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  • 1
    Online Resource
    Online Resource
    Elsevier BV ; 2011
    In:  Clinical Microbiology and Infection Vol. 17, No. 1 ( 2011-01), p. 102-103
    In: Clinical Microbiology and Infection, Elsevier BV, Vol. 17, No. 1 ( 2011-01), p. 102-103
    Type of Medium: Online Resource
    ISSN: 1198-743X
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2011
    detail.hit.zdb_id: 2020034-1
    SSG: 12
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  • 2
    In: Tuberculosis, Elsevier BV, Vol. 89, No. 2 ( 2009-3), p. 158-162
    Type of Medium: Online Resource
    ISSN: 1472-9792
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2009
    detail.hit.zdb_id: 2058561-5
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  • 3
    Online Resource
    Online Resource
    American Meteorological Society ; 2021
    In:  Journal of Physical Oceanography ( 2021-09-02)
    In: Journal of Physical Oceanography, American Meteorological Society, ( 2021-09-02)
    Abstract: Coastal upwelling rates are classically determined by the intensity of the upper-ocean offshore Ekman transport. But (sub-)mesoscale turbulence modulates offshore transport, hence the net upwelling rate. Eddy effects generally oppose the Ekman circulation, resulting in so-called “eddy cancellation”, a process well studied in the Southern Ocean. Here we investigate how air-sea heat/buoyancy fluxes modulate eddy cancellation in an idealized upwelling model. We run CROCO simulations with constant winds but varying heat fluxes with and without submesoscale-rich turbulence. Eddy cancellation is consistently evaluated with three different methods that all account for the quasi-isopycnal nature of ocean circulation away from the surface. For zero heat fluxes the release of available potential energy by baroclinic instabilities is strongest and leads, near the coast, to nearly full cancellation of the Ekman cross-shore circulation by eddy effects, i.e. , zero net mean upwelling flow. With increasing heat fluxes eddy cancellation is reduced and the transverse flow progressively approaches the classical Ekman circulation. Sensitivity of the eddy circulation to synoptic changes in air-sea heat fluxes is felt down to 125 m depth despite short experiments of tens of days. Mesoscale dynamics dominate the cancellation effect in our simulations which might also hold for the real ocean as the relevant processes act below the surface boundary layer. Although the idealized setting overemphasis the role of eddies and thus studies with more realistic settings should follow, our findings have important implications for the overall understanding of upwelling system dynamics.
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2021
    detail.hit.zdb_id: 2042184-9
    detail.hit.zdb_id: 184162-2
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  • 4
    In: Blood, American Society of Hematology, Vol. 126, No. 23 ( 2015-12-03), p. 1983-1983
    Abstract: Introduction: Diffuse large B-cell lymphoma (DLBCL) is the largest subgroup of malignant lymphoma. Today more than 80% of the patients will achieve partial or complete remission. However more than 20 % will either relapse or present with refractory disease. The standard approach for patients without major comorbidity is salvage treatment followed by high dose therapy with autologous stem cell transplant (HDT). This potentially curative treatment is toxic with many side effects and procedure related mortality, and therefore identification of patients eligible for HDT is a difficult challenge. Objectives: Patients with relapse of de novo DLBCL and transformed indolent lymphoma (TIL) were included. The aim was to identify clinical prognostic markers that can identify patients who will not benefit from HDT. Methods: From the national lymphoma