Results of computer assisted navigation in Total Knee Arthroplasty (TKA): comparison with the conventional method

The aim of this retrospective study was to compare the clinical and radiographic results after TKA (PFC, DePuy), performed either by computer assisted navigation (CAS, Brainlab, Johnson&Johnson) or by conventional means. Material and methods: Between May and December 2006 we reviewed 36 conventional TKA performed between 2002 and 2003 (group A) and 37 navigated TKA performed between 2005 and 2006 (group B) by the same experienced surgeon. The mean age in group A was 74 years (range 62-90) and 73 (range 58-85) in group B with a similar age distribution. The preoperative mechanical axes in group A ranged from -13° varus to +13° valgus (mean absolute deviation 6.83°, SD 3.86), in group B from -13° to +16° (mean absolute deviation 5.35, SD 4.29). Patients with a previous tibial osteotomy or revision arthroplasty were excluded from the study. Examination was done by an experienced orthopedic resident independent of the surgeon. All patients had pre- and postoperative long standing radiographs. The IKSS and the WOMAC were utilized to determine the clinical outcome. Patient's degree of satisfaction was assessed on a visual analogous scale (VAS). Results: 32 of the 37 navigated TKAs (86,5%) showed a postoperative mechanical axis within the limits of 3 degrees of valgus or varus deviation compared to only 24 (66%) of the 36 standard TKAs. This difference was significant (p = 0.045). The mean absolute deviation from neutral axis was 3.00° (range -5° to +9°, SD: 1.75) in group A in comparison to 1.54° (range -5° to +4°, SD: 1.41) in group B with a highly significant difference (p = 0.000). Furthermore, both groups showed a significant postoperative improvement of their mean IKSS-values (group A: 89 preoperative to 169 postoperative, group B 88 to 176) without a significant difference between the two groups. Neither the WOMAC nor the patient's degree of satisfaction - as assessed by VAS - showed significant differences. Operation time was significantly higher in group B (mean 119.9 min.) than in group A (mean 99.6 min., p <0.000). Conclusion: Our study showed consistent significant improvement of postoperative frontal alignment in TKA by computer assisted navigation (CAS) compared to standard methods, even in the hands of a surgeon well experienced in standard TKA implantation. However, the follow-up time of this study was not long enough to judge differences in clinical outcome. Thus, the relevance of computer navigation for clinical outcome and survival of TKA remains to be proved in long term studies to justify the longer operation time. References 1 Stulberg SD. Clin Orth Rel Res. 2003;(416):177-84. 2 Chauhan SK. JBJS Br. 2004;86(3):372-7. 3 Bäthis H, et al. Orthopäde. 2006;35(10):1056-65.

Cirugía bariatrica : gastrogastroplastia laparoscopica y bypass gástrico en pacientes con obesidad mórbida

La obesidad es un problema de salud global siendo la cirugía bariatrica el mejor tratamiento demostrado. El Bypass gástrico (BGYR) es el método más utilizado que combina restricción y malabsorcion; sin embargo los procedimientos restrictivos se han popularizado recientemente. La Gastro-gastroplastia produce restricción gástrica reversible por medio de un pouch gástrico con anastomosis gastrogástrica y propusimos su evaluación Métodos: Estudio retrospectivo no randomizado que evaluó archivos de pacientes con GG y BGYR laparoscópicos entre febrero de 2008 y Abril de 2011 Resultados: 289 pacientes identificados: 180 GG y 109 BGYR de los cuales 138 cumplieron criterios de inclusión, 77 (55.8%) GG y 61 (44,2%) BGYR, 18 (13%) hombres y 120 (87%) mujeres. Para GG la mediana del peso inicial fue 97,15 (± 17,3) kg, IMC inicial de 39,35 (± 3,38) kg/m2 y exceso de peso de 37,1 (±11,9). La mediana de IMC a los 1, 6 y 12 meses fue 34,8 (±3,58) kg/m2, 30,81 (±3,81) kg/m2, 29,58 (±4,25) kg/m2 respectivamente. La mediana de % PEP 1, 6 y 12 meses fue 30,9 (±14,2) %, 61,88 (±18,27) %, 68,4 (±19,64) % respectivamente. Para BGYR la mediana del peso inicial fue 108,1 (± 25,4) kg, IMC inicial 44,4 (± 8,1) y exceso de peso de 48,4 (±15,2) %. La mediana de IMC a los 1, 6 y 12 meses fue 39 (±7,5) kg/m2, 33,31 (±4,9) kg/m2, 30,9 (±4,8) kg/m2 respectivamente. La mediana de % PEP 1, 6 y 12 meses fue 25,9 (±12,9) %, 61,87 (±18,62) %, 71,41 (±21,09) % respectivamente. Seguimiento a un año Conclusiones: La gastro-gastroplastia se plantea como técnica restrictiva, reversible, con resultados óptimos en reducción de peso y alternativa quirúrgica en pacientes con obesidad. Son necesarios estudios a mayor plazo para demostrar mantenimiento de cambios en el tiempo

