University of Maine

About: University of Maine is a education organization based out in Orono, Maine, United States. It is known for research contribution in the topics: Population & Ice sheet. The organization has 8637 authors who have published 16932 publications receiving 590124 citations. The organization is also known as: University of Maine at Orono.

Dealing with Stakeholders: How Reputation, Credibility and Framing Influence the Game

Abstract: Reputation is clearly a growing area of research and practitioner interest. Models that assist in our understanding of research and that aid practitioners in managing reputation are to be encouraged. In this paper, a model of reputation formation is proposed and the notion of reputation in issue, stakeholder, and process areas is addressed. Examples of these elements of reputation are offered, to help sharpen our understanding of reputation in action. In addition, the impact of credibility and framing on reputation is closely reviewed. Credibility refers to the organization’s past history and how it develops reputational expectations over time. Framing is a process of ordering beliefs around an issue. In this paper, three questions are raised for consideration and suggestions are offered for further research and practitioner action.

Climate control of terrestrial carbon exchange across biomes and continents

Abstract: Understanding the relationships between climate and carbon exchange by terrestrial ecosystems is critical to predict future levels of atmospheric carbon dioxide because of the potential accelerating effects of positive climate–carbon cycle feedbacks. However, directly observed relationships between climate and terrestrial CO2 exchange with the atmosphere across biomes and continents are lacking. Here we present data describing the relationships between net ecosystem exchange of carbon (NEE) and climate factors as measured using the eddy covariance method at 125 unique sites in various ecosystems over six continents with a total of 559 site-years. We find that NEE observed at eddy covariance sites is (1) a strong function of mean annual temperature at mid- and high-latitudes, (2) a strong function of dryness at mid- and low-latitudes, and (3) a function of both temperature and dryness around the mid-latitudinal belt (45°N). The sensitivity of NEE to mean annual temperature breaks down at ~ 16 °C (a threshold value of mean annual temperature), above which no further increase of CO2 uptake with temperature was observed and dryness influence overrules temperature influence.

Measurement Issues in Emotion Research With Children and Adolescents

Abstract: The need for a multimethod approach to the study of emotion in children and adolescents is crucial, as is a multilevel analysis in which emotional experience is assessed at a variety of levels (Solomon, 2002). This review highlights the critical role of emotion theory when constructing and selecting appropriate assessment tools with a focus on Functionalist theory that emphasizes the importance of contextual variables (Barrett & Campos, 1987). The review begins with an examination of theoretical and pragmatic issues in emotion measurement followed by discussions of four basic methods of emotion assessment (i.e., self-report, other-report, observation, neurophysiology). Implications of emotion assessment for clinical practice and future directions for research conclude the review.

Stratigraphic effects of tubificids in profundal lake sediments1

Abstract: Experiments conducted with natural mixed populations of 800 and 1,800 tubificids m−2 in sediment from Messalonskee Lake, Maine, showed average sediment transport by alimentation at 10°C 2–3 times greater than highest rates previously reported. More than 95% of feeding on introduced pollen was at depths above 7 cm, with greatest feeding at 3–4 cm. Small amounts of pollen were raised to the surface from as deep as 15 cm. Downward transport was 14 and 19% of upward. Small pollen grains (< 40 µ) were fed upon and displaced at higher rates than large grains. Organic matter was less in the surface layer of feces than in sediment from feeding depths and in surface sediment where no worms were present. A mathematical model was used to appraise the stratigraphic effects of the worms by deriving age-frequency composition of sediment at various depths.