellite images to gather spatial data

REMOTE SENSING. Topic 10 Fundamentals of Digital Multispectral Remote Sensing MULTISPECTRAL SCANNERS MULTISPECTRAL SCANNERS

BASICS OF REMOTE SENSING

Copyrighted Material. Contents

Satellite Imagery Characteristics, Uses and Delivery to GIS Systems. Wayne Middleton April 2014

Looking at 637 nm VIIRS band, S-NPP

Land Cover Analysis to Determine Areas of Clear-cut and Forest Cover in Olney, Montana. Geob 373 Remote Sensing. Dr Andreas Varhola, Kathry De Rego

JP Stevens High School: Remote Sensing

Atmospheric Correction (including ATCOR)

Sources of Geographic Information

Railroad Valley Playa for use in vicarious calibration of large footprint sensors

Fundamentals of Remote Sensing

A (very) brief introduction to Remote Sensing: From satellites to maps!

Earth s Gravitational Pull

Final Examination Introduction to Remote Sensing. Time: 1.5 hrs Max. Marks: 50. Section-I (50 x 1 = 50 Marks)

Using Freely Available. Remote Sensing to Create a More Powerful GIS

2017 REMOTE SENSING EVENT TRAINING STRATEGIES 2016 SCIENCE OLYMPIAD COACHING ACADEMY CENTERVILLE, OH

366 Glossary. Popular method for scale drawings in a computer similar to GIS but without the necessity for spatial referencing CEP

A broad survey of remote sensing applications for many environmental disciplines

Introduction to Satellite Remote Sensing

SATELLITE OCEANOGRAPHY

Part 1: New spectral stuff going on at NIST. Part 2: TSI Traceability of TRF to NIST

earthobservation.wordpress.com

typical spectral signatures of photosynthetically active and non-photosynthetically active vegetation (Beeri et al., 2007)

How to Access Imagery and Carry Out Remote Sensing Analysis Using Landsat Data in a Browser

Processing Aster Data for Atmospheric Correction Geomatica 2014 Tutorial

Evaluation of FLAASH atmospheric correction. Note. Note no SAMBA/10/12. Authors. Øystein Rudjord and Øivind Due Trier

Remote Sensing 4113 Lab 08: Filtering and Principal Components Mar. 28, 2018

Outline. Introduction. Introduction: Film Emulsions. Sensor Systems. Types of Remote Sensing. A/Prof Linlin Ge. Photographic systems (cf(

ASTER and USGS EROS Emergency Imaging for Hurricane Disasters

Chapters 1-3. Chapter 1: Introduction and applications of photogrammetry Chapter 2: Electro-magnetic radiation. Chapter 3: Basic optics

Sensor resolutions from space: the tension between temporal, spectral, spatial and swath. David Bruce UniSA and ISU

to Geospatial Technologies

1 W. Philpot, Cornell University The Digital Image

Course overview; Remote sensing introduction; Basics of image processing & Color theory

MR-i. Hyperspectral Imaging FT-Spectroradiometers Radiometric Accuracy for Infrared Signature Measurements

Transcription:

CHARACTERISTICS OF REMOTELY SENSED IMAGERY Radiometric Resolution

There are a number of ways in which images can differ. One set of important differences relate to the various resolutions that images express. Resolution: the fineness of detail that can be distinguished in an image. Detail, however, can refer to several different dimensions. RESOLUTION?

Spatial Information Imagers Altimeters Sounders Temporal Information (Platformdependent) Spectral Information Spectrometers Polarimeters Scatterometers Radiometers SpectroRadiometers Intensity Information ELEMENTS OF RESOLUTION

HOW CAN IMAGES DIFFER?

Air photos: characteristics of emulsion of film (related to grain size). Digital images: number of data storage units, or bits, that the sensor has available to capture the range of energy or brightness levels. RADIOMETRIC RESOLUTION DEFINED

At the heart of any computer program or digital remote sensing system is the binary system (bits) that represents numeric values using two symbols, 0 or 1. In computing, word is the term for the natural unit of data used by a particular computer design. A word is simply a fixed-sized group of bits that are handled as a unit by the system. Common word sizes are 8 bits, 16, 32 or 64 bits. Landsat satellites Quickbird 1 1 1 1 1 1 1 1 1 1 1 2047 11 11 2048 BINARY? WORD?

