Solar ultraviolet-B radiation and vitamin D: a cross-sectional population-based study using data from the 2007 to 2009 Canadian Health Measures Survey

Background: Exposure to solar ultraviolet-B (UV-B) radiation is a major source of vitamin D3. Chemistry climate models project decreases in ground-level solar erythemal UV over the current century. It is unclear what impact this will have on vitamin D status at the population level. The purpose of this study was to measure the association between ground-level solar UV-B and serum concentrations of 25-hydroxyvitamin D (25(OH)D) using a secondary analysis of the 2007 to 2009 Canadian Health Measures Survey (CHMS). Methods: Blood samples collected from individuals aged 12 to 79 years sampled across Canada were analyzed for 25(OH)D (n=4,398). Solar UV-B irradiance was calculated for the 15 CHMS collection sites using the Tropospheric Ultraviolet and Visible Radiation Model. Multivariable linear regression was used to evaluate the association between 25(OH)D and solar UV-B adjusted for other predictors and to explore effect modification. Results: Cumulative solar UV-B irradiance averaged over 91 days (91-day UV-B) prior to blood draw correlated significantly with 25(OH)D. Independent of other predictors, a 1 kJ/m 2 increase in 91-day UV-B was associated with a significant 0.5 nmol/L (95% CI 0.3-0.8) increase in mean 25(OH)D (P =0.0001). The relationship was stronger among younger individuals and those spending more time outdoors. Based on current projections of decreases in ground-level solar UV-B, we predict less than a 1 nmol/L decrease in mean 25(OH)D for the population. Conclusions: In Canada, cumulative exposure to ambient solar UV-B has a small but significant association with 25(OH)D concentrations. Public health messages to improve vitamin D status should target safe sun exposure with sunscreen use, and also enhanced dietary and supplemental intake and maintenance of a healthy body weight.

Data assimilation with correlated observation errors: experiments with a 1-D shallow water model

Remote sensing observations often have correlated errors, but the correlations are typically ignored in data assimilation for numerical weather prediction. The assumption of zero correlations is often used with data thinning methods, resulting in a loss of information. As operational centres move towards higher-resolution forecasting, there is a requirement to retain data providing detail on appropriate scales. Thus an alternative approach to dealing with observation error correlations is needed. In this article, we consider several approaches to approximating observation error correlation matrices: diagonal approximations, eigendecomposition approximations and Markov matrices. These approximations are applied in incremental variational assimilation experiments with a 1-D shallow water model using synthetic observations. Our experiments quantify analysis accuracy in comparison with a reference or ‘truth’ trajectory, as well as with analyses using the ‘true’ observation error covariance matrix. We show that it is often better to include an approximate correlation structure in the observation error covariance matrix than to incorrectly assume error independence. Furthermore, by choosing a suitable matrix approximation, it is feasible and computationally cheap to include error correlation structure in a variational data assimilation algorithm.

Search for squarks and gluinos in events with jets and missing transverse energy using 2.1 fb(-1) of p(p)over-bar collision data at root s=1.96 TeV - D phi Collaboration

A data sample corresponding to an integrated luminosity of 2.1 fb(-1) collected by the D phi detector at the Fermilab Tevatron Collider was analyzed to search for squarks and gluinos produced in p (p) over bar collisions at a center-of-mass energy of 1.96 TeV. No evidence for the production of such particles was observed in topologies involving jets and missing transverse energy, and 95% C.L. lower limits of 379 GeV and 308 GeV were set on the squark and gluino masses, respectively, within the framework of minimal supergravity with tan beta = 3, A(0) = 0, and mu < 0. The corresponding previous limits are improved by 54 GeV and 67 GeV. (c) 2008 Elsevier B.V. All rights reserved.

Ricostruzione di un data-set ad alta risoluzione (30 secondi d'arco) di temperature massime e minime giornaliere per un'area ad orografia complessa (Trentino Alto-Adige)

