976 resultados para Physical geography -- Periodicals -- Indexes
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Land use intensification is estimated to result in an overall increase in sediment delivery to the Great Barrier Reef lagoon by a factor of approximately four. Modelling suggests that, following land use intensification, croplands cause the greatest increase of sediment yield and sediment concentration, whereas erosion of grazing land is the main contemporary source of sediments, primarily owing to the large spatial extent of this land use. The spatial pattern of sediment yield to the coast after land use intensification is strongly correlated with the pattern under natural conditions, although the greatest increase is estimated to have occurred in the wet-dry catchments. Sediment transport and resuspension processes have led to the development of a strongly sediment-partitioned shelf, with modern mud-rich sediments almost exclusively restricted to the inner and inner-middle shelf, northward-facing embayments and in the lee of headlands. Elevated sediment concentrations increase the potential transport rates of nutrients and other pollutants. Whether increased sediment supply to the coastal zone has impacted on reefs remains a point of contention. More sediment load data need to be collected and analysed in order to make detailed estimates of catchment yields and establish the possible sediment impact on the Great Barrier Reef.
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Published eyewitness accounts and stories form Aboriginal Australians are used to provide an overview of the geographical extent and characteristics of cooperative fishing between Aboriginal Australians and dolphins in eastern Australia. These sources indicate that cooperative fishing was geographically widespread in eastern Australia, involved both bottlenose dolphins and orcas, and had a significance (emotional and Spiritual) to Aboriginal people beyond the acquisition of food. These fishing interactions represent both context and precedent for the economic and emotional-objectives of contemporary human-dolphin interactions such as dolphin provisioning. (C) 2002 International Society for Anthrozoology.
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Dissertação apresentada como requisito parcial para obtenção do grau de Mestre em Ciência e Sistemas de Informação Geográfica
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If widespread deforestation in Amazon results in reduced evaporative water flux, then either a decrease in evaporation is compensated locally by reduced rainfall,or else changed moisture balance expresses itself downwind in the yet undisturbed forest. The question of where rain will occur is crucial. It is suggested that the appearance of clouds and the occurrence of rainout is governed primarily by the interplay of local meteorologic and physical geography parameters with the atmospheric stability structure except for a few well-defined periods when rain is dominated by large scale atmospheric instability. This means that the study of these phenomena (local heat balances,studies on cloud formation mechanism, vertical atmospheric stability, etc.) must be made on the scale of the cloud size, a few tens of kilometers at most.
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Ecological economics is a recently developed field, which sees the economy as a subsystem of a larger finite global ecosystem. Ecological economists question the sustainability of the economy because of its environmental impacts and its material and energy requirements, and also because of the growth of population. Attempts at assigning money values to environmental services and losses, and attempts at correcting macroeconomic accounting, are part of ecological economics, but its main thrust is rather in developing physical indicators and indexes of sustainability. Ecological economists also work on the relations between property rights and resource management, they model the interactions between the economy and the environment, they study ecological distribution conflicts, they use management tools such as integrated environmental assessment and multi-criteria decision aids, and they propose new instruments of environmental policy.
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This article lies within the sphere of studies initiated recently in various social sciences and which aim to introduce women's problems as an element of analysis, or in other words, the gender perspective. In the field of geography, the earliest contributions of this nature were made in English-speaking countries. It is only in the 1980s that similar contributions begin to appear in Spanish geography, albeit sporadically . In the first part of this article, an analysis is made of the presence of women geographers in Spanish universities, based on a questionnaire submitted to twenty-six departments of geography. The questionnaires provide information on the age, sex and marital status of women staff, and other relevant facts. It becomes evident that women lecturers are in the minority in Spanish university Geography Departments, especially in the top posts, although the percentage compares favourably with English-speaking countries. The second part of the article consists of a study of the written contributions of women geographers through the analysis of the various geographical magazines published by geography departments and other related bodies. The author reaches the conclusion that the percentage of articles written by women geographers is even lower than the corresponding percentage of staff members. Especially noteworthy is the very limited number of articles in the fields of physical geography and geographical theory, in contrast to a certain tendency to publish studies on, for example, population or urban topics with a highly restricted territorial scope
La Géographie française et le risque d'inondation: de la géographie physique à la géographie humaine
