981 resultados para cloud droplet number concentration
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The cytokinesis-block micronucleus (CBMN) assay is one of the standard cytogenetic tools employed to assess chromosomal damage subsequent to exposure to genotoxic/cytotoxic agents, and is widely applicable to plant, animal and human cells. In the present study, the CBMN assay was used to assess the baseline damage in binuclear human peripheral blood lymphocytes exposed to 25 µg/L p,p'-DDT for 1, 2, 24, and 48 h by measuring the frequency of micronuclei, nucleoplasmic bridges and nuclear buds. These new scoring criteria facilitated the detection of different types of clastogenic and aneugenic effects induced by this type of pollutant. With these criteria, CBMN can also be used to measure nucleoplasmic bridges which are considered to be consequences of chromosome rearrangements and nuclear buds which are biomarkers of altered gene amplification and gene dosage. The total number of micronuclei observed in binuclear human peripheral blood lymphocytes of the exposed samples (ranging from 32 to 47) was significantly greater (P < 0.05) than that detected in the unexposed (0 time) control sample, where the total number of micronuclei was 7. The number of nucleoplasmic bridges and nuclear buds obtained after 24 and 48 h was also significantly (P < 0.05) greater in the samples treated with p,p'-DDT than in the unexposed control samples. Thus, our results confirmed the usefulness of the new criteria applicable for the CBMN assay employed in measuring the DNA damage and its role of a sensitive cytogenetic biomarker.
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In this study, a neuro-fuzzy estimator was developed for the estimation of biomass concentration of the microalgae Synechococcus nidulans from initial batch concentrations, aiming to predict daily productivity. Nine replica experiments were performed. The growth was monitored daily through the culture medium optic density and kept constant up to the end of the exponential phase. The network training followed a full 3³ factorial design, in which the factors were the number of days in the entry vector (3,5 and 7 days), number of clusters (10, 30 and 50 clusters) and internal weight softening parameter (Sigma) (0.30, 0.45 and 0.60). These factors were confronted with the sum of the quadratic error in the validations. The validations had 24 (A) and 18 (B) days of culture growth. The validations demonstrated that in long-term experiments (Validation A) the use of a few clusters and high Sigma is necessary. However, in short-term experiments (Validation B), Sigma did not influence the result. The optimum point occurred within 3 days in the entry vector, 10 clusters and 0.60 Sigma and the mean determination coefficient was 0.95. The neuro-fuzzy estimator proved a credible alternative to predict the microalgae growth.
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Digitalization and technology megatrends such as Cloud services have provided SMEs with a suitable atmosphere and conditions to internationalize and seek for further business growth. There is a limited amount of research on Cloud services from the business perspective and the limitations and challenges SMEs encounter when pursuing international business growth. Thus, the main research question of this study was how Cloud services may enable Finnish SMEs to overcome international growth challenges. The research question was further divided into three sub-questions dealing with matters related to features and characteristics of Cloud services, limitations and challenges Finnish SMEs experience when pursuing international growth of business, and benefits and advantages of utilizing Cloud services to mitigate and suppress international growth challenges. First, the theoretical framework of this study was constructed based on the existing literature on Cloud services, SMEs, and international growth challenges. After this, qualitative research approach and methodology were applied for this study. The data was collected through six semi-structured expert interviews in person with representatives of IBM, Exidio, Big Data Solutions, and Comptel. After analyzing the collected data by applying thematic analysis method, the results were compared with the existing theory and the original framework was modified and complemented accordingly. Resource scarcity, customer base expansion and retention, and lack of courage to try new things and take risks turned out to be major international growth challenges of Finnish SMEs. Due to a number of benefits and advantages of utilizing Cloud services including service automation, consumption-based pricing model, lack of capital expenditures (capex) and huge upfront investments, lightened organization structure, cost savings, speed, accessibility, scalability, agility, geographical expansion potential, global reaching and covering, credibility, partners, enhanced CRM, freedom, and flexibility, it can be concluded that Cloud services can help directly and indirectly Finnish SMEs to mitigate and overcome international growth challenges and enable further business growth.
