1 00:00:00,000 --> 00:00:21,520 Hi, I'm Sean O'Keefe, I'm the Administrator of the National Aeronautics and Space Administration, 2 00:00:21,520 --> 00:00:24,320 and also the father of three kids. 3 00:00:24,320 --> 00:00:31,640 I'm excited by the opportunities that we can provide from NASA to inspire that next generation of explorers. 4 00:00:31,640 --> 00:00:36,880 Matter of fact, I'm here at Belmont Ridge Middle School to lend a hand on a NASA Connect activity. 5 00:00:36,880 --> 00:00:43,360 NASA Connect lets viewers experience the exciting and important work that engineers, scientists, and technicians do every day. 6 00:00:43,360 --> 00:00:51,080 Work that's about the future, and for which you, our next generation, will have the opportunity to pick up and carry to new heights and possibly other planets. 7 00:00:51,080 --> 00:00:56,840 There are many hands-on and web-based activities from NASA Connect that the family can do together at home. 8 00:00:56,840 --> 00:01:00,840 I encourage you to learn more about those activities in today's program. 9 00:01:00,840 --> 00:01:05,480 On this episode of NASA Connect, you'll learn how weather affects our daily lives. 10 00:01:05,480 --> 00:01:14,640 You'll see national and international scientists using satellite technology to help improve weather forecasting and improve our ability to predict long-term climate change. 11 00:01:14,640 --> 00:01:20,440 You'll also be introduced to two NASA satellite Earth science missions, CloudSat and Calypso. 12 00:01:20,440 --> 00:01:26,800 In your home or classroom, you will apply math, science, and technology concepts with two really cool activities. 13 00:01:26,800 --> 00:01:30,800 All in this episode of NASA Connect, the A-Train Express. 14 00:01:30,800 --> 00:01:59,800 Music 15 00:01:59,800 --> 00:02:07,400 Bonjour! I'm Jennifer Pulley, and welcome to NASA Connect, the show that connects you to math, science, technology, and NASA. 16 00:02:07,400 --> 00:02:11,400 On today's episode, we're filming on location in France. 17 00:02:11,400 --> 00:02:17,800 Voila! As you can see, France is a beautiful European country that is rich in culture and history. 18 00:02:17,800 --> 00:02:21,800 Here's a quick tour of some of the places we've seen during our trip to France. 19 00:02:21,800 --> 00:02:50,800 Music 20 00:02:51,800 --> 00:02:56,800 Music 21 00:02:56,800 --> 00:03:01,800 As you can see, France is a great place to visit, especially when you have nice weather. 22 00:03:01,800 --> 00:03:06,800 Speaking of the weather, what is one of the first things you want to know when you wake up in the morning? 23 00:03:06,800 --> 00:03:11,800 Well, if you're like me, you'll think, hmm, I wonder what the weather's going to be like today. 24 00:03:11,800 --> 00:03:15,800 You depend on information about the weather for a variety of reasons. 25 00:03:15,800 --> 00:03:20,800 You need to decide what to wear to school, and you need to plan for after-school activities if they're outdoors. 26 00:03:20,800 --> 00:03:28,800 Do you realize that the weather in the United States can have a significant effect on what the weather will be like here in France? 27 00:03:28,800 --> 00:03:34,800 Storms heading eastward from the Atlantic coast can bring wind and rain to Europe a few days later. 28 00:03:34,800 --> 00:03:39,800 We truly live in a global society where we all are interconnected in some way. 29 00:03:39,800 --> 00:03:43,800 Today's program will focus on predicting weather and climate change. 30 00:03:43,800 --> 00:03:51,800 You will learn that we need to work together internationally to answer some of the questions that Earth scientists from around the world ask every day. 31 00:03:51,800 --> 00:03:57,800 But before we get to those questions, let's first learn about the fundamentals of weather and climate. 32 00:03:57,800 --> 00:04:02,800 During the course of the program, you will be asked to answer several inquiry-based questions. 33 00:04:02,800 --> 00:04:10,800 After the questions appear on the screen, your teacher will pause the program to allow you time to answer and discuss the questions. 34 00:04:10,800 --> 00:04:14,800 This is your time to explore and become critical thinkers. 35 00:04:14,800 --> 00:04:19,800 Students working in groups take a few minutes to answer the following questions. 36 00:04:19,800 --> 00:04:22,800 How is weather different from climate? 37 00:04:22,800 --> 00:04:27,800 List and discuss various kinds of weather you have experienced. 38 00:04:27,800 --> 00:04:30,800 What are some factors that determine weather? 39 00:04:30,800 --> 00:04:32,800 What climate do you live in? 40 00:04:32,800 --> 00:04:36,800 It's now time to pause the program and answer the questions. 41 00:04:36,800 --> 00:04:39,800 Okay, guys, let's talk about weather. 