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Relation between temperature and mortality in thirteen Spanish cities

In this study we examined the shape of the association between temperature and mortality in 13 Spanish cities representing a wide range of climatic and socio demographic conditions. The temperature value linked with minimum mortality (MMT) and the slopes before and after the turning point (MMT) were calculated. Most cities showed a V-shaped temperature-mortality relationship. MMTs were generally higher in cities with warmer climates. Cold and heat effects also depended on climate: effects were greater in hotter cities but lesser in cities with higher variability. The effect of heat was greater than the effect of cold. The effect of cold and MMT was, in general, greater for cardio-respiratory mortality than for total mortality, while the effect of heat was, in general, greater among the elderly

Effect of Temperature on the Development and Survival of the Argentine Ant, Linepithema humile

The influence of temperature on the developmental times and survival of insects can largely determine their distribution. For invasive species, like the Argentine ant, Linepithema humile Mayr (Hymenoptera: Formicidae), these data are essential for predicting their potential range based on mechanistic models. In the case of this species, such data are too scarce and incomplete to make accurate predictions based on its physiological needs. This research provides comprehensive new data about brood survival and developmental times at a wide range of temperatures under laboratory conditions. Temperature affected both the complete brood development from egg to adult worker and each of the immature stages separately. The higher the temperature, the shorter the development times. Brood survival from egg to adult was low, with the maximum survival rate being only 16% at 26º C. Temperature also affected survival of each of the immature stages differently: eggs were negatively affected by high temperatures, while larvae were negatively affected by low temperatures, and the survival of pupae was apparently independent of environmental temperature. At 32º C no eggs survived, while at 18º C less than 2% of the eggs hatched into larva. The data from the present study are essential for developing prediction models about the distribution range of this tramp species based on its physiological needs in relation to temperature

Distinct Unfolding and Refolding Pathways of Ribonuclease A Revealed by Heating and Cooling Temperature Jumps

Heating and cooling temperature jumps (T-jumps) were performed using a newly developed technique to trigger unfolding and refolding of wild-type ribonuclease A and a tryptophan-containing variant (Y115W). From the linear Arrhenius plots of the microscopic folding and unfolding rate constants, activation enthalpy (ΔH#), and activation entropy (ΔS#) were determined to characterize the kinetic transition states (TS) for the unfolding and refolding reactions. The single TS of the wild-type protein was split into three for the Y115W variant. Two of these transition states, TS1 and TS2, characterize a slow kinetic phase, and one, TS3, a fast phase. Heating T-jumps induced protein unfolding via TS2 and TS3; cooling T-jumps induced refolding via TS1 and TS3. The observed speed of the fast phase increased at lower temperature, due to a strongly negative ΔH# of the folding-rate constant. The results are consistent with a path-dependent protein folding/unfolding mechanism. TS1 and TS2 are likely to reflect X-Pro114 isomerization in the folded and unfolded protein, respectively, and TS3 the local conformational change of the β-hairpin comprising Trp115. A very fast protein folding/unfolding phase appears to precede both processes. The path dependence of the observed kinetics is suggestive of a rugged energy protein folding funne

Desenvolupament d'un sistema de previsió de risc d'infecció per Stemphylium vesicarium. Avaluació, validació i implementació en parcel·les experimentals en camps comercials de perera

