To place the current study in the context of Holocene moisture evolution across the Tibetan Plateau, we applied a five-scale moisture index and average link clustering to all available continuous palaeo-climate records from the Tibetan Plateau to possibly find general patterns of moisture evolution on the Plateau.
The GRNN models could automatically determine the best smoothing parameters, which were 0.6 and 0.3 for predicting the moisture content and average temperature, respectively.
For random network designs, we develop a simple model that can be used to estimate the sampling uncertainty (expressed as standard deviation of sampling error as a percentage of the areal mean soil moisture) as a function of the number of sensors, mean soil moisture content and averaging area.
The model with initial steam condensation was found to be able to predict the center temperature and average moisture content of the product undergoing LPSSD very well.
The latexes were characterized regarding solids content with a HR73 Halogen Moisture Analyzer (Mettler Toledo) and average particle size (intensity-weighted diameter) with a Nicomp particle sizer (PSS Santa Barbara, USA) at a fixed scattering angle of 90°.
To solve this problem, a soil moisture disaggregation algorithm based on thermal inertia relationship between daily temperature change and average soil moisture modulated by vegetation conditions has been formulated.
The predicted temperature and average moisture-content profiles with respect to time were in good agreement with some experimental data from the literature.
The correlation (r2) between the first principal component (PC1) of multi-temporal C-HH SAR data and average soil moisture was 0.88 (p = < .0001) during the leaf-off season and 0.87 (p = < .0001) during the leaf-on season, while the correlation between PC1 and average percent area inundated was 0.82 (p = < .0001) and 0.47 (p = .0016) during the leaf-off and leaf-on seasons, respectively.
The corn stover was approximately 3 months old with an initial moisture content of 11.6% and average cross-section diameter of around 18 mm.
Representative point measurements were used to estimate the watershed scale (∼25 km) soil moisture average and shown to be accurate indicators with low variance and bias of the watershed scale soil moisture distribution.
