On Assateague Island, an undeveloped barrier island along Maryland and Virginia, a foredune was constructed to protect the island from the erosion and breaching threat caused by permanent jetties ...built to maintain Ocean City Inlet. Scientists and engineers integrated expertise in vegetation, wildlife, geomorphology, and coastal engineering in order to design a habitat restoration project that would be evaluated in terms of coastal processes rather than static features. Development of specific restoration targets, thresholds for intervention, and criteria to evaluate long-term project success were based on biological and geomorphological data and coastal engineering models. A detailed long-term monitoring plan was established to measure project sustainability. The foredune unexpectedly acted as near-total barrier to both overwash and wind, and the dynamic ecosystem underwent undesirable habitat changes including conversion of early-succession beach habitat to herbaceous and shrub communities, diminishing availability of foraging habitat and thereby reducing productivity of the Federally-listed Threatened Charadrius melodus (piping plover). To address these impacts, multiple notches were cut through the constructed foredune. The metric for initial geomorphological success—restoration of at least one overwash event per year across the constructed foredune, if occurring elsewhere on the island—was reached. New overwash fans increased island stability by increasing interior island elevation. At every notch, areas of sparse vegetation increased and the new foraging habitat was utilized by breeding pairs during the 2010 breeding season. However, the metric for long-term biological success—an increase to 37% sparsely vegetated habitat on the North End and an increase in piping plover productivity to 1.25 chicks fledged per breeding pair—has not yet been met. By 2010 there was an overall productivity of 1.2 chicks fledged per breeding pair and a 1.7% decrease in sparsely vegetated habitat. Ideally, overwash restoration will sustain the availability of foraging habitat, but future foredune modifications may be necessary to maintain or increase overwash processes and piping plover habitat in the project area.
To achieve desired environmental outcomes, environmental condition and trends need to be rigorously measured and communicated to resource managers, scientists, and a broader general audience. ...However, there is often a disconnect between responsive ecosystem monitoring and decision making for strategic long-term management. This project demonstrates how historical monitoring data can be synthesized and used for future planning and decision making, thereby closing the management feedback cycle. This study linked disparate datasets, collected for a variety of purposes and across multiple temporal and spatial scales, in order to assess and quantify current habitat conditions. The results inform integrated resource management decision-making at Assateague Island National Seashore (Maryland and Virginia, USA) by using ecological reference conditions to identify monitoring needs, areas of high vulnerability, and areas with potential for improved management. The approach also provides a framework that can be applied in the future to assess the effectiveness of these management decisions on the condition of island habitats, and is a replicable demonstration of incorporating diverse monitoring datasets into an adaptive management cycle.
We present an analysis of the impact of heterogeneous chemistry on the partitioning of nitrogen species measured by the Upper Atmosphere Research Satellite (UARS) instruments. The UARS measurements ...utilized include N2O, HNO3, and ClONO2 from the cryogenic limb array etalon spectrometer (CLAES), version 7 (v.7), and temperature, methane, ozone, H2O, HCl, NO and NO2 from the halogen occultation experiment (HALOE), version 18. The analysis is carried out for the UARS data obtained between January 1992 and September 1994 in the 100- to 1-mbar (approx. 17-47 km) altitude range and over 10 deg latitude bins from 70 deg S to 70 deg N. The spatiotemporal evolution of aerosol surface area density (SAD) is adopted from analysis of the Stratospheric Aerosol and Gas Experiment (SAGE) II data. A diurnal steady state photochemical box model, constrained by the temperature, ozone, H2O, CH4, aerosol SAD, and columns of O2 and O3 above the point of interest, has been used as the main tool to analyze these data. Total inorganic nitrogen (NOY) is obtained by three different methods: (1) as a sum of the UARS-measured NO, NO2, HNO3, and ClONO2; (2) from the N2O-NOY correlation; and (3) from the CH4-NOY correlation. To validate our current understanding of stratospheric heterogeneous chemistry for post-Pinatubo conditions, the model-calculated monthly averaged NO(x)/NO(y) ratios and the NO, NO2, and HNO3 profiles are compared with the UARS-derived data. In general, the UARS-constrained box model captures the main features of nitrogen species partitioning in the post-Pinatubo years, such as recovery of NO(x) after the eruption, their seasonal variability and vertical profiles. However, the model underestimates the NO2 content, particularly in the 30- to 7-mbar (approx. 23-32 km) range. Comparisons of the calculated temporal behavior of the partial columns of NO2 and HNO3 and ground-based measurements at 45 deg S and 45 deg N are also presented. Our analysis indicates that ground-based and HALOE v.18 measurements of the NO2 vertical columns are consistent within the range of their uncertainties and are systematically higher (up to 50%) than the model results at midlatitudes in both hemispheres. Reasonable agreement is obtained for HNO3 columns at 45 deg S, suggesting some problems with nitrogen species partitioning in the model. Outstanding uncertainties are discussed.
The distribution and optical characteristics of Antarctic polar stratospheric clouds (PSCs) during the winter of 1992 as seen from the cryogenic limb array etalon spectrometer (CLAES) on the NASA ...Upper Atmosphere Research Satellite (UARS) are presented. The CLAES measurements are the first extensive stratospheric aerosol observations through much of the Antarctic polar night. An analysis of the vertical and areal distribution using the aerosol absorption coefficient measured at 780 cm−1 is presented, including a polar map showing the frequency of PSC occurrence during the two CLAES Antarctic viewing periods June 11 to July 10 and August 16 to September 18. The PSC seasonal evolution from CLAES is compared with a climatology based on the Stratospheric Aerosol Measurements II (SAM II) system. The frequency of PSC occurrence in the CLAES data sampled at latitudes similar to those observed with SAM II shows general agreement with the climatology. Some obvious differences between details of the PSC evolution seen by CLAES and the climatology are investigated with 1992 SAM II aerosol extinction data and shown to be due to intra‐annual variations specific to 1992, which appear in both data sets.
