Bio-optical characteristics of the Patagonia Shelf break waters: Implications for ocean color algorithms

被引:11
|
作者
Ferreira, Amabile [1 ]
Garcia, Carlos A. E. [1 ]
Dogliotti, Ana I. [2 ]
Garcia, Virginia M. T. [1 ]
机构
[1] Univ Fed Rio Grande FURG, Inst Oceanog, BR-96201900 Rio Grande, Brazil
[2] Inst Astron & Fis Espacio IAFE CONICET, Buenos Aires, DF, Argentina
关键词
Phytoplankton; Absorption; Scattering; Remote sensing reflectance; Patagonia; INHERENT OPTICAL-PROPERTIES; LIGHT-ABSORPTION; CASE-1; WATERS; BEAM ATTENUATION; CHLOROPHYLL-A; NATURAL PHYTOPLANKTON; ENGLISH-CHANNEL; SOUTH-PACIFIC; CELL-SIZE; VARIABILITY;
D O I
10.1016/j.rse.2013.05.022
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Bio-optical data for spring and summer phytoplankton blooms at 176 stations along the Patagonia Shelf break and adjacent areas were collected from October 2006 to January 2009 during six cruises. Data included chlorophyll-a concentration (Chla), coefficients of particulate absorption, a(p)(lambda), phytoplankton absorption, a(ph)(lambda), beam attenuation, c(p)(660), diffuse attenuation, K-d(lambda), and hyperspectral remote sensing reflectance, R-rs(lambda). Surface Chla varied within a wide range from 0.10 to 18.87 mg m(-3) (mean of 2.82 +/- 3.35), reflecting differences in both, the timing of the blooms and the geographical sampling area. Considerable dispersion was verified for a(p)(lambda), c(p)(660), and K-bio(440) (K-d(440) minus diffuse attenuation for pure water) as a function of Chla. A hierarchical cluster analysis (HCA) applied to the R-rs(lambda) spectra (N = 116) resulted in three classes ordered by spectral features that varied according to Chla. Class 1 (N = 22), Class 2 (N = 52), and Class 3 (N = 42) were grouped according to the R-rs(lambda) associated with Chla average of 0.86 (+/- 0.51), 2.42 (+/- 1.62), and 8.40 mg m(-3) (+/- 3.96), respectively. The estimation of Chla and a(ph)(lambda) by empirical and semi-analytical algorithms was evaluated using satellite data. Errors in the Chla estimates from the empirical algorithm OC4v6 using in situ R-rs(lambda) showed significant statistical relationships with Chla, a(ph)(440) / Chla, and b(p)(660) / Chla (where b(p)(660) = c(p)(660) - a(p)(660)). Although reasonable agreements were found between the measured and satellite-estimated values, the dependence of the OC4v6 errors on the Chla-specific phytoplankton absorption and particulate scattering coefficients reinforces the need to regionally refine both empirical and semi-analytical algorithms to improve satellite estimates of the bio-optical variables for the Patagonia region. (C) 2013 Elsevier Inc. All rights reserved.
引用
收藏
页码:416 / 432
页数:17
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