WEBVTT FILE 1 00:00:00.010 --> 00:00:04.000 The Earth is constantly hit by solar radiation. 2 00:00:04.020 --> 00:00:08.010 That radiation is the driving force for life on Earth. 3 00:00:08.030 --> 00:00:12.010 However, not all of the radiation that reaches the Earth is absorbed. 4 00:00:12.030 --> 00:00:16.030 In fact, the Earth's ability to reflect a portion of the solar radiation is vital 5 00:00:16.050 --> 00:00:20.040 to sustain the balance that allows life as we know it to thrive. 6 00:00:20.060 --> 00:00:24.050 The fraction of solar radiation a surface reflects 7 00:00:24.070 --> 00:00:28.070 is called its "albedo." An albedo of 1 means that 8 00:00:28.090 --> 00:00:32.070 100% of incoming radiation is reflected. An albedo of 0 9 00:00:32.090 --> 00:00:36.070 means that 0% of incoming radiation is reflected and all of it 10 00:00:36.090 --> 00:00:40.080 is absorbed. On sunny days, you may have noticed that if you walk 11 00:00:40.100 --> 00:00:44.080 barefoot on dark asphalt, it burns your feet more than the lighter concrete. 12 00:00:44.100 --> 00:00:48.080 This is because the dark surface of the black asphalt has a lower albedo 13 00:00:48.100 --> 00:00:52.080 than the lighter-colored concrete. It absorbs more of the incoming radiation and 14 00:00:52.100 --> 00:00:56.100 is much warmer as a result. 15 00:00:56.120 --> 00:01:00.110 Surfaces throughout the Earth have different albedos. NASA is able to measure these differences 16 00:01:00.130 --> 00:01:04.120 with many instruments, including those on the Aqua satellite. These measurements 17 00:01:04.140 --> 00:01:08.140 can tell scientists essential information about the Earth's environment. 18 00:01:08.160 --> 00:01:12.160 Snow-covered ice in the polar regions has a high albedo. 19 00:01:12.180 --> 00:01:16.170 It reflects the majority of incoming radiation, which helps to cool the Earth. 20 00:01:16.190 --> 00:01:20.170 As the Earth's temperature rises with the increase in greenhouse gases, 21 00:01:20.190 --> 00:01:24.190 sea ice in the polar regions can be expected to retreat. 22 00:01:24.210 --> 00:01:28.200 This replaces an ice surface with a water surface, which has a much lower 23 00:01:28.220 --> 00:01:32.220 albedo. This causes more energy to be absorbed, and accelerates the warming 24 00:01:32.240 --> 00:01:36.240 process. The low albedo of dark 25 00:01:36.260 --> 00:01:40.260 green vegetation allows it to absorb sunlight and use it in photosynthesis, 26 00:01:40.280 --> 00:01:44.280 a fundamental process necessary to bring energy into the biosphere. 27 00:01:44.300 --> 00:01:48.300 Satellite imagery helps scientists to see how the albedo of these areas 28 00:01:48.320 --> 00:01:52.310 changes over time, through both natural processes and human alteration. 29 00:01:52.330 --> 00:01:56.330 As we move from rural to urban areas, many factors change, 30 00:01:56.350 --> 00:02:00.360 including the albedo. This causes urban areas to generally be 31 00:02:00.380 --> 00:02:04.380 warmer than their surroundings, a phenomenon known as the "urban heat island effect." 32 00:02:04.400 --> 00:02:08.400 Understanding albedo can lead to suggestions to help reduce 33 00:02:08.420 --> 00:02:12.410 this effect. One possibility would be to paint roofs white in hot regions, 34 00:02:12.430 --> 00:02:16.430 thereby reflecting solar radiation. Though it may not 35 00:02:16.450 --> 00:02:20.450 feel like it's affecting you directly, abledo is critical to the climate of the 36 00:02:20.470 --> 00:02:24.480 entire planet. By measuring and understanding albedo, we can see how our environment 37 00:02:24.500 --> 00:02:28.510 is changing in response to our alterations and how it may impact the 38 00:02:28.530 --> 00:02:32.087 relationship between solar radiation and the Earth.