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

遥感学报 Pub Date : 2021-07-13 DOI:10.34133/2021/9842702
G. Wei, Z. Lee, Xiuling Wu, Xiaolong Yu, S. Shang, Ricardo M Letelier
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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. 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引用次数: 3

摘要

对于“纯”淡水(afwλ)和“纯”海水(aswλ)的吸收系数如何(如果)随温度(T)变化,人们一直很感兴趣,但文献中报道的T的影响在蓝色区域有很大不同。与以往基于实验室测量的研究不同,我们采用了基于约18年(2002-2020)MODIS海洋颜色和温度测量的方法,以及现场测量的叶绿素浓度和浮游植物吸收系数,研究了T与412和443 nm总吸收系数(λ)之间的关系。在~19 ~ 27℃的观测温度范围内,夏季a412和a443的值基本持平(略有下降)。由于叶绿素在此期间没有可检测到的变化,因此结果表明,在此T范围内,T对asw412和asw443的影响可以忽略不计。作为补充,盐度对afwλ的影响也使用三个独立的测定aswλ和afwλ进行了评估,从这些观测结果中发现了良好的一致性。
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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.
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遥感学报
遥感学报 Social Sciences-Geography, Planning and Development
CiteScore
3.60
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3200
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