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Les inondations, comme tous les risques naturels, ont été un thème qui est revenu souvent au long de l'histoire de la géographie française, mais toujours — et contrairement à ce qui se passe dans la géographie anglo-saxonne —, en relation à la géographie physique. Dans cet article, nous voulons expliquer les raisons de la présence de la géographie physique dans le traitement du risque d'inondation : nous mettons en relation les différents moments de la géographie française avec l'analyse du risque d'inondation et révisons le contenu des références aux inondations entre les géographes ou écoles géographiques les plus représentatifs
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L'étude des risques naturels est devenu un sujet de débat entre les géographes physiques français, de plus en plus conscients de l'exposition croissante des sociétés aux risques naturels et du besoin d'évaluer leurs compétences et leurs moyens d'intervention. Mais l'étude des risques naturels a aussi été un sujet récurrent dans l'histoire de la géographie française. Cet article prétend être une approche au traitement qu'a reçu ce thème dans les Annales de Géographie depuis sa création jusqu'h aujourd’hui. Après avoir distingué trois étapes (1891-1930, 1930-1975 et 1975-1991) on a établi les rapports existants entre les différents moments de la géographie française et l'étude des risques naturels et on a analysé autant le contenu des notices sur les divers évènements catastrophiques que les travaux des auteurs les plus représentatifs. I1 s'agit, en résumé, de proposer une réflexion sur la façon dont la géographie française a abordé ce sujet
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Recent advances in remote sensing technologies have facilitated the generation of very high resolution (VHR) environmental data. Exploratory studies suggested that, if used in species distribution models (SDMs), these data should enable modelling species' micro-habitats and allow improving predictions for fine-scale biodiversity management. In the present study, we tested the influence, in SDMs, of predictors derived from a VHR digital elevation model (DEM) by comparing the predictive power of models for 239 plant species and their assemblages fitted at six different resolutions in the Swiss Alps. We also tested whether changes of the model quality for a species is related to its functional and ecological characteristics. Refining the resolution only contributed to slight improvement of the models for more than half of the examined species, with the best results obtained at 5 m, but no significant improvement was observed, on average, across all species. Contrary to our expectations, we could not consistently correlate the changes in model performance with species characteristics such as vegetation height. Temperature, the most important variable in the SDMs across the different resolutions, did not contribute any substantial improvement. Our results suggest that improving resolution of topographic data only is not sufficient to improve SDM predictions - and therefore local management - compared to previously used resolutions (here 25 and 100 m). More effort should be dedicated now to conduct finer-scale in-situ environmental measurements (e.g. for temperature, moisture, snow) to obtain improved environmental measurements for fine-scale species mapping and management.
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En el presente trabajo se realiza, de un modo sucinto, un repaso selectivo de diferentes concepciones modernas de la Geografia Física. Se resaltan las principales ideas clave y aportaciones seminales, lo que permite, finalmente, trazar una concepción sinóptico-evolutiva de la materia. Se trata, pues, como punto de partida, de responder qué ha de entenderse por Geografia Física, sin pretender abarcar la totalidad de la evolución histórica de la disciplina, ni desarrollar de una forma exhaustiva sus diferentes concepciones. Si ése fuera el propósito, difícilmente escaparíamos a una postura petulante, presumiblemente condenada al fracaso, cuando la laboriosa y meritoria obra de GREGORY (1985) -practicarnente sin precedentes- presenta unas ciertas limitaciones al respecto (Cox, 1986). Se va, por el contrario, a definir lo que -en el lenguaje de la propia Geografia Física- con sus "coordenadas" epistemológicas; es decir, los ejes directrices modernos que han guiado su desarrollo.
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There is much policy interest in the possible linkages that might exist between land use and downstream fluvial flood risk. On the one hand, this position is sustained by observations from plot- and field-scale studies that suggest land management does affect runoff. On the other, upscaling these effects to show that land-management activities impact upon flood risk at larger catchment scales has proved to be elusive. This review considers the reasons for why this upscaling is problematic. We argue that, rather than it reflecting methodological challenges associated with the difficulties of modelling hydrological processes over very large areas and during extreme runoff events, it reflects the fact that any linkage between land management and flood risk cannot be generalized and taken out of its specific spatial (catchment) and temporal (flood event) context. We use Sayer's (1992) notion of a `chaotic conception' to describe the belief that there is a simple and general association between land management and downstream flood risk rather than the impacts of land management being spatially and temporally contingent in relation to the particular geographical location, time period and scale being considered. Our argument has important practical consequences because it implies that land-management activities to reduce downstream flood risk will be different to traditional flood-reduction interventions such as levees. The purpose of demonstration projects then needs careful consideration such that conclusions made for one project are not transferred uncritically to other scales of analysis or geographical locations.