I. Foehn winds of southern California. II. Foehn wind cyclo-genesis. III. Weather conditions associated with the Akron disaster. IV. The Los Angeles storm of December 30, 1933 to January 1, 1934

I. Foehn winds of southern California.
An investigation of the hot, dry and dust laden winds occurring in the late fall and early winter in the Los Angeles Basin and attributed in the past to the influences of the desert regions to the north revealed that these currents were of a foehn nature. Their properties were found to be entirely due to dynamical heating produced in the descent from the high level areas in the interior to the lower Los Angeles Basin. Any dust associated with the phenomenon was found to be acquired from the Los Angeles area rather than transported from the desert. It was found that the frequency of occurrence of a mild type foehn of this nature during this season was sufficient to warrant its classification as a winter monsoon. This results from the topography of the Los Angeles region which allows an easy entrance to the air from the interior by virtue of the low level mountain passes north of the area. This monsoon provides the mild winter climate of southern California since temperatures associated with the foehn currents are far higher than those experienced when maritime air from the adjacent Pacific Ocean occupies the region.

II. Foehn wind cyclo-genesis.
Intense anticyclones frequently build up over the high level regions of the Great Basin and Columbia Plateau which lie between the Sierra Nevada and Cascade Mountains to the west and the Rocky Mountains to the east. The outflow from these anticyclones produce extensive foehns east of the Rockies in the comparatively low level areas of the middle west and the Canadian provinces of Alberta and Saskatchewan. Normally at this season of the year very cold polar continental air masses are present over this territory and with the occurrence of these foehns marked discontinuity surfaces arise between the warm foehn current, which is obliged to slide over a colder mass, and the Pc air to the east. Cyclones are easily produced from this phenomenon and take the form of unstable waves which propagate along the discontinuity surface between the two dissimilar masses. A continual series of such cyclones was found to occur as long as the Great Basin anticyclone is maintained with undiminished intensity.

III. Weather conditions associated with the Akron disaster.
This situation illustrates the speedy development and propagation of young disturbances in the eastern United States during the spring of the year under the influence of the conditionally unstable tropical maritime air masses which characterise the region. It also furnishes an excellent example of the superiority of air mass and frontal methods of weather prediction for aircraft operation over the older methods based upon pressure distribution.

IV. The Los Angeles storm of December 30, 1933 to January 1, 1934.
This discussion points out some of the fundamental interactions occurring between air masses of the North Pacific Ocean in connection with Pacific Coast storms and the value of topographic and aerological considerations in predicting them. Estimates of rainfall intensity and duration from analyses of this type may be made and would prove very valuable in the Los Angeles area in connection with flood control problems.

Joint Anglo-Soviet biological surveillance exercise on River Dnieper

As one part of an on-going programme concerned with environmental protection as provided for under the terms of a UK/USSR Joint Environmental Protection Agreement signed in London, 21 May 1974, a seminar — ”The elaboration of the scientific basis for monitoring the quality of surface water by hydrobiological indices” was held at Valdai in Russia 12—14 July, 1976. As a continuation of this theme it was agreed that delegations of hydrobiologists from each side should carry out reciprocal visits to carry out comparative field tests on selected systems of biological surveillance in use in the respective countries. In May 1978 a team of British hydrobiologists visited the USSR, under the auspices of the Department of Environment, to carry out joint exercises on the River Dnieper and some tributaries. This paper reports the results of selected methods used by the British side when applied to the conditions found in the River Dnieper.

Comparison of systems of biological indication approved during the course of the joint Anglo-Soviet investigations held under the auspices of the Institute of Hydrobiology of the Academy of Sciences of the Ukrainian SSR

In accordance with the plan for joint Anglo-Soviet scientific and technical collaboration on environmental problems, the comparative evaluation of systems of hydrobiological analysis of the surface water quality started in 1977 at the Regional Laboratory of the Severn-Trent Water Authority in Nottingham were continued in the spring of 1978. The investigations were carried out under the auspices of the Institute of Hydrobiology of the Academy of Sciences of the Ukrainian SSR. Hydrobiological and hydrochemical samples were collected by Soviet and British specialists from the Kiev reservoir and the rivers Dnieper, Sozh, Desna and Snov. The samples were processed on the expedition ships and in the Laboratory for the Hydrobiology of Small Water Bodies of the Institute of Hydrobiology of the Academy of Sciences of the Ukrainian SSR. The possible approved methods to be adopted were evaluated from the samples using the phytoperiphyton, phytoplankton, zooplankton and zoobenthos against a background of hydrochemical characteristics. The study concludes that weather conditions complicated the work on testing the systems of biological indication of water quality and made it inadvisable to use those methods of comparison which were used when similar work was carried out in Nottingham.

Poéticas da visualidade em João Cabral de Melo Neto e Joan Miró: a poesia como crítica de arte

A tese focaliza alguns dos principais poemas de João Cabral de Melo Neto desenvolvidos como crítica poética. O mote da investigação é a construção de uma lírica crítico-discursiva, uma produção artística que avalia a arte com os termos, os instrumentos da própria arte. Esta perspectiva analítica é deflagrada pelos primeiros românticos (Schlegel e Novalis) e expande-se em duas direções: tanto o poema escrito a partir de uma reflexão sobre a arte ou a natureza (crítico em sua gênese), quanto a crítica, transmutada em poesia. A abordagem comparativa de estâncias do poeta com obras picturais nelas referenciadas evidencia o constante diálogo do poeta com as poéticas da visualidade e com as concepções estéticas da modernidade, mormente com a poética de Joan Miró. Através da abordagem comparativa, materializam-se dois caminhos privilegiados de experimentação estética: o percurso do poético ao plástico, em João Cabral; o caminho inverso, na obra do pintor catalão do plástico ao poético. Para ambos os artistas, os processos de exploração das linguagens artísticas ocasionam, como consequência extrema, a dissolução do plástico e do poético, rumo ao inefável na pintura e na poesia. Para Miró, os signos plásticos são poéticos, porque guardam em si um universo de possibilidades significativas que transcendem a ordem da própria coisa em si. E o alcance das transformações que a sua poética empreende afetará a poesia de modo análogo: os signos poéticos mostram-se plenamente poéticos, ao transcenderem a forma e o sentido, no âmbito da plasticidade da palavra. Se a palavra pode se tornar matéria (passar da abstração para a concreção), a matéria pintada pode ser poesia. Integram a constelação teórica desta investigação os principais filósofos que discutem o caráter crítico da poesia, desde os filósofos do primeiro romantismo (Schlegel e Novalis), até aqueles cujo pensamento está relacionado à modernidade ou à pós-modernidade (Benjamin, Adorno, Lyotard, Blumenberg e Agamben)