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It was achieved through the recognition and correlation of regional surfaces that have allowed the subdivision of this unit into distinct depositional sequences, and the reconstruction of its depositional history.
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Those factors are estimated from readily available information, such as earthquake magnitude and hypocentral depth, time of the event, or they had to be compiled from generally more rare data on fault characteristics, regional surface morphology, antecedent rainfall or general climatic background of the affected region and the regional geology.
The latter depends on the thermal conductivities of the overlying formations (Table 1) and the regional surface heat flow.
The local isostatic consequences of this active faulting are instead superimposed onto this "background" of regional surface uplift.
Such combined heat and head monitoring at field sites is useful for calibrating regional surface-groundwater models.
The accelerated warming of the Arctic climate may alter the local and regional surface energy balances, for which changing land surface temperatures (LSTs) are a key indicator.
Hence, in order to supplement rain-fed agriculture by irrigation, a detailed understanding of local and regional surface water and groundwater resources is important.
Wind erosion processes in the typical temperate Xilingele grassland of North China result in significant regional surface soil fine particle and carbon loss.
On the basis of freely accessible regional surface meteorological data, this paper proposes a height-dependent linear correction model for a priori ZDD.
The study derives information from an analysis of seven deep boreholes, along with seismic surveys, regional surface geological mapping and hydrochemical and hydrogeological analysis.
The results of the work of Zubovich et al. (2010), analyzing the regional surface velocity field using GPS data, corroborate the inference that this basin might currently still rotate.
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