1,721,464 research outputs found
Introduction
No full textOur continuously changing global environment requires continuous and detailed monitoring for us to understand how ecosystems are structured and function in response to climatic changes. Understanding the arctic ecosystems is of particular importance (Oechel et al., 1997). Indeed, rather than in boreal and temperate regions, the forecasted climatic changes will be first and most pronounced in the Arctic. Hence, performing long-term monitoring of an arctic ecosystem provides us with the unique ability to not only give "early warnings" of climate change impacts but also, and perhaps even more important, predict how and where in the ecosystem these will be most pronounced and with what consequences for stability, structure and function. Since 1995, Zackenberg Ecological Research Operations (ZERO) has monitored annually over 1500 variables concurrently across the physical and biological compartments of a single high-arctic terrestrial ecosystem in central Northeast Greenland. This makes ZERO the most integrated and comprehensive long-term monitoring and research programme presently operating in the Arctic. This book explores the complex physical and ecological long-term dynamics of a high-arctic terrestrial ecosystem. Since the book is based on data from ZERO, this introductory chapter presents the structural and organisational foundation for ZERO. Following our introduction are four chapters providing the climatic and ecological background together with a presentation of the study area. The rest of the book is devoted entirely to the physical, ecological and ecosystem processes
High Arctic soil CO2 and CH4 production controlled by temperature, water, freezing and snow
No full textSoil gas production processes, mainly anaerobic or aerobic soil respiration, drive major gas fluxes across the soil-atmosphere interface. Carbon dioxide (CO2) effluxes, an efflux which in most ecosystems is a result of both autotrophic and heterotrophic respiration, in particular have received international attention. The importance of both CO2 and methane (CH4) fluxes are emphasised in the Arctic because of the large amount of soil organic carbon stored in terrestrial ecosystems and changes in uptake and release due to climate changes. This chapter focuses on controls on spatial and temporal trends in subsurface CO2 and CH4 production as well as on transport and release of gases from the soil observed in the valley Zackenbergdalen. A dominance of near-surface temperatures controlling both spatial and seasonal trends is shown based on data obtained using closed chamber and eddy-correlation techniques as well as in manipulated field plots and in controlled incubation experiments. Despite variable temperature sensitivities reported, most data can be fairly well fitted to exponential temperature-dependent equations. The water content (at wet sites linked to the depth to the water table) is a second major factor regulating soil respiration processes, but the effect is quite different in contrasting vegetation types. Dry heath sites are shown to be periodically water limited during the growing season and respond therefore with high respiration rates when watered. In contrast, water saturated conditions during most of the growing season in the fen areas hinder the availability of oxygen, resulting in both CO2 and CH4 production. Thus, water table drawdown results in decreasing CH4 effluxes but increasing CO2 effluxes. Additional controls on gas production are shown to be related to the availability of substrate and plant productivity. Subsurface gas production will produce partial and total pressure gradient causing gas transport, which in well-drained soils is mainly controlled by diffusion, whereas gas advection, bubbles and transport through roots and stems may be important in more saturated soils. Bursts of CO2 gas have been observed during spring thaw and confirmed in controlled soil thawing experiments. Field observations as well as experimental work suggest that such bursts represent partly on-going soil respiration and a physical release of gas produced during the winter. The importance of winter soil respiration is emphasised because of the fact that microbial respiration in Zackenberg samples is noted down to a least -18 degrees C. Hence, the importance of winter respiration and burst events in relation to seasonal and future climate trends requires more than just summer measurements. For example, the autumn period seems important as snowfall prior to low air temperature may insulate the soil, keeping soil temperatures high. This will extend the period of high soil respiration rates and thereby increase the importance of the winter period for the annual carbon balance. Because of the complexity of factors controlling subsurface gas production, we conclude that different parts of the landscape will respond quite differently to the same climate changes as well as that short-term effects are likely to be different from long-term effects
Going Beyond Counting First Authors in Author Co-citation Analysis
Full text linkThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
The effect of vegetation type and snow depth on annual CO2 efflux in a high arctic tundra region
Full text linkThis thesis evaluates the effect of vegetation type and increased snow depth on soil temperature and annual CO2 efflux in an arctic tundra region. Snow fences were set up to manipulate snow accumulation in heath and meadow vegetation on Spitsbergen. Field campaigns lasted from July 2007 - July 2008. CO2 efflux, measured by means of a dark and closed-dynamic soil flux chamber, showed seasonal variation and was lowest in winter time. Soil temperature had a strong influence on efflux year-round, whereas vegetation type was a major driver in the growing season. Temperature based ecosystem respiration models were used to estimate annual efflux to 125 g C m-2 in heath and
162 g C m-2 in meadow sites. CO2 efflux during the 241 days long winter was about
40 g C m-2 in both vegetation types and thus contributed significantly to the annual efflux. Snow fences enhanced snow depth with about 1 m, led to significantly higher soil temperatures and increased winter effluxes with 29-87 %. Increased snow cover resulted in a delayed start of the growing season and led to moister- and for heath sites also cooler- soil conditions in summer. In meadow sites, deeper snow cover had a negative effect on the growth of non-woody plants. The results indicate that changes in winter precipitation can affect the carbon balance of arctic tundra regions by alteration of the soil temperature regime and subsequent enhancement of winter respiration
Variations on the Author
Full text link“Variations on the Author” discusses two of Eduardo Coutinho’s recent films (Um Dia na Vida, from 2010, and Últimas Conversas, posthumously released in 2015) and their contribution to the general question of documentary authorship. The director’s filmography is characterized by a consistent yet self-effacing form of authorial self-inscription: Coutinho often features as an interviewer that rather than express opinions propels discourses; an interviewer that is good at listening. This mode of self-inscription characterizes him as an author who is not expressive but who is nonetheless markedly present on the screen. In Um Dia na Vida, however, Coutinho is completely absent form the image, while Últimas Conversas, on the contrary, includes a confessional prologue that moves the director from the margins to the center of his films. This article examines the ways in which these works stand out in the filmography of a director who offers new insights into the notion of cinematic authorship
Appropriate Similarity Measures for Author Cocitation Analysis
Full text linkWe provide a number of new insights into the methodological discussion about author cocitation analysis. We first argue that the use of the Pearson correlation for measuring the similarity between authors’ cocitation profiles is not very satisfactory. We then discuss what kind of similarity measures may be used as an alternative to the Pearson correlation. We consider three similarity measures in particular. One is the well-known cosine. The other two similarity measures have not been used before in the bibliometric literature. Finally, we show by means of an example that our findings have a high practical relevance.information science;Pearson correlation;cosine;similarity measure;author cocitation analysis
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