L'estemfiliosi de la perera és una malaltia fúngica ocasionada pel fong Deuteromicet Stemphylium vesicarium. Els símptomes característics d'aquesta malaltia són lesions necròtiques en fulles i fruits, provocant el depreciament econòmic d'aquests últims. Si les condicions climàtiques són favorables aquesta malaltia pot arribar a provocar la pèrdua total de la producció. La malaltia es localitza bàsicament en la conca mediterrània, sent les zones fructícoles de Girona a Catalunya i Emilia-Romagna a Itàlia els llocs on les pèrdues de producció són més grans. Actualment l'únic mètode de control és la cobertura permanent dels òrgans de la planta amb fungicides. Per obtenir aquesta protecció és necessari realitzar aplicacions preventives amb una cadència fixa, setmanal o quinzenal, de diferents fungicides en els arbres. Aquesta cadència d'aplicació comporta que al llarg del període vegetatiu de la perera es realitzin entre 20 i 25 aplicacions de fungicida, per cadències setmanals, o entre 10 i 13 aplicacions si la cadència és quinzenal. Aquest elevat nombre de tractaments comporta uns efectes toxicològics a nivell mediambiental i per a la salut humana, un augment del cost econòmic de la producció i en alguns casos afavorir l'aparició de resistències del patogen a determinats fungicides. Molts d' aquests tractaments es realitzen sense que les condicions ambientals siguin favorables a l'inici d'infeccions del fong, i són per tant innecessàries. Amb l'objectiu d'obtenir una eina per determinar el risc d'infeccions en funció de les condicions climàtiques i realitzar d'aquesta manera els tractaments amb fungicides només quan són necessaris, es va elaborar el Sistema pel Tractament Racionalitzat de l'Estemfiliosi de la Perera (STREP). El model consisteix en relacionar quantitativament amb la severitat de la malaltia els paràmetres climàtics de durada del període d'humectació i temperatura mitjana durant aquests períodes. En aquest treball s'ha determinat l'eficàcia en el control de la malaltia per diferents fungicides aplicats de manera preventiva amb una cadència fixa en diferents finques comercials i durant varis anys. S'ha constatat que no hi ha cap producte totalment eficaç en el control de la malaltia, sent l'eficàcia obtinguda mitjana. Aquesta eficàcia de control esta en funció del nivell de pressió de la malaltia, obtenint eficàcies inferiors quan el nivell en els testimonis no tractats és elevat. En assajos en condicions controlades s'ha determinat que els fungicides analitzats aplicats de manera curativa o postinfecciosa, quan ja s'han iniciat les infeccions, presenten una eficàcia més baixa que quan s'apliquen preventivament. El tiram és el producte amb una eficàcia més elevada en la major part de les condicions experimentals. S' ha analitzat durant 5 anys, 1992-1996, en diferents plantacions de perera de Girona, la dinàmica dels paràmetres ambientals de durada deis períodes amb humectació, la temperatura mitjana de l'aire, la temperatura mitjana durant els períodes d'humectació, la durada dels períodes amb humitat relativa superior al 90% i la pluviometria. S 'ha constatat que la humectació deguda a la rosada és la principal causa d'humectació i que és un procés lent i continu. Les durades més freqüents d'humectació han estat períodes inferiors a 12 hores i les temperatures més freqüents durant aquests períodes han estat entre 11 i 21°C. S'ha determinat també que existeixen períodes amb humitat relativa elevada però sense formació de pel·lícula d'aigua i s'ha observat que ocasionalment existeixen períodes breus d'interrupció de la humectació en que poden existir humanitats relatives elevades o baixes. La capacitat predictiva del model STREP ha estat avaluada mitjançant 42 assajos en condicions naturals i controlades, determinant que en més del 95 % dels casos avaluats les prediccions de malaltia s'han correspost amb les observades, i que només en dos casos el model ha infraestimat el nivell de risc d'infecció. Demostrant així que el model STREP és fiable en les seves prediccions. S'ha estudiat l'efecte de la humitat relativa durant els períodes interromputs d'humectació i les durades d'aquests períodes, en les infeccions produïdes pel fong. S'ha constatat que el model STREP hauria d'incorporar com a períodes separats els períodes d'humectació interromputs amb relatives elevades (>98%) s'haurien de considerar com a períodes continus. Per una altra banda s'ha comprovat que els períodes amb humitats relatives elevades sense formació d'humectació en condicions naturals no són suficients per provocar l'inici d'infeccions de S. Vesicarium. S'ha utilitzat el model STREP com a eina per guiar els tractaments fungicides en diferents parcel·les de finques comercials durant dos anys. D'aquests assajos es pot concloure que utilitzant valors de risc acumulat SA:0.4 com a llindar per a realitzar els tractaments es controla la malaltia amb una eficàcia semblant als tractaments setmanals, però amb una reducció del nombre d'aplicacions necessàries entre un 25 i un 50%. Utilitzar un llindar SA:0.6 en finques amb varietats sensibles i una pressió d'inòcul del patogen elevada presenta bons resultats però inferiors als obtinguts amb tractaments setmanals, no obstant l'estalvi de tractaments ha estat molt important (50-70%). De tots aquests resultats es conclou que el model STREP és adequat per ésser utilitzat en programes pilot a escala comercial en el control racional de l'estemfiliosi de la perera. En funció d'aquests resultats es considerarà la seva implementació en Estacions d'Avisos Fitosanitaris.

The response of tropospheric circulation to perturbations in lower-stratospheric temperature

A multiple regression analysis of the NCEP-NCAR reanalysis dataset shows a response to increased solar activity of a weakening and poleward shift of the subtropical jets. This signal is separable from other influences, such as those of El Nino-Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO), and is very similar to that seen in previous studies using global circulation models (GCMs) of the effects of an increase in solar spectral irradiance. The response to increased stratospheric (volcanic) aerosol is found in the data to be a weakening and equatorward shift of the jets. The GCM studies of the solar influence also showed an impact on tropospheric mean meridional circulation with a weakening and expansion of the tropical Hadley cells and a poleward shift of the Ferrel cells. To understand the mechanisms whereby the changes in solar irradiance affect tropospheric winds and circulation, experiments have been carried out with a simplified global circulation model. The results show that generic heating of the lower stratosphere tends to weaken the subtropical jets and the tropospheric mean meridional circulations. The positions of the jets, and the extent of the Hadley cells, respond to the distribution of the stratospheric heating, with low-latitude heating forcing them to move poleward, and high-latitude or latitudinally uniform heating forcing them equatorward. The patterns of response are similar to those that are found to be a result of the solar or volcanic influences, respectively, in the data analysis. This demonstrates that perturbations to the heat balance of the lower stratosphere, such as those brought about by solar or volcanic activity, can produce changes in the mean tropospheric circulation, even without any direct forcing below the tropopause.

