99 research outputs found

    Sentinel-3 Mission Performance Centre: Ensuring a high-quality altimetric dataset

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    Sentinel-3A is scheduled for launch in Oct. 2015, with Sentinel-3B to follow 18 months later. Together these missions are to take oceanographic remote-sensing into a new operational realm. To achieve this a large number of processing, calibration and validation tasks have to be applied to their data in order to assess for quality, absolute bias, short-term changes and long-term drifts. ESA has funded the Sentinel-3 Mission Performance Centre (S3MPC) to carry out this evaluation on behalf of ESA and EUMETSAT. The S3MPC is run by a consortium led by ACRI [1] and this paper describes the work on the calibration/validation (cal/val) of the Surface Topography Mission (STM), which is co-ordinated by CLS and PML

    Simian virus 40 inhibits differentiation and maturation of rhesus macaque DC-SIGN+-dendritic cells

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    Dendritic cells (DC) are the initiators and modulators of the immune responses. Some species of pathogenic microorganisms have developed immune evasion strategies by controlling antigen presentation function of DC. Simian virus 40 (SV40) is a DNA tumor virus of rhesus monkey origin. It can induce cell transformation and tumorigenesis in many vertebrate species, but often causes no visible effects and persists as a latent infection in rhesus monkeys under natural conditions. To investigate the interaction between SV40 and rhesus monkey DC, rhesus monkey peripheral blood monocyte-derived DC were induced using recombinant human Interleukin-4 (rhIL-4) and infective SV40, the phenotype and function of DC-specific intracellular adhesion molecule-3 grabbing nonintegrin (DC-SIGN)+ DC were analyzed by flow cytometry (FCM) and mixed lymphocyte reaction (MLR). Results showed that SV40 can down-regulate the expression of CD83 and CD86 on DC and impair DC-induced activation of T cell proliferation. These findings suggest that SV40 might also cause immune suppression by influencing differentiation and maturation of DC

    Activin A Induces Langerhans Cell Differentiation In Vitro and in Human Skin Explants

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    Langerhans cells (LC) represent a well characterized subset of dendritic cells located in the epidermis of skin and mucosae. In vivo, they originate from resident and blood-borne precursors in the presence of keratinocyte-derived TGFβ. Ιn vitro, LC can be generated from monocytes in the presence of GM-CSF, IL-4 and TGFβ. However, the signals that induce LC during an inflammatory reaction are not fully investigated. Here we report that Activin A, a TGFβ family member induced by pro-inflammatory cytokines and involved in skin morphogenesis and wound healing, induces the differentiation of human monocytes into LC in the absence of TGFβ. Activin A-induced LC are Langerin+, Birbeck granules+, E-cadherin+, CLA+ and CCR6+ and possess typical APC functions. In human skin explants, intradermal injection of Activin A increased the number of CD1a+ and Langerin+ cells in both the epidermis and dermis by promoting the differentiation of resident precursor cells. High levels of Activin A were present in the upper epidermal layers and in the dermis of Lichen Planus biopsies in association with a marked infiltration of CD1a+ and Langerin+ cells. This study reports that Activin A induces the differentiation of circulating CD14+ cells into LC. Since Activin A is abundantly produced during inflammatory conditions which are also characterized by increased numbers of LC, we propose that this cytokine represents a new pathway, alternative to TGFβ, responsible for LC differentiation during inflammatory/autoimmune conditions

    The role of dendritic cells in the immunopathogenesis of psoriasis

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    Psoriasis vulgaris is a chronic inflammatory skin disease that is marked by a complex interplay of dendritic cells (DCs), T-cells, cytokines, and downstream transcription factors as part of a self-sustaining type 1 cytokine network. As integral players of the immune system, DCs represent antigen-presenting cells that are crucial for efficient activation of T-cells and B-cells. DCs have also been linked to distinct chronic inflammatory conditions, including psoriasis. In the setting of psoriasis therapy, DC/T cell interactions serve as a potential target for biologic response modifiers. Here we describe the major DC subsets as well as the immunologic involvement of DCs within the context of psoriatic lesions

