G. Wei, Z. Lee, Xiuling Wu, Xiaolong Yu, S. Shang, Ricardo M Letelier
{"title":"温度对卫星和现场测量推断的纯海水蓝色波长吸收系数的影响","authors":"G. Wei, Z. Lee, Xiuling Wu, Xiaolong Yu, S. Shang, Ricardo M Letelier","doi":"10.34133/2021/9842702","DOIUrl":null,"url":null,"abstract":"<jats:p>There has been a long history of interest on how (if) the absorption coefficient of “pure” fresh water (<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M1\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>fw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math>) and “pure” seawater (<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M2\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>sw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math>) changes with temperature (<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M3\"><mml:mi>T</mml:mi></mml:math>), yet the impact of <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M4\"><mml:mi>T</mml:mi></mml:math> reported in the literature differs significantly in the blue domain. Unlike the previous studies based on laboratory measurements, we took an approach based on ~18 years (2002–2020) of MODIS ocean color and temperature measurements in the oligotrophic oceans, along with field measured chlorophyll concentration and phytoplankton absorption coefficient, to examine the relationship between <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M5\"><mml:mi>T</mml:mi></mml:math> and the total absorption coefficient (<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M6\"><mml:mi>a</mml:mi><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math>) at 412 and 443 nm. We found that the values of <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M7\"><mml:mi>a</mml:mi><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mn>412</mml:mn></mml:mrow></mml:mfenced></mml:math> and <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M8\"><mml:mi>a</mml:mi><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mn>443</mml:mn></mml:mrow></mml:mfenced></mml:math> in the summer are nearly flat (slightly decreasing) for the observed <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M9\"><mml:mi>T</mml:mi></mml:math> range of ~19–27 °C. Since there are no detectable changes of chlorophyll during this period, the results suggest that <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M10\"><mml:mi>T</mml:mi></mml:math> has a negligible impact on <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M11\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>sw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mn>412</mml:mn></mml:mrow></mml:mfenced></mml:math> and <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M12\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>sw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mn>443</mml:mn></mml:mrow></mml:mfenced></mml:math> in this <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M13\"><mml:mi>T</mml:mi></mml:math> range. As a complement, the impact of salinity on <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M14\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>fw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math> was also evaluated using three independent determinations of <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M15\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>sw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math> and <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" id=\"M16\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>fw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\"(\" close=\")\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math>, where good agreements were found from these observations.</jats:p>","PeriodicalId":38304,"journal":{"name":"遥感学报","volume":" ","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-07-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Impact of Temperature on Absorption Coefficient of Pure Seawater in the Blue Wavelengths Inferred from Satellite and In Situ Measurements\",\"authors\":\"G. Wei, Z. Lee, Xiuling Wu, Xiaolong Yu, S. Shang, Ricardo M Letelier\",\"doi\":\"10.34133/2021/9842702\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<jats:p>There has been a long history of interest on how (if) the absorption coefficient of “pure” fresh water (<mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M1\\\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>fw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math>) and “pure” seawater (<mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M2\\\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>sw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math>) changes with temperature (<mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M3\\\"><mml:mi>T</mml:mi></mml:math>), yet the impact of <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M4\\\"><mml:mi>T</mml:mi></mml:math> reported in the literature differs significantly in the blue domain. Unlike the previous studies based on laboratory measurements, we took an approach based on ~18 years (2002–2020) of MODIS ocean color and temperature measurements in the oligotrophic oceans, along with field measured chlorophyll concentration and phytoplankton absorption coefficient, to examine the relationship between <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M5\\\"><mml:mi>T</mml:mi></mml:math> and the total absorption coefficient (<mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M6\\\"><mml:mi>a</mml:mi><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math>) at 412 and 443 nm. We found that the values of <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M7\\\"><mml:mi>a</mml:mi><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mn>412</mml:mn></mml:mrow></mml:mfenced></mml:math> and <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M8\\\"><mml:mi>a</mml:mi><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mn>443</mml:mn></mml:mrow></mml:mfenced></mml:math> in the summer are nearly flat (slightly decreasing) for the observed <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M9\\\"><mml:mi>T</mml:mi></mml:math> range of ~19–27 °C. Since there are no detectable changes of chlorophyll during this period, the results suggest that <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M10\\\"><mml:mi>T</mml:mi></mml:math> has a negligible impact on <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M11\\\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>sw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mn>412</mml:mn></mml:mrow></mml:mfenced></mml:math> and <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M12\\\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>sw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mn>443</mml:mn></mml:mrow></mml:mfenced></mml:math> in this <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M13\\\"><mml:mi>T</mml:mi></mml:math> range. As a complement, the impact of salinity on <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M14\\\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>fw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math> was also evaluated using three independent determinations of <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M15\\\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>sw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math> and <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\" id=\\\"M16\\\"><mml:msub><mml:mrow><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mtext>fw</mml:mtext></mml:mrow></mml:msub><mml:mfenced open=\\\"(\\\" close=\\\")\\\"><mml:mrow><mml:mi>λ</mml:mi></mml:mrow></mml:mfenced></mml:math>, where good agreements were found from these observations.</jats:p>\",\"PeriodicalId\":38304,\"journal\":{\"name\":\"遥感学报\",\"volume\":\" \",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-07-13\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"遥感学报\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.34133/2021/9842702\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"遥感学报","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.34133/2021/9842702","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Impact of Temperature on Absorption Coefficient of Pure Seawater in the Blue Wavelengths Inferred from Satellite and In Situ Measurements
There has been a long history of interest on how (if) the absorption coefficient of “pure” fresh water (afwλ) and “pure” seawater (aswλ) changes with temperature (T), yet the impact of T reported in the literature differs significantly in the blue domain. Unlike the previous studies based on laboratory measurements, we took an approach based on ~18 years (2002–2020) of MODIS ocean color and temperature measurements in the oligotrophic oceans, along with field measured chlorophyll concentration and phytoplankton absorption coefficient, to examine the relationship between T and the total absorption coefficient (aλ) at 412 and 443 nm. We found that the values of a412 and a443 in the summer are nearly flat (slightly decreasing) for the observed T range of ~19–27 °C. Since there are no detectable changes of chlorophyll during this period, the results suggest that T has a negligible impact on asw412 and asw443 in this T range. As a complement, the impact of salinity on afwλ was also evaluated using three independent determinations of aswλ and afwλ, where good agreements were found from these observations.