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As reactive extraction grown more and more popular in a variety of technological applications, optimizing its performance becomes more and more important. The process of complex formation is affected by a great number of both physical and chemical properties of all the components involved, and sometimes their interference with one another makes improving the effectiveness of such processes very difficult. In this Master’s Theses, the processes of complex formation between the aqueous phase - represented by copper sulfate water solution, and organic phase – represented by Acorga M5640 solvent extractor, were studied in order to establish the effect these components have on reactive extraction performance and to determine which step is bottlenecking the process the most.
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During the expansion of steam in turbine, the steam crosses the saturation line and hence subsequent turbine stages run under wet condition. The stages under wet condition run with low efficiency as compared to stages running with supersaturated steam and the life of the last stage cascade is reduced due to erosion. After the steam crosses the saturation line it does not condense immediately but instead it becomes supersaturated which is a meta-stable state and reversion of equilibrium results in the formation of large number of small droplets in the range of 0.05 - 1 μm. Although these droplets are small enough to follow the stream lines of vapor however some of the fog droplets are deposited on the blade surface. After deposition they coagulate into films and rivulets which are then drawn towards the trailing edge of the blade due to viscous drag of the steam. These large droplets in the range of radius 100 μm are accelerated by steam until they impact on the next blade row causing erosion. The two phenomenon responsible for deposition are inertial impaction and turbulent-diffusion. This work shall discuss the deposition mechanism in steam turbine in detail and numerically model and validate with practical data.
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En el presente estudio se analizan los efectos de los fotoperiodos ambientales de otoño e invierno y los fotoperiodos experimentales de 24, 12 y 0 horas de luz artificial sobre la calidad del semen de machos reproductores porcinos de raza Landrace. El estudio se realizó sobre 30 machos postpuberales de 8 meses de edad y testados con el fin de comprobar la homogeneidad. Los machos fueron distribuidos aleatóriamente en los 3 grupos de luz artificial durante 3 meses. El tratamiento de 12 horas de luz artificial fue considerado como grupo control. Previamente al inicio de cada tratamiento, se sometió a cada grupo de machos al fotoperiodo ambiental correspondiente a la época del año; así, se caracterizó también la calidad seminal en otoño e invierno, manteniendo la temperatura constante. La nave experimental que acogió a los machos tiene una superficie de 100 m2 y una altura de 3,5 m. Un pasillo central divide la nave en dos hileras de 5 y 6 celdas respectivamente. En una de las celdas pequeñas se instaló el maniquí y fue utilizada para las extracciones de semen. La iluminación artificial se consiguió con la instalación de 6 lámparas fluorescentes en el techo del pasillo central que proporcionaron una luz homogénea superior a 200 lux. Así mismo, la nave se mantuvo en todo momento a 21±1ºC y la humedad relativa osciló entre el 60-75%. A todos los verracos se les proporcionó una dieta nutritiva y equilibrada y se les sometió a un regimen de extracciones de semen de 2 veces por semana, habiendo sido previamente entrenados en la monta del maniquí. Les muestras de semen fueron recogidas según la técnica de la mano enguantada (Martín, 1982; Daza, 1992) y se analizaron los siguientes parámetros: el volumen y el pH seminales, la concentración, la vitalidad y la motilidad espermáticas, la resistencia acrosómica de los espermatozoides, la morfología espermàtica a partir de la frecuencia de los espermatozoides maduros, inmaduros y aberrantes, la producción testicular y el número de dosis seminales. Se analizó, además, bioquímicamente el plasma seminal al principio y al final de cada tratamiento experimental de luz artificial a partir de la concentración de proteína total, de la identificación de residuos fosforilados de proteína y del contenido de azúcares. También se determinaron los índices de fertilidad y prolificidad. El volumen y el pH de los eyaculados se utilizaron como marcadores del estado funcional de las glándulas sexuales accesorias; la concentración espermàtica como un indicador de la actividad testicular (Pinart y col., 1999). La vitalidad y la motilidad espermáticas fueron estimadores del grado de diferenciación del espermatozoide tanto a nivel testicular como epididimario; la resistencia acrosómica fue utilizada para valorar el nivel de diferenciación de la membrana acrosómica durante la espermiogénesis y/o