1 00:00:01,890 --> 00:00:06,870 Clouds. They seem so simple. When they appear darker we pack 2 00:00:06,870 --> 00:00:10,260 an umbrella. When they're nowhere in sight, we pack extra 3 00:00:10,260 --> 00:00:15,180 sunscreen. Either way, we look to clouds for more information 4 00:00:15,210 --> 00:00:18,960 than you might realize. But for all that they can tell us they 5 00:00:18,960 --> 00:00:22,440 actually remain quite mysterious, especially when it 6 00:00:22,440 --> 00:00:27,030 comes to how they impact the climate. The question is because 7 00:00:27,030 --> 00:00:30,300 clouds are produced by the climate, how will it change in 8 00:00:30,300 --> 00:00:34,230 climate impact clouds? And conversely, clouds have an 9 00:00:34,230 --> 00:00:38,100 impact on our climate. So how will a change in clouds affect a 10 00:00:38,100 --> 00:00:38,940 change in climate? 11 00:00:39,800 --> 00:00:46,460 Welcome to Clouds 101. Like all good mysteries, this one begins 12 00:00:46,460 --> 00:00:50,330 with a sophisticated scientific concept, Earth's radiation 13 00:00:50,330 --> 00:00:54,830 budget. Earth's radiation budget describes the delicate balance 14 00:00:54,830 --> 00:00:58,160 between the sun's radiant energy that reaches Earth, and the 15 00:00:58,160 --> 00:01:01,940 radiant energy that flows from Earth back out to space. About 16 00:01:01,970 --> 00:01:05,990 30% of the sun's incoming energy, essentially, the light 17 00:01:05,990 --> 00:01:09,410 and heat we're familiar with is reflected back to space by 18 00:01:09,410 --> 00:01:12,200 gaseous molecules in the atmosphere, tiny particles 19 00:01:12,200 --> 00:01:17,480 called aerosols, land, snow and ice surfaces, and by clouds. The 20 00:01:17,480 --> 00:01:21,860 remaining energy from the sun, roughly 70%, is absorbed by the 21 00:01:21,860 --> 00:01:25,970 planet. Most of this absorbed energy heats up Earth's surface, 22 00:01:25,970 --> 00:01:29,360 while the rest is absorbed in the atmosphere by gas molecules, 23 00:01:29,360 --> 00:01:34,280 clouds, and aerosols. So heat can be both absorbed and 24 00:01:34,280 --> 00:01:39,020 reflected by clouds. We'll come back to this later. Heat is also 25 00:01:39,020 --> 00:01:42,950 separately emitted by earth into space in the form of thermal 26 00:01:42,950 --> 00:01:46,970 infrared radiation, which is the kind of heat humans can only see 27 00:01:46,970 --> 00:01:50,600 through night vision goggles. For Earth's temperature to 28 00:01:50,600 --> 00:01:54,710 remain constant, the absorbed solar radiation and outgoing 29 00:01:54,710 --> 00:01:58,760 thermal infrared radiation must balance one another. If the 30 00:01:58,760 --> 00:02:01,850 Earth's system is changed, either through natural phenomena 31 00:02:01,850 --> 00:02:05,570 like volcanic activity, or through unnatural phenomena like 32 00:02:05,570 --> 00:02:09,680 humans burning fossil fuels, an imbalance in Earth's radiation 33 00:02:09,680 --> 00:02:13,190 budget occurs, and as a result, the earth's temperature 34 00:02:13,220 --> 00:02:16,730 eventually increases or decreases to restore an energy 35 00:02:16,730 --> 00:02:20,930 balance. In recent decades, satellite and surface 36 00:02:20,930 --> 00:02:24,410 measurements clearly show an energy imbalance taking place 37 00:02:24,410 --> 00:02:29,330 that's been increasing. Over the past 150 years. The large rise 38 00:02:29,330 --> 00:02:32,120 in carbon dioxide emissions, which accumulate in the 39 00:02:32,120 --> 00:02:35,960 atmosphere, has created an enhanced greenhouse effect. This 40 00:02:35,960 --> 00:02:39,770 means that energy from the sun still easily reaches Earth, but 41 00:02:39,800 --> 00:02:42,710 Earth's thermal infrared radiation has a harder time 42 00:02:42,710 --> 00:02:47,150 getting out into space. This has caused a decrease in how much 43 00:02:47,150 --> 00:02:51,320 heat Earth sheds. Consequently, we have observed a rise in 44 00:02:51,320 --> 00:02:54,230 Earth's global mean surface temperature, an increased 45 00:02:54,230 --> 00:02:58,580 melting of snow and sea ice, sea level rise, and more extreme 46 00:02:58,580 --> 00:03:01,910 weather events. So that brings us back to the mystery of 47 00:03:01,910 --> 00:03:06,110 clouds' long term effects on climate. Here's what we know so 48 00:03:06,110 --> 00:03:10,790 far. Clouds impact the radiation budget in two ways: by 49 00:03:10,790 --> 00:03:14,270 reflecting solar radiation back to space, which leads to a 50 00:03:14,270 --> 00:03:18,620 cooling effect on the climate, and by absorbing heat emitted 51 00:03:18,620 --> 00:03:21,800 from below the clouds that would have otherwise escaped to space 52 00:03:21,800 --> 00:03:24,950 if the clouds weren't present, leading to a warming effect. 