Deposition of dinitrogen pentoxide, N 2 O 5 , to the snowpack at high latitudes
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Abstract
Abstract. Dinitrogen pentoxide, N2O5, is an important nighttime intermediate in the oxidation of NOx that is hydrolysed on surfaces. We conducted a field campaign in Fairbanks, Alaska during November 2009 to measure the gradient and derive a flux (and deposition velocity) of N2O5 depositing to snowpack using the aerodynamic gradient method. The deposition velocity of N2O5 under Arctic winter conditions was found to be 0.59 ± 0.47 cm s−1, which is the first measurement of this parameter to our knowledge. Based on the measured deposition velocity, we compared the chemical loss rate of N2O5 via snowpack deposition to the total steady state loss rate and found that deposition to snowpack is at least 1/8th of the total chemical removal of N2O5 that is located within the first few meters above the ground surface.
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As urban-polluted air transports away from the city and mixes with ozone-rich air, nocturnal nitrogen oxide chemistry becomes active, leading to deposition of nitric acid and particulate nitrate.
“As urban-polluted air transports away from the city and mixes with ozone-rich air, nocturnal nitrogen oxide chemistry becomes active (Apodaca et al., 2008; Huff et al., 2011) leading to deposition of nitric acid and particulate nitrate.”
From Local Arctic Air Pollution: A Neglected but Serious Problem (2018) · cites this paper as Huff et al., 2011
The Introduction (page not provided) describes nighttime oxidation of NO₂ by ozone, formation of N₂O₅, and its conversion to nitric acid. The paper also reports polluted air moving from Fairbanks to its field site, but does not establish mixing with ozone-rich air or deposition of both nitric acid and particulate nitrate; its Conclusions concern deposition of N₂O₅ to snow. (LLM, conf=0.84)
Experimental — accuracy not yet measuredHeterogeneous reactions can also occur on ice particles and at the snow surface, leading to deposition of N2O5.
“Heterogeneous reactions can also occur on ice particles and at the snow surface, leading to deposition of N2O5 (Apodaca et al., 2008; Huff et al., 2011).”
From Local Arctic Air Pollution: A Neglected but Serious Problem (2018) · cites this paper as Huff et al., 2011
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- Andersen, H. V. and Hovmand, M. F.: Ammonia and nitric acid dry deposition and throughfall, 5 Water Air Soil Pollut., 85, 2211-2216, doi:10.1007/BF01186162, 1995. · DOI
- Anderson, P. S. and Neff, W. D.: Boundary layer physics over snow and ice, Atmos. Chem. Phys., 8, 3563-3582, doi:10.5194/acp-8-3563-2008, 2008. · DOI
- Apodaca, R. L., Huff, D. M., and Simpson, W. R.: The role of ice in N 2 O 5 heterogeneous hydrolysis at high latitudes, Atmos. Chem. Phys., 8, 7451-7463, doi:10.5194/acp-8-7451- 10 2008, 2008. · DOI
- Arya, S. P.: Introduction to micrometeorology, second ed., Academic press, 420 pp., 2001.
- Ayers, J. D. and Simpson, W. R.: Measurements of N 2 O 5 near Fairbanks, Alaska, J. Geophys. Res., 111, D14309, doi:10.1029/2006JD007070, 2006. · DOI · Paper page
- Bertram, T. H., Thornton, J. A., Riedel, T. P., Middlebrook, A. M., Bahreini, R., Bates, T. S., Quinn, P. K., and Coffman, D. J.: Direct observations of N 2 O 5 reactivity on ambient aerosol particles, Geophys. Res. Lett., 36, L19803, doi:10.1029/2009gl040248, 2009. · DOI
- Bertram, T. H. and Thornton, J. A.: Toward a general parameterization of N 2 O 5 reactivity on aqueous particles: the competing effects of particle liquid water, nitrate and chloride, Atmos. Chem. Phys., 9, 8351-8363, doi:10.5194/acp-9-8351-2009, 2009. · DOI
- Brown, S. S., Stark, H., Ciciora, S. J., and Ravishankara, A. R.: In-situ measurement of atmo- Williams, E. J., Kuster, W. C., Goldan, P. D., Angevine, W. M., Trainer, M., Fehsenfeld, F. C., and Ravishankara, A. R.: Vertical profiles in NO 3 and N 2 O 5 measured from an aircraft: Results from the NOAA P-3 and surface platforms during the New England air quality study 2004, J. Geophys. Res., 112, D22304, doi:10.1029/2007jd008883, 2007b. · DOI
- Bytnerowicz, A., Percy, K., Riechers, G., Padgett, P., and Krywult, M.: Nitric acid vapor effects on forest trees -deposition and cuticular changes, Chemosphere, 36, 697-702, doi:10.1016/S0045-6535(97)10110-2, 1998. · DOI
- Cadle, S. H., Dasch, J. M., and Mulawa, P. A.: Atmospheric concentrations and the deposition velocity to snow of nitric acid, sulfur dioxide and various particulate species, Atmos. Environ., 19, 1819-1827, doi:10.1016/0004-6981(85)90008-3, 1985. trogen deposition in the western united states, BioScience, 53, 404-420, doi:10.1641/0006- 3568(2003)053[0404:EEONDI]2.0.CO;2, 2003. · DOI
