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AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS


Click on the titles below to find US government-authored or -collected reports written by AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS

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A NEW RADAR FOR MEASURING WINDS, IN: AMERICAN METEOROLOGICAL SOCIETY BULLETIN, VOL57, NO 9, P1120-1125 SEP 1976
Authors:  R.B. CHADWICK; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.


PRELIMINARY RESULTS FROM THE GATE ACOUSTIC ECHO SOUNDER, IN: AMERICAN METEOROLOGICAL SOCIETY BULLETIN, VOL57, NO9, P1142-1147 SEP 1976
Authors:  AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.


TOTAL ATTENUATION MEASUREMENTS OF THE INTERTROPICAL CONVERGENCE ZONE BY SATELLITE ALTIMETER, IN: AMERICAN METEOROLOGICAL SOCIETY BULLETIN,VOL57, NO9, P1151-1152 SEP 1976
Authors:  C.L. PARSONS; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.


LIDAR MEASUREMENT OF STRATOSPHERIC DUST FROM ST AUGUSTINE VOLCANO IN: AMERICAN METEOROLOGICAL SOCIETY BULLETIN,VOL57, NO9, P1152- 1153 SEP 1976
Authors:  E.E. REMSBURG; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.


WAVE PATTERNS WITH AN ALBERTA HAILSTORM, IN: AMERICAN METEOROLOGICAL SOCIETY BULLETIN, VOL57, NO7, P780-787 JUL 1976
Authors:  C. Warner; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.


CALCULATION OF THE MAGNETIC HYPERFINE STRUCTURE OF SPECTRAL LINES WITH ALLOWANCE FOR THE FINITE SIZE OF THE ATOMIC NUCLEUS AND A STUDY OF THE DENSITY OF NUCLEAR MAGNETISM, OCT 1968
Authors:  V. V. Klingo; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.A formula is derived for the correction of the hyperfine structure constant owing to the fact that nuclear magnetism differs in nature from a point magnetic dipole. A possible form of the angular part of the magnetic density is examined for a specified radial part of the density of nuclear magnetism. These angular parts are phenomenologically defined and are able to make a contribution to the magnetic hyperfine structure constant. ...


IMPROVEMENT IN THE THEORETICAL DETERMINATION OF THE FINE STRUCTURE OF TERMS OF ATOMIC SPECIES OF BORON, CARBON, AND NITROGEN TYPE, OCT 1968
Authors:  A. P. Iutsis; R. S. Dagis; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The state of theoretical determination of the fine structure of light atoms is described. It is shown that the approximation of the two-electron states model must be used when the calculation of the fine structure is refined on the basis of a multiconfiguration approximation. The expression for the matrix elements of spin-dependent interactions is derived for the case of two unfilled shells and specialized for the case where one of ...


THE CONDITIONS OF OBSERVATION OF THE ZODIACAL LIGHT DURING A SOLAR ECLIPSE, JUN 1968
Authors:  V. G. FesenKov; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The expected luminance of the zodiacal light in the vicinity of the sun is evaluated by two different methods. It is shown that the corresponding polarization is rather great and is oriented toward the sun. It makes it possible to analyze the observed integral luminance of the sky background during the solar eclipse and to distinguish the zodiacal component. (Author)


ON THE DAY AIRGLOW, JUN 1968
Authors:  V. M. Morozov; I. S. Shklovskii; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Bedinger's well-known results regarding anomalous day-sky brightness at high altitudes are critically analyzed. On the basis of data obtained from observations of the sky brightness during total solar eclipses, as well as from other sources, the authors arrive at the conclusion that the aforementioned results of observations of the day-sky brightness were due to instrumental effects. (Author)


MANUAL ON SHORT-TERM PREDICTION OF IONOSPHERIC GEOMAGNETIC STORMS AND RADIO-PROPAGATION FORECASTING SERVICE, JUN 1968
Authors:  R. A. Zevakina; E. V. Lavrova; L. N. Lyakhova; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The main features of ionospheric-geomagnetic storms and their probable causes are reviewed. Disturbances in short-wave radio propagation during such storms are discussed. The principles of short-term prediction of ionospheric-geomagnetic storms are summarized and all kinds of Izmiran's forecasts are described. The application of these forecasts and current ionospheric data to calculation of usable radio propagation frequencies is explained. This Manualiis of interest to radio-communication operators as well as to geophysicists ...


