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It is a scientist's mission to try to remain unbiased. However, certain factors play a role in scientific analyses that are not controlled by conscious thought. These factors are potentially very important in areas of science where interpretations are based on a scientist's ability to identify patterns or structures. One such area is the micromorphology of glacial sediments. In this paper we investigate the role of an analyst's experience in relation to pattern perception with specific reference to turbate microstructures in glacial diamictons. An experiment was conducted on 52 participants, which demonstrated that, as may be expected, more experienced (glacial) micromorphologists tend to exhibit a higher sensitivity-to-signal, but that complete novices, if given clear instructions, can reach levels of sensitivity similar to those of experts. It also showed, perhaps more surprisingly, that response bias does not decrease with experience. We discuss psychological factors, such as the drive for success and consistency, that may have contributed to these results and investigate their possible implications in the micromorphological analysis and interpretation of glacial sediments.

Four typical arrangements for relating faith to schooling were developed in Canada during the nineteenth century. All resulted from compromises between the assimilating traditions of Christian Constantinianism and Enlightenment liberalism. These arrangements only reluctantly accommodate the religious diversity within society. Although scholars classify Alberta's system as non-sectarian public schooling with minority denominational districts, evidence suggests the advent of a new pragmatic pluriform public school system. This new system contains many types of school authorities and structures; all but one permit some form of faith-based schooling. A broad spectrum of faiths is expressed within these school authorities. (Contains 8 notes and 1 table.)

The Canadian province of Alberta runs a unique school system that offers ten options for school plurality and choice, nine of which provide some form of faith-based schooling. This article argues that Alberta has created a pragmatic version of a "pluriform school system." This system breaks with the assumption, shared by many Christian school supporters, that faith-based schooling ought to be delivered in the private sphere. The article describes these options for choice, identifies the historical motivators that sparked efforts to pluralize the system, and lists the key consequences and problems flowing from this system.

Northern high-alpine regions are currently experiencing rapid warming, which often results in the degradation of sub-surface permafrost and the upslope advancement of vegetation. The present study combines remotely sensed MODIS Land Surface Temperatures (LSTs) and the Normalised Difference Vegetation Index (NDVI) with observed air temperatures to model the thermal and vegetational dynamics in NE Jotunheimen (Norway) for the period 1957–2019. An altitudinal transect on the north-facing slope of Galdhøpiggen was used for ground truthing. Results indicate a substantial warming trend since the late 1950s, accompanied by increased NDVI. The spatial and temporal patterns of observed change were not uniform. Winter surface temperatures increased most rapidly, by 2.4–2.8°C at mid- and low altitudes (600–1500 m a.s.l.). The highest increases in NDVI (by ∼0.1) were detected during the growing season (April–September) and over the mid-range altitudes (1050–1500 m a.s.l.), that is, above the tree line on Galdhøpiggen. We attribute this to increased shrubification at these altitudes. Our results confirm that the surface temperatures near the previously estimated lower altitudinal limit of permafrost (∼1450 m a.s.l.) have continued to increase during the past decade, likely facilitating further permafrost degradation. Finally, we demonstrate that mapping remotely sensed mean growing season LSTs below 0°C can be used to identify areas suitable for continuous sub-surface permafrost, and mean June–September LSTs above 7°C can detect areas suitable for tree (Betula pubescens) growth in NE Jotunheimen. [ABSTRACT FROM AUTHOR]

Using data from the Canadian National Election Study, the paper examines whether religious schooling will lead to increased prejudice and intolerance, noting relationships with public funding. In general, Christians and Jews with religious schooling had similar or better scores on tolerance of Jews and non-whites than did public school students. (SM)