Abstract 3722
Despite advances in treatments for B-cell leukemias and lymphomas, many patients ultimately relapse and succumb to disease following multiple courses of therapy. Bispecific antibody ...fragments that can simultaneously engage T cells and tumor cells have been shown, in the literature, to destroy tumor cells by effectively redirecting the cytotoxic function of T cells. T-cell engaging bispecific molecules linking anti-CD19 and anti-CD3 binding domains in the context of novel SCORPION™ (multi-specific protein therapeutic) proteins were evaluated both in vitro and in vivo for function and stability.
Redirected T-cell cytotoxicity (RTCC) was measured by combining CD19 positive or negative cell lines with SCORPION proteins in the presence of human T cells. In a similar assay context, CFSE-labeled T cells were monitored for activation and proliferation. Functional RTCC assays were also used to analyze serum stability of SCORPION molecules in vitro and to complete an in vivo pharmacokinetic analysis. In vivo efficacy was assessed by monitoring the rate of tumor outgrowth of Ramos xenografts co-implanted with human peripheral blood mononuclear cells (PBMC) in NOD/SCID mice after treatment with SCORPION molecules.
SCORPION molecules potently mediate target-specific T-cell cytotoxicity toward tumor cell lines presenting cell surface CD19, with EC50 values for cytotoxicity at low pM concentrations. These molecules also demonstrate induction of T-cell activation and proliferation in the presence of target-bearing tumor cells but not in the absence of target expression. SCORPION molecules retain stable function following incubation at 37°C in mouse serum for up to a week in vitro, and pharmacokinetic analysis of SCORPION protein function in BALB/c mouse serum following intravenous administration resulted in half-life estimates of 69–84 hours. In efficacy studies conducted in NOD/SCID mice, SCORPION proteins significantly inhibited the outgrowth of Ramos tumor xenografts in the presence of human effector cells.
SCORPION molecules targeting CD19 and CD3 effectively harness the cytotoxic activity of T cells to kill CD19 positive tumor cells both in vitro and in vivo and show potential for further investigation as possible therapeutic agents for B-cell malignancies.
Chenault:Emergent BioSolutions: Employment. Gottschalk:Emergent BioSolutions: Employment. Hernandez-Hoyos:Emergent BioSolutions: Employment. Wiens:Emergent BioSolutions: Employment. Gordon:Emergent BioSolutions: Employment. Klee:Emergent BioSolutions: Employment, Equity Ownership. Bienvenue:Emergent BioSolutions: Employment. Dasovich:Emergent BioSolutions: Employment. Kumer:Emergent BioSolutions: Employment. Aguilar:Emergent BioSolutions: Employment. Bannink:Emergent BioSolutions: Employment, Equity Ownership. McMahan:Emergent BioSolutions: Employment, Equity Ownership. Natarajan:Emergent BioSolutions: Employment, Equity Ownership. Algate:Emergent BioSolutions: Employment, Equity Ownership. Blankenship:Emergent BioSolutions: Employment, Equity Ownership, Patents & Royalties.
We present an analysis of the impact of heterogeneous chemistry on the partitioning of nitrogen species measured by the Upper Atmosphere Research Satellite (UARS) instruments. The UARS measurements ...utilized include N2O, HNO3, and ClONO2 from the cryogenic limb array etalon spectrometer (CLAES), version 7 (v.7), and temperature, methane, ozone, H2O, HCl, NO and NO2 from the halogen occultation experiment (HALOE), version 18. The analysis is carried out for the UARS data obtained between January 1992 and September 1994 in the 100-to 1-mbar (approx. 17-47 km) altitude range and over 10 degrees latitude bins from 70 S to 70 N. The spatiotemporal evolution of aerosol surface area density (SAD) is adopted from analysis of the Stratospheric Aerosol and Gas Experiment (SAGE) II data. A diurnal steady state photochemical box model, constrained by the temperature, ozone, H2O, CH4, aerosol SAD, and columns of O2 and O3 above the point of interest, has been used as the main tool to analyze these data. Total inorganic nitrogen (NOy) is obtained by three different methods: (1) as a sum of the UARS-measured NO, NO2, HNO3, and ClONO2; (2) from the N2O-NOy correlation, and (3) from the CH4-NOy correlation. To validate our current understanding of stratospheric heterogeneous chemistry for post-Pinatubo conditions, the model-calculated monthly averaged NOx/NOy ratios and the NO, NO2, and HNO3 profiles are compared with the UARS-derived data. In general, the UARS-constrained box model captures the main features of nitrogen species partitioning in the post-Pinatubo years, such as recovery of NOx after the eruption, their seasonal variability and vertical profiles. However, the model underestimates the NO2 content, particularly in the 30- to 7-mbar (approx.23-32 km) range. Comparisons of the calculated temporal behavior of the partial columns of NO2 and HNO3 and ground-based measurements at 45 S and 45 N are also presented. Our analysis indicates that ground-based and HALOE v.18 measurements of the NO2 vertical columns are consistent within the range of their uncertainties and are systematically higher (up to 50%) than the model results at midlatitudes in both hemispheres. Reasonable agreement is obtained for HNO3 columns at 45 S, suggesting some problems with nitrogen species partitioning in the model. Outstanding uncertainties are discussed.
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