53 00:03:25,910 --> 00:03:29,360 Which of these effects dominates in any given location depends 54 00:03:29,360 --> 00:03:33,020 upon the cloud type. High altitude clouds are typically 55 00:03:33,020 --> 00:03:36,890 thinner and colder than low clouds, allowing for more solar 56 00:03:36,890 --> 00:03:40,340 radiation to pass through them and reach Earth's surface. And 57 00:03:40,340 --> 00:03:43,520 because they're cooler, they emit less thermal infrared 58 00:03:43,520 --> 00:03:46,760 radiation to space, so they have a net warming effect on the 59 00:03:46,760 --> 00:03:50,060 climate. Clouds at low altitudes, on the other hand, 60 00:03:50,090 --> 00:03:53,570 are generally thicker and reflect more solar radiation 61 00:03:53,570 --> 00:03:58,040 back out to space. They're also typically warmer, so they emit 62 00:03:58,040 --> 00:04:01,490 more thermal infrared radiation and therefore have a net cooling 63 00:04:01,490 --> 00:04:05,420 effect on the climate. We also know that when the climate 64 00:04:05,420 --> 00:04:09,200 warms, Earth can respond in ways that leads to further warming. 65 00:04:09,620 --> 00:04:13,310 For example, as temperatures increase, we see snowpack and 66 00:04:13,310 --> 00:04:16,880 sea ice melting away in polar regions, a loss of white 67 00:04:16,880 --> 00:04:20,840 surfaces that reflect the solar radiation. That means darker 68 00:04:20,840 --> 00:04:24,140 colored land and oceans left behind absorb more solar 69 00:04:24,140 --> 00:04:27,800 radiation, and so more heat is added to the climate system. 70 00:04:28,400 --> 00:04:32,450 This cycle of more heat, more melt and more absorption of 71 00:04:32,450 --> 00:04:36,410 solar radiation is called a feedback cycle. And it doesn't 72 00:04:36,410 --> 00:04:41,960 end there. A feedback cycle also happens with clouds. Climate 73 00:04:41,960 --> 00:04:45,620 models predict a decrease in low altitude cloud coverage over the 74 00:04:45,620 --> 00:04:49,340 globe as the climate warms, since low clouds are the highly 75 00:04:49,340 --> 00:04:53,330 reflective type, a decrease in low cloud coverage means more 76 00:04:53,330 --> 00:04:56,000 heat will be added to the Earth's system, leading to 77 00:04:56,000 --> 00:04:59,870 further warming. And clouds impact the climate in another 78 00:04:59,870 --> 00:05:04,430 way too: Through the water cycle producing rain and snowfall. 79 00:05:05,120 --> 00:05:08,180 Water at Earth's surface evaporates, providing the 80 00:05:08,180 --> 00:05:11,690 atmosphere with a supply of water vapor. Depending on the 81 00:05:11,690 --> 00:05:15,440 air temperature and atmospheric pressure, the air can only hold 82 00:05:15,440 --> 00:05:19,790 so much water vapor until it becomes saturated. When that air 83 00:05:19,790 --> 00:05:23,330 saturated with water vapor cools, the water vapor turns 84 00:05:23,330 --> 00:05:26,360 back into liquid water droplets and forms clouds. 85 00:05:27,930 --> 00:05:31,436 When these droplets or ice crystals accumulate, that is 86 00:05:31,500 --> 00:05:35,453 what we call a cloud. When the droplets or ice crystals within 87 00:05:35,516 --> 00:05:39,214 the cloud grow to be large enough, they eventually fall to 88 00:05:39,278 --> 00:05:42,912 the ground or ocean as rain, snow or hail. This brings us 89 00:05:42,976 --> 00:05:46,801 back to the mystery at hand. Because clouds both reflect and 90 00:05:46,865 --> 00:05:50,244 absorb energy from the sun impacting both ends of the 91 00:05:50,308 --> 00:05:54,197 radiation balance and play a massive role in the water cycle, 92 00:05:54,261 --> 00:05:57,576 any changes in clouds will result in a change in our 93 00:05:57,640 --> 00:06:01,465 climate. But clouds are also produced by our climate, so any 94 00:06:01,529 --> 00:06:05,290 change in climate will result in a change in clouds. As you 95 00:06:05,354 --> 00:06:08,924 probably now realize the relationship between clouds and 96 00:06:08,988 --> 00:06:12,240 the climate is incredibly complex, and NASA is on a 97 00:06:12,303 --> 00:06:16,320 mission to understand it. Using NASA's Earth Observing fleet of 98 00:06:16,384 --> 00:06:19,827 satellites like Calipso and instruments like Ceres and 99 00:06:19,890 --> 00:06:23,652 MODIS, scientists have been collecting vital data on clouds 100 00:06:23,716 --> 00:06:27,669 to be able to precisely model their behavior. A key ingredient 101 00:06:27,732 --> 00:06:31,621 to unraveling the mystery of clouds lies in the collection of 102 00:06:31,685 --> 00:06:35,447 global accurate multi decadal climate data records of cloud 103 00:06:35,511 --> 00:06:39,272 properties and their influence on Earth's radiation budget. 104 00:06:39,336 --> 00:06:43,480 Once we can accurately and fully understand the physics of clouds 105 00:06:43,544 --> 00:06:47,624 through observations, that data can then be used to help improve 106 00:06:47,688 --> 00:06:51,960 climate and weather models so we can better prepare for the future.