CORRELATION DETERMINATIONS OF IONOSPHERIC DRIFT CHARACTERISTICS (REZULTATY OPREDELENIYA KHARAKTERISTIK IONOSFERNYKH DREIFOV KORRELYATSIONNYM METODOM). MAR 1968
Authors:  L. V. Grishkevich; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.It is shown that when experimental records of the amplitude fading of signals from the ionosphere are made by the method proposed in (1, 2), the results must be analyzed critically. The paper includes the description of an experiment that permits rather accurate determination of the characteristics of ionospheric drifts with the most general assumptions about the statistical nature of the ionosphere. (Author)


STUDIES OF THE CRYSTALLOGRAPHY OF AL2O3. MAR 1968
Authors:  AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The report covers studies of the crystallography of Al2O3. It contains a collection of articles translated from proceedings of the Institute of Crystallography Academy of Sciences of the U.S.S.R. (Author)


AUTOMATION OF A SAMPLE COLLECTOR FOR MEASURING THE LIQUID-WATER CONTENT OF FOG BY A METHOD DEVISED BY V. A. ZAITSEV. JAN 1968
Authors:  L. Z. Prokh; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.A trap device for taking samples of the liquid-water content of fog by a method originated by V. A. Zaitsev, used in the Ukrainian Hydrometeorological Scientific Research Institute, is described. (Author)


DISSIPATION OF STRATUS CLOUDS IN A TURBULENT ATMOSPHERE. JAN 1968
Authors:  Yu. V. Shulepov; M. V. Buikov; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The report contains the horizontal dissipation of a spatially homogeneous stratus cloud in a turbulent atmosphere, in which isothermy, an inversion in the supracloud layer, and downdrafts are present; the time required for total dissipation of the cloud is computed. (Author)


PRELIMINARY RESULTS OF A STUDY OF STEADY PRECIPITATION, BASED ON DATA OF A DENSE RAIN-GAGE NETWORK. JAN 1968
Authors:  M. P. Leonov; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.A method of investigation is presented and the properties of fields of steady precipitation are studied on the basis of the observations of a dense rain-gage network at the weather experiment range (WER) for six winter months of 1960-1962. The study deals with steady precipitation over the entire WER, the synoptic processes producing it, the optimum areas for averaging, the horizontal inhomogeneity of precipitation distribution on charts of semidiurnal and ...


VERTICAL THICKNESS AND STRUCTURE OF CLOUD COVER IN FRONTAL ZONES OVER THE UKRAINE DURING VARIOUS SYNOPTIC PROCESSES. JAN 1968
Authors:  I. N. Ponomarenko; A. M. Koshenko; T. N. Zabolotskaya; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Data on the vertical thickness and detail of the spatial structure of frontal cloud systems during various processes were obtained by analyzing 650 aircraft flights in atmospheric frontal zones. (Author)


THE THICKNESS AND RADIATION CHARACTERISTICS OF ST AND SC CLOUDS AS DETERMINED BY THE INTENSITY OF TOTAL RADIATION AT THE SURFACE OF THE EARTH. JAN 1968
Authors:  N. I. Goisa; T. V. Zheleznyakova; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The relation between the intensity of total radiation at the surface of the earth and the thickness of St and Sc clouds is investigated. Nomograms are plotted which permit the thickness of St and Sc layers to be determined with adequate accuracy. The nomograms are used to compute the coefficients of the total extinction of radiation by clouds and to derive the relationship of these coefficients with the altitude of ...


