Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/22639
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Spatial variability of absorption coefficients over a biogeochemical gradient in a large and optically complex shallow lake
Other Titles: Light absorption in Lake Balaton
Authors: Riddick, Caitlin
Hunter, Peter
Tyler, Andrew
Martinez-Vicente, Victor
Horvath, Hajnalka
Kovacs, Attila W
Voros, Lajos
Preston, Tom
Presing, Matyas
Contact Email: p.d.hunter@stir.ac.uk
Keywords: absorption
IOPs
chlorophyll-a
phycocyanin
phytoplankton
Lake Balaton
Issue Date: Oct-2015
Publisher: Wiley-Blackwell
Citation: Riddick C, Hunter P, Tyler A, Martinez-Vicente V, Horvath H, Kovacs AW, Voros L, Preston T & Presing M (2015) Spatial variability of absorption coefficients over a biogeochemical gradient in a large and optically complex shallow lake, Journal of Geophysical Research: Oceans, 120 (10), pp. 7040-7066.
Abstract: In order to improve robustness of remote sensing algorithms for lakes, it is vital to understand the variability of inherent optical properties (IOPs) and their mass-specific representations (SIOPs). In this study, absorption coefficients for particulate and dissolved constituents were measured at 38 stations distributed over a biogeochemical gradient in Lake Balaton, Hungary. There was a large range of phytoplankton absorption (a ph(λ)) over blue and red wavelengths (aph(440) = 0.11–4.39 m−1, aph(675) = 0.048–2.52 m−1), while there was less variability in chlorophyll-specific phytoplankton absorption (a*ph(λ)) in the lake (a*ph(440) = 0.022 ± 0.0046 m2mg−1, a*ph(675) = 0.010 ± 0.0020 m2mg−1) and adjoining wetland system, Kis-Balaton (a*ph(440) = 0.017 ± 0.0015 m2mg−1, a*ph(675) = 0.0088 ± 0.0017 m2mg−1). However, in the UV, a*ph(350) significantly increased with increasing distance from the main inflow (Zala River). This was likely due to variable production of photoprotective pigments (e.g., MAAs) in response to the decreasing gradient of colored dissolved organic matter (CDOM). The slope of CDOM absorption (SCDOM) also increased from west to east due to larger terrestrial CDOM input in the western basins. Absorption by nonalgal particles (aNAP(λ)) was highly influenced by inorganic particulates, as a result of the largely mineral sediments in Balaton. The relative contributions to the absorption budget varied more widely than oceans with a greater contribution from NAP (up to 30%), and wind speed affected the proportion attributed to NAP, phytoplankton, or CDOM. Ultimately, these data provide knowledge of the heterogeneity of (S)IOPs in Lake Balaton, suggesting the full range of variability must be considered for future improvement of analytical algorithms for constituent retrieval in inland waters.
Type: Journal Article
URI: http://hdl.handle.net/1893/22639
DOI Link: http://dx.doi.org/10.1002/2015JC011202
Rights: This item has been embargoed for a period. During the embargo please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study. Publisher policy allows this work to be made available in this repository. Published as Riddick, C. A. L., P. D. Hunter, A. N. Tyler, V. Martinez-Vicente, H. Horváth, A. W. Kovács, L. Vörös, T. Preston, and M. Présing (2015), Spatial variability of absorption coefficients over a biogeochemical gradient in a large and optically complex shallow lake, J. Geophys. Res. Oceans, 120, 7040–7066, doi:10.1002/2015JC011202. http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015JC011202/abstract
Affiliation: University of Stirling
Biological and Environmental Sciences
Biological and Environmental Sciences
Plymouth Marine Laboratory
Hungarian Academy of Sciences
Hungarian Academy of Sciences
Balaton Limnological Institute
Scottish Universities Environmental Research Centre
Hungarian Academy of Sciences

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