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1

Strömberg, Arne G. B. "The Caledonides in Jämtland." Geologiska Föreningen i Stockholm Förhandlingar 108, no. 3 (September 1986): 305–8. http://dx.doi.org/10.1080/11035898609454717.

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2

Jaarnek, A. M., K. Norrby, B. Stencrantz, and J. Winoy. "Planning and Budgeting in Jämtland." European Journal of Public Health 2, no. 3-4 (1992): 173–74. http://dx.doi.org/10.1093/eurpub/2.3-4.173.

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3

Holm, Olof. "The Dating of Västerhus Cemetery A Contribution to the Study of Christianization in Jämtland." Current Swedish Archaeology 14, no. 1 (June 10, 2021): 109–42. http://dx.doi.org/10.37718/csa.2006..06.

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In this article, the author uses different dating methods to try to show that the Västerhus cemetery was established between c. 1125 and 1250 and that it ceased to be used between c. 1375 and 1500.This time period is later than the dates proposed previously on the basis of 14C analyses of skeletons from the cemetery. In the author's opinion, the 14C dates are probably misleading on account of reservoir effects. The Västerhus church and cemetery —which yielded one of the best preserved and rnost well-studied medieval skeletal materials in northern Europe —were thus not established at the time of Jämtland's official Christianization, as earlier claimed, but instead one or a few generations later. The author points out that several other early churches and cemeteries in Jämtland are just as late. Similar gaps in time between the official Christianization and the widespread building of churches are also known from other parts of Scandinavia.
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4

Holm, Olof. "Förstörelsen av helgonbilder i reformationstidens Jämtland." Historisk tidsskrift 96, no. 04 (December 11, 2017): 389–419. http://dx.doi.org/10.18261/issn.1504-2944-2017-03-02.

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5

LUNDQVIST, JAN, and W. G. MOOK. "Finite date of the Jämtland Interstadial." Boreas 10, no. 2 (January 16, 2008): 133–35. http://dx.doi.org/10.1111/j.1502-3885.1981.tb00477.x.

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6

Holm, Olof. "Digerdödens följder för jordägandet – exemplet jämtland." Historisk tidsskrift 90, no. 01 (April 7, 2011): 7–32. http://dx.doi.org/10.18261/issn1504-2944-2011-01-02.

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7

Gustafsson, Harald. "Jämtland och den jämtländska världen 1000-1645." Scandinavian Journal of History 37, no. 5 (December 2012): 679–80. http://dx.doi.org/10.1080/03468755.2012.726824.

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8

Rushton, Adrian W. A., and Thomas Weidner. "The Furongian trilobiteIrvingellafrom Jämtland and Ångermanland, Sweden." GFF 132, no. 3-4 (September 2010): 193–200. http://dx.doi.org/10.1080/11035897.2010.529502.

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9

Donner-Amnell, Jakob. "Elinvoimaista ja kestävää kehitystä kasvuseutujen ulkopuolella?" Terra 132, no. 3 (November 25, 2020): 115–31. http://dx.doi.org/10.30677/terra.95473.

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This article studies how two peripheral Nordic regions (Jämtland, Sweden and Kainuu, Finland) have coped with demographic, economic, and sustainability challenges during 2010s. Hard hit by depopulation and globalization, they have implemented many measures to increase vitality, diversification, and sustainability of their economies. The process, the outcome, and local actors’ views have been analysed by utilising perspectives from regional development, smart shrinking, and sustainability transitions literatures. Research results show that Jämtland and Kainuu have succeeded in diversifying their economy, better their employment, and take steps towards sustainability by relying on place-specific resources and on collaboration with external actors. They still have challenges, especially related to demography and regional imbalance, but also potential for a stronger role in achieving national goals for a sustainable, carbon neutral society. Based on these findings, some conclusions concerning the future of these and similar regions and the design of national policies affecting them can be reached.
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10

Berglund, Mikael, and Niklas Dahlström. "Post-glacial fault scarps in Jämtland, central Sweden." GFF 137, no. 4 (September 24, 2015): 339–43. http://dx.doi.org/10.1080/11035897.2015.1036361.

