Observations of suspended particle patterns in nearshore northeastern Pacific Ocean waters by ERTS-1 imagery
ERTS-1 imagery of sediment suspension in nearshore northeastern Pacific Ocean waters
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ERTS-1 imagery of sediment suspension in nearshore northeastern Pacific Ocean waters
ERTS-1 imagery of ocean currents in Gulf of Mexico
ERTS-1 imagery for commercial fishing management in northeastern Gulf of California
ERTS-1 imagery for commercial fishing information in Mississippi Sound
Comparison of multispectral imagery and aerial surveys of Massachusetts bays
ERTS-1 imagery for water depth estimation around Great Bahama Bank
Natural resource inventory and monitoring in Oregon with ERTS-1 imagery
Preliminary test of ERTS-1 imagery for improving definition of natural streamflow, using two basins in Chesapeake Bay area
Application of ERTS-1 imagery to flood inundation mapping in East and West Nishnabotna basins of southwestern Iowa
Flood damage assessment in southeastern Arizona (near upper Gila River) using ERTS-1 imagery
SRI satellite image analyzer console for mapping southern Arizona plant communities from ERTS-1 imagery
Hydrologic studies of Lake Ontario basin using high altitude and ERTS-1 imagery
ERTS-1 imagery for mapping and detecting changes in snow cover on land and glaciers
Detection of turbidity dynamics in Tampa Bay, Florida using multispectral imagery from ERTS-1
The author has identified the following significant results. The most important result to date is the demonstration of the special value of repetitive ERTS-1 multiband coverage for detecting previously unknown fracture lineaments despite the presence of a deep glacial overburden. The Illinois Basin is largely covered with glacial drift and few rock outcrops are present. A contribution to the geological understanding of Illinois and Indiana has been made. Analysis of ERTS-1 imagery has provided useful information to the State of Indiana concerning the surface mined lands. The contrast between healthy vegetation and bare ground as imaged by Band 7 is sharp and substantial detail can be obtained concerning the extent of disturbed lands, associated water bodies, large haul roads, and extent of mined lands revegetation. Preliminary results of analysis suggest a reasonable correlation between image-detected fractures and mine roof fall accidents for a few areas investigated. ERTS-1 applications to surface mining operations appear probable, but further investigations are required. The likelihood of applying ERTS-1 derived fracture data to improve coal mine safety in the entire Illinois Basin is suggested from studies conducted in Indiana.
The author has identified the following significant results. A reconstituted, simulated color-infrared ERTS-1 image covering the western Seward Peninsula was prepared and it is used for identifying and mapping vegetation types by direct visual examination. The image, NASA ERTS E-1009-22095, was obtained approximately at 1110 hours, 165 degrees WMT on August 1, 1972. Seven major colors are identified. Four of these are matched with units on existing vegetation maps: bright red - shrub thicket; light gray-red - upland tundra; medium gray-red - coastal coastal wet tundra; gray - alpine barrens. The three colors having no map equivalents are tentatively interpreted as follows: pink - grassland tundra; dark gray-red - burn scars; light orange-red - senescent vegetation. A vegetation map, drawn by tracing on an acetate overlay of the image is presented. Significantly more information is depicted than on existing maps with regards to vegetation types and their areal distribution. Furthermore the preparation of the new map from ERTS-1 imagery required little time relative to conventional methods and extent of areal coverage.
The author has identified the following significant results. Two ancient watercourses have been observed on ERTS-1 imagery. These lie in the Waterpocket Fold area, north of the Marble Canyon section of the Colorado River, in Arizona and Utah. A third old watercourse of interest is an ancient canyon of the Colorado and is located on image no. 1156-17260. Image no. 1051-17414 contains some very useful information concerning the hydrology, sedimentology, and biology of Great Salt Lake and Bear Lake in Utah. In Great Salt Lake, there is a sharp line between the portion of the lake north of the railroad causeway and that south of the causeway. There is a marked difference in salinity across the causeway, and this is reflected in different algal species. On the same image, sediment plumes in Bear Lake clearly delineate the circulation pattern, and provide excellent indications of bottom contours over much of the area. Image no. 1051-17420 contains part of Great Salt Lake and all of Utah Lake. The latter displays a very interesting surface pattern which is probably due to an algal bloom which has been swirled into a spiral by the circulation of the lake.
The author has identified the following significant results. Initial imagery from the first ERTS indicates that satellite-acquired data is of value in determining the location and extent of range fire in the Sand Hills region of Nebraska. Preliminary results suggest that it can also provide a tool for monitoring soil erosion by wind and evaluating the recovery of vegetation in burned areas.