Avaliação de Índices de Função Sistólica do Ventrículo Esquerdo em Canis lupus familiaris por Técnica de Ecocardiografia Doppler

A função cardíaca é fortemente condicionada pela mioarquitectura do coração, pelo que o estudo da relação morfologia-função ventricular nos mamíferos é de grande importância no diagnóstico e tratamento de patologias cardíacas. O cálculo dos volumes cardíacos durante todo o ciclo cardíaco tem uma importância fundamental para o estudo da função ventricular e para a definição dos padrões hemodinâmicos. Foi objectivo deste trabalho, o estudo de índices de função sistólica ventricular esquerda, em 25 cães (Cannis lupus familiaris), através da utilização de diferentes técnicas ecocardiográficas, como o Modo M, ecocardiografia bidimensional, Doppler tecidular e a ecocardiografia de contraste. Foi utilizado contraste ultrasonográfico, para melhorar a definição do endocárdio e possibilitar maior rigor no cálculo dos volumes ventriculares, e na avaliação da função ventricular sisto-diastólica global e regional. Os resultados apresentados foram sujeitos a tratamento estatístico com software Analyze-it. O Doppler tecidular mostrou ser um método robusto para avaliar a função sistólica. A ecocardiografia de contraste permitiu não só obter uma melhor definição endocárdica, como obter valores de fracção de ejecção com diferença estatisticamente significativa. Como os três métodos utilizados avaliam diferentes aspectos da função sistólica, função ventricular radial, circunferencial e longitudinal, não podem ser comparados directamente entre si.

Cloud-radar observations of insects in the UK convective boundary layer

Radar has been applied to the study of insect migration for almost 40 years, but most entomological radars operate at X-band (9.4 GHz, 3.2 cm wavelength), and can only detect individuals of relatively large species, such as migratory grasshoppers and noctuid moths, over all of their flight altitudes. Many insects (including economically important species) are much smaller than this, but development of the requisite higher power and/or higher frequency radar systems to detect these species is often prohibitively expensive. In this paper, attention is focussed upon the uses of some recently-deployed meteorological sensing devices to investigate insect migratory flight behaviour, and especially its interactions with boundary layer processes. Records were examined from the vertically-pointing 35 GHz ‘Copernicus’ and 94 GHz ‘Galileo’ cloud radars at Chilbolton (Hampshire, England) for 12 cloudless and convective occasions in summer 2003, and one of these occasions (13 July) is presented in detail. Insects were frequently found at heights above aerosol particles, which represent passive tracers, indicating active insect movement. It was found that insect flight above the convective boundary layer occurs most often during the morning. The maximum radar reflectivity (an indicator of aerial insect biomass) was found to be positively correlated with maximum screen temperature.

Radar studies of the vertical distribution of insects migrating over southern Britain: the influence of temperature inversions on nocturnal layer concentrations

Insects migrating over two sites in southern UK (Malvern in Worcestershire, and Harpenden in Hertfordshire) have been monitored continuously with nutating vertical-looking radars (VLRs) equipped with powerful control and analysis software. These observations make possible, for the first time, a systematic investigation of the vertical distribution of insect aerial density in the atmosphere, over temporal scales ranging from the short (instantaneous vertical profiles updated every 15 min) to the very long (profiles aggregated over whole seasons or even years). In the present paper, an outline is given of some general features of insect stratification as revealed by the radars, followed by a description of occasions during warm nights in the summer months when intense insect layers developed. Some of these nocturnal layers were due to the insects flying preferentially at the top of strong surface temperature inversions, and in other cases, layering was associated with higher-altitude temperature maxima, such as those due to subsidence inversions. The layers were formed from insects of a great variety of sizes, but peaks in the mass distributions pointed to a preponderance of medium-sized noctuid moths on certain occasions.

Comparison of balloon-carried atmospheric motion sensors with Doppler lidar turbulence measurements

Magnetic sensors have been added to a standard weather balloon radiosonde package to detect motion in turbulent air. These measure the terrestrial magnetic field and return data over the standard uhf radio telemetry. Variability in the magnetic sensor data is caused by motion of the instrument package. A series of radiosonde ascents carrying these sensors has been made near a Doppler lidar measuring atmospheric properties. Lidar-retrieved quantities include vertical velocity (w) profile and its standard deviation (w). w determined over 1 h is compared with the radiosonde motion variability at the same heights. Vertical motion in the radiosonde is found to be robustly increased when w>0.75 m s−1 and is linearly proportional to w. ©2009 American Institute of Physics