Cirugía bariatrica : gastrogastroplastia laparoscópica y bypass gástrico en pacientes con obesidad mórbida

La obesidad es un problema de salud global siendo la cirugía bariatrica el mejor tratamiento demostrado. El Bypass Gástrico (BGYR) es el método más utilizado que combina restricción y malabsorcion; sin embargo los procedimientos restrictivos se han popularizado recientemente. La Gastro-gastroplastia produce restricción gástrica reversible por medio de un pouch gástrico con anastomosis gastrogástrica y propusimos su evaluación Métodos: Estudio retrospectivo no randomizado que evaluó archivos de pacientes con GG y BGYR laparoscópicos entre Febrero de 2008 y Abril de 2011 Resultados: 289 pacientes identificados: 180 GG y 109 BGYR de los cuales 138 cumplieron criterios de inclusión, 77 (55.8%) GG y 61 (44,2%) BGYR, 18 (13%) hombres y 120 (87%) mujeres. Para GG la mediana del peso inicial fue 97,15 (± 17,3) kg, IMC inicial de 39,35 (± 3,38) kg/m2 y exceso de peso de 37,1 (±11,9). La mediana de IMC a los 1, 6 y 12 meses fue 34,8 (±3,58) kg/m2, 30,81 (±3,81) kg/m2, 29,58 (±4,25) kg/m2 respectivamente. La mediana de % PEP 1, 6 y 12 meses fue 30,9 (±14,2) %, 61,88 (±18,27) %, 68,4 (±19,64) % respectivamente. Para BGYR la mediana del peso inicial fue 108,1 (± 25,4) kg, IMC inicial 44,4 (± 8,1) y exceso de peso de 48,4 (±15,2) %. La mediana de IMC a los 1, 6 y 12 meses fue 39 (±7,5) kg/m2, 33,31 (±4,9) kg/m2, 30,9 (±4,8) kg/m2 respectivamente. La mediana de % PEP 1, 6 y 12 meses fue 25,9 (±12,9) %, 61,87 (±18,62) %, 71,41 (±21,09) % respectivamente. Seguimiento a un año. Conclusiones: La gastro-gastroplastia se plantea como técnica restrictiva, reversible, con resultados óptimos en reducción de peso y alternativa quirúrgica en pacientes con obesidad. Son necesarios estudios a mayor plazo para demostrar mantenimiento de cambios en el tiempo.

