• 한국광학회지
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• 제15권4호
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• pp.325-330
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• 2004

진공자외선 파장영역에서 광학부품의 분광특성을 측정할 수 있는 중수소광원과 진공단색화장치, 시료챔버 및 광 검출기 구조의 진공자외선 분광반사율계를 제작하였다. 제작된 진공자외선 분광반사율계는 115nm∼330 nm의 분광영역에서 약 3.0${\times}$$10^{-4}$ Pa의 기압에서 작동하였다. 253.652 nm와 184.95 nm의 수은 선스펙트럼으로 진공단색화장치의 파장을 교정하여 그 분해능이 0.012 nm이고, 파장정확도가 $\pm$0.03 nm 임을 확인하였다. 중수소 광원을 이용하여 115 nm∼230 nm 파장대역의 진공자외선 영역에서 여러 가지 광학부품들에 이용되고 있는 재료(MgF$_2$, CaF$_2$, BaF$_2$, SiO$_2$, Sapphire)들의 분광투과율과 반사율을 측정하였다.

• 한국환경과학회지
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• 제10권6호
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• pp.431-436
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• 2001

Variations in phytoplankton concentrations result from changes of the ocean color caused by phytoplankton pigments. Thus, ocean spectral reflectance for low chlorophyll waters are blue and high chlorophyll waters tend to have green reflectance. In the Korea region, clear waters and the open sea in the Kuroshio regions of the East China Sea have low chlorophyll. As one moves even closer In the northwestern part of the East China Sea, the situation becomes much more optically complicated, with contributions not only from higher concentration of phytoplankton, but also from sediments and dissolved materials from terrestrial and sea bottom sources. The color often approaches yellow-brown in the turbidity waters (Case Ⅱ waters). To verify satellite ocean color retrievals, or to develop new algorithms for complex case Ⅱ regions requires ship-based studies. In this study, we compared the chlorophyll retrievals from NASA's SeaWiFS sensor with chlorophyll values determined with standard fluorometric methods during two cruises on Korean NFRDI ships. For the SeaWiFS data, we used the standard NASA SeaWiFS algorithm to estimate the chlorophyll_a distribution around the Korean waters using Orbview/ SeaWiFS satellite data acquired by our HPRT station at NFRDl. We studied In find out the relationship between the measured chlorophyll_a from the ship and the estimated chlorophyll_a from the SeaWiFs satellite data around the northern part of the East China Sea, in February, and May, 2000. The relationship between the measured chlorophyll_a and the SeaWiFS chlorophyll_a shows following the equations (1) In the northern part of the East China Sea. Chlorophyll_a =0.121Ln(X) + 0.504, R²= 0.73 (1) We also determined total suspended sediment mass (55) and compared it with SeaWiFS spectral band ratio. A suspended solid algorithm was composed of in-.situ data and the ratio (L/sub WN/(490 ㎚)L/sub WN/(555 ㎚) of the SeaWiFS wavelength bands. The relationship between the measured suspended solid and the SeaWiFS band ratio shows following the equation (2) in the northern part of the East China Sea. SS = -0.703 Ln(X) + 2.237, R²= 0.62 (2) In the near future, NFRDI will develop algorithms for quantifying the ocean color properties around the Korean waters, with the data from regular ocean observations using its own research vessels and from three satellites, KOMPSAT/OSMl, Terra/MODIS and Orbview/SeaWiFS.