THE ZONAL DISTRIBUTION OF RADIATION REFLECTED FROM VARIOUS NATURAL SURFACES. JAN 1968
Authors:  N. I. Goisa; M. P. Fedorova; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Data are presented on the zonal distribution of radiation reflected by a field of barley in the ear formation stage, a field of barley in the stage of waxy maturity, barley stubble, Sudan grass, dry snow, snow covered with an ice crust, and stratus cloud cover. (Author)


ANNUAL VARIATION OF THE ELECTRIC POTENTIAL OF THE ATMOSPHERE AT A HEIGHT OF 6000 M AND THE CHARGE OF A COLUMN OF AIR IN THE 0-6666 M LAYER. JAN 1968
Authors:  I. M. Imyanitov; E. V. Chubarina; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The annual variation of space charges in the atmosphere in the 0-6000 m layer as well as the characteristics of the variation in the 0-500, 500-3500, and 3500-6000 m layers are investigated. It is shown that the range of the annual variation is very large and may account for a significant part of the annual unitary variation of the atmospheric electric field intensity. An inverse variation of the space charges ...


THE SOLAR WIND AND INTERPLANETARY MAGNETIC FIELDS. JAN 1968
Authors:  E. R. Mustel; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The report discusses recent findings concerning the causes and distribution of the interplanetary magnetic fields, and its relation to the solar wind.


MODIFICATION OF THE CLOUD DROPLET SPECTRUM BY THE INTRODUCTION OF PARTICLES THAT STRONGLY ABSORB SOLAR RADIATION. JAN 1968
Authors:  M. V. Buikov; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.This paper deals with a process of cloud droplet growth by repeated distillation in a mixture of cloud droplets and droplets containing a reagent that intensifies the absorption of short-wave radiation by these droplets. It is shown that a substantial growth of the cloud droplets occurs several tens of hours after modification, given favorable assumptions concerning the details of the process. The temperature increase inside the cloud due to the ...


FREQUENCY OF THICK CONVECTIVE CLOUDS OVER THE UKRAINE. JAN 1968
Authors:  G. F. Prikhotko; Z. M. Yashovskaya; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Data are given on the frequency of Cu cong and Cb of 5/10 or more sky cover over the Ukraine in summer. They are based on observations made six times daily at 103 weather stations. (Author)


THE STORED WATER OF STRATUS AND STRATOCUMULUS CLOUDS OVER THE UKRAINE IN THE COLD HALF OF THE YEAR. JAN 1968
Authors:  I. P. Polovina; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The stored water of St-Sc cloud masses is calculated on the basis of their lifetime, thickness, rate of transport, and average water content. The amount of precipitation that can be expected from these clouds is calculated on the assumption that the stored water will be completely precipitated. (Author)


SOME RESULTS OF TESTS ON THUNDERSTORM DETECTORS WITH A SMALL RANGE OF COVERAGE. JAN 1968
Authors:  K. A. Semenov; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Experimental data on thunderstorm discharges recorded within a radius of 10-20 km by instruments with a variety of designs are compared and analyzed in the present paper. (Author)


RADAR INVESTIGATION OF DYNAMIC PROCESSES IN THE ATMOSPHERE (RADIOLOKATSIONNOE ISSLEDOVANIE DINAMICHESKIKH PROTSESSOV V ATMOSFERE). JAN 1968
Authors:  A. G. Gorelik; Yu. V. Melnichuk; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The radar methods employed at present for meteorological purposes are based on the relation between the mean power of the reflected signal and the microstructure of the reflecting object. These methods have been quite fruitful for remote measurement of precipitation intensity as well as for solving problems related to the structure of precipitation etc. However, radar methods can be very useful not only for studying the microstructure of clouds and ...


