1,287 research outputs found

    Experimental Demonstration of Spectral Intensity Optical Coherence Tomography

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    We demonstrate experimentally quantum-inspired, spectral-domain intensity optical coherence tomography. We show that the technique allows for both axial resolution improvement and dispersion cancellation compared to conventional optical coherence tomography. The method does not involve scanning and it works with classical light sources and standard photodetectors. The measurements are in excellent agreement with the theoretical predictions. We also propose an approach that enables the elimination of potential artifacts arising from multiple interfaces

    Geomagnetic disturbances on ground associated with particle precipitation during SC

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    We have examined several cases of magnetosphere compression by solar wind pressure pulses using a set of instruments located in the noon sector of auroral zone. We have found that the increase in riometric absorption (sudden commencement absorption, SCA) occurred simultaneously with the beginning of negative or positive magnetic variations and broadband enhancement of magnetic activity in the frequency range above 0.1 Hz. Since magnetic variations were observed before the step-like increase of magnetic field at equatorial station (main impulse, MI), the negative declinations resembled the so-called preliminary impulse, PI. In this paper a mechanism for the generation of PI is introduced whereby PI's generation is linked to SCA – associated precipitation and the local enhancement of ionospheric conductivity leading to the reconstruction of the ionospheric current system prior to MI. Calculation showed that PI polarity depends on orientation of the background electric field and location of the observation point relative to ionospheric irregularity. For one case of direct measurements of electric field in the place where the ionospheric irregularity was present, the sign of calculated disturbance corresponded to the observed one. High-resolution measurements on IRIS facility and meridional chain of the induction magnetometers are utilized for the accurate timing of the impact of solar wind irregularity on the magnetopause

    Journal Staff

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    Multi-decadal studies of community and ecosystemdynamics are rare; however, this time frame is most relevant for assessing the impact of anthropogenic influences and climate change on ecosystems. For this reason, we investigated changes in vegetation and microtopography over 52 years in two contrasting mire ecosystems, one ombrotrophic (bog) and one minerotrophic (fen), representing different successional stages and contrasting hydrological settings. In both peatlands, floristic composition was recorded in the same permanent plots (n = 55-56, 0.25 m(2)) in both 1960 and 2012 and microtopography was mapped over a large area (ca. 2500 m(2)) that encompassed these same plots. We quantified and compared the community-level changes and internal spatial dynamics, tested associations between pH/microtopography and community/species change, and examined how the area and location of hummock microforms had changed over time. The bog exhibited little site level change in vegetation, where few species changed significantly in cover and plot frequency. However, detailed analyses revealed some large within-plot changes over time in the bog, illustrating that bogs can be highly dynamic systems at a fine scale. In contrast, the rich fen experienced a clear directional change; specifically, bryophyte abundance decreased by 70% and brown mosses were almost extinct. Although pH had decreased over time at the rich fen, this decrease at the plot-level was not associated with the decline of brown moss abundance. The microtopographic structure did not change substantially at the bog where similar to 70% was covered by lawn/hummocks; however, in the rich fen hummocks expanded (from 10% to 16% cover) and moved or expanded down slope. Our study suggests, that at the site-level, the bog ecosystem was more resistant to environmental changes over time compared to the rich fen, as evidenced by shifts in vegetation and microtopography. The contrasting scales of vegetation dynamics observed within a bog (i.e., within-plot changes vs. site-level) indicate that plant-environment feedbacks contribute to the peatland level stability. While in rich fens, internal feedbacks may be weaker and the ecosystem's vegetation and microtopographic structure are vulnerable to shifting hydrological fluxes

    Teacher Education in the Arctic

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    Peer reviewedPublisher PD

    Proceedings of the Morpho Challenge 2010 Workshop

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    In natural language processing many practical tasks, such as speech recognition, information retrieval and machine translation depend on a large vocabulary and statistical language models. For morphologically rich languages, such as Finnish and Turkish, the construction of a vocabulary and language models that have a sufficient coverage is particularly difficult, because of the huge amount of different word forms. In Morpho Challenge 2010 unsupervised and semi-supervised algorithms are suggested to provide morpheme analyses for words in different languages and evaluated in various practical applications. As a research theme, unsupervised morphological analysis has received wide attention in conferences and scientific journals focused on computational linguistic and its applications. This is the proceedings of the Morpho Challenge 2010 Workshop that contains one introduction article with a description of the tasks, evaluation and results and six articles describing the participating unsupervised and supervised learning algorithms. The Morpho Challenge 2010 Workshop was held at Espoo, Finland in 2-3 September, 2010.reviewe

    The Importance of Reindeer in Northern Finland during World War II (1939–45) and the Post-War Reconstruction

