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  • Climate and thermodynamic systems of maximum dissipation
  • Some thermodynamic criteria for river channel changes
  • A theoretical model of river channel changes is presented, which shows some nonequilibrium thermodynamic criteria of a river channel to bedding and equilibrium.
  • Structure of an evolutive hailstorm, part II: Thermodynamic structure and airflow in the near environment
  • Equilibrium and nonequilibrium statistical thermodynamical approaches to modeling spatial interaction dynamics
  • Thermodynamic and economic concepts as related to resource-use policies
  • Non-invasive geophysical investigation and thermodynamic analysis of a palsa in Lapland, Northwest Finland
  • Climatic warming ; Cold area ; Collapse structures ; Finland ; Geophysics ; Ground penetrating radar ; Humid environment ; Model ; Northwest Finland ; Palsa ; Permafrost ; Soil temperature ; Thermodynamics
  • Non-invasive geophysical prospecting and a thermodynamic model were used to examine the structure, depth and lateral extent of the frozen core of a palsa near Lake Peerajärvi. A simple thermodynamic model verified that the current climatic
  • core of the palsa. The presence of the frozen core could also be traced as minima in surface temperature and ground conductivity measurements. These field methods and thermodynamic models can be utilised in studies of climate impact on Arctic wetlands.
  • Spatial and temporal variations in the thermodynamics since the Last Glacial Maximum at Jutulstraumen drainage basin, East Antarctica
  • Topics in dynamical meteorology. 3. Thermodynamics
  • The AA. intend to consider phenomenological as well as statistical thermodynamic landscape models. From maps, the entropy of various landscapes will be calculated according to the two types of models mentioned and conclusions will be drawn regarding
  • Modelling within a thermodynamic framework : a footnote to Sanders (1999)
  • With the help of thermodynamic parameters is proved, that non-regenerative waste deposits in any case wear an enormous dangerous potential. Non-regenerative deposits (for example special, poison, noxious and selective deposits) must be handled
  • as long as such kind of deposits as the deposited substances are a dangerous potential for the biosphere. From the thermodynamical point of view there exist no tight deposits. Regenerative deposits (for example municipal wastes, mixed noxious and building
  • The AA. provide a summary of the current state of knowledge pertaining to the geophysical, thermodynamic and dielectric properties of snow on sea ice. They first give a detailed description of snow thermophysical properties such as thermal
  • -year sea ice. Finally, they discuss the annual evolution of the Arctic system through snow thermodynamic and aeolian processes, with linkages to microwave remote sensing.
  • Thermodynamic and circulation characteristics of winter monsoon tropical mesoscale convection
  • Atmospheric thermodynamics.
  • Inefficiency of spatial prices using the thermodynamic formalism
  • The spatial, temporal, and thermodynamic characteristics of Southern-Atlantic United States tornado events
  • the difficulty of measuring thermal energy in the field, its inefficient use in nature, and the uncertainty with which it and form can be related, thermodynamic equilibria concepts would appear, presently, to offer geomorphologists only very limited opportunities.
  • In the thermodynamic theory of aquatic ecosystems the non-linear relations between rates and affinities of biological processes, such as primary production, respiration, grazing etc. can be determined using an optimun principle. Especially
  • This paper focuses on dehydration of hornblende during the retrograde metamorphism to examine the rock-fluid interaction which produced the charnockite-enderbite suites in the Northern Marginal Zone, Zimbabwe, on the basis of available thermodynamic
  • Principal factors causing avalanches are discussed: topography, meteorology, snow conditions and mechanical factors. The types of crystals forming each layer are of great importance because they relate thermodynamic factors to characteristic snow