How do phytoplankton respond to atmospheric
nitrogen deposition in the western North Atlantic, an area downwind of large agricultural and industrial centers?
Not exact matches
In an upcoming paper, Max Bothwell, a scientist at Environment Canada, proposed that climate change is one of four factors — along with atmospheric
deposition of
nitrogen from fossil fuel burning — boosting the blooms.
A substantial portion of the planet is greening
in response to increasing atmospheric carbon dioxide,
nitrogen deposition, global warming and land use change.
Glaser et al. show that dust
deposition mediated by frequent tropical storms was an important source of nutrients for the Everglades until about 2800 years ago, when a climatic shift
in the tropical Atlantic and Gulf of Mexico led to weather patterns that sharply decreased the level of dust inputs and led to a drier climate and a gradual loss of soil phosphorus, carbon, and
nitrogen.
By analyzing data from 270 monitoring sites around the country, Zhang and his colleagues found that the amount of
nitrogen deposition, as measured
in precipitation, had increased by 60 % — or 8 kilograms per hectare per year — between 1980 and 2010.
The flux of nutrients associated with this discharge consists of an annual median of three million tonnes of
nitrogen, twenty thousand of phosphorus, and three million of silica, which represent a magnitude of inorganic nutrients comparable to that of external sources traditionally considered
in marine studies, such as the atmospheric
deposition and riverine runoff.
Thus, past and future increases
in atmospheric
nitrogen deposition have the potential to alter the base of the marine food web; and,
in the long term, the structure of the ecosystem.
Given the likelihood that the magnitude of atmospheric
nitrogen deposition will continue to increase
in the future, the North Pacific Ocean could rapidly switch to having surplus nitrate.
Their analysis, which could discern human - derived
nitrogen from natural
nitrogen fixation, revealed that the oceanic nitrate concentration increased significantly over the last 30 years
in surface waters of the North Pacific due largely to the enhanced
deposition of
nitrogen from the atmosphere.
Their assessment revealed a consistent picture of increasing nitrate concentrations, the magnitude and pattern of which can only be explained by the observed increase
in atmospheric
nitrogen deposition.
«Fifty - four percent of that is fertilizer — the Haber - Bosch process; 11 percent is atmospheric
deposition — the plus side of pollution; 18 percent is
in situ fixation,» or
nitrogen - fixing cover crops, like legumes, Sanchez said.
Possible mechanisms include (iv) fertilization of phytoplankton growth
in the Southern Ocean by increased
deposition of iron - containing dust from the atmosphere after being carried by winds from colder, drier continental areas, and a subsequent redistribution of limiting nutrients; (v) an increase
in the whole ocean nutrient content (e.g., through input of material exposed on shelves or
nitrogen fixation); and (vi) an increase
in the ratio between carbon and other nutrients assimilated
in organic material, resulting
in a higher carbon export per unit of limiting nutrient exported.
Reduction of forest soil respiration
in response to
nitrogen deposition.
I'd suspect that a change
in soil microbiology might also change the way the soil holds onto water — and we know we're getting changes due to increased
deposition of
nitrogen, for example, from the air.
These forcings are spatially heterogeneous and include the effect of aerosols on clouds and associated precipitation [e.g., Rosenfeld et al., 2008], the influence of aerosol
deposition (e.g., black carbon (soot)[Flanner et al. 2007] and reactive
nitrogen [Galloway et al., 2004]-RRB-, and the role of changes
in land use / land cover [e.g., Takata et al., 2009].
According to the scientists, there is no evidence that trees are growing faster
in Panama, despite the «long - term increases
in nitrogen deposition and atmospheric carbon dioxide».
A research group led by the South Korean Pohang University has measured the effects of atmospheric and fluvial
nitrogen deposition [through nitrate]
in the coastal seas around China, Korea and Japan.
Here we construct a database of worldwide RS observations matched with high - resolution historical climate data and find a previously unknown temporal trend
in the RS record after accounting for mean annual climate, leaf area,
nitrogen deposition and changes
in CO2 measurement technique.
