Výsledky vyhledávání

Numerical simulation of the interaction between ammonium nitrate aerosol and convective boundary-layer dynamics

Autor: Barbaro, E., Krol, M. C., de Arellano, J. Vila-Guerau, Marine and Atmospheric Research, Sub Atmospheric physics and chemistry

Publikováno v: Atmospheric Environment 105 (2015)
Atmospheric Environment, 105, 202. Elsevier Limited
Atmospheric Environment
Atmospheric Environment, 105, 202-211

We investigate the interaction between the ammonium nitrate aerosol ((NO3)-N-A) abundance and convective boundary-layer (CBL) dynamics by means of a large-eddy simulation (LES) framework In our LES model the CBL dynamics is solved coupled with radiat

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::868d60d1cf70752d9546c9e4f6c13268
https://doi.org/10.1016/j.atmosenv.2015.01.048

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Akademický článek

Tropospheric ozone over a tropical Atlantic station in the Northern Hemisphere: Paramaribo, Surinam (6°N, 55°W).

Autor: Peters, W.^1,2 Wouter.Peters@noaa.gov, Krol, M. C.¹, Fortuin, J. P. F.³, Kelder, H. M.³, Thompson, A. M.⁴, Becker, C. R.⁵, Lelieveld, J.⁶, Crutzen, P. J.⁶

Publikováno v: Tellus: Series B. Feb2004, Vol. 56 Issue 1, p21-34. 14p. 2 Diagrams, 8 Graphs.

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Akademický článek

Continuing emissions of methyl chloroform from Europe.

Autor: Krol, M. C., Lelieveld, J., Oram, D. E., Sturrock, G. A., Penkett, S. A., Brenninkmeijer, C. A. M., Gros, V., Williams, J., Scheeren, H. A.

Publikováno v: Nature. 1/9/2003, Vol. 421 Issue 6919, p131. 5p.

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What can (CO)-C-14 measurements tell us about OH?

Autor: Krol, M. C., Meirink, J. F., Bergamaschi, P., Mak, J. E., Lowe, D., Joeckel, P., Houweling, S., Roeckmann, T.

Publikováno v: Krol, M C, Meirink, J F, Bergamaschi, P, Mak, J E, Lowe, D, Joeckel, P, Houweling, S & Roeckmann, T 2008, ' What can (CO)-C-14 measurements tell us about OH? ', Atmospheric Chemistry and Physics, vol. 8, no. 16, pp. 5033-5044 . https://doi.org/10.5194/acp-8-5033-2008
Atmospheric Chemistry and Physics, 8(16), 5033-5044. European Geosciences Union

The possible use of (CO)-C-14 measurements to constrain hydroxyl radical (OH) concentrations in the atmosphere is investigated. (CO)-C-14 is mainly produced in the upper atmosphere from cosmic radiation. Measurements of (CO)-C-14 at the surface show

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::b31a28f50006a42097f6acbd4044b17d
https://doi.org/10.5194/acp-8-5033-2008

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Simulating the integrated summertime Delta(CO2)-C-14 signature from anthropogenic emissions over Western Europe

Autor: Bozhinova, D., van der Molen, M. K., van der Velde, Ivar, Krol, M. C., van der Laan, S., Meijer, H. A. J., Peters, W.

Publikováno v: Atmospheric Chemistry and Physics, 14(14), 7273-7290. COPERNICUS GESELLSCHAFT MBH

Radiocarbon dioxide (14CO2, reported in Δ14CO2) can be used to determine the fossil fuel CO2 addition to the atmosphere, since fossil fuel CO2 no longer contains any 14C. After the release of CO2 at the source, atmospheric transport causes dilution

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=narcis______::8bab40d9c64bc3860bc41ea57ce978e9
https://research.rug.nl/en/publications/bef5d8e6-e780-4497-8b61-f51c3c307c00

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The importance of crop growth modeling to interpret the Δ14CO2 signature of annual plants

Autor: Bozhinova, D., Combe, M., Palstra, S. W. L., Meijer, H. A. J., Krol, M. C., Peters, W.

Publikováno v: Global Biogeochemical Cycles, 27(3), 792-803. AMER GEOPHYSICAL UNION

The C-14/C abundance in CO2((CO2)-C-14) promises to provide useful constraints on regional fossil fuel emissions and atmospheric transport through the large gradients introduced by anthropogenic activity. The currently sparse atmospheric (CO2)-C-14 m

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=narcis______::8b42a587dc6a6fa25617c9490136359d
https://research.rug.nl/en/publications/067cd619-2ae5-4cfd-8397-a3d1f133dfce

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