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In addition to the welcome snow and rain that March brought to the Tehachapi area, the third month of 2006 was also the coldest of the winter, with colder overnight lows than December, January or February.Just a few degrees difference in temperature makes a profound difference in our weather: only two or three degrees Fahrenheit one way or the other will determine whether a storm brings rain or snow, whether Highway 58 will be open or closed, it will determine whether we have dew or frost, and that small margin will even decide if fruit blossoms survive to produce fruit in the summer and fall.Tehachapi spring storms tend to balance right on the margin, veering between snowy rain or rainy snow, sometimes warming into straight rain and other times cooling into pure snow.After one of these recent hybrid storms on March 21, the temperature dropped just to freezing in the night and produced ice at the surface, though the soil didn’t freeze and there was still liquid water beneath...
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