分层水体对表层辐照度比影响的蒙特卡罗分析

doi:10.11978/j.issn.1009-5470.2012.01.042

热带海洋学报 ›› 2012, Vol. 31 ›› Issue (1): 42-49.doi: 10.11978/j.issn.1009-5470.2012.01.042cstr: 32234.14.j.issn.1009-5470.2012.01.042

分层水体对表层辐照度比影响的蒙特卡罗分析

黄二辉 , 杨燕明

国家海洋局第三海洋研究所海洋声学与遥感开放实验室 , 福建厦门 361005

收稿日期:2010-07-06 修回日期:2010-10-18 出版日期:2012-03-10 发布日期:2012-03-13
通讯作者: 黄二辉
作者简介: 黄二辉 (1978 — ), 男 , 福建省厦门市人 , 硕士 , 助理研究员 , 主要从事海洋遥感方面的研究工作。 E-mail huangerhui@gmail.com
基金资助:
国家海洋局基本科研业务费专项资金资助项目 ( 海三科 2007013); 国家海洋局青年基金重点项目 (2009429); 卫星海洋环境动力学国家重点实验室开放研究 (200507) 资助

Analysis of influence of stratified water bodies on underwater irradiance ratio by Monte Carlo model

HUANG Er-hui, YANG Yan-ming

Open Lab of Ocean Acoustic and Remote Sensing , Third Institute of Oceanography , SOA , Xiamen 361005, China

Received:2010-07-06 Revised:2010-10-18 Online:2012-03-10 Published:2012-03-13

摘要/Abstract

摘要： 众多海洋观测数据表明, 在真光层深度范围内, 海水固有光学特性和光学有效组分的剖面分层分布是广泛存在的, 而很多遥感反演模型的建立基于均一分布假设, 尤其是在经验模型的建立中, 往往只利用某一深度或各深度平均的光学有效组分浓度与水体光谱的统计关系。文章通过模拟平静水面水下光的辐射传输, 分别研究了叶绿素、无机悬浮物浓度垂直分布结构对水下辐照度比的影响, 并对比了两类分层水体权重函数等效浓度计算式及相应水下辐照度比, 结果表明, 对于分层水体, 透射深度和层化强度是影响等效浓度值计算误差的主要因素, 透射越深, 表层层化越强, 水体层化对水下辐照度比的影响就越大, 但其计算误差也越大。Gondon等效浓度计算结果比较接近实际值, 而Zaneveld计算式则高估了分层水体的等效浓度值。

关键词: 分层水体, 蒙特卡罗, 权重函数, 等效浓度

Abstract: Many in-situ data indicate that the vertical stratification of the inherent optical properties and optical active constitutes in euphoric depth is a common phenomenon in most ocean water. Most of satellite retrieval algorithms of the optical constitutes concentration are, however, based on the assumption of homogeneous ocean water, especially for empirical retrieval models, which are usually based on the statistical relation between the reflectance spectral of surface and the depth-averaged constitute concentration or that of a certain depth. Using the underwater optical radiative transfer model, the influences of vertically stratified concentration of chlorophyll and suspended sediment matter on the irradiance ratio at the depth of 0^- m are respectively analyzed. The two computation formulas of depth-weighted equivalent concentration of stratified water and their responding irradiance ratio at 0^- m depth are then compared. The results indicate that the primary error sources is the light penetration depth and the intensity of stratification: the deeper the penetration and the more distinct stratification, the greater the effect of stratified water on the value of irradiance ratio at 0^- m depth, as well as the error of depth-weighted equivalent concentration. Gordon’s computation results of equivalent concentration are more accurate, and the Zaneveld ’s results overestimate the equivalent concentration of stratified water.

Key words: stratified water bodies, Monte Carlo, weight function, depth-weighted equivalent concentration

中图分类号:

P733.3

黄二辉,杨燕明. 分层水体对表层辐照度比影响的蒙特卡罗分析 [J]. 热带海洋学报, 2012, 31(1): 42-49.

HUANG Er-hui,YANG Yan-ming. Analysis of influence of stratified water bodies on underwater irradiance ratio by Monte Carlo model [J]. Journal of Tropical Oceanography, 2012, 31(1): 42-49.

