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Juan de Dios Barrios, M.S. Research Associate Nick J. Rahall Appalachian Transportation Institute and James O. Brumfield, Ph. D. College of Science Marshall.

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Presentation on theme: "Juan de Dios Barrios, M.S. Research Associate Nick J. Rahall Appalachian Transportation Institute and James O. Brumfield, Ph. D. College of Science Marshall."— Presentation transcript:

1 Juan de Dios Barrios, M.S. Research Associate Nick J. Rahall Appalachian Transportation Institute and James O. Brumfield, Ph. D. College of Science Marshall University November, 9, 2008 Historical Landsat Images for Rivers and Streams

2  Geographic Information Systems Computer software tools for analyzing geo- referenced spatial data.  Remote Sensing Systems Sensor Systems used to collect information some remote distance from the subject.  Global Positioning Systems Earth Orbital Satellites Systems used to determined position on the earth’s surface. Water Dynamics Workshop, November 2008. Burlington Vermont

3  The power of Geospatial Sciences is based in the capability to integrate different geospatial data into a comprehensive geoanalytical system.  This can result in the development of proper applications for scientific, social and cultural models. Water Dynamics Workshop, November 2008. Burlington Vermont

4  A historical record of the Earth’s land surface from July 1972 to July1976.  First Satellite, Landsat I Launched 7/23/1972 Named Earth Resources Technology (ERTS-1). Later NASA changed the name to Landsat 1  Second Satellite, Landsat II Launched 7/22/75 Named Earth Resources Technology (ERTS-B). Later NASA changed the name to Landsat 2 Water Dynamics Workshop, November 2008. Burlington Vermont

5  Altitude 920 Km  18 day coverage  185 km wide image swaths  Sun-synchronous Crossing times  Landsat 1 8:30 am  Landsat 2 9:00 am With Landsat I and II operational 9 day imaging cycles Water Dynamics Workshop, November 2008. Burlington Vermont

6 Landsats I and II  Return Beam Vidicon (RBV) RBV did not have film down linked to ground receiving stations  Multispectral Scanner (MSS) down linked to ground receiving stations stored on tape and converted to scanned film. Water Dynamics Workshop, November 2008. Burlington Vermont

7  Four Bands Green 0.5-0.6 µm. Red0.6-0.7 µm. Infrared0.7-0.8 µm. Infrared 0.8-1.1 µm. Water Dynamics Workshop, November 2008. Burlington Vermont

8

9 Band 1 (Green)  Healthy vegetation Band 2 (Red)  Chlorophyll Water Dynamics Workshop, November 2008. Burlington Vermont

10 Near Infrared  Healthy green vegetation  Water lands Water Dynamics Workshop, November 2008. Burlington Vermont

11  In a Near Infrared, Red and Green (false color) combination Water bodies appear brown to blue to black in color. Deep clear water appears dark blue to black in color, while sediment-laden or shallow waters appear lighter in color. Urban areas appear blue-gray in color. Water Dynamics Workshop, November 2008. Burlington Vermont

12 BAND FIVEBAND SIX Water Dynamics Workshop, November 2008. Burlington Vermont

13 N 37-05 W088-53 Water Dynamics Workshop, November 2008. Burlington Vermont

14 BAND FOURBAND FIVE Water Dynamics Workshop, November 2008. Burlington Vermont

15 N39-02 w091-09 Water Dynamics Workshop, November 2008. Burlington Vermont

16  Marshall University College of Science has access to imagery from July 1972 to July 1976 of Landsat I and Landsat II providing an opportunity for global coverage.  Only selected digital information is available in the form of tiff files.  Availability of data is currently under evaluation.  The data can be made available for educational research or academic uses. Water Dynamics Workshop, November 2008. Burlington Vermont

17 Juan de Dios Barrios barrios1@marshall.edu


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