SCIENTIFIC ABSTRACT SHATILIN, A.L. - SHATILOV, A.P.

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CIA-RDP86-00513R001548710018-6
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December 31, 1967
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SCIENTIFIC ABSTRACT
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GALEMIN, I.M.,-, SHATILIN, A.L. Drawing pig iron from the hearth before blowing out a blarnt furnace. Metallurg 8 no.124-6 Ja 163. (KIRA 1.61l) (Blast fi=an-ea-Me-intenance and repair) LI Z.17 1 7 1 ik I fV KONDRATIYEV. N.Ye., kandidat tekhnichaskikh nauk; ANDREYANOV, V.G., kandidat takhnichaskikh nauk, redaktor; SHATI re- daktor; BRkYNIKA, M.I., tekhnicheskiy reda or. [Calculation of wind movements and changes in reservoir banks) Raschety vetrovogo volnenlia i pereformirovaniia beregov vodo.- khraniliRhch. Pod red. V.G.Andraianova. Leningrad, Gidrometeoro- logicheakoe izd-vo, 1953. 106 p. [Microfilm] (MLRA 8:2) (Reservoirs) (Winds) (Waves) 6 KWMIN, P,P.,Imnd.geograf.naWk; SHATILIMk, M.K.,otv.red.; SOLOVEYCHIK, A.A., telchn.rod. [Effect of forests on the thawing of snow] Vliianie lesa na snagotaianie. Leningrad. Gidrometeor.izd-vo 1954. 67 p. (Leningrad. Gos&&arstvennyi gidrologicheskii institut. Trudy, no.42) (MIRA 12:1) (Thawing) (Forest influences) YITGENOV, Ilikolay Ivanovich; STWAZHINSKIY, V.A., redaktor; SHATILINk, M.K., redaktor; SOLOVEYCHIK, A.A., takhnicheskiy redaktor. , [ocean currents] Morskie techeniia. Leningrad, Gidrometeorlogichaskce izd-vo, 1954. 106 p. (MIRA 8:4) (ocean currents) BOCHKOV, A.P., kandidat tekhnicheskikh nauk; SOKOLOVSKIY, D.L., doktor tekhnicheakikh nauk, professor, redaktor; SHATILINA, M.K., redaktor; SOLOTSYCHIK, A.A., tekhnicheskiy redaktor.- [Influence of forests and afforestation improvement measures on the vlow of rivers in the forest steppe zone of IVropean Russia] Vliianie less, i agrolesomeliorativnykh meropriiatii na vodnost' rek lesoetepnol zony evropelskoi chasti SSSR. Pod red. D.L.Sokolovskogo. Leningrad, Gidrometeorologicheskoe izd-vo, 1954. 133 P. [Miorofilm] (MMA 7:11) (Forest influences) (Rivers) ZAYKOV, B.D., doktor geografichaskikh nan , professor; ~ redaktor; BRAYNINA, M.I., tekhnicheskiy redaktor _W~LINA.:K.K., [High waters and floods in rivers of the U.S.S.R. during the historical period] Vyaokie polovodlia i pavodki na rekakh SSSR za istericheakoe vremia. Leningrad. Gidrometeorologichaskoe izd-vo. 1954. 133 P. (MLRA 7:10) (Floods) ALEKIN, Oleg Aleksandrovich; SHATILINA, M.G., redaktor; VORONKOV, P.P otvetstvennyy redaktor';-jL&UM, M~Ta., tekhnicheskiy redaktor. [Chemical analysis of inland waters; study under stationary conditions] Khimicheskii analiz vod sushi; pri atatsionarnom ikh isuchenii. Leningrad, Gidrometeorologicheskoe izd-vo, 1954. 199 P. (KF.RA 8-.2) (Water--Analysis) ANDRZYNVA, Yakaterina Vla4imirovna; KOIASNIK. S.V.i redaktor- SHATILINA, redektor; BIUYNINA, K.L. tekhaicheakiy [1U.N.Shokel'skii, ocaaaographer, meteorologist, geographer] IU.M.Shokallskii - okeanQgraf, meteorolog. geograf. Isd. 2-ost Uaingrad. Gidrometeor. izd-vo. 1956. 52 p. NLRA 10:10) le Chlau-korrospondent Akedemii nauk USSR (for loleedk)' (S4okallokii, W11i Mikhailovich, 1856-1940) DUVANIN, Aleimandr Ivanovich; SIEZHINSKjY, V..A., otvetstvennyy redak-tor; --494~T- 1~ 3.,K., re"ktor; BRAYNIM., M.I., tekhnicheBkiv redaktor CSea level] Uroven, moria. lomingrad, Gidrometaorologichask-oe izd-vo. 1950'. 5B P. (MLRA 10:4) (ocean) POPC7, Yevgeniy Grigorlyevich; SHATILINA. M.K., red,-; FLAUM, H.U., tekhn. red, [Analysis of the runoff formation of plains rivers] Analls formiro- vaniia stolm ravninnykh rek. Ieningrad, Gidromateor. izd-vo. 1956. 130 P. (NIRk 11:7) (Rivers) (Runoff) DIMAKSYAII, Arta3hes Movsesovich; ZBORYKIN, K.A.,otyetstvennyy redaktor; SaTILIKA, M.K.,redaktor; SOMIKIIIN, K.F.,tekhnicheskiy rodaktor [New telemetering instruments for hydrometeorological r)urposes] Novye teletzmeritellnye gidrometeorologicheskie pribory. Leningrad, Gidrometeor. izd-vo, 1957. 135 P. (MLRA 10:5) (Meteorological instruments) (Telemetering) bUGOL'fU':j,,.V.., Irina Vladimiroviia; ZAYKOV, B.D., doktor geograficheakildi nauk. redaktor. redaktor; BRAYNIDA, M.I., tekhnicheskiy r r L.9roding streams and their extension over the territory of the U..'j,.S.R.] Selevye potoki iikh resprostranenie as territorii Sssi. ?od. red. B.D.Zaikova. Leningrad, Gidrometeor. izd-vo, 1957. 150 3. (Aros's. on) (MLRh 10:10) KALIMN, Genadiy Favlovich; MAKAROVA, Tatlyana Timofe7evr*.; SOMOV, N.V., otvetstvennyy redaktor; SHATILINA.M.K., redaktor; FLAUM, M.Ya., tekhnicheski.r [Hydrometeorological factors determining the occurrence of high water in the flat land rivers of European Russiaj Gidormeteorologi- ches*e usloviia formirovaniia vysokogo polovodlia na ravninnykh rei*kh'Evropeiskoi territorii SSSR. Leningrad, Gidrometeor4izd- vo 1957. 