maduración epididimària (Briz i col., 1996; Pinart i col., 1999). Referente a la morfología espermática, los espermatozoides inmaduros fueron marcadores de anomalías en la maduración de éstos a lo largo del conducto epididimario y los espermatozoides aberrantes se utilizaron como marcadores de una diferenciación defectuosa a nivel de testículo (anomalías primarias) y a nivel de conducto epididimario (anomalías secundarias) (Briz i col., 1996). La concentración de proteína total se utilizó para valorar la integridad funcional de las membranas del espermatozoide y la actividad de las glándulas sexuales accesorias. La identificación de proteínas con residuos de tirosina fosforilados fue un estimador de la viabilidad celular y la actividad de las glándulas sexuales, y el contenido de azúcares como un indicador de la producción de las vesículas seminales. La determinación del volumen y el pH de los eyaculados se realizó en las instalaciones de la granja a partir de semen fresco el mismo día de la extracción. El resto de parámetros se analizaron en el laboratorio durante las 48 horas posteriores a la extracción a partir de semen diluido en BTS (diluyente de Bestville) (Daza, 1992) y transportado y conservado a 15ºC. Las muestras fueron previamente filtradas con el fin de eliminar la tapioca. El estudio estadístico de los resultados obtenidos se realizó a partir del análisis de la varianza (ANOVA) con un nivel de significación de =0,05. En cuanto al estudio comparativo de los fotoperiodos ambientales estacionales se ha observado un incremento significativo del pH del eyaculado en los machos expuestos a otoño (P0,0001), mientras que el volumen seminal se mantiene en valores similares en ambos tratamientos (P=0,1650). La concentración espermàtica, la producción espermàtica y el número de dosis seminales que se pueden preparar a partir de un eyaculado se duplica en los verracos sometidos al fotoperiodo de primavera (P0,0001). La vitalidad y la motilidad espermáticas no experimentan cambios significativos entre tratamientos (P=0,3440 y P=0,9220, respectivamente). La resistencia osmótica de los acrosomas desciende únicamente en los machos expuestos a condiciones estacionales de otoño (P0,0001). En referencia a la morfología espermàtica aunque no se observan diferencias entre primavera y otoño (P0,05), sí se detecta un incremento de los porcentajes de espermatozoides inmaduros y aberrantes en ambos fotoperiodos estacionales, y en especial en los machos expuestos a condiciones fotoperiódicas de otoño. Según los resultados obtenidos en este estudio la calidad seminal de los verracos es inferior en el fotoperiodo de otoño debido a un descenso de la concentración y la producción espermáticas, un aumento del pH seminal, una disminución de la resistencia de la membrana acrosómica y a un incremento en la frecuencia de espermatozoides inmaduros y aberrantes. Parece ser, pues, que en el otoño tiene lugar la disminución de la producción testicular, cambios en la actividad de las glándulas sexuales accesorias y disfunciones en el proceso de diferenciación testicular y epididimària de los espermatozoides y especialmente del acrosoma. En relación a los resultados obtenidos en el estudio de los diferentes fotoperiodos artificiales se observa que la iluminación continua provoca un aumento significativo del volumen del eyaculado en el primer y segundo mes de tratamiento (P0,0001), disminuyendo en el tercer mes. La oscuridad absoluta no modifica este parámetro (P0,05). En cuanto al pH seminal la iluminación continua provoca un incremento progresivo del valor del pH a lo largo del periodo experimental (P0,0001), mientras que la oscuridad absoluta tiene un efecto más irregular. La exposición de los machos a iluminación continua y a oscuridad absoluta se manifiesta en un descenso de la concentración y la producción espermáticas que se mantiene hasta el segundo mes de tratamiento (P0,0001), observándose un incremento en el tercer mes de exposición de los machos a oscuridad absoluta (P=0,1010). De todas maneras, este descenso es mas severo en los machos sometidos a iluminación continua ya que no presentan recuperación. La vitalidad y la motilidad espermáticas no se ven alteradas por la iluminación continua y la oscuridad absoluta, ni tampoco el contenido de los azúcares mayoritarios del plasma seminal (P0,005). La glucosa aparece como un azúcar minoritario y sí que presenta concentraciones inferiores en los tratamientos experimentales de luz continua y de oscuridad absoluta (P0,0001 y P=0,0002, respectivamente). La resistencia osmótica de los acrosomas desciende en ambos tratamientos artificiales extremos de luz continua y oscuridad total (P0,0001), aunque en los machos expuestos a iluminación continua se produce una recuperación a partir del segundo mes de tratamiento (P=0,4930). Dado que tampoco se han observado diferencias significativas en las concentraciones de proteína total (P0,05), es probable que las anomalías de la membrana acrosómica se originen durante el proceso