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    We studied the consequences of World War II (WWII, 1939–45) for reindeer herding in northern Finland, evaluated the significance of the livelihood for the population during and after the war, and identified the factors that made successful reconstruction of the livelihood possible. The study is based on qualitative content analysis of articles published in the professional journal Poromies (‘Reindeer Herder’) during the period 1931–67. Reindeer were an important source of food, transport, clothing, footwear, and skins for soldiers during the war. Approximately 220 000 reindeer were slaughtered to provide food, averting the compulsory slaughter of 88 000 cows. Herders’ skills were highly valued during the war. The herds and herders figured in the reconstruction of northern Finland and contributed to the war reparations owed the Soviet Union. During the period 1939–45 the number of reindeer fell dramatically, and the cession of Finnish territories to the Soviet Union and destruction of fences made herding difficult. In addition, the area of pastureland available to reindeer decreased. The combined effects of military operations, a labour shortage, an increased number of predators, and difficult weather and snow conditions led to losses of reindeer. The recovery of the livelihood to its pre-war level took 10 years. We argue that in addition to improved post-war pasture conditions—a result of decreased reindeer densities and favourable weather—the rapid recovery of reindeer herding can be attributed to the high motivation, diligence, and experiential knowledge of herders and the herding administration gained in rebuilding the livelihood after WWI (1914–18). Both groups understood that in northern Finland it would be economically wiser to invest in reindeer husbandry rather than cattle farming since reindeer are better adapted than cattle to the harsh climate and to forage grown in low-productive soils. Reindeer herding was based on natural pastures and labour, whereas cattle farming relied on crop cultivation, as well as expensive buildings, machinery, and fertilizers.Nous avons Ă©tudiĂ© les consĂ©quences de la DeuxiĂšme Guerre mondiale (1939–1945) sur l’élevage des rennes dans le nord de la Finlande, Ă©valuĂ© l’importance des moyens de subsistance de la population pendant et aprĂšs la guerre et dĂ©terminĂ© les facteurs permettant la reconstruction rĂ©ussie des moyens de subsistance. L’étude est basĂ©e sur une analyse du contenu qualitatif d’articles publiĂ©s dans la revue professionnelle Poromies (« Ă©leveur de rennes ») entre 1931 et 1967. Les rennes Ă©taient une source importante de nourriture, de transport, de vĂȘtements, de chaussures et de peaux pour les soldats durant la guerre. Environ 220 000 rennes se sont fait abattre pour fournir de la nourriture, Ă©vitant l’abattage obligatoire de 88 000 vaches. Les compĂ©tences des Ă©leveurs Ă©taient trĂšs recherchĂ©es pendant la guerre. Les troupeaux et les Ă©leveurs ont jouĂ© un rĂŽle dans la reconstruction du nord de la Finlande et contribuĂ© aux rĂ©parations de guerre pour dommages causĂ©s Ă  l’Union soviĂ©tique. De 1939 Ă  1945, on a assistĂ© Ă  un dĂ©clin trĂšs important de la population de rennes; la cession des territoires finlandais Ă  l’Union soviĂ©tique et la destruction de clĂŽtures ont rendu l’élevage difficile. De plus, les zones de pĂąturage des rennes ont diminuĂ©. Les effets des opĂ©rations militaires alliĂ©s Ă  la pĂ©nurie de main-d’oeuvre, Ă  l’augmentation du nombre de prĂ©dateurs, aux conditions mĂ©tĂ©orologiques difficiles et aux conditions de la neige ont entraĂźnĂ© la perte de rennes. Le rĂ©tablissement des moyens de subsistance Ă  leur niveau d’avant-guerre a pris dix ans. Nous soutenons qu’en plus de l’amĂ©lioration des conditions de pĂąturage d’aprĂšs-guerre (le rĂ©sultat du dĂ©clin de la densitĂ© de population de rennes et de conditions mĂ©tĂ©orologiques favorables), le rĂ©tablissement rapide de l’élevage de rennes peut ĂȘtre attribuĂ© au niveau de motivation Ă©levĂ©, Ă  la diligence et aux connaissances acquises par l’expĂ©rience des Ă©leveurs ainsi qu’à l’administration des troupeaux dĂ©coulant de la reconstruction des moyens de subsistance aprĂšs la PremiĂšre Guerre mondiale (1914–1918). Les deux groupes ont compris que pour le nord de la Finlande, il coĂ»terait moins cher d’investir dans les activitĂ©s d’élevage de rennes plutĂŽt que dans les activitĂ©s d’élevage des bovins, car les rennes s’adaptent mieux que les bovins au climat rigoureux et au fourrage qui pousse dans les sols moins productifs. L’élevage de rennes reposait sur les pĂąturages naturels et le travail, tandis que l’élevage des bovins reposait sur la culture des plantes, sans compter les bĂątiments, la machinerie et les engrais coĂ»teux