Cambios observados en las variables clínicas y paraclínicas en las primeras 48 horas de hospitalización en la Unidad de Cuidados Intensivos de pacientes con neumonía severa adquirida en la comunidad y su relación con la mortalidad

El pronóstico de la Neumonía Adquirida en la Comunidad Severa (NAC-S) depende de decisiones terapéuticas instauradas tempranamente. Los cambios fisiológicos ocurridos en las primeras horas pueden ser difíciles de detectar. No existe ningún modelo para la determinación temprana del éxito de la terapia instaurada en NAC-S. Metodología: Descripción de la totalidad de los pacientes con NAC-S hospitalizados en la Unidad de Cuidado Intensivo de la Fundación Cardioinfantil entre los años 2008 y 2012 haciendo comparaciones entre grupos (muertos vs. supervivientes) y entre momentos (0, 24 y 48 horas desde el ingreso a la UCI) y realizando regresión logística binaria. Resultados: Entre los pacientes que fallecieron la necesidad de soporte vasoactivo fue mayor en todos los momentos evaluados (sig=0.001), en la línea de base tuvieron mayores requerimientos de la Fracción Inspirada de O2 (mediana 0.55% vs. 0.50%, sig=0.011), a las 24 horas tuvieron pH (mediana 7.345 vs.7.370, sig=0.025) y tensión arterial diastólica (mediana 58.5mmHg vs.61.0mmHg, sig =0.049) menores, y a las 48 horas glicemia (mediana 157mg/dL vs.142mg/dL, sig =0.026) creatinina (mediana 1.1mg/dL vs.0.7mg/dL, sig =0.062) y nitrógeno ureico (mediana 35mg/dL vs. 22mg/dL, sig =0.003) mayores comparados con los pacientes que sobrevivieron. Entre los pacientes supervivientes hubo una disminución de la frecuencia cardiaca entre las 0 y 24 horas (mediana 97lpm vs. 86lpm, sig =0.000) y entre las 0 y las 48 horas (mediana 97lpm vs. 81lpm, sig=0.000) y una disminución de los neutrófilos entre las 0 y las 48 horas (mediana 9838 vs. 8617, sig=0.062). Conclusiones: Nuestros hallazgos sugieren la existencia de una secuencia de fenómenos fisiopatológicos que al ser reconocida temprana y claramente permitiría establecer un plan de reanimación más especifico y eficaz. Estas diferencias se pueden plantear en el contexto de un modelo mixto predictivo

Perfil de mercado de las provincias de Canadá a 2012

El proyecto Perfiles de Mercado de las Provincias de Canadá a 2012 busca actualizar las cifras del comercio bilateral presentes en el proyecto que lleva el mismo nombre y que adicionalmente cuenta con estadísticas, variaciones, perfiles demográficos, políticos y económicos de cada una de las provincias canadienses. Los análisis realizados y las conclusiones derivadas de este proyecto fueron suministrados luego de una priorización de los 10 principales productos demandados por cada provincia y a su vez los 10 principales productos exportados por Colombia a cada una de las provincias. Asimismo, verificando coincidencias entre la oferta y la demanda de bienes entre las provincias y Colombia. El potencial que los exportadores encontrarán en este archivo ha sido determinado en base en los productos más comercializados entre los dos países. La información proveída es considerada como una herramienta muy útil tanto para exportadores, empresarios y diferentes agentes de mercado que deseen empezar a hacer negocios con Canadá. Este documento contiene la introducción de cada provincia de Canadá así como los productos que más se destacan en el comercio bilateral y las oportunidades que sobresalen luego de la entrada en vigencia del TLC entre las partes. Adicionalmente, un ranking de los productos que a opinión de los autores (basados en la cifra comercializada de cada uno de los productos entre los países), tienen más oportunidades de entrar fácilmente al mercado canadiense, sea por acción de su bajo arancel o por acción de la demanda por parte de las provincias.

Genotipificación de HLA-B en pacientes colombianos afectados por el síndrome Stevens-Johnson y la Necrólisis Epidérmica Tóxica

Las reacciones alérgicas a medicamentos cutáneas severas (RAM) como el Síndrome Stevens Johnson (SJS) y la Necrólisis Epidérmica Tóxica (NET),caracterizadas por exantema, erosión de la piel y las membranas mucosas, flictenas, desprendimiento de la piel secundario a la muerte de queratinocitos y compromiso ocular. Son infrecuentes en la población pero con elevada morbi-mortalidad, se presentan luego de la administración de diferentes fármacos. En Asia se ha asociado el alelo HLA-B*15:02 como marcador genético para SJS. En Colombia no hay datos de la incidencia de estas RAM, ni de la relación con medicamentos específicos o potenciales y tampoco estudios de aproximación genómica de genes de susceptibilidad.

