RESUMO
INTRODUCTION: Secondhand smoke exposure increases the risk of premature death and disease in children and non-smoking adults. As a result, many US states and local jurisdictions have enacted comprehensive indoor smoking restrictions (ISR). Indoor vaping restrictions (IVR) have also been adopted to protect against exposure to secondhand e-cigarette aerosol. This study aimed to quantify state and national US coverage of policies restricting indoor cigarette and e-cigarette use over time. METHODS: Data from the American Nonsmokers Rights' Foundation on US ISR from 1990 to 2021 and IVR from 2006 to 2021 were analyzed. Combining these data with 2015 US Census population estimates, the percentage of state and national residents covered by partial and comprehensive restrictions in bars, restaurants, and workplaces, were calculated (analysis in 2023-2024) over time. RESULTS: Between 1990-2021, national coverage of comprehensive ISR increased for bars (0% to 67.3%), restaurants (0% to 78.2%), and workplaces (0% to 77.5%). Partial ISR coverage decreased for bars (14.8% to 13.9%), restaurants (40.2% to 15.4%) and workplaces (40.2% to 22.5%). From 2006 to 2021, comprehensive IVR coverage increased for bars (0% to 43.5%), restaurants (0% to 51.5%), and workplaces (0% to 53.2%). Despite these increases in coverage, by the end of 2021, <50% of the population was protected by comprehensive ISR for bars, restaurants, and workplaces in 19, 12, and 14 states, respectively. CONCLUSIONS: The percentage of the US population protected by ISR and IVR has increased over time. However, gaps in coverage remain, which may contribute to disparities in tobacco-related disease and death.
RESUMO
Several indices of large-scale patterns of surface temperature variation were used to investigate climate change in North America over the 20th century. The observed variability of these indices was simulated well by a number of climate models. Comparison of index trends in observations and model simulations shows that North American temperature changes from 1950 to 1999 were unlikely to be due to natural climate variation alone. Observed trends over this period are consistent with simulations that include anthropogenic forcing from increasing atmospheric greenhouse gases and sulfate aerosols. However, most of the observed warming from 1900 to 1949 was likely due to natural climate variation.