Zobrazeno 1 - 10
of 252
pro vyhledávání: '"B Gioli"'
Publikováno v:
Environmental Research Letters, Vol 13, Iss 6, p 064014 (2018)
Vegetation has a substantial impact on the local climate. Land cover changes through afforestation or deforestation can amplify or mitigate climate warming by changes in biophysical and biogeochemical mechanisms. In the montane to subalpine area of t
Externí odkaz:
https://doaj.org/article/2a7b5fe665824b5c979139d629cdb5c4
Publikováno v:
Environmental Research Letters, Vol 11, Iss 4, p 044021 (2016)
Mountain regions and the important ecosystem services they provide are considered to be very vulnerable to the current warming, and recent studies suggest that high-mountain environments experience more rapid changes in temperature than environments
Externí odkaz:
https://doaj.org/article/281f78c0f77649cfbcb3a532cadfe340
Autor:
L. Brilli, P. Toscano, F. Carotenuto, S. Di Lonardo, P. Di Tommasi, V. Magliulo, A. Manco, L. Vitale, A. Zaldei, B. Gioli
Publikováno v:
Heliyon, Vol 10, Iss 8, Pp e29356- (2024)
Landfills play a key role as greenhouse gas (GHGs) emitters, and urgently need assessment and management plans development to swiftly reduce their climate impact. In this context, accurate emission measurements from landfills under different climate
Externí odkaz:
https://doaj.org/article/2efd3caac3c345f18613f93d0dcadca2
Autor:
F. Carotenuto, T. Georgiadis, B. Gioli, C. Leyronas, C. E. Morris, M. Nardino, G. Wohlfahrt, F. Miglietta
Publikováno v:
Atmospheric Chemistry and Physics, Vol 17, Pp 14919-14936 (2017)
Microbial aerosols (mainly composed of bacterial and fungal cells) may constitute up to 74 % of the total aerosol volume. These biological aerosols are not only relevant to the dispersion of pathogens, but they also have geochemical implications.
Externí odkaz:
https://doaj.org/article/6cc3e610065845deb6852721bcb538be
Akademický článek
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Autor:
S. Sabbatini, N. Arriga, T. Bertolini, S. Castaldi, T. Chiti, C. Consalvo, S. Njakou Djomo, B. Gioli, G. Matteucci, D. Papale
Publikováno v:
Biogeosciences, Vol 13, Iss 1, Pp 95-113 (2016)
The production of bioenergy in Europe is one of the strategies conceived to reduce greenhouse gas (GHG) emissions. The suitability of the land use change from a cropland (REF site) to a short-rotation coppice plantation of hybrid poplar (SRC site) wa
Externí odkaz:
https://doaj.org/article/e6ac84effbbf481d8367e2900b0061d8
Autor:
P. Kountouris, C. Gerbig, K.-U. Totsche, A. J. Dolman, A. G. C. A. Meesters, G. Broquet, F. Maignan, B. Gioli, L. Montagnani, C. Helfter
Publikováno v:
Biogeosciences, Vol 12, Iss 24, Pp 7403-7421 (2015)
Assigning proper prior uncertainties for inverse modelling of CO2 is of high importance, both to regularise the otherwise ill-constrained inverse problem and to quantitatively characterise the magnitude and structure of the error between prior and "t
Externí odkaz:
https://doaj.org/article/74b0a5a5bf6f488882a3d3b2f9763e7e
Autor:
C. Darbieu, F. Lohou, M. Lothon, J. Vilà-Guerau de Arellano, F. Couvreux, P. Durand, D. Pino, E. G. Patton, E. Nilsson, E. Blay-Carreras, B. Gioli
Publikováno v:
Atmospheric Chemistry and Physics, Vol 15, Iss 17, Pp 10071-10086 (2015)
We investigate the decay of planetary boundary layer (PBL) turbulence in the afternoon, from the time the surface buoyancy flux starts to decrease until sunset. Dense observations of mean and turbulent parameters were acquired during the Boundary Lay
Externí odkaz:
https://doaj.org/article/e267a2652f094696987da5a62cfca18c
Autor:
H. P. Pietersen, J. Vilà-Guerau de Arellano, P. Augustin, A. van de Boer, O. de Coster, H. Delbarre, P. Durand, M. Fourmentin, B. Gioli, O. Hartogensis, F. Lohou, M. Lothon, H. G. Ouwersloot, D. Pino, J. Reuder
Publikováno v:
Atmospheric Chemistry and Physics, Vol 15, Iss 8, Pp 4241-4257 (2015)
We study the influence of the large-scale atmospheric contribution to the dynamics of the convective boundary layer (CBL) in a situation observed during the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) field campaign. We employ two mo
Externí odkaz:
https://doaj.org/article/144dc157f9db4d23afabb1e7aed73497
Autor:
M. Lothon, F. Lohou, D. Pino, F. Couvreux, E. R. Pardyjak, J. Reuder, J. Vilà-Guerau de Arellano, P Durand, O. Hartogensis, D. Legain, P. Augustin, B. Gioli, D. H. Lenschow, I. Faloona, C. Yagüe, D. C. Alexander, W. M. Angevine, E Bargain, J. Barrié, E. Bazile, Y. Bezombes, E. Blay-Carreras, A. van de Boer, J. L. Boichard, A. Bourdon, A. Butet, B. Campistron, O. de Coster, J. Cuxart, A. Dabas, C. Darbieu, K. Deboudt, H. Delbarre, S. Derrien, P. Flament, M. Fourmentin, A. Garai, F. Gibert, A. Graf, J. Groebner, F. Guichard, M. A. Jiménez, M. Jonassen, A. van den Kroonenberg, V. Magliulo, S. Martin, D. Martinez, L. Mastrorillo, A. F. Moene, F. Molinos, E. Moulin, H. P. Pietersen, B. Piguet, E. Pique, C. Román-Cascón, C. Rufin-Soler, F. Saïd, M. Sastre-Marugán, Y. Seity, G. J. Steeneveld, P. Toscano, O. Traullé, D. Tzanos, S. Wacker, N. Wildmann, A. Zaldei
Publikováno v:
Atmospheric Chemistry and Physics, Vol 14, Iss 20, Pp 10931-10960 (2014)
Due to the major role of the sun in heating the earth's surface, the atmospheric planetary boundary layer over land is inherently marked by a diurnal cycle. The afternoon transition, the period of the day that connects the daytime dry convective boun
Externí odkaz:
https://doaj.org/article/341938db44f1413b81fb462fc9976a1d