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11

Ahlberg, Per. "Agnostid trilobites from the Ordovician of Jämtland, Sweden." Geologiska Föreningen i Stockholm Förhandlingar 110, no. 3 (September 1988): 267–78. http://dx.doi.org/10.1080/11035898809455451.

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12

Cherns, Lesley. "A medusoid from the Late Ordovician or Early Silurian of Jämtland, central Sweden." Journal of Paleontology 68, no. 4 (July 1994): 716–21. http://dx.doi.org/10.1017/s0022336000026159.

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Patanacta pedina n. gen. and sp. is interpreted as a medusoid from the late Ordovician or early Silurian of Jämtland, central Sweden. The unique specimen is from the Kyrkås Quartzite Formation, a poorly fossiliferous, allochthonous sequence of metasediments in a lower nappe of the frontal zone of the Scandinavian Caledonides. A marginal marine depositional environment is inferred for the Kyrkås facies.
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13

Norrby, K. "Activities of Local Political Board in PHC in Jämtland." European Journal of Public Health 2, no. 3-4 (1992): 175. http://dx.doi.org/10.1093/eurpub/2.3-4.175.

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14

Sturkell, E. F. F. "The marine Lockne impact structure, Jämtland, Sweden: a review." Geologische Rundschau 87, no. 3 (December 14, 1998): 253–67. http://dx.doi.org/10.1007/s005310050208.

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15

Palm, Hans. "Seismic images of Caledonian structures in Jämtland and Tröndelag." Geologiska Föreningen i Stockholm Förhandlingar 113, no. 2-3 (September 10, 1991): 263. http://dx.doi.org/10.1080/11035899109453873.

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16

Mötus, Mari-Ann. "Tabulate corals from the Lower Silurian of Jämtland (Sweden)." GFF 126, no. 4 (December 1, 2004): 339–52. http://dx.doi.org/10.1080/11035890401264339.

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17

Sturkell, Erik F. F., Curt Broman, Per Forsberg, and Peter Torssander. "Impact-related hydrothermal activity in the Lockne impact structure, Jämtland, Sweden." European Journal of Mineralogy 10, no. 3 (June 22, 1998): 589–606. http://dx.doi.org/10.1127/ejm/10/3/0589.

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18

Tornevi, Andreas, Camilla Andersson, Ana Cristina Carvalho, Joakim Langner, Nikolai Stenfors, and Bertil Forsberg. "Respiratory Health Effects of Wildfire Smoke during Summer of 2018 in the Jämtland Härjedalen Region, Sweden." International Journal of Environmental Research and Public Health 18, no. 13 (June 29, 2021): 6987. http://dx.doi.org/10.3390/ijerph18136987.

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During the summer of 2018 Sweden experienced a high occurrence of wildfires, most intense in the low-densely populated Jämtland Härjedalen region. The aim of this study was to investigate any short-term respiratory health effects due to deteriorated air quality generated by the smoke from wildfires. For each municipality in the region Jämtland Härjedalen, daily population-weighted concentrations of fine particulate matter (PM2.5) were calculated through the application of the MATCH chemistry transport model. Modelled levels of PM2.5 were obtained for two summer periods (2017, 2018). Potential health effects of wildfire related levels of PM2.5 were examined by studying daily health care contacts concerning respiratory problems in each municipality in a quasi-Poisson regression model, adjusting for long-term trends, weekday patterns and weather conditions. In the municipality most exposed to wildfire smoke, having 9 days with daily maximum 1-h mean of PM2.5 > 20 μg/m3, smoke days resulted in a significant increase in daily asthma visits the same and two following days (relative risk (RR) = 2.64, 95% confidence interval (CI): 1.28–5.47). Meta-estimates for all eight municipalities revealed statistically significant increase in asthma visits (RR = 1.68, 95% CI: 1.09–2.57) and also when grouping all disorders of the lower airways (RR = 1.40, 95% CI: 1.01–1.92).
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19

Larsson, Martin N. A., Matti W. Leino, and Jenny Hagenblad. "Genetic Diversity in 19th Century Barley (Hordeum vulgare) Reflects Differing Agricultural Practices and Seed Trade in Jämtland, Sweden." Diversity 13, no. 7 (July 9, 2021): 315. http://dx.doi.org/10.3390/d13070315.

