17 research outputs found
Les conceptions de la médiatisation au début du XIXÚme siÚcle
Tout au long du XIXe siĂšcle, la nĂ©cessitĂ© de construire un nouvel ordre social a suscitĂ© une rĂ©flexion sur la place Ă donner Ă la mĂ©diatisation dans cette reconstruction.âLes auteurs examinent plus particuliĂšrement comment, au cours de la premiĂšre partie du siĂšcle, la presse est apparue susceptible, en contribuant Ă la formation de lâopinion publique et Ă la rĂ©crĂ©ation dâun lien social, de constituer dĂ©sormais un instrument indispensable Ă lâexercice du pouvoir au sein dâune sociĂ©tĂ© marquĂ©e par une exigence croissante de publicitĂ©
Measuring global ocean heat content to estimate the earth energy imbalance
The energy radiated by the Earth toward space does not compensate the incoming radiation from the Sun leading to a small positive energy imbalance at the top of the atmosphere (0.4â1 Wmâ2). This imbalance is coined Earthâs Energy Imbalance (EEI). It is mostly caused by anthropogenic greenhouse gas emissions and is driving the current warming of the planet. Precise monitoring of EEI is critical to assess the current status of climate change and the future evolution of climate. But the monitoring of EEI is challenging as EEI is two orders of magnitude smaller than the radiation fluxes in and out of the Earth system. Over 93% of the excess energy that is gained by the Earth in response to the positive EEI accumulates into the ocean in the form of heat. This accumulation of heat can be tracked with the ocean observing system such that today, the monitoring of Ocean Heat Content (OHC) and its long-term change provide the most efficient approach to estimate EEI. In this community paper we review the current four state-of-the-art methods to estimate global OHC changes and evaluate their relevance to derive EEI estimates on different time scales. These four methods make use of: (1) direct observations of in situ temperature; (2) satellite-based measurements of the ocean surface net heat fluxes; (3) satellite-based estimates of the thermal expansion of the ocean and (4) ocean reanalyses that assimilate observations from both satellite and in situ instruments. For each method we review the potential and the uncertainty of the method to estimate global OHC changes. We also analyze gaps in the current capability of each method and identify ways of progress for the future to fulfill the requirements of EEI monitoring. Achieving the observation of EEI with sufficient accuracy will depend on merging the remote sensing techniques with in situ measurements of key variables as an integral part of the Ocean Observing System
Altimetry for the future: Building on 25 years of progress
In 2018 we celebrated 25 years of development of radar altimetry, and the progress achieved by this methodology in the fields of global and coastal oceanography, hydrology, geodesy and cryospheric sciences. Many symbolic major events have celebrated these developments, e.g., in Venice, Italy, the 15th (2006) and 20th (2012) years of progress and more recently, in 2018, in Ponta Delgada, Portugal, 25 Years of Progress in Radar Altimetry. On this latter occasion it was decided to collect contributions of scientists, engineers and managers involved in the worldwide altimetry community to depict the state of altimetry and propose recommendations for the altimetry of the future. This paper summarizes contributions and recommendations that were collected and provides guidance for future mission design, research activities, and sustainable operational radar altimetry data exploitation. Recommendations provided are fundamental for optimizing further scientific and operational advances of oceanographic observations by altimetry, including requirements for spatial and temporal resolution of altimetric measurements, their accuracy and continuity. There are also new challenges and new openings mentioned in the paper that are particularly crucial for observations at higher latitudes, for coastal oceanography, for cryospheric studies and for hydrology. The paper starts with a general introduction followed by a section on Earth System Science including Ocean Dynamics, Sea Level, the Coastal Ocean, Hydrology, the Cryosphere and Polar Oceans and the ââGreenâ Ocean, extending the frontier from biogeochemistry to marine ecology. Applications are described in a subsequent section, which covers Operational Oceanography, Weather, Hurricane Wave and Wind Forecasting, Climate projection. Instrumentsâ development and satellite missionsâ evolutions are described in a fourth section. A fifth section covers the key observations that altimeters provide and their potential complements, from other Earth observation measurements to in situ data. Section 6 identifies the data and methods and provides some accuracy and resolution requirements for the wet tropospheric correction, the orbit and other geodetic requirements, the Mean Sea Surface, Geoid and Mean Dynamic Topography, Calibration and Validation, data accuracy, data access and handling (including the DUACS system). Section 7 brings a transversal view on scales, integration, artificial intelligence, and capacity building (education and training). Section 8 reviews the programmatic issues followed by a conclusion
Altimetry for the future: building on 25 years of progress
In 2018 we celebrated 25âŻyears of development of radar altimetry, and the progress achieved by this methodology in the fields of global and coastal oceanography, hydrology, geodesy and cryospheric sciences. Many symbolic major events have celebrated these developments, e.g., in Venice, Italy, the 15th (2006) and 20th (2012) years of progress and more recently, in 2018, in Ponta Delgada, Portugal, 25 Years of Progress in Radar Altimetry. On this latter occasion it was decided to collect contributions of scientists, engineers and managers involved in the worldwide altimetry community to depict the state of altimetry and propose recommendations for the altimetry of the future. This paper summarizes contributions and recommendations that were collected and provides guidance for future mission design, research activities, and sustainable operational radar altimetry data exploitation. Recommendations provided are fundamental for optimizing further scientific and operational advances of oceanographic observations by altimetry, including requirements for spatial and temporal resolution of altimetric measurements, their accuracy and continuity. There are also new challenges and new openings mentioned in the paper that are particularly crucial for observations at higher latitudes, for coastal oceanography, for cryospheric studies and for hydrology.