The relationship between N2O fluxes and NO3 — concentrations is consistent with observations from small streams (Baulch et al. 2011) as well as observed positive relationships between concentrations of N2O and NO3 —
in reservoirs (Beaulieu et al. 2015) and
in lakes receiving atmospheric
nitrogen deposition (McCrackin and Elser 2011).
However,
in many developing regions, an increase
in nitrogen deposition is projected for the end of the 21st century, mostly related to the projected increases
in NH3 emissions due to agricultural activities.
Increased uptake
in the past decade may be a consequence of a reduced rate of deforestation [217] and fertilization of the biosphere by atmospheric CO2 and
nitrogen deposition [187].
Modeling and field studies confirm a major role of
nitrogen deposition, working
in concert with CO2 fertilization,
in causing a large increase
in net primary productivity of temperate and boreal forests.
Scientific confidence of the occurrence of climate change include, for example, that over at least the last 50 years there have been increases
in the atmospheric concentration of CO2; increased
nitrogen and soot (black carbon)
deposition; changes
in the surface heat and moisture fluxes over land; increases
in lower tropospheric and upper ocean temperatures and ocean heat content; the elevation of sea level; and a large decrease
in summer Arctic sea ice coverage and a modest increase
in Antarctic sea ice coverage.
Reduction of forest soil respiration
in response to
nitrogen deposition.
These human forcings include greenhouse gas emissions (e.g. CO2, methane, CFCs), aerosol emissions and
deposition [e.g., black carbon (soot), sulfates, and reactive
nitrogen], and changes
in land use and land cover.
Globally, biodiversity (represented by species richness and relative abundance) may decrease by 13 to 19 % due to a combination of land - use change, climate change and
nitrogen deposition under four scenarios by 2050 relative to species present
in 1970 (Duraiappah et al., 2005).
In freshwater systems, acidifying depositions occur following the release of nitrogen oxides (NOx) and sulfur dioxide (SO2) into the atmosphere, mainly from the combustion of fossil fuels, which then may fall in dry or wet for
In freshwater systems, acidifying
depositions occur following the release of
nitrogen oxides (NOx) and sulfur dioxide (SO2) into the atmosphere, mainly from the combustion of fossil fuels, which then may fall
in dry or wet for
in dry or wet form.
«We got exactly the same results when we applied CO2 alone, but when we factored
in realistic treatments — warming, changes
in nitrogen deposition, changes
in precipitation — growth was actually suppressed.»
Beyond health, additional impacts of emissions such as ocean acidification, biodiversity loss, ecosystem impacts of
nitrogen deposition, and changes
in visibility are omitted, suggesting that these damages are conservative and leaving ample opportunities to further improve the comprehensiveness of social cost metrics.
The climate feedbacks involved with these changes, which are key
in understanding the climate system as a whole, include: + the importance of aerosol absorption on climate + the impact of aerosol deposition which affects biology and, hence, emissions of aerosols and aerosol precursors via organic nitrogen, organic phosphorus and iron fertilization + the importance of land use and land use changes on natural and anthropogenic aerosol sources + the SOA sources and impact on climate, with special attention on the impact human activities have on natural SOA formation In order to quantitatively answer such questions I perform simulations of the past, present and future atmospheres, and make comparisons with measurements and remote sensing data, all of which help understand, evaluate and improve the model's parameterizations and performance, and our understanding of the Earth syste
in understanding the climate system as a whole, include: + the importance of aerosol absorption on climate + the impact of aerosol
deposition which affects biology and, hence, emissions of aerosols and aerosol precursors via organic
nitrogen, organic phosphorus and iron fertilization + the importance of land use and land use changes on natural and anthropogenic aerosol sources + the SOA sources and impact on climate, with special attention on the impact human activities have on natural SOA formation
In order to quantitatively answer such questions I perform simulations of the past, present and future atmospheres, and make comparisons with measurements and remote sensing data, all of which help understand, evaluate and improve the model's parameterizations and performance, and our understanding of the Earth syste
In order to quantitatively answer such questions I perform simulations of the past, present and future atmospheres, and make comparisons with measurements and remote sensing data, all of which help understand, evaluate and improve the model's parameterizations and performance, and our understanding of the Earth system.