A METHOD OF AUTOMATING THE PRESENTATION OF INFORMATION DURING COMPLEX AIR PHOTO INTERPRETATION

A method of complex image processing, i.e., the simultaneous use of various kinds of remote sensing imagery in the mapping and study of geographic features, is outlined. It features the use of computerized techniques (a) to identify shots or frames of auxiliary types of imagery containing the same specific geographic features identified on the principal type of imagery [this through the scanning of code lines containing information about the coordinates of imaging, flight direction and altitude of the plane or sensing platform, etc.], and (b) to precisely locate the features of interest within these shots or frames. Translated from: Izvestiya vysshykh uchebnykh zavededeniy, Geodeziya i aerofotos'yemka, 1986, No. 1, pp. 86–91.     

USE OF THE CARTOGRAPHIC METHOD IN THE STUDY OF CHANNEL PROCESSES

A second paper on floodplain and channel mapping describes how the “cartographic method” (the use of maps to derive information about the world not readily available through other means of investigation) is applied through the use of special maps depicting the sizes and types of river channels, the character of floodplains and of channel deformation, and the general conditions responsible for channel evolution. The uses, strengths, and limitations of channel maps at small, intermediate, and large scales are discussed, as well as methods of cartographic presentation that have proven most effective. Translated from: Geografiya i prirodnyye resursy, 1986, No. 3, pp. 99-108.     

VEGETATION AS A CRITERION FOR INTERPRETING THE MOISTURE REGIME OF A LANDSCAPE

Vegetation signatures on aerial photographs and space imagery are used as indicators of soil moisture differences in a Siberian taiga landscape. The authors use remote sensing products to identify all major habitat types resulting from variable soil moisture regimes that were observed on the ground. These types are described, as are their interpretation keys and the effects of scale change on habitat discrimination. Translated from: Kosmicheskiye metody izucheniya prirodnoy sredy Sibiri i Dal'nego Vostoka, Novosibirsk, 1983, pp. 63-74.     

INTERPRETATION OF STORM SURGES AND RELATED PHENOMENA ON SPACE IMAGERY

A final paper on water-level monitoring from space outlines principles for the use of space imagery in interpretation of short-term changes in the position of shorelines and coastal water levels resulting from storm surges and strong offshore winds. Over 100 images of various types, seasons, and storm-surge conditions, carefully referenced with field data on slope, vegetation cover, water level, and wind direction, were used to determine “maximal” and “minimal” positions of the Caspian shoreline for the period 1973-1983. This information is useful in understanding the seasonal regime of water-level fluctuations and anticipating flooding associated with winds of a given velocity. Translated from: Izvestlya vysshikh uchebnykh zavedenly, geodeziya i aerofotos'yemka, 1986, No. 4, pp. 93-97.     

DEVELOPMENT OF QUANTITATIVE METHODS OF STUDYING THE EARTH FROM SPACE

The paper surveys the development of “space geography”–a field of knowledge applying the methods of remote sensing, the physical sciences, and mathematics in the solution of geographic problems. Early advances featured methodological improvements (use of quantitative methods in image processing), whereas future research must focus upon perfecting our knowledge of: (a) relationships underlying the use of these methods, i.e., between environmental parameters and reflectance values, (b) methods of effectively combining different types of imagery, and image products and field work, in research, and (c) appropriate quantitative indices for feature recognition. Examples of the operationalization of such concerns are demonstrated for land-use and soil mapping projects. Translated from: Izvestiya, AN SSSR, seriya geograficheskaya, 1985, No. 5, pp. 110–116.     

PRINCIPLES OF THE COMPARISON AND INTERPRETATION OF MULTITEMPORAL IMAGERY

General principles are outlined for the use of a series of remote sensing images (obtained for the same area of the earth's surface for different points in time) in the detection of significant changes in land use and environmental conditions. Emphasis is placed on visual methods of interpretation, and a number of different methods for graphically analyzing the dynamics of earth surface features on photographic image products are described. A final section describes procedures for cartographically representing the dynamics of features interpreted from multitemporal images. Translated by Jay Mitchell; PlanEcon, Inc.; Washington, DC 20005 from: Vestnik Moskovskogo Universiteta, geografiya, 1987, No. 6, pp. 57-60.     

PROBLEMS AND PROSPECTS OF THE COMPLEX ECOLOGICAL-GEOGRAPHIC MAPPING OF SIBERIA

A review of basic theoretical principles of “ecological” mapping and types of maps of the environment sets the stage for a more detailed treatment of ecological-geographic maps—maps portraying a wide range of nature-society and nature-nature relationships—as they are used in support of economic development and environmental monitoring in Siberia. Particular attention is devoted to the compilation of map series, which include ecological-geographical maps, for the Lake Baykal area, BAM service zone, West Siberia, and specific territorial production complexes (e.g., Kansk-Achinsk TPC). Translated from: Geografiya i prirodnyye resursy, 1987, No. 3, pp. 10-18.     

