Journal of Applied Meteorology: Recent submissions
Now showing items 801-820 of 6019
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Electrical and Microphysical Measurements in Warm Cumulus Clouds Before and After Seeding
(American Meteorological Society, 1976)Electrical and microphysical measurements were made in warm maritime and inland cumulus clouds, before and after seeding, by repeated aircraft penetrations at a single level, a few hundred meters above cloud base. Such ... -
A Solar Aureole Radiometer for Atmospheric Aerosol Studies
(American Meteorological Society, 1976)A method of minimizing the effects of direct solar scatter in aureole measurements is described. Experimental results for ?clear? and polluted conditions are illustrated. The effects of large particles on the shape of the ... -
Comparison of Radiation Computations Using Observed and Estimated Precipitable Water
(American Meteorological Society, 1976)Hourly values of total solar radiation are computed by two methods at 11 stations in all regions of the United States for a two-year period. In the first method, precipitable water is computed from radiosonde observations ... -
Determination of the Cirrus Outflow Divergence as Seen by Satellite
(American Meteorological Society, 1976)Certain methods are tested to estimate the divergence of the outflow anvil of tropical cloud clusters. These methods are based on the change of digitized brightness values given by a sequence of satellite pictures. From ... -
Multimoment Doppler Display for Severe Storm Identification
(American Meteorological Society, 1976)A single-Doppler data display has been developed which allows simultaneous presentation of the principal moments of the Doppler spectrum while retaining ease of viewing and interpretation. Display severe storm signatures ... -
Change in the Transmissivity Parameter with Atmospheric Path Length
(American Meteorological Society, 1976)Calculations and measurements show that the transmissivity parameter t is an increasing function of the optical air mass m. An equation for estimating t for several model atmospheres is presented, and the direct beam flux ... -
Comments on “Discussion of the Elsasser Formulation for Infrared Fluxes”
(American Meteorological Society, 1976)Charlock and Herman (1976, hereafter CH) have criticized the formulation of the radiative flux equation of Zdunkowski et al. (ZBL), 1966. While Zdunkowski (Z) finds their paper very interesting, he does not agree with all ... -
Eigenvector Analysis for Prediction of Time Series
(American Meteorological Society, 1976)The theorem of singular value decomposition is used to represent a data matrix X as the product of a system with a response R to a forcing function F. Algebraically, R is the matrix of principal components and F the transpose ... -
Comments on “Simulation of Weatherlike Doppler Spectra and Signals”
(American Meteorological Society, 1976)tract -
A Pseudospectral Model for Dispersion of Atmospheric Pollutants
(American Meteorological Society, 1976)An Eulerian model, describing the dispersion of pollutants in gases and fluids, is developed. The model is based on numerical integration of the dispersion equation, including the effect of advection, diffusion, sinks and ... -
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Wind Sets from SMS Images: An Assessment of Quality for GATE
(American Meteorological Society, 1976)In this study we explore the accuracy, representativeness and reproducibility of tracer winds in the area of the 1974 GARP Atlantic Tropical Experiment (GATE). These winds were generated by tracking clouds in Synchronous ... -
Numerical Simulation of the Orographically Induced Precipitation Distribution for Use in Hydrologic Analysis
(American Meteorological Society, 1976)A fine-mesh mesoscale numerical model is used to simulate the orographic precipitation process for the purpose of improving estimates of the spatial distribution of precipitation in mountainous areas. Results from integrations ... -
A Note on “The Behavior of Large, Low-Surface-Tension Water Drops Falling at Terminal Velocity in Air”
(American Meteorological Society, 1976)A heuristic explanation of Ryan's (1976) observations of water drop breakup is given in terms of the Rayleigh-Taylor instability of two superposed fluids. The critical values for drop instability agree with the observations. ... -
Climatology of Wind Direction Fluctuations at Risø
(American Meteorological Society, 1976)Standard deviations of wind direction fluctuations at 76 m at Ris? for the first half year of 1975 have been analyzed as functions of wind speed and temperature lapse rate, either measured near the surface or near the level ... -
Tropical Cyclone Motion and Surrounding Parameter Relationships
(American Meteorological Society, 1976)Ten years of rawinsonde data for 30 stations in the western North Pacific have been composited relative to tropical cyclone center positions. This information is used to study tropical cyclone motion and surrounding parameter ... -
Temperature Gradients and Clear-Air Turbulence Probabilities
(American Meteorological Society, 1976)From the end of October 1973 to the beginning of January 1974, Continental Airlines operated one of its Boeing 747 aircraft with special instrumentation for the study of clear-air turbulence (CAT). The observations were ... -
Use of Compressed Air for Supercooled Fog Dispersal
(American Meteorological Society, 1976)Experiments have been performed under controlled and free environment conditions to determine the technical feasibility of using the cooling resulting from the adiabatic expansion of compressed air to initiate ice crystal ... -
Depolarization of Lidar Returns from Virga and Source Cloud
(American Meteorological Society, 1976)The observed depolarization of polarized lidar signals scattered from virga and a source cloud may be interpreted to show that the source cloud is largely glaciated, and the virga is composed of ice crystals not randomly ... -
A Comparison of Two Optical Methods for Measuring Line Averages of Thermal Exchanges Above Warm Water Surfaces
(American Meteorological Society, 1976)Line averages of the vertical transports of sensible and latent heats in the surface boundary layer are determined above a warm water surface by the use of two optical, line-of-sight, remote-sensing techniques. In one ...