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Landrace crops are important genetic resources, both for plant breeding efforts and for studying agrarian history. The distribution of genetic diversity among landraces can reflect effects of climate, economic structure, and trade also over a limited spatial and temporal scale. In this study, we have SNP genotyped historical barley seed samples from the late 19th century, together with extant barley landrace accessions from Jämtland, Sweden, a county centrally located, situated between Sweden and Norway. We found two main genetic clusters, one associated with the main agricultural district around lake Storsjön and one in the peripheral areas. Data was also compared with genotypes from landraces from across the Scandinavian peninsula. Accessions from the peripheral part of Jämtland show genetic similarity to accessions from a large part of central Scandinavia, while the accessions from the Storsjön district are more differentiated. We suggest that these dissimilarities in genetic diversity distribution are explained by differences in the relative importance of agriculture and trading. We further compared the historical material with ex situ preserved extant landraces from the same region and found that their genetic diversity was not always representative of the given provenience. The historical material, in contrast, proved particularly valuable for assessing how crop genetic diversity has historically been influenced by economic focus.
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20

Dahlqvist, Peter, and Stig M. Bergström. "The lowermost Silurian of Jämtland, central Sweden: conodont biostratigraphy, correlation and biofacies." Transactions of the Royal Society of Edinburgh: Earth Sciences 96, no. 1 (March 2005): 1–19. http://dx.doi.org/10.1017/s0263593300001218.

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ABSTRACTThe Late Ordovician–Early Silurian succession in Jämtland includes the marine Kogsta Siltstone, which is unconformably overlain by the shallow-water Ede Quartzite that grades into the open-marine Berge Limestone. A Hirnantia shelly fauna dates the uppermost Kogsta Siltstone as Hirnantian, and shelly fossils indicate an Aeronian age for the Berge Limestone. Biostratigraphically highly diagnostic conodonts of the early-middle Aeronian Pranognathus tenuis Zone provide the first firm date of the Upper Ede Quartzite and the lowermost Berge Limestone. The Lower Ede Quartzite has not yielded fossils, but sedimentological data suggest it to be of Hirnantian age and reflect the glacio-eustatic low-stand. The contact between the Lower and Upper Ede Quartzite, here taken to be the Ordovician–Silurian boundary, appears to be an unconformity associated with a stratigraphic gap that at least includes the Rhuddanian Stage. The biostratigraphically important conodonts Pranognathus tenuis, Kockelella? manitoulinensis, and Pranognathus siluricus are recorded from Sweden for the first time, and these and other conodonts are used for correlations with coeval units in Europe and North America. In a regional review of Aeronian conodont faunas, three intergrading, apparently depth-related, conodont biofacies are recognised, the Jämtland conodonts representing the one characteristic of the shallowest water.
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21

Almqvist, Bjarne S. G., Hagen Bender, Amanda Bergman, and Uwe Ring. "Magnetic properties of pseudotachylytes from western Jämtland, central Swedish Caledonides." Solid Earth 11, no. 3 (May 7, 2020): 807–28. http://dx.doi.org/10.5194/se-11-807-2020.

