Optical Closure of Apparent Optical Properties in Coastal Waters off Goa

Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulati...
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Autor*in:	Talaulikar, Madhubala [verfasserIn] Suresh, T. [verfasserIn] Desa, Elgar [verfasserIn] Inamdar, Arun [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	Inherent optical properties Apparent optical properties Optical closure Hydrolight Coastal waters

Übergeordnetes Werk:	Enthalten in: Journal of the Indian Society of Remote Sensing - Neu Delhi : Springer India, 2008, 43(2014), 1 vom: 25. Juli, Seite 163-171
Übergeordnetes Werk:	volume:43 ; year:2014 ; number:1 ; day:25 ; month:07 ; pages:163-171

Links:	Volltext

DOI / URN:	10.1007/s12524-014-0393-5

Katalog-ID:	SPR02602022X

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520			\|a Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area.
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publishDate	2014
allfields	10.1007/s12524-014-0393-5 doi (DE-627)SPR02602022X (SPR)s12524-014-0393-5-e DE-627 ger DE-627 rakwb eng 550 ASE Talaulikar, Madhubala verfasserin aut Optical Closure of Apparent Optical Properties in Coastal Waters off Goa 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area. Inherent optical properties (dpeaa)DE-He213 Apparent optical properties (dpeaa)DE-He213 Optical closure (dpeaa)DE-He213 Hydrolight (dpeaa)DE-He213 Coastal waters (dpeaa)DE-He213 Suresh, T. verfasserin aut Desa, Elgar verfasserin aut Inamdar, Arun verfasserin aut Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 43(2014), 1 vom: 25. Juli, Seite 163-171 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:43 year:2014 number:1 day:25 month:07 pages:163-171 https://dx.doi.org/10.1007/s12524-014-0393-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 43 2014 1 25 07 163-171
spelling	10.1007/s12524-014-0393-5 doi (DE-627)SPR02602022X (SPR)s12524-014-0393-5-e DE-627 ger DE-627 rakwb eng 550 ASE Talaulikar, Madhubala verfasserin aut Optical Closure of Apparent Optical Properties in Coastal Waters off Goa 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area. Inherent optical properties (dpeaa)DE-He213 Apparent optical properties (dpeaa)DE-He213 Optical closure (dpeaa)DE-He213 Hydrolight (dpeaa)DE-He213 Coastal waters (dpeaa)DE-He213 Suresh, T. verfasserin aut Desa, Elgar verfasserin aut Inamdar, Arun verfasserin aut Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 43(2014), 1 vom: 25. Juli, Seite 163-171 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:43 year:2014 number:1 day:25 month:07 pages:163-171 https://dx.doi.org/10.1007/s12524-014-0393-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 43 2014 1 25 07 163-171
allfields_unstemmed	10.1007/s12524-014-0393-5 doi (DE-627)SPR02602022X (SPR)s12524-014-0393-5-e DE-627 ger DE-627 rakwb eng 550 ASE Talaulikar, Madhubala verfasserin aut Optical Closure of Apparent Optical Properties in Coastal Waters off Goa 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area. Inherent optical properties (dpeaa)DE-He213 Apparent optical properties (dpeaa)DE-He213 Optical closure (dpeaa)DE-He213 Hydrolight (dpeaa)DE-He213 Coastal waters (dpeaa)DE-He213 Suresh, T. verfasserin aut Desa, Elgar verfasserin aut Inamdar, Arun verfasserin aut Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 43(2014), 1 vom: 25. Juli, Seite 163-171 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:43 year:2014 number:1 day:25 month:07 pages:163-171 https://dx.doi.org/10.1007/s12524-014-0393-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 43 2014 1 25 07 163-171
allfieldsGer	10.1007/s12524-014-0393-5 doi (DE-627)SPR02602022X (SPR)s12524-014-0393-5-e DE-627 ger DE-627 rakwb eng 550 ASE Talaulikar, Madhubala verfasserin aut Optical Closure of Apparent Optical Properties in Coastal Waters off Goa 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area. Inherent optical properties (dpeaa)DE-He213 Apparent optical properties (dpeaa)DE-He213 Optical closure (dpeaa)DE-He213 Hydrolight (dpeaa)DE-He213 Coastal waters (dpeaa)DE-He213 Suresh, T. verfasserin aut Desa, Elgar verfasserin aut Inamdar, Arun verfasserin aut Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 43(2014), 1 vom: 25. Juli, Seite 163-171 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:43 year:2014 number:1 day:25 month:07 pages:163-171 https://dx.doi.org/10.1007/s12524-014-0393-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 43 2014 1 25 07 163-171
