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Reconsidering the change in global biosphere productivity between the Last Glacial Maximum and present day from the triple oxygen isotopic composition of air trapped in ice coresLANDAIS, A; LATHIERE, J; BARKAN, E et al.Global biogeochemical cycles. 2007, Vol 21, Num 1, issn 0886-6236, GB1025.1-GB1025.13Article

Future tropospheric ozone simulated with a climate-chemistry-biosphere modelHAUGLUSTAINE, D. A; LATHIERE, J; SZOPA, S et al.Geophysical research letters. 2005, Vol 32, Num 24, pp L24807.1-L24807.5, issn 0094-8276Article

Aerosol and ozone changes as forcing for climate evolution between 1850 and 2100SZOPA, Sophie; BALKANSKI, Y; IDELKADI, A et al.Climate dynamics. 2013, Vol 40, Num 9-10, pp 2223-2250, issn 0930-7575, 28 p.Article

Contribution of anthropogenic and natural sources to atmospheric methane variabilityBOUSQUET, P; CIAIS, P; LANGENFELDS, R. L et al.Nature (London). 2006, Vol 443, Num 7110, pp 439-443, issn 0028-0836, 5 p.Article

On the role of atmospheric chemistry in the global CO2 budgetFOLBERTH, G; HAUGLUSTAINE, D. A; CIAIS, P et al.Geophysical research letters. 2005, Vol 32, Num 8, pp L08801.1-L08801.4, issn 0094-8276Article

Past and future changes in biogenic volatile organic compound emissions simulated with a global dynamic vegetation modelLATHIERE, J; HAUGLUSTAINE, D. A; DE NOBLET-DUCOUDRE, N et al.Geophysical research letters. 2005, Vol 32, Num 20, pp L20818.1-L20818.4, issn 0094-8276Article

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