Sentence examples for wetness condition from inspiring English sources

The hydrological controls, however, are the effective rainfall that reflects the antecedent wetness condition of the catchment which was calculated from the determined catchment curve number (CN).

Soil depth and wetness condition did not appear to affect the selection of kriging for soil moisture interpolation, because they did not significantly change the ratio of sample spacing over correlation range and the relationship with the auxiliary variables.

Interestingly, we found that for 9 out of the 11 paired hillslopes, 40 70% of the temporal variation in the scaling factors can be explained by the antecedent wetness condition and the maximum hourly rain accumulation.

"On a scale of wetness conditions," Femia and Werrell note, " 'where a reading of -4 or below is considered extreme drought,' a 2010 report by the National Center for Atmospheric Research shows that Syria and its neighbors face projected readings of -8 to -15 as a result of climatic changes in the next 25 years".

Plant species that inhabit these environments integrate responses to broadly fluctuating wetness conditions.

The topographic wetness index (TWI) has become a widely used tool to describe wetness conditions at the catchment scale.

Conceptual models describing salt and water movement through the different landforms and under different antecedent catchment wetness conditions are presented.

The paper assess the effectiveness of the approach applied to monthly means of temperature and rainfall, to predict soil wetness conditions.

Three temporal scales (half-hourly, daily, and 10-days) and three time periods corresponding to typical soil wetness conditions, including frozen soil in winter times, are discussed.

The seasonal variation in contribution can be attributed into differences in soil wetness conditions; lower contribution was found at intermediate wetness for spatial variances of temporal mean and temporal anomalies.

In the forest stream, elevated DOC concentrations (max: 3.5 mgC l−1) during precipitation events were due to hydrologic flushing of soluble organic matter in upper soil horizons, with a strong dependency on pre-storm wetness conditions.