El costo de la atención ambulatoria del lupus eritematoso sistémico en Colombia. Contrastes y comparaciones con otras poblaciones.

Introducción: el lupus eritematoso sistémico (LES) es considerado una enfermedad de alto costo. La expresión clínica de la enfermedad depende de la ubicación geografía y la etnicidad. El objetivo de este estudio fue el calcular los costos ambulatorios relacionado al LES en una cohorte colombiana, identificar los predictores de costos y comparar nuestro resultados con otras poblaciones. Métodos: Se realizó una aproximación de tipo prevalencia en 100 pacientes LES en quienes se evaluaron los costos directos médicos, directos no médicos, indirectos e intangibles. Todos los costos médicos fueron evaluados usando una metodología abajo hacia arriba. Los costos directos fueron valorados desde una perspectiva social usando una metodología de micro-costeo. Los costos indirectos se evaluaron mediante una aproximación de capital humano, y los costos intangibles calculados a partir de los años de vida ajustados por calidad (AVAC). Se analizaron los datos por medio de un análisis multivariado. Para comparaciones con otras poblaciones todos los costos fueron expresados como la razón entre los costos y producto interno bruto nacional per cápita. Resultados: La media de costos totales fue 13.031±9.215 USD (ajustados por el factor de conversión de paridad del poder adquisitivo), lo cual representa el 1,66 del PIB per capita de Colombia. Los costos directos son el 64% de los costos totales. Los costos médicos representan el 80% de los costos directos,. Los costos indirectos fueron el 10% y los costos intangibles el 25% de los costos totales. Los medicamentos representaron el 45% de los costos directos. Mayores costos se relacionaron con el estrato socioeconómico, seguro médico privado, AVAC, alopecia, micofenolato mofetilo, y terapia anticoagulante. Los costos directos ajustados de los pacientes con LES en Colombia fueron mayores que en Norte América y en Europa. Conclusiones: el LES impone una carga económica importante para la sociedad. Los costos relacionados con la atención médica y AVAC fueron los principales contribuyentes al alto costo de la enfermedad. Estos resultados pueden ser referencia para determinar políticas en salud pública así como comparar el gasto en salud de forma internacional.

Percepción del riesgo biológico en el personal asistencial en un hospital de alta complejidad de la ciudad de Bogotá.

OBJETIVOS: Identificar la percepción del riesgo biológico de los trabajadores asistenciales del Hospital Central de la Policía Nacional en la ciudad de Bogotá. METODOS: se realizó un estudio analítico de corte transversal para describir la percepción acerca del riesgo biológico en 159 trabajadores asistenciales de un hospital de alta complejidad en la ciudad de Bogotá (Colombia), la información se recolectó por medio de la utilización de la encuesta validada nota técnica 578 (Portell M, Solé M, 2001). Se realizó la caracterización de la población por variables de sexo, edad, tiempo de experiencia y servicio al cual pertenece y se promediaron las respuestas obtenidas para cada ítem encuestado, obteniendo una clasificación para cada dimensión de percepción de riesgo baja (1 a 3), media (4 a 5) o alta (6 a 7). Resultados: De los 159 trabajadores asistenciales encuestados el 80.4% eran de género femenino, el 22.2% pertenecían al servicio de urgencias, el 16,5% al servicio de medicina interna y el 9.5% al servicio de pediatría, de los encuestados el 62.9% fueron auxiliares de enfermería, el 21,4% enfermeras jefes y el 6.9% médicos. Se obtuvo una percepción de riesgo alta (media aritmética mayor de 5) para todas las variables incluidas en la encuesta, demostrando conocimiento de todo el personal acerca de la alta exposición a accidentes de tipo biológico. No se encontró asociación entre la labor desempeñada y la percepción del riesgo biológico, sin embargo, se encontró una asociación entre el tiempo de experiencia del trabajador y una disminución en la magnitud del riesgo percibido (Chi cuadrado de asociación, p=0.042). Conclusiones: Los trabajadores asistenciales identifican la magnitud del riesgo biológico al que se encuentran expuestos en sus labores del día a día, sin embargo, es necesaria una mayor participación por parte del personal directivo y de los responsables de la prevención en temas de reacción ante accidentes y en la valoración del riesgo, especialmente en personas que llevan mucho tiempo desempeñando la labor.

