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900 "Ancho" => 1434 "Tamanyo" => 132739 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0045" class="elsevierStyleSimplePara elsevierViewall">Photo of the convex (a) and linear (b) transducers.</p>" ] ] ] "autores" => array:1 [ 0 => array:2 [ "autoresLista" => "Alberto García-Ortega, Andrés Briones-Gómez, Sandra Fabregat, Raquel Martínez-Tomás, Miguel Ángel Martínez-García, Enrique Cases" "autores" => array:6 [ 0 => array:2 [ "nombre" => "Alberto" "apellidos" => "García-Ortega" ] 1 => array:2 [ "nombre" => "Andrés" "apellidos" => "Briones-Gómez" ] 2 => array:2 [ "nombre" => "Sandra" "apellidos" => "Fabregat" ] 3 => array:2 [ "nombre" => "Raquel" "apellidos" => "Martínez-Tomás" ] 4 => array:2 [ "nombre" => "Miguel Ángel" "apellidos" => "Martínez-García" ] 5 => array:2 [ "nombre" => "Enrique" "apellidos" => "Cases" ] ] ] ] ] "idiomaDefecto" => "en" "Traduccion" => array:1 [ "es" => array:9 [ "pii" => "S0300289615003208" "doi" => "10.1016/j.arbres.2015.07.012" "estado" => "S300" 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"tieneTextoCompleto" => true "paginas" => array:1 [ 0 => array:2 [ "paginaInicial" => "239" "paginaFinal" => "243" ] ] "autores" => array:1 [ 0 => array:4 [ "autoresLista" => "Josef Vodička, Šárka Vejvodová, David Šmíd, Jakub Fichtl, Vladimír Špidlen, Stanislav Kormunda, Jiří Hostýnek, Jiří Moláček" "autores" => array:8 [ 0 => array:4 [ "nombre" => "Josef" "apellidos" => "Vodička" "email" => array:1 [ 0 => "vodicka@fnplzen.cz" ] "referencia" => array:2 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">a</span>" "identificador" => "aff0005" ] 1 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">*</span>" "identificador" => "cor0005" ] ] ] 1 => array:3 [ "nombre" => "Šárka" "apellidos" => "Vejvodová" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">a</span>" "identificador" => "aff0005" ] ] ] 2 => array:3 [ "nombre" => "David" "apellidos" => "Šmíd" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">a</span>" "identificador" => "aff0005" ] ] ] 3 => array:3 [ "nombre" => "Jakub" "apellidos" => "Fichtl" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">a</span>" "identificador" => "aff0005" ] ] ] 4 => array:3 [ "nombre" => "Vladimír" "apellidos" => "Špidlen" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">a</span>" "identificador" => "aff0005" ] ] ] 5 => array:3 [ "nombre" => "Stanislav" "apellidos" => "Kormunda" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">a</span>" "identificador" => "aff0005" ] ] ] 6 => array:3 [ "nombre" => "Jiří" "apellidos" => "Hostýnek" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">b</span>" "identificador" => "aff0010" ] ] ] 7 => array:3 [ "nombre" => "Jiří" "apellidos" => "Moláček" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">a</span>" "identificador" => "aff0005" ] ] ] ] "afiliaciones" => array:2 [ 0 => array:3 [ "entidad" => "Department of Surgery, Faculty of Medicine in Plzeň, Charles University in Prague, University Hospital in Plzeň, Czech Republic" "etiqueta" => "a" "identificador" => "aff0005" ] 1 => array:3 [ "entidad" => "Czech Hydrometeorological Institute, Plzeň branch, Czech Republic" "etiqueta" => "b" "identificador" => "aff0010" ] ] "correspondencia" => array:1 [ 0 => array:3 [ "identificador" => "cor0005" "etiqueta" => "⁎" "correspondencia" => "Corresponding author." ] ] ] ] "titulosAlternativos" => array:1 [ "es" => array:1 [ "titulo" => "¿Tienen los fenómenos meteorológicos alguna influencia en la aparición de neumotórax espontáneo?" ] ] "resumenGrafico" => array:2 [ "original" => 0 "multimedia" => array:7 [ "identificador" => "fig0005" "etiqueta" => "Fig. 1" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr1.jpeg" "Alto" => 1686 "Ancho" => 2261 "Tamanyo" => 239320 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0045" class="elsevierStyleSimplePara elsevierViewall">Receiving Operating Curve (ROC) of the respective factors.</p>" ] ] ] "textoCompleto" => "<span class="elsevierStyleSections"><span id="sec0005" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0065">Introduction</span><p id="par0005" class="elsevierStylePara elsevierViewall">Spontaneous pneumothorax (SP) develops as a result of the rupture of subpleural blebs, emphysematous bullae or other damage to the pleura or alveolar walls. The rupture may be caused, among other things, by an increase in transpulmonary pressure.