Sentence examples for moisture statistics from inspiring English sources

This paper develops a conceptual and analytical framework for linking hydro-climatic change at the surface and soil-groundwater conditions in the subsurface, and quantifying long-term development of soil moisture statistics in a changing climate.

Moreover, climate related "bioclimatic" variables could be calculated (e.g. rates of evapotranspiration, soil moisture availability, extreme climate statistics, plant hardiness measures, etc)., which act as metrics or surrogates for more specific climate-change mediated processes.

The probability distribution of the soil moisture deficit, i.e., statistics of topography, is generated from digital elevation model data by using a multidirectional flow routing algorithm, which is tied to an adaptive error correction (pit infill) scheme needed for low-relief areas such as coastal plains.

TOPMODEL formulations permit dynamically consistent calculations of both the saturated fraction within the watershed (partial contributing area) and the groundwater flow that supports this area, from knowledge of the mean depth of the water table and a probability density function for soil moisture deficit derived from topographic statistics.

The severity level of the soil moisture state is computed after comparison with long term statistics derived from a long term simulation.

One can define new Soil Moisture Accounting models, routing models, calibration methods, objective functions, and evaluation statistics, while retaining as much of the default framework as is useful.

Nevertheless, the Cuauhtemoc la Fragua Douglas fir chronology has a strong moisture signal for the past 500 years in spite of the weak verification statistics (14, 18 ).

We used descriptive statistics and Bayesian geostatistical models to quantify and compare the plant community and soil properties (soil moisture, organic carbon concentration, total microbial abundance, and electrical conductivity) across plots.

Exploratory statistics were used to identify 12 field characteristics that would be useful in determining the spatial distribution of soil moisture, including terrain features (slope and elevation), soil physical and chemical properties and geoelectric measurements (EC for each date).

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