1 00:00:02,040 --> 00:00:06,720 Speaker 1: Welcome to brain Stuff from How Stuff Works, Pay brain 2 00:00:06,760 --> 00:00:11,440 Speaker 1: Stuff Lauren Vogelbaum. Here. You might remember when in Republican 3 00:00:11,520 --> 00:00:14,440 Speaker 1: Senator James Inhoff of Oklahoma set out to refute the 4 00:00:14,560 --> 00:00:18,360 Speaker 1: quote hysteria over global warming by tossing a snowball around 5 00:00:18,360 --> 00:00:22,239 Speaker 1: inside the US capital. The obvious implication was, how could 6 00:00:22,239 --> 00:00:25,200 Speaker 1: the climate be changing that radically from humans burning fossil 7 00:00:25,239 --> 00:00:28,400 Speaker 1: fuels and pumping greenhouse gases into the atmosphere, since we 8 00:00:28,480 --> 00:00:31,640 Speaker 1: still have snowfall and chilly temperatures on a winter day. 9 00:00:32,120 --> 00:00:34,440 Speaker 1: But even if you're not a U. S. Senator from 10 00:00:34,479 --> 00:00:37,360 Speaker 1: an oil producing state, you might be wondering how it 11 00:00:37,440 --> 00:00:40,479 Speaker 1: is that scientists can predict climate trends over many years 12 00:00:40,680 --> 00:00:42,800 Speaker 1: but can't predict what the weather will be three weeks 13 00:00:42,800 --> 00:00:46,320 Speaker 1: from today. The reason is that weather and climate are 14 00:00:46,320 --> 00:00:50,040 Speaker 1: two very different things. Basically, whether it is what happens 15 00:00:50,080 --> 00:00:52,640 Speaker 1: today or tomorrow or this week, it's the day to 16 00:00:52,720 --> 00:00:56,840 Speaker 1: day variations. Climate, meanwhile, happens over many years. It's the 17 00:00:56,880 --> 00:01:01,160 Speaker 1: combined long term average of weather events. Scientists look at 18 00:01:01,160 --> 00:01:04,680 Speaker 1: climate in terms of fixed thirty year periods. Right now, 19 00:01:04,720 --> 00:01:07,880 Speaker 1: for example, scientists are comparing the daily temperature to the 20 00:01:08,040 --> 00:01:13,080 Speaker 1: period that started in nineteen eighty one and ended in one. 21 00:01:13,200 --> 00:01:16,120 Speaker 1: They'll shift forward ten years and start comparing temperatures to 22 00:01:16,120 --> 00:01:21,160 Speaker 1: the period between nine and twenty and so on. Scientists 23 00:01:21,160 --> 00:01:23,399 Speaker 1: rely on thirty year periods because it's an amount of 24 00:01:23,440 --> 00:01:26,360 Speaker 1: time that's long enough to produce meaningful comparisons, but just 25 00:01:26,400 --> 00:01:29,040 Speaker 1: short enough that any changes that occur will be subtle 26 00:01:29,280 --> 00:01:32,800 Speaker 1: without being imperceptible. Twenty years might not show enough change, 27 00:01:32,959 --> 00:01:35,360 Speaker 1: and fifty years might be too drastic. To make sense 28 00:01:35,360 --> 00:01:38,640 Speaker 1: of those, thirty year periods help us put the weather 29 00:01:38,680 --> 00:01:41,840 Speaker 1: on a particular day in the right context. Comparing the 30 00:01:41,920 --> 00:01:45,520 Speaker 1: temperature on December to the same day a hundred years 31 00:01:45,560 --> 00:01:48,680 Speaker 1: ago wouldn't provide that much useful information because the climate 32 00:01:48,720 --> 00:01:51,400 Speaker 1: was too different then, but comparing it to the average 33 00:01:51,400 --> 00:01:53,960 Speaker 1: of the temperature readings for every December five between nine 34 00:01:54,560 --> 00:01:57,720 Speaker 1: and twenty ten, when the climate conditions were pretty much constant, 35 00:01:58,040 --> 00:02:00,280 Speaker 1: makes it possible to say whether a given to number 36 00:02:00,320 --> 00:02:04,440 Speaker 1: five is an unusually cold or warm day. We spoke 37 00:02:04,440 --> 00:02:07,760 Speaker 1: with Jonathan Martin, a professor of atmospheric and oceanic studies 38 00:02:07,800 --> 00:02:11,560 Speaker 1: at the University of Wisconsin Madison. He explained or trying 39 00:02:11,560 --> 00:02:15,359 Speaker 1: to compare apples to apples when it comes to prediction. 40 00:02:15,520 --> 00:02:19,799 Speaker 1: Whether in climate are also very different. Weather forecasting, Martin explains, 41 00:02:20,040 --> 00:02:23,079 Speaker 1: is based upon observation of conditions that are already occurring 42 00:02:23,160 --> 00:02:26,560 Speaker 1: in real time in the atmosphere. Because those conditions only 43 00:02:26,600 --> 00:02:29,240 Speaker 1: exist for a short time, whether it can be reliably 44 00:02:29,280 --> 00:02:32,760 Speaker 1: forecast only over relatively short periods of ten to fourteen 45 00:02:32,840 --> 00:02:36,919 Speaker 1: days at most, though Martin said that's theoretical, My confidence 46 00:02:37,000 --> 00:02:40,679 Speaker 1: ends at day eight. Envisioning climate, in contrast, is much 47 00:02:40,680 --> 00:02:43,840 Speaker 1: more low resolution. Scientists are trying to project what the 48 00:02:43,840 --> 00:02:46,000 Speaker 1: trend will be over a long period, not what the 49 00:02:46,040 --> 00:02:48,359 Speaker 1: weather will be like on a specific day fifty or 50 00:02:48,400 --> 00:02:51,720 Speaker 1: a hundred years from now. That involves gathering and crunching 51 00:02:51,880 --> 00:02:55,200 Speaker 1: huge amounts of data in powerful computers and doing modeling. 