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Most of this hydrographic system is dry (Fig. 2), except during snowmelt or following exceptional rainfall.
Episodic acidification during snowmelt is a natural phenomenon that can be intensified by acidic deposition from heavy industry.
The year-to-year variation in these processes determines the stream response to clear-cutting during snowmelt.
A second model of the volume of inflow during snowmelt constrained the magnitude of seasonal variability in isotopic composition.
By considering surface subsurface hydrologic response during snowmelt, we demonstrate the importance of accurately characterizing the hydraulic conductivity.
We show how peatland characteristics dampen the effect of intense rain, and how soil freeze-thaw processes regulate surface and groundwater partitioning during snowmelt.
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Typically, the creek and its tributaries are not at risk of becoming too acidic for the optimal health of fish, but in early spring during snowmelts, the levels approach the limit that brook trout can tolerate.
Trends analysis of maximum and minimum streamflow indicates a strong (>+50%) and statistically significant increase in 11-day flow events during the late fall/winter and during the snowmelt period (late April/mid-May), followed by a significant decrease in the 11-day flow events during the post-snowmelt period (late May and into the summer).
The low-salinity areas formed along the coast of the bay and were less saline during the snowmelt period (March to April) than during early summer May too June).
The highest monthly solute gross yields over the year (comprising 43% of the total annual solute gross yield) are recorded in the spring period (three-month period from April to June), which is due to high runoff during spring snowmelt and comparably higher TDS values than during major glacier melt in summer (July August).
Elevated concentrations occurred during intensive snowmelt events.
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CEO of Professional Science Editing for Scientists @ prosciediting.com