<a class="elsevierStyleCrossRefs" href="#bib0095"><span class="elsevierStyleSup">1–5</span></a> Since cases of SP often occur in groups within a short timescale, some authors suggest that they can develop as a result of weather phenomena that cause changes in transpulmonary pressure. These theories have been discussed repeatedly in the literature, but the findings are inconsistent.<a class="elsevierStyleCrossRefs" href="#bib0095"><span class="elsevierStyleSup">1,2,6–12</span></a> The aim of this study was to evaluate the possible influence of certain weather phenomena (changes in air pressure and temperature, wind speed, storms) on the emergence of SP among patients in the Plzeň Region (Czech Republic).</p></span><span id="sec0010" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0070">Materials and Methods</span><p id="par0010" class="elsevierStylePara elsevierViewall">This is a retrospective analysis of 450 cases of spontaneous pneumothorax in 394 patients treated between 1991 and 2013 at the Surgery Department of the University Hospital in Plzeň. The patient population consisted of 318 men and 76 women with the mean age of 42 years; the youngest patient was 13 years old, while the oldest was 90 years old. Two hundred and eight (208) patients had so-called primary pneumothorax (52.8%), and 186 patients had secondary pneumothorax (47.2%). The population of the Plzeň region is over 573.000 inhabitants. Meteorological data for the region were obtained from the Plzeň office of the Czech Hydrometeorological Institute. The average sea-level pressure for the Plzeň area is 1013<span class="elsevierStyleHsp" style=""></span>hPa, and the average daily pressure variation is 4<span class="elsevierStyleHsp" style=""></span>hPa. The long-term average air temperature in this region is 8<span class="elsevierStyleHsp" style=""></span>°C, while the average daily temperature deviation is 1.9<span class="elsevierStyleHsp" style=""></span>°C. We observed changes in average daily values of atmospheric pressure in hPa, the average daily air temperature in degrees Celsius, the maximum daily wind gust in m/s, and occurrence of storms for each day of that period and their potential effect on the development of SP compared to the previous period.</p><p id="par0015" class="elsevierStylePara elsevierViewall">Development of SP was described using clusters, where a cluster was defined as at least 2 cases of SP over 3 days. When such clusters were detected, we analyzed the first day of the cluster or the values of parameters over the previous 5 days. In addition to the defined clusters, we found an isolated SP rarely, where the decisive day was the day of SP development, or values of parameters investigated over the maximum of the previous 5 days. We examined the values of the parameters on the day of SP development compared to the previous day. We also examined the differences and quotients of the parameters between the onset date of SP (cluster) and the previous day, the differences and quotients of the values over the 5 days prior to development of SP, and the absolute value of these differences and quotients. Onset of SP was indicated as the first day of symptoms.</p><p id="par0020" class="elsevierStylePara elsevierViewall">Statistical analysis was performed using SAS (SAS Institute Inc., Cary, NC, USA). Basic statistical data were calculated for the parameters measured in the entire population and in the respective groups. Distribution of the individual parameters in different groups and subgroups was compared using a Wilcoxon two-sample test. Cut-off values of changes in the study parameters were identified using ROC curves and maximizing the Chi-square test criterion. Multivariate analysis of the impact of various factors on the development of SP was performed using logistic regression. The individual factors, and various combinations of cut-off values of the examined factors were combined using “OR” and “AND” statistics (criteria for presumed development of SP). The risk of SP development at different values of the examined variables, and “OR” and “AND” combinations, were expressed using the Odds Ratio (plus 95% confidence interval). Statistical significance was set at alpha=5%.</p></span><span id="sec0015" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0075">Results</span><p id="par0025" class="elsevierStylePara elsevierViewall">Men were significantly more affected than women in the study population, while the elderly were more affected in the female cohort. Development of SP occurred in 450 (5.35%) of the total of 8401 monitored days. A total of 54 clusters were identified, which resulted in 105 cases of SP (23.3%). Outside the clusters, we recorded 345 cases of SP (76.7%).