Airborne spectral measurements of ocean directional reflectance

The Cloud Absorption Radiometer (CAR) was flown aboard the University of Washington Convair 580 (CV-580) research aircraft during the Chesapeake Lighthouse and Aircraft Measurements for Satellites (CLAMS) field campaign and obtained measurements of bidirectional reflectance distribution function (BR...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of the atmospheric sciences 2005-04, Vol.62 (4), p.1072-1092
Hauptverfasser: GATEBE, Charles K, KING, Michael D, LYAPUSTIN, Alexei I, ARNOLD, G. Thomas, REDEMANN, Jens
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 1092
container_issue 4
container_start_page 1072
container_title Journal of the atmospheric sciences
container_volume 62
creator GATEBE, Charles K
KING, Michael D
LYAPUSTIN, Alexei I
ARNOLD, G. Thomas
REDEMANN, Jens
description The Cloud Absorption Radiometer (CAR) was flown aboard the University of Washington Convair 580 (CV-580) research aircraft during the Chesapeake Lighthouse and Aircraft Measurements for Satellites (CLAMS) field campaign and obtained measurements of bidirectional reflectance distribution function (BRDF) of the ocean in July and August 2001 under different illumination conditions with solar zenith angles ranging from 15' to 46'. The BRDF measurements were accompanied by concurrent measurements of atmospheric aerosol optical thickness and column water vapor above the airplane. The method of spherical harmonics with Cox-Munk wave-slope distribution is used in a new algorithm developed for this study to solve the atmosphere-ocean radiative transfer problem and to remove the effects of the atmosphere from airborne measurements. The algorithm retrieves simultaneously the wind speed and full ocean BRDF (sun's glitter and water-leaving radiance) from CAR measurements and evaluates total albedo and equivalent albedo for the water-leaving radiance outside the glitter. Results show good overall agreement with other measurements and theoretical simulations, with the anisotropy of the water-leaving radiance clearly seen. However, the water-leaving radiance does not show a strong dependence on solar zenith angle as suggested by some theoretical studies. The spectral albedo was found to vary from 4.1%-5.1% at l = 0.472 k m to 2.4%-3.5% for l . 0.682 k m. The equivalent water-leaving albedo ranges from 1.0%-2.4% at l = 0.472 k m to 0.1%-0.6% for l = 0.682 k m and 0.1%-0.3% for l = 0.870 k m. Results of the validation of the Cox-Munk model under the conditions measured show that although the model reproduces the shape of sun's glitter on average with an accuracy of better than 30%, it underestimates the center of the sun's glitter reflectance by about 30% for low wind speeds ( < 2-3 m s-1). In cases of high wind speed, the model with Gram-Charlier expansion seems to provide the best fit.
doi_str_mv 10.1175/JAS3386.1
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_29021335</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>17334233</sourcerecordid><originalsourceid>FETCH-LOGICAL-c454t-f79720b442df77832cb68afc39f25d3f23cca9fc6a7e80c0fa7d02d7b5f2e37f3</originalsourceid><addsrcrecordid>eNqFkU1LxDAQhoMouK4e_AdFUPDQNZnJR3uSZfGTBQ_quaRpAl3aZk3ag__eLLsgeHEuwzDPvAPvS8glowvGlLh7Xb4jFnLBjsiMCaA55bI8JjNKAXJeQnFKzmLc0FSg2IzcL9tQ-zDYLG6tGYPust7qOAXb22GMmXeZN1YPWdOGtG_9kIhgXZcGPRh7Tk6c7qK9OPQ5-Xx8-Fg95-u3p5fVcp0bLviYO1UqoDXn0DilCgRTy0I7g6UD0aADNEaXzkitbEENdVo1FBpVCwcWlcM5udnrboP_mmwcq76NxnadHqyfYgUlBYYo_gcLoQTl9F-QKUQOiAm8-gNu_BSSD0kMJUdQsHt7u4dM8DEmg6ptaHsdvitGq10y1SGZiiX2-iCoo9GdC8nINv4eSEWlRIU_GOGMkQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>236432725</pqid></control><display><type>article</type><title>Airborne spectral measurements of ocean directional reflectance</title><source>American Meteorological Society</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><source>Alma/SFX Local Collection</source><creator>GATEBE, Charles K ; KING, Michael D ; LYAPUSTIN, Alexei I ; ARNOLD, G. Thomas ; REDEMANN, Jens</creator><creatorcontrib>GATEBE, Charles K ; KING, Michael D ; LYAPUSTIN, Alexei I ; ARNOLD, G. Thomas ; REDEMANN, Jens</creatorcontrib><description>The