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Contrasting optical properties of surface waters across the Fram Strait and its potential biological implications. / Pavlov, A.K.; Granskog, M.A.; Stedmon, C.A.; Ivanov, B.V.; Hudson, S.R.; Falk-Petersen, S.

In: Journal of Marine Systems, 2015, p. 62-72.

Research output: Contribution to journal › Article

Harvard

Pavlov, AK, Granskog, MA, Stedmon, CA, Ivanov, BV, Hudson, SR & Falk-Petersen, S 2015, 'Contrasting optical properties of surface waters across the Fram Strait and its potential biological implications', Journal of Marine Systems, pp. 62-72. https://doi.org/10.1016/j.jmarsys.2014.11.001

APA

Pavlov, A. K., Granskog, M. A., Stedmon, C. A., Ivanov, B. V., Hudson, S. R., & Falk-Petersen, S. (2015). Contrasting optical properties of surface waters across the Fram Strait and its potential biological implications. Journal of Marine Systems, 62-72. https://doi.org/10.1016/j.jmarsys.2014.11.001

Vancouver

Pavlov AK, Granskog MA, Stedmon CA, Ivanov BV, Hudson SR, Falk-Petersen S. Contrasting optical properties of surface waters across the Fram Strait and its potential biological implications. Journal of Marine Systems. 2015;62-72. https://doi.org/10.1016/j.jmarsys.2014.11.001

Author

Pavlov, A.K. ; Granskog, M.A. ; Stedmon, C.A. ; Ivanov, B.V. ; Hudson, S.R. ; Falk-Petersen, S. / Contrasting optical properties of surface waters across the Fram Strait and its potential biological implications. In: Journal of Marine Systems. 2015 ; pp. 62-72.

BibTeX

@article{23cba1b8e6984bffae0fcaf3e8f51c7c,
title = "Contrasting optical properties of surface waters across the Fram Strait and its potential biological implications",
abstract = "Underwater light regime is controlled by distribution and optical properties of Colored Dissolved Organic Matter (CDOM) and particulate matter. Surface waters of the Fram Strait is a region where two contrasting water masses are found. Polar water in the East Greenland Current and Atlantic water in the West Spitsbergen Current differ with regards to temperature, salinity and other properties. We present data on absorption properties of CDOM and particles across the Fram Strait (along 79 °N) putting a special emphasis on a contrast observed in Polar and Atlantic waters in September 2009 and 2010. CDOM absorption in the Polar Water of the East Greenland Current was significantly higher (more than 3-fold) compared to Atlantic Water in the West Spitsbergen Current, with values (at 350 nm) of 0.565 ± 0.100 (in 2009) and 0.458 ± 0.117 (in 2010), and 0.138 ± 0.036 (in 2009) and 0.153 ± 0.039 (in 2010), for Polar and Atlantic waters respectively. At the same time, we observed different pattern in particle absorption",
keywords = "Colored dissolved organic matter (CDOM) Dissolved organic matter Light attenuation Optical properties Oceanic boundary layer Marine ecology Arctic Ocean Fram Strait",
author = "A.K. Pavlov and M.A. Granskog and C.A. Stedmon and B.V. Ivanov and S.R. Hudson and S. Falk-Petersen",
year = "2015",
doi = "10.1016/j.jmarsys.2014.11.001",
language = "English",
pages = "62--72",
journal = "Journal of Marine Systems",
issn = "0924-7963",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Contrasting optical properties of surface waters across the Fram Strait and its potential biological implications

AU - Pavlov, A.K.

AU - Granskog, M.A.

AU - Stedmon, C.A.

AU - Ivanov, B.V.

AU - Hudson, S.R.

AU - Falk-Petersen, S.

PY - 2015

Y1 - 2015

N2 - Underwater light regime is controlled by distribution and optical properties of Colored Dissolved Organic Matter (CDOM) and particulate matter. Surface waters of the Fram Strait is a region where two contrasting water masses are found. Polar water in the East Greenland Current and Atlantic water in the West Spitsbergen Current differ with regards to temperature, salinity and other properties. We present data on absorption properties of CDOM and particles across the Fram Strait (along 79 °N) putting a special emphasis on a contrast observed in Polar and Atlantic waters in September 2009 and 2010. CDOM absorption in the Polar Water of the East Greenland Current was significantly higher (more than 3-fold) compared to Atlantic Water in the West Spitsbergen Current, with values (at 350 nm) of 0.565 ± 0.100 (in 2009) and 0.458 ± 0.117 (in 2010), and 0.138 ± 0.036 (in 2009) and 0.153 ± 0.039 (in 2010), for Polar and Atlantic waters respectively. At the same time, we observed different pattern in particle absorption

AB - Underwater light regime is controlled by distribution and optical properties of Colored Dissolved Organic Matter (CDOM) and particulate matter. Surface waters of the Fram Strait is a region where two contrasting water masses are found. Polar water in the East Greenland Current and Atlantic water in the West Spitsbergen Current differ with regards to temperature, salinity and other properties. We present data on absorption properties of CDOM and particles across the Fram Strait (along 79 °N) putting a special emphasis on a contrast observed in Polar and Atlantic waters in September 2009 and 2010. CDOM absorption in the Polar Water of the East Greenland Current was significantly higher (more than 3-fold) compared to Atlantic Water in the West Spitsbergen Current, with values (at 350 nm) of 0.565 ± 0.100 (in 2009) and 0.458 ± 0.117 (in 2010), and 0.138 ± 0.036 (in 2009) and 0.153 ± 0.039 (in 2010), for Polar and Atlantic waters respectively. At the same time, we observed different pattern in particle absorption

KW - Colored dissolved organic matter (CDOM) Dissolved organic matter Light attenuation Optical properties Oceanic boundary layer Marine ecology Arctic Ocean Fram Strait

U2 - 10.1016/j.jmarsys.2014.11.001

DO - 10.1016/j.jmarsys.2014.11.001

M3 - Article

SP - 62

EP - 72

JO - Journal of Marine Systems

JF - Journal of Marine Systems

SN - 0924-7963

ER -

ID: 4003814