177 P. (MLRA 10:6) (Favers) PHASE I BOOK EXPLOITATION 361 Moscow. Tsentrallnyy institut prognozov. Trudy. vyp. 49: Voprosy dologosrochnykh prognozov (Transactions. v. 49: Problems in Long-range Forecasting) Leningrad, Gidrometeoizdat, 1957. 287 P. 1,250 copies printed. Sponsoring Agency: Glavnoye uDravlenlye gidrometeorolog~choskoy sluzhby pri Sovete Ministrov EFFR. Ed.: (title page): Morskoy, G.I.; Ed. (inside book-): Shatilina, M..K.; Tech. Ed.: Braynina, M.I. PURPOSE: The collection of articles is intended for specialists in the field of weather forecasting, especially those interested in long-term prognostication. COVERAGE: The articles in this collection illustrate the present position of long-range weather forecasting. The problems discussed include the formulation of large mid-monthly Card l/ 10 Problems in Long-range Forecasting 361 temperature anomalies, the analysis -of cycles and anti-cycleoge- nesis in meridional" circulation and factors causing the appearanue of autumnal frosts together with possibilities for forecasting them. TABLE OF CONTENTS: Morskoy, G.I.; Semenov, V.G.; and Kats, A.L. Formation of Air Temperature Anomalies on Soviet Territory in the Winter Months 3 The authors define the term anomaly (or a larger anornaly) as a departure from a certain average climatological pattern, or, in other words, from the average temperature during a given period. The authors survey the occurrence of mean temperature anomalies during three winter months (December, January, and February) and analyze possibilities of forecasting such anomalies for one month in advance. In general, wide departures Card 2/10 Problems In Long-range Forecasting 361 from average temperatures are believed to be caused by disturbances In the interrelationship -between air circulation and thermal conditions at the surface layer of the atmosphere. The entire article is divided into three chapters each one separate factor causing the occurrence of anomalies. In thv-. first-chapter, G.I. Morskoy states that the ho.oizontal transfer of air masses is the main factor in the formation of average temperature anomalies. He also deduces the ratio between the zonal circulation of the atmosphere and the generLl thermal conditions of the atmosphere. The author suggests a new mathematical approach in calculating the mean monthly temperature anomalies for absolute topography at the 500 millibar level. In Chapter 2, V.G. Semenov analyzes the influence of the surface layer of the atmosphere on the transfer of air masses arid-how this transfer causes the occurrence of anomalies. In the third chapter,A.L. Kats surveys the meridional and latitudinal circulation of the atmosphere and evaluates the contribution Card 3/10 Problems in Long-range Forecasting -61 of this transfer of air masses to temperature anomalies. The meridional and latitudinal circulations are calculated for a number of regions and altitudes in the Northern hemisphere. The number of focuses on the Soviet territory, where large- scale anomalies are formed during the three winter months, is found to fluctuate between 2 and 4. This article is based on the results of an analysis of 8 forecasts made on the 25th of each preceding month, for December., January and February of 1955-57. Data on forecasts were compiled separately by three different bureaus of the Central Institute of Forecasting (TSIP), viz., the long-term prediction division (ODPP), the division of dynamic meteorology (ODM), and the division for methodological Improvement of forecasting service (ORUMDFP). There are 55 maps, 52 tables in the text and 24 tables in the appendix. There are 30 references, 16 of which are Soviet, 11 are English and 3 are German. Card 4/ 10 Problems in Long-range Forecasting 361 Rafailova, Kh. Kh. Influence of the Artic Region on the Character of Merldional Circulation of Air in Europe and Western Siberia. 181 The circulation of atmosphere in the Arctic was studied by B.P. Mulltanovskiy. 