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Investigation of Atmospheric Effects on Retrieval of Sun-Induced Fluorescence Using Hyperspectral Imagery
Significant research progress has recently been made in estimating fluorescence in the oxygen absorption bands, however, quantitative retrieval of fluorescence data is still affected by factors such as atmospheric effects. In this paper, top-of-atmosphere (TOA) radiance is generated by the MODTRAN 4...
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Published in: | Sensors (Basel, Switzerland) Switzerland), 2016-04, Vol.16 (4), p.480-480 |
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description | Significant research progress has recently been made in estimating fluorescence in the oxygen absorption bands, however, quantitative retrieval of fluorescence data is still affected by factors such as atmospheric effects. In this paper, top-of-atmosphere (TOA) radiance is generated by the MODTRAN 4 and SCOPE models. Based on simulated data, sensitivity analysis is conducted to assess the sensitivities of four indicators-depth_absorption_band, depth_nofs-depth_withfs, radiance and Fs/radiance-to atmospheric parameters (sun zenith angle (SZA), sensor height, elevation, visibility (VIS) and water content) in the oxygen absorption bands. The results indicate that the SZA and sensor height are the most sensitive parameters and that variations in these two parameters result in large variations calculated as the variation value/the base value in the oxygen absorption depth in the O₂-A and O₂-B bands (111.4% and 77.1% in the O₂-A band; and 27.5% and 32.6% in the O₂-B band, respectively). A comparison of fluorescence retrieval using three methods (Damm method, Braun method and DOAS) and SCOPE Fs indicates that the Damm method yields good results and that atmospheric correction can improve the accuracy of fluorescence retrieval. Damm method is the improved 3FLD method but considering atmospheric effects. Finally, hyperspectral airborne images combined with other parameters (SZA, VIS and water content) are exploited to estimate fluorescence using the Damm method and 3FLD method. The retrieval fluorescence is compared with the field measured fluorescence, yielding good results (R² = 0.91 for Damm vs. SCOPE SIF; R² = 0.65 for 3FLD vs. SCOPE SIF). Five types of vegetation, including ailanthus, elm, mountain peach, willow and Chinese ash, exhibit consistent associations between the retrieved fluorescence and field measured fluorescence. |
doi_str_mv | 10.3390/s16040480 |
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In this paper, top-of-atmosphere (TOA) radiance is generated by the MODTRAN 4 and SCOPE models. Based on simulated data, sensitivity analysis is conducted to assess the sensitivities of four indicators-depth_absorption_band, depth_nofs-depth_withfs, radiance and Fs/radiance-to atmospheric parameters (sun zenith angle (SZA), sensor height, elevation, visibility (VIS) and water content) in the oxygen absorption bands. The results indicate that the SZA and sensor height are the most sensitive parameters and that variations in these two parameters result in large variations calculated as the variation value/the base value in the oxygen absorption depth in the O₂-A and O₂-B bands (111.4% and 77.1% in the O₂-A band; and 27.5% and 32.6% in the O₂-B band, respectively). A comparison of fluorescence retrieval using three methods (Damm method, Braun method and DOAS) and SCOPE Fs indicates that the Damm method yields good results and that atmospheric correction can improve the accuracy of fluorescence retrieval. Damm method is the improved 3FLD method but considering atmospheric effects. Finally, hyperspectral airborne images combined with other parameters (SZA, VIS and water content) are exploited to estimate fluorescence using the Damm method and 3FLD method. The retrieval fluorescence is compared with the field measured fluorescence, yielding good results (R² = 0.91 for Damm vs. SCOPE SIF; R² = 0.65 for 3FLD vs. SCOPE SIF). Five types of vegetation, including ailanthus, elm, mountain peach, willow and Chinese ash, exhibit consistent associations between the retrieved fluorescence and field measured fluorescence.