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Abstract. Fault kinematics can provide information on the relationship and assembly of tectonic units in an orogen. Magnetic fabric studies of faults where pseudotachylytes form have recently been used to determine direction and sense of seismic slip in prehistoric earthquakes. Here we apply this methodology to study magnetic fabrics of pseudotachylytes in field structures of the Köli Nappe Complex (central Swedish Caledonides), with the aim to determine fault kinematics and decipher the role of seismic faulting in the assembly of the Caledonian nappe pile. Because the pseudotachylyte veins are thin, we focused on small (ca. 0.2 to 0.03 cm3) samples for measuring the anisotropy of magnetic susceptibility. The small sample size challenges conventional use of magnetic anisotropy and results acquired from such small specimens demand cautious interpretation. Importantly, we find that magnetic fabric results show inverse proportionality among specimen size, degree of magnetic anisotropy and mean magnetic susceptibility, which is most likely an analytical artifact related to instrument sensitivity and small sample dimensions. In general, however, it is shown that the principal axes of magnetic susceptibility correspond to the orientation of foliation and lineation, where the maximum susceptibility (k1) is parallel to the mineral lineation, and the minimum susceptibility (k3) is dominantly oriented normal to schistosity. Furthermore, the studied pseudotachylytes develop distinct magnetic properties. Pristine pseudotachylytes preserve a signal of ferrimagnetic magnetite that likely formed during faulting. In contrast, portions of the pseudotachylytes have altered, with a tendency of magnetite to break down to form chlorite. Despite magnetite breakdown, the altered pseudotachylyte mean magnetic susceptibility is nearly twice that of altered pseudotachylyte, likely originating from the Fe-rich chlorite, as implied by temperature-dependent susceptibility measurements and thin-section observations. Analysis of structural and magnetic fabric data indicates that seismic faulting occurred during exhumation into the upper crust, but these data yield no kinematic information on the direction and sense of seismic slip. Additionally, the combined structural field and magnetic fabric data suggest that seismic faulting was postdated by brittle E–W extensional deformation along steep normal faults. Although the objective of finding kinematic indicators for the faulting was not fully achieved, we believe that the results from this study may help guide future studies of magnetic anisotropy with small specimens (<1 cm3), as well as in the interpretation of magnetic properties of pseudotachylytes.
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22

Eriksson, Mikael, and Ingmar Bergström. "Familial malignant blood disease in the county of Jämtland, Sweden." European Journal of Haematology 38, no. 3 (April 24, 2009): 241–45. http://dx.doi.org/10.1111/j.1600-0609.1987.tb01170.x.

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23

Boethius, G. "Recording of Drug Prescriptions in the County of Jämtland, Sweden." Acta Medica Scandinavica 202, no. 1-6 (April 24, 2009): 241–51. http://dx.doi.org/10.1111/j.0954-6820.1977.tb16821.x.

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24

Wu, Rong-Chang, Mikael Calner, Oliver Lehnert, Olof Peterffy, and Michael M. Joachimski. "Lower–Middle Ordovician δ13C chemostratigraphy of western Baltica (Jämtland, Sweden)." Palaeoworld 24, no. 1-2 (March 2015): 110–22. http://dx.doi.org/10.1016/j.palwor.2015.01.003.

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25

Sturkell, Erik F. F., and Jens Ormö. "Magnetometry of the marine, Ordovician Lockne impact structure, Jämtland, Sweden." Journal of Applied Geophysics 38, no. 3 (January 1998): 195–207. http://dx.doi.org/10.1016/s0926-9851(97)00031-1.

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26

Simon, Stephan. "Caledonian deformation of basement in the Lockne area, Jämtland, central Sweden." Geologiska Föreningen i Stockholm Förhandlingar 109, no. 4 (December 15, 1987): 269–73. http://dx.doi.org/10.1080/11035898709453088.

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27

STURKELL, ERIK F. F. "Resurge morphology of the marine Lockne impact crater, Jämtland, central Sweden." Geological Magazine 135, no. 1 (January 1998): 121–27. http://dx.doi.org/10.1017/s0016756897007875.

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In the Brunflo area of Jämtland, central Sweden, a Cambrian to Ordovician sedimentary sequence rests on a Proterozoic crystalline basement. The area lies just outside the site of the middle Ordovician Lockne impact, and it later experienced Caledonian overthrusting. The degree of Caledonian tectonization of the Palaeozoic varies, but an autochthonous Cambrian and Ordovician sequence apparently occurs in the greater part of the area, particularly in the north. The pre-impact sedimentary succession is 81 m thick in the autochthon, with the Middle Ordovician Furudal Limestone as uppermost member. Brunflo village is located just outside the crater, 8–9 km north of its centre, but the area was affected by the impact. The impact-generated ejecta and resurge deposits rest on a surface which cuts the sedimentary strata at a low angle. This surface cuts at progressively higher stratigraphic levels at increasing distance from the crater. According to observations in the autochthon the impact generated an erosion surface dipping 1–2° towards the crater centre. The sequence of events that shaped this surface began with bombardment with high-speed ejecta closely followed by resurging water. The resurge mixed ejecta clasts with the products of resurge erosion to form the resurge deposits. No rim wall can be traced at the Lockne impact structure, probably because a rim wall, if it formed, collapsed in the modification stage owing to local lithological conditions and because the remains of it were completely eroded in the resurge phase. It is suggested the rim wall formed in sedimentary strata with unlithified clays at their base, and that this clay was unable to support it.
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28