    Transcutaneous immunization as preventative and therapeutic regimens to protect against experimental otitis media due to nontypeable Haemophilus influenzae

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    We have developed three nontypeable Haemophilus influenzae (NTHI) adhesin-derived immunogens that are significantly efficacious against experimental otitis media (OM) due to NTHI when delivered parenterally. We now expanded our preventative immunization strategies to include transcutaneous immunization (TCI) as a less invasive, but potentially equally efficacious, regimen to prevent OM due to NTHI. Additionally, we examined the potential of TCI as a therapeutic immunization regimen to resolve ongoing experimental OM. Preventative immunization with NTHI outer membrane protein (OMP) P5- and type IV pilus-targeted immunogens, delivered with the adjuvant LT(R192G-L211A), induced significantly earlier clearance of NTHI from the nasopharynges and middle ears of challenged chinchillas compared with receipt of immunogen or adjuvant alone. Moreover, therapeutic immunization resulted in significant resolution of established NTHI biofilms from the middle ear space of animals compared with controls. These data advocate TCI with the adhesin-directed immunogens as an efficacious regimen for prevention and resolution of experimental NTHI-induced OM

    Barrier Tissue Macrophages: Functional Adaptation to Environmental Challenges

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    Macrophages are found throughout the body, where they have crucial roles in tissue development, homeostasis and remodeling, as well as being sentinels of the innate immune system that can contribute to protective immunity and inflammation. Barrier tissues, such as the intestine, lung, skin and liver, are exposed constantly to the outside world, which places special demands on resident cell populations such as macrophages. Here we review the mounting evidence that although macrophages in different barrier tissues may be derived from distinct progenitors, their highly specific properties are shaped by the local environment, which allows them to adapt precisely to the needs of their anatomical niche. We discuss the properties of macrophages in steady-state barrier tissues, outline the factors that shape their differentiation and behavior and describe how macrophages change during protective immunity and inflammation

    Observed subsurface signature of Southern Ocean sea level rise

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    International audienceSatellite altimetry data show a strong increase in sea level in various parts of the Southern Ocean over the 1990s. In this paper, we examine the causes of the observed sea level rise in the region south of Australia, using 13 years of repeat hydrographic data from the WOCE SR3 sections, and the SURVOSTRAL XBT and surface salinity data. The hydrographic data show a poleward shift in the position of the Subtropical and the Subantarctic Fronts over the period. In the Antarctic Zone, the Antarctic Surface Water has become warmer and fresher, and the Winter Water tongue has become warmer, fresher, thinner and shallower. Increased freshening south of the Polar Front is linked to increased precipitation over the 1990s. Temperature changes over the upper 500 m account for only part of the altimetric sea level rise. The CTD sections show that the deeper layers are also warmer and slightly saltier and the observed sea level can be explained by steric expansion over the upper 2000 m. ENSO variability impacts on the northern part of the section, and a simple Sverdrup transport model shows how large-scale changes in the wind forcing, related to the Southern Annular Mode, may contribute to the deeper warming to the south

    A new assessment of the error budget of global mean sea level rate estimated by satellite altimetry over 1993-2008