</description><identifier>ISSN: 1424-8220</identifier><identifier>EISSN: 1424-8220</identifier><identifier>DOI: 10.3390/s16040480</identifier><identifier>PMID: 27058542</identifier><language>eng</language><publisher>Switzerland: MDPI AG</publisher><subject>Accuracy ; airborne data ; Atmospheric effects ; Chlorophyll ; DOAS ; FLD-like method ; Fluorescence ; Laboratories ; Mathematical models ; Methods ; Moisture content ; Oxygen ; oxygen-absorption depth ; Radiance ; Radiation ; Remote sensing ; Retrieval ; Sensitivity analysis ; Sensors ; Sun ; sun-induced fluorescence ; Vegetation</subject><ispartof>Sensors (Basel, Switzerland), 2016-04, Vol.16 (4), p.480-480</ispartof><rights>Copyright MDPI AG 2016</rights><rights>2016 by the authors; licensee MDPI, Basel, Switzerland. 2016</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c535t-250f39b04439a22c51299fd219abc8f33886709d985a4df6f1d92b00abcf70ec3</citedby><cites>FETCH-LOGICAL-c535t-250f39b04439a22c51299fd219abc8f33886709d985a4df6f1d92b00abcf70ec3</cites><orcidid>0000-0003-4377-8560 ; 0000-0001-5160-4574 ; 0000-0001-5843-3106 ; 0000-0002-2070-3278</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/1780817729/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/1780817729?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>230,314,723,776,780,881,25731,27901,27902,36989,36990,44566,53766,53768,74869</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/27058542$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Ni, Zhuoya</creatorcontrib><creatorcontrib>Liu, Zhigang</creatorcontrib><creatorcontrib>Li, Zhao-Liang</creatorcontrib><creatorcontrib>Nerry, Françoise</creatorcontrib><creatorcontrib>Huo, Hongyuan</creatorcontrib><creatorcontrib>Sun, Rui</creatorcontrib><creatorcontrib>Yang, Peiqi</creatorcontrib><creatorcontrib>Zhang, Weiwei</creatorcontrib><title>Investigation of Atmospheric Effects on Retrieval of Sun-Induced Fluorescence Using Hyperspectral Imagery</title><title>Sensors (Basel, Switzerland)</title><addtitle>Sensors (Basel)</addtitle><description>Significant research progress has recently been made in estimating fluorescence in the oxygen absorption bands, however, quantitative retrieval of fluorescence data is still affected by factors such as atmospheric effects. In this paper, top-of-atmosphere (TOA) radiance is generated by the MODTRAN 4 and SCOPE models. Based on simulated data, sensitivity analysis is conducted to assess the sensitivities of four indicators-depth_absorption_band, depth_nofs-depth_withfs, radiance and Fs/radiance-to atmospheric parameters (sun zenith angle (SZA), sensor height, elevation, visibility (VIS) and water content) in the oxygen absorption bands. The results indicate that the SZA and sensor height are the most sensitive parameters and that variations in these two parameters result in large variations calculated as the variation value/the base value in the oxygen absorption depth in the O₂-A and O₂-B bands (111.4% and 77.1% in the O₂-A band; and 27.5% and 32.6% in the O₂-B band, respectively). A comparison of fluorescence retrieval using three methods (Damm method, Braun method and DOAS) and SCOPE Fs indicates that the Damm method yields good results and that atmospheric correction can improve the accuracy of fluorescence retrieval. Damm method is the improved 3FLD method but considering atmospheric effects. Finally, hyperspectral airborne images combined with other parameters (SZA, VIS and water content) are exploited to estimate fluorescence using the Damm method and 3FLD method. The retrieval fluorescence is compared with the field measured fluorescence, yielding good results (R² = 0.91 for Damm vs. SCOPE SIF; R² = 0.65 for 3FLD vs. SCOPE SIF). Five types of vegetation, including ailanthus, elm, mountain peach, willow and Chinese ash, exhibit consistent associations between the retrieved fluorescence and field measured fluorescence.