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Articles, 2 registres trobats
Articles 2 registres trobats  
1.
21 p, 4.0 MB ORCHIDEE-SOM : modeling soil organic carbon (SOC) and dissolved organic carbon (DOC) dynamics along vertical soil profiles in Europe / Camino Serrano, Marta (Centre de Recerca Ecològica i Aplicacions Forestals) ; Guenet, Bertrand (Laboratoire des Sciences du Climat et de l'Environnement) ; Luyssaert, Sebastiaan (University Amsterdam. Department of Ecological Sciences) ; Ciais, Philippe (Laboratoire des Sciences du Climat et de L’Environnement) ; Bastrikov, Vladislav (Laboratoire des Sciences du Climat et de L’Environnement) ; De Vos, Bruno (INBO. Research Institute for Nature and Forest) ; Gielen, Bert (University of Antwerp. Department of Biology) ; Gleixner, Gerd (Max Planck Institute for Biogeochemistry) ; Jornet-Puig, Albert (Laboratoire des Sciences du Climat et de l'Environment) ; Kaiser, Klaus (Martin Luther University. Soil Science and Soil Protection) ; Kothawala, Dolly (Evolutionary Biology Centre. Department of Limnology) ; Lauerwald, Ronny (University of Exeter. College of Engineering, Mathematics and Physical Sciences) ; Peñuelas, Josep (Centre de Recerca Ecològica i Aplicacions Forestals) ; Schrumpf, Marion (Max Planck Institute for Biogeochemistry) ; Vicca, Sara (Universiteit Antwerpen. Departement Biology) ; Vuichard, Nicolas (Laboratoire des Sciences du Climat et de l'Environment) ; Walmsley, David (Leuphana Universität Lüneburg. Institute of Ecology, Faculty of Sustainability) ; Janssens, Ivan A. (Universiteit Antwerpen. Departement Biology)
Current land surface models (LSMs) typically represent soils in a very simplistic way, assuming soil organic carbon (SOC) as a bulk, and thus impeding a correct representation of deep soil carbon dynamics. [...]
2018 - 10.5194/gmd-11-937-2018
Geoscientific model development, Vol. 11, issue 3 (March 2018) , p. 937-957  
2.
17 p, 3.5 MB Representation of dissolved organic carbon in the JULES land surface model (vn4.4_JULES-DOCM) / Nakhavali, Mahdi (University of Exeter. College of Engineering, Mathematics, and Physical Sciences) ; Friedlingstein, Pierre (University of Exeter. College of Engineering, Mathematics and Physical Sciences) ; Lauerwald, Ronny (University of Exeter. College of Engineering, Mathematics and Physical Sciences) ; Tang, Jing (Københavns universitet. Department of Biology) ; Chadburn, Sarah (University of Exeter. College of Engineering, Mathematics and Physical Sciences) ; Camino Serrano, Marta (Centre de Recerca Ecològica i Aplicacions Forestals) ; Guenet, Bertrand (Laboratoire des Sciences du Climat et de l'Environnement) ; Harper, Anna B. (University of Exeter. College of Engineering, Mathematics, and Physical Science) ; Walmsley, David (Leuphana Universität Lüneburg) ; Peichl, Matthias (Sveriges lantbruksuniversitet) ; Gielen, Bert (University of Antwerp. Department of Biology)
Current global models of the carbon (C) cycle consider only vertical gas exchanges between terrestrial or oceanic reservoirs and the atmosphere, thus not considering the lateral transport of carbon from the continents to the oceans. [...]
2018 - 10.5194/gmd-11-593-2018
Geoscientific model development, Vol. 11 (2018) , p. 593–609,  

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