Dati climatici ad alta risoluzione sono attualmente molto richiesti essendo indispensabili per la valutazione degli impatti dei cambiamenti climatici alla scala locale in svariati campi d'applicazione. Per aumentare l'offerta di tali dati per il territorio italiano viene presentata in questo studio la realizzazione di un data-set con risoluzione di trenta secondi d'arco, per le temperature massime e minime giornaliere per il Trentino Alto Adige, per il periodo che va dal 1951 al 2014. La metodologia utilizzata per proiettare i dati meteorologici di un set di stazioni su di un grigliato ad alta risoluzione si basa sull'assunzione che la struttura spazio-temporale del campo di una variabile meteorologica su una determinata area possa essere descritta dalla sovrapposizione di due campi:i valori normali relativi e un periodo standard, ovvero la climatologia,e le deviazioni da questi, ovvero le anomalie. La climatologia mensile verrà interpolata sull'intero dominio tramite una regressione lineare pesata della temperatura rispetto alla quota,stimata separatamente per ogni nodo del grigliato,con pesi legati alla topografia del territorio,in modo da attribuire di volta in volta la massima importanza alle stazioni con caratteristiche più simili a quella del punto di griglia considerato. Da questa sarà possibile tramite la sovrapposizione con le anomalie mensili ricostruite sul medesimo grigliato, ottenute mediante un'interpolazione basata su una media pesata,ottenere un grigliato a 30 secondi d'arco, di serie temporali mensili in valori assoluti. Combinando poi l'interpolazione dei rapporti delle anomalie giornaliere relative alla media mensile per un set di stazioni con i campi mensili precedentemente stimati,sarà possibile costruire il data-set a risoluzione giornaliera. Prima di quest'ultima fase sarà necessario effettuare un'operazione di sincronizzazione dei dati giornalieri per assicurarsi che non vi siano sfasamenti nelle serie utilizzate. I risultati confermano l'efficacia nell'utilizzo di tale metodo su regioni orograficamente complesse, sia nel confronto diretto con i casi di studio,nei quali si nota bene la discriminazione spaziale effettuata dal modello, che nella valutazione dell'accuratezza e della precisione dei risultati. I dati ottenuti non sono affetti da errori sistematici,mentre l'errore medio assoluto risulta pari od inferiore ai $2^{\circ}$C, in linea con precedenti studi realizzati su altre aree alpine. Il metodo e i risultati risultano soddisfacenti ma ulteriormente migliorabili, sia tramite un ulteriore ottimizzazione del modello usato, che con un aumento nella qualità dei dati sui quali è stato svolto lo studio.

Realizzazione di un data-set ad alta risoluzione (30 secondi d'arco) di precipitazioni mensili su un'area ad orografia complessa (Trentino Alto-Adige)

In questa tesi si presenta la realizzazione di un data-set ad alta risoluzione (30 secondi d'arco) di precipitazioni mensili (per il periodo 1921-2014), per la regione del Trentino-Alto Adige. Esso è basato su una densa rete di stazioni con osservazioni di lunga durata, sottoposte ai necessari controlli di qualità. La tecnica di interpolazione si basa sull'assunzione che la configurazione spazio-temporale del campo di una variabile meteorologica su una certa area possa essere descritta con la sovrapposizione di due campi: i valori normali relativi a un periodo standard (1961-1990), ossia le climatologie, e le deviazioni da questi, ossia le anomalie. Le due componenti possono venire ricostruite tramite metodologie diverse e si possono basare su data-set indipendenti. Per le climatologie bisogna avere un elevato numero di stazioni (anche se disponibili per un lasso temporale limitato); per le anomalie viceversa la densità spaziale ha un rilievo minore a causa della buona coerenza spaziale della variabilità temporale, mentre è importante la qualità dei dati e la loro estensione temporale. L'approccio utilizzato per le climatologie mensili è la regressione lineare pesata locale. Per ciascuna cella della griglia si stima una regressione lineare pesata della precipitazione in funzione dell'altitudine; si pesano di più le stazioni aventi caratteristiche simili a quelle della cella stessa. Invece le anomalie mensili si ricavano, per ogni cella di griglia, grazie a una media pesata delle anomalie delle vicine stazioni. Infine la sovrapposizione delle componenti spaziale (climatologie) e temporale (anomalie) consente di ottenere per ogni nodo del grigliato una serie temporale di precipitazioni mensili in valori assoluti. La bontà dei risultati viene poi valutata con gli errori quadratici medi (RMSE) e i coefficienti di correlazione di Pearson delle singole componenti ricostruite. Per mostrare le potenziali applicazioni del prodotto si esaminano alcuni casi studio.

A Surface Displacement Analysis for Volcan Pacaya from October 2001 through March 2013 by Means of 3-D Modeling of Precise Position GPS Data