42 00:04:39,800 --> 00:04:43,800 Basically, weather is the daily condition of the Earth's atmosphere. 43 00:04:43,800 --> 00:04:51,800 Weather is produced by the interaction of several factors, which include heat, air pressure, winds, and moisture. 44 00:04:51,800 --> 00:04:54,800 Let's briefly look at each one of those factors. 45 00:04:54,800 --> 00:05:00,800 Heat, transferred from the sun, is absorbed by the Earth and spread through the atmosphere. 46 00:05:00,800 --> 00:05:07,800 Air temperature varies from place to place because the sun's rays strike the Earth at different angles. 47 00:05:07,800 --> 00:05:13,800 Air pressure is the measure of the force of the air pressing down on the Earth's surface. 48 00:05:13,800 --> 00:05:16,800 Air pressure depends on the density of the air. 49 00:05:16,800 --> 00:05:20,800 Denser air exerts more pressure than less dense air. 50 00:05:20,800 --> 00:05:28,800 Air pressure on the Earth can vary considerably from location to location due to unequal heating of the atmosphere. 51 00:05:28,800 --> 00:05:33,800 These air pressure differences cause the movement of air, which we call wind. 52 00:05:33,800 --> 00:05:39,800 Finally, the amount of moisture in the air, called relative humidity, also influences weather. 53 00:05:39,800 --> 00:05:45,800 Moisture in the atmosphere condenses, causing clouds to develop and precipitation to fall to the Earth. 54 00:05:45,800 --> 00:05:50,800 So, have you come up with the difference between weather and climate? 55 00:05:50,800 --> 00:05:53,800 I said earlier that weather is the daily condition of the Earth's atmosphere. 56 00:05:53,800 --> 00:05:55,800 But what about climate? 57 00:05:55,800 --> 00:06:01,800 Well, for most of us, climate means a location is hot, cold, wet, or dry. 58 00:06:01,800 --> 00:06:08,800 You see, climate is the average weather conditions for a specific region over an extended period of time. 59 00:06:08,800 --> 00:06:14,800 The climate of any place is determined by two main factors, temperature and precipitation. 60 00:06:14,800 --> 00:06:21,800 The Earth is divided into three major climate zones based on the average temperature of these zones. 61 00:06:21,800 --> 00:06:25,800 They are the tropical, temperate, and polar zones. 62 00:06:25,800 --> 00:06:28,800 Can you determine what climate zone you live in? 63 00:06:28,800 --> 00:06:33,800 To learn more about weather and climate, check out the following NASA website. 64 00:06:33,800 --> 00:06:41,800 Have you ever been in a situation where the weather forecast called for sunny skies, yet it ended up raining all day long? 65 00:06:41,800 --> 00:06:44,800 You think, oh, if I only had my umbrella. 66 00:06:44,800 --> 00:06:51,800 But you know, guys, the job of predicting weather accurately is a difficult one because our atmosphere, it's constantly changing. 67 00:06:51,800 --> 00:06:56,800 You see, in order to predict the weather accurately for the hours and days ahead, 68 00:06:56,800 --> 00:07:01,800 weather forecasters must analyze information they receive from a number of sources, 69 00:07:01,800 --> 00:07:07,800 including local weather observers, weather balloons, weather stations, and satellites. 70 00:07:07,800 --> 00:07:13,800 Speaking of satellites, NASA has a train of satellites called the Afternoon Constellation, 71 00:07:13,800 --> 00:07:16,800 nicknamed the A-Train, which are orbiting the Earth. 72 00:07:16,800 --> 00:07:22,800 And they're collecting all sorts of data, including data that will help predict weather and climate change. 73 00:07:22,800 --> 00:07:28,800 Two additional satellites, CloudSat and Calypso, will soon be launched to be a part of that train. 74 00:07:28,800 --> 00:07:34,800 CloudSat will help improve weather prediction by studying the different aspects of clouds, as its name implies. 75 00:07:34,800 --> 00:07:41,800 Calypso will help predict climate change and how aerosols or particles affect the Earth's atmosphere. 76 00:07:41,800 --> 00:07:46,800 Later on in the program, Dr. Didier Tonray will tell us all about aerosols. 77 00:07:46,800 --> 00:07:49,800 But first, let's visit with Dr. Graham Stevens. 78 00:07:49,800 --> 00:07:52,800 He's the principal investigator on the CloudSat mission. 79 00:07:52,800 --> 00:07:55,800 Thank you, Jennifer. 80 00:07:55,800 --> 00:07:58,800 We rely on accurate weather predictions for many activities. 81 00:07:58,800 --> 00:08:02,800 Farmers need to know the best times to plant and harvest their crops. 82 00:08:02,800 --> 00:08:07,800 Airplane takeoffs, landings, and flight paths are scheduled according to local weather conditions. 83 00:08:08,800 --> 00:08:12,800 Weather forecasts alert people to severe storms that could endanger life or property. 