</p><p id="par0030" class="elsevierStylePara elsevierViewall">In cases of SP, statistically significantly increases in the absolute values of changes in air pressure were recorded between the date of onset of SP and the day preceding the day of SP occurrence (Wilcoxon test: <span class="elsevierStyleItalic">P</span>-value=.0360). Using multivariate analysis (logistic regression), this factor was designated as the only statistically significant air pressure factor influencing development of SP. Air pressure changes of more than ±6.1<span class="elsevierStyleHsp" style=""></span>hPa increased risk for SP by 1.41 times (Chi-square test: <span class="elsevierStyleItalic">P</span>-value=.0017; 95% confidence interval of the risk: 1.14–1.76) (statistically the strongest cut-off).</p><p id="par0035" class="elsevierStylePara elsevierViewall">Similar statistically significant differences were found in air temperature on the day of occurrence of SP compared to the days without SP (Wilcoxon test: <span class="elsevierStyleItalic">P</span>-value=.0002). When the absolute value of the air temperature changed by more than ±0.9<span class="elsevierStyleHsp" style=""></span>°C, the risk of SP was 1.55 times higher (Chi-square test: <span class="elsevierStyleItalic">P</span>-value=.0002; 95% confidence interval of risk: 1.23–1.94) (statistically the strongest cut-off).</p><p id="par0040" class="elsevierStylePara elsevierViewall">We found statistically significant differences in wind speed on the day of development of SP, where the wind speed was higher in the SP group (Wilcoxon test: <span class="elsevierStyleItalic">P</span>-value=.0163). However, some of the wind speed changes were less clear. After further statistical analysis, we concluded that the difference between the minimum and maximum value of the wind speed over the 5 days prior to development of SP was significantly lower in the SP group (Wilcoxon test: <span class="elsevierStyleItalic">P</span>-value=.0438). Multivariate analysis (logistic regression) identified the difference between the minimum and maximum wind speed as the most statistically significant factor. When the wind speed differed by less than 13<span class="elsevierStyleHsp" style=""></span>m/s over the 5 days prior to onset of SP, the risk of SP was 2.16 times higher (Chi-square test: <span class="elsevierStyleItalic">P</span>-value=.0004; 95% confidence interval of the risk: 1.40–3.34) (statistically the strongest cut-off). (<a class="elsevierStyleCrossRef" href="#fig0005">Fig. 1</a>).</p><elsevierMultimedia ident="fig0005"></elsevierMultimedia><p id="par0045" class="elsevierStylePara elsevierViewall">We also examined different combinations of the factors studied (wind temperature, pressure, speed) and their possible cut-offs at the development of SP. If the difference between temperatures was greater than ±0.9<span class="elsevierStyleHsp" style=""></span>°C or that of wind speed over the 5 days prior to onset of SP less than 13<span class="elsevierStyleHsp" style=""></span>m/s (the “OR” combination), the risk of SP was 3.24 times higher (Chi-square test: <span class="elsevierStyleItalic">P</span>-value=.0143; 95% confidence interval of the risk: 1.20–8.74). This condition was met in 99.11% of all SP studied. Other variants of the “OR” combinations have not yielded similarly good results. When the pressure difference was greater than ±6.1<span class="elsevierStyleHsp" style=""></span>hPa and the temperature difference greater than ±0.9<span class="elsevierStyleHsp" style=""></span>°C or the difference in wind speed over the 5 days prior to onset of SP was less than 10.7<span class="elsevierStyleHsp" style=""></span>m/s (“AND” combination), the risk of SP was 2.04 times higher (Chi-square test: <span class="elsevierStyleItalic">P</span> value=<.0001; 95% confidence interval of the risk: 1.59–2.60). Other variants of the “AND” combinations have not yielded such good results. (<a class="elsevierStyleCrossRef" href="#fig0010">Fig. 2</a>)</p><elsevierMultimedia ident="fig0010"></elsevierMultimedia><p id="par0050" class="elsevierStylePara elsevierViewall">Storms had no effect on the development of SP. Similarly, there was no significant difference in the occurrence of SP between the individual months of the year or seasons.