SOME CHARACTERISTICS OF RADIATION IN FOG, 1968
Authors:  I. V. Koshelenko; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Data are presented on the radiation balance and total radiation in fog at ground level, at the top of the fog layer, and within the fog. The mean attenuation factors of long-wave and short-wave radiation in a fog layer are calculated on the basis of these data. (Author)


INTENSIFICATION OF PRECIPITATION OVER A WEATHER EXPERIMENT RANGE IN THE WINTER OF 1963-1964. DEC 1967
Authors:  M. P. Leonov; T. D. Nerobeeva; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The authors present their results from 17 experiments on the intensification of natural precipitation conducted over a weather experiment range in the winter of 1963-1964. The positive effect of seeding is confirmed by the data of a precipitation-gauge network and by radar observations. (Author)


SOME RESULTS OF RADAR INVESTIGATIONS OF THE VERTICAL STRUCTURE OF SHOWERS AND THUNDERSTORMS. DEC 1967
Authors:  E. M. Salman; K. S. Zhupakhin; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The general laws of the vertical structure of showers and thunderstorms, investigated by radar during the summer of 1962, are examined. (Author)


RADAR ANALYSIS OF CLOUD AND PRECIPITATION FIELDS. DEC 1967
Authors:  B. Sh. Divinskaya; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Some radar characteristics of cloud and precipitation fields and their connection with meteorological conditions and the synoptic situation are examined. The possibility of using radar observations to construct charts of the height of a cloud field and vertical cross sections through clouds is indicated. (Author)


THE EVOLUTION OF STRATUS CLOUDS IN THE SURFACE BOUNDARY LAYER OF THE ATMOSPHERE. DEC 1967
Authors:  Yu. V. Shulepov; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The evolution of stratus clouds, whose base is in the surface boundary layer of the atmosphere, is investigated. Formulas are derived that describe the displacement of the base of stratus clouds during a brief time interval (t less than or equal to 10 to 20 min). (Author)


THEORETICAL STUDY OF TRANSITIONS WITH DIFFERENT TYPES OF COUPLING USING THE NITROGEN ATOM AS AN EXAMPLE. DEC 1967
Authors:  Z. B. Rudzikas; Ya. I. Vizbaraite; A. P. Yutsis; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.A theoretical study is made of transitions of the type '2p(2) (3P) 3d(2S+1)Lf to 2p(2) (3P) 4fL (K) F' with the application of both LS0-coupling and J0L-coupling for the configuration 2p(2)4f.


PROPERTIES AND MEANS OF COMPUTING THE WIGNER COEFFICIENTS AND 6J COEFFICIENTS. DEC 1967
Authors:  A. A. Bandzaitis; K. P. Zhukauskas; A. Yu. Matulis; A. P. Yutsis; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The Wigner coefficient in the form given by Regge (Nuovo Cimento v10 p544 1958) and the 6j coefficient as given by Racah (Phys. Rev. v62 p438 1942) were set up for computer calculation.


TURBULENT FLOW OF MOMENTUM IN THE CASE OF UNSTABLE STRATIFICATION AND CONDITIONS CLOSE TO NEUTRAL EQUILIBRIUM (Turbulentnyi Potok Kolichestva Dvizheniya pri Neustoichivoi Stratifikatsii i Usloviyakh, Blizkikh k Bezrazlichnomu Ravnovesiyu), AUG 1967
Authors:  A. S. Gurvich; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The study of turbulent exchange in the surface layer of the atmosphere is of great interest in meteorology. Actually, the basic transfer of heat and moisture into the bottom layers of the atmosphere is a result of the turbulent exchange in the very lowest layers of air. Of practical interest is the study of the relation of the vertical profiles of wind velocity and temperature to turbulent exchange, since this ...


INTERACTION BETWEEN AN INSTRUMENT CAVITY AND A FLOW OF RAREFIED GAS. JUL 1967
Authors:  A. I. Ivanovskii; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The article concerns problems of the interaction between the cavity of a measuring instrument and a flow of rarefied gas. The admittance of a cylindrical tube is computed both for the instrument at rest and for an axial oncoming flow. The admittance and a number of other characteristics are calculated for a rigid tube with dissociation of the particles at the walls. Formulas are derived for the density of a ...


