Abondances of gram-negative bacteria in the environment - floodplains of the Ain, Doubs, and Loue Rivers - 2015-2016
19 sites (16 wetlands and 3 rivers) with different physicochemical characteristics and distributed along three rivers (Ain, Doubs, and Loue) were sampled. The abundances of some gram-negative bacteria (Escherichia coli, extended-spectrum beta-lactamase (ESBL)-producing Escherichia coli, Klebsiella ...
Physicochemical characteristics of water and sediment - Ain River floodplain - 2019-2020
34 sites (16 wetland sites, 15 river sites, and 3 groundwaters) distributed along the Ain River with different physicochemical characteristics were sampled. The physicochemical characteristics of the wetlands were measured in situ or after laboratory analysis.
Abondances and genotypic characteristics of gram-negative bacteria in the environment - Ain River floodplain - 2019-2020
34 sites (16 wetland sites, 15 river sites, and 3 groundwaters) distributed along the Ain River with different physicochemical characteristics were sampled. The abundances of some gram-negative bacteria (Escherichia coli, extended-spectrum beta-lactamase (ESBL)-producing E. coli, Klebsiella ...
Characterising low-mass dense cores with the Onsala 20m radiotelescope
The data set contains spectra of rotational emission of 12CO, 13CO, C18O (J=1-0), CS (2-1), and N2H+ (J=1-0) for 159 low-mass sources from the dense-core catalogue of the Galactic Cold Cores programme (Montillaud et al. 2015, A&A). The spectra were obtained by pointed observations using the Onsala ...
Downscaling CMIP5 climate projections over the Mont-Blanc Massif at a 200-m resolution
Statistical downscaling of outputs (daily minimum and maximum air temperature at 2-m) of 13 Earth System Models (simulations: HIST period 1950-2006; RCP2.6 and RCP8.5 period 2006-2100) at a 200-m resolution over and around the Mont-Blanc Massif (Western Europe, border between France and Italy and ...
Climate simulations at a kilometer scale over the Mont-Blanc
Ten-member ensemble simulations performed over the Mont-Blanc massif with the ARW/WRF regional climate model, period 1979-2012, forced by ERA-Interim reanalyses