84 00:08:12,800 --> 00:08:20,800 And most people want to know what the weather will be like as they go to and from work and school or plan outdoor activities. 85 00:08:20,800 --> 00:08:24,800 But do you think weather predictions or forecasts are always correct? 86 00:08:24,800 --> 00:08:27,800 What do you think causes errors in weather forecasts? 87 00:08:27,800 --> 00:08:31,800 You know, Jennifer is right when she stated that weather prediction is difficult. 88 00:08:31,800 --> 00:08:36,800 The atmosphere is constantly changing and even though we receive weather data from a variety of sources 89 00:08:36,800 --> 00:08:42,800 such as weather stations, satellites, weather balloons, and ground-based observers, 90 00:08:42,800 --> 00:08:46,800 it is still impossible to predict the weather correctly 100% of the time. 91 00:08:46,800 --> 00:08:50,800 One of the ways of improving our prediction of weather and climate 92 00:08:50,800 --> 00:08:54,800 is to develop new technologies that helps us understand how the atmosphere works. 93 00:08:54,800 --> 00:08:58,800 A new satellite that will help improve weather prediction is NASA's CloudSat satellite. 94 00:08:58,800 --> 00:09:04,800 CloudSat will provide the first vertical cloud profiling from space, improving weather and climate forecasts. 95 00:09:04,800 --> 00:09:08,800 Before we continue with the specifics of the CloudSat mission, 96 00:09:08,800 --> 00:09:12,800 here are a few questions I would like you and your peers to discuss and answer. 97 00:09:12,800 --> 00:09:14,800 What is a cloud? 98 00:09:14,800 --> 00:09:16,800 What types of clouds exist? 99 00:09:16,800 --> 00:09:18,800 Which clouds make which weather? 100 00:09:18,800 --> 00:09:20,800 Why is it important to study clouds? 101 00:09:20,800 --> 00:09:22,800 It's now time to pause the program. 102 00:09:22,800 --> 00:09:24,800 So how did you do with your questions? 103 00:09:24,800 --> 00:09:26,800 You know, clouds are all made of water. 104 00:09:26,800 --> 00:09:30,800 Sometimes they are made of tiny drops, far apart and held up by the wind. 105 00:09:30,800 --> 00:09:36,800 Other times they are made of big drops, held up for a while by very strong upward winds inside the cloud. 106 00:09:36,800 --> 00:09:41,800 In this kind of cloud, the drops become too heavy to stay up, so they fall to earth as rain, 107 00:09:41,800 --> 00:09:44,800 or if it's cold enough, they fall to earth as snow, hail, or sleet. 108 00:09:44,800 --> 00:09:47,800 Clouds are classified based on three factors. 109 00:09:47,800 --> 00:09:52,800 Their shape, the altitude at which they occur, and whether they are producing precipitation. 110 00:09:52,800 --> 00:09:54,800 Clouds come in three basic shapes. 111 00:09:54,800 --> 00:09:56,800 Cumulus clouds, which are heaped and puffy. 112 00:09:56,800 --> 00:09:59,800 Stratus clouds, which are layered. 113 00:09:59,800 --> 00:10:01,800 And cirrus clouds, which are wispy. 114 00:10:01,800 --> 00:10:06,800 Clouds also occur in three altitude ranges, specifically the altitude of the cloud base. 115 00:10:06,800 --> 00:10:10,800 High clouds, which occur above 6,000 metres and designated by cirrus, 116 00:10:10,800 --> 00:10:17,800 or cirro, are cirrus, cirrocumulus, and cirrostratus. 117 00:10:17,800 --> 00:10:22,800 Middle clouds, which occur between 2,000 and 6,000 metres and are designated by alto, 118 00:10:22,800 --> 00:10:26,800 are altocumulus and altostratus. 119 00:10:26,800 --> 00:10:33,800 Low clouds, which occur below 2,000 metres are stratus, nimbostratus, 120 00:10:33,800 --> 00:10:38,800 cumulus, stratocumulus, cumulonimbus, and fog. 121 00:10:38,800 --> 00:10:41,800 I bet you didn't think fog was a cloud. 122 00:10:41,800 --> 00:10:43,800 It's a cloud that touches the ground. 123 00:10:43,800 --> 00:10:47,800 Clouds that incorporate the word nimbus, or the prefix nimbo, 124 00:10:47,800 --> 00:10:50,800 are clouds from which precipitation is falling. 125 00:10:50,800 --> 00:10:52,800 Can you think of another type of cloud? 126 00:10:52,800 --> 00:10:54,800 I'll leave the answer to that question up to you. 127 00:10:54,800 --> 00:10:58,800 So how many of you are wondering how to keep all those clouds in order? 128 00:10:58,800 --> 00:11:00,800 You know, it's tough even for me. 129 00:11:00,800 --> 00:11:03,800 That's why I use this globe cloud chart as a reference. 130 00:11:03,800 --> 00:11:06,800 You'll learn more about globe later in the program. 131 00:11:06,800 --> 00:11:09,800 So why is it important to study clouds? 132 00:11:09,800 --> 00:11:12,800 Clouds exert an enormous influence on our weather and climate. 133 00:11:12,800 --> 00:11:16,800 They are nature's way of moving fresh water from place to place on Earth. 