STUDY OF THE STRATIFICATION OF THE RADIATION BALANCE IN THE BOUNDARY LAYER OF THE ATMOSPHERE (K Issledovaniyu Stratifikatsii Radiatsionnogo Balansa v Pogranichnom Sloe Atmosfery), JUN 1967
Authors:  L. Z. Prokh; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Results are given of soundings carried out in the boundary layer of the atmosphere from the gondola of a balloon using a Yanishevskii pyrgeometer. (Author)


EXPERIMENTAL DATA ON THE LIQUID-WATER CONTENT OF FRONTAL CLOUDS OVER THE STEPPE PORTION OF THE UKRAINE (Vodnost Frontalnykh Oblakov nad Stepnoi Chastyu Ukrainy po Eksperimentalnym Dannym), JUN 1967
Authors:  I. N. Ponomarenko; T. N. Zabolotskaya; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The paper contains an analysis of about 1700 liquid-water content measurements made in 1961-1963 during experimental flights through the cloud systems of atmospheric fronts over the steppe portion of the Ukraine. We study data on the liquid-water content, mean temperature, and thickness of different types of frontal clouds as well as data on the properties of liquid-water content distribution as a function of meteorological parameters. An empirical graph is given ...


RECORDING SPECTROPHOTOMETER FOR GROUND AND BALLOON MEASUREMENTS OF THE BRIGHTNESS OF THE DAYTIME SKY, APR 1967
Authors:  N. M. Gopshtein; V. T. Kushpil; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.A detailed description is given of an instrument for measuring the brightness of the sky in the 0.58 to 1.87 microns region of the spectrum at heights up to 30 km. The calibration of the instrument and techniques for analysis of the measurements are also described. (Author)


GROUND MEASUREMENTS OF THE ANGULAR DISTRIBUTION AND SPECTRAL COMPOSITION OF DIFFUSE SKY RADIATION, APR 1967
Authors:  V. I. Kushpil; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The results of ground measurements of the sky brightness are cited for the spectral region 0.58 to 1.87 microns with various scattering angles and compared with data in the literature. (Author)


INTENSITY OF RADIATION FROM AUREOLE UNDER STANDARD CONDITIONS, APR 1967
Authors:  G. L. Shubova; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The intensity of radiation from aureole is estimated for standard conditions. The radiant intensity of radiation from sunward is studied as a function of the mass of the atmsophere and of the surface albedo. (Author)


CHARACTERISTICS OF FRONTAL CLOUDS SUSCEPTIBLE TO MODIFICATION OF NATURAL PRECIPITATION, APR 1967
Authors:  I. N. Ponomarenko; A. M. Koshenko; T. N. Zabolotskaya; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Data are given on the phase composition of clouds in frontal zones over the Ukraine and the characteristics of frontal cloud systems susceptible to artificial initiation of precipitation.


RELATION BETWEEN THE NUMBER OF THUNDERSTORMS AND THE AMOUNT OF SFERICS THAT PRODUCE A FIELD STRENGTH GREATER THAN A GIVEN LEVEL, APR 1967
Authors:  K. N. Barkalova; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The relation between the number of thunderstorms over the European continent and the amount of sferics that create a field strength greater than a given level is examined. The sferics were recorded in Voyeykovo and Odessa. (Author)


THUNDERSTORM ACTIVITY IN THE LENINGRAD REGION IN 1962. MAR 1967
Authors:  A. I. Astashenko; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Data are given on the distribution of thunderstorm activity in the Leningrad region. They are based on the observations of one radio direction-finding station near Leningrad.


THE FREQUENCY SPECTRUM OF SMALL-SCALE TEMPERATURE PULSATIONS. MAR 1967
Authors:  A. S. Gurvich; T. K. Kravchenko; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Experimental study of the high-frequency region of the spectrum of temperature and wind-speed pulsations is of interest for turbulence theory and for a number of practical problems associated, e. g., with the scattering of short sonic and ultrasonic waves in atmospheric turbulence. The present paper contains a brief description of the means of preparing miniature, quick-response temperature-pulsation sensors and some results of measurements of the high-frequency region of the temperature-pulsation ...


