VERIFICATION PLAN OF OCEAN COLOR AND TEMPERATURE SCANNER ATMOSPHERIC CORRECTION AND PHYTOPLANKTON PIGMENT BY MOORED OPTICAL BUOY SYSTEM

Citation
M. Kishino et al., VERIFICATION PLAN OF OCEAN COLOR AND TEMPERATURE SCANNER ATMOSPHERIC CORRECTION AND PHYTOPLANKTON PIGMENT BY MOORED OPTICAL BUOY SYSTEM, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D14), 1997, pp. 17197-17207
Citations number
17
Categorie Soggetti
Metereology & Atmospheric Sciences
Volume
102
Issue
D14
Year of publication
1997
Pages
17197 - 17207
Database
ISI
Abstract
A moored optical buoy system has been developed by the National Space Development Agency of Japan (NASDA) for verification of ocean-observin g remote sensing sensors of the Advanced Earth Observing Satellite (AD EOS). An underwater spectral radiometer was specifically designed for this optical system. The two upward radiance and downward irradiance c orrectors were connected with fiber optical system and were placed at the depth of 1.5 m and 6.5 m. The collector parts of the radiometer we re extended from the center of the buoy system in order to avoid self shading with 3 m and 1.2 m arms at the depth of 1.5 m and 6.5 m, respe ctively. Spectral incident irradiance was measured at top of the buoy system. Phytoplankton pigment concentrations were monitored by Aquatra cka-III fluorometer placed at the bottom of the surface float. Atmosph eric temperature, pressure, humidity, wind speed and direction, water temperature at a depth of 1.2 m and 6.5 m, and wave height and directi on were also monitored. In this paper, we present results from test de ployment during January 16 to March 15, 1995, in the Suruga Bay, off S hizuoka, Japan, and compare the water-leaving radiance obtained by buo y with one observed by ship. The chlorophyll a concentrations calculat ed from water-leaving radiance were also compared with chlorophyll flu orescence measured by fluorometer. It was proved that the self shading and wind affected the radiance and irradiance in the sea. It becomes clear that the quality check of the buoy data is very important for ve rification of the satellite data. We present also the verification pla n of atmospheric correction and phytoplankton pigment for ADEOS/ocean color and temperature scanner (OCTS) using the sea truth data obtained from this buoy system and ships.