Cloud Absorption Radiometer (CAR) was flown aboard the University of Washington Convair 580 (CV-580) research aircraft during the Chesapeake Lighthouse and Aircraft Measurements for Satellites (CLAMS) field campaign and obtained measurements of bidirectional reflectance distribution function (BRDF) of the ocean in July and August 2001 under different illumination conditions with solar zenith angles ranging from 15' to 46'. The BRDF measurements were accompanied by concurrent measurements of atmospheric aerosol optical thickness and column water vapor above the airplane. The method of spherical harmonics with Cox-Munk wave-slope distribution is used in a new algorithm developed for this study to solve the atmosphere-ocean radiative transfer problem and to remove the effects of the atmosphere from airborne measurements. The algorithm retrieves simultaneously the wind speed and full ocean BRDF (sun's glitter and water-leaving radiance) from CAR measurements and evaluates total albedo and equivalent albedo for the water-leaving radiance outside the glitter. Results show good overall agreement with other measurements and theoretical simulations, with the anisotropy of the water-leaving radiance clearly seen. However, the water-leaving radiance does not show a strong dependence on solar zenith angle as suggested by some theoretical studies. The spectral albedo was found to vary from 4.1%-5.1% at l = 0.472 k m to 2.4%-3.5% for l . 0.682 k m. The equivalent water-leaving albedo ranges from 1.0%-2.4% at l = 0.472 k m to 0.1%-0.6% for l = 0.682 k m and 0.1%-0.3% for l = 0.870 k m. Results of the validation of the Cox-Munk model under the conditions measured show that although the model reproduces the shape of sun's glitter on average with an accuracy of better than 30%, it underestimates the center of the sun's glitter reflectance by about 30% for low wind speeds ( &lt; 2-3 m s-1). In cases of high wind speed, the model with Gram-Charlier expansion seems to provide the best fit.</description><identifier>ISSN: 0022-4928</identifier><identifier>EISSN: 1520-0469</identifier><identifier>DOI: 10.1175/JAS3386.1</identifier><identifier>CODEN: JAHSAK</identifier><language>eng</language><publisher>Boston, MA: American Meteorological Society</publisher><subject>Aircraft ; Albedo ; Algorithms ; Anisotropy ; Atmosphere ; Atmospheric aerosols ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Meteorology ; Ocean-atmosphere interaction ; Radiative transfer ; Reflectance ; Sun ; Water vapor ; Wind speed</subject><ispartof>Journal of the atmospheric sciences, 2005-04, Vol.62 (4), p.1072-1092</ispartof><rights>2005 INIST-CNRS</rights><rights>Copyright American Meteorological Society Apr 2005</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c454t-f79720b442df77832cb68afc39f25d3f23cca9fc6a7e80c0fa7d02d7b5f2e37f3</citedby><cites>FETCH-LOGICAL-c454t-f79720b442df77832cb68afc39f25d3f23cca9fc6a7e80c0fa7d02d7b5f2e37f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,778,782,3670,27911,27912</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=16706637$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>GATEBE, Charles K</creatorcontrib><creatorcontrib>KING, Michael D</creatorcontrib><creatorcontrib>LYAPUSTIN, Alexei I</creatorcontrib><creatorcontrib>ARNOLD, G. Thomas</creatorcontrib><creatorcontrib>REDEMANN, Jens</creatorcontrib><title>Airborne spectral measurements of ocean directional reflectance</title><title>Journal of the atmospheric sciences</title><description>The Cloud Absorption Radiometer (CAR) was flown aboard the University of Washington Convair 580 (CV-580) research aircraft during the Chesapeake Lighthouse and Aircraft Measurements for Satellites (CLAMS) field campaign and obtained measurements of bidirectional reflectance distribution function (BRDF) of the ocean in July and August 2001 under different illumination conditions with solar zenith angles ranging from 15' to 46'. The BRDF measurements were accompanied by concurrent measurements of atmospheric aerosol optical thickness and column water vapor above the airplane. The method of spherical harmonics with Cox-Munk