Skills of the user-relevant ocean indicators

This document demonstrates the capability of seasonal forecasting systems to predict observable and user-relevant ocean climate indicators

Copernicus Ocean State Report, issue 6

The 6th issue of the Copernicus OSR incorporates a large range of topics for the blue, white and green ocean for all European regional seas, and the global ocean over 1993–2020 with a special focus on 2020

Characterization of plasmids harboring blaCTX-M genes in Escherichia coli from French pigs

International audienceResistance to extended-spectrum cephalosporins is prevalent in French pig E. coli isolates. The aim of this study was to characterize the plasmids and genes present in pathogenic and commensal extended-spectrum cephalosporins -resistant isolates. The resistance plasmids of 26 strains were sequenced and then analyzed to identify resistance and virulence genes. Results showed that resistance to extended-spectrum cephalosporins in French pig E. coli isolates is-as in other food animals in France-mainly carried by highly similar blaCTX-M-1 IncI1/ST3 plasmids. These plasmids very often bear other resistance genes such as resistance to sulphonamides (sul2), trimethoprim (dfrA17) and aminoglycosides (aadA5), and occasionally to tetracycline (tet(A)), macrolides (mph(A) and erm genes), phenicols (floR) or streptomycin (strA, strB). Few virulence genes were detected, including colicins, heat-stable enterotoxins, adhesins or temperature-sensitive hemagglutinins. The other cefotaximases detected were blaCTX-M-27 and blaCTX-M-14, the latter being on an IncF plasmid which showed very close identity to a human epidemic plasmid. Importantly, resistance genes for quinolones or polymyxins were never detected on the extended-spectrum cephalosporins resistance plasmids. These results are helpful to evidence the risk of co-selecting cephalosporins -resistance using antibiotics outside this group. They also highlight the occasional presence in pigs of human epidemic plasmids

CERA-20C: A Coupled Reanalysis of the Twentieth Century

CERA-20C is a coupled reanalysis of the twentieth century which aims to reconstruct the past weather and climate of the Earth system including the atmosphere, ocean, land, ocean waves, and sea ice. This reanalysis is based on the CERA coupled atmosphere-ocean assimilation system developed at ECMWF. CERA-20C provides a 10 member ensemble of reanalyses to account for errors in the observational record as well as model error. It benefited from the prior experience of the retrospective atmospheric analysis ERA-20C. The dynamical model and the data assimilation systems initially developed for NWP had been modified to take into account the evolution of the radiative forcing and the observing system. To limit the impact of changes in the observing system throughout the century, only conventional surface observations have been used in the atmosphere. CERA-20C improves the specification of the background and the observation errors, two key elements to ensure a consistent weighting of the uncertainties across geophysical variables, space, and time. The quality of CERA-20C has been evaluated against other centennial reanalyses and independent observations. Although CERA-20C inherits some limitations of ERA-20C to represent correctly the tropical cyclones in the first part of the century, it shows significant improvements in the troposphere, compared to ERA-20C and 20CRv2c (the twentieth century reanalysis produced by NOAA/CIRES). A preliminary study of the climate variability in CERA-20C has been carried out. CERA-20C improves on the representation of atmosphere-ocean heat fluxes and mean sea level pressure compared to previous uncoupled ocean and atmospheric historical reanalyses performed at ECMWF

The EU-FP7 ERA-CLIM2 project contribution to advancing science and production of Earth-system climate reanalyses

The main goals and activities of the ERA-CLIM2 project are presented, and some of its key results, included the first ensemble of coupled reanalysis of the 20th century, are discussed. ERA-CLIM2 is a European Union Seventh Framework Project started in January 2014 and due to be completed in December 2017. It aimed to produce coupled reanalyses, which are physically consistent data sets describing the evolution of the global atmosphere, ocean, land-surface, cryosphere and the carbon cycle. ERA-CLIM2 has contributed to advancing the capacity for producing state-of-the-art climate reanalyses that extend back to the early 20th century. ERA-CLIM2 has led to the generation of the first European ensemble of coupled ocean, sea-ice, land and atmosphere reanalyses of the 20th century. The project has funded work to rescue and prepare observations, and to advance the data-assimilation systems required to generate operational reanalyses, such as the ones planned by the European Union Copernicus Climate Change Service. This paper summarizes the main goals of the project, discusses some of its main areas of activities, and presents some of its key results

Gathering users and developers to shape together the next-generation ocean reanalyses: Ocean reanalyses workshop of the European Copernicus Marine Service

International audienc

CERA-20C: A Coupled Reanalysis of the Twentieth Century

CERA‐20C is a coupled reanalysis of the twentieth century which aims to reconstruct the past weather and climate of the Earth system including the atmosphere, ocean, land, ocean waves, and sea ice. This reanalysis is based on the CERA coupled atmosphere‐ocean assimilation system developed at ECMWF. CERA‐20C provides a 10 member ensemble of reanalyses to account for errors in the observational record as well as model error. It benefited from the prior experience of the retrospective atmospheric analysis ERA‐20C. The dynamical model and the data assimilation systems initially developed for NWP had been modified to take into account the evolution of the radiative forcing and the observing system. To limit the impact of changes in the observing system throughout the century, only conventional surface observations have been used in the atmosphere. CERA‐20C improves the specification of the background and the observation errors, two key elements to ensure a consistent weighting of the uncertainties across geophysical variables, space, and time. The quality of CERA‐20C has been evaluated against other centennial reanalyses and independent observations. Although CERA‐20C inherits some limitations of ERA‐20C to represent correctly the tropical cyclones in the first part of the century, it shows significant improvements in the troposphere, compared to ERA‐20C and 20CRv2c (the twentieth century reanalysis produced by NOAA/CIRES). A preliminary study of the climate variability in CERA‐20C has been carried out. CERA‐20C improves on the representation of atmosphere‐ocean heat fluxes and mean sea level pressure compared to previous uncoupled ocean and atmospheric historical reanalyses performed at ECMWF.© 2018 The Author