52 00:02:56,200 --> 00:02:58,920 Speaker 1: We also spoke with Jeffrey S. Duke's director of the 53 00:02:58,960 --> 00:03:02,800 Speaker 1: Climate Change Research Center at Purdue University. He said, in 54 00:03:02,880 --> 00:03:06,320 Speaker 1: one sense, climate does not affect weather. It's a description 55 00:03:06,360 --> 00:03:08,880 Speaker 1: of the weather over a long period. You could turn 56 00:03:08,880 --> 00:03:11,239 Speaker 1: that around and say that climate provides you with information 57 00:03:11,240 --> 00:03:13,200 Speaker 1: about how likely you are to get a given type 58 00:03:13,240 --> 00:03:15,840 Speaker 1: of weather at a given time of year. But historically 59 00:03:16,040 --> 00:03:18,959 Speaker 1: the climate has been determined by the weather over long periods. 60 00:03:19,960 --> 00:03:23,200 Speaker 1: He continued In another sense, though, climate for a given 61 00:03:23,240 --> 00:03:26,000 Speaker 1: location is determined by a bunch of factors, such as 62 00:03:26,040 --> 00:03:28,840 Speaker 1: the latitude and position on the planet, which affects how 63 00:03:28,840 --> 00:03:31,880 Speaker 1: it is influenced by the circulation of the atmosphere and oceans, 64 00:03:31,880 --> 00:03:35,320 Speaker 1: and the daytime heating of continents. Climate is also influenced 65 00:03:35,320 --> 00:03:37,920 Speaker 1: by the composition of the atmosphere, the transport of water 66 00:03:38,040 --> 00:03:41,640 Speaker 1: from soil to air by plants, and other factors. On 67 00:03:41,680 --> 00:03:44,960 Speaker 1: a given day, the sum of all these influences determines 68 00:03:45,040 --> 00:03:47,760 Speaker 1: the weather, but as some of these larger scale factors 69 00:03:47,840 --> 00:03:50,560 Speaker 1: change over time, they will drag the weather and the 70 00:03:50,600 --> 00:03:54,840 Speaker 1: climate along with them. In recent years, some of the 71 00:03:54,840 --> 00:03:58,240 Speaker 1: sharp distinction between weather and climate has blurred slightly as 72 00:03:58,240 --> 00:04:02,200 Speaker 1: scientists have used increasingly phisticated models and accumulated knowledge in 73 00:04:02,280 --> 00:04:04,360 Speaker 1: an effort to figure out the extent to which some 74 00:04:04,520 --> 00:04:07,520 Speaker 1: specific weather events, say a hurricane, a heat wave, or 75 00:04:07,560 --> 00:04:11,000 Speaker 1: a monster snowstorm, is actually a function of climate change 76 00:04:11,200 --> 00:04:15,280 Speaker 1: driven by humans releasing greenhouse emissions into the atmosphere. By 77 00:04:15,320 --> 00:04:19,200 Speaker 1: running thousands of computer simulations, they can conduct what if experiments, 78 00:04:19,400 --> 00:04:22,000 Speaker 1: seeing how the atmosphere would behave if you removed one 79 00:04:22,080 --> 00:04:25,599 Speaker 1: factor or another. Although such analysis is still a work 80 00:04:25,600 --> 00:04:28,799 Speaker 1: in progress, Martin thinks that eventually it will be possible 81 00:04:28,839 --> 00:04:31,440 Speaker 1: to determine the extent to which specific weather events are 82 00:04:31,480 --> 00:04:34,920 Speaker 1: influenced by climate change. Some of that research is already 83 00:04:34,920 --> 00:04:38,920 Speaker 1: bearing results. The National Oceanic and Atmospheric Administration presented a 84 00:04:38,960 --> 00:04:42,680 Speaker 1: paper in December in which they concluded that three extreme 85 00:04:42,720 --> 00:04:46,640 Speaker 1: weather events in that year's record global heat, extreme heat 86 00:04:46,720 --> 00:04:49,520 Speaker 1: over Asia, and unusually warm waters in the Bearing Sea 87 00:04:49,839 --> 00:04:52,680 Speaker 1: would not have been possible without human caused climate change. 88 00:04:57,800 --> 00:05:00,480 Speaker 1: Today's episode was written by Patrick J. Keiger and produced 89 00:05:00,480 --> 00:05:02,719 Speaker 1: by Tyler Clang. For more on this and lots of 90 00:05:02,720 --> 00:05:05,679 Speaker 1: other stormy topics, visit our home planet, how stuff Works 91 00:05:05,760 --> 00:05:16,960 Speaker 1: dot com. M