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    ISI Document Delivery No.: V17LH Times Cited: 64 Cited Reference Count: 34 Cited References: Ablain M., 2007, OSTST HOB Altamimi Z, 2007, J GEOPHYS RES-SOL EA, V112, DOI 10.1029/2007JB004949 Altamimi Z, 2002, J GEOPHYS RES-SOL EA, V107, DOI 10.1029/2001JB000561 Beckley BD, 2007, GEOPHYS RES LETT, V34, DOI 10.1029/2007GL030002 BRETHERTON FP, 1976, DEEP-SEA RES, V23, P559, DOI 10.1016/0011-7471(76)90001-2 Carrere L, 2003, GEOPHYS RES LETT, V30, DOI 10.1029/2002GL016473 CAZENAVE A, 2004, REV GEOPHYS, V42, DOI DOI 10.1029/2003RG000139 Chambers DP, 2003, J GEOPHYS RES-OCEANS, V108, DOI 10.1029/2003JC001839 Chambers DP, 1998, J GEOPHYS RES-OCEANS, V103, P12885, DOI 10.1029/98JC01197 Church J.A., 2001, CHANGES SEA LEVEL CL Church JA, 2006, GEOPHYS RES LETT, V33, DOI 10.1029/2005GL024826 Fernandes MJ, 2006, SENSORS-BASEL, V6, P131, DOI 10.3390/s6030131 Gaspar P, 2002, J ATMOS OCEAN TECH, V19, P1690, DOI 10.1175/1520-0426(2002)0192.0.CO;2 Jevrejeva S, 2008, GEOPHYS RES LETT, V35, DOI 10.1029/2008GL033611 Kalnay E, 1996, B AM METEOROL SOC, V77, P437, DOI 10.1175/1520-0477(1996)0772.0.CO;2 Kennedy AJ, 2007, J GEOPHYS RES-OCEANS, V112, DOI 10.1029/2006JC003904 Landerer FW, 2008, J GEOPHYS RES-OCEANS, V113, DOI 10.1029/2008JC004767 Leuliette EW, 2004, MAR GEOD, V27, P79, DOI 10.1080/01490410490465193 Mitchum GT, 2000, MAR GEOD, V23, P145, DOI DOI 10.1080/01490410050128591 Mitchum GT, 1998, J ATMOS OCEAN TECH, V15, P721, DOI 10.1175/1520-0426(1998)0152.0.CO;2 Nerem RS, 2006, CR GEOSCI, V338, P1077, DOI 10.1016/j.crte.2006.09.001 Nerem RS, 2001, SATELLITE ALTIMETRY, P329 Nerem RS, 2001, SEA LEVEL RISE HIST, P121 Ngo-Duc T, 2005, J GEOPHYS RES-ATMOS, V110, DOI 10.1029/2004JD004940 Peltier R., 2004, ANN REV EARTH PL SC, V32, P111, DOI [10.1146/annurev. earth.32.082503.144359, DOI 10.1146/ANNUREV.EARTH.32.082503.144359] Ponte R. M., 2003, J ATMOS OCEAN TECH, V2, P301 Ray RD, 2004, J PHYS OCEANOGR, V34, P1922, DOI 10.1175/1520-0485(2004)0342.0.CO;2 Salstein DA, 2008, J GEOPHYS RES-ATMOS, V113, DOI 10.1029/2007JD009531 Scharroo R, 2004, MAR GEOD, V27, P279, DOI 10.1080/01490410490465265 Tapley B, 2005, J GEODESY, V79, P467, DOI 10.1007/s00190-005-0480-z University Of Michigan, 2007, SCIENCEDAILY Uppala SM, 2005, Q J ROY METEOR SOC, V131, P2961, DOI 10.1256/qj.04.176 Woppelmann G, 2007, GLOBAL PLANET CHANGE, V57, P396, DOI 10.1016/j.gloplacha.2007.02.002 Zlotnicki V, 2004, MAR GEOD, V27, P241, DOI 10.1080/01490410490465625 Ablain, M. Cazenave, A. Valladeau, G. Guinehut, S. 65 COPERNICUS GESELLSCHAFT MBH GOTTINGEN OCEAN SCIA new error budget assessment of the global Mean Sea Level (MSL) determined by TOPEX/Poseidon and Jason-1 altimeter satellites between January 1993 and June 2008 is presented using last altimeter standards. We discuss all potential errors affecting the calculation of the global MSL rate. We also compare altimetry-based sea level with tide gauge measurements over the altimetric period. Applying a statistical approach, this allows us to provide a realistic error budget of the MSL rise measured by satellite altimetry. These new calculations highlight a reduction in the rate of sea level rise since 2005, by similar to 2 mm/yr. This represents a 60% reduction compared to the 3.3 mm/yr sea level rise (glacial isostatic adjustment correction applied) measured between 1993 and 2005. Since November 2005, MSL is accurately measured by a single satellite, Jason-1. However the error analysis performed here indicates that the recent reduction in MSL rate is real
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