de espermiogénesis y/o maduración epididimària. La exposición de los verracos a oscuridad absoluta no altera la morfología espermàtica de los eyaculados, aunque se observa un aumento de la frecuencia de espermatozoides con anomalías en la forma de la cola en el primer mes (P0,0001), y un aumento de la frecuencia de espermatozoides inmaduros con gota distal y de espermatozoides con anomalías en el número de colas en el tercer mes de experimentación (P=0,0030 y P0,0001). La luz continua, sin embargo, provoca un incremento de la frecuencia de espermatozoides inmaduros con gota distal (P0,0001) y de espermatozoides con anomalías en la forma de la cola (P=0,0040) ya en el primer mes. El fotoperiodo provoca un descenso de la fertilidad de los machos expuestos a oscuridad absoluta en el tercer mes de tratamiento (P0,0001) y un incremento de ésta en los machos sometidos a iluminación continua (P=0,0005). La prolificidad no se ve modificada por ambas condiciones extremas de luz artificial (P0,05). Así pues, los resultados obtenidos demuestran que el fotoperiodo afecta la actividad testicular, provoca alteraciones en la actividad de las glándulas sexuales accesorias, altera el proceso de expulsión de la gota citoplasmática y provoca anomalías en el proceso de diferenciación de la cola tanto a nivel testicular como epididimario, siendo los verracos expuestos a luz continua más sensibles a estos parámetros que los verracos sometidos a oscuridad absoluta. El fotoperiodo, sin embargo, no altera de forma esencial la integridad de las membranas del espermatozoide ni la capacidad fecundante de éste.
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Avian communities in cloud forests have high levels of endemism and are at major risk given the accelerated rate of habitat fragmentation. Nevertheless, the response of these communities to changes in fragment size remains poorly understood. We evaluated species richness, bird community density, community composition, and dominance as indicators of the response to fragment size in a fragmented cloud forest landscape in central Veracruz, Mexico. Medium-sized fragments had statistically higher than expected species richness and more even communities, which may be a reflection of the intermediate disturbance hypothesis, in which medium-sized fragments are exploited by both forest and disturbance-associated species. Bird density also reached higher values in medium-sized fragments, which may indicate a carrying capacity in this habitat. However, large cloud forest fragments had a distinct taxonomic and functional composition, attributable to an increased number of understory insectivore species and canopy frugivores. By comparison, omnivorous species associated with human-altered habitats were more abundant in smaller fragments. Hence, although medium-sized cloud forest fragments had higher species richness and high bird density, large forest tracts maintained a distinct avian community composition, particularly of insectivorous and frugivorous species. Furthermore, the underlying response to fragmentation can only be properly addressed when contrasting several community attributes, such as richness, density, composition, and species dominance. Therefore, cloud forest conservation should aim to preserve the remaining large forest fragments to maintain comprehensive avian communities and avoid local extinctions.
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Radiation schemes in general circulation models currently make a number of simplifications when accounting for clouds, one of the most important being the removal of horizontal inhomogeneity. A new scheme is presented that attempts to account for the neglected inhomogeneity by using two regions of cloud in each vertical level of the model as opposed to one. One of these regions is used to represent the optically thinner cloud in the level, and the other represents the optically thicker cloud. So, along with the clear-sky region, the scheme has three regions in each model level and is referred to as “Tripleclouds.” In addition, the scheme has the capability to represent arbitrary vertical overlap between the three regions in pairs of adjacent levels. This scheme is implemented in the Edwards–Slingo radiation code and tested on 250 h of data from 12 different days. The data are derived from cloud retrievals using radar, lidar, and a microwave radiometer at Chilbolton, southern United Kingdom. When the data are grouped into periods equivalent in size to general circulation model grid boxes, the shortwave plane-parallel albedo bias is found to be 8%, while the corresponding bias is found to be less than 1% using Tripleclouds. Similar results are found for the longwave biases. Tripleclouds is then compared to a more conventional method of accounting for inhomogeneity that multiplies optical depths by a constant scaling factor, and Tripleclouds is seen to improve on this method both in terms of top-of-atmosphere radiative flux biases and internal heating rates.