134 00:11:16,800 --> 00:11:19,800 Clouds play a very important part in maintaining Earth's temperature. 135 00:11:19,800 --> 00:11:24,800 We need to understand how clouds reflect the sun's energy back into space 136 00:11:24,800 --> 00:11:26,800 or trap the Earth's energy in the atmosphere. 137 00:11:26,800 --> 00:11:29,800 We call this Earth's radiation budget. 138 00:11:29,800 --> 00:11:32,800 Using the CloudSat satellite, for the very first time, 139 00:11:32,800 --> 00:11:35,800 we'll be able to measure the altitude and properties of clouds. 140 00:11:35,800 --> 00:11:38,800 CloudSat radar will slice through the atmosphere, 141 00:11:38,800 --> 00:11:41,800 providing vertical cross-sectional view of clouds 142 00:11:41,800 --> 00:11:44,800 and furnish new weather and climate data, 143 00:11:44,800 --> 00:11:49,800 including cloud layer thickness, cloud top and base altitude, 144 00:11:49,800 --> 00:11:51,800 and water and ice contents. 145 00:11:51,800 --> 00:11:55,800 Existing space-based systems only observe the uppermost layer of clouds 146 00:11:55,800 --> 00:11:58,800 and cannot reliably detect the presence of multiple cloud layers 147 00:11:58,800 --> 00:12:01,800 nor determine the cloud water and ice content. 148 00:12:01,800 --> 00:12:05,800 The penetration of CloudSat's radar into and through clouds 149 00:12:05,800 --> 00:12:08,800 will yield a new capability that fills a critical gap 150 00:12:08,800 --> 00:12:11,800 in existing and planned space-borne observational systems. 151 00:12:11,800 --> 00:12:15,800 With this new technology, CloudSat will improve weather predictions, 152 00:12:15,800 --> 00:12:20,800 increasing the accuracy of severe weather, hurricanes, and flood warnings. 153 00:12:20,800 --> 00:12:25,800 And now, Jennifer, I think the students are ready to size up the clouds. 154 00:12:25,800 --> 00:12:26,800 Back to you. 155 00:12:28,800 --> 00:12:30,800 Thanks, Dr. Stephens. 156 00:12:30,800 --> 00:12:33,800 I really had no idea how much the clouds impacted our weather. 157 00:12:33,800 --> 00:12:36,800 Well, now it's time to see how much you've learned, 158 00:12:36,800 --> 00:12:38,800 and it's time for you to size up the clouds. 159 00:12:38,800 --> 00:12:43,800 Students from the School of International Studies at Meadowbrook in Norfolk, Virginia, 160 00:12:43,800 --> 00:12:46,800 will preview Part 1 of this program's hands-on activity. 161 00:12:48,800 --> 00:12:53,800 NASA Connect asks us to show you this program's hands-on activity. 162 00:12:53,800 --> 00:12:57,800 In this activity, you will set up three simulated clouds 163 00:12:57,800 --> 00:12:59,800 representing three different cloud types. 164 00:12:59,800 --> 00:13:05,800 You will use different methods to estimate precipitation content in each cloud type. 165 00:13:05,800 --> 00:13:08,800 The precipitation from each cloud will be released, 166 00:13:08,800 --> 00:13:13,800 and you will compare your estimates with what is actually occurring on the ground. 167 00:13:14,800 --> 00:13:16,800 In addition to learning about weather forecasting, 168 00:13:16,800 --> 00:13:21,800 we will also be using math skills like estimation, percentages, averages, and ratios. 169 00:13:22,800 --> 00:13:25,800 You can download a copy of the Educator Guide containing directions 170 00:13:25,800 --> 00:13:28,800 and a list of materials from the NASA Connect website. 171 00:13:29,800 --> 00:13:32,800 Teachers should cut a three-quarter inch diameter hole 172 00:13:32,800 --> 00:13:36,800 in the center of the bottom of three different foam cups. 173 00:13:37,800 --> 00:13:39,800 Cover the hole with a Post-It note. 174 00:13:39,800 --> 00:13:42,800 Place about one ounce of M&M's in a plastic bag. 175 00:13:42,800 --> 00:13:46,800 Twist the bag tightly and tie the excess bag in a knot. 176 00:13:47,800 --> 00:13:50,800 Cut off the excess to make a compact bundle. 177 00:13:50,800 --> 00:13:53,800 Make a second bag following the same procedure. 178 00:13:53,800 --> 00:13:54,800 Select any cup. 179 00:13:54,800 --> 00:13:57,800 Pour in about half full of M&M's. 180 00:13:57,800 --> 00:14:02,800 Then add a bundle of M&M's and fill more loose M&M's into the cup 181 00:14:02,800 --> 00:14:04,800 until it is three-quarters full. 182 00:14:05,800 --> 00:14:09,800 The loose M&M's will represent the amount of precipitation in each cloud. 183 00:14:10,800 --> 00:14:13,800 Fill the second cup to about one-third full of M&M's. 184 00:14:14,800 --> 00:14:18,800 Fill the third cup to about one-fourth full of M&M's. 185 00:14:18,800 --> 00:14:22,800 Add a bundle of M&M's and then continue filling with loose M&M's 186 00:14:22,800 --> 00:14:24,800 until the cup is one-half full. 187 00:14:24,800 --> 00:14:29,800 Secure the lids on the cups by taping the joint with masking tape or transparent tape. 188 00:14:30,800 --> 00:14:35,800 Invert the cups and label each cup cloud type X, Y, and Z. 189 00:14:35,800 --> 00:14:39,800 Below this, write the actual capacity of the cups chosen. 