The response of a uniform horizontal temperature gradient to heating

The response of a uniform horizontal temperature gradient to prescribed fixed heating is calculated in the context of an extended version of surface quasigeostrophic dynamics. It is found that for zero mean surface flow and weak cross-gradient structure the prescribed heating induces a mean temperature anomaly proportional to the spatial Hilbert transform of the heating. The interior potential vorticity generated by the heating enhances this surface response. The time-varying part is independent of the heating and satisfies the usual linearized surface quasigeostrophic dynamics. It is shown that the surface temperature tendency is a spatial Hilbert transform of the temperature anomaly itself. It then follows that the temperature anomaly is periodically modulated with a frequency proportional to the vertical wind shear. A strong local bound on wave energy is also found. Reanalysis diagnostics are presented that indicate consistency with key findings from this theory.

Precipitating convection in cold air: virtual potential temperature structure

Simulations of precipitating convection are used to illustrate the importance of the turbulent kinetic energy (TKE) budget in determining the virtual potential-temperature structure of the convecting atmosphere. Two sets of simulations are presented: in one the surface temperature was increased to simulate cold air flowing over a warmer surface and in the second a cooling profile, representing cold-air advection, was imposed. It is shown that the terms in the TKE budgets for both sets of simulations scale in the same way, but that the non-dimensional profiles are different. It is suggested that this is associated with the effects of sublimation of ice. It is shown that the magnitudes of the transport and precipitation terms in the virtual potential temperature budget are determined by the scaling of the TKE budget. Some implications of these results for parametrizations of moist convection are discussed. Copyright © 2007 Royal Meteorological Society

Composition and cure temperature: The influence on properties of final flexible PU cold cure foam parts

Foams are cellular structures, produced by gas bubbles formed during the polyurethane polymerization mixture. Flexible PU foams meet the following two criteria: have a limited resistance to an applied load, being both permeable to air and reversibly deformable. There are two main types of flexible foams, hot and cold cure foams differing in composition and processing temperatures. The hot cure foams are widely applied and represent the main composition of actual foams, while cold cure foams present several processing and property advantages, e.g, faster demoulding time, better humid aging properties and more versatility, as hardness variation with index changes are greater than with hot cure foams. The processing of cold cure foams also is attractive due to the low energy consumption (mould temperature from 30 degrees to 65 degrees C) comparatively to hot cure foams (mould temperature from 30 degrees to 250 degrees C). Another advantage is the high variety of soft materials for low temperature processing moulds. Cold cure foams are diphenylmethane diisocyanate (MDI) based while hot cure foams are toluene diisocyanate (TDI) based. This study is concerned with Viscoelastic flexible foams MDI based for medical applications. Differential Scanning Calorimetry (DSC) was used to characterize the cure kinetics and Dynamical Mechanical Analisys to collect mechanical data. The data obtained from these two experimental procedures were analyzed and associated to establish processing/properties/operation conditions relationships. These maps for the selection of optimized processing/properties/operation conditions are important to achieve better final part properties at lower costs and lead times.

Temperature and moist-stability effects on midlatitude orographic precipitation

Idealized, convection-resolving simulations of moist orographic flows are conducted to investigate the influence of temperature and moist stability on the drying ratio (DR), defined as the fraction of the impinging water mass removed as orographic precipitation. In flow past a long ridge, where most of the air rises over the barrier rather than detouring around it, DR decreases as the surface temperature (Ts) increases, even as the orographic cap cloud becomes statically unstable at higher Ts and develops embedded convection. This behaviour is explained by a few physical principles: (1) the Clausius–Clapeyron equation dictates that the normalized condensation rate decreases as the flow gets warmer, (2) the replacement of ice-phase precipitation growth with warm-rain processes decreases the efficiency by which condensate is converted to precipitation, thereby lowering precipitation efficiency, and (3) embedded convection acts more to vertically redistribute moisture than to enhance precipitation. Over an isolated mountain, the effects of (1) and (2) are counteracted by moisture deflection around the barrier, which is stronger in the colder, more stable flows.

Temperature trends derived from Stratospheric Sounding Unit radiances: the effect of increasing CO2 on the weighting function

Stratospheric Sounding Units (SSU) on the NOAA operational satellites have been the main source of near global temperature trend data above the lower stratosphere. They have been used extensively for comparison with model-derived trends. The SSU senses in the 15 micron band of CO2 and hence the weighting function is sensitive to changes in CO2 concentrations. The impact of this change in weighting function has been ignored in all recent trend analyses. We show that the apparent trends in global mean brightness temperature due to the change in weighting function vary from about -0.4 K/decade to 0.4 K/decade depending on the altitude sensed by the different SSU channels. For some channels, this apparent trend is of a similar size to the trend deduced from SSU data but ignoring the change in weighting function. In the mid-stratosphere, the revised trends are now significantly more negative and in better agreement with model-calculated trends.