Child and parent perspectives of life quality of children with physical impairments compared with non-disabled peers

Publisher's version (útgefin grein).Background: Life quality has become a widely used concept within rehabilitation and occupational therapy practice. Aim: This study explored child and parent perspectives of life quality of children with physical impairments compared with a group of non-disabled children. Method: Data were collected with the Icelandic self- and proxy-reported versions of the KIDSCREEN-27. For children with physical impairments, reports from 34 children and 40 parents were included in the analyses, and in control group reports from 429 children and 450 parents were included. Results: Children with physical impairments evaluated their life quality within the average range on four out of five life quality dimensions. The lowest scores were within the physical well-being dimension. Self-reported scores of children with physical impairments were higher than those of their parents on all dimensions except autonomy and parent relations. Thus, the parents considered more environmental and personal factors to negatively influence their child’s life quality than children did themselves. Conclusion: Children with physical impairments experience their life quality similarly to non-disabled children. Significance: Focus on life quality can help occupational therapists to identify what circumstances positively or negatively influence client well-being and to focus more on contextual factors that contribute to disablement.We would like to thank the families who participated in the study. We would also like to thank Professor Barbara E Gibson at the University of Toronto who contributed to the research. The study was supported by the Icelandic Research Fund under Grant number 174299-051; and the Doctoral Grants of The University of Iceland Research Fund.Peer Reviewe

Evolution of deformation and stress changes during the caldera collapse and dyking at Bárdarbunga, 2014–2015: Implication for triggering of seismicity at nearby Tungnafellsjökull volcano

Stress transfer associated with an earthquake, which may result in the seismic triggering of aftershocks (earthquake–earthquake interactions) and/or increased volcanic activity (earthquake–volcano interactions), is a well-documented phenomenon. However limited studies have been undertaken concerning volcanic triggering of activity at neighbouring volcanoes (volcano–volcano interactions). Here we present new deformation and stress modelling results utilising a wealth of diverse geodetic observations acquired during the 2014–2015 unrest and eruption within the Bárdarbunga volcanic system. These comprise a combination of InSAR, GPS, LiDAR, radar profiling and optical satellite measurements. We find a strong correlation between the locations of increased seismicity at nearby Tungnafellsjökull volcano and regions of increased tensile and Coulomb stress changes. Our results suggest that stress transfer during this major event has resulted in earthquake triggering at the neighbouring Tungnafellsjökull volcano by unclamping faults within the associated fissure swarm. This work has immediate application to volcano monitoring; to distinguish the difference between stress transfer and new intrusive activity

Temporal stress changes associated with the 2008 May 29 Mw 6 earthquake doublet in the western South Iceland Seismic Zone

On 2008 May 29, two magnitude Mw ~ 6 earthquakes occurred on two adjacent N-S faults in the western South Iceland Seismic Zone. The first main shock was followed approximately 3 s later by the rupture on a parallel fault, about 5 km to the west. An intense aftershock sequence was mostly confined to the western fault and an E-W aligned zone, extending west of the main shock region into the Reykjanes oblique rift. In this study, a total of 325 well-constrained focal mechanisms were obtained using data from the permanent Icelandic SIL seismic network and a temporary network promptly installed in the source region following the main shocks, which allowed a high-resolution stress inversion in short time intervals during the aftershock period. More than 800 additional focal mechanisms for the time period 2001-2009, obtained from the permanent SIL network, were analysed to study stress changes associated with the main shocks. Results reveal a coseismic counter-clockwise rotation of the maximum horizontal stress of 11 +/- 10 degrees ( 95 per cent confidence level) in the main rupture region. From previous fault models obtained by inversion of geodetic data, we estimate a stress drop of about half of the background shear stress on the western fault. With a stress drop of 8-10 MPa, the pre-event shear stress is estimated to 16-20 MPa. The apparent weakness of the western fault may be caused by fault properties, pore fluid pressure and the vicinity of the fault to the western rift zone, but may also be due to the dynamic stress increase on the western fault by the rupture on the eastern fault. Further, a coseismic change of the stress regime-from normal faulting to strike-slip faulting-was observed at the northern end of the western fault. This change could be caused by stress heterogeneities, but may also be due to a southward shift in the location of the aftershocks as compared to prior events

Icelandic rhythmics: Annual modulation of land elevation and plate spreading by snow load

International audienceWe find strong correlation between seasonal variation in CGPS time series and predicted response to annual snow load in Iceland. The load is modeled using Green's functions for an elastic halfspace and a simple sinusoidal load history on Iceland's four largest ice caps. We derive E = 40 ± 15 GPa as a minimum value for the effective Young's modulus in Iceland, increasing with distance from the Eastern Volcanic Zone. We calculate the elastic response over all of Iceland to maximum snow load at the ice caps using E = 40 GPa. Predicted annual vertical displacements are largest under the Vatnajökull ice cap with a peak-to-peak seasonal displacement of ∼37 mm. CGPS stations closest to the ice cap experience a peak-to-peak seasonal displacement of ∼16 mm, consistent with our model. East and north of Vatnajökull we find the maximum of annual horizontal displacements of ∼6 mm resulting in apparent modulation of plate spreading rates in this area

A new high-rate continuous GPS network in Iceland for crustal deformation research

Edytem equipe 2 2003-201