Análisis de la política exterior norteamericana hacia Turquía, en materia de seguridad, y su influencia en el Kurdistán. Periodo 2003-2009

Este estudio tiene como objetivo analizar los elementos que articulan la Política Exterior de los Estados Unidos hacia Turquía, en materia de seguridad, y su influencia en el Kurdistán, ya que en el periodo 2003-2009 se presentaron acontecimientos que marcaron la vida política, económica, militar y social de la región del Medio Oriente, caracterizado por la presencia de los Estados Unidos. Esta investigación se desarrollara de acuerdo con el modelo de monografía, para dar un análisis teórico sobre el tema delimitado anteriormente. Se espera que el presente estudio sirva para que el lector comprenda las diferentes actuaciones de los Estados Unidos en el escenario internacional, para la consecución de sus intereses y que tenga un acercamiento en las diferentes relaciones entre los Estados para entender mejor los acontecimientos que se presentaron en el periodo a analizar.

Translating climate forecasts into agricultural terms: advances and challenges

Seasonal climate prediction offers the potential to anticipate variations in crop production early enough to adjust critical decisions. Until recently, interest in exploiting seasonal forecasts from dynamic climate models (e.g. general circulation models, GCMs) for applications that involve crop simulation models has been hampered by the difference in spatial and temporal scale of GCMs and crop models, and by the dynamic, nonlinear relationship between meteorological variables and crop response. Although GCMs simulate the atmosphere on a sub-daily time step, their coarse spatial resolution and resulting distortion of day-to-day variability limits the use of their daily output. Crop models have used daily GCM output with some success by either calibrating simulated yields or correcting the daily rainfall output of the GCM to approximate the statistical properties of historic observations. Stochastic weather generators are used to disaggregate seasonal forecasts either by adjusting input parameters in a manner that captures the predictable components of climate, or by constraining synthetic weather sequences to match predicted values. Predicting crop yields, simulated with historic weather data, as a statistical function of seasonal climatic predictors, eliminates the need for daily weather data conditioned on the forecast, but must often address poor statistical properties of the crop-climate relationship. Most of the work on using crop simulation with seasonal climate forecasts has employed historic analogs based on categorical ENSO indices. Other methods based on classification of predictors or weather types can provide daily weather inputs to crop models conditioned on forecasts. Advances in climate-based crop forecasting in the coming decade are likely to include more robust evaluation of the methods reviewed here, dynamically embedding crop models within climate models to account for crop influence on regional climate, enhanced use of remote sensing, and research in the emerging area of 'weather within climate'.

Report of the 2010 assessment of the scientific assessment panel: future ozone and its impact on surface UV