THERMAL PROPERTIES OF AMPHIBOLES AS A FUNCTION OF ALKALI CONTENT. FEB 1967
Authors:  A. F. Korzhinskii; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Some authors hold that amphiboles also contain zeolitic water that is given off in the 400-500C range, which creates a corresponding additional endothermal effect in the temperature diagram. Optical pyrometer studies of 24 specimens of amphiboles of various compositions did not show the presence of zeolitic water in even a single case. The result of these studies of different amphiboles (tremolite-actinolite series, nephrites, common hornblendes, pargasite, and arfvedsonite) was to ...


TWO-CONFIGURATION APPROXIMATION FOR ATOMIC SPECIES OF OXYGEN TYPE. FEB 1967
Authors:  A. B. Bolotin; I. I. Shironas; M. Yu. Braiman; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The parameters of analytic orbitals are evaluated for the configurations 1s(2) 2s2p(5) and 1s(2) 2p(6) of the atomic species O, F(+), Ne(++), Na(3+), and Mg(4+). The energy correction is found for the application of the two-configuration approximation 1s(2) 2s(2) 2p(4) - 1s(2) 2p(6). The theoretical results are compared with experimental data wherever possible. Values are determined for the total dipole strength and other transition-theory quantities, viz., the transition probability and ...


SOME RESULTS OF METEOR OBSERVATIONS AT TWO WAVELENGTHS. FEB 1967
Authors:  I. V. Bairachenko; V. I. Melnik; R. I. Moisya; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Results of radar tracking of meteors at frequencies of 31.26 MHz and 46.2 MHz are presented. The initial radii of the ionized meteor trails are determined by analysis of the general amplitude-time characteristics of the radar echo obtained on two wavelengths. (Author)


LIST OF TRANSLATIONS 1966: FOREIGN LITERATURE RELATING TO THE GEOPHYSICAL SCIENCES. FEB 1967
Authors:  AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The translations cited are complete, with figures, equations, and literature cited. The 'List of Translations' is divided alphabetically by language, and the items are numbered chronologically by date of translation under each language heading.


THE TESTING OF CABLES, WIRES, STRAPS, ETC. (ISPYTANIYA TROSSOV, PROVOLOK, LENT I PR.). NOV 1966
Authors:  AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.The strength of cables, wires, straps, tubing, etc. has been tested with a special instrument called the cable tester. The instrument is mounted on flat tunnel No. 1. It is set up as follows: The axis of the instrument, steel tube AB, rests on antifriction rollers R and R sub 1, which are similar to the rollers used in the Atwood machine. Two arms, D and D sub 1, are ...


COHERENT AMPLIFICATION OF RADIO EMISSION IN THE COSMIC MEDIUM (KOGERENTNOE USILENIE RADIOIZLUCHENIYA V KOSMICHESKOI SREDE), NOV 1966
Authors:  D. A. Varshalovich; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.In hydrogen atoms located in an oriented flux of nonpolarized ultraviolet radiation with a continuous spectrum in the 1216-912A region, an inversion occurs in the population of the hyperfine structure levels of the ground state 1 sub S 1/2. The foregoing provides grounds for believing that coherent amplification of radiation is a widespread phenomenon in the universe. (Author)


HYPERFINE STRUCTURE OF LIGHT ATOMIC SPECIES WITH S AND P VALENCE ELECTRONS. NOV 1966
Authors:  L. A. Auzin; I. M. Zak; V. V. Klingo; V. K. Shurgurov; AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
The full text of this report is not available and therefore is not for sale. This information is provided for reference purposes only.Expressions are found for the hyperfine structure of atomic species in configurations ss1, sp, pp1, p2, p3, and sp3. Values of the radial part and derivative of the wave function at the origin or coordinates are given for He and Li(+) in the configuration 1s2p, for H(-), He, Li(+), Be(2+), and B(3+) in the configuration 2p2, for Be, B(+), C(2+), and N(3+) in the configurations 1s2 2p2 and 1s2 2s2p, ...


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