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The early Holocene was characterized by greater amounts of summer precipitation and less winter precipitation than modern.
By this period, summer precipitation is projected to decrease by 24 46% and annual precipitation by 14 23%.
Summer precipitation is 200 300 mm with annual precipitation approximately 1,500 mm for both.
Soil moisture levels were assessed over four periods after summer precipitation to examine soil moisture depletion.
We also found increased oak recruitment associated with fires that occurred in low summer precipitation years.
Redistribution was designed by subtracting 40% summer precipitation and adding to spring and fall.
The drip water Mg/Ca ratios were higher with decreased summer precipitation.
In most cases the summer precipitation recharges stream water via base flow.
Results indicate that the most important source of groundwater in the DLH comes from summer precipitation.
The drip water Mg/Ca ratios were significantly lower with increased summer precipitation.
"So in terms of real impacts, the lack of summer precipitation doesn't mean that much," Mass added.
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