allfieldsSound	10.1007/s12524-014-0393-5 doi (DE-627)SPR02602022X (SPR)s12524-014-0393-5-e DE-627 ger DE-627 rakwb eng 550 ASE Talaulikar, Madhubala verfasserin aut Optical Closure of Apparent Optical Properties in Coastal Waters off Goa 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area. Inherent optical properties (dpeaa)DE-He213 Apparent optical properties (dpeaa)DE-He213 Optical closure (dpeaa)DE-He213 Hydrolight (dpeaa)DE-He213 Coastal waters (dpeaa)DE-He213 Suresh, T. verfasserin aut Desa, Elgar verfasserin aut Inamdar, Arun verfasserin aut Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 43(2014), 1 vom: 25. Juli, Seite 163-171 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:43 year:2014 number:1 day:25 month:07 pages:163-171 https://dx.doi.org/10.1007/s12524-014-0393-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 43 2014 1 25 07 163-171
language	English
source	Enthalten in Journal of the Indian Society of Remote Sensing 43(2014), 1 vom: 25. Juli, Seite 163-171 volume:43 year:2014 number:1 day:25 month:07 pages:163-171
sourceStr	Enthalten in Journal of the Indian Society of Remote Sensing 43(2014), 1 vom: 25. Juli, Seite 163-171 volume:43 year:2014 number:1 day:25 month:07 pages:163-171
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topic_facet	Inherent optical properties Apparent optical properties Optical closure Hydrolight Coastal waters
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container_title	Journal of the Indian Society of Remote Sensing
authorswithroles_txt_mv	Talaulikar, Madhubala @@aut@@ Suresh, T. @@aut@@ Desa, Elgar @@aut@@ Inamdar, Arun @@aut@@
publishDateDaySort_date	2014-07-25T00:00:00Z
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author	Talaulikar, Madhubala
spellingShingle	Talaulikar, Madhubala ddc 550 misc Inherent optical properties misc Apparent optical properties misc Optical closure misc Hydrolight misc Coastal waters Optical Closure of Apparent Optical Properties in Coastal Waters off Goa
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topic_title	550 ASE Optical Closure of Apparent Optical Properties in Coastal Waters off Goa Inherent optical properties (dpeaa)DE-He213 Apparent optical properties (dpeaa)DE-He213 Optical closure (dpeaa)DE-He213 Hydrolight (dpeaa)DE-He213 Coastal waters (dpeaa)DE-He213
topic	ddc 550 misc Inherent optical properties misc Apparent optical properties misc Optical closure misc Hydrolight misc Coastal waters
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title	Optical Closure of Apparent Optical Properties in Coastal Waters off Goa
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title_full	Optical Closure of Apparent Optical Properties in Coastal Waters off Goa
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title_sort	optical closure of apparent optical properties in coastal waters off goa
title_auth	Optical Closure of Apparent Optical Properties in Coastal Waters off Goa
abstract	Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area.
abstractGer	Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area.
abstract_unstemmed	Abstract Inherent and apparent optical properties were measured for coastal waters off Goa, a site on the west coast of India using the in-situ measuring profiling optical instruments. The optical closure was obtained using the radiative transfer model, Hydrolight (Sequoia Inc.). Hydrolight simulations were carried out at all stations using “average particle” Petzold phase function and Fournier Forand phase function with optimum bbp/bp value. The optical properties derived from Hydrolight simulations were then compared with the measured optical properties. The widely used “average particle” phase function measured by Petzold 1972 for coastal waters was found to provide poor results for most of the stations while for few others it was found to produce results comparable to Fournier Forand phase function. The mean percentage deviation for water leaving radiance (remote sensing reflectance) simulated using Petzold and Fournier Forand phase function for wavelength 488 nm varied from 3.8 to 240.7 % (3.8 to 240.8 %) and 1.0 to 48.9 % (1.0 % to 49.0 %) respectively. These closure studies are essential in strengthening the confidence in models or algorithms developed for ocean color remote sensing and also in better understanding of the marine optical properties of waters of the study area.
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title_short	Optical Closure of Apparent Optical Properties in Coastal Waters off Goa
url	https://dx.doi.org/10.1007/s12524-014-0393-5
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author2	Suresh, T. Desa, Elgar Inamdar, Arun
author2Str	Suresh, T. Desa, Elgar Inamdar, Arun
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doi_str	10.1007/s12524-014-0393-5
up_date	2024-07-03T18:23:37.467Z
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Optical Closure of Apparent Optical Properties in Coastal Waters off Goa

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