1 00:00:06,230 --> 00:00:03,350 now for all the attention that's paid to 2 00:00:08,150 --> 00:00:06,240 science work done by human crew members 3 00:00:10,310 --> 00:00:08,160 there is a good bit of science research 4 00:00:12,230 --> 00:00:10,320 being conducted by instruments located 5 00:00:15,190 --> 00:00:12,240 on the outside of the international 6 00:00:17,029 --> 00:00:15,200 space station the hyperspectral imager 7 00:00:19,029 --> 00:00:17,039 for the coastal oceans has been 8 00:00:21,429 --> 00:00:19,039 gathering data for nearly five years 9 00:00:22,630 --> 00:00:21,439 about the conditions of ocean waters all 10 00:00:23,990 --> 00:00:22,640 over the world 11 00:00:26,630 --> 00:00:24,000 this morning we're going to learn more 12 00:00:29,029 --> 00:00:26,640 about it from mary kappas the hico 13 00:00:31,029 --> 00:00:29,039 facility manager who joins us from her 14 00:00:32,709 --> 00:00:31,039 office at the naval research laboratory 15 00:00:34,470 --> 00:00:32,719 in washington d.c 16 00:00:36,229 --> 00:00:34,480 mary for starters tell me about the 17 00:00:38,069 --> 00:00:36,239 hardware itself and 18 00:00:40,470 --> 00:00:38,079 when was it launched and where on the 19 00:00:41,510 --> 00:00:40,480 station is it located 20 00:00:44,310 --> 00:00:41,520 okay 21 00:00:46,549 --> 00:00:44,320 hico is a hyperspectral imager which is 22 00:00:48,790 --> 00:00:46,559 made up of a camera that is the focal 23 00:00:51,189 --> 00:00:48,800 plane that records the data 24 00:00:53,029 --> 00:00:51,199 four optics for collecting the light and 25 00:00:54,950 --> 00:00:53,039 a spectrometer for dispersing the 26 00:00:56,869 --> 00:00:54,960 broadband incoming light into separate 27 00:00:59,029 --> 00:00:56,879 wavelength bins 28 00:01:00,790 --> 00:00:59,039 hico was built as a demonstration 29 00:01:03,430 --> 00:01:00,800 project under the navy's innovative 30 00:01:04,869 --> 00:01:03,440 naval prototype program and so it had to 31 00:01:06,950 --> 00:01:04,879 incorporate innovative cost 32 00:01:08,070 --> 00:01:06,960 effectiveness and project acceleration 33 00:01:10,630 --> 00:01:08,080 methods 34 00:01:12,469 --> 00:01:10,640 to do that nrl designed hico based on 35 00:01:14,550 --> 00:01:12,479 decades of airborne hyperspectral 36 00:01:17,270 --> 00:01:14,560 experience that was focused on coastal 37 00:01:19,190 --> 00:01:17,280 oceans and they incorporated commercial 38 00:01:20,390 --> 00:01:19,200 off-the-shelf parts for most of the 39 00:01:21,830 --> 00:01:20,400 system 40 00:01:23,990 --> 00:01:21,840 we designed hico to capture the 41 00:01:26,310 --> 00:01:24,000 complexities subtleties and scale of 42 00:01:28,710 --> 00:01:26,320 ocean coastal dynamics 43 00:01:31,830 --> 00:01:28,720 heiko was built in 18 months and 44 00:01:34,630 --> 00:01:31,840 launched in september 2009 it's on the 45 00:01:36,390 --> 00:01:34,640 japanese exposed module the gem 46 00:01:38,789 --> 00:01:36,400 and it's in an enclosure that provides 47 00:01:40,789 --> 00:01:38,799 protection during iss maneuvers and a 48 00:01:42,950 --> 00:01:40,799 quite dark place for acquiring dark 49 00:01:44,630 --> 00:01:42,960 scenes needed for calibration 50 00:01:47,429 --> 00:01:44,640 there's a commercial off-the-shelf 51 00:01:49,590 --> 00:01:47,439 rotation stage also that