Sturkell, Erik. "Tremadocian Ceratopyge Limestone identified by means of conodonts, in Jämtland, Sweden." Geologiska Föreningen i Stockholm Förhandlingar 113, no. 2-3 (September 10, 1991): 185–88. http://dx.doi.org/10.1080/11035899109453854.

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29

Högdahl, K., L. P. Gromet, and S. Claesson. "The geochronology of a ductile shear zone in Jämtland, central Sweden." GFF 118, sup004 (October 1996): 14–15. http://dx.doi.org/10.1080/11035899609546276.

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30

Dahlqvist, Peter, Leif Johansson, and Ulf Söderlund. "Provenance of Late Ordovician clastic sedimentary rocks in Jämtland, central Sweden." GFF 128, no. 4 (December 2006): 311–20. http://dx.doi.org/10.1080/11035890601284311.

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31

GRAHN, YNGVE. "Chitinozoan biostratigraphy of the early Caradocian Lockne impact structure, Jämtland, Sweden." Meteoritics & Planetary Science 32, no. 6 (November 1997): 745–51. http://dx.doi.org/10.1111/j.1945-5100.1997.tb01564.x.

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32

DAHLQVIST, PETER. "Late Ordovician (Hirnantian) depositional pattern and sea-level change in shallow marine to shoreface cycles in central Sweden." Geological Magazine 141, no. 5 (September 2004): 605–16. http://dx.doi.org/10.1017/s0016756804009446.

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The Upper Ordovician Kyrkås Quartzite Formation at the Nifsåsen Quarry (Jämtland, Sweden) exhibits c. 90 m of siliciclastic sedimentary rocks deposited on a shallow shelf at the craton-attached part of the Caledonian foreland basin. Five lithologies are distinguished, including claystone, mudstone, siltstone, subarkose and sublitharenite. Based on these five lithologies, sedimentary structures and biota, three marine facies associations are defined: the Mudstone association (FA1) deposited close to storm wave base, the Sandstone/mudstone association (FA2) formed between storm and fair-weather wave bases, and the Sandstone association (FA3) accumulated above fair-weather wave base. The facies associations are arranged in two sequences, c. 50 and 40 m thick, separated by a transgressive surface, indicating repeated shoreline progradation. Both sequences commence with marine heterolithic shales and siltstones, with upwardly increasing frequency of tempestites. Continued shoaling is indicated by a dominance of hummocky and trough (locally tabular) cross-stratified sandstone beds in the upper part of each sequence. Sand beds are increasingly amalgamated up-sequence, reflecting progressively diminishing accommodation space. The depositional style and sedimentary structures indicate that the study area was storm-dominated with an abundant supply of siliciclastic material. Biostratigraphic data tie the depositional changes to the globally recognized Late Ordovician (Hirnantian) glacial interval. These data suggest that the first sequence was formed during the initial phase of regression in the earliest Hirnantian. The lowermost part of the overlying sequence contains elements of a typical Hirnantia fauna followed by beds yielding Normalograptus persculptus, suggesting a second regressive cycle in the Jämtland basin during the early N. persculptus Biozone.
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33

Jakobsson, Mikael. "Burial Layout, Society and Sacred Geography - A Viking Age Example from Jämtland." Current Swedish Archaeology 5, no. 1 (June 10, 2021): 79–98. http://dx.doi.org/10.37718/csa.1997.06.

