New production across the shelf-edge in the northeastern North Sea during the stratified summer period

Research output: Contribution to journalJournal articleResearchpeer-review

Standard

New production across the shelf-edge in the northeastern North Sea during the stratified summer period. / Bendtsen, Jørgen; Richardson, Katherine.

In: Journal of Marine Systems, Vol. 211, 103414, 2020.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Bendtsen, J & Richardson, K 2020, 'New production across the shelf-edge in the northeastern North Sea during the stratified summer period', Journal of Marine Systems, vol. 211, 103414. https://doi.org/10.1016/j.jmarsys.2020.103414

APA

Bendtsen, J., & Richardson, K. (2020). New production across the shelf-edge in the northeastern North Sea during the stratified summer period. Journal of Marine Systems, 211, [103414]. https://doi.org/10.1016/j.jmarsys.2020.103414

Vancouver

Bendtsen J, Richardson K. New production across the shelf-edge in the northeastern North Sea during the stratified summer period. Journal of Marine Systems. 2020;211. 103414. https://doi.org/10.1016/j.jmarsys.2020.103414

Author

Bendtsen, Jørgen ; Richardson, Katherine. / New production across the shelf-edge in the northeastern North Sea during the stratified summer period. In: Journal of Marine Systems. 2020 ; Vol. 211.

Bibtex

@article{c589e4d2aa28423a9c4d87c991f60f4b,
title = "New production across the shelf-edge in the northeastern North Sea during the stratified summer period",
abstract = "New production of organic matter from photosynthesis based on “new” nitrate transported into the illuminated surface layer fuels temperate ecosystems during periods of stratification when surface waters are nutrient limited. Published observations from the northeastern North Sea show a large spatial heterogeneity in vertical nitrate fluxes and suggest shelf edge mixing may be the major source for new production here during the stratified summer season. In the current study, we further investigate these empirical findings with a numerical model, where physical transports and mixing are evaluated against observations of temperature, salinity, nutrients and dissipation of turbulent kinetic energy. The relatively shallow central North Sea is separated from the deep Norwegian trench by a strong shelf edge current. This shelf edge frontal zone is characterized by a vertical separation of the surface and benthic boundary layers by an intermediate layer exhibiting low turbulence. A new nitrate assimilation model, driven by light and nitrate availability, is developed and applied for quantifying the potential for, and distribution of, new production in the area. New production in the frontal zone above the shelf edge is located in a narrow high productive (~100 mg C m−2 day−1) band. This is in qualitative accordance with observations. The model results also suggest, however, that new production of similar magnitude occurs above the deep Norwegian trench, where a shallow nutricline in combination with mesoscale eddy activity leads to increased transport of nitrate to the surface layer. Increased new production along the shelf edge could potentially impact ecosystem structure and may explain the relatively high species richness and fishing activity recorded in this part of the North Sea.",
keywords = "Biological pump, New production, Nitrate assimilation, North Sea, Regional modelling, Shelf edge",
author = "J{\o}rgen Bendtsen and Katherine Richardson",
year = "2020",
doi = "10.1016/j.jmarsys.2020.103414",
language = "English",
volume = "211",
journal = "Journal of Marine Systems",
issn = "0924-7963",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - New production across the shelf-edge in the northeastern North Sea during the stratified summer period

AU - Bendtsen, Jørgen

AU - Richardson, Katherine

PY - 2020

Y1 - 2020

N2 - New production of organic matter from photosynthesis based on “new” nitrate transported into the illuminated surface layer fuels temperate ecosystems during periods of stratification when surface waters are nutrient limited. Published observations from the northeastern North Sea show a large spatial heterogeneity in vertical nitrate fluxes and suggest shelf edge mixing may be the major source for new production here during the stratified summer season. In the current study, we further investigate these empirical findings with a numerical model, where physical transports and mixing are evaluated against observations of temperature, salinity, nutrients and dissipation of turbulent kinetic energy. The relatively shallow central North Sea is separated from the deep Norwegian trench by a strong shelf edge current. This shelf edge frontal zone is characterized by a vertical separation of the surface and benthic boundary layers by an intermediate layer exhibiting low turbulence. A new nitrate assimilation model, driven by light and nitrate availability, is developed and applied for quantifying the potential for, and distribution of, new production in the area. New production in the frontal zone above the shelf edge is located in a narrow high productive (~100 mg C m−2 day−1) band. This is in qualitative accordance with observations. The model results also suggest, however, that new production of similar magnitude occurs above the deep Norwegian trench, where a shallow nutricline in combination with mesoscale eddy activity leads to increased transport of nitrate to the surface layer. Increased new production along the shelf edge could potentially impact ecosystem structure and may explain the relatively high species richness and fishing activity recorded in this part of the North Sea.

AB - New production of organic matter from photosynthesis based on “new” nitrate transported into the illuminated surface layer fuels temperate ecosystems during periods of stratification when surface waters are nutrient limited. Published observations from the northeastern North Sea show a large spatial heterogeneity in vertical nitrate fluxes and suggest shelf edge mixing may be the major source for new production here during the stratified summer season. In the current study, we further investigate these empirical findings with a numerical model, where physical transports and mixing are evaluated against observations of temperature, salinity, nutrients and dissipation of turbulent kinetic energy. The relatively shallow central North Sea is separated from the deep Norwegian trench by a strong shelf edge current. This shelf edge frontal zone is characterized by a vertical separation of the surface and benthic boundary layers by an intermediate layer exhibiting low turbulence. A new nitrate assimilation model, driven by light and nitrate availability, is developed and applied for quantifying the potential for, and distribution of, new production in the area. New production in the frontal zone above the shelf edge is located in a narrow high productive (~100 mg C m−2 day−1) band. This is in qualitative accordance with observations. The model results also suggest, however, that new production of similar magnitude occurs above the deep Norwegian trench, where a shallow nutricline in combination with mesoscale eddy activity leads to increased transport of nitrate to the surface layer. Increased new production along the shelf edge could potentially impact ecosystem structure and may explain the relatively high species richness and fishing activity recorded in this part of the North Sea.

KW - Biological pump

KW - New production

KW - Nitrate assimilation

KW - North Sea

KW - Regional modelling

KW - Shelf edge

U2 - 10.1016/j.jmarsys.2020.103414

DO - 10.1016/j.jmarsys.2020.103414

M3 - Journal article

AN - SCOPUS:85088639894

VL - 211

JO - Journal of Marine Systems

JF - Journal of Marine Systems

SN - 0924-7963

M1 - 103414

ER -

ID: 249944930