SCIENTIFIC SUMMARY Globally averaged total column ozone has declined over recent decades due to the release of ozone-depleting substances (ODSs) into the atmosphere. Now, as a result of the Montreal Protocol, ozone is expected to recover from the effects of ODSs as ODS abundances decline in the coming decades. However, a number of factors in addition to ODSs have led to and will continue to lead to changes in ozone. Discriminating between the causes of past and projected ozone changes is necessary, not only to identify the progress in ozone recovery from ODSs, but also to evaluate the effectiveness of climate and ozone protection policy options. Factors Affecting Future Ozone and Surface Ultraviolet Radiation • At least for the next few decades, the decline of ODSs is expected to be the major factor affecting the anticipated increase in global total column ozone. However, several factors other than ODS will affect the future evolution of ozone in the stratosphere. These include changes in (i) stratospheric circulation and temperature due to changes in long-lived greenhouse gas (GHG) abundances, (ii) stratospheric aerosol loading, and (iii) source gases of highly reactive stratospheric hydrogen and nitrogen compounds. Factors that amplify the effects of ODSs on ozone (e.g., stratospheric aerosols) will likely decline in importance as ODSs are gradually eliminated from the atmosphere. • Increases in GHG emissions can both positively and negatively affect ozone. Carbon dioxide (CO2)-induced stratospheric cooling elevates middle and upper stratospheric ozone and decreases the time taken for ozone to return to 1980 levels, while projected GHG-induced increases in tropical upwelling decrease ozone in the tropical lower stratosphere and increase ozone in the extratropics. Increases in nitrous oxide (N2O) and methane (CH4) concentrations also directly impact ozone chemistry but the effects are different in different regions. • The Brewer-Dobson circulation (BDC) is projected to strengthen over the 21st century and thereby affect ozone amounts. Climate models consistently predict an acceleration of the BDC or, more specifically, of the upwelling mass flux in the tropical lower stratosphere of around 2% per decade as a consequence of GHG abundance increases. A stronger BDC would decrease the abundance of tropical lower stratospheric ozone, increase poleward transport of ozone, and could reduce the atmospheric lifetimes of long-lived ODSs and other trace gases. While simulations showing faster ascent in the tropical lower stratosphere to date are a robust feature of chemistry-climate models (CCMs), this has not been confirmed by observations and the responsible mechanisms remain unclear. • Substantial ozone losses could occur if stratospheric aerosol loading were to increase in the next few decades, while halogen levels are high. Stratospheric aerosol increases may be caused by sulfur contained in volcanic plumes entering the stratosphere or from human activities. The latter might include attempts to geoengineer the climate system by enhancing the stratospheric aerosol layer. The ozone losses mostly result from enhanced heterogeneous chemistry on stratospheric aerosols. Enhanced aerosol heating within the stratosphere also leads to changes in temperature and circulation that affect ozone. • Surface ultraviolet (UV) levels will not be affected solely by ozone changes but also by the effects of climate change and by air quality change in the troposphere. These tropospheric effects include changes in clouds, tropospheric aerosols, surface reflectivity, and tropospheric sulfur dioxide (SO2) and nitrogen dioxide (NO2). The uncertainties in projections of these factors are large. Projected increases in tropospheric ozone are more certain and may lead to reductions in surface erythemal (“sunburning”) irradiance of up to 10% by 2100. Changes in clouds may lead to decreases or increases in surface erythemal irradiance of up to 15% depending on latitude. Expected Future Changes in Ozone Full ozone recovery from the effects of ODSs and return of ozone to historical levels are not synonymous. In this chapter a key target date is chosen to be 1980, in part to retain the connection to previous Ozone Assessments. Noting, however, that decreases in ozone may have occurred in some regions of the atmosphere prior to 1980, 1960 return dates are also reported. The projections reported on in this chapter are taken from a recent compilation of CCM simulations. The ozone projections, which also form the basis for the UV projections, are limited in their representativeness of possible futures since they mostly come from CCM simulations based on a single GHG emissions scenario (scenario A1B of Emissions Scenarios. A Special Report of Working Group III of the Intergovernmental Panel on Climate Change, Cambridge University Press, 2000) and a single ODS emissions scenario (adjusted A1 of the previous (2006) Ozone Assessment). Throughout this century, the vertical, latitudinal, and seasonal structure of the ozone distribution will be different from what it was in 1980. For this reason, ozone changes in different regions of the atmosphere are considered separately. • The projections of changes in ozone and surface clear-sky UV are broadly consistent with those reported on in the 2006 Assessment. • The capability of making projections and attribution of future ozone changes has been improved since the 2006 Assessment. Use of CCM simulations from an increased number of models extending through the entire period of ozone depletion and recovery from ODSs (1960–2100) as well as sensitivity simulations have allowed more robust projections of long-term changes in the stratosphere and of the relative contributions of ODSs and GHGs to those changes. • Global annually averaged total column ozone is projected to return to 1980 levels before the middle of the century and earlier than when stratospheric halogen loading returns to 1980 levels. CCM projections suggest that this early return is primarily a result of GHG-induced cooling of the upper stratosphere because the effects of circulation changes on tropical and extratropical ozone largely cancel. Global (90°S–90°N) annually averaged total column ozone will likely return to 1980 levels between 2025 and 2040, well before the return of stratospheric halogens to 1980 levels between 2045 and 2060. • Simulated changes in tropical total column ozone from 1960 to 2100 are generally small. The evolution of tropical total column ozone in models depends on the balance between upper stratospheric increases and lower stratospheric decreases. The upper stratospheric increases result from declining ODSs and a slowing of ozone