allows heiko to 52 00:01:52,389 --> 00:01:49,600 aim side to side 53 00:01:54,550 --> 00:01:52,399 now for those of us who are scientists 54 00:01:56,550 --> 00:01:54,560 what is hyperspectral 55 00:02:01,429 --> 00:01:56,560 mean 56 00:02:03,910 --> 00:02:01,439 incoming light into separate wavelengths 57 00:02:04,870 --> 00:02:03,920 in lots of separate narrow contiguous 58 00:02:06,950 --> 00:02:04,880 bands 59 00:02:09,029 --> 00:02:06,960 the operative concept is separating the 60 00:02:11,110 --> 00:02:09,039 wavelengths so the term hyperspectral 61 00:02:12,790 --> 00:02:11,120 doesn't specify the range of wavelengths 62 00:02:14,229 --> 00:02:12,800 because that's different for different 63 00:02:16,070 --> 00:02:14,239 kinds of sensors 64 00:02:17,350 --> 00:02:16,080 now for heiko the incoming light source 65 00:02:19,030 --> 00:02:17,360 is the sun 66 00:02:21,670 --> 00:02:19,040 which covers lots of wavelengths in one 67 00:02:24,150 --> 00:02:21,680 broadband and hico records just the 68 00:02:26,470 --> 00:02:24,160 visible especially the blue through the 69 00:02:30,150 --> 00:02:26,480 near infrared specifically it goes from 70 00:02:33,270 --> 00:02:30,160 350 nanometers out to 1080 nanometers in 71 00:02:35,030 --> 00:02:33,280 128 bands that are 5.7 nanometers wide 72 00:02:37,509 --> 00:02:35,040 which is fine enough 73 00:02:39,589 --> 00:02:37,519 to resolve features of optically active 74 00:02:41,910 --> 00:02:39,599 substances in water 75 00:02:43,830 --> 00:02:41,920 now for one spot that 76 00:02:46,070 --> 00:02:43,840 that'd be one pixel in a collected image 77 00:02:47,830 --> 00:02:46,080 you can look at a spectrum 78 00:02:49,430 --> 00:02:47,840 that shows how light is reflected or 79 00:02:51,350 --> 00:02:49,440 absorbed at each wavelength and 80 00:02:52,710 --> 00:02:51,360 different materials absorb or reflect 81 00:02:54,949 --> 00:02:52,720 light differently based on their 82 00:02:57,589 --> 00:02:54,959 chemical composition particle size and 83 00:02:59,509 --> 00:02:57,599 shape etc so we're doing spectroscopy 84 00:03:01,830 --> 00:02:59,519 like chemists do in the lab only our 85 00:03:03,990 --> 00:03:01,840 samples aren't neatly prepared and all 86 00:03:05,830 --> 00:03:04,000 in one type we can tell whether there's 87 00:03:07,430 --> 00:03:05,840 a high concentration of phytoplankton or 88 00:03:09,030 --> 00:03:07,440 suspended sediments or other water 89 00:03:10,390 --> 00:03:09,040 constituents and these elements are 90 00:03:12,949 --> 00:03:10,400 indicative of the health of ocean 91 00:03:15,030 --> 00:03:12,959 ecosystems or visibility in the water or 92 00:03:18,070 --> 00:03:15,040 the dynamics of flows and is that your 93 00:03:20,149 --> 00:03:18,080 your specific target phytoplanktons 94 00:03:22,309 --> 00:03:20,159 um that's that's one of the things it's 95 00:03:25,589 --> 00:03:22,319 overall what are the what's the 96 00:03:28,229 --> 00:03:25,599 constituents of the water and we look at 97 00:03:29,750 --> 00:03:28,239 optical properties and then we convert 98 00:03:32,390 --> 00:03:29,760 that into physical properties like 99 00:03:34,949 --> 00:03:32,400 phytoplankton suspended sediments 100 00:03:36,789 --> 00:03:34,959 dissolved organic matter etc and that in 101 00:03:38,149 --> 00:03:36,799 turn can be 