The paper starts with a general introduction followed by a section on Earth System Science including Ocean Dynamics, Sea Level, the Coastal Ocean, Hydrology, the Cryosphere and Polar Oceans and the âGreenâ Ocean, extending the frontier from biogeochemistry to marine ecology. Applications are described in a subsequent section, which covers Operational Oceanography, Weather, Hurricane Wave and Wind Forecasting, Climate projection. Instrumentsâ development and satellite missionsâ evolutions are described in a fourth section. A fifth section covers the key observations that altimeters provide and their potential complements, from other Earth observation measurements to in situ data. Section 6 identifies the data and methods and provides some accuracy and resolution requirements for the wet tropospheric correction, the orbit and other geodetic requirements, the Mean Sea Surface, Geoid and Mean Dynamic Topography, Calibration and Validation, data accuracy, data access and handling (including the DUACS system). Section 7 brings a transversal view on scales, integration, artificial intelligence, and capacity building (education and training). Section 8 reviews the programmatic issues followed by a conclusion
Le rejet de la délibération : du dogmatisme à l'élitisme
En 1828, Charles de Rémusat constate que la société française est désormais décrite trÚs fréquemment comme « livrée à l'anarchie des opinions ». Il constate également que, si ce jugement a été formulé d'abord par les réactionnaires catholiques, qui « présentent la théocratie comme la seule digue qui puisse contenir le torrent », il a été repris par les saint-simoniens, qui « n'attendent le retour de l'ordre que d'un systÚme social qui ferait de l'humanité un grand couvent polytechnique gouver..
Voies de signalisation de lâapoptose mĂ©diĂ©es par les sphingolipides
Divers sphingolipides sont aujourdâhui reconnus comme Ă©tant douĂ©s de propriĂ©tĂ©s biologiques et/ou agissant comme seconds messagers. Parmi eux, le cĂ©ra- mide (ou N-acylsphingosine) et la sphingosine se comportent comme des mĂ©diateurs gĂ©nĂ©ralement proapoptotiques. Ainsi, le cĂ©ramide relaie le signal cytotoxique dâun certain nombre dâagents de stress qui, soit, stimulent sa biosynthĂšse de novo, soit, activent lâhydrolyse de sphingomyĂ©line par des sphingomyĂ©linases. Par exemple, la gĂ©nĂ©ration prĂ©coce de cĂ©ramide induite par le TNF est mĂ©diĂ©e par une sphingomyĂ©linase neutre dont lâactivitĂ© est sous la dĂ©pendance de la protĂ©ine adaptatrice FAN, contrĂŽlant ainsi lâactivation des caspases et le processus apoptotique. De plus, lâactivitĂ© de cette sphingomyĂ©linase neutre semble ĂȘtre modulĂ©e nĂ©gativement par la cavĂ©oline, un constituant essentiel de certains microdomaines membranaires. Par ailleurs, la sphingosine kinase est une enzyme-clĂ© du mĂ©tabolisme des sphingolipides car elle contrĂŽle les taux intracellulaires de deux molĂ©cules aux effets antagonistes, la sphingosine, pro-apoptotique, et la sphingosine 1-phosphate, anti-apoptotique. Le mĂ©tabolisme du cĂ©ramide et de la sphingosine est donc considĂ©rĂ© actuellement comme au cĆur d'un ensemble de voies de signalisation rĂ©gulant le devenir de la cellule
La médiatisation des problÚmes publics