</p></span><span id="sec0020" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0080">Discussion</span><p id="par0055" class="elsevierStylePara elsevierViewall">Spontaneous pneumothorax develops from rupture of emphysematous bullae, subpleural blebs, or from other pleural anomalies. These ruptures may be caused, among other reasons, by an increase in the transpulmonary pressure under the influence of certain weather changes.<a class="elsevierStyleCrossRefs" href="#bib0095"><span class="elsevierStyleSup">1–5</span></a> In the last 2 decades, several studies addressing this phenomenon have been published, but their findings are inconclusive.<a class="elsevierStyleCrossRefs" href="#bib0095"><span class="elsevierStyleSup">1,2,6–12</span></a> These studies most often monitored the effects of changes in atmospheric pressure and air temperature, but also studied the effects of phenomena such as air humidity, sunshine duration, amount of precipitation, and storms among others.<a class="elsevierStyleCrossRefs" href="#bib0125"><span class="elsevierStyleSup">7,9–13</span></a> The values of these parameters are usually examined on the day of onset of SP and compared to the days preceding the onset of SP, or to the period between the days, or to days without SP.<a class="elsevierStyleCrossRefs" href="#bib0110"><span class="elsevierStyleSup">4,7,9,11,12</span></a></p><p id="par0060" class="elsevierStylePara elsevierViewall">A significant number of SP cases, according to the experience of some authors, are found in clusters, i.e. multiple cases of SP may develop in a short time. Therefore, they defined clusters of occurrence involving at least 2 cases of SP in an interval of 3 days. In their respective patient populations, Alifano reported 84% of SP in 76 clusters; Smit 73%, Bertolaccini 81%, and Özpolat 70.5% occurrence of SP cases in 188 clusters.<a class="elsevierStyleCrossRefs" href="#bib0095"><span class="elsevierStyleSup">1,3,14,15</span></a> Our occurrence of 23.3% of cases in 54 clusters is lower, but in our opinion, this was caused by a relatively small number of SP cases examined over a relatively long period of time (22 years).</p><p id="par0065" class="elsevierStylePara elsevierViewall">Zhang found significant differences in the average daily values of air pressure between days with and without SP, but not between the onset date of SP and the preceding day.<a class="elsevierStyleCrossRef" href="#bib0150"><span class="elsevierStyleSup">12</span></a> In contrast, Alifano found a difference in the atmospheric pressure between the day before the onset and the day of onset of SP; the occurrence date in this case was also designated as the first cluster day.<a class="elsevierStyleCrossRef" href="#bib0095"><span class="elsevierStyleSup">1</span></a> This is consistent with our results; we found significantly higher differences in the absolute values of changes in air pressure between the onset date of SP and the day prior to the day of onset of SP. Bense concluded that a decrease in atmospheric pressure by at least 10<span class="elsevierStyleHsp" style=""></span>hPa in 24<span class="elsevierStyleHsp" style=""></span>h is associated with a statistically significant increase in the number of cases of SP in the following 2 days.<a class="elsevierStyleCrossRef" href="#bib0120"><span class="elsevierStyleSup">6</span></a> The influence of a drop in air pressure on the development of SP was also reported by Haga, Özpolat and Schieman.<a class="elsevierStyleCrossRefs" href="#bib0100"><span class="elsevierStyleSup">2,3,5</span></a> In contrast, Diaz considers an increase in atmospheric pressure to be a risk factor for SP, finding that it increases the likelihood of SP 1.15-fold with each 1<span class="elsevierStyleHsp" style=""></span>hPa increase in atmospheric pressure.<a class="elsevierStyleCrossRef" href="#bib0135"><span class="elsevierStyleSup">9</span></a> In our patient group, changes in air pressure of more than ±6.1<span class="elsevierStyleHsp" style=""></span>hPa increased the risk of SP by 1.41-fold, i.e. both a marked increase and decrease in air pressure are associated with risk for development of SP. Morales, Bertolaccini and Scott accepted the effects of changes in air pressure on the development of SP.<a class="elsevierStyleCrossRefs" href="#bib0110"><span class="elsevierStyleSup">4,14,16</span></a> In contrast, Obuchi, Sakai, Chen and others found that changes in atmospheric pressure have no influence on the occurrence of SP.