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Remote Sensing of the Land Surface: High Spatial Resolution. Michael D. King & Compton J. Tucker Outline Land remote sensing at high spatial resolution Satellite sensors enabling remote sensing of land cover at high spatial resolution Landsat RBV, MSS, TM, ETM+ Spot HRV Terra ASTER
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Remote Sensing of the Land Surface:High Spatial Resolution Michael D. King & Compton J. Tucker Outline • Land remote sensing at high spatial resolution • Satellite sensors enabling remote sensing of land cover at high spatial resolution • Landsat RBV, MSS, TM, ETM+ • Spot HRV • Terra ASTER • Orbital characteristics • Instrument characteristics • Spacecraft, spatial resolution, swath width, sensor characteristics, and unique characteristics • Land properties as observed by Landsat and ASTER
Definition of Orbital Period of a Satellite The orbital period of a satellite around a planet is given by where T0 = orbital period (sec) Rp = planet radius (6380 km for Earth) H¢ = orbit altitude above planet’s surface (km) gs = acceleration due to gravity (0.00981 km s-2 for Earth)
Landsat-1, -2, and -3 Observatory Configuration Solar array Multispectral Scanner (MSS) Data collection antenna Return Beam Vidicon (RBV) cameras
Spectral Sensitivity of the Four Landsat MSS Bands • Bands compared with the spectral sensitivity of the three emulsion layers used in color and color infrared film
Band 2 Band 5 Band 7 Band 4 Band 3 Band 1 Landsat 5 TM Landsat 7 ETM+ EO-1 ALI EO-1 Hyperion Bare soil Senescent vegetation Green Vegetation
Landsat-4 and -5 Observatory Configuration High gain antenna Multispectral Scanner (MSS) Solar array S-band antenna Thematic Mapper (TM)
Thematic Mapper Optical Path and Projection of Detector IFOVs on the Earth’s Surface
Schematic of TM Scan Line Correction Process (a) Uncompensated scan lines (b) Correction for satellite motion (c) Compensated scan lines
Side-Lap Composting, no interpolation
Side-Lap Composting, no interpolation
Multi-pass compositing, no Interpolation Before After
Landsat’s Bands • Landsat collects monochrome images in each band by measuring radiance & reflectance in each channel. When viewed individually, these images appear as shades of gray
Color Composites • The human eye is not sensitive to ultraviolet or infrared light • To build a composite image from remote sensing data that makes sense to our eyes, we must use colors from the visible portion of the EM spectrum—red, green, and blue
‘True Color’ Landsat TM Image • This image was produced using the red, green, & blue bands from Landsat’s Thematic Mapper • Note the washed out appearance of the landscape due to atmospheric effects R = 0.66 µm G = 0.56 µm B = 0.48 µm
“False Color” Landsat Image Channels 4, 3, 2 Channels 5, 4, 2 • These images were produced using near-infrared, red, and green bands • Notice how vegetation is more clearly distinguished from nonvegetation
Landsat 7 Launched April 15, 1999
Enhanced Thematic Mapper Plus (ETM+) • NASA & USGS, Landsat 7 • launched April 15, 1999 • 705 km polar orbit, descending (10:00 a.m.) • Sensor Characteristics • 7 spectral bands ranging from 0.48 to 11.5 µm • 1 panchromatic band (0.5-0.9 µm) • cross-track scan mirror with 185 km swath width • Spatial resolutions: • 15 m (panchromatic) • 30 m (spectral) • Calibration: • 5% reflectance accuracy • 1% thermal IR accuracy • onboard lamps, blackbody, and shutter • solar diffuser
Thematic Mapper Optical Path and Projection of Detector IFOVs on the Earth’s Surface
Landsat 7 Goals & Objectives • Land use and land cover change • Agricultural evaluations, forest management inventories, water resource estimates, coastal zone appraisals • Growth patterns of urban development, Spring run-off contaminants in lakes, land use in tropical rainforests, health of temperate conical forests, mapping wildfire hazards in Yosemite • Vegetation patterns • Annual cycle of vegetation dynamics, drought stress, and flooding • Dune reactivation in the US Great Plains, precision farming and land management • Glaciers and snow cover • Growth and retreat • Gradual changes in the Antarctic ice sheet • Geological surveys • Volcanic hazards and lava lakes
Chesapeake & Delaware Bays R = 0.66 µm G = 0.56 µm B = 0.48 µm May 28, 1999 Baltimore Washington
Benefits of Landsat 7 over other Missions • Mission Continuity • Spanning 25 years of multispectral imaging of the Earth’s surface, starting in 1972 • Global Survey Mission • Approximately one quarter of the Earth’s landmass is imaged every 16 days • Every landmass will have seasonal coverage • Affordable Data Products • Landsat 7 data products are available from the EROS Data Center • Prices dropped from approximately $5,000 (Landsat’s 4 & 5) to $600 (Landsat 7) per scene
Washington, DC Landsat 5 Infrared band Landsat 7 panchromatic band 1991 1999
Washington, DC Detail Landsat 5 Infrared band Landsat 7 panchromatic band 1991 1999
Phoenix Development and Growth:1973-1992 Multispectral Scanner (MSS)
San Francisco Bay from Landsat 7 R = 0.66 µm G = 0.56 µm B = 0.48 µm Bay Bridge Golden Gate Bridge Oakland Airport
Cape Canaveral R = 0.66 µm G = 0.56 µm B = 0.48 µm
Flood of the Mississippi River in 1993 Landsat 5 TM Before the floods After the floods
Flood of the Limpopo River in Mozambique • The Limpopo River in Mozambique before and after the flooding from Cyclone Eline • About 700 people were killed and thousands were displaced by this event Landsat 7 ETM+ August 22, 1999 March 2, 2000
Bolivia from Landsat: 1984-1998 Thematic Mapper R = 2.21 µm G = 0.83 µm B = 0.56 µm Garden of the Gods Country Club Colorado College