SNOOP. The effect of ship Nox deposition on cyanobacteria blooms. Marine Systems Institute at Tallinn University of Technology. Urmas Raudsepp. Aim. Additional atmospheric deposition of nitrogen caused by shipping likely
The effect of ship Nox deposition on cyanobacteria blooms
Marine Systems Institute at Tallinn University of Technology
Additional atmospheric deposition of nitrogen caused by shipping likely
result in changes of phytoplankton spring bloom and summer nitrogen-fixing
cyanobacteria bloom dynamics.
The task was to assess the degree of inter-annual variability of
spring and summer phytoplankton blooms and nitrogen fixation in
response to a shipnitrogen deposition on the background of
natural variability of environmental conditions in the Gulf of Finland.
Two 10-year runs with coupled3D physical and biological-chemical model were
performed using atmospheric deposition of NOx without ship deposition and including
ship deposition (year 2008).
Model domain was the whole Baltic Sea
Gulf of Finland
Blue line B along longitude 23º30’E marks the western boundary of the Gulf of
Finland basin in the present study
Model validation (monitoring station LL7)
D is mean of observations
M is mean of simulated data
SD is standard deviation
CFis cost function
Cost function definition (Eilola et al. 2009):
SD is standard deviation of observations
Cost function values:
0–1 indicate good result,
1–2 indicate reasonable result
and >2 indicate poor result.
The 10-year mean, standard deviation and cost function values of temperature (T, ºC), salinity (S), dissolved oxygen (O, ml l–1), nitrate (N, mmol m–3), phosphate (P, mmol m–3) for the surface (s) and near-bottom (b) layers and chlorophyll (Chl, mg m–3).
Atmospheric and ship NOx deposition to the Gulf in 2008
Monthly atmospheric NOx deposition (t N month–1) without ship deposition (black bars)
and ship NOx deposition (t N month–1) (shaded bars) to the Gulf of Finland area in 2008.
Annual atmospheric NOx deposition was 13.7 kton and ship NOx deposition
1.6 kton to the Gulf of Finland area.Annual ships NOx deposition is about 12%
from total atmospheric deposition.Ship NOx deposition is highestin May, June,
July and August(20-30%).
Distribution of annual ship NOx deposition (kg N km–2 y–1) to the Gulf of Finland area.
The annual ship NOx deposition was larger in the western and central Gulf
(up to 70 kg N km–2 y–1) compared to the eastern part (10-40 kg N km–2 y–1).
Winter nutrient conditions in the Gulf of Finlandupper layer
Mean winter ratio of dissolved inorganic nitrogen
to phosphorus (DIN:DIP) in the upper 10-m water
DIN:DIP ratio was low, varying inter-annually
from 8.5 to 11.5.
The increase of DIN:DIP ratio caused by ship
NOx deposition was minor (about 1%)
compared with natural variability.
Mean winter excess phosphate (eP=DIP–DIN/16)
in the upper 10-m layer.
Black bars show excess phosphate without ship
NOx deposition and shaded bars show excess
phosphate ship NOx deposition included.
The addition of ship NOx deposition reduced
excess phosphate from 1 to 2.5% depending
on DIN and DIP resources in the upper layer.
Annual phytoplankton primary production and nitrogen fixation
by cyanobacteria (in nitrogen units).
Annual primary production of phytoplankton over the Gulf area.
Green bars indicate phytoplankton production and blue bars nitrogen fixation by cyanobacteria.
Simulations performed without ship NOx deposition.
Note different scales.
Impact of ship NOx deposition on the phytoplankton primary production
and nitrogen fixationby cyanobacteria
Changes of the annual phytoplankton primary production (green bars) and
cyanobacteria nitrogen fixation (blue bars) caused by ship NOx deposition in
the Gulf water column.
Changes are calculated:
primary production with ships−primary production without ships
nitrogen fixation with ships − nitrogen fixation without ships.
10-year mean decrease of nitrogen fixation rate in the Gulf
Distribution of 10-year mean decreaseof nitrogen fixation rate
(ship NOx deposition included–without ship NOx deposition) in the Gulf of Finland
Annual averaged nitrogen fixation over the Gulf area was 1300 kg N km-2 y-1
The 10-year simulation with coupled hydrodynamic and ecological model
forced by ship NOx deposition showed changes in the dynamics of
phytoplankton spring bloom and summer N-fixing cyanobacteria bloom.
Due to the phytoplankton composition (green algae+cyanobacteria) the
annualtotal biomass in the Gulf is actually limited by phosphorus, i.e. the
increase of green algae primary production is practically compensated
by the decrease of nitrogen fixation by cyanobacteria.