190 00:14:39,800 --> 00:14:41,800 Line up the cups on a table. 191 00:14:41,800 --> 00:14:47,800 Students will estimate how many ounces of precipitation each cloud type contains. 192 00:14:47,800 --> 00:14:49,800 Write the estimate onto the data sheet. 193 00:14:49,800 --> 00:14:53,800 Next, remove the post-it note and shine a flashlight into the hole. 194 00:14:53,800 --> 00:14:58,800 Make a new estimate of how many ounces of precipitation each cloud type contains 195 00:14:58,800 --> 00:15:00,800 and record it on your data sheet. 196 00:15:00,800 --> 00:15:02,800 Do this for each cloud type. 197 00:15:02,800 --> 00:15:07,800 Choose a person to weigh each cloud type cup on a scale. 198 00:15:07,800 --> 00:15:09,800 Record the weight ounces. 199 00:15:09,800 --> 00:15:13,800 Remember, weight ounces do not equal volume ounces. 200 00:15:13,800 --> 00:15:17,800 Once you have collected all of the data, you will be able to use it 201 00:15:17,800 --> 00:15:22,800 Once you have collected all of the data, you will revise your precipitation estimate. 202 00:15:22,800 --> 00:15:24,800 Based on your data, answer these questions. 203 00:15:24,800 --> 00:15:27,800 How does the data compare with your estimates? 204 00:15:27,800 --> 00:15:30,800 What factors might cause differences? 205 00:15:30,800 --> 00:15:34,800 If you had another cloud type of a different size, 206 00:15:34,800 --> 00:15:39,800 would the data collected make for a more accurate precipitation forecast? 207 00:15:39,800 --> 00:15:41,800 Discuss these findings with your class. 208 00:15:44,800 --> 00:15:45,800 Great job, you guys! 209 00:15:45,800 --> 00:15:47,800 Okay, now let's review. 210 00:15:47,800 --> 00:15:51,800 First, we learned the difference between weather and climate. 211 00:15:51,800 --> 00:15:57,800 Then, we learned how weather is produced by several factors like heat energy and moisture. 212 00:15:57,800 --> 00:16:01,800 Next, Dr. Graham Stevens told us how the CloudSat satellite 213 00:16:01,800 --> 00:16:05,800 will be able to help improve weather prediction across the globe. 214 00:16:09,800 --> 00:16:14,800 Now let's focus our attention on aerosols, climate changes, and Calypso. 215 00:16:14,800 --> 00:16:19,800 For that, we're going to head to the Space Agency of France, or CNES. 216 00:16:19,800 --> 00:16:23,800 What NASA is to America, CNES is to France. 217 00:16:23,800 --> 00:16:26,800 So, let's go speak with Dr. Didier Tonray. 218 00:16:26,800 --> 00:16:32,800 He's a principal investigator of Parasol and a co-investigator for the Calypso mission. 219 00:16:32,800 --> 00:16:36,800 Calypso is a satellite that's being built by both France and the United States. 220 00:16:37,800 --> 00:16:40,800 Launch! 221 00:16:40,800 --> 00:16:41,800 Merci, Jennifer. 222 00:16:41,800 --> 00:16:46,800 The climate of the Earth has not remained constant through the course of time. 223 00:16:46,800 --> 00:16:47,800 It has changed. 224 00:16:47,800 --> 00:16:52,800 In general, living things have affected changes in climate, 225 00:16:52,800 --> 00:16:55,800 and changes in climate have affected living things. 226 00:16:55,800 --> 00:16:59,800 Working in groups, see if you can answer the following question. 227 00:16:59,800 --> 00:17:03,800 What are some reasons why our climate has changed over time? 228 00:17:04,800 --> 00:17:08,800 Teacher, you may now pause the program so students can answer the question. 229 00:17:08,800 --> 00:17:14,800 From reports of increasing temperature, we think that the Earth's climate is maybe changing. 230 00:17:14,800 --> 00:17:17,800 But the processes behind these changes are not as clear. 231 00:17:17,800 --> 00:17:22,800 Two of the biggest uncertainties in understanding and predicting climate change 232 00:17:22,800 --> 00:17:25,800 are the effect of clouds and aerosols. 233 00:17:25,800 --> 00:17:32,800 The Calypso, or Cloud Aerosol LiDAR and Infrared Pathfinder Satellite Observation Satellite mission 234 00:17:32,800 --> 00:17:36,800 will help us answer significant questions about climate processes 235 00:17:36,800 --> 00:17:40,800 by providing new information on clouds and aerosols. 236 00:17:40,800 --> 00:17:43,800 Dr. Stephens provided you with some information on clouds, 237 00:17:43,800 --> 00:17:46,800 so now let's concentrate on aerosols. 238 00:17:46,800 --> 00:17:48,800 What are aerosols? 239 00:17:48,800 --> 00:17:51,800 Aerosols are tiny particles suspended in the air. 240 00:17:51,800 --> 00:17:58,800 Some occur naturally, originating from volcanoes, dust storms, forests and grassland fires, 241 00:17:58,800 --> 00:18:01,800 living vegetation and sea spray. 