SPECTRAL REFLECTANCE CURVES

RR is a measurement of how sensitive a sensor is to differences in energy (photons), or radiance values (reflectance). > the sensitivity = the finer/higher the radiometric resolution. Increasing radiometric resolution can improve the discrimination of features that have similar spectral responses, but slightly different reflectance levels. Resolution is a function of the analog-to-digital conversion. We also need to consider the sensor s Signal to Noise ratio. RADIOMETRIC RESOLUTION

A satellite sensor measures radiance at the sensor itself, not surface reflectance from the target. In other words, the sensor is only measuring the photon intensity when they hit the detector surface. If satellite instruments could measure surface reflectance, the task of interpreting images would be a lot easier, and classified land cover products would be much more accurate. SPECTRAL REFLECTANCE?

Surface reflectance is the ratio of the intensity of light reflected from a surface over the intensity of incident light. Unfortunately, the orientation of the surface feature (usually due to slope and aspect), bidirectional reflectance, and atmospheric scattering and absorption complicate our ability to accurately measure surface reflectance. SPECTRAL REFLECTANCE?

TOA VERSUS ATMOSPHERICALLY- CORRECTED SPECTRUMS.

So, although we refer to spectral reflectance curves, they are primarily pedagogical tools since the satellite sensor isn t actually recording the spectral reflectance of the object per se. We hope / anticipate that the radiance values recorded by the sensor act as useful surrogates for the actual reflectance values. SPECTRAL REFLECTANCE CURVES

Output [0 255] Output [0,1,2,3] Output [0,1] % Reflectance Input [0 100%] Sensors convert (quantize) the continuous values into integer values, the range of which depends on the number of bits being used by the sensor. RADIANCE MAPPING }

4 8 bit 16 bit BITS PER PIXEL

How many different shades of gray can we distinguish? Typically it is stated that we can only distinguish 16 levels of grey, although some say that we can distinguish up to 30, but we also know that unless a (black & white) photo is scanned using 256 shades of gray, it doesn t look right. A computer, of course, can distinguish every unique colour or shade of gray. Colour images: How many colour values are possible in a 3 colour, 3 band Landsat image? 2 8 x 2 8 x 2 8 = 256 x 256 x 256 = >16 million THE VALUE OF NUMBERS

A DEM represented using 2, 4, 8 and over 256 colours THE NUMBER OF VALUES

8-bit radiometric resolution 2 8 = 256 levels per colour 3-bit radiometric resolution 2 3 = 8 levels per colour RADIOMETRIC RESOLUTION

Landsat 3: 6 bits Spot, Landsat (after 3): 8 bits Ikonos, Quickbird: 11 bits ASTER VNIR and SWIR: 8 bits; TIR: 12 bits Often the quantization values aren t reported or easily determined (e.g.). TYPICAL QUANTIZATION VALUES

Standards for storing and processing digital images can be different than the radiometric resolution of data Example Quickbird satellite: 11 bit radiometric resolution provided as 8 bit or 16 bit 8 bit: shadows may appear black 16 bit: detail is visible in shadows due to small differences recorded in wavelength reflectance 8 bit 16 bit DIGITAL STORAGE AND DISPLAY

Thermal resolution is often described in terms of the NETD (Noise Equivalent Temperature Difference), or the MRTD (Minimum Resolvable Temperature Difference). Both of these criteria refer to the ability of the system to detect a small change in temperature of an object in the field of view. For the GOES 1-M sensor, the resolution is about 1K For MODIS, it varies by band NASA Terra satellite image of San Diego wildfires. Red pixels indicate fire activity WHAT OF THERMAL (IR) SENSORS RADIOMETRIC RESOLUTION?

Radiometric resolution determines the range of radiance values that can be discerned from an image. The higher the quantization rate, the finer the distinctions that can be made. With the hyper radiometric resolutions now available from some sensors, we are able to discern details in areas that previously were too dark (or too bright). SUMMARY URL