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新喀里多尼亚泻湖及开阔海域水体内生源光学特性及其叶绿素浓度卫星反演。

Inherent optical properties and satellite retrieval of chlorophyll concentration in the lagoon and open ocean waters of New Caledonia.

机构信息

Université de la Méditerranée, IRD, UR Camelia, BP A5, 98848 Nouméa Cedex, New Caledonia.

出版信息

Mar Pollut Bull. 2010;61(7-12):503-18. doi: 10.1016/j.marpolbul.2010.06.039. Epub 2010 Aug 4.

Abstract

The retrieval of chlorophyll-a concentration from remote sensing reflectance (Rrs) data was tested with the NASA OC4v4 algorithm on the inner New Caledonian lagoon (Case 2) and adjacent open ocean (Case 1) waters. The input to OC4v4 was Rrs measured in situ or modeled from water's inherent optical properties (2001-2007). At open ocean stations, backscattering and absorption coefficients were correlated with chlorophyll (R(2)=0.31-0.51, respectively), in agreement with models for Case 1 waters. Taking spectrofluorometric measurement as reference, the OC4v4 model leads to an average underestimation of 33% of the chlorophyll concentration. For the lagoon waters, OC4v4 performed inadequately because the backscattering coefficient, highly correlated with turbidity and suspended matter (R(2)=0.98), was poorly correlated to chlorophyll (R(2)=0.42). The OC4v4 performance was better in deep lagoon waters for stations with a TDT index (Tchla x depth/turbidity) higher than 19 mg m(-2) NTU(-1) (R(2)=0.974, bias=10.2%). Global Imager Rrs provided a good estimate of Tchla (R(2)=0.79, N=28) in the deeper part of the lagoon.

摘要

利用 NASA OC4v4 算法对新喀里多尼亚泻湖内部(案例 2)和相邻开阔海域(案例 1)的遥感反射率(Rrs)数据进行了叶绿素-a 浓度反演测试。OC4v4 的输入是在现场测量或根据水体固有光学特性建模的 Rrs(2001-2007 年)。在开阔海域站,后向散射和吸收系数与叶绿素呈正相关(分别为 R²=0.31-0.51),与案例 1 水域的模型一致。以光谱荧光测量为参考,OC4v4 模型导致叶绿素浓度的平均低估了 33%。对于泻湖水域,OC4v4 的性能不佳,因为与浊度和悬浮物高度相关的后向散射系数(R²=0.98)与叶绿素的相关性较差(R²=0.42)。对于 TDT 指数(Tchla x 深度/浊度)高于 19 mg m⁻² NTU⁻¹的站,OC4v4 在深泻湖水域的性能更好(R²=0.974,偏差=10.2%)。在泻湖较深的区域,全球成像仪的 Rrs 能够很好地估算 Tchla(R²=0.79,N=28)。

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