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Preliminary results yielded qualitative and quantitative estimates for surface rock abundances.
The U.S. Geological Survey (USGS) errors for hydrologic measurements ranging from "excellent (5%)" to "fair (15%)" [ Sauer and Meyer, 1992] were used to provide error estimates for surface water reservoir storage.
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We obtain bilinear restriction estimates for surfaces with vanishing curvatures.
On the basis of numerical results, and with consideration of some particular material parameters, the probable service life period of contacting surfaces is estimated for surface curvatures and loadings that are most commonly encountered in engineering practice.
JULES was driven using spatially distributed air temperatures from the empirical model, along with distributed solar and long-wave radiation flux estimates adjusted for surface slope and aspect, and sky-view in order to model the surface energy balance and predict thermal climate at the vegetation surface (skin temperature).
Sources were not estimated for surfaces that represented deep white matter, ventricles, or noncortical structures unlikely to generate extracranial MEG or EEG signals.
Estimates for land surface impacts from subsidence are as high as 1 million ha (Hu 2009).
The enthalpy estimates for the surface species and transition states were obtained by correcting the electronic energies, as obtained from our DFT calculations, for ZPE contributions and temperature variations.
For example, Wohlfahrt et al. (2009) noted that widely varying estimates for the surface conductance to water vapor were obtained by inverting the Penman Monteith combination equation depending on how ɛ was dealt with.
Applications of satellite observations are discussed for case studies of specific events, for estimates of surface concentrations, and to improve emission inventories of trace gases and aerosols.
These simulations provide a basis for estimates of surface and void tortuosities, which are essential in the interpretation and extrapolation of diffusion rates in complex porous media.
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