<a class="elsevierStyleCrossRefs" href="#bib0125"><span class="elsevierStyleSup">7,8,10,11,13,15,17</span></a></p><p id="par0070" class="elsevierStylePara elsevierViewall">Our results are in line with Zhang and Sakai, insofar as we found statistically significant differences in air temperature (both increase and decrease) on days of SP occurrence versus days without SP.<a class="elsevierStyleCrossRefs" href="#bib0145"><span class="elsevierStyleSup">11,12</span></a> However, we cannot confirm the conclusions of Obuchi and Smit, who both found an increase in air temperature to have a significant effect on SP 1 or 2 days before occurrence.<a class="elsevierStyleCrossRefs" href="#bib0155"><span class="elsevierStyleSup">13,15</span></a> Other authors, such as Celik, Alifano and others found no effect of changes in air temperature on development of SP.<a class="elsevierStyleCrossRefs" href="#bib0095"><span class="elsevierStyleSup">1,2,7,8</span></a></p><p id="par0075" class="elsevierStylePara elsevierViewall">Our results regarding the effects of wind speed on the development of SP are somewhat contradictory. On the one hand, we found significant differences in wind speed on the onset date of SP, where the wind speed was higher in the SP group, but on the other hand, the same SP group showed significantly lower minimum and maximum values of wind speed over the 5 days prior to onset of SP. This relationship was paradoxically identified by multivariate analysis as the most statistically significant factor of SP development. Of the foregoing authors, only Schieman reported significant conclusions regarding wind speed in his study: like us, he recorded significantly stronger wind speed on the days of SP compared to those without SP.<a class="elsevierStyleCrossRef" href="#bib0115"><span class="elsevierStyleSup">5</span></a> We cannot explain why temperature and wind speed changes influence development of SP; we merely present statistically significant results. We can only assume that it can be associated with pressure changes related to wind speed or temperature changes.</p><p id="par0080" class="elsevierStylePara elsevierViewall">Probably the most interesting results of our study, in view of the existing literature, were obtained by examination of the impact of the combination of parameters. Air temperature seems to be a decisive factor both in the “OR” and in the “AND” combinations. By combining “OR” changes in air temperature and wind speed, we managed to explain the occurrence of more than 99% of SPs studied (3.24-fold higher risk of SP). We believe that this is probably the most important finding of our study. However, even the results of our “AND” combination (2.04-fold higher risk of developing SP) analyses indicate that changes in the weather phenomena studied have a significant effect, and that this effect is magnified when the phenomena occur simultaneously. Of the foregoing authors, both Özpolat and Schieman conducted a similar analysis, and reached the same conclusion regarding the effects of pressure or air temperature; Schieman, however, found a greater difference in wind speed than that found in our study.<a class="elsevierStyleCrossRefs" href="#bib0105"><span class="elsevierStyleSup">3,5</span></a></p><p id="par0085" class="elsevierStylePara elsevierViewall">Unlike Alifano or Smit, for example, we found no correlation between the occurrence of storms or lightning and onset of SP.<a class="elsevierStyleCrossRefs" href="#bib0095"><span class="elsevierStyleSup">1,15</span></a> Similarly, we found no monthly or seasonal differences in onset of SP, a finding echoed by most authors.<a class="elsevierStyleCrossRefs" href="#bib0115"><span class="elsevierStyleSup">5,7,10,18</span></a></p></span><span id="sec0025" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0085">Conclusion</span><p id="par0090" class="elsevierStylePara elsevierViewall">Our findings show that certain weather phenomena, such as changes in atmospheric pressure, air temperature and wind speed, are undoubtedly involved in the development of SP. However, they would not seem to be the only factors causing rupture of blebs or emphysematous bullae. Other risk factors, such as sport activity, definitely play an important role. Our findings are unclear insofar as we could not find any factor, or combination of factors, that would show a clear separation of risk and non-risk days in relation to the development of SP. More detailed information in this area could be obtained from further studies with more SP cases over a shorter period of time.