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Nakayama, Masashige,Nishio, Fumihiko,Tanikawa, Tomonori,Cho, Kohei,Shimoda, Haruhisa 대한원격탐사학회 1999 International Symposium on Remote Sensing Vol.15 No.1
It is very important for monitoring the interannual variability of sea ice extents in the Okhotsk Sea because the glabal warming has firstly appeared around the Okhotsk Sea, locating around the southernmost region of sea ice cover in the Northern Hemisphere. In order to develop the sea ice concentration algorithm by microwave sensors onboard satellite, electromagnetic properties of sea ice in the Okhotsk Sea, therefore, were observed by airborne microwave radiometer (AMR), which has the same frequencies as AMSR (Advanced Microwave Scanning Radiometer), ADEOS-II, launching on November, 2000. On this study, it is discussed how to make the image of AMR-EFOV and the video image with nadir angle under flight at the same time, and superimpose the brightness temperature data by AMIt-EFOV on the video mosaiced images. For comparing SPOT image, it is clearly that the variation of brightness temperature is small in 89GHz V-pol without the sea ice types and increase at the lower frequency-band.