Two types of Cold Fronts
{"Image DocumentName": "Two types of Cold Fronts", "Image ImageDescription": "Anafront: A cold front breeds more precipitation when weak upper-level winds relative to stronger surface winds stretch the cold front out and the slope of the cold air becomes much less. This usually occurs when the upper-level winds become parallel to the front. Katafront: Some cold fronts produce very little or no precipitation as they move across the country. The only sign a front has moved through your area is a sudden change in winds and temperature.", "Image XResolution": "37", "Image YResolution": "37", "Image ResolutionUnit": "Pixels/Centimeter", "Image Software": "SlidePlayer", "Image YCbCrPositioning": "Centered"}