Orbital Debris Quarterly News

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When Do Opponents of Gay Rights Mobilize? Explaining Political Participation in Times of Backlash against Liberalism

Existing research suggests that supporters of gay rights have outmobilized their opponents, leading to policy changes in advanced industrialized democracies. At the same time, we observe the diffusion of state-sponsored homophobia in many parts of the world. The emergence of gay rights as a salient political issue in global politics leads us to ask, “Who is empowered to be politically active in various societies?” What current research misses is a comparison of levels of participation (voting and protesting) between states that make stronger and weaker appeals to homophobia. Voters face contrasting appeals from politicians in favor of and against gay rights globally. In an analysis of survey data from Europe and Latin America, we argue that the alignment between the norms of sexuality a state promotes and an individual’s personal attitudes on sexuality increases felt political efficacy. We find that individuals who are tolerant of homosexuality are more likely to participate in states with gay-friendly policies in comparison with intolerant individuals. The reverse also holds: individuals with low education levels that are intolerant of homosexuality are more likely to participate in states espousing political homophobia

PECCI Code (Python Estimation for Carbon Concentration and Isotopes) for Calculating the Concentration and Stable Carbon Isotopic Composition of Dissolved Inorganic Carbon (DIC) in Precipitation for northwestern Arkansas

In karst settings, hydrograph separations using isotopic tracers are commonly and effectively used to quantify the proportions of rain rapidly delivered to springs along fractures and conduits during storm events. Dissolved inorganic carbon (DIC) is an effective, non‐conservative tracer for use in hydrograph separations of karst waters because of the ubiquitous nature of carbon in the sources of waters to caves and springs and unique concentrations and isotopic compositions of carbon inputs. DIC concentration and isotopic composition (δ¹³C‐DIC) in rain are typically calculated based on atmospheric carbon dioxide (CO₂) using equilibrium carbonate reactions and stable carbon isotope fractionation values. As atmospheric CO₂ changes, traditional assumptions applied in attaining calculated values can result in error, and better estimates of rain DIC are needed. The concentration and isotopic composition of rain DIC in the karst of northwestern Arkansas was calculated using Python™ programming language based on local atmospheric CO₂ and rain pH data from 2011 to 2013. Python™ provides an open‐source code and rapid means to complete iterative calculations, and the PECCI code (Python™ Estimation for Carbon Concentration and Isotopes) can be used for rain DIC calculations in other areas. Measured northwestern Arkansas atmospheric CO₂ had a median concentration of 397.7 ± 4.3 ppm and increased slightly over three years and median δ¹³C‐CO₂ was ‐8.5 ±0.4 ‰. Rain samples exhibited a median pH of 5.6 ±0.4. Calculated rain DIC ranged from 0.17 to 0.34 mg/L and δ13C‐DIC ranged from ‐8.5‰ to ‐8.2‰ between 5 and 30 °C. At an average annual temperature of 14.6 °C, rain DIC was calculated to be 0.25 mg/L and δ¹³C‐DIC was ‐8.34 ‰. Although the variations in DIC are small, the concentration and isotopic composition of end‐member sources in hydrograph separations controls the final hydrologic budget calculations. The PECCI code can be modified to calculate rain DIC for otherstudy sites or time periods