WEBVTT FILE 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.