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ln the Viking Age cotnmunity in the Lake Storsjön district in central Jämtland the landscape, the society and the religion formed a conceptual totality. The political power had religious overtones and was legitimized through the topography of the district, which was comprehended by the inhabitants as god-given. This result has been achieved through structural analysis of two different source materials. One is an analysis of the sacred place-names in the district. The other analysis has used the richly furnished Viking Age cemetery of Röstahammaren, in particular its most well-equipped grave, male grave IV. There are structural parallels between these materials,
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34

Omberg, M. "(P1-82) Implementation of an Active Vaccination Strategy Increased the Pandemic Influenza A (H1N1) 2009 Vaccine Coverage among Swedish Children." Prehospital and Disaster Medicine 26, S1 (May 2011): s125. http://dx.doi.org/10.1017/s1049023x11004146.

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IntroductionThe European Center for Disease Control and Prevention (ECDC) identified young children as a group at higher risk of developing severe pandemic influenza A (H1N1) 2009 infection compared with the general population. Since children have high attack rates and seem essential in augmenting local outbreaks of influenza, vaccination of children was an important objective in the Swedish pandemic influenza A (H1N1) 2009 vaccination campaign. Children < 13 years of age were recommended to take two doses of the pandemic vaccine (Pandemrix®).ObjectiveThe objective of this study was to compare the vaccination coverage among children 1–12 years of age in different councils in the County of Jämtland, Sweden that either implemented an active advocating or a passive vaccination strategy. The active strategy included direct information to parents promoting vaccination, individual appointments, collaboration between different care providers, and visits of vaccination teams to day care centers and schools, whereas no specific measures, except general information in press and media, were undertaken in councils using a passive approach.MethodsAll pandemic vaccinations in the County of Jämtland were registered in a Web-based registration software system. Vaccine coverage was determined by comparing the actual number of children residing in different councils with the number of vaccinated children.ResultsA total of 4,162 of 6,000 children (69.3%) residing in councils using an active vaccination strategy were vaccinated compared with 5,059 of 9,373 children (53.9%) living in councils using a passive vaccination strategy (p < 0.0001)ConclusionsImplementation of an active advocating vaccination strategy during the Swedish pandemic influenza A (H1N1) 2009 vaccination campaign resulted in a significantly higher vaccination coverage rate compared with a passive vaccination strategy.
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35

Farnes, Elisabeth. "Norsk Arkeologisk Selskaps tur til Jämtland og Härjedalen 26.–29. mai 2016." Viking 80 (September 10, 2017): 243. http://dx.doi.org/10.5617/viking.5483.

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36

Rosell, Catherine, Johanna Andersson, Karin Kockum, Otto Lilja-Lund, Lars Söderström, and Katarina Laurell. "Prevalence of idiopathic normal pressure hydrocephalus - a pilot study in Jämtland, Sweden." Fluids and Barriers of the CNS 12, Suppl 1 (2015): O55. http://dx.doi.org/10.1186/2045-8118-12-s1-o55.

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37

Sturkell, E. F. F., A. Ekelund, and R. Törnberg. "Gravity modelling of Lockne, a marine impact structure in Jämtland, central Sweden." Tectonophysics 296, no. 3-4 (November 1998): 421–35. http://dx.doi.org/10.1016/s0040-1951(98)00149-8.

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38

Toverud, Öivind. "Geochemical prospecting for gold in the county of Jämtland, upper central Sweden." Journal of Geochemical Exploration 32, no. 1-3 (April 1989): 61–63. http://dx.doi.org/10.1016/0375-6742(89)90047-2.

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39

Jian-Hua, Zhang. "Review of the Ordovician conodont zonal index Eoplacognathus suecicus Bergström, 1971." Journal of Paleontology 73, no. 3 (May 1999): 487–93. http://dx.doi.org/10.1017/s0022336000027992.

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Over 600 elements of the Ordovician conodont index Eoplacognathus suecicus Bergström, 1971, were obtained from the Segerstad and Skärlöv Limestones at the Lunne section, which is the type locality of E. suecicus, and at the Kullstaberg section both in Jämtland, Sweden. Specimens of E. suecicus from different stratigraphic levels and representing different growth stages show obvious morphological differences. The stratigraphically early elements of E. suecicus are very similar to the stratigraphically late elements of Eoplacognathus pseudoplanus (Viira), being distinguished mainly by the appearance of the secondary postero-lateral denticle row in the stelliplanate element. Eoplacognathus suecicus apparently was derived from E. pseudoplanus, and probably evolved into Eoplacognathus lindstroemi (Hamar).
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40

Lundqvist, Jan. "The Revsund Area, Central Jämtland—An Example of Preglacial Weathering and Landscape Formation." Geografiska Annaler: Series A, Physical Geography 70, no. 4 (December 1988): 291–98. http://dx.doi.org/10.1080/04353676.1988.11880259.