    No association of BMI and body adiposity with cardiometabolic biomarkers among a small sample of reindeer herders of sub-Arctic Finland

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    The rising global obesity rate is alarming due to its real health and socioeconomic consequences. Finland, like other circumpolar regions, is also experiencing a rise in obesity . Here we assess BMI, body adiposity, and measures of cardiometabolic health among a small population of reindeer herders in sub-Arctic Finland. We collected anthropometric and biomarker measures at two different time points: October 2018 (N = 20) and January 2019 (N = 21) with a total of 25 unique individuals across the data collection periods (ages 20–64). Anthropometric measures included height, weight, age, and body composition. Biomarkers included measures of cholesterol, fasting glucose, HDL cholesterol, LDL cholesterol, and triglyceride levels. Over 70% of this sample was classified as “overweight” and “obese” as categorised by BMI and 64% classified as “overfat” based on body fat percentage. However, there was no significant relationship between BMI and body fat percentage with any of the measured biomarkers. Although the sample size is small, the results of this study suggest there might not be a strong correlation between BMI, body adiposity, and cardiometabolic health indices within this population – a pattern that has been documented elsewhere. However, further study is needed to confirm this lack of a correlation

    High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes

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    International audienceThe ionospheric D-layer is a narrow bandwidth radar target often with a very small scattering cross section. The target autocorrelation function can be obtained by transmitting a series of relatively short coded pulses and computing the correlation between data obtained from different pulses. The spatial resolution should be as high as possible and the spatial side lobes of the codes used should be as small as possible. However, due to the short pulse repetition period (in the order of milliseconds) at any instant, the radar receives detectable scattered signals not only from the pulse illuminating the D-region but also from 3?5 ambiguous-range pulses, which makes it difficult to produce a reliable estimate near zero lag of the autocorrelation function. A new experimental solution to this measurement problem, using a selected set of 40-bit random codes with 4 ”s elements giving 600 m spatial resolution is presented. The zero lag is approximated by dividing the pulse into two 20-bit codes and computing the correlation between those two pulses. The lowest altitudes of the E-layer are measured by dividing the pulse into 5 pieces of 8 bits, which allows for computation of 4 lags. In addition, coherent integration of data from four pulses is used for obtaining separately the autocorrelation function estimate for the lowest altitudes and in cases when the target contains structures with a long coherence time. Design details and responses of the experiment are given, and analysed test data are shown

    EU Peatlands: Current Carbon Stocks and Trace Gas Fluxes

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    Peatlands in Europe has formed a significant sink for atmospheric CO2 since the last glacial maximum. Currently they are estimated to hold ca. 42 Gt carbon in the form of peat and are therefore a considerable component in the European carbon budget. Due to the generally wet soil conditions in peatlands they are also significant emitters of the strong greenhouse gas (GHG) methane (CH4) and in some cases also of nitrous oxide (N2O). The EU funded CarboEurope-GHG Concerted Action attempts to develop a reliable and complete greenhouse gas budget for Europe and this report aims to provide a review and synthesis of the available information about GHG exchanges in European peatlands and their underlying processes. A best estimate for all the European countries shows that some are currently sinks for atmospheric CO2 while others are sources. In contrast, for CH4 and N2O, only the sources are relevant. Whilst some countries are CO2 sinks, all countries are net GHG emitters from peatlands. The results presented, however, carry large uncertainties, which cannot be adequately quantified yet. One outstanding uncertainty is the distribution of land use types, particular in Russia, the largest European peat nation. The synthesis of GHG exchange, nevertheless, indicates some interesting features. Russia hosts an estimated 41% of European peatlands and contributes most to all GHG exchanges (CO2: 25%, CH4: 52%, N2O: 26%, Total: 37%). Germany is the second-largest emitter (12% of European total) although it contains only 3.2% of European peatlands. The reason is the use of most of the peatland area for intensive cropland and grassland. The largest CO2 emitters are countries with large agricultural peatland areas (Russia, Germany, Belarus, Poland), the largest N2O emitters are those with large agricultural fen areas (Russia, Germany, Finland). In contrast, the largest CH4 emitters are concentrated in regions with large areas of intact mires, namely Russia and Scandinavia. High average emission densities above 3.5 t C-equiv. ha-1 are found in the Southeast Mediterranean, Germany and the Netherlands where agricultural use of peatlands is intense. Low average emission densities below 0.3 t C-equiv. ha-1 occur where mires and peatland forests dominate, e.g. Finland and the UK. This report concludes by pointing at key gaps in our knowledge about peatland carbon stocks and GHG exchanges which include insufficient basic information on areal distribution of peatlands, measurements of peat depth and also a lack of flux datasets providing full annual budgets of GHG exchanges
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