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Terrain generation

Terrain generated using the radialized logit transform on the logistic vari-... [Pg.240]

For terrain generation, student experiments, and possible inclusion in statistical software packages, I have found the transformation given by... [Pg.244]

If readers are interested in using the preceding for 3-D extraterrestrial terrain generation, convert the z distribution to a radial one in polar coordinates, and use the Ulamized variables y as angles ... [Pg.244]

AERMOD AERMOD is the next generation air dispersion modeling system and consists of 3 components - AERMOD (air dispersion model), AERMET (meteorological data preprocessor) and AERMAP (terrain preprocessor). A brief overview of the model can be found in the mod-desc.txt file which can be downloaded from the site. [Pg.330]

Fig. 9-3 Conceptual model to describe the interaction between chemical weathering of bedrock and down-slope transport of solid erosion products. It is assumed that chemical weathering is required to generate loose solid erosion products of the bedrock. Solid curve portrays a hypothetical relationship between soil thickness and rate of chemical weathering of bedrock. Dotted lines correspond to different potential transport capacities. Low potential transport capacity is expected on a flat terrain, whereas high transport is expected on steep terrain. For moderate capacity, C and F are equilibrium points. (Modified with permission from R. F. Stallard, River chemistry, geology, geomorphology, and soils in the Amazon and Orinoco basins. In J. I. Drever, ed. (1985), "The Chemistry of Weathering," D. Reidel Publishing Co., Dordrecht, The Netherlands.)... Fig. 9-3 Conceptual model to describe the interaction between chemical weathering of bedrock and down-slope transport of solid erosion products. It is assumed that chemical weathering is required to generate loose solid erosion products of the bedrock. Solid curve portrays a hypothetical relationship between soil thickness and rate of chemical weathering of bedrock. Dotted lines correspond to different potential transport capacities. Low potential transport capacity is expected on a flat terrain, whereas high transport is expected on steep terrain. For moderate capacity, C and F are equilibrium points. (Modified with permission from R. F. Stallard, River chemistry, geology, geomorphology, and soils in the Amazon and Orinoco basins. In J. I. Drever, ed. (1985), "The Chemistry of Weathering," D. Reidel Publishing Co., Dordrecht, The Netherlands.)...
The geology of Cyprus is dominated by four distinct terranes - the Troodos Ophiolite Complex composed of mafic and ultramafic rocks, the Circum-Troodos Sedimentary Sequence containing calcarenites, siltstones and carbonates, the Mamonia Complex composed of igneous, sedimentary and metamorphic rocks and the Kyrenia Terrain containing a series of allochthonous massive and recrystallised limestones dolomites and marbles. These terranes generate highly varied landscapes (Fig 1). [Pg.503]

Robert Lespieau s aim to establish a disciplinary specialization of "chemical theories" in France was partially realized in the work of some of his students, especially Dupont, Prevost, and Kirrmann. For the first time, a clearly defined research school in France practiced the art of "theoretical chemistry" in their study of organic structure and reaction mechanisms. They self-consciously employed physical methods and apparatus, and they stayed in contact with a small network of physicists who were teachers, friends of Lespieau, or immediate colleagues. They had a laboratory terrain that was the home meeting place, no matter what their current affiliation. They had a common history that could be traced back generation by generation in the Ecole Normale laboratory to Berthollet, the "father" of chemical mechanics. [Pg.178]

On and on I droned. Three so-called Mars generators (modified Venturi aircraft jets) would disseminate streams of BZ in the general direction of the trailer truck. To deal with vagaries in the wind patterns, the truck would move forward or backward along the circle as required to track the cloud. Upon reaching the desired dose the volunteers and booth occupants, all still wearing ftrll protective clothing, would jump into a pickup truck and race across the sandy terrain back to where we had started. [Pg.143]

We believe the major shortcoming of these models is inadequate meteorological input. In particular we need better descriptions of flow within the canopy and vertical flow profiles generated by drainage flow rather than mesoscale winds. We also need a fully operational three dimensional, complex terrain winds model. [Pg.94]

Iceland s potential to generate power from hydroelectric dams is also considerable because of the country s large area of mountainous terrain, glacial melt, and reliable precipitation. Hydroelectric plants in the country currently have a capacity of approximately 1,000 mw12 and supply more than 6.8 million Mwh per year of electricity.13 In March 2003, Iceland approved plans for an Alcoa Inc. aluminum smelter and a 630 mw hydroelectric facility to provide power for this very electricity-intensive process.14 This decision has encountered opposition from environmental groups because the resulting reservoir will flood land in an undeveloped wilderness area. [Pg.191]

The most critical parameter for the introduction of hydrogen technologies in Segments II and III is cost effectiveness versus concurrent solutions such as grid extension and diesel engine generator sets. Previous studies have shown that grid extension costs are approximately 20,000 /km and potentially increase up to 25,000-30,000 /km in remote areas with complex terrain (Vallve and Serrasolses, 1997). [Pg.146]

Another approach is to follow a genetic model for continental crust formation, for example in island arcs, oceanic plateaus or Archean granite-greenstone terrains. For example, the full vertical crustal sequence of a mature island-arc has been reconstructed in the Hidaka belt in Hokkaido, Japan over a total thickness of 30 km. This arc contains high-grade metamorphic rocks representative of lower crustal material and its average rate of crustal heat generation is 0.83 p.W m (Furukawa and Uyeda, 1989 Furukawa and Shinjoe, 1997). [Pg.1333]


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See also in sourсe #XX -- [ Pg.244 ]




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