参考文献

[1] DENG Ming, LI Yan. Use of SeaWiFS imagery to detect three-dimensional distribution of suspended sediment [J]. International Journal of Remote Sensing, 2003, 24(3): 519-534. [2] G ordon H R. Estimation of the depth of sunlight penetration in the sea for remote sensing [J]. Applied Optics, 1975, 14(2): 413-416. [3] 刘英, 李国胜. 渤海海域 MODIS 波段衰减深度研究 [J]. 海洋学报, 2009, 31(3): 21-29. [4] Gordon H R. Remote sensing of optical properties in continuously stratified waters [J]. Applied Optical, 1978, 17(12): 1893-1897. [5] Gordon H R, Clark D K. Remote sensing optical properties of a stratified ocean: an improved interpretation [J]. Applied Optics, 1980, 19: 3428-3430. [6] Zaneveld J R V. Remotely sensed reflectance and its dependence on vertical structure: a theoretical derivation [J]. Applied Optics, 1982, 21(22): 4146-4150. [7] Gordon H R. Diffuse reflectance of the ocean: influence of non-uniform phytoplankton pigment profile [J]. Applied Optics, 1992, 31(12): 2116-2129. [8] Gordon H R. , Boynton G C. Radiance-irradiance inversion algorithm for estimating the absorption and backscattering coefficients of natural waters: vertically stratified water bodies [J]. Applied Optics, 1998, 37(18): 3386-3896. [9] Malgorzata S, Dariusz S. Effects of a nonuniform vertical profile of chlorophyll concentration on remote-sensing reflectance of the ocean [J]. Applied Optics, 2005, 44(9): 1735-1747. [10] Zaneveld J R, Barnard A, Boss A. Theoretical derivation of the depth average of remotely sensed optical parameters [J]. Optics Express, 2005, 13(22): 9052-9061. [11] Leathers R A, Downes T V, Davis C O, et al. Monte Carlo radiative transfer simulations for ocean optics: A practical guide[R]//Naval Research Laboratory. Report. NRL/MR/5660-04-8819, 2004: 1-50. [12] 唐军武. 海洋光学特性模拟与遥感模型 [D]. 北京: 中国科学院遥感应用技术研究所, 1999: 72-91. [13] Lewis M R, Cullen J J, Platt T. Phytoplankton and thermal structure of the upper ocean: consequences of non-uniformity in the chlorophyll profile [J]. Journal of Geophysical Research. 1983, 88: 2565-2570. [14] Platt T, Sathyendranath S, Caverhill C, et al. , Ocean primary production and available light: further algorithms for remote sensing [J]. Deep-Sea Research, 1988, 35: 855-879. [15] 韩丹岫. 黄东海悬浮物浓度垂向分布的统计分析与实验研究 [D]. 青岛: 中国科学院海洋研究所, 2006: 77-80. [16] Pope R M, Fry E S. Absorption spectrum (380-700 nm) of pure water. Ⅱ. Integrating cavity measurements [J]. Applied Optics, 1997, 36(33): 8710-8723. [17] Bukata R P, Jerome J H, Kondratyev K Y, et al. Optical Properties and Remote Sensing of Inland And Coastal Waters [M]. New York: Chemical Rubber Company Press, 1995: 154-235. [18] Petzold T J. Volume Scattering Functions for Selected Ocean Waters [R]. //Technical Report SIO 72–78. Scripps Institution of Oceanography, University of California, SanDiego, LaJolla, Calif, 1972: 1-79. [19] Mobley C D, Gentili B, Gordon H R, et al. Comparison of numerical models for computing under water light fields [J]. Applied Optics, 1993, 32(36): 7484-7504.

分层水体对表层辐照度比影响的蒙特卡罗分析

Analysis of influence of stratified water bodies on underwater irradiance ratio by Monte Carlo model

PDF (PC)

赞

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 13

Metrics

本文评价

推荐阅读 0

[1]	蔡建楠, 刘海龙, 姜波, 陈吟晖, 李杰鸿, 吴思晓, 梁建霞, 黄华, 邢前国. 珠江口河网水体非光学活性水质参数高光谱反演[J]. 热带海洋学报, 2021, 40(1): 58-64.
[2]	张雨, 王桂芬, 许占堂, 杨跃忠, 周雯, 郑文迪, 曾凯, 邓霖. 基于浮标观测的东海赤潮高发区秋、冬季漫射衰减系数的反演[J]. 热带海洋学报, 2020, 39(5): 71-83.
[3]	郑文迪, 周雯, 曹文熙, 王桂芬, 邓霖, 徐文龙, 许占堂, 李彩, 蔡建南. 2016年夏季南海海盆水体颗粒物粒径分布特征*[J]. 热带海洋学报, 2018, 37(5): 74-85.
[4]	徐文龙, 王桂芬, 周雯, 许占堂, 曹文熙. 南海东北部夏季叶绿素a浓度垂向变化特征及其对水动力过程的响应^*[J]. 热带海洋学报, 2018, 37(5): 62-73.
[5]	王桂芬, 徐文龙, 周雯, 许占堂, 曹文熙. 基于船载走航观测高光谱颗粒物吸收系数反演浮游植物粒级结构*[J]. 热带海洋学报, 2018, 37(5): 50-61.
[6]	胡水波, 曹文熙, 王桂芬, 许占堂. 利用MODIS跟踪监测一个冷涡对海洋表层生物光学参数的影响^*[J]. 热带海洋学报, 2016, 35(3): 1-10.
[7]	刘素敏, 杨顶田. 海水酸化对鹿角珊瑚光谱特性影响的分析[J]. 热带海洋学报, 2014, 33(6): 41-47.
[8]	陈智杰, 姜泽毅, 张欣欣. 开放式光生物反应器内光传输数学模型研究[J]. 热带海洋学报, 2013, 32(6): 36-41.
[9]	李彩, 曹文熙, 柯天存, 周雯, 杨跃忠, 卢桂新, 郭超英, 王桂芬, 孙兆华. 水体体散射函数测量技术研究进展[J]. 热带海洋学报, 2013, 32(5): 65-72.
[10]	王林，赵冬至，杨建洪，姜玲玲，刘永健. 强壮前沟藻Amphidinium carterae Hulburt生消过程中水体总吸收特性研究[J]. 热带海洋学报, 2013, 32(2): 88-93.
[11]	王桂芬曹文熙 , 殷建平, 周雯孙兆华, 杨倩. 海洋颗粒有机碳浓度水色遥感研究进展[J]. 热带海洋学报, 2012, 31(6): 48-56.
[12]	周虹丽, 朱建华, 李铜基, 汪小勇. 中国近海非色素颗粒物的光学特性*[J]. 热带海洋学报, 2012, 31(6): 57-61.
[13]	叶海彬,杨顶田,杨超宇. 经验模态与小波分解在光学遥感内波参数提取中的应用[J]. 热带海洋学报, 2012, 31(2): 47-54.