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Despite the importance of microphysical cloud processes on the climate system, some topics are under-explored. For example, few measurements of droplet charges in nonthunderstorm clouds exist. Balloon carried charge sensors can be used to provide new measurements. A charge sensor is described for use with meteorological balloons, which has been tested over a range of atmospheric temperatures from -60 to 20 degrees C, in cloudy and clear air. The rapid time response of the sensor (to >10 V s(-1)) permits charge densities from 100 fC m(-3) to 1 nC m(-3) to be determined, which is sufficient for it to act as a cloud edge charge detector at weakly charged horizontal cloud boundaries.
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Abstract Foggy air and clear air have appreciably different electrical conductivities. The conductivity gradient at horizontal droplet boundaries causes droplet charging, as a result of vertical current flow in the global atmospheric electrical circuit. The charging is poorly known, as both the current flow through atmospheric water droplet layers and the air conductivity are poorly characterised experimentally. Surface measurements during three days of continuous fog using new instrument techniques show that a shallow (of order 100 m deep) fog layer still permits the vertical conduction current to pass. Further, the conductivity in the fog is estimated to be approximately 20% lower than in clear air. Assuming a fog transition thickness of one metre, this implies a vertical conductivity gradient of order 10 fS m−2 at the boundary. The actual vertical conductivity gradient at a cloud boundary would probably be greater, due to the presence of larger droplets in clouds compared to fog, and cleaner, more conductive clear air aloft.
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We performed an ensemble of twelve five-year experiments using a coupled climate-carbon-cycle model with scenarios of prescribed atmospheric carbon dioxide concentration; CO2 was instantaneously doubled or quadrupled at the start of the experiments. Within these five years, climate feedback is not significantly influenced by the effects of climate change on the carbon system. However, rapid changes take place, within much less than a year, due to the physiological effect of CO2 on plant stomatal conductance, leading to adjustment in the shortwave cloud radiative effect over land, due to a reduction in low cloud cover. This causes a 10% enhancement to the radiative forcing due to CO2, which leads to an increase in the equilibrium warming of 0.4 and 0.7 K for doubling and quadrupling. The implications for calibration of energy-balance models are discussed.
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[1] Cloud cover is conventionally estimated from satellite images as the observed fraction of cloudy pixels. Active instruments such as radar and Lidar observe in narrow transects that sample only a small percentage of the area over which the cloud fraction is estimated. As a consequence, the fraction estimate has an associated sampling uncertainty, which usually remains unspecified. This paper extends a Bayesian method of cloud fraction estimation, which also provides an analytical estimate of the sampling error. This method is applied to test the sensitivity of this error to sampling characteristics, such as the number of observed transects and the variability of the underlying cloud field. The dependence of the uncertainty on these characteristics is investigated using synthetic data simulated to have properties closely resembling observations of the spaceborne Lidar NASA-LITE mission. Results suggest that the variance of the cloud fraction is greatest for medium cloud cover and least when conditions are mostly cloudy or clear. However, there is a bias in the estimation, which is greatest around 25% and 75% cloud cover. The sampling uncertainty is also affected by the mean lengths of clouds and of clear intervals; shorter lengths decrease uncertainty, primarily because there are more cloud observations in a transect of a given length. Uncertainty also falls with increasing number of transects. Therefore a sampling strategy aimed at minimizing the uncertainty in transect derived cloud fraction will have to take into account both the cloud and clear sky length distributions as well as the cloud fraction of the observed field. These conclusions have implications for the design of future satellite missions. This paper describes the first integrated methodology for the analytical assessment of sampling uncertainty in cloud fraction observations from forthcoming spaceborne radar and Lidar missions such as NASA's Calipso and CloudSat.