Developing a long‐term understanding of the cryosphere is important in the study of past climatic change. Here we used a nested approach combining diverse instrumental (monthly meteorological data from four weather stations, as well as gridded data) and proxy data (based on blue intensity measurements from local tree ring records) to create a reconstruction of past summer temperature for the central Jotunheimen area in southern Norway. This record was then used to reconstruct annual glacier mass balance from 1962, the start of the yearly measurements, back to 1722, immediately prior to the regional Little Ice Age maximum. Our reconstruction of the 'average' Jotunheimen cumulative glacier mass balance is based on three representative glaciers (Storbreen, Hellstugubreen and Gråsubreen) that were synthesized into one composite record which we term 'Gjennomsnittsbreen' ('mean glacier' in Norwegian) to filter out localized controls on the behaviour of individual glaciers. While not ignoring the role of precipitation on glacier mass balance, our reconstruction demonstrates that glaciers in this region exhibit a strong summer temperature control and appear to have been declining more or less continuously since the mid‐18th century. However, it also shows that this long‐term trend of overall retreat in Jotunheimen is punctuated by relatively short‐lived periods of neutral or occasionally positive glacier mass balance, signifying periods of stillstand or small‐scale glacier advance. These periods or 'events' in our reconstruction were compared with an independent record of 12 moraine‐building events developed using lichenometry. A minimum of 10 of the moraine‐building events identifiable in our reconstruction were also identifiable in the lichenometric data which affords confidence in the performance of our interrogative model. A critical implication of this successful glacier mass balance reconstruction based on just summer temperature is that for Jotunheimen – in contrast to Norwegian maritime glaciers further to the west – there is no need (as was proposed in some previous studies) to invoke large, prolonged increases in winter snowfall to explain glacier advances, not even for events such as the Little Ice Age. [ABSTRACT FROM AUTHOR]

An environmental reconstruction based on palynological evidence preserved in peat was carried out to examine late-Holocene alpine tree line dynamics in the context of past climatic changes on Galdhøpiggen (Jotunheimen, southern Norway). We analysed a peat core taken from a mire at the present-day tree line (1000 m a.s.l.), c. 450 m downslope from the lower limit of sporadic permafrost. We adopted a combination of commonly used indicators of species' local presence to reconstruct past vegetation assemblages, such as the relative pollen abundance (%), pollen accumulation rate (PAR), and presence of indicator species. Additionally, fossil pollen from the peat sequence was compared to modern pollen from a surface moss polster to establish a modern analogue. The results were compared with studies covering the late-Holocene climatic changes in the area. The reconstruction demonstrates that a pine-dominated woodland reached above the present-day tree line at c. 4300 cal. yr BP, suggesting a warmer climate suitable for Scots pine (Pinus sylvestris) growth at this altitude. Scots pine retreated to lower altitudes between c. 3400 and 1700 cal. yr BP, accompanied by the descent of the low-alpine shrub-dominated belt, in response to cooling climatic conditions. The colder period covered c. 1700–170 cal. yr BP, and an open downy birch (Betula pubescens) woodland became widespread at 1000 m a.s.l., whilst pine remained sparse at this altitude. From c. 170 cal. yr BP onwards, warming allowed pine to re-establish its local presence alongside downy birch at 1000 m a.s.l. [ABSTRACT FROM AUTHOR]

Between 1958 and 1967, neo-Calvinist immigrants resisted the assimilating pressure of Alberta's liberal-inspired public school system by arguing that public funding should be extended to independent schools. This essay analyzes how neo-Calvinist ideas about the nature of society, the place of religion in public life, the purpose of schools, and the state's task in regards to plurality directly challenged mainstream thinking on these issues. The essay argues that the neo-Calvinists believed their new idea of a pluriform public order created space for Albertans to imagine public policies that could escape the assimilating tendencies of mainstream liberalism. Entre 1958 et 1967, les immigrants neo-calvinistes ont resiste aux pressions assimilatrices du systeme liberal d'ecoles publiques de l'Alberta en affirmant que les fonds publics devraient egalement financer les ecoles independantes. Le present article analyse comment les idees neo-calvinistes portant sur la nature de la societe, la place de la religion dans la vie publique, la raison d'etre des ecoles et la tache de l'etat en matiere de pluralite ont directement influe sur la facon de penser du grand public sur ces sujets. L'article avance que les Neo-calvinistes croyaient que leur nouvelle idee d'un ordre public pluriforme permettait aux Albertains d'imaginer des politiques publiques qui pourraient echapper aux tendances assimilatrices du liberalisme conventionnel.