destruction resulting from GHG-induced cooling. Ozone decreases in the lower stratosphere mainly result from an increase in tropical upwelling. From 1960 until around 2000, a general decline is simulated, followed by a gradual increase to values typical of 1980 by midcentury. Thereafter, although total column ozone amounts decline slightly again toward the end of the century, by 2080 they are no longer expected to be affected by ODSs. Confidence in tropical ozone projections is compromised by the fact that simulated decreases in column ozone to date are not supported by observations, suggesting that significant uncertainties remain. • Midlatitude total column ozone is simulated to evolve differently in the two hemispheres. Over northern midlatitudes, annually averaged total column ozone is projected to return to 1980 values between 2015 and 2030, while for southern midlatitudes the return to 1980 values is projected to occur between 2030 and 2040. The more rapid return to 1980 values in northern midlatitudes is linked to a more pronounced strengthening of the poleward transport of ozone due to the effects of increased GHG levels, and effects of Antarctic ozone depletion on southern midlatitudes. By 2100, midlatitude total column ozone is projected to be above 1980 values in both hemispheres. • October-mean Antarctic total column ozone is projected to return to 1980 levels after midcentury, later than in any other region, and yet earlier than when stratospheric halogen loading is projected to return to 1980 levels. The slightly earlier return of ozone to 1980 levels (2045–2060) results primarily from upper stratospheric cooling and resultant increases in ozone. The return of polar halogen loading to 1980 levels (2050–2070) in CCMs is earlier than in empirical models that exclude the effects of GHG-induced changes in circulation. Our confidence in the drivers of changes in Antarctic ozone is higher than for other regions because (i) ODSs exert a strong influence on Antarctic ozone, (ii) the effects of changes in GHG abundances are comparatively small, and (iii) projections of ODS emissions are more certain than those for GHGs. Small Antarctic ozone holes (areas of ozone <220 Dobson units, DU) could persist to the end of the 21st century. • March-mean Arctic total column ozone is projected to return to 1980 levels two to three decades before polar halogen loading returns to 1980 levels, and to exceed 1980 levels thereafter. While CCM simulations project a return to 1980 levels between 2020 and 2035, most models tend not to capture observed low temperatures and thus underestimate present-day Arctic ozone loss such that it is possible that this return date is biased early. Since the strengthening of the Brewer-Dobson circulation through the 21st century leads to increases in springtime Arctic column ozone, by 2100 Arctic ozone is projected to lie well above 1960 levels. Uncertainties in Projections • Conclusions dependent on future GHG levels are less certain than those dependent on future ODS levels since ODS emissions are controlled by the Montreal Protocol. For the six GHG scenarios considered by a few CCMs, the simulated differences in stratospheric column ozone over the second half of the 21st century are largest in the northern midlatitudes and the Arctic, with maximum differences of 20–40 DU between the six scenarios in 2100. • There remain sources of uncertainty in the CCM simulations. These include the use of prescribed ODS mixing ratios instead of emission fluxes as lower boundary conditions, the range of sea surface temperatures and sea ice concentrations, missing tropospheric chemistry, model parameterizations, and model climate sensitivity. • Geoengineering schemes for mitigating climate change by continuous injections of sulfur-containing compounds into the stratosphere, if implemented, would substantially affect stratospheric ozone, particularly in polar regions. Ozone losses observed following large volcanic eruptions support this prediction. However, sporadic volcanic eruptions provide limited analogs to the effects of continuous sulfur emissions. Preliminary model simulations reveal large uncertainties in assessing the effects of continuous sulfur injections. Expected Future Changes in Surface UV. While a number of factors, in addition to ozone, affect surface UV irradiance, the focus in this chapter is on the effects of changes in stratospheric ozone on surface UV. For this reason, clear-sky surface UV irradiance is calculated from ozone projections from CCMs. • Projected increases in midlatitude ozone abundances during the 21st century, in the absence of changes in other factors, in particular clouds, tropospheric aerosols, and air pollutants, will result in decreases in surface UV irradiance. Clear-sky erythemal irradiance is projected to return to 1980 levels on average in 2025 for the northern midlatitudes, and in 2035 for the southern midlatitudes, and to fall well below 1980 values by the second half of the century. However, actual changes in surface UV will be affected by a number of factors other than ozone. • In the absence of changes in other factors, changes in tropical surface UV will be small because changes in tropical total column ozone are projected to be small. By the middle of the 21st century, the model projections suggest surface UV to be slightly higher than in the 1960s, very close to values in 1980, and slightly lower than in 2000. The projected decrease in tropical total column ozone through the latter half of the century will likely result in clear-sky surface UV remaining above 1960 levels. Average UV irradiance is already high in the tropics due to naturally occurring low total ozone columns and high solar elevations. • The magnitude of UV changes in the polar regions is larger than elsewhere because ozone changes in polar regions are larger. For the next decades, surface clear-sky UV irradiance, particularly in the Antarctic, will continue to be higher than in 1980. Future increases in ozone and decreases in clear-sky UV will occur at slower rates than those associated with the ozone decreases and UV increases that occurred before 2000. In Antarctica, surface clear-sky UV is projected to return to 1980 levels between 2040 and 2060, while in the Arctic this is projected to occur between 2020 and 2030. By 2100, October surface clear-sky erythemal irradiance in Antarctica is likely to be between 5% below to 25% above 1960 levels, with considerable uncertainty. This is consistent with multi-model-mean October Antarctic total column ozone not returning to 1960 levels by 2100. In contrast, by 2100, surface clear-sky UV in the Arctic is projected to be 0–10% below 1960 levels.