Volcán Pacaya is one of three currently active volcanoes in Guatemala. Volcanic activity originates from the local tectonic subduction of the Cocos plate beneath the Caribbean plate along the Pacific Guatemalan coast. Pacaya is characterized by generally strombolian type activity with occasional larger vulcanian type eruptions approximately every ten years. One particularly large eruption occurred on May 27, 2010. Using GPS data collected for approximately 8 years before this eruption and data from an additional three years of collection afterwards, surface movement covering the period of the eruption can be measured and used as a tool to help understand activity at the volcano. Initial positions were obtained from raw data using the Automatic Precise Positioning Service provided by the NASA Jet Propulsion Laboratory. Forward modeling of observed 3-D displacements for three time periods (before, covering and after the May 2010 eruption) revealed that a plausible source for deformation is related to a vertical dike or planar surface trending NNW-SSE through the cone. For three distinct time periods the best fitting models describe deformation of the volcano: 0.45 right lateral movement and 0.55 m tensile opening along the dike mentioned above from October 2001 through January 2009 (pre-eruption); 0.55 m left lateral slip along the dike mentioned above for the period from January 2009 and January 2011 (covering the eruption); -0.025 m dip slip along the dike for the period from January 2011 through March 2013 (post-eruption). In all bestfit models the dike is oriented with a 75° westward dip. These data have respective RMS misfit values of 5.49 cm, 12.38 cm and 6.90 cm for each modeled period. During the time period that includes the eruption the volcano most likely experienced a combination of slip and inflation below the edifice which created a large scar at the surface down the northern flank of the volcano. All models that a dipping dike may be experiencing a combination of inflation and oblique slip below the edifice which augments the possibility of a westward collapse in the future.

German Total Ankle Replacement Register of the German Foot and Ankle Society (D. A. F.) - presentation of design and reliability of the data as well as first results

INTRODUCTION Even though arthroplasty of the ankle joint is considered to be an established procedure, only about 1,300 endoprostheses are implanted in Germany annually. Arthrodeses of the ankle joint are performed almost three times more often. This may be due to the availability of the procedure - more than twice as many providers perform arthrodesis - as well as the postulated high frequency of revision procedures of arthroplasties in the literature. In those publications, however, there is often no clear differentiation between revision surgery with exchange of components, subsequent interventions due to complications and subsequent surgery not associated with complications. The German Orthopaedic Foot and Ankle Association's (D. A. F.) registry for total ankle replacement collects data pertaining to perioperative complications as well as cause, nature and extent of the subsequent interventions, and postoperative patient satisfaction. MATERIAL AND METHODS The D. A. F.'s total ankle replacement register is a nation-wide, voluntary registry. After giving written informed consent, the patients can be added to the database by participating providers. Data are collected during hospital stay for surgical treatment, during routine follow-up inspections and in the context of revision surgery. The information can be submitted in paper-based or online formats. The survey instruments are available as minimum data sets or scientific questionnaires which include patient-reported outcome measures (PROMs). The pseudonymous clinical data are collected and evaluated at the Institute for Evaluative Research in Medicine, University of Bern/Switzerland (IEFM). The patient-related data remain on the register's module server in North Rhine-Westphalia, Germany. The registry's methodology as well as the results of the revisions and patient satisfaction for 115 patients with a two year follow-up period are presented. Statistical analyses are performed with SAS™ (Version 9.4, SAS Institute, Inc., Cary, NC, USA). RESULTS About 2½ years after the register was launched there are 621 datasets on primary implantations, 1,427 on follow-ups and 121 records on re-operation available. 49 % of the patients received their implants due to post-traumatic osteoarthritis, 27 % because of a primary osteoarthritis and 15 % of patients suffered from a rheumatic disease. More than 90 % of the primary interventions proceeded without complications. Subsequent interventions were recorded for 84 patients, which corresponds to a rate of 13.5 % with respect to the primary implantations. It should be noted that these secondary procedures also include two-stage procedures not due to a complication. "True revisions" are interventions with exchange of components due to mechanical complications and/or infection and were present in 7.6 % of patients. 415 of the patients commented on their satisfaction with the operative result during the last follow-up: 89.9 % of patients evaluate their outcome as excellent or good, 9.4 % as moderate and only 0.7 % (3 patients) as poor. In these three cases a component loosening or symptomatic USG osteoarthritis was present. Two-year follow-up data using the American Orthopedic Foot and Ankle Society Ankle and Hindfoot Scale (AOFAS-AHS) are already available for 115 patients. The median AOFAS-AHS score increased from 33 points preoperatively to more than 80 points three to six months postoperatively. This increase remained nearly constant over the entire two-year follow-up period. CONCLUSION Covering less than 10 % of the approximately 240 providers in Germany and approximately 12 % of the annually implanted total ankle-replacements, the D. A. F.-register is still far from being seen as a national registry. Nevertheless, geographical coverage and inclusion of "high-" (more than 100 total ankle replacements a year) and "low-volume surgeons" (less than 5 total ankle replacements a year) make the register representative for Germany. The registry data show that the number of subsequent interventions and in particular the "true revision" procedures are markedly lower than the 20 % often postulated in the literature. In addition, a high level of patient satisfaction over the short and medium term is recorded. From the perspective of the authors, these results indicate that total ankle arthroplasty - given a correct indication and appropriate selection of patients - is not inferior to an ankle arthrodesis concerning patients' satisfaction and function. First valid survival rates can be expected about 10 years after the register's start.