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Abstract Despite widespread interest in science communication, public engagement with science, and engaged research, a large gap exists between the theories behind science engagement and how it is practiced within the scientific community. The scholarship of science engagement is also fractured, with knowledge and insights fragmented across discourses related to science communication, informal science learning, participatory research, and sustainability science. In the present article, we share a planning tool for integrating evidence and theory from these discourses into effective programs and projects. The ECO framework promotes three distinct and interacting modes of science engagement practice: formative engagement (listening and relationship building), codesign and coproduction (action-oriented partnerships), and broader outreach (expanding networks and dissemination). By planning engagement activities with attention to these three modes of engagement, scientists and scientific research organizations will be better poised to address urgent needs for stronger connections between science and society and increased use of scientific research in decision-making. 

Winters in northeastern North America have warmed faster than summers, with impacts on ecosystems and society. Global climate models (GCMs) indicate that winters will continue to warm and lose snow in the future, but uncertainty remains regarding the magnitude of warming. Here, we project future trends in winter indicators under lower and higher climate-warming scenarios based on emission levels across northeastern North America at a fine spatial scale (1/16°) relevant to climate-related decision making. Under both climate scenarios, winters continue to warm with coincident increases in days above freezing, decreases in days with snow cover, and fewer nights below freezing. Deep snowpacks become increasingly short-lived, decreasing from a historical baseline of 2 months of subnivium habitat to <1 month under the warmer, higher-emissions climate scenario. Warmer winter temperatures allow invasive pests such as Adelges tsugae (Hemlock Woolly Adelgid) and Dendroctonus frontalis (Southern Pine Beetle) to expand their range northward due to reduced overwinter mortality. The higher elevations remain more resilient to winter warming compared to more southerly and coastal regions. Decreases in natural snowpack and warmer temperatures point toward a need for adaptation and mitigation in the multi-million-dollar winter-recreation and forest-management economies. 

Abstract Resilience is the ability of ecosystems to maintain function while experiencing perturbation. Globally, forests are experiencing disturbances of unprecedented quantity, type, and magnitude that may diminish resilience. Early warning signals are statistical properties of data whose increase over time may provide insights into decreasing resilience, but there have been few applications to forests. We quantified four early warning signals (standard deviation, lag-1 autocorrelation, skewness, and kurtosis) across detrended time series of multiple ecosystem state variables at the Hubbard Brook Experimental Forest, New Hampshire, USA and analyzed how these signals have changed over time. Variables were collected over periods from 25 to 55 years from both experimentally manipulated and reference areas and were aggregated to annual timesteps for analysis. Long-term (>50 year) increases in early warning signals of stream calcium, a key biogeochemical variable at the site, illustrated declining resilience after decades of acid deposition, but only in watersheds that had previously been harvested. Trends in early warning signals of stream nitrate, a critical nutrient and water pollutant, likewise exhibited symptoms of declining resilience but in all watersheds. Temporal trends in early warning signals of some of groups of trees, insects, and birds also indicated changing resilience, but this pattern differed among, and even within, groups. Overall, ∼60% of early warning signals analyzed indicated decreasing resilience. Most of these signals occurred in skewness and kurtosis, suggesting ‘flickering’ behavior that aligns with emerging evidence of the forest transitioning into an oligotrophic condition. The other ∼40% of early warning signals indicated increasing or unchanging resilience. Interpretation of early warning signals in the context of system specific knowledge is therefore essential. They can be useful indicators for some key ecosystem variables; however, uncertainties in other variables highlight the need for further development of these tools in well-studied, long-term research sites. 

This study initially reports on qualitative interviews (n = 17) with scientists at two Long Term Ecological Research (LTER) sites in the northeastern United States. These interviews suggest the need for greater attention to the role of communication professionals and institutional leadership in fostering high-quality public engagement. The study also reports on a follow-up quantitative survey (n = 68) conducted to better understand the degree to which LTER scientists’ views about communication professionals were meaningfully associated with perceptions about the need for robust engagement funding. The project was initially designed based on the Integrated Behavioral Model to assess how individual LTER scientists’ engagement-related attitudes, normative beliefs, and efficacy beliefs affected their communication activities. However, the combined results highlight the potential value of additional research and theorization aimed at better understanding the factors that might lead to greater cooperation between scientists and organizational communicators. 

This paper is the culmination of several meaning-making activities between an external researcher, PES practitioners, and social scientist researchers who considered the unique contributions that can be made through RPPs on PES (that is, research-practice partnerships on public engagement with science). Based on the experiences from three RPP projects, the group noted that the PES context may be particularly suited to RPPs, and identified the importance of working as thinking-partners who support reciprocal decision-making. Recommendations are made in support of using these approaches to advance practical knowledge-building and reduce shared frustrations about the disconnect between research and practice in PES. 

This paper is the culmination of several meaning-making activities between an external researcher, PES practitioners, and social scientist researchers who considered the unique contributions that can be made through RPPs on PES (that is, research-practice partnerships on public engagement with science). Based on the experiences from three RPP projects, the group noted that the PES context may be particularly suited to RPPs, and identified the importance of working as thinking-partners who support reciprocal decision-making. Recommendations are made in support of using these approaches to advance practical knowledge-building and reduce shared frustrations about the disconnect between research and practice in PES. 

Abstract Ice storms are important winter weather events that can have substantial environmental, economic, and social impacts. Mapping and assessment of damage after these events could be improved by making ice accretion measurements at a greater number of sites than is currently available. There is a need for low-cost collectors that can be distributed broadly in volunteer observation networks; however, use of low-cost collectors necessitates understanding of how collector characteristics and configurations influence measurements of ice accretion. A study was conducted at the Hubbard Brook Experimental Forest in New Hampshire that involved spraying water over passive ice collectors during freezing conditions to simulate ice storms of different intensity. The collectors consisted of plates composed of four different materials and installed horizontally; two different types of wires strung horizontally; and rods of three different materials, with three different diameters, and installed at three different inclinations. Results showed that planar ice thickness on plates was 2.5–3 times as great as the radial ice thickness on rods or wires, which is consistent with expectations based on theory and empirical evidence from previous studies. Rods mounted on an angle rather than horizontally reduced the formation of icicles and enabled more consistent measurements. Results such as these provide much needed information for comparing ice accretion data. Understanding of relationships among collector configurations could be refined further by collecting data from natural ice storms under a broader range of weather conditions.