1 00:00:00,520 --> 00:00:03,840 Speaker 1: Welcome to Brainstuff from house stuff works dot com where 2 00:00:03,840 --> 00:00:08,600 Speaker 1: smart happens. Hi Am Marshall Brain with today's question, if 3 00:00:08,600 --> 00:00:12,399 Speaker 1: the temperature is thirty degrees fahrenheit outside, why do we 4 00:00:12,560 --> 00:00:16,360 Speaker 1: sometimes get snow and other times we get freezing rain. 5 00:00:17,239 --> 00:00:20,040 Speaker 1: When you watch the local weather report on the evening news, 6 00:00:20,120 --> 00:00:24,360 Speaker 1: you always hear the current temperature. It may be, for example, 7 00:00:24,480 --> 00:00:29,040 Speaker 1: thirty two degrees fahrenheit or zero degrees celsius outside. That's 8 00:00:29,240 --> 00:00:33,200 Speaker 1: useful information, but if it's precipitating, it is only one 9 00:00:33,320 --> 00:00:36,760 Speaker 1: part of the puzzle. It turns out that the atmosphere 10 00:00:36,960 --> 00:00:41,080 Speaker 1: is layered, and these layers control the form that precipitation 11 00:00:41,120 --> 00:00:44,600 Speaker 1: will take on the ground. The local weather report only 12 00:00:44,680 --> 00:00:49,519 Speaker 1: gives us the ground level temperature. In order to understand sleet, snow, 13 00:00:49,600 --> 00:00:53,400 Speaker 1: and freezing rain. What we need to know is perhaps 14 00:00:53,479 --> 00:00:58,880 Speaker 1: four to six different temperature readings at different altitudes. Precipitation 15 00:00:59,080 --> 00:01:02,760 Speaker 1: starts in the cloud as snow. As it falls, it 16 00:01:02,880 --> 00:01:05,120 Speaker 1: may travel through a layer of air that has a 17 00:01:05,160 --> 00:01:09,640 Speaker 1: temperature greater than thirty two degrees fahrenheit. This layer melts 18 00:01:09,720 --> 00:01:13,120 Speaker 1: the snow into rain. If the temperature at ground level 19 00:01:13,280 --> 00:01:16,520 Speaker 1: is below freezing, then the water may refreeze in the 20 00:01:16,560 --> 00:01:19,800 Speaker 1: air and then we get sleep. Or if the layer 21 00:01:19,840 --> 00:01:23,440 Speaker 1: of subfreezing air at ground level is thin, the precipitation 22 00:01:23,600 --> 00:01:26,720 Speaker 1: falls as rain, but then it freezes once it touches 23 00:01:26,760 --> 00:01:30,080 Speaker 1: the freezing object on the ground. For snow to fall, 24 00:01:30,600 --> 00:01:33,480 Speaker 1: all the layers of air that the snow falls through 25 00:01:33,600 --> 00:01:37,560 Speaker 1: once it leaves the cloud must be sub freezing. The 26 00:01:37,640 --> 00:01:40,840 Speaker 1: warm middle layers are normally caused by the movement of 27 00:01:40,920 --> 00:01:45,040 Speaker 1: warm fronts or cold fronts through the area. In the southeast, 28 00:01:45,160 --> 00:01:48,560 Speaker 1: temperatures often hover around thirty two degrees Fahrenheits, so the 29 00:01:48,600 --> 00:01:51,960 Speaker 1: form of precipitation can change all the time. In more 30 00:01:52,040 --> 00:01:55,680 Speaker 1: northern areas, the temperature is well below freezing in all 31 00:01:55,800 --> 00:02:00,200 Speaker 1: the layers, so snow is a sure thing. You have 32 00:02:00,240 --> 00:02:03,920 Speaker 1: any ideas or suggestions for this podcast, If so, please 33 00:02:03,920 --> 00:02:06,640 Speaker 1: send me an email at podcast at how stuff works 34 00:02:06,680 --> 00:02:09,760 Speaker 1: dot com. For more on this and thousands of other topics, 35 00:02:09,800 --> 00:02:12,679 Speaker 1: go to how stuff works dot com and be sure 36 00:02:12,680 --> 00:02:14,720 Speaker 1: to check out the brain stuff blog on the how 37 00:02:14,800 --> 00:02:16,320 Speaker 1: stuff works dot com home page.