by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory in Boulder, Colo .
Written in English
|Statement||A.J. Palmer, M.V. Trevorrow.|
|Series||NOAA technical memorandum ERL ETL -- 280.|
|Contributions||Environmental Technology Laboratory (Environmental Research Laboratories)|
|The Physical Object|
|Pagination||iii, 14 p.|
|Number of Pages||14|
Jul 20, · Delta-k-lidar sensing of the ocean surface. Palmer AJ. A new lidar technique for detecting ocean surface waves is analyzed theoretically. The method is based on the Deltak-radar technique and detects the modulation of the low-frequency product of two Cited by: 8. Surface waves play a central role in many oceanic and atmospheric processes as well as in remote sensing and probing of the ocean surface by instruments. . Ocean Current Estimated From X-Band Radar Sea Surface Images Article in IEEE Transactions on Geoscience and Remote Sensing 40(4) · May with Reads How we measure 'reads'Author: Rune Gangeskar. The Mars Climate Orbiter was a kilogram robotic space probe launched by NASA on December 11, to study the Martian climate, Martian atmosphere, and surface changes and to act as the communications relay in the Mars Surveyor'98 program for.
GMTI Publications All publications sorted by Thesis resulting from the effective ocean surface currents but also from effects like e. g. orbital motions of longer waves. Thus the actual surface ocean currents differ from the measured interferometric velocities. The processed ATI phase is the starting point for the determination of. online version of the program book. Please click the following link to download and install: When you are finished installing, please return to this window and PRESS. This banner text can have markup.. web; books; video; audio; software; images; Toggle navigation. The ATI phase being directly proportional to the interferometric velocity contains not only contributions resulting from the effective ocean surface currents but also from effects like e. g. orbital motions of longer waves. Thus the actual surface ocean currents differ from the measured interferometric velocities.
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