242 00:18:01,800 --> 00:18:04,800 Human activities, such as the burning of fossil fuels 243 00:18:04,800 --> 00:18:09,800 and the alteration of natural surface cover, also generate aerosols. 244 00:18:09,800 --> 00:18:13,800 Average over the globe, aerosols made by human activities 245 00:18:13,800 --> 00:18:19,800 currently account for 10% of the total amount of aerosols in our atmosphere. 246 00:18:19,800 --> 00:18:23,800 Most of that 10% is concentrated in the northern hemisphere. 247 00:18:23,800 --> 00:18:25,800 Can you think of a reason why? 248 00:18:25,800 --> 00:18:29,800 We have much to learn about the way aerosols affect global and regional climate. 249 00:18:29,800 --> 00:18:33,800 We don't know in what regions of the planet the amount of atmospheric aerosol 250 00:18:33,800 --> 00:18:37,800 is increasing, decreasing or remaining constant. 251 00:18:37,800 --> 00:18:42,800 Overall, we don't know whether aerosols are warming or cooling the planet. 252 00:18:42,800 --> 00:18:45,800 So why do we care about aerosols? 253 00:18:45,800 --> 00:18:50,800 Aerosols tend to cause cooling of the Earth's surface immediately below them. 254 00:18:50,800 --> 00:18:52,800 Because they reflect sunlight back into space, 255 00:18:52,800 --> 00:18:57,800 aerosols have a direct cooling effect by reducing the amount of solar radiation 256 00:18:57,800 --> 00:18:59,800 that reaches the surface. 257 00:18:59,800 --> 00:19:03,800 It is thought that aerosol cooling may partially offset expected global warming 258 00:19:03,800 --> 00:19:07,800 that is attributed to increases in the amount of carbon dioxide 259 00:19:07,800 --> 00:19:10,800 and other gases from human activity. 260 00:19:10,800 --> 00:19:13,800 Did you realize that if there were no aerosols in the atmosphere, 261 00:19:13,800 --> 00:19:15,800 there would be no clouds? 262 00:19:15,800 --> 00:19:19,800 What can you say about the relationship between clouds and aerosols? 263 00:19:19,800 --> 00:19:22,800 Aerosols are believed to have an indirect effect on climate 264 00:19:22,800 --> 00:19:25,800 by changing the properties of clouds. 265 00:19:25,800 --> 00:19:28,800 As aerosol concentration increases within a cloud, 266 00:19:28,800 --> 00:19:32,800 the water in the cloud gets spread over many more particles, 267 00:19:32,800 --> 00:19:36,800 each of which is correspondingly smaller. 268 00:19:36,800 --> 00:19:39,800 In this way, changing aerosol in the atmosphere 269 00:19:39,800 --> 00:19:45,800 can change the frequency of cloud occurence, cloud thickness and rainfall amounts. 270 00:19:45,800 --> 00:19:50,800 Also, clouds with low aerosol concentration and few large droplets 271 00:19:50,800 --> 00:19:52,800 do not scatter light well 272 00:19:52,800 --> 00:19:56,800 and allow much of the sunlight to pass through and reach the surface. 273 00:19:56,800 --> 00:20:00,800 However, the high aerosol concentration in these clouds 274 00:20:00,800 --> 00:20:04,800 allows for the formation of many small liquid water droplets. 275 00:20:04,800 --> 00:20:12,800 Up to 90% of visible radiation or light is reflected back to space by such clouds 276 00:20:12,800 --> 00:20:14,800 without reaching Earth's surface. 277 00:20:14,800 --> 00:20:18,800 Probably the best-known evidence of the effect of aerosols in the atmosphere 278 00:20:18,800 --> 00:20:20,800 occurred in 1991. 279 00:20:20,800 --> 00:20:24,800 A severe volcanic eruption from Mount Pinatubo, Philippines, 280 00:20:24,800 --> 00:20:29,800 put an estimated 20 million tons of sulfur dioxide into the atmosphere. 281 00:20:29,800 --> 00:20:33,800 Aerosols from that eruption stayed in the atmosphere so long 282 00:20:33,800 --> 00:20:38,800 that average global temperature over the following year cooled by about half a degree. 283 00:20:38,800 --> 00:20:41,800 So, earlier in the program, Jennifer was right 284 00:20:41,800 --> 00:20:45,800 in that weather in the United States affects the weather here in France 285 00:20:45,800 --> 00:20:47,800 and all over the globe. 286 00:20:47,800 --> 00:20:48,800 And the reverse is true. 287 00:20:48,800 --> 00:20:54,800 Scientists have been observing clouds and aerosols globally from space for many years 288 00:20:54,800 --> 00:20:58,800 using sensors that measure the amount of energy leaving Earth. 289 00:20:58,800 --> 00:21:03,800 The sensors observe how clouds and aerosols vary with latitude and longitude 290 00:21:03,800 --> 00:21:07,800 but provide little information of what is inside the clouds 291 00:21:07,800 --> 00:21:10,800 or on how they vary with altitude. 