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RSSJ
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Chapter 4 Water Applications
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Typical remote sensing reflectance from the ocean a: waters with very high SS and CDOM b: high SS and CDOM c: moderate SS, CDOM, and some phytoplankton d: clear water e: moderate chlorophyll and SS f: moderate chlorophyll
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Water quality (chlorophyll-a concentration ) distributions in the Lake Biwa and the Ise Bay (top). Water qualities (Turbidity and chlorophyll-a concentration) in the Lake Tega-numa (bottom)
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Primary production derived by the model using three variables (a) Sea surface temperature (b) Chlorophyll-a concentration (c) Photosynthetically available radiation (d) Primary productivity H: High value L: Low value
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Oil spill distribution on May 23, 2010 observed by PALSAR in the Gulf of Mexico
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Warm eddies off the Sanriku observed by thermal infrared images by AVHRR (a) June 10, 1982 (b) August 15, 1982
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Monthly mean sea surface temperatures along the equatorial Pacific from 1996.11 to 1997.6 observed by OCTS on ADEOS
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Sea surface temperature of the Sendai Bay on 2003.05.02 by MODIS on Terra
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Lights observed by satellite borne sensor
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Spectral reflectance of coral reef and algae with spectral bands of Landsat ETM+ A typical spectral property of coral reef is indicated by the arrow. This spectral property is missing when the spectrum within a relatively broad band of a multispectral sensor is averaged. Bleached coral reefs can be differentiated from healthy coral reefs or seaweeds because of a high spectral reflectance.
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The Shiraho Coral reef and its classification The distribution of coral reefs and others is ambiguous with a lower spatial resolution, as information from coral reef and bottom properties are mixed. IKONOS image with a spatial resolution of 4 m Landsat ETM+ image with a spatial resolution of 30 m
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Sea ice extent (white areas) on September 16, 2007 and a median of sea ice distribution in September from 1979 to 2000 (a purple line polygon)
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Sea ice concentration in the Sea of Okhotsk on February 24, 2010
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Wind speed and direction around Typhoon 0310 in the east off Taiwan observed by the SeaWinds microwave scatterometer on ADEOS-II at 02:09Z on August 6, 2003
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Wave patterns observed by a synthetic aperture radar
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Sea surface height in the North Pacific on January 7, 2009
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Surface currents estimated from the sea surface height observed by microwave altimeters on January 5, 2005
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Missions for sea surface salinity (top) SMOS by ESA (bottom) Aquarius by NASA
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L-band (1.413 GHz) brightness temperature as a function of sea surface temperature and salinity for vertical (top) and horizontal polarizations (bottom)
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Algorithm to predict potential fishing fields A fishing model is generated from satellite data and catch data.
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Prediction map of potential fishing field for monthly mean and real fishing fields (white circle)
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Flow chart to extract possible reproduction areas
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Possible reproduction areas of sagittated calamari in February (Red areas in the ocean)
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Mapping the most suitable areas for scallops aquaculture
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Analysis of infrastructure by high resolution satellite data
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Model for appropriate scallops aquaculture (suitability of 8 levels)
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