'He concluded that the polar region is not a solid high-pressure zone, but, contrary to previously expressed opinions, is composed of a number of cyclonic and anticyclonic areas. Other Soviet scientists, namely B.L. Dzerdzeyevskiy and L.A. Vitel's confIrmed Mul'tanovskiy's theory and proved that all circulation phenomena such as occur in moderate zones, exist also in the polar zone. The present article analyzes the effect of.air circulation in the polar area on the behavior of meridional processes, carrying cold arctic air masses to temperate zones and thus bearing directly on changes in weather. Consequently, any weather forecasting In the moderate zone must account for meridional processes drifting in from the North. The author Card 5/10 Problems in Long-range Forecasting 361 examines four possible types of thermobaric fields in the troposphere over the Artic and also a number of variations. Maps accompany this analysis and provide data nn absolute and relative topography at 500 millibar level for all the types Involved. The author concludes that a certain definite character of the baric field in the Arctic produces a definite type of meridional movements and that thermal conditions of air masses in the Arctic are good Indices for the developing synoptic , situation in the moderate zone. There are 11 tables, 22 maps, and 17 references, of which 13 are Soviet and 4 are English. Bagrov, N.A. Application of the Principle of Similarity in Forecasting Mean Monthly Air Temperatures 231 By the "principle of similarit " the author understands an attempt to trace similarities Tanalogies) in the development of two or more atmospheric macroprocesses. The principle can be applied in long-term forecasts when an atomospheric process bears a similarity to a process which occur-red some time in the past but during the same season and in the same locality. Card 6/10 Problems in Long-range Forecasting 361 The author analyzes the applications of this principle and refers to S.T. Pagova who opposed it and to L.A. Vitelts who modified it. The latter worked out a theory of rhythmicity (rhythmical recurrence) of temperature processes. Vitells' theory is given in brief, but the author of the article rejects it. The author establishes indices of similarity and demonstrates their applicability in deducing mean monthly temperatures The data used cover a period -)f over 50 years and are derived from 45 unsDecified Ezelographical localities in Russia shown on an enclosed map. The percentage of correct forecasts by the principle of similarity has hardly ever exceeded 70 percent; on an average It amounted to 63.2 percent. The author urges expansion of this method of study and the inclusion of localities outside Russia. He suggests examination of other factors, such as near-surface pressure, to which the principle of similarity could be applied. There are 8 maps, 7 tables and 14 references, of which 8 are Soviet, 2 German and 4 English. Card 7/10 Problems in Long-range Forecasting 361 Zverev, N.I. Influence of Ocean and Land Temperature on Atmospheric Circulation During the Warm Season in the Far East 250 The author analyzes the influence of thermal nonuniformity of the surface layer on the atmospheric circulation and discusses some implications from observation results pertinent to weather forecasting. The author defines nonuniforraity as the phenomenon of the accumulation of heat in the surface layer and the unequal distribution of this heat in latitudinal and meridional directions. The article consists of two chapters. One examines the formation of temperature contrasts between ocean and land and the other examines the auestion of period- icity, i.e., the existence of definite -natural temperature intervals (from 6 to 12 days), and the connection of such periods with temperatures of the near-surface air layer.. The subject of temperature variation was studied by personnel of the'long-term forecast division of the Far Eastern Scientific r Research Institute of Hydrometeorology (D)f NIGMI).The- Lnst-itute Card 8/10 Problems in Long-range Forecasting 3061 compiled daily temperature maps for sea and land in 1934-38. In addition, the author availed himself of the material collected in the archives of the Central Institute of Fore- casts (TSIP). There are 12 maps, 6 tables, and 8 Soviet references. Byal.ynitskaya, V.(',., and Ped', D.A. Formation of Night Frosts in Ukraine 264 The authors place night frosts in Ukraine into the category of those that are dangerous, i.e., capable of damaging crops. This type of frosts is common both in autumn and in spring, but the authors analyze only the occurence of frosts in May. Crimea is included in this study. Tabular material includes statistics of occurrence and duration of frosts. The &.oticle analyzes the thermobaric field during the occurrence of frosts and.compares it with the field when frost is absent. Pertinent Card 9/10 Problems in Long-range Forecasting 361 Indices are deduced and data given on how to forecast the onset of frosts one to two days ln advance. There are 13 tables in the text and 2 in the appendix,