Výsledky vyhledávání - "Klaassen, W."

Akademický článek

Fetch requirements near a forest edge

Autor: van Breugel, P.B., Klaassen, W., Moors, E.J.

Publikováno v: In Physics and Chemistry of the Earth, Part B 1999 24(1-2):125-131

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Akademický článek

Landscape Roughness Parameters for Sherwood Forest – Validation of Aggregation Models.

Autor: Bottema, M.¹, Klaassen, W.¹, Hopwood, W. P.²

Publikováno v: Boundary-Layer Meteorology. Nov1998, Vol. 89 Issue 2, p317-347. 31p.

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Akademický článek

Landscape Roughness Parameters for Sherwood Forest – Experimental Results.

Autor: Bonttema, M.¹, Klaassen, W.¹, Hopwood, W. P.²

Publikováno v: Boundary-Layer Meteorology. Nov1998, Vol. 89 Issue 2, p285-316. 32p.

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Micrometeorology of air/sea fluxes of carbon dioxide and dimethylsulphide

Autor: Stoll MHC, Baar de HJW, Zemmelink HJ, Klaassen W, Gieskes WWC, NOP

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Externí odkaz: https://explore.openaire.eu/search/publication?articleId=narcis______::873104e8128b40f71e9d0e516145e662
http://hdl.handle.net/10029/258273

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Fluxes and gas transfer rates of the biogenic trace gas DMS derived from atmospheric gradients

Autor: Zemmelink, H. J., Dacey, J. W. H., Hintsa, E. J., McGillis, W. R., Gieskes, W. W. C., Klaassen, W., de Groot, Henk, de Baar, H. J. W.

Publikováno v: Journal of geophysical research-Oceans, 109(C8):ARTN C08S10, 1-8. AMER GEOPHYSICAL UNION

[1] Gas transfer rates were determined from vertical profile measurements of atmospheric dimethylsulfide (DMS) gradients over the equatorial Pacific Ocean obtained during the GasEx-2001 cruise. A quadratic relationship between gas transfer velocity a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=narcis______::6e4e09aef9fe4ae135edc99ab0f0f8b2
https://research.rug.nl/en/publications/777c973e-d6ce-42ab-bc4f-038143abc257

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The contribution of ocean-leaving DMS to the global atmospheric burdens of DMS, MSA, SO2, and NSS SO4=

Autor: Gondwe, M., Krol, M., Gieskes, W., Klaassen, W., de Baar, H.

Publikováno v: Global Biogeochemical Cycles, 17(2):1056, 1-18. AMER GEOPHYSICAL UNION

[1] The contribution of ocean-derived DMS to the atmospheric burdens of a variety of sulphur compounds (DMS, MSA, SO2, and nss SO4=) is quantified from season to season. Such quantification, especially for nss SO4= (the climate-relevant product of DM

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=narcis______::e58408035db92e0f09dd7f429e3c540e
https://research.rug.nl/en/publications/df47abaa-008f-4665-b129-dc526a0ea86b

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