Observations of the depth of ice particle evaporation beneath frontal cloud to improve NWP modelling
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The evaporation (sublimation) of ice particles beneath frontal ice cloud can provide a significant source of diabatic cooling which can lead to enhanced slantwise descent below the frontal surface. The strength and vertical extent of the cooling play a role in determining the dynamic response of the atmosphere, and an adequate representation is required in numerical weather-prediction (NWP) models for accurate forecasts of frontal dynamics. In this paper, data from a vertically pointing 94 GHz radar are used to determine the characteristic depth-scale of ice particle sublimation beneath frontal ice cloud. A statistical comparison is made with equivalent data extracted from the NWP mesoscale model operational at the Met Office, defining the evaporation depth-scale as the distance for the ice water content to fall to 10% of its peak value in the cloud. The results show that the depth of the ice evaporation zone derived from observations is less than 1 km for 90% of the time. The model significantly overestimates the sublimation depth-scales by a factor of between two and three, and underestimates the local ice water content by a factor of between two and four. Consequently the results suggest the model significantly underestimates the strength of the evaporative cooling, with implications for the prediction of frontal dynamics. A number of reasons for the model discrepancy are suggested. A comparison with radiosonde relative humidity data suggests part of the overestimation in evaporation depth may be due to a high RH bias in the dry slot beneath the frontal cloud, but other possible reasons include poor vertical resolution and deficiencies in the evaporation rate or ice particle fall-speed parametrizations.
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The role of convective processes in moistening the atmosphere during suppressed periods of the suppressed phase of a Madden-Julian oscillation is investigated in cloud-resolving model (CRM) simulations, and the impact of moistening on the subsequent evolution of convection is assessed as part of a Global Energy and Water Cycle Experiment Cloud System Study (GCSS) intercomparison project. The ability of single-column model (SCM) versions of a number of state-of-the-art climate and numerical weather prediction models to capture these convective processes is also evaluated. During the suppressed periods, the CRMs are found to simulate a maximum moistening around 3 km, which is associated with a predominance of shallow convection. All SCMs produce adequate amounts of shallow convection during the suppressed periods, comparable to that seen in CRMs, but the relatively drier SCMs have higher precipitation rates than the relatively wetter SCMs and CRMs. The relatively drier SCMs dry, rather than moisten, the lower troposphere below the melting level. During the transition periods, convective processes act to moisten the atmosphere above the level at which mean advection changes from moistening to drying, despite an overall drying effect for the column. The SCMs capture some essence of this moistening at upper levels. A gradual transition from shallow to deep convection is simulated by the CRMs and the wetter SCMs during the transition periods, but the onset of deep convection is delayed in the drier SCMs. This results in lower precipitation rates for these SCMs during the active periods, although much better agreement exists between the models at this time.
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A poor representation of cloud structure in a general circulation model (GCM) is widely recognised as a potential source of error in the radiation budget. Here, we develop a new way of representing both horizontal and vertical cloud structure in a radiation scheme. This combines the ‘Tripleclouds’ parametrization, which introduces inhomogeneity by using two cloudy regions in each layer as opposed to one, each with different water content values, with ‘exponential-random’ overlap, in which clouds in adjacent layers are not overlapped maximally, but according to a vertical decorrelation scale. This paper, Part I of two, aims to parametrize the two effects such that they can be used in a GCM. To achieve this, we first review a number of studies for a globally applicable value of fractional standard deviation of water content for use in Tripleclouds. We obtain a value of 0.75 ± 0.18 from a variety of different types of observations, with no apparent dependence on cloud type or gridbox size. Then, through a second short review, we create a parametrization of decorrelation scale for use in exponential-random overlap, which varies the scale linearly with latitude from 2.9 km at the Equator to 0.4 km at the poles. When applied to radar data, both components are found to have radiative impacts capable of offsetting biases caused by cloud misrepresentation. Part II of this paper implements Tripleclouds and exponential-random overlap into a radiation code and examines both their individual and combined impacts on the global radiation budget using re-analysis data.