دانلود مقاله ISI انگلیسی شماره 96442
ترجمه فارسی عنوان مقاله

طبقه بندی بیو اپتیک فضایی-زمانی در آبهای نیمه استوائی پویا در غرب آمریکای شمالی

عنوان انگلیسی
Spatial-temporal bio-optical classification of dynamic semi-estuarine waters in western North America
کد مقاله سال انتشار تعداد صفحات مقاله انگلیسی
96442 2017 14 صفحه PDF
منبع

Publisher : Elsevier - Science Direct (الزویر - ساینس دایرکت)

Journal : Estuarine, Coastal and Shelf Science, Volume 199, 5 December 2017, Pages 35-48

پیش نمایش مقاله
پیش نمایش مقاله  طبقه بندی بیو اپتیک فضایی-زمانی در آبهای نیمه استوائی پویا در غرب آمریکای شمالی

چکیده انگلیسی

A large set of bio-optical data were collected as part of five research cruises and bi-weekly trips aboard a ship of opportunity in the west coast of Canada, to assess the spatial and temporal variability of above-water reflectance in this contrasted coastal environment. To accomplish this, in situ biophysical and optical measurements were collected in conjunction with above-water hyperspectral remote sensing reflectance (Rrs) at 145 stations. The concentrations of measured biophysical data varied considerably; chlorophyll a (Chla) (mean = 1.64, range: 0.10–7.20 μg l−1), total suspended matter (TSM) (3.09, 0.82–20.69 mg l−1), and absorption by chromophoric dissolved organic matter (CDOM) (acdom(443nm)) (0.525, 0.007–3.072 m-1), thus representing the spatio-temporal variability of the Salish Sea. Optically, a similar large range was also found; particulate scattering (bp(650nm)) (1.316, 0.250–7.450 m-1), particulate backscattering (bbp(650nm)) (0.022, 0.005–0.097 m-1), total beam attenuation coefficient (ct(650)) (1.675, 0.371–9.537 m-1) and particulate absorption coefficient (ap(650nm)) (0.345, 0.048–2.020 m-1). An empirical orthogonal function (EOF) analysis revealed that Rrs variability was highly correlated to bp (r = 0.90), bbp (r = 0.82) and concentration of TSM (r = 0.80), which highlighted the dominant role of water turbidity in this region. Hierarchical clustering analysis was applied to the normalized Rrs spectra to define optical water classes. Class 1 was defined by the highest Rrs values, particularly above 570 nm, indicating more turbid waters; Class 2 was dominated by high Chla and TSM concentrations, which is shown by high Rrs at 570 nm as well as fluorescence and absorption peaks; Class 3 shows strong fluorescence signatures accompanied by low TSM influence; and Class 4 is most representative of clear waters with a less defined absorption peak around 440 nm. By understanding the bio-optical factors which control the variability of the Rrs spectra this study aims to develop a sub-regional characterization of this coastal region aiming to improve bio-optical algorithms in this complex coastal area.