</p></span><span id="sec0030" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0090">Funding</span><p id="par0095" class="elsevierStylePara elsevierViewall">Supported by the <span class="elsevierStyleGrantSponsor" id="gs1">MZ IGA</span><span class="elsevierStyleGrantNumber" refid="gs1">NT14227</span>, <span class="elsevierStyleGrantNumber" refid="gs1">NS9644</span> and <span class="elsevierStyleGrantNumber" refid="gs1">NT14332-3</span> grants.</p></span><span id="sec0035" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0095">Authors’ Contribution</span><p id="par0100" class="elsevierStylePara elsevierViewall">Josef Vodička – study design, collection of data, data analysis/interpretation, writing of the manuscript. Šárka Vejvodová – study design, collection of data. David Šmíd – collection of data, data analysis/interpretation. Jakub Fichtl - collection of data, data analysis/interpretation. Vladimír Špidlen – collection of data. Stanislav Kormunda – data analysis/interpretation, writing of the manuscript. Jiří Hostýnek – study design, collection of data. Jiří Moláček – revision of the manuscript.</p></span><span id="sec0040" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0100">Conflict of Interests</span><p id="par0105" class="elsevierStylePara elsevierViewall">The authors declare they have no conflict of interest directly or indirectly related to the manuscript contents.</p></span></span>" "textoCompletoSecciones" => array:1 [ "secciones" => array:13 [ 0 => array:3 [ "identificador" => "xres631369" "titulo" => "Abstract" "secciones" => array:4 [ 0 => array:2 [ "identificador" => "abst0005" "titulo" => "Introduction" ] 1 => array:2 [ "identificador" => "abst0010" "titulo" => "Methods" ] 2 => array:2 [ "identificador" => "abst0015" "titulo" => "Results" ] 3 => array:2 [ "identificador" => "abst0020" "titulo" => "Conclusion" ] ] ] 1 => array:2 [ "identificador" => "xpalclavsec644198" "titulo" => "Keywords" ] 2 => array:3 [ "identificador" => "xres631368" "titulo" => "Resumen" "secciones" => array:4 [ 0 => array:2 [ "identificador" => "abst0025" "titulo" => "Introducción" ] 1 => array:2 [ "identificador" => "abst0030" "titulo" => "Métodos" ] 2 => array:2 [ "identificador" => "abst0035" "titulo" => "Resultados" ] 3 => array:2 [ "identificador" => "abst0040" "titulo" => "Conclusión" ] ] ] 3 => array:2 [ "identificador" => "xpalclavsec644197" "titulo" => "Palabras clave" ] 4 => array:2 [ "identificador" => "sec0005" "titulo" => "Introduction" ] 5 => array:2 [ "identificador" => "sec0010" "titulo" => "Materials and Methods" ] 6 => array:2 [ "identificador" => "sec0015" "titulo" => "Results" ] 7 => array:2 [ "identificador" => "sec0020" "titulo" => "Discussion" ] 8 => array:2 [ "identificador" => "sec0025" "titulo" => "Conclusion" ] 9 => array:2 [ "identificador" => "sec0030" "titulo" => "Funding" ] 10 => array:2 [ "identificador" => "sec0035" "titulo" => "Authors’ Contribution" ] 11 => array:2 [ "identificador" => "sec0040" "titulo" => "Conflict of Interests" ] 12 => array:1 [ "titulo" => "References" ] ] ] "pdfFichero" => "main.pdf" "tienePdf" => true "fechaRecibido" => "2015-02-08" "fechaAceptado" => "2015-07-06" "PalabrasClave" => array:2 [ "en" => array:1 [ 0 => array:4 [ "clase" => "keyword" "titulo" => "Keywords" "identificador" => "xpalclavsec644198" "palabras" => array:4 [ 0 => "Spontaneous pneumothorax" 1 => "Atmospheric pressure" 2 => "Air temperature" 3 => "Wind speed" ] ] ] "es" => array:1 [ 0 => array:4 [ "clase" => "keyword" "titulo" => "Palabras clave" "identificador" => "xpalclavsec644197" "palabras" => array:4 [ 0 => "Neumotórax espontáneo" 1 => "Presión atmosférica" 2 => "Temperatura ambiental" 3 => "Velocidad del viento" ] ] ] ] "tieneResumen" => true "resumen" => array:2 [ "en" => array:3 [ "titulo" => "Abstract" "resumen" => "<span id="abst0005" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0010">Introduction</span><p id="spar0005" class="elsevierStyleSimplePara elsevierViewall">The objective of this study was to assess the impact of weather phenomena on the occurrence of spontaneous pneumothorax (SP) in the Plzeň region (Czech Republic).</p></span> <span id="abst0010" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0015">Methods</span><p id="spar0010" class="elsevierStyleSimplePara elsevierViewall">A retrospective analysis of 450 cases of SP in 394 patients between 1991 and 2013. We observed changes in average daily values of atmospheric pressure, air temperature and daily maximum wind gust for each day of that period and their effect on the development of SP.