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One of the basic properties of the atmosphere is that moisture increases with temperature.
Toward the south, moisture increases from 18 inches (460 mm) to a maximum of 80 inches (2,000 mm) annually, and the scrub forest gives way to tall trees.
In addition, higher simulated soil moisture increases estimated E/ET.
Furthermore, results of correlation analysis show that the topsoil moisture increases with the MTSFG decreases.
When the soil moisture increases, the interference signal's frequency may decrease or remain the same, while their phases increase.
By applying ethanol 70%, the moisture increases by ∼0.5% w.b., whereas applying temperature decreases moisture by ∼2% w.b.
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WPC and feed moisture increased redness, yellowness and decreased luminosity.
As temperature and moisture increased, loss of crystalline structure and degree of gelatinization also increased.
WPC and moisture increased crystallinity, but only WPC increased solubility and decrease the retrogradation tendency.
Generally, topographic influence on soil moisture increased with topographic variation (slope percent in this study).
As the antecedent moisture increased, the relative contribution of the season on DP increased from 0.0%to16.4%4%.
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