MAPPING THE SOILS OF THE MAJOR NATURAL ZONES OF THE USSR FROM REMOTE SENSING IMAGERY

The authors describe the results of their experience in the use of remote sensing imagery to map the distribution of soils within the major natural zones (e.g., wooded steppe, taiga, semidesert) of the USSR. Considerable attention is devoted to instrumental-visual methods of interpretation before the focus shifts to automated interpretation and methods of map compilation, particularly general mapping at intermediate and large scales. One section assesses the relative sizes of mesorelief forms and fields in various natural zones in an effort to determine at what image scales the soil types indicated by these features will be identifiable. Translated by Edward Torrey, Alexandria, VA 22308 from: G. V. Dobrovol'skiy and V. L. Andronikov, eds., Aerokosmicheskiye metody v pochvovedenii i ikh ispol'zovaniye v sel'skom khozyaystve: sbornik nauchnykh trudov [Remote Sensing Methods in Soil Science and Their Utilization in Agriculture: A Collection of Scientific Works]. Moscow: Nauka, 1990, pp. 22-34.     

USE OF SPACE PHOTOGRAPHS IN THE MAKING AND REVISION OF SMALL-SCALE MAPS

A brief review paper focuses on Soviet strategies for the use of space imagery, particularly photographic products (1:2,000,000 to 1:4,200,000 scale) from manned spaceflights, in the revision of small-scale general reference maps. Principles for the interpretation and mapping of basic map elements appearing on space photographs are outlined. Space photographs provide for reduction in time spent in map editing and the more correct analysis of the reliability of information and its generalization. A technology of map revision based on the joint use of original photographs and photomaps, with the transfer of revisions from photomaps to map originals, is proposed. Translated from: Geodeziya i kartografiya, 1986, No. 8, pp. 29-33.     

MAPS OF USE OF THE ENVIRONMENT IN THE BURYAT REPUBLIC

A team of Russian geographers describes the development of a program for mapping land use/resource development and the condition of the environment in Russia's Buryat Republic. Three ecological maps recently compiled in the Republic, using a single cartographic base and employing standardized methods, are described. The last such map is a map of environmental use that reflects both a resource-development and an environmental-protection perspective. The article includes detailed examples of the legend of the latter map. Translated by Edward Torrey, Alexandria, VA from: Geografiya i prirodnyye resursy, 1998, No. 3, pp. 23-29.     

SATELLITE IMAGERY OF CLOUD COVER IN THE STUDY OF SHORT-WAVE RADIATION AT THE EARTH'S SURFACE

A method is proposed for analyzing properties of solar radiation at the earth's surface based on satellite observations of cloud cover. It is shown that the amount of incident solar radiation is clearly governed by type of weather conditions and, more specifically, by the quantity and types of clouds. This affords a basis for predicting solar radiation receipt at the earth's surface. Translated by Edward Torrey, Alexandria, VA 22308 from: Vestnik Moskovskogo Universiteta, geografiya, 1989, No. 2, pp. 83–85.     

EVALUATION OF THE COEFFICIENT OF TERRESTRIAL REFRACTION

Abstract

In a previous article on this subject (Empire Survey Review, January 1937) the writer sought to show that for trigonometrical observations of vertical angles made near noon in the Tropics the coefficient of refraction depends chiefly on height above ground level in the case of stations sited within a few hundred feet above the general level of the ground surface. Indeed, the computed values of the coefficient K show a definite and appreciable increase with “h”, the height of the observing station above ground level; it is usually assumed that K decreases with increase in height above the Mean-Sea-Level surface. From analysis of the results obtained by varying h but holding the heights above Mean Sea Level fixed the writer came to the conclusion that the variations in K could only be due to abnormal values of dt/dh and d²t/dh², “t” denoting the air temperature. Now it is generally recognized by meteorologists that abnormal lapse-rates of temperature do frequently occur in the lower air layers in the Tropics; but up to the present time no temperature soundings in Nigeria are available. Recently, however, the writer came across the results of the aerological soundings made by an expedition in East Africa during the year 1908. The results of many of the soundings were of no use for the purpose of this paper; many of the observations were not taken at or near noon, and in others counterlapses of temperature in the lower layers indicated that conditions were not normal. A set of observations taken at Mombasa between 10 and 11 a.m. were eventually chosen as offering an example of what might reasonably occur in the lower layers of the atmosphere.     

REMOTE SENSING-BASED MONITORING OF GEOSYSTEMS USING MORPHOMETRIC METHODS

A Russian geographer assesses past experience with (and potential applications of) the principles and methods of landscape morphometry in the remote sensing-based monitoring of geosystems. Considerable attention is devoted to methods of calculating indices measuring the shape, nonuniformity, relative location, proximity, connectivity, and fractal dimensions of strips and patches—two basic types of forms found on remote sensing imagery. Translated by Edward Torrey, Alexandria, VA 22308 from: Geografiya i prirodnyye resursy, 1998, No. 4, pp. 97-103.     