</p></span> <span id="abst0015" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0020">Results</span><p id="spar0015" class="elsevierStyleSimplePara elsevierViewall">The risk of developing SP is 1.41 times higher (<span class="elsevierStyleItalic">P</span>=.0017) with air pressure changes of more than ±6.1<span class="elsevierStyleHsp" style=""></span>hPa. When the absolute value of the air temperature changes by more than ±0.9<span class="elsevierStyleHsp" style=""></span>°C, the risk of developing SP is 1.55 times higher (<span class="elsevierStyleItalic">P</span>=.0002). When the wind speed difference over the 5 days prior to onset of SP is less than 13<span class="elsevierStyleHsp" style=""></span>m/s, then the risk of SP is 2.16 times higher (<span class="elsevierStyleItalic">P</span>=.0004). If the pressure difference is greater than ±6.1<span class="elsevierStyleHsp" style=""></span>hPa and the temperature difference is greater than ±0.9<span class="elsevierStyleHsp" style=""></span>°C or the wind speed difference during the 5 days prior to onset of SP is less than 10.7<span class="elsevierStyleHsp" style=""></span>m/s, the risk of SP is 2.04 times higher (<span class="elsevierStyleItalic">P</span>≤.0001).</p></span> <span id="abst0020" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0025">Conclusion</span><p id="spar0020" class="elsevierStyleSimplePara elsevierViewall">Changes in atmospheric pressure, air temperature and wind speed are undoubtedly involved in the development of SP, but do not seem to be the only factors causing rupture of blebs or emphysematous bullae.</p></span>" "secciones" => array:4 [ 0 => array:2 [ "identificador" => "abst0005" "titulo" => "Introduction" ] 1 => array:2 [ "identificador" => "abst0010" "titulo" => "Methods" ] 2 => array:2 [ "identificador" => "abst0015" "titulo" => "Results" ] 3 => array:2 [ "identificador" => "abst0020" "titulo" => "Conclusion" ] ] ] "es" => array:3 [ "titulo" => "Resumen" "resumen" => "<span id="abst0025" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0035">Introducción</span><p id="spar0025" class="elsevierStyleSimplePara elsevierViewall">El objetivo de este estudio fue evaluar la influencia de los fenómenos meteorológicos en la aparición de neumotórax espontáneo (NE) en la región de Pilsen (República Checa).</p></span> <span id="abst0030" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0040">Métodos</span><p id="spar0030" class="elsevierStyleSimplePara elsevierViewall">Análisis retrospectivo de 450 casos de NE en 394 pacientes durante los años 1991–2013. Se analizaron los valores diarios medios de presión atmosférica, temperatura ambiental y la velocidad máxima diaria del viento y sus cambios cada día en ese período, en relación con la aparición de NE.</p></span> <span id="abst0035" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0045">Resultados</span><p id="spar0035" class="elsevierStyleSimplePara elsevierViewall">El riesgo de desarrollar NE aumentó 1,41 veces (<span class="elsevierStyleItalic">P</span>=0,0017) en el caso de cambios mayores de ±6,1<span class="elsevierStyleHsp" style=""></span>hPa en la presión atmosférica. Cuando el valor absoluto de los cambios de temperatura ambiental era mayor de ±0,9<span class="elsevierStyleHsp" style=""></span>°C, el riesgo de aparición de NE aumentó 1,55 veces (<span class="elsevierStyleItalic">P</span>=0,0002). Cuando la diferencia en los cambios en la velocidad del viento en los 5 días previos al inicio de NE era menor de 13<span class="elsevierStyleHsp" style=""></span>m/s, el riesgo de NE aumentaba 2,16 veces (<span class="elsevierStyleItalic">P</span>=0,0004). Si la diferencia de presión era mayor de ±6,1<span class="elsevierStyleHsp" style=""></span>hPa y la diferencia de temperatura mayor de ±0,9<span class="elsevierStyleHsp" style=""></span>°C o la diferencia en la velocidad del viento en los 5 días previos al inicio de NE era inferior a 10,7<span class="elsevierStyleHsp" style=""></span>m/s, el riesgo de NE aumentaba 2,04 veces (<span class="elsevierStyleItalic">P</span>≤0,0001).</p></span> <span id="abst0040" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0050">Conclusión</span><p id="spar0040" class="elsevierStyleSimplePara elsevierViewall">Los cambios en la presión atmosférica, la temperatura ambiental y la velocidad del viento están indudablemente involucrados en la aparición de NE. Sin embargo, no parecen ser los únicos factores causantes de la rotura de las vesículas o las ampollas enfisematosas.