Snowfall

Let the snowflakes fall! Enjoy a cold-weather adventure in this updated classic from the author of Apples and Pumpkins. Snow falls and falls all through the night. And when morning comes, it’s time for fun! Watch the snowplows sweep the streets. Shovel walkways! Build a snowman! Sled! Ski! There are so many wonderful things to do in this magical snow-covered world! This updated edition of a wintry favorite includes new jacket art from Lizzy Rockwell and refreshed interior art and design.

Desperate to see the world beyond her grandfather's vicarage, sixteen-year-old Charlotte convinces her older brother to take her along on a mountain-climbing trip to Switzerland, where her life becomes intertwined with an assortment of people in Victorian society.

Snowfall Surprise (Candy Apple)

The Regional Snowfall Index, or RSI, is a numerical system developed by the National Oceanic and Atmospheric Administration (NOAA) in the United States to help quantify and compare the severity of snowstorms across different regions. The RSI takes into account several factors, including the amount of snowfall, the area affected, and the population density of the affected region. By using this index, meteorologists and emergency management officials can better prepare for and respond to snowstorms. The RSI is calculated on a scale of 1 to 5, with 5 being the most severe. A Category 1 snowstorm is considered a moderate event, affecting a relatively small area with limited population. A Category 5 snowstorm, on the other hand, is a major event affecting a large region with high population density and potentially catastrophic impacts. The RSI is a valuable tool for assessing and communicating the potential impacts of snowfall, allowing officials to make more informed decisions regarding resource allocation and emergency response.

The snowy winter of 1978 in Massachusetts allowed five opportunities to test the dependability of a CPS-9, 3.2-cm radar to determine snowfall rate and total snowfall accumulation at up to seven measuring sites within 50 km of the radar. Spaced at intervals of 0.5 -to 1-h, 166 snowfall-rate measurements yielded a correlation coefficient of 0.88. However, in correlating the total storm snowfall, the amount of radar-measured snowfall above a reference snowfall measurement site was made equal to the snowfall actually measured at this location. This calibration technique improved the storm snowfall correlation coefficient to 0.96.