registry patients with relapse of B-cell lymphoma in Denmark in the period 2000-2012, who underwent HDT, were extracted. Medical records were reviewed for clinical, pathological, and treatment information, and outcome. Patients were followed until death or emigration or until February 1, 2015. The Kaplan-Meier method was used to estimate overall survival (OS) and progression free survival (PFS). Cox regression models were used to assess prognostic factors. Results: A total of 370 patients were included, 174 with de novo DLBCL, and 196 with TIL, 143 of the 196 had histologically confirmed transformation. Median age was 58 (22-73), and 59% of the patients were male. With a median follow-up of 82 months from HDT, the 5-year OS was 52% and the 5-year PFS was 44% (median PFS 3.2 years). For the DLBCL patients the 5-year OS was 43% and the 5-year PFS was 38%. For TIL patients the OS was 62% and the PFS 49% (figure 1). During the first 100 days, 29 patients (8%) were admitted to the intensive care unit (14 DLBCL), and only four of these patients were alive at six months. The non-relapse mortality (NRM) at day 100 was 6 % for both groups, after five years 25% for DLBCL and 15% for TIL. No significant difference in 5-year PFS was seen between sexes or age, but patients younger than 58 had better 5-year OS compared to patients aged 58 or above (p=0.047). There was no difference in relapse treatment (DHAP vs ICE). Smoking (ever vs. never) caused a significantly worse OS (p=0.034). All IPI-factors, except Ann Arbor stage, was of prognostic importance (PFS). Primary refractory disease was of poor prognostic importance (p=0.001), and in patients, for whom the time from last salvage treatment to reinfusion of stem cells was more than 2 months, had a worse outcome (p=0.006). Patients, with less than 20 days of hospital admission in the period from the date of relapse to start of HDT, had a significantly higher survival (OS and PFS) (p 〉 0.001). In a multivariate analysis (PFS), LDH above upper normal reference, HR 1.4 (95% CI: 1.0;2.1), involvement of more than one extranodal site, HR 1.6 (1.1;2.3) primary refractory disease, HR 1.6 (1.1;2.3) and more than two earlier relapses, HR 1.9 (1.1;3.5) were all factors associated with adverse outcome. For OS, the multivariate analysis showed, that patients with TIL had a better outcome, HR 0.7 (0.5;0.9), compared to DLBCL. Age above 58, HR 1.5 (1.1;2.1), involvement of more than one extranodal site, HR 1.9 (1.4;2.8), and primary refractory disease, HR 1.6 (1.1;2.3) were factors associated with adverse outcome. Discussion: In this population based study we find a 5-year OS of 52% after HDT and a 5-year PFS of 44%. Patients with TIL have a significantly higher 5-year PS (49%) than patients with de novo DLBCL (38%) whereas NRM is identical for the two groups at day 100 (6%). However, NRM increases subsequently more for DLBCL than for TIL over time to 25% and 15 % respectively after five years. Furthermore we show that hospitalization days less than 20 and postponement of stem cell infusion beyond 2 month after harvest may be useful parameters that can identify patients that have better or worse outcome after HDT. This nationwide study cohort with the long follow-up period is applicable to a general population of patients, and this may explain the somewhat lower outcome compared to other published HDT cohorts. Figure 1. Progression Free Survival (PFS) curves for Diffuse Large B-Cell Lymphomas (DLBCL) and Transformed Indolent Lymphomas (TIL) after high dose therapy with autologous stem cell transplant Figure 1. Progression Free Survival (PFS) curves for Diffuse Large B-Cell Lymphomas (DLBCL) and Transformed Indolent Lymphomas (TIL) after high dose therapy with autologous stem cell transplant Disclosures Brown: Bayer: Consultancy; Roche: Consultancy, Speakers Bureau.