- Geyer, A. and Stutz, J.: Vertical profiles of NO 3 , N 2 O 5 , O 3 , and NO x in the nocturnal bound- ary layer: 2. Model studies on the altitude dependence of composition and chemistry, J. Geophys. Res., 109, D12307, doi:10.1029/2003jd004211, 2004. References Tables Figures Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | J. Atmos. Chem., 10, 427-449, doi:10.1007/bf00115784, 1990. · DOI
- Lovett, G. M.: Atmospheric deposition of nutrients and pollutants in North America: An ecolog- ical perspective, Ecol. Appl., 4, 630-650, doi:10.2307/1941997, 1994. · DOI
- Matsumoto, J., Imai, H., Kosugi, N., and Kajii, Y.: In situ measurement of N 2 O 5 in the urban at- mosphere by thermal decomposition/laser-induced fluorescence technique, Atmos. Environ., 39, 6802-6811, doi:10.1016/j.atmosenv.2005.07.055 2005. · DOI
- Mozurkewich, M. and Calvert, J. G.: Reaction probability of N 2 O 5 on aqueous aerosols, J. Geophys. Res., 93, 15889-15896, doi:10.1029/JD093iD12p15889, 1988. · DOI
- Nieuwstadt, F. T. M.: The turbulent structure of the stable, nocturnal boundary layer, J. Atmos. Sci., 41, 2202-2216, doi:10.1175/1520-0469(1984)041<2202:TTSOTS>2.0.CO;2, 1984. · DOI
- Pardyjak, E. R., Monti, P., and Fernando, H. J. S.: Flux richardson number measurements in stable atmospheric shear flows, J. Fluid Mech., 459, 307-316, doi:10.1017/S0022112002008406, 2002. · DOI
- Riemer, N., Vogel, H., Vogel, B., Schell, B., Ackermann, I., Kessler, C., and Hass, H.: Im- 20 pact of the heterogeneous hydrolysis of N 2 O 5 on chemistry and nitrate aerosol formation in the lower troposphere under photosmog conditions, J. Geophys. Res., 108(D4), 4144, doi:10.1029/2002jd002436, 2003. · DOI
- Roberts, J. M., Osthoff, H. D., Brown, S. S., and Ravishankara, A. R.: N 2 O 5 oxidizes chloride to Cl 2 in acidic atmospheric aerosol, Science, 321, 1059, doi:10.1126/science.1158777, 2008. · DOI
- Sommariva, R., Osthoff, H. D., Brown, S. S., Bates, T. S., Baynard, T., Coffman, D., de Gouw, J. A., Goldan, P. D., Kuster, W. C., Lerner, B. M., Stark, H., Warneke, C., Williams, E. J., Fehsenfeld, F. C., Ravishankara, A. R., and Trainer, M.: Radicals in the marine boundary P., Wolfe, G. M., Quinn, P. K., Middlebrook, A. M., Alexander, B., and Brown, S. S.: A large atomic chlorine source inferred from mid-continental reactive nitrogen chemistry, Nature, 464, 271-274, doi:10.1038/nature08905, 2009. · DOI · Paper page
- Van Doren, J. M., Watson, L. R., Davidovits, P., Worsnop, D. R., Zahniser, M. S., and Kolb, C. E.: Uptake of dinitrogen pentoxide and nitric acid by aqueous sulfuric acid droplets, J. Phys. 10 Chem., 95, 1684-1689, doi:10.1021/j100157a037, 1991. · DOI
- Watt, S. A., Wagner-Riddle, C., Edwards, G., and Vet, R. J.: Evaluating a flux-gradient approach for flux and deposition velocity of nitrogen dioxide over short-grass surfaces, Atmos. Environ., 38, 2619-2626, doi:10.1016/j.atmosenv.2004.02.021, 2004. · DOI
- Wesely, M. L. and Hicks, B. B.: A review of the current status of knowledge on dry deposition, 15 Atmos. Environ., 34, 2261-2282, doi:10.1016/j.atmosenv.2004.02.021, 2000. · DOI
- Wood, E. C., Bertram, T. H., Wooldridge, P. J., and Cohen, R. C.: Measurements of N 2 O 5 , NO 2 , and O 3 east of the San Francisco Bay, Atmos. Chem. Phys., 5, 483-491, doi:10.5194/acp-5- 483-2005, 2005. · DOI
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Self-citation
- Authors
- Huff, D. M., Joyce, P. L., Fochesatto, G. J., & Simpson, W. R.
- Affiliations
- University of Alaska Fairbanks (US)
- Venue
- Atmospheric Chemistry and Physics
- Publisher
- Copernicus GmbH
- Published
- 2011-05-26
- Volume
- 11
- Issue
- 10
- Pages
- 4929-4938
- ISSN
- 1680-7316 (ISSN-L)
- 1680-7324
- OpenAlex
- W2125854225
- Cited by
- 27
- References
- 0
- Citations by year
- 2026: 2 · 2025: 3 · 2024: 1 · 2023: 1 · 2022: 1 · 2021: 1 · 2020: 2 · 2019: 1 · 2018: 1 · 2017: 2 · 2016: 1 · 2015: 3 · 2014: 4 · 2013: 1 · 2012: 3
- FWCI
- 1.53
- Type
- journal article
- Language
- en
- Open access
- gold
- doi.org
- Licence
- Locations
- Atmospheric chemistry and physics (publishedVersion, cc-by)
- DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion, cc-by-sa)
- Funders
- National Science Foundation (0926220)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric chemistry and aerosols
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric Ozone and Climate
- Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric aerosols and clouds
- Keywords
- dinitrogen pentoxide, snowpack, deposition velocity, Arctic winter, NOx oxidation, atmospheric chemistry, Fairbanks, Alaska
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