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Notes on Ch. 9 & 10Satellite Mapping of Earth Resources and Earth’s Atmosphere and Water Resources,[object Object],1,[object Object]
Natural resource analysis has never had a high priority in satellite funding.,[object Object],Highest priorities: Defense, National Security, Communications, Commercial, Weather.,[object Object],A great deal of analysis has been done with limited resources.,[object Object],The CIA and Pentagon have the best toys.,[object Object],2,[object Object],Some Remarks,[object Object]
Started in 1972.,[object Object],First called ERTS (Earth Resource Technology Satellite) Figure 9-1 Landsat vehicles.,[object Object],System designed to follow a specific orbit that would bring it back over the same locus on the Earth’s surface, thereby providing repetitive coverage to monitor change through time. See Figure 9-2.,[object Object],Returns to a specific location every 18 days.,[object Object],3,[object Object],Landsat,[object Object]
Primary tool of Landsat.,[object Object],Records reflected and/or radiated energy from the Earth simultaneously in four contiguous bands of the EMS.,[object Object],Provides multiple data sets to produce geographically registered images (one for each band).,[object Object],Each scene covers 115 miles by 115 miles (185km) in the shape of a parallelogram. ,[object Object],Overlap provided between scenes.,[object Object],4,[object Object],Multispectral Scanning System (MSS),[object Object]
Differences in the bands sensed between the different LandsatS. See Figure 9-3.,[object Object],The bands on the MSS can be selected to give the same results as Color Infrared Film (CIR),[object Object],5,[object Object],MSS (continued),[object Object]
Picture element.,[object Object],The smallest area on the ground that is detected by a sensor.,[object Object],A general measure of the sensitivity of a digital scanner,[object Object],The MSS on the first three Landsats could detect a minimum of 79 sq. meters. The value recorded is the average reflectance for the pixel.,[object Object],6,[object Object],Pixel,[object Object]
This is a fairly coarse density.,[object Object],To see an object on MSS it should normal be about twice the width of a pixel. Objects with great contrast can be seen at single pixel density.,[object Object],MSS data needs extensive processing to create a useful image.,[object Object],7,[object Object],Pixel (continued),[object Object]
Starting on Landsat 4 a new scanner.,[object Object],Offered increased ground resolution, a greater number of spectral bands, and faster return time to image a particular Earth surface location (16 days vs. 18),[object Object],Spectral bands modified to improve detection of soil, rock , and vegetation.,[object Object],Ground resolution improved to 30meters,[object Object],8,[object Object],Thematic Mapper (TM),[object Object]
Assigning the reflectance values of data from sensed bands to the standard red, green, and blue layers of color film using filters.,[object Object],A common technique with satellite data.,[object Object],9,[object Object],False Color Images,[object Object]
A European (French) natural resource satellite,[object Object],Système Pour L’Observation de la Terre,[object Object],Started in 1977. SPOT 1 launched in 1986.,[object Object],First big job: acquiring images of the Chernobyl accident in the Soviet Union in May.,[object Object],10,[object Object],SPOT,[object Object]
Orbital path similar to Landsat. Sunsynchronous (passing over the same latitude at the same local time). Required 26 days to return to the same location.,[object Object],Has higher resolution than Landsat, but the area of one scene is much smaller.,[object Object],11,[object Object],SPOT (continued),[object Object]
Panchromatic: 0.5 to 0.73 micrometers. See EMS on Fig. 3-1. Ground resolution of 10m squared.,[object Object],Multispectral: 0.5-0.59 green, 0.61 to 0.68 red, and 0.79 to 0.89 micrometers IR. Pixel resolution 20m squared.,[object Object],Adjustable viewing angle 27o east or west of the orbital path. Allows for the creation of stereo pairs.,[object Object],12,[object Object],Sensors on SPOT,[object Object]
Large format camera on Space Shuttle. Multi-camera system to provide cartographic quality images. Can exactly locate position on earth’s surface and the nadir of the image.,[object Object],Shuttle hand-held photography.,[object Object],Advantages and Disadvantages of imagery from manned flights???,[object Object],13,[object Object],NASA Manned Flight Images,[object Object]
http://earthobservatory.nasa.gov/,[object Object],Landsat program home page: http://landsat.gsfc.nasa.gov/,[object Object],SPOT http://www.spot.com,[object Object],14,[object Object],Web Links,[object Object]
Weather forecasting. (fire fighting),[object Object],Climate changes,[object Object],Pollution and particulate matter.,[object Object],Figure 10-1 and 2. Satellites and sensing tools.,[object Object],15,[object Object],Satelite mapping of Earth’s Atmosphere and Water Resources,[object Object]
Most of these satellites focus on the visible, reflected IR, and thermal IR portions of the EMS. Fig. 10-3 shows the transmission windows.,[object Object],Types of operational satellites (Figure 10-4):,[object Object],Polar orbiters- follows path roughly parallel to the earth’s axis from pole to pole.,[object Object],Geostationary – orbit and speed that positions them above any point on the Earth where they maintain position constantly,[object Object],16,[object Object],Spectral Bands Utilized,[object Object]
Known by acronym GOES – Geostationary Operational Environmental Satellite. Several in service since 1975,[object Object],Day-night capability. Sensor is VISSR – Visible-Infrared Spin-Scan Radiometer). Records energy in:,[object Object],One visible band: 0.55 – 0.70 microns,[object Object],Thermal IR 10.5 – 12.5 microns,[object Object],17,[object Object],Geostationary Weather Satellites ,[object Object]
Figure 10-7 full disc visible image of part of the earth and its cloud cover,[object Object],All clouds at any elevation show up in this image. ,[object Object],Allows nephanalysis – the study of cloud patterns and formations.,[object Object],18,[object Object],GOES continued,[object Object]
Figure 10-8 full disc infrared image.,[object Object],Images have geographic grid of meridians and parallels and continent and political boundaries,[object Object],Full disc IR shows thermal values for land, water, and clouds.,[object Object],Polarity of gray tones shows warmer temperatures as dark and colder temperatures as light. ,[object Object],Coldest, highest clouds are white. Lower clouds dark. Most unstable clouds most visible.,[object Object],19,[object Object],GOES continued,[object Object]
The visible and thermal IR images combined give good cloud information. Can be compared day to day.,[object Object],Comparing areas with or devoid of clouds can show high pressure and low pressure areas.,[object Object],Water vapor imagery. Uses energy radiated in the 6.7 micron band. At this wavelength the radiation is absorbed and reradiated by water in the gaseous state.,[object Object],GOES satellite viewer: http://www.goes.noaa.gov/,[object Object],NOAA Weather forecast for Mont Alto, PA,[object Object],20,[object Object],GOES continued,[object Object]
Numerous satellites and scanners have been used to sense environmental data since 1060,[object Object],NESDIS http://www.nesdis.noaa.gov/,[object Object],Some of the products include:,[object Object],Temperature soundings in the atmosphere,[object Object],Ice analysis in the polar regions and Great Lakes,[object Object],Vegetation index ,[object Object],Snow cover ,[object Object],Tropical cyclones,[object Object],Wildfires,[object Object],21,[object Object],Polar Orbiter Satellites,[object Object]

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Satellite Mapping

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