    Type of Medium: Online Resource
    ISSN: 0006-4971 , 1528-0020
    RVK:
    RVK:
    Language: English
    Publisher: American Society of Hematology
    Publication Date: 2015
    detail.hit.zdb_id: 1468538-3
    detail.hit.zdb_id: 80069-7
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  • 5
    In: International Journal of Cardiology, Elsevier BV, Vol. 178 ( 2015-01), p. 292-296
    Type of Medium: Online Resource
    ISSN: 0167-5273
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2015
    detail.hit.zdb_id: 1500478-8
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  • 6
    In: The Lancet Oncology, Elsevier BV, Vol. 21, No. 3 ( 2020-03), p. 412-420
    Type of Medium: Online Resource
    ISSN: 1470-2045
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2020
    detail.hit.zdb_id: 2049730-1
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  • 7
    Online Resource
    Online Resource
    SAGE Publications ; 2011
    In:  Journal of Attention Disorders Vol. 15, No. 8 ( 2011-11), p. 646-655
    In: Journal of Attention Disorders, SAGE Publications, Vol. 15, No. 8 ( 2011-11), p. 646-655
    Abstract: Objective: The study examined executive function deficits (EFD) in school-age children (7 to 14 years) with ADHD. Method: A clinical sample of children diagnosed with ADHD ( n = 49) was compared to a population sample ( n = 196) on eight executive function (EF) measures. Then, the prevalence of EFD in clinical and non-clinical children was examined at the individual level according to three methods previously applied to define EFD, and a fourth method was included to control for the effect of age on performance. Results: Children with ADHD were significantly more impaired on measures of EF than children without ADHD at the group level. However, only about 50% of children with ADHD were found to have EFD at the individual level, and results appeared relatively robust across methods applied to define EFD. Conclusion: As a group, children with ADHD displayed more problems on neuropsychological measures of EF than non-clinical children; at the individual level, there appeared to be heterogeneity in EF impairment.
    Type of Medium: Online Resource
    ISSN: 1087-0547 , 1557-1246
    Language: English
    Publisher: SAGE Publications
    Publication Date: 2011
    detail.hit.zdb_id: 2188086-4
    SSG: 5,2
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  • 8
    In: Ocean Science, Copernicus GmbH, Vol. 16, No. 6 ( 2020-11-09), p. 1347-1366
    Abstract: Abstract. The intraseasonal evolution of physical and biogeochemical properties during a coastal trapped wave event off central Peru is analysed using data from an extensive shipboard observational programme conducted between April and June 2017, and remote sensing data. The poleward velocities in the Peru–Chile Undercurrent were highly variable and strongly intensified to above 0.5 m s−1 between the middle and end of May. This intensification was likely caused by a first-baroclinic-mode downwelling coastal trapped wave, excited by a westerly wind anomaly at the Equator and originating at about 95∘ W. Local winds along the South American coast did not impact the wave. Although there is general agreement between the observed cross-shore-depth velocity structure of the coastal trapped wave and the velocity structure of first vertical mode solution of a linear wave model, there are differences in the details of the two flow distributions. The enhanced poleward flow increased water mass advection from the equatorial current system to the study site. The resulting shorter alongshore transit times between the Equator and the coast off central Peru led to a strong increase in nitrate concentrations, less anoxic water, likely less fixed nitrogen loss to N2 and a decrease of the nitrogen deficit compared to the situation before the poleward flow intensification. This study highlights the role of changes in the alongshore advection due to coastal trapped waves for the nutrient budget and the cumulative strength of N cycling in the Peruvian oxygen minimum zone. Enhanced availability of nitrate may impact a range of pelagic and benthic elemental cycles, as it represents a major electron acceptor for organic carbon degradation during denitrification and is involved in sulfide oxidation in sediments.
