Research into individuals' intended behavior and performance has traditionally adopted explicitly measured, self-report constructs, and outcomes. More recently, research has shown that completing explicit self-report measures of constructs may effect subsequent behavior, termed the "mere measurement" effect. The aim of the present experiment was to investigate whether implicit measures of motivation showed a similar mere measurement effect on subsequent behavior. It may be the case that measuring the implicit systems affects subsequent implicit interventions (e.g., priming), observable on subsequent behavior. Priming manipulations were also given to participants in order to investigate the interaction between measurement and priming of motivation. Initially, a 2 [implicit association test (IAT: present vs. absent) ×2 (Prime: autonomous vs. absent) and a 2 (IAT: present vs. absent) × 2 (Prime: controlled vs. absent)] between participants designs were conducted, these were them combined into a 2 (IAT: present vs. absent) ×3 (Prime: autonomous vs. controlled vs. absent) between participants design, with attempts at a novel task taken as the outcome measure. Implicit measure completion significantly decreased behavioral engagement. Priming autonomous motivation significantly facilitated, and controlled motivation significantly inhibited performance. Finally, there was a significant implicit measurement × priming interaction, such that priming autonomous motivation only improved performance in the absence of the implicit measure. Overall, this research provides an insight into the effects of implicit measurement and priming of motivation and the combined effect of completing both tasks on behavior.

Research flights with the National Center for Atmospheric Research (NCAR) C-130 airborne laboratory were conducted over the equatorial ocean during the Pacific Atmospheric Sulfur Experiment (PASE). The focused, repetitive flight plans provided a unique opportunity to explore the principal pathways of sulfur processing in remote marine environments in close detail. Fast airborne measurements of SO2 using the Drexel University APIMS (Atmospheric Pressure Ionization Mass Spectrometer) instrument further provided unprecedented insight into the complete budget of this important sulfur gas. In general, turbulent mixing in the marine boundary layer (MBL) continuously depletes SO2 due to the shallow convection of the tropical trade wind regime by venting the gas into the buffer layer (BuL) above. However, on nearly one-third of the flights a net import of SO2 into the MBL from the BuL was observed. Concurrent measurements of the DMS budget allowed for a heterogeneous S(IV) oxidation rate to be inferred from the SO2 budget residual. The average heterogeneous loss rate was found to be 0.05 h−1, which taken in conjunction with the observed aerosol surface area distributions and O3 levels indicates that the supermicron aerosols maintain a near neutral pH. The average dry deposition velocity of SO2 was found to be 0.4 cm s−1, about 30% lower than predicted by standard parameterizations. The yield of SO2 from DMS oxidation was found to be near unity. The mission averages indicate that approximately 57% of the SO2 in the MBL is lost to aerosols, 27% is subject to dry deposition, 7% is mixed into the BuL, and 10% is oxidized by OH.

Impairments in social cognition are common in schizophrenia and predict poor functional outcome. The purpose of this proof-of-concept randomized, parallel group clinical trial was to assess whether intranasal oxytocin (OT), given before social cognitive training, enhances learning of social cognitive skills. Twenty seven male outpatients with schizophrenia participated in a 6-week (12 session) training on social cognitive skills. Training focused on three domains: facial affect recognition, social perception, and empathy. Subjects were randomly assigned (double blind) to receive either intranasal OTor placebo 30 min before each session. Participants did not receive OT between sessions or on the day of assessments. We evaluated scores on social-cognition measures, as well as clinical symptoms and neurocognition, at baseline, 1 week following the final training session, and 1 month later. Our prespecified primary outcome measure was a social-cognition composite score comprised of five individual measures. There were main effects of time (indicating improvement across the combined-treatment groups) on the social-cognition composite score at both 1 week and 1 month following completion of training. Subjects receiving OT demonstrated significantly greater improvements in empathic accuracy than those receiving placebo at both posttreatment and 1 month follow up. There were no OT-related effects for the other social cognitive tests, clinical symptoms, or neurocognition. This study provides initial support for the idea that OT enhances the effectiveness of training when administered shortly before social cognitive training sessions. The effects were most pronounced on empathic accuracy, a high-level social cognitive process that is not easily improved in current social cognitive remediation programs.

Carbonyl sulfide (COS) and other trace gases were measured in firn air collected near South Pole (89.98°S) and from air trapped in ice at Siple Dome, Antarctica (81.65°S). The results, when considered with ambient air data and previous ice core measurements, provide further evidence that atmospheric mixing ratios of COS over Antarctica between 1650 and 1850 A.D. were substantially lower than those observed today. Specifically, the results suggest annual mean COS mixing ratios between 300 and 400 pmol mol⁻¹ (ppt) during 1650–1850 A.D. and increases throughout most of the twentieth century. Measurements of COS in modern air and in the upper layers of the firn at South Pole indicate ambient, annual mean mixing ratios between 480 and 490 ppt with substantial seasonal variations. Peak mixing ratios are observed during austral summer in ambient air at South Pole and Cape Grim, Tasmania (40.41°S). Provided COS is not produced or destroyed in firn, these results also suggest that atmospheric COS mixing ratios have decreased 60–90 ppt (10–16%) since the 1980s in high latitudes of the Southern Hemisphere. The history derived for atmospheric mixing ratios of COS in the Southern Hemisphere since 1850 is closely related to historical anthropogenic sulfur emissions. The fraction of anthropogenic sulfur emissions released as COS (directly or indirectly) needed to explain the secular changes in atmospheric COS over this period is 0.3–0.6%.