102 00:03:40,390 --> 00:03:38,159 converted to look at what is the 103 00:03:43,190 --> 00:03:40,400 visibility or the water depth for 104 00:03:45,910 --> 00:03:43,200 example and what is the value of doing 105 00:03:48,390 --> 00:03:45,920 this test from orbit instead of going 106 00:03:50,149 --> 00:03:48,400 down to the waterfront and and taking a 107 00:03:50,869 --> 00:03:50,159 water sample and testing it 108 00:03:52,710 --> 00:03:50,879 so 109 00:03:55,589 --> 00:03:52,720 well in addition to the the spectrum for 110 00:03:58,470 --> 00:03:55,599 each pixel we get a whole spatial array 111 00:04:02,070 --> 00:03:58,480 our our image size is 50 kilometers by 112 00:04:03,990 --> 00:04:02,080 200 kilometers so in each scene we we 113 00:04:05,910 --> 00:04:04,000 basically have a three-dimensional image 114 00:04:07,670 --> 00:04:05,920 cube so the spectra tell us about the 115 00:04:08,710 --> 00:04:07,680 material composition and the spatial 116 00:04:10,710 --> 00:04:08,720 display 117 00:04:12,550 --> 00:04:10,720 shows the pattern of that composition so 118 00:04:14,550 --> 00:04:12,560 in the coastal oceans 119 00:04:16,469 --> 00:04:14,560 that allows us to see how high 120 00:04:18,150 --> 00:04:16,479 concentrations of some component let's 121 00:04:20,469 --> 00:04:18,160 say suspended sediment 122 00:04:23,270 --> 00:04:20,479 relates to the outflows from rivers 123 00:04:25,270 --> 00:04:23,280 um the shape of the coastline etc 124 00:04:26,710 --> 00:04:25,280 so now really what that does is the 125 00:04:28,469 --> 00:04:26,720 spaceborne location gives you this 126 00:04:30,629 --> 00:04:28,479 spatial extent 127 00:04:31,830 --> 00:04:30,639 while your boat samples is very 128 00:04:33,990 --> 00:04:31,840 localized 129 00:04:35,749 --> 00:04:34,000 so that spaceborne sensor allows you to 130 00:04:37,110 --> 00:04:35,759 do repeat visits without having to stay 131 00:04:38,550 --> 00:04:37,120 on site in a boat 132 00:04:40,870 --> 00:04:38,560 but i think i should point out that 133 00:04:42,629 --> 00:04:40,880 these two approaches work best together 134 00:04:44,629 --> 00:04:42,639 we need that in-situ sampling to 135 00:04:46,230 --> 00:04:44,639 calibrate and confirm the hyperspectral 136 00:04:48,469 --> 00:04:46,240 measurements which is really the case 137 00:04:50,550 --> 00:04:48,479 for any remotely sensed measurement 138 00:04:51,430 --> 00:04:50,560 heiko met all its goals within the first 139 00:04:53,270 --> 00:04:51,440 year 140 00:04:54,870 --> 00:04:53,280 the first image transmitted to earth was 141 00:04:57,030 --> 00:04:54,880 a good clean image 142 00:04:59,430 --> 00:04:57,040 and since then we've constantly worked 143 00:05:01,350 --> 00:04:59,440 to improve our calibration and we engage 144 00:05:03,029 --> 00:05:01,360 scientists throughout academia to work 145 00:05:05,029 --> 00:05:03,039 with the data and to help advance the 146 00:05:06,790 --> 00:05:05,039 processing and conduct useful scientific 147 00:05:08,790 --> 00:05:06,800 studies 148 00:05:10,870 --> 00:05:08,800 if you want some examples um researchers 149 00:05:13,670 --> 00:05:10,880 have used hico to map 150 00:05:15,749 --> 00:05:13,680 the contents of the water and the bottom 151 00:05:17,830 --> 00:05:15,759 in areas in the bahamas and australia 152 00:05:19,590 --> 00:05:17,840 they mapped out bottom depth bottom 153 00:05:22,070 --> 00:05:19,600 types such as different types of sand 154 00:05:23,510 --> 00:05:22,080 and seagrass and water constituents such 155 00:05:25,110 --> 00:05:23,520 as chlorophyll 156 00:05:27,510 --> 00:05:25,120 other researchers looked in san 157 00:05:29,830 --> 00:05:27,520 francisco and monterey bays to determine 158 00:05:31,590 --> 00:05:29,840 the water quality and make maps showing 159 00:05:35,830 --> 00:05:31,600 the extent and concentration of 160 00:05:38,550 --> 00:05:35,840 phytoplankton blooms and sediment plumes 161 00:05:40,469 --> 00:05:38,560 now i understand that hico is now a part 162 00:05:42,629 --> 00:05:40,479 of the international space station 163 00:05:44,150 --> 00:05:42,639 national laboratory what does that mean 164 00:05:45,350 --> 00:05:44,160 for it in in terms of day-to-day 165 00:05:47,830 --> 00:05:45,360 operation 166 00:05:50,629 --> 00:05:47,840 well it's been providing some really big 167 00:05:52,629 --> 00:05:50,639 pluses the direct tie to nasa 168 00:05:54,550 --> 00:05:52,639 enabled us to get additional data 169 00:05:56,629 --> 00:05:54,560 streams to help improve our geolocation 170 00:05:59,270 --> 00:05:56,639 accuracy and we were also able to get a 171 00:06:01,430 --> 00:05:59,280 faster data transmission rate and that 172 00:06:03,590 --> 00:06:01,440 enabled us to schedule up to two images 173 00:06:04,950 --> 00:06:03,600 per orbit and in the past we've been 174 00:06:06,469 --> 00:06:04,960 limited to one 175 00:06:09,029 --> 00:06:06,479 and another thing is that all the hico 176 00:06:11,110 --> 00:06:09,039 data is now available on nasa's ocean 177 00:06:13,830 --> 00:06:11,120 color website where researchers 178 00:06:15,909 --> 00:06:13,840 worldwide can browse and download it and 179 00:06:18,790 --> 00:06:15,919 by being co-located with traditional 180 00:06:20,870 --> 00:06:18,800 ocean color sensor data such as modis 181 00:06:24,150 --> 00:06:20,880 and viirs and so forth that encourages 182 00:06:25,830 --> 00:06:24,160 new users and multi-sensor projects 183 00:06:27,909 --> 00:06:25,840 how long do you figure hico will 184 00:06:28,790 --> 00:06:27,919 continue to operate 185 00:06:30,230 --> 00:06:28,800 well 186 00:06:31,830 --> 00:06:30,240 it can operate as long as it keeps 187 00:06:33,749 --> 00:06:31,840 working and so far the health of the 188 00:06:35,510 --> 00:06:33,759 system is very good and the other 189 00:06:36,790 --> 00:06:35,520 limitation would be the real estate on 190 00:06:38,870 --> 00:06:36,800 the iss 191 00:06:40,870 --> 00:06:38,880 so high cost lifespan depends on whether 192 00:06:43,029 --> 00:06:40,880 there's other plans for that spot and 193 00:06:45,110 --> 00:06:43,039 right now there's no immediate plans 194 00:06:47,430 --> 00:06:45,120 so we look forward to several more years 195 00:06:49,110 --> 00:06:47,440 of operation from the iss well mary 196 00:06:50,870 --> 00:06:49,120 thank you very much for for those couple 197 00:06:53,749 --> 00:06:50,880 of minutes and teaching us about what 198 00:06:55,350 --> 00:06:53,759 hico is doing there i appreciate that 199 00:06:58,150 --> 00:06:55,360 thank you for the opportunity mary 200 00:06:59,830 --> 00:06:58,160 kappas is the hico facility manager at