/begin_header /identifier_product_doi=10.5067/SeaBASS/OCEAN_COLOR_CAL_VAL/DATA001 /received=20070831 /investigators=Zhongping_Lee /affiliations=Naval_Research_Laboratory /contact=zplee@nrlssc.navy.mil ! experiment=Hudson_Plume_NY_Bight /experiment=Ocean_Color_Cal_Val ! cruise=hudson_plume_may_2007 /cruise=ocval1 /data_file_name=Rrs2007125_st2_05c.sim.sb /documents=SPECTRIX_README.TXT /calibration_files=zplee@nrlssc.navy.mil /data_type=above_water /start_date=20070505 /end_date=20070505 /start_time=17:55:00[GMT] /end_time=17:56:00[GMT] /north_latitude=40.460900[DEG] /south_latitude=40.460900[DEG] /east_longitude=-73.715433[DEG] /west_longitude=-73.715433[DEG] /water_depth=NA /data_status=final /station=St2_05c /cloud_percent=NA /measurement_depth=0 /secchi_depth=NA /wave_height=NA /wind_speed=NA ! COMMENTS ! Remote sensing reflectance (ratio of water-leaving radiance to downwelling irradiance just above the surface) is ! calculated based on the method described in Lee et al (1996), where Raman contribution in the reflected skylight ! is removed by applying a Fresnel factor (~0.022), while aerosol and others in the reflected skylight are removed ! iteratively by incorporating a reflectance model. ! ! Environmental conditions = broken clouds around the sun /missing=-99.0 /delimiter=tab /fields=wavelength,rrs /units=nm,sr^-1 /end_header 400 0.001610047 405 0.001639474 410 0.001657444 415 0.001684529 420 0.001722076 425 0.001770874 430 0.001825696 435 0.001844163 440 0.00190217 445 0.001987214 450 0.002088438 455 0.002178217 460 0.00223747 465 0.002298755 470 0.002396023 475 0.002521096 480 0.002642426 485 0.002761692 490 0.0028264 495 0.002874883 500 0.002950844 505 0.0030692 510 0.003228187 515 0.003387993 520 0.00358891 525 0.003786628 530 0.003956139 535 0.004114397 540 0.004263548 545 0.004425919 550 0.004596824 555 0.004794986 560 0.005046905 565 0.005266087 570 0.005407898 575 0.005443365 580 0.005359722 585 0.005099993 590 0.004757094 595 0.004351036 600 0.003788602 605 0.003273088 610 0.003046028 615 0.002873253 620 0.002742894 625 0.002633673 630 0.002536257 635 0.002448886 640 0.002394824 645 0.002345324 650 0.002271325 655 0.002109328 660 0.001837871 665 0.001660568 670 0.001616942 675 0.001694138 680 0.001812504 685 0.001922311 690 0.001966231 695 0.00184469 700 0.001662029 705 0.001444972 710 0.001225619 715 0.001017115 720 0.000822286 725 0.000673374 730 0.00053194 735 0.000432274 740 0.000395687 745 0.000375032 750 0.000360649 755 0.000358925 760 0.000308995 765 0.000348378 770 0.000332214 775 0.000329359 780 0.000334817 785 0.000338561 790 0.000344878 795 0.000358839 800 0.000370009