2020
DOI: 10.1029/2019ef001453
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Greater Contribution From Agricultural Sources to Future Reactive Nitrogen Deposition in the United States

Abstract:  Agricultural NH3 emission will be the dominant source for atmospheric reactive nitrogen.  Additional nitrogen deposition will hinder the reduction of deposition to levels under critical loads.  Increasing agricultural NH3 emission will increase total nitrogen load in several protected remote watersheds.

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Cited by 4 publications
(5 citation statements)
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“…NH 3 column densities retrieved from IASI on board the Metop-A satellite are assimilated to constrain spatially resolved NH 3 emissions using the 2011 NEI as the a priori inventory (Clarisse et al, 2009;Van Damme et al, 2014;USEPA, 2014). The polar sun-synchronous satellite has a 12 km diameter footprint at nadir and a bidaily global coverage.…”
Section: Iasi-nh 3 Observationsmentioning
confidence: 99%
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“…NH 3 column densities retrieved from IASI on board the Metop-A satellite are assimilated to constrain spatially resolved NH 3 emissions using the 2011 NEI as the a priori inventory (Clarisse et al, 2009;Van Damme et al, 2014;USEPA, 2014). The polar sun-synchronous satellite has a 12 km diameter footprint at nadir and a bidaily global coverage.…”
Section: Iasi-nh 3 Observationsmentioning
confidence: 99%
“…Bottom-up inventories calculate the NH 3 emissions based on estimated activity levels and corresponding emission factors, both of which are subject to high uncertainties, particularly for agricultural sources, the major contributor (Cooter et al, 2012;McQuilling and Adams, 2015). Several studies have utilized NH 3 column density retrieved from the Infrared Atmospheric Sounding Interferometer (IASI) (Clarisse et al, 2009;Van Damme et al, 2015b) or the Atmospheric Infrared Sounder (AIRS; Warner et al, 2016) as well as the inferred surface mixing ratio of NH 3 from the Crosstrack Infrared Sounder (CrIS; Shephard et al, 2020) to characterize the spatiotemporal distribution of NH 3 . These satellite measurements are useful for supplementing emission inventories to identify and quantify underestimated or missing emission hotspots, especially in intensive agricultural zones (Van Damme et al, 2018;Dammers et al, 2019;Clarisse et al, 2019).…”
Section: Introductionmentioning
confidence: 99%
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“…Owing to abundant precipitation and reactive nitrogen deposition, the atmospheric wet nitrogen deposition in southwest China exceeds the average annual wet nitrogen deposition (NH 4 + -N and nitrate-N) fluxes in the country, measuring 15.8 ± 11.1 kg•N•hm −1 •yr −1 [47,48]. Hence, disparities in environmental N deposition result in variations in litter decomposition rates, and when atmospheric N deposition surpasses the capacity of forest ecosystems to retain N, N saturation transpires, consequently impeding litter decomposition, and the degree of nitrogen limitation in the local ecosystem determines this threshold [46,49]. To summarize, N addition level and environmental N deposition are two pivotal factors governing litter decomposition [50].…”
Section: Simulation Of the Effect Of Nitrogen Deposition On Litter De...mentioning
confidence: 99%
“…Additionally, 22.3% of black cherry trees in FIA plots are experiencing exceedances of their survival probability N CL (Figure 6). Many of these exceedances occur along the eastern side of the Mississippi River Basin where agricultural activities result in higher Nr deposition and in the North Carolina region where Nr deposition is high due to concentrated animal feeding operations (Chen et al, 2020). Some species (e.g., paper birch) have similar spatial distributions in probabilities of exceedance for growth rate and survival probability, while others (e.g., sugar maple) have a greater number of high probability exceedance locations for one ecological response (e.g., survival probability) but not the other.…”
Section: Spatially Varying Exceedances In N Clsmentioning
confidence: 99%