</description><subject>Accuracy</subject><subject>airborne data</subject><subject>Atmospheric effects</subject><subject>Chlorophyll</subject><subject>DOAS</subject><subject>FLD-like method</subject><subject>Fluorescence</subject><subject>Laboratories</subject><subject>Mathematical models</subject><subject>Methods</subject><subject>Moisture content</subject><subject>Oxygen</subject><subject>oxygen-absorption depth</subject><subject>Radiance</subject><subject>Radiation</subject><subject>Remote sensing</subject><subject>Retrieval</subject><subject>Sensitivity analysis</subject><subject>Sensors</subject><subject>Sun</subject><subject>sun-induced fluorescence</subject><subject>Vegetation</subject><issn>1424-8220</issn><issn>1424-8220</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNqNkktv1DAURiMEoqWw4A-gSGxgEbh-JfYGqar6iFQJCejacvxIPUriwU5Gmn-PZ6YdtWxgFSvf8bHv9S2K9wi-ECLga0I1UKAcXhSniGJacYzh5ZP1SfEmpRUAJoTw18UJboBxRvFp4dtpY9PsezX7MJXBlefzGNL63kavy0vnrJ5TmZMfdo7ebtSwY34uU9VOZtHWlFfDEqJN2k7alnfJT315s13bmNZ5a8x8O6rexu3b4pVTQ7LvHr5nxd3V5a-Lm-r2-3V7cX5baUbYXGEGjogOKCVCYawZwkI4g5FQneYu35_XDQgjOFPUuNohI3AHkFPXgNXkrGgPXhPUSq6jH1XcyqC83P8IsZcqzl4PVtYCHBUWHKs5FU5xYzorkGFNAzmz2fXt4Fov3WhNrnFX0TPp82Ty97IPG0k5AyFoFnx6EMTwe8mNlqPPrRoGNdmwJIk4cAQsk_9GGwGiwTX-H5RDPp_srR__QldhiVN-gD3FUdNgkanPB0rHkFK07lgiArkbMXkcscx-eNqTI_k4U-QPLTnLBw</recordid><startdate>20160406</startdate><enddate>20160406</enddate><creator>Ni, Zhuoya</creator><creator>Liu, Zhigang</creator><creator>Li, Zhao-Liang</creator><creator>Nerry, Françoise</creator><creator>Huo, Hongyuan</creator><creator>Sun, Rui</creator><creator>Yang, Peiqi</creator><creator>Zhang, Weiwei</creator><general>MDPI AG</general><general>MDPI</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X7</scope><scope>7XB</scope><scope>88E</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>K9.</scope><scope>M0S</scope><scope>M1P</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>7X8</scope><scope>7TG</scope><scope>KL.</scope><scope>7SP</scope><scope>7TB</scope><scope>7U5</scope><scope>8FD</scope><scope>FR3</scope><scope>L7M</scope><scope>5PM</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0003-4377-8560</orcidid><orcidid>https://orcid.org/0000-0001-5160-4574</orcidid><orcidid>https://orcid.org/0000-0001-5843-3106</orcidid><orcidid>https://orcid.org/0000-0002-2070-3278</orcidid></search><sort><creationdate>20160406</creationdate><title>Investigation of Atmospheric Effects on Retrieval of Sun-Induced Fluorescence Using Hyperspectral Imagery</title><author>Ni, Zhuoya ; 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In this paper, top-of-atmosphere (TOA) radiance is generated by the MODTRAN 4 and SCOPE models. Based on simulated data, sensitivity analysis is conducted to assess the sensitivities of four indicators-depth_absorption_band, depth_nofs-depth_withfs, radiance and Fs/radiance-to atmospheric parameters (sun zenith angle (SZA), sensor height, elevation, visibility (VIS) and water content) in the oxygen absorption bands. The results indicate that the SZA and sensor height are the most sensitive parameters and that variations in these two parameters result in large variations calculated as the variation value/the base value in the oxygen absorption depth in the O₂-A and O₂-B bands (111.4% and 77.1% in the O₂-A band; and 27.5% and 32.6% in the O₂-B band, respectively). A comparison of fluorescence retrieval using three methods (Damm method, Braun method and DOAS) and SCOPE Fs indicates that the Damm method yields good results and that atmospheric correction can improve the accuracy of fluorescence retrieval. Damm method is the improved 3FLD method but considering atmospheric effects. Finally, hyperspectral airborne images combined with other parameters (SZA, VIS and water content) are exploited to estimate fluorescence using the Damm method and 3FLD method. The retrieval fluorescence is compared with the field measured fluorescence, yielding good results (R² = 0.91 for Damm vs. SCOPE SIF; R² = 0.65 for 3FLD vs. SCOPE SIF). 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subjects | Accuracy airborne data Atmospheric effects Chlorophyll DOAS FLD-like method Fluorescence Laboratories Mathematical models Methods Moisture content Oxygen oxygen-absorption depth Radiance Radiation Remote sensing Retrieval Sensitivity analysis Sensors Sun sun-induced fluorescence Vegetation |
title | Investigation of Atmospheric Effects on Retrieval of Sun-Induced Fluorescence Using Hyperspectral Imagery |
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