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41

Cherns, Lesley, and Lars Karis. "Late Ordovician – early Silurian transgressive sedimentation in the Jämtland basin, central Swedish Caledonides." GFF 117, no. 1 (March 1995): 23–30. http://dx.doi.org/10.1080/11035899509546193.

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42

Sturkell, Erik F. F. "Impact-related Ir anomaly in the Middle Ordovician Lockne impact structure, Jämtland, Sweden." GFF 120, no. 4 (December 1998): 333–36. http://dx.doi.org/10.1080/11035899801204333.

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43

Lorendahl, Bengt. "New cooperatives and local development: A study of six cases in Jämtland, Sweden." Journal of Rural Studies 12, no. 2 (April 1996): 143–50. http://dx.doi.org/10.1016/0743-0167(96)00006-x.

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44

Månsson, Kristina. "Middle Ordovician olenid trilobites (Triarthrus Green and Porterfieldia Cooper) from Jämtland, central Sweden." Transactions of the Royal Society of Edinburgh: Earth Sciences 89, no. 1 (1998): 47–62. http://dx.doi.org/10.1017/s0263593300002352.

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AbstractTriarthrinid trilobites are described from the Middle Ordovician Andersön Shale and Örån Shale of Jämtland, central Sweden. The faunas include at least five species, belonging to two genera, Porterfieldia Cooper 1953 and Triarthrus Green 1832. Porterfieldia is represented by a single species, Porterfieldia humilis (Hadding 1913), while at least four species belong to Triarthrus: T. freji Thorslund, 1940, T. jemtlandicus Linnarsson, 1875, T. latissimus nom. nov. and T. linnarssoni Thorslund, 1940. P. humilis is found only in the lower Andersön Shale, equivalent to the Hustedograptus teretiusculus Zone. T. freji, T. jemtlandicus and T. latissimus occur frequently in the upper part of the Anderson Shale, which comprises the Nemagraptus gracilis Zone, and probably also the lower part of the Diplograptus multidens Zone. T. linnarssoni occurs throughout the Örån Shale (mainly Dicranograptus clingani Zone). T. jemtlandicus and T. aff. linnarssoni are also sporadically present in the lower and middle parts of the Oran Shale. Almost all growth stages of T. latissimus, from the anaprotaspid stage and onwards, are represented and the ontogeny is described. The early stages are, however, comparatively uncommon.
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45

Tornevi, Andreas, Camilla Andersson, Ana Carvalho, Joakim Langner, and Bertil Forsberg. "Potential Health Impacts from a Wildfire Smoke Plume over Region Jämtland Härjedalen, Sweden." Atmosphere 14, no. 10 (September 26, 2023): 1491. http://dx.doi.org/10.3390/atmos14101491.

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In the summer of 2018, Sweden experienced widespread wildfires, particularly in the region of Jämtland Härjedalen during the final weeks of July. We previously conducted an epidemiological study and investigated acute respiratory health effects in eight municipalities relation to the wildfire air pollution. In this study, we aimed to estimate the potential health impacts under less favorable conditions with different locations of the major fires. Our scenarios focused on the most intense plume from the 2018 wildfire episode affecting the largest municipality, which is the region’s only city. Combining modeled PM2.5 concentrations, gridded population data, and exposure–response functions, we assessed the relative increase in acute health effects. The cumulative population-weighted 24 h PM2.5 exposure during the nine highest-level days reached 207 μg/m3 days for 63,227 inhabitants. We observed a small number of excess cases, particularly in emergency unit visits for asthma, with 13 additional cases compared to the normal 12. Overall, our scenario-based health impact assessment indicates minor effects on the studied endpoints due to factors such as the relatively small population, limited exposure period, and moderate increase in exposure compared to similar assessments. Nonetheless, considering the expected rise in fire potential due to global warming and the long-range transport of wildfire smoke, raising awareness of the potential health risks in this region is important.
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46

Sjöstedt, Angelika. "”Längtan efter något som man anar, men inte vet riktigt vad det är ens”." lambda nordica 24, no. 1 (July 28, 2019): 67–87. http://dx.doi.org/10.34041/ln.v24.565.