wave-slope distribution is used in a new algorithm developed for this study to solve the atmosphere-ocean radiative transfer problem and to remove the effects of the atmosphere from airborne measurements. The algorithm retrieves simultaneously the wind speed and full ocean BRDF (sun's glitter and water-leaving radiance) from CAR measurements and evaluates total albedo and equivalent albedo for the water-leaving radiance outside the glitter. Results show good overall agreement with other measurements and theoretical simulations, with the anisotropy of the water-leaving radiance clearly seen. However, the water-leaving radiance does not show a strong dependence on solar zenith angle as suggested by some theoretical studies. The spectral albedo was found to vary from 4.1%-5.1% at l = 0.472 k m to 2.4%-3.5% for l . 0.682 k m. The equivalent water-leaving albedo ranges from 1.0%-2.4% at l = 0.472 k m to 0.1%-0.6% for l = 0.682 k m and 0.1%-0.3% for l = 0.870 k m. Results of the validation of the Cox-Munk model under the conditions measured show that although the model reproduces the shape of sun's glitter on average with an accuracy of better than 30%, it underestimates the center of the sun's glitter reflectance by about 30% for low wind speeds ( &lt; 2-3 m s-1). In cases of high wind speed, the model with Gram-Charlier expansion seems to provide the best fit.</description><subject>Aircraft</subject><subject>Albedo</subject><subject>Algorithms</subject><subject>Anisotropy</subject><subject>Atmosphere</subject><subject>Atmospheric aerosols</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Meteorology</subject><subject>Ocean-atmosphere interaction</subject><subject>Radiative transfer</subject><subject>Reflectance</subject><subject>Sun</subject><subject>Water vapor</subject><subject>Wind speed</subject><issn>0022-4928</issn><issn>1520-0469</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkU1LxDAQhoMouK4e_AdFUPDQNZnJR3uSZfGTBQ_quaRpAl3aZk3ag__eLLsgeHEuwzDPvAPvS8glowvGlLh7Xb4jFnLBjsiMCaA55bI8JjNKAXJeQnFKzmLc0FSg2IzcL9tQ-zDYLG6tGYPust7qOAXb22GMmXeZN1YPWdOGtG_9kIhgXZcGPRh7Tk6c7qK9OPQ5-Xx8-Fg95-u3p5fVcp0bLviYO1UqoDXn0DilCgRTy0I7g6UD0aADNEaXzkitbEENdVo1FBpVCwcWlcM5udnrboP_mmwcq76NxnadHqyfYgUlBYYo_gcLoQTl9F-QKUQOiAm8-gNu_BSSD0kMJUdQsHt7u4dM8DEmg6ptaHsdvitGq10y1SGZiiX2-iCoo9GdC8nINv4eSEWlRIU_GOGMkQ</recordid><startdate>20050401</startdate><enddate>20050401</enddate><creator>GATEBE, Charles K</creator><creator>KING, Michael D</creator><creator>LYAPUSTIN, Alexei I</creator><creator>ARNOLD, G. Thomas</creator><creator>REDEMANN, Jens</creator><general>American Meteorological Society</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8AF</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>M1Q</scope><scope>M2O</scope><scope>M2P</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>R05</scope><scope>S0X</scope><scope>7U5</scope></search><sort><creationdate>20050401</creationdate><title>Airborne spectral measurements of ocean directional reflectance</title><author>GATEBE, Charles K ; KING, Michael D ; LYAPUSTIN, Alexei I ; ARNOLD, G. Thomas ; REDEMANN, Jens</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c454t-f79720b442df77832cb68afc39f25d3f23cca9fc6a7e80c0fa7d02d7b5f2e37f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Aircraft</topic><topic>Albedo</topic><topic>Algorithms</topic><topic>Anisotropy</topic><topic>Atmosphere</topic><topic>Atmospheric aerosols</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Meteorology</topic><topic>Ocean-atmosphere interaction</topic><topic>Radiative transfer</topic><topic>Reflectance</topic><topic>Sun</topic><topic>Water vapor</topic><topic>Wind speed</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>GATEBE, Charles K</creatorcontrib><creatorcontrib>KING, Michael D</creatorcontrib><creatorcontrib>LYAPUSTIN, Alexei I</creatorcontrib><creatorcontrib>ARNOLD, G. Thomas</creatorcontrib><creatorcontrib>REDEMANN, Jens</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies &amp; Aerospace Collection</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>eLibrary</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Military