SATELLITE MEASUREMENTS OF LAND PARAMETERS AS PART OF AN INTERNATIONAL PROGRAM OF CLIMATE RESEARCH

The role of remote sensing in one aspect of the World Climate Research Program is summarized. More specifically, unresolved theoretical and methodological problems are outlined for the use of remote sensing imagery (in conjunction with the International Land Surface Climatology Project) to derive quantitative parameters of land (and ice) surface characteristics. These parameters are raw data for models of the overall circulation of the atmosphere, which can be used to generate maps of albedo, surface roughness, hydrology, etc. A list of preliminary standards for satellite monitoring of land surface characteristics is included. Translated from: Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, 1988, No. 2, pp. 161-165.     

STUDY AND MAPPING OF LAND USE FROM REMOTE SENSING IMAGERY IN AGRICULTURAL MONITORING

A series of soil and agricultural land-use monitoring activities planned and carried out under the auspices of a local branch of the recently formed State Agro-industrial Committee is outlined. A general discussion of the place of agricultural monitoring within the overall system of environmental monitoring is followed by detailed examples of the use of space photography in preparation of photomapbases of local-level land use maps and in the compilation of the thematic detail of related agricultural maps. Translated from: Geografiya i prirodnyye resursy, 1987, No. 1, pp. 145-149.     

SUB-SATELLITE COLLECTION OF SUPPLEMENTAL REMOTE SENSING INFORMATION

This paper, the third in a series on the design, payloads, and operation of Soviet earth resource observation satellites [see MSRS, 1984, No. 4 and 1985, No. 1], describes the collection of supplemental sub-satellite information. More specifically, it outlines how the Soviets use satellite-synchronized aerial, ground, and water-borne sensors to gather auxiliary information used in the improvement of space imagery (data verification and correction, instrument calibration, etc.). A later section demonstrates procedures for selection and preparation of field test sites (for ground truth), and design of sub-satellite information measurement complexes. Translated from: Priroda Zemli iz kosmosa, A. P. Tishchenko and S. V. Viktorov, eds. Leningrad: Gidrometeoizdat, 1984, pp. 35-38.     

MAPPING THE DYNAMICS OF COMPLEX ECOSYSTEMS BASED ON SEQUENTIAL REMOTE SENSING IMAGERY

A quantitative method for mapping the contemporary dynamics of ecosystems is described. Particular reference is to the mapping of the desertification of complex ecosystems of the lower reaches of the Amudar'ya using a time series of four surveys. The types of ecological transitions identified from remote sensing imagery and their frequencies are described. Translated by Edward Torrey, Alexandria, VA 22308 from: Izvestiya Akademii Nauk, seriya geograficheskaya, 1994, No. 5, pp. 112-122.     

INTERPRETATION OF ECOLOGICAL-SOIL CHARACTERISTICS OF WOODED STEPPE ZONE IN THE CENTRAL RUSSIAN UPLAND

The authors describe how remote sensing imagery can be employed in the identification of different types of chernozem soils in a predominantly agricultural zone (forest steppe), where natural vegetation (normally one of the best vegetation indicators) has been largely displaced by farm fields. A multi-stage methodology is outlined whereby small-scale imagery is used to delineate large regions of similar bioclimatic-geologic characteristics, from which areas of similar soil formation conditions are distinguished. Multispectral and multitemporal space imagery then is employed to detect less salient ecological-soil differences that can affect phototone and image texture. Translated by Edward Torrey, Alexandria, VA 22308 from: G. V. Dobrovol'skiy and V. L. Andronikov, eds., Aerokosmicheskiye metody v pochvovedenii i ikh ispol'zovaniye v sel'skom khozyaystve: sbornik nauchnykh trudov [Remote Sensing Methods in Soil Science and Their Utilization in Agriculture: A Collection of Scientific Works]. Moscow: Nauka, 1990, pp 103–109.     

MAPPING THE STRUCTURE OF THE SOIL COVER OF THE TAIGA FROM REMOTE SENSING IMAGERY

An experiment is described in which multiscalar remote sensing imagery is sequentially employed in the detection of various rankings of soil types endemic to the taiga natural zone in the northern USSR. Relief features, vegetation associations, extent of surface water, and drainage patterns visible on imagery at scales from 1:12,000,000 to 1:5,000, also examined at low altitude and in the field at a series of test sites, served as indicators of various soil cover types. Considerable attention is given to an explanation of why these features can be considered valid indicators of taiga soil types as well as to the appearance of the indicators on band-specific (black-and-white) and color composite imagery. Translated from: Izvestiya Akademii Nauk SSSR, seriya geograficheskaya, 1987, No. 3, pp. 87-99.