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I handen håller jag en rektangulär häftad och grå smårutig skrivbok med rödfärgade kanter. Boken har tillhört min gammelmormor Ingeborg Göransson. Hon föddes i en jordbrukarfamilj i Offerdals socken i Jämtland 1893. Det är under hennes tid som seminarist i Östersund under åren 1912 till 1914 och sedermera lärarinna i byn Enarsvedjan i Offerdal från 1914 till 1918, som anteckningarna i boken är skrivna. I denna artikel gör jag en queerläsning såväl av Ingeborgs egna anteckningar som av berättelser om hennes liv utifrån muntliga utsagor. Min läsning av Ingeborgs texter innebär en dubbel analytisk akt: att samtidigt både ifrågasätta heteronormativitet som tolkningsram för livshistorier oavsett tid och rum och problematisera det som i vår tid blivit till normativa föreställningar om hur och var queera liv kan levas.
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47

Ekblom, Robert, and Peter Carlsson. "Beräkning av dubbelbeckasinens Gallinago media bestånd i Sverige baserat på nya inventeringar vid Ånnsjön och Storlien." Ornis Svecica 17, no. 1 (January 1, 2007): 37–47. http://dx.doi.org/10.34080/os.v17.22705.

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An estimate of the total Swedish population of the Great Snipe Gallinago media is presented. Today, the Scandinavian Great Snipe population is found only in the mountain range of Sweden and Norway. The present population estimate is based on recent census work in the western part of the province of Jämtland, holding approximately 10% of the known Swedish leks. Suitable habitats were identified on vegetation maps, and selected areas were visited during the lekking season from mid-May to mid-June. The population densities found in these sample areas were extrapolated to the total area of suitable habitat in the Swedish mountain range. We estimate the total Swedish population to comprise around 1,800 lekking males, presumably corresponding to a similar number of breeding females.
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48

Månsson, Kristina. "Dionidid and raphiophorid trilobites from the middle Ordovician (Viruan Series) of Jämtland, central Sweden." Transactions of the Royal Society of Edinburgh: Earth Sciences 90, no. 4 (1999): 317–29. http://dx.doi.org/10.1017/s0263593300002650.

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AbstractDionidid and raphiophorid trilobites are described from the middle Ordovician (Viruan Series) of Jämtland, central Sweden. The family Dionididae is represented by one genus, Dionide Barrande, 1847, and the family Raphiophoridae by five genera, Ampyx Dalman, 1827, Ampyxella Dean, 1960, Ampyxoides Whittington, 1965, Cnemidopyge Whittard, 1955 and Lonchodomas Angelin, 1854. Seven species are described and discussed. Three of these are new: Dionide jemtlandica sp. nov., Ampyxoides minor sp. nov. and Lonchodomas striolatus sp. nov.. The majority of the trilobites described are from the Andersön Shale, equivalent to the H. teretiusculus, N. gracilis and lowermost D. multidens Zones (upper Llanvirn and lower Caradoc), and the Örån Shale, equivalent to the lower D. dingani and the uppermost D. multidens Zones (middle Caradoc). Meraspid and early holaspid material of D. jemtlandica is described.
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Borglund, Erik A. M., Lena-Maria Öberg, and Thomas Persson Slumpi. "Success Factors for Police Investigations in a Hybrid Environment: The Jämtland Police Authority Case." International Journal of Police Science & Management 14, no. 1 (March 2012): 83–93. http://dx.doi.org/10.1350/ijps.2012.14.1.264.

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50

Bennike, Ole, and Ronnie Liljegren. "Dating of a muskox (Ovibos moschatus) skull fragment from Jämtland, Sweden: Middle Weichselian age." GFF 136, no. 2 (February 12, 2014): 406–9. http://dx.doi.org/10.1080/11035897.2013.848929.

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