MĂ©diatiser : le travail de journalistes et seulement de ceux-ci ? Quels enjeux pour les acteurs sociaux dâun processus oĂč se joue lâune des formes de la publicisation ? MĂ©diatiser : un travail de relation, de mise en rĂ©seaux aboutissant Ă du rĂ©dactionnel, Ă©tape ultime de la mĂ©diatisation ? Ou un travail de mise en circulation de discours dans des espaces multiples offerts Ă des lectures publiques ? MĂ©diatiser : quels enjeux et quels points de vue pour les chercheurs ? Au travers de lâanalyse des « problĂšmes publics », ce numĂ©ro dâEtudes de communication sâoffre comme un espace de dialogue interdisciplinaire oĂč Sciences de lâInformation et de la Communication, Anthropologie, Science Politique, Histoire, Sciences du Langage conjuguent leurs perspectives pour mieux analyser ce qui est Ă lâĆuvre dans lâacte de « mĂ©diatiser », ce qui se construit dans le processus social de « mĂ©diatisation ». ComitĂ© scientifique de ce numĂ©ro : Pierre Achard, Patrick Charaudeau, Bernard MiĂšge, Pierre Moeglin, Jean Mouchon, Eric Neveu, Roger Odin, Michael Palmer, Jean-François TĂ©tu, Yves Winkin. ComitĂ© de rĂ©daction de ce numĂ©ro : Olivier Chantraine, Pierre Delcambre, Bernard Delforce, Elisabeth Fichez, Martine HĂ©doux, Bernard Leconte, François Poulle, Christine Revuz
Switched allotype expression in an immunoglobulinânonsecreting rabbit lymphoid cell line fused with rabbit gangliocytes
The Simian virus 40âtransformed rabbit spleen cell TRSCâ1 synthesizes intracellular whole IgG molecules of the a1b4 allotype. Two hypoxanthineâguanine phosphoryl transferaseâdeficient mutants were derived from this line. One of these, TRSCâ1â8, was used in somatic cell fusion experiments together with gangliocytes from a rabbit immunized against ÎČâgalactosidase. Out of nineteen hybrid clones surviving in selective medium, only one, L17, was shown to produce free Îł chains which express the a2 allotype of the donor rabbit rather than the a1 marker of the parents TRSCâ1â8 line. The inability to restore IgG secretion in hybrids suggests that dominant regulatory controls are exerted by the TRSCâ1 genome on Ig production. This supports the notion that the TRSCâ1 line originated from a splenocyte that had not reached the final plasmocyte differentiation stage at the time of viral transformation. Copyright © 1981 WILEYâVCH Verlag GmbH & Co. KGaA, WeinheimSCOPUS: ar.jFLWNAinfo:eu-repo/semantics/publishe
Epoetin alfa facilitates presurgical autologous blood donation in non-anaemic patients scheduled for orthopaedic or cardiovascular surgery
Patients expected to need at least three units of blood for their elective cardiovascular or orthopaedic surgery, were allocated randomly to receive intravenous (i.v.) Epoetin alfa 600 IU kg-1 (n = 27), 300 IU kg-1 (n = 30) or placebo (n = 23), on days 1, 4 and 7. Provided haemoglobin †11 g dL-1, one unit of blood was collected on days 1, 4, 7, 11 and 14. Iron supplementation was given throughout the study. Surgery was scheduled between days 18 and 21. Significantly more patients treated with Epoetin alfa (100% for 600 IU kg-1; 97% for 300 IU kg-1) were able to donate †4 units of blood compared with placebo (78%) (P = 0.011 and P = 0.032). No significant differences were seen in total patient exposure to homologous blood 17.4%, 3.3% and 17.4%, respectively). Mean red cell volume donated (P = 0.005 for 600 IU kg-1; P = 0.158 for 300 IU kg-l both vs. placebo) and production (P < 0.001 and P = 0.012, respectively) were dose related. Twenty-four patients became iron deficient. No differences in the incidence of adverse events were seen between the groups.SCOPUS: ar.jinfo:eu-repo/semantics/publishe