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Titlebook: Introduction to satellite oceanography; G. A. Maul Book 1985 Martinus Nijhoff Publishers, Dordrecht 1985 Ocean.Oceanography.Orbit.remote s

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發(fā)表于 2025-3-21 19:23:23 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Introduction to satellite oceanography
編輯G. A. Maul
視頻videohttp://file.papertrans.cn/475/474343/474343.mp4
叢書名稱Remote Sensing of Earth Resources and Environment
圖書封面Titlebook: Introduction to satellite oceanography;  G. A. Maul Book 1985 Martinus Nijhoff Publishers, Dordrecht 1985 Ocean.Oceanography.Orbit.remote s
描述Satelli te oceanography, as the term is used in this book, is a generic term that means application of the technology of aerospace electromagnetic remote sensing to the study of the oceans. The key words here are "application of technology ??. to the study of the oceans." The goal is to learn more about our planet‘s hydrosphere. As such, remote sensing technology is another tool in the oceanographer‘s sea bag, just like a bathythermograph or a plankton net. But is a whole book necessary if remote sensing is just another tool? While it is true that no one has written a whole book on plankton nets, volumes have been written about what is found in those nets. Today‘s state-of-the-art measurements from spacecraft or aircraft first must be interpreted in terms of their physics; then the interpretations must be understood in terms of oceanic processes. This is not materially different from the analogy to Ii plankton net; marine biolo- gists still argue about what didn‘t get caught in the net.
出版日期Book 1985
關鍵詞Ocean; Oceanography; Orbit; remote sensing; satellite; temperature; remote sensing/photogrammetry
版次1
doihttps://doi.org/10.1007/978-94-009-5061-0
isbn_softcover978-94-010-8740-7
isbn_ebook978-94-009-5061-0
copyrightMartinus Nijhoff Publishers, Dordrecht 1985
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 21:04:26 | 只看該作者
Remote Sensing of Earth Resources and Environmenthttp://image.papertrans.cn/i/image/474343.jpg
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Introduction to Ocean Remote Sensing, surface topography. NOAA/TIROS is an operational meteorological satellite with sensors that can measure sea surface temperature, and locate Lagrangian drifters. NROSS, the Navy Remote Ocean Sensing System, is planned by the U.S. Navy with instruments for measuring surface winds, sea surface topogra
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Physics of Radiation,ia on the left; obtained by NOAA-4. Lower panel is a radar image of the Beaufort Sea obtained from the synthetic aperture radar on SEASAT. Spatial resolution of the upper panel is approximately one kilometer, and was obtained by measuring reflected sunlight. The lower panel has a spatial resolution
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發(fā)表于 2025-3-22 13:12:52 | 只看該作者
Infrared Remote Sensing,ssed into maps of global surface temperature for scientific analysis. The upper panel shows surface temperatures for January 1979, the middle panel for July 1979, and the bottom panel shows the difference from January to July. The original maps are produced in color using red to indicate warm temper
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發(fā)表于 2025-3-22 18:48:56 | 只看該作者
Visible Remote Sensing,how variations in ocean color that are correlated with phytoplankton abundance. The original image uses reds and oranges for higher productivity zones, and shades of blue for zones of lower productivity. This reproduction of the original off the central California coast shows higher abundance near t
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Microwave Remote Sensing,ions due to gravity are typically 100 times larger than due to currents. The upper panel shows the mean sea surface topography from the SEASAT altimeter, computer processed to show variations as if illuminated from the northwest. The numbers identify major features such as trenches, fracture zones,
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發(fā)表于 2025-3-23 04:28:26 | 只看該作者
Book 1985preted in terms of their physics; then the interpretations must be understood in terms of oceanic processes. This is not materially different from the analogy to Ii plankton net; marine biolo- gists still argue about what didn‘t get caught in the net.
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發(fā)表于 2025-3-23 05:46:32 | 只看該作者
t be interpreted in terms of their physics; then the interpretations must be understood in terms of oceanic processes. This is not materially different from the analogy to Ii plankton net; marine biolo- gists still argue about what didn‘t get caught in the net.978-94-010-8740-7978-94-009-5061-0
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