Background

PrEP, a biomedical HIV prevention option, continues to be underutilized among transgender women who could benefit from sustained use, especially women of color and those who identify as Latina and/or reside in the southeastern US.

Objective

We explored the barriers and facilitators experienced by transgender women who live in Florida regarding accessing, using, and/or staying on PrEP.

Methods

In-depth interviews and focus groups were conducted in either Spanish or English with adult transgender women living in Florida (N = 22). The interviews were audio-recorded, transcribed, and coded in ATLAS.ti using thematic analyses.

Results

The mean age of the participants was 42.2 years. Among the participants, 73% were Hispanic/Latina, 59% were foreign-born, and approximately one-third were living with HIV (but had past experience with PrEP). Transgender women cited the following barriers to accessing or considering PrEP: (1) costs and benefits of PrEP use; (2) under-representation in clinical trials resulting in unknown or misinformation regarding PrEP side effects; (3) chronic poverty; and (4) trauma and discrimination. Other stressors, such as behavioral healthcare needs, were identified.

Conclusions

Our analysis revealed interlocking systems of oppression like transphobia, discrimination, and misgendering, which were common barriers experienced by our participants. These synergistically epidemic (i.e., syndemic) barriers contributed to their feelings of being systematically excluded in social spaces, research, public health planning and policies, laws, and social programs related to PrEP. These structural barriers are impediments to HIV preventive care but also act as a source of stress that contributes to mental health problems, financial vulnerability, substance abuse, and other deleterious health outcomes.

Measurements of trace gases in air trapped in polar firn (unconsolidated snow) demonstrate that natural sources of chlorofluorocarbons, halons, persistent chlorocarbon solvents and sulphur hexafluoride to the atmosphere are minimal or non-existent. Atmospheric concentrations of these gases, reconstructed back to the late nineteenth century, are consistent with atmospheric histories derived from anthropogenic emission rates and known atmospheric lifetimes. The measurements confirm the predominance of human activity in the atmospheric budget of organic chlorine, and allow the estimation of atmospheric histories of halogenated gases of combined anthropogenic and natural origin. The pre-twentieth-century burden of methyl chloride was close to that at present, while the burden of methyl bromide was probably over half of today's value.

We differentiate the event-by-event n-γ multiplicity data from Cf252(sf) with respect to the energies of the emitted particles as well as their relative angles of emission. We determine that neutron emission enhances γ-ray emission around 0.7 and 1.2 MeV, but the only directional alignment was observed for Eγ≤0.7 MeV and tended to be parallel and antiparallel to neutrons emitted in the same event. The emission of γ rays at other energies was determined to be nearly isotropic. The presence of the emission and alignment enhancements is explained by positive correlations between neutron emission and quadrupole γ-ray emission along rotational bands in the de-exciting fragments. This observation corroborates the hypothesis of positive correlations between the angular momentum of a fragment and its intrinsic excitation energy. The results of this work are especially relevant in view of the recent theoretical and experimental interest in the generation of angular momentum in fission. Specifically, we have determined an alignment of the fragment's angular momenta in a direction perpendicular to the direction of motion. We interpret the lack of n-γ angular correlations for fission fragments near closed shells as a weakening of the alignment process for spherical nuclei. Lastly, we have observed that statistical γ rays are emitted isotropically, indicating that the average angular momentum removed by this radiation is small. These results, and the analysis tools presented in this work, represent a stepping stone for future analysis of n-γ emission correlations and their connection to angular momentum properties.

Observations during the 2006 dry season of highly elevated concentrations of cyanides in the atmosphere above Mexico City (MC) and the surrounding plains demonstrate that biomass burning (BB) significantly impacted air quality in the region. We find that during the period of our measurements, fires contribute more than half of the organic aerosol mass and submicron aerosol scattering, and one third of the enhancement in benzene, reactive nitrogen, and carbon monoxide in the outflow from the plateau. The combination of biomass burning and anthropogenic emissions will affect ozone chemistry in the MC outflow.

Formaldehyde (HCHO) columns measured from space provide constraints on emissions of volatile organic compounds (VOCs). Quantitative interpretation requires characterization of errors in HCHO column retrievals and relating these columns to VOC emissions. Retrieval error is mainly in the air mass factor (AMF) which relates fitted backscattered radiances to vertical columns and requires external information on HCHO, aerosols, and clouds. Here we use aircraft data collected over North America and the Atlantic to determine the local relationships between HCHO columns and VOC emissions, calculate AMFs for HCHO retrievals, assess the errors in deriving AMFs with a chemical transport model (GEOS-Chem), and draw conclusions regarding space-based mapping of VOC emissions. We show that isoprene drives observed HCHO column variability over North America; HCHO column data from space can thus be used effectively as a proxy for isoprene emission. From observed HCHO and isoprene profiles we find an HCHO molar yield from isoprene oxidation of 1.6 ± 0.5, consistent with current chemical mechanisms. Clouds are the primary error source in the AMF calculation; errors in the HCHO vertical profile and aerosols have comparatively little effect. The mean bias and 1σ uncertainty in the GEOS-Chem AMF calculation increase from <1% and 15% for clear skies to 17% and 24% for half-cloudy scenes. With fitting errors, this gives an overall 1σ error in HCHO satellite measurements of 25-31%. Retrieval errors, combined with uncertainties in the HCHO yield from isoprene oxidation, result in a 40% (1σ) error in inferring isoprene emissions from HCHO satellite measurements. Copyright 2006 by the American Geophysical Union.