12/9/2023 0 Comments New york city snowfall totals![]() The biggest similarity between all of the above states is that from one end to another there is a dramatic geological change. The states with the greatest amount of variation, ones where the snowfall at least doubles, include For example, in Maryland, the coast only has 10 inches of snowfall, whereas the western half sees 7x that. On the other hand, we have states that have aggressive variations in how much snow can fall from one end to another. While there are two peaks that can experience frequent winter storms, the entire rest of the state sees little to no snowfall. It’s always so warm in Florida that even if it snows, there will not be much, and it will melt almost immediately. If it were to snow in Florida, it’s in very particular and rare conditions, and it is unlikely that any will stay on the ground as prolonged freezing temperatures are required for snow not to melt upon impact. These states includeĭue to its location, climate, and shape, the state of Florida sees an average of almost no snow or 0.01 inches. With that in mind, we have excluded two states from the region calculation because there was almost no data to report. Since we are talking about states with snow, it makes sense that some states, specifically southern ones, will have either no data or strange data to relate. Note: The table with regional data included is the only one that takes days of snowfall and any median into account. These figures tell very different stories because there is heavy snowfall in the eastern half of Northern California and very little on the west coast, but just relaying the average would give an incredibly distorted picture of what to expect come winter. For example, in Northern California, there is an annual average snowfall of 14.3 inches, but there is a median of 0.7 inches. Medians are helpful because they give a better representation of the figures that occur the most, where averages can be swayed by less large values. This same direction is taken when you only have two figures to compare. If you have an even number of figures, you will find the average of the two in question. That way, whether you are packing for a trip or thinking about relocating, you will have a better idea of what your winter days could look like.įor context, the median is found when you take all the figures, line them up from least to greatest, and select the one that is perfectly in the middle. To counter possible inaccuracies and false expectations, we included a table that holds the average and median of both the days per year it snows, but also the inches. ![]() The issue arises when the state is massive and has many varying regions and varying amounts of snow in each region. In general, this is a perfectly effective strategy for predicting snowfall in a state. The average snowfall is measured by taking the averages of each region, adding them together, and dividing the sum by how many region averages were initially used. We take that into account by looking both at the average per state, but also the average and median per region. As you will see with many large states, some areas get much more snow than others. For example, Arizona is a very large state with extreme variance in climate, ecosystems, and elevation from one end to another. Moisture is a huge factor in snow production which means that sometimes states experience conditions that can be too cold for snow.Īverage snowfall is calculated to represent what anyone in the state can expect to experience over the course of winter, but that isn’t exactly accurate, especially when discussing any state that has either large or distinct regions. You might think that the states with reputations for being the coldest would also be the snowiest, but that’s not the case. Storms will get their start over the Great Lakes and then pass all the way from Minnesota to Maine. Because moisture is an essential element needed to form clouds and snow, very cold air blows across a large, warmer body of water, causing a large snowstorm. The flakes that become the largest move down through air slightly warmer than 0℃ and stick to even more ice crystals.Ī lot of heavy snowfalls occur around the Great Lakes region due to something called the lake effect. ![]() Another way snow falls is through the collection of tiny ice crystals that eventually stick together, becoming heavy enough to fall to the ground. Most storms are born from a phenomenon called “frontal lifting,” where a warm and cold airmass collide, causing two different events, 1) due to the lesser density of the warm air, it’s pushed up and over the mass of cool air and 2) essentially freeze-drying the moisture in the warm air, creating snow.
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