292 00:21:10,800 --> 00:21:14,800 For the first time, the CALIPSO satellite will provide vertical, 293 00:21:14,800 --> 00:21:19,800 curtained-like images of the atmosphere on a global scale using a LiDAR. 294 00:21:19,800 --> 00:21:22,800 The LiDAR technique is similar to radar in operation, 295 00:21:22,800 --> 00:21:29,800 but LiDAR uses short pulses of laser light instead of radio waves to prompt the atmosphere. 296 00:21:29,800 --> 00:21:34,800 The LiDAR data from CALIPSO will allow us to determine precisely 297 00:21:34,800 --> 00:21:39,800 the altitudes of clouds and aerosol layers and the extent of layer overlap 298 00:21:39,800 --> 00:21:44,800 to identify the composition of clouds and to estimate the abundance and sizes of aerosols. 299 00:21:44,800 --> 00:21:49,800 CALIPSO is a highly advanced research tool to study the Earth's atmosphere 300 00:21:49,800 --> 00:21:53,800 and will provide the international community with a data set 301 00:21:53,800 --> 00:21:57,800 that is essential for a better understanding of the Earth's climate. 302 00:21:57,800 --> 00:22:00,800 With more confidence in climate model predictions, 303 00:22:00,800 --> 00:22:07,800 international leaders will be able to make more informed policy decisions about global climate change. 304 00:22:08,800 --> 00:22:11,800 So the next time you wake up on a hazy summer day, 305 00:22:11,800 --> 00:22:15,800 you can tell your friends that the haziness may be caused by sandstorms 306 00:22:15,800 --> 00:22:20,800 or volcanic eruptions that occur halfway around the world. 307 00:22:20,800 --> 00:22:23,800 Now back to you, Jennifer. Au revoir. 308 00:22:26,800 --> 00:22:28,800 Merci, Dr. Tonray. 309 00:22:28,800 --> 00:22:31,800 Well, now that you are experts on aerosols, 310 00:22:31,800 --> 00:22:35,800 let's head to Collège Cantolando, located in Bordeaux, France, 311 00:22:35,800 --> 00:22:40,800 for part deux of this program's hands-on activity, the Globe Aerosol Protocol. 312 00:22:55,800 --> 00:22:58,800 In this activity, called Aerosols Protocol, 313 00:22:58,800 --> 00:23:04,800 you will use a sun photometer to measure the aerosol optical thickness of the atmosphere 314 00:23:04,800 --> 00:23:11,800 or how much of the sun's light is scattered or absorbed by particles suspended in the air. 315 00:23:11,800 --> 00:23:14,800 Remember, you can download a copy of the educator guide 316 00:23:14,800 --> 00:23:19,800 containing directions and list of materials from the NASA Connect website. 317 00:23:19,800 --> 00:23:23,800 When you are ready to go outside, put your sun photometer in an insulated bag 318 00:23:23,800 --> 00:23:25,800 to keep it at room temperature. 319 00:23:25,800 --> 00:23:31,800 Putting your sun photometer in a bag will help minimize any temperature sensitivity problems. 320 00:23:31,800 --> 00:23:33,800 To begin taking measurements with your sun photometer, 321 00:23:33,800 --> 00:23:37,800 flip the power switch on and then select the green channel. 322 00:23:37,800 --> 00:23:40,800 Hold the instrument in front of you about chest high. 323 00:23:40,800 --> 00:23:43,800 Point the sun photometer at the sun 324 00:23:43,800 --> 00:23:49,800 and then find the spot made by the sun as it shines through the front alignment bracket. 325 00:23:49,800 --> 00:23:52,800 Remember, guys, never look directly into the sun. 326 00:23:52,800 --> 00:23:56,800 Use the mark on the rear alignment bracket as a guide 327 00:23:56,800 --> 00:24:00,800 to align the sunspot until it rests on the color dot. 328 00:24:00,800 --> 00:24:04,800 It is normal for the readout to fluctuate within a few millivolts. 329 00:24:04,800 --> 00:24:10,800 Record only the highest reading that you see over a period of about 15 seconds. 330 00:24:10,800 --> 00:24:15,800 Record the value on the data sheet and the time of the reading to within 15 seconds. 331 00:24:15,800 --> 00:24:18,800 Now take the dark voltage reading. 332 00:24:18,800 --> 00:24:21,800 Cover the two holes on the sun photometer. 333 00:24:21,800 --> 00:24:25,800 Record the value of the dark voltage reading on the data sheet. 334 00:24:25,800 --> 00:24:27,800 Switch to the red channel. 335 00:24:27,800 --> 00:24:33,800 Record the maximum voltage and the time just as you did with the green channel. 336 00:24:33,800 --> 00:24:37,800 Then take the dark voltage reading again just like before. 337 00:24:37,800 --> 00:24:42,800 You need to repeat the process for the green and red channels two more times, 338 00:24:42,800 --> 00:24:46,800 giving you a total of three data points for each channel. 339 00:24:46,800 --> 00:24:51,800 Next, using your cloud chart as a guide, observe and record cloud conditions. 340 00:24:51,800 --> 00:24:54,800 Determine what types of clouds are in the sky. 341 00:24:54,800 --> 00:24:57,800 Record your observation on the data chart. 