RESUMEN
This report describes the rapid implementation of a statewide observational surveillance program to monitor the public's wearing of face masks in public spaces during community spread of Coronavirus disease 2019 (COVID-19). It describes how the Hawai'i State Department of Health partnered with University of Hawai'i faculty to develop and implement the surveillance program. The surveillance program involved organizing volunteers to conduct weekly direct observations in designated locations. A smartphone application (app) was created to record real-time observational surveillance data. From September 5, 2020, to March 13, 2021, a total of 84 577 observations were conducted across the state. Eighty-three percent of those observed were correctly wearing a face mask, 7% were wearing a face mask incorrectly, and 10% were not wearing a mask. Following the 2-week pilot phase of the project, volunteers were surveyed regarding facilitators and barriers for conducting observations and motivations for volunteering. Feedback was used to refine project procedures. With few states having implemented such a surveillance program, the information reported in this article may inform communities interested in tracking mask-wearing behaviors in the context of the COVID-19 pandemic.
Asunto(s)
COVID-19/prevención & control , Conductas Relacionadas con la Salud , Máscaras , Pandemias , Técnicas de Observación Conductual , Hawaii , Humanos , Salud Pública , SARS-CoV-2 , Conducta Social , Encuestas y CuestionariosRESUMEN
Lava erupts into cold sea water on the ocean floor at mid-ocean ridges (at depths of 2,500 m and greater), and the resulting flows make up the upper part of the global oceanic crust. Interactions between heated sea water and molten basaltic lava could exert significant control on the dynamics of lava flows and on their chemistry. But it has been thought that heating sea water at pressures of several hundred bars cannot produce significant amounts of vapour and that a thick crust of chilled glass on the exterior of lava flows minimizes the interaction of lava with sea water. Here we present evidence to the contrary, and show that bubbles of vaporized sea water often rise through the base of lava flows and collect beneath the chilled upper crust. These bubbles of steam at magmatic temperatures may interact both chemically and physically with flowing lava, which could influence our understanding of deep-sea volcanic processes and oceanic crustal construction more generally. We infer that vapour formation plays an important role in creating the collapse features that characterize much of the upper oceanic crust and may accordingly contribute to the measured low seismic velocities in this layer.