</p></span>" "secciones" => array:4 [ 0 => array:2 [ "identificador" => "abst0025" "titulo" => "Introducción" ] 1 => array:2 [ "identificador" => "abst0030" "titulo" => "Métodos" ] 2 => array:2 [ "identificador" => "abst0035" "titulo" => "Resultados" ] 3 => array:2 [ "identificador" => "abst0040" "titulo" => "Conclusión" ] ] ] ] "NotaPie" => array:1 [ 0 => array:2 [ "etiqueta" => "☆" "nota" => "<p class="elsevierStyleNotepara" id="npar0005">Please cite this article as: Vodička J, Vejvodová Š, Šmíd D, Fichtl J, Špidlen V, Kormunda S, et al. ¿Tienen los fenómenos meteorológicos alguna influencia en la aparición de neumotórax espontáneo? Arch Bronconeumol. 2016;52:239–243.</p>" ] ] "multimedia" => array:2 [ 0 => array:7 [ "identificador" => "fig0005" "etiqueta" => "Fig. 1" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr1.jpeg" "Alto" => 1686 "Ancho" => 2261 "Tamanyo" => 239320 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0045" class="elsevierStyleSimplePara elsevierViewall">Receiving Operating Curve (ROC) of the respective factors.</p>" ] ] 1 => array:7 [ "identificador" => "fig0010" "etiqueta" => "Fig. 2" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr2.jpeg" "Alto" => 1823 "Ancho" => 2515 "Tamanyo" => 176606 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0050" class="elsevierStyleSimplePara elsevierViewall">The risk of spontaneous pneumothorax by individual factors studied.</p>" ] ] ] "bibliografia" => array:2 [ "titulo" => "References" "seccion" => array:1 [ 0 => array:2 [ "identificador" => "bibs0005" "bibliografiaReferencia" => array:18 [ 0 => array:3 [ "identificador" => "bib0095" "etiqueta" => "1" "referencia" => array:1 [ 0 => array:2 [ "contribucion" => array:1 [ 0 => array:2 [ "titulo" => "Atmospheric pressure influences the risk of pneumothorax: beware of the storm!" 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Year/Month | Html | Total | |
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2024 November | 5 | 2 | 7 |
2024 October | 43 | 17 | 60 |
2024 September | 36 | 15 | 51 |
2024 August | 57 | 37 | 94 |
2024 July | 56 | 16 | 72 |
2024 June | 52 | 32 | 84 |
2024 May | 81 | 25 | 106 |
2024 April | 35 | 24 | 59 |
2024 March | 39 | 14 | 53 |
2024 February | 32 | 25 | 57 |
2023 March | 7 | 4 | 11 |
2023 February | 32 | 23 | 55 |
2023 January | 26 | 22 | 48 |
2022 December | 41 | 28 | 69 |
2022 November | 36 | 14 | 50 |
2022 October | 24 | 39 | 63 |
2022 September | 33 | 24 | 57 |
2022 August | 39 | 33 | 72 |
2022 July | 33 | 40 | 73 |
2022 June | 43 | 42 | 85 |
2022 May | 53 | 35 | 88 |
2022 April | 92 | 34 | 126 |
2022 March | 77 | 37 | 114 |
2022 February | 96 | 31 | 127 |
2022 January | 88 | 38 | 126 |
2021 December | 56 | 35 | 91 |
2021 November | 67 | 44 | 111 |
2021 October | 53 | 41 | 94 |
2021 September | 31 | 44 | 75 |
2021 August | 23 | 29 | 52 |
2021 July | 31 | 29 | 60 |
2021 June | 50 | 50 | 100 |
2021 May | 46 | 38 | 84 |
2021 April | 111 | 116 | 227 |
2021 March | 64 | 23 | 87 |
2021 February | 38 | 31 | 69 |
2021 January | 38 | 20 | 58 |
2020 December | 44 | 29 | 73 |
2020 November | 34 | 17 | 51 |
2020 October | 49 | 20 | 69 |
2020 September | 47 | 16 | 63 |
2020 August | 46 | 20 | 66 |
2020 July | 73 | 27 | 100 |
2020 June | 30 | 8 | 38 |
2020 May | 47 | 12 | 59 |
2020 April | 57 | 26 | 83 |
2020 March | 45 | 12 | 57 |
2020 February | 48 | 19 | 67 |
2020 January | 50 | 18 | 68 |
2019 December | 47 | 19 | 66 |
2019 November | 33 | 22 | 55 |
2019 October | 19 | 12 | 31 |
2019 September | 20 | 9 | 29 |
2019 August | 28 | 11 | 39 |
2019 July | 33 | 24 | 57 |
2019 June | 31 | 20 | 51 |
2019 May | 46 | 19 | 65 |
2019 April | 34 | 36 | 70 |
2019 March | 41 | 24 | 65 |
2019 February | 42 | 19 | 61 |
2019 January | 40 | 21 | 61 |
2018 December | 43 | 21 | 64 |
2018 November | 70 | 32 | 102 |
2018 October | 72 | 21 | 93 |
2018 September | 24 | 8 | 32 |
2018 July | 2 | 0 | 2 |
2018 May | 16 | 0 | 16 |
2018 April | 23 | 4 | 27 |
2018 March | 16 | 4 | 20 |
2018 February | 22 | 12 | 34 |
2018 January | 13 | 8 | 21 |
2017 December | 27 | 7 | 34 |
2017 November | 23 | 5 | 28 |
2017 October | 24 | 4 | 28 |
2017 September | 26 | 15 | 41 |
2017 August | 19 | 13 | 32 |
2017 July | 23 | 8 | 31 |
2017 June | 48 | 14 | 62 |
2017 May | 40 | 13 | 53 |
2017 April | 24 | 8 | 32 |
2017 March | 19 | 9 | 28 |
2017 February | 11 | 16 | 27 |
2017 January | 15 | 5 | 20 |
2016 December | 29 | 20 | 49 |
2016 November | 29 | 21 | 50 |
2016 October | 41 | 29 | 70 |
2016 September | 26 | 10 | 36 |
2016 August | 39 | 5 | 44 |