342 00:24:57,800 --> 00:25:02,800 Next, determine the percentage of cloud cover and record the value on the data sheet. 343 00:25:02,800 --> 00:25:05,800 Now you need to observe the sky conditions. 344 00:25:05,800 --> 00:25:09,800 What is the sky color? Is the sky clear or hazy? 345 00:25:09,800 --> 00:25:14,800 Is the sky obscured by fog, smoke, or haze? 346 00:25:14,800 --> 00:25:16,800 Record these observations on the data sheet. 347 00:25:16,800 --> 00:25:19,800 Finally, record the current temperature. 348 00:25:19,800 --> 00:25:24,800 When you get back into your classroom, log on to the following website. 349 00:25:24,800 --> 00:25:27,800 You will record all your data into the database. 350 00:25:27,800 --> 00:25:32,800 The database will automatically convert your voltage readings to aerosol optical thickness. 351 00:25:32,800 --> 00:25:37,800 To learn more about assessing a sun photometer, check out the NASA Connect website. 352 00:25:40,800 --> 00:25:42,800 Très bien. Super job, you guys. 353 00:25:42,800 --> 00:25:45,800 You sure did collect a lot of data in your aerosol protocol. 354 00:25:45,800 --> 00:25:50,800 Now, don't throw it away because it could be useful to scientists from around the world. 355 00:25:50,800 --> 00:25:56,800 Say, how would you like to be a part of a really cool international science program? 356 00:25:56,800 --> 00:26:01,800 Well, Dr. Diane Robinson, Calypso Outreach Director from Hampton University, 357 00:26:01,800 --> 00:26:05,800 and Dr. Teresa Kennedy with Globe International can tell you more. 358 00:26:05,800 --> 00:26:10,800 Thanks, Jennifer. Those are great activities that can be used with Globe and Calypso, 359 00:26:10,800 --> 00:26:15,800 the satellite being built right here at the Alcatel building in Cannes, France. 360 00:26:15,800 --> 00:26:18,800 If you would like to participate with this experiment 361 00:26:18,800 --> 00:26:21,800 or other Earth science activities related to satellite observation, 362 00:26:21,800 --> 00:26:25,800 the Globe program is actively looking for students to work with scientists worldwide. 363 00:26:25,800 --> 00:26:29,800 Globe is a cooperative worldwide effort to collect environmental observations 364 00:26:29,800 --> 00:26:31,800 into a large database on the Internet, 365 00:26:31,800 --> 00:26:34,800 and we welcome the French to be the newest members to Globe. 366 00:26:34,800 --> 00:26:37,800 Students around the world collect real data in all Earth science areas. 367 00:26:38,800 --> 00:26:42,800 The measurements collected by students are sent to the Globe database via the Web or e-mail 368 00:26:42,800 --> 00:26:45,800 and used by students and scientists around the world. 369 00:26:45,800 --> 00:26:50,800 The student information is used in a real way with the data collected by scientists and satellites 370 00:26:50,800 --> 00:26:53,800 to give us a greater idea about how the environment works. 371 00:26:53,800 --> 00:26:57,800 Once submitted, these data are publicly available on the Globe website 372 00:26:57,800 --> 00:27:00,800 and are displayed graphically with Globe visualization tools. 373 00:27:00,800 --> 00:27:05,800 An important aspect of the program is that students are encouraged to communicate directly with Globe scientists 374 00:27:05,800 --> 00:27:08,800 to better understand the importance and impact of their data. 375 00:27:08,800 --> 00:27:11,800 Another important aspect is that the information you collect 376 00:27:11,800 --> 00:27:15,800 can and does make a difference to understanding our world around us. 377 00:27:15,800 --> 00:27:20,800 More than a million students in over 14,000 schools have joined the Globe effort, 378 00:27:20,800 --> 00:27:22,800 and the numbers are growing. 379 00:27:22,800 --> 00:27:24,800 Won't you join the effort? 380 00:27:24,800 --> 00:27:28,800 For more information, go to our website at www.globe.gov. 381 00:27:28,800 --> 00:27:30,800 Back to you, Jennifer. 382 00:27:32,800 --> 00:27:34,800 Thanks, Diane and Teresa. 383 00:27:34,800 --> 00:27:37,800 Well, guys, that wraps up another episode of NASA Connect. 384 00:27:37,800 --> 00:27:44,800 Students, don't forget to check out the website for this program's Web activities and the student challenge. 385 00:27:44,800 --> 00:27:47,800 Hey, got a question, comment, or suggestion? 386 00:27:47,800 --> 00:27:51,800 Then e-mail them to connect at lark.nasa.gov. 387 00:27:51,800 --> 00:27:57,800 So until next time, stay connected to math, science, technology, and NASA. 388 00:27:57,800 --> 00:27:59,800 Au revoir. 389 00:28:00,800 --> 00:28:04,800 NASA Jet Propulsion Laboratory 390 00:28:04,800 --> 00:28:08,800 California Institute of Technology 391 00:28:29,800 --> 00:28:34,800 NASA Jet Propulsion Laboratory California Institute of Technology