Database</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies &amp; Aerospace Database</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>University of Michigan</collection><collection>SIRS Editorial</collection><collection>Solid State and Superconductivity Abstracts</collection><jtitle>Journal of the atmospheric sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>GATEBE, Charles K</au><au>KING, Michael D</au><au>LYAPUSTIN, Alexei I</au><au>ARNOLD, G. Thomas</au><au>REDEMANN, Jens</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Airborne spectral measurements of ocean directional reflectance</atitle><jtitle>Journal of the atmospheric sciences</jtitle><date>2005-04-01</date><risdate>2005</risdate><volume>62</volume><issue>4</issue><spage>1072</spage><epage>1092</epage><pages>1072-1092</pages><issn>0022-4928</issn><eissn>1520-0469</eissn><coden>JAHSAK</coden><abstract>The Cloud Absorption Radiometer (CAR) was flown aboard the University of Washington Convair 580 (CV-580) research aircraft during the Chesapeake Lighthouse and Aircraft Measurements for Satellites (CLAMS) field campaign and obtained measurements of bidirectional reflectance distribution function (BRDF) of the ocean in July and August 2001 under different illumination conditions with solar zenith angles ranging from 15' to 46'. The BRDF measurements were accompanied by concurrent measurements of atmospheric aerosol optical thickness and column water vapor above the airplane. The method of spherical harmonics with Cox-Munk wave-slope distribution is used in a new algorithm developed for this study to solve the atmosphere-ocean radiative transfer problem and to remove the effects of the atmosphere from airborne measurements. The algorithm retrieves simultaneously the wind speed and full ocean BRDF (sun's glitter and water-leaving radiance) from CAR measurements and evaluates total albedo and equivalent albedo for the water-leaving radiance outside the glitter. Results show good overall agreement with other measurements and theoretical simulations, with the anisotropy of the water-leaving radiance clearly seen. However, the water-leaving radiance does not show a strong dependence on solar zenith angle as suggested by some theoretical studies. The spectral albedo was found to vary from 4.1%-5.1% at l = 0.472 k m to 2.4%-3.5% for l . 0.682 k m. The equivalent water-leaving albedo ranges from 1.0%-2.4% at l = 0.472 k m to 0.1%-0.6% for l = 0.682 k m and 0.1%-0.3% for l = 0.870 k m. Results of the validation of the Cox-Munk model under the conditions measured show that although the model reproduces the shape of sun's glitter on average with an accuracy of better than 30%, it underestimates the center of the sun's glitter reflectance by about 30% for low wind speeds ( &lt; 2-3 m s-1). In cases of high wind speed, the model with Gram-Charlier expansion seems to provide the best fit.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/JAS3386.1</doi><tpages>21</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0022-4928
ispartof Journal of the atmospheric sciences, 2005-04, Vol.62 (4), p.1072-1092
issn 0022-4928
1520-0469
language eng
recordid cdi_proquest_miscellaneous_29021335
source American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection
subjects Aircraft
Albedo
Algorithms
Anisotropy
Atmosphere
Atmospheric aerosols
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
Ocean-atmosphere interaction
Radiative transfer
Reflectance
Sun
Water vapor
Wind speed
title Airborne spectral measurements of ocean directional reflectance
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-15T18%3A47%3A30IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Airborne%20spectral%20measurements%20of%20ocean%20directional%20reflectance&rft.jtitle=Journal%20of%20the%20atmospheric%20sciences&rft.au=GATEBE,%20Charles%20K&rft.date=2005-04-01&rft.volume=62&rft.issue=4&rft.spage=1072&rft.epage=1092&rft.pages=1072-1092&rft.issn=0022-4928&rft.eissn=1520-0469&rft.coden=JAHSAK&rft_id=info:doi/10.1175/JAS3386.1&rft_dat=%3Cproquest_cross%3E17334233%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=236432725&rft_id=info:pmid/&rfr_iscdi=true