Emission Measurements of the Concorde Supersonic Aircraft in the Lower Stratosphere

Autor: Fahey, D. W., Keim, E. R., Boering, K. A., Brock, C. A., Wilson, J. C., Jonsson, H. H., Anthony, S., Hanisco, T. F., Wennberg, P. O., Miake-Lye, R. C., Salawitch, R. J., Louisnard, N., Woodbridge, E. L., Gao, R. S., Donnelly, S. G., Wamsley, R. C., Del Negro, L. A., Solomon, S., Daube, B. C., Wofsy, S. C., Webster, C. R., May, R. D., Kelly, K. K., Loewenstein, M., Podolske, J. R., Chan, K. R.

Publikováno v: Science, 1995 Oct 01. 270(5233), 70-74.

Externí odkaz: https://www.jstor.org/stable/2888214

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Can N 2 O stable isotopes and isotopomers be useful tools to characterize sources and microbial pathways of N 2 O production and consumption in tropical soils?

Autor: Park, S., Perez, T., Boering, K. A, Trumbore, S. E, Gil, J., Marquina, S., Tyler, S. C

Publikováno v: Park, S.; Perez, T.; Boering, K. A; Trumbore, S. E; Gil, J.; Marquina, S.; et al.(2011). Can N 2 O stable isotopes and isotopomers be useful tools to characterize sources and microbial pathways of N 2 O production and consumption in tropical soils?. Global Biogeochemical Cycles, 25(1), n/a-n/a. doi: 10.1029/2009GB003615. UC Irvine: Department of Earth System Science, UCI. Retrieved from: http://www.escholarship.org/uc/item/11n4z4cv

Nitrous oxide (N2O) is an important greenhouse gas in which the main sources are tropical rainforest and agricultural soils. N2O is produced in soils by microbial processes, which are enhanced by the application of nitrogenous fertilizers. The soil N

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______325::043913fb1fca83f21f556c7230f9cef7
http://www.escholarship.org/uc/item/11n4z4cv

Mechanisms responsible for high N2O emissions from subarctic permafrost peatlands studied via stable isotope techniques.

Autor: Gil, J., Pérez, T., Boering, K., Martikainen, P. J., Biasi, C.

Publikováno v: Global Biogeochemical Cycles; Jan2017, Vol. 31 Issue 1, p172-189, 18p

The distribution of hydrogen, nitrogen, and chlorine radicals in the lower stratosphere: Implications for changes in O_3 due to emission of NO_y from supersonic aircraft

Autor: Salawitch, R. J., Wofsy, S. C., Wennberg, P. O., Cohen, R. C., Anderson, J. G., Fahey, D. W., Gao, R. S., Keim, E. R., Woodbridge, E. L., Stimpfle, R. M., Koplow, J. P., Kohn, D. W., Webster, C. R., May, R. D., Pfister, L., Gottlieb, E. W., Michelsen, H. A., Yue, G. K., Wilson, J. C., Brock, C. A., Jonsson, H. H., Dye, J. E., Baumgardner, D., Proffitt, M. H., Loewenstein, M., Podolske, J. R., Elkins, J. W., Dutton, G. S., Hintsa, E. J., Dessler, A. E., Weinstock, E. M., Kelly, K. K., Boering, K. A., Daube, B. C., Chan, K. R., Bowen, S. W.

In situ measurements of hydrogen, nitrogen, and chlorine radicals obtained in the lower stratosphere during SPADE are compared to results from a photochemical model that assimilates measurements of radical precursors and environmental conditions. Mod

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od________38::5f139083610db2722251c861c3be1d15
https://resolver.caltech.edu/CaltechAUTHORS:20140716-091039510