    Type of Medium: Online Resource
    ISSN: 1812-0792
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2020
    detail.hit.zdb_id: 2183769-7
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  • 9
    In: Biogeosciences, Copernicus GmbH, Vol. 18, No. 12 ( 2021-06-17), p. 3605-3629
    Abstract: Abstract. Filaments and fronts play a crucial role for a net offshore and downward nutrient transport in Eastern Boundary Upwelling Systems (EBUSs) and thereby reduce regional primary production. Most studies on this topic are based on either observations or model simulations, but only seldom are both approaches are combined quantitatively to assess the importance of filaments for primary production and nutrient transport. Here we combine targeted interdisciplinary shipboard observations of a cold filament off Peru with submesoscale-permitting (1/45∘) coupled physical (Coastal and Regional Ocean Community model, CROCO) and biogeochemical (Pelagic Interaction Scheme for Carbon and Ecosystem Studies, PISCES) model simulations to (i) evaluate the model simulations in detail, including the timescales of biogeochemical modification of the newly upwelled water, and (ii) quantify the net effect of submesoscale fronts and filaments on primary production in the Peruvian upwelling system. The observed filament contains relatively cold, fresh, and nutrient-rich waters originating in the coastal upwelling. Enhanced nitrate concentrations and offshore velocities of up to 0.5 m s−1 within the filament suggest an offshore transport of nutrients. Surface chlorophyll in the filament is a factor of 4 lower than at the upwelling front, while surface primary production is a factor of 2 higher. The simulation exhibits filaments that are similar in horizontal and vertical scale compared to the observed filament. Nitrate concentrations and primary production within filaments in the model are comparable to observations as well, justifying further analysis of nitrate uptake and subduction using the model. Virtual Lagrangian floats were released in the subsurface waters along the shelf and biogeochemical variables tracked along the trajectories of floats upwelled near the coast. In the submesoscale-permitting (1/45∘) simulation, 43 % of upwelled floats and 40 % of upwelled nitrate are subducted within 20 d after upwelling, which corresponds to an increase in nitrate subduction compared to a mesoscale-resolving (1/9∘) simulation by 14 %. Taking model biases into account, we give a best estimate for subduction of upwelled nitrate off Peru between 30 %– 40 %. Our results suggest that submesoscale processes further reduce primary production by amplifying the downward and offshore export of nutrients found in previous mesoscale studies, which are thus likely to underestimate the reduction in primary production due to eddy fluxes. Moreover, this downward and offshore transport could also enhance the export of fresh organic matter below the euphotic zone and thereby potentially stimulate microbial activity in regions of the upper offshore oxygen minimum zone.
    Type of Medium: Online Resource
    ISSN: 1726-4189
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2021
    detail.hit.zdb_id: 2158181-2
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  • 10
    In: Biogeosciences, Copernicus GmbH, Vol. 17, No. 18 ( 2020-09-25), p. 4663-4679
    Abstract: Abstract. The eastern tropical South Pacific (ETSP) represents one of the most productive areas in the ocean that is characterised by a pronounced oxygen minimum zone (OMZ). Particulate organic matter (POM) that sinks out of the euphotic zone is supplied to the anoxic sediments and utilised by microbial communities, and the degradation of POM is associated with the production and reworking of dissolved organic matter (DOM). The release of DOM to the overlying waters may, therefore, represent an important organic matter escape mechanism from remineralisation within sediments but has received little attention in OMZ regions so far. Here, we combine measurements of dissolved organic carbon (DOC) and dissolved organic nitrogen (DON) with DOM optical properties in the form of chromophoric (CDOM) and fluorescent (FDOM) DOM from pore waters and near-bottom waters of the ETSP off Peru. We evaluate diffusion-driven fluxes and net in situ fluxes of DOC and DON to investigate processes affecting DOM cycling at the sediment–water interface along a transect at 12∘ S. To our knowledge, these are the first data for sediment release of DON and pore water CDOM and FDOM for the ETSP off Peru. Pore water DOC accumulated with increasing sediment depth, suggesting an imbalance between DOM production and remineralisation within sediments. High DON accumulation resulted in very low pore water DOC ∕ DON ratios (≤1) which could be caused by an “uncoupling” in DOC and DON remineralisation. Diffusion-driven fluxes of DOC and DON exhibited high spatial variability and ranged from 0.2±0.1 to 2.5±1.3 mmolm-2d-1 and from -0.04±0.02 to 3.3±1.7 mmolm-2d-1, respectively. Generally low net in situ DOC and DON fluxes, as well as a steepening of spectral inclination (S) of CDOM and an increase in humic-like DOM at the sediment–water interface over time, indicated active microbial DOM utilisation. The latter may potentially be stimulated by the presence of nitrate (NO3-) and nitrite (NO2-) in the water column. The microbial DOC utilisation rates, estimated in our study, are potentially sufficient to support denitrification rates of 0.2–1.4 mmolm-2d-1, suggesting that the sediment release of DOM may on occasion contribute to nitrogen loss processes in the ETSP off Peru.
    Type of Medium: Online Resource
    ISSN: 1726-4189
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2020
    detail.hit.zdb_id: 2158181-2
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