The capability-affordance model: a method for analysis and modelling of capabilities and affordances

Existing capability models lack qualitative and quantitative means to compare business capabilities. This paper extends previous work and uses affordance theories to consistently model and analyse capabilities. We use the concept of objective and subjective affordances to model capability as a tuple of a set of resource affordance system mechanisms and action paths, dependent on one or more critical affordance factors. We identify an affordance chain of subjective affordances by which affordances work together to enable an action and an affordance path that links action affordances to create a capability system. We define the mechanism and path underlying capability. We show how affordance modelling notation, AMN, can represent affordances comprising a capability. We propose a method to quantitatively and qualitatively compare capabilities using efficiency, effectiveness and quality metrics. The method is demonstrated by a medical example comparing the capability of syringe and needless anaesthetic systems.

Climate change and infectious disease: time for a new normal?

At present, there is a clarion call for action on climate change across the global health landscape. At the recent WHO-sponsored conference on health and climate (held in Geneva, Switzerland, on Aug 27–29, 2014) and the UN Climate Summit (New York, USA, on Sept 23, 2014), participants were encouraged to act decisively to change the current trajectory of climate disruption. Health inequalities, including those related to infectious diseases, have now been pushed to centre stage. This approach represents a step-change in thinking. But as we are urged toward collective action, is it time to rethink our approach to research, especially in relation to climate change and infectious disease?