salmonoid wrote:
Chaz wrote:
It shows the value of snow pack and or spring run-off. There is on run-off as yet and there certainly is no snow pack.
The effect of "snow pack" on surface water in Pennsylvania is exaggerated, I think. This is not the west, where vast reaches are normally covered in deep snow at high elevations and where the melt is potentially a slow, long melt. Snow in PA is only about 10% of the liquid that falls.
A few feet of compacted snow is still just a few inches of liquid. It adds a bit to the flow rate of streams, but the bulk comes from rain and runoff it creates. There is some truth to late spring and late fall being a time of groundwater recharge. Ground is not frozen and plants are not suckling up the water during both those time frames, so snow melt can end up in the ground.
What we are seeing now in many streams are base groundwater flows, which are normally masked by runoff from April showers.