TOM ADAMSON: Hello everyone, and welcome to another episode of Eyes on Earth, a podcast produced at the USGS EROS Center. Our podcast focuses on our ever changing planet and on the people here at EROS and across the globe who use remote sensing to monitor and study the health of Earth. My name is Tom Adamson. On Eyes on Earth, we often talk about the fact that Landsat is the gold standard for Earth observation. One of the reasons is the calibration and validation work that goes on at EROS to ensure its accuracy and reliability. One of the ways the team validates what they have so carefully calibrated is to take measurements on the ground while Landsat passes by overhead. We have one of those validation sites here at EROS. I spoke to Jeff Irwin and Travis Kropuenske, who take care of the EROS test site, and who head out there every time one of the Landsat satellites passes over the site. Well, not quite every single pass. We'll let them explain that when we get to it. Most importantly, we're going to go out to the test site during a Landsat pass so you can get a sense for what that work is like. Jeff Irwin is the EROS survey and field campaign lead. He oversees all fieldwork that happens for the EROS Cal/Val Center of Excellence, in addition to elevation related projects that we do for the National Geospatial Program and the Coastal National Elevation Database. Travis Kropuenske, contractor to the USGS EROS, is a field surveyor and data processor, and he carries the mobile field spectrometer for this Landsat field validation work. Can you describe some of the instruments and some of the tools that you use when you go out to the test site? JEFF IRWIN: Yeah. So we have two field spectrometers; they're called ASD FieldSpec 4s. Each one of those is actually three instruments. It has a VNIR channel-- ADAMSON: visible near-infrared-- IRWIN: And then there's two shortwave infrared instruments as well. So they have a pretty high spectral resolution for measuring parts of the electromagnetic spectrum that we care about related to Landsat. One of them is mobile and one of them is static. The mobile one measures eight transects that we have out at our site. And the static one measures a calibration panel continuously while we're doing that. We have eight transects spread out at our site. They're 150 meters long, and they're 20 meters apart. So we sample along those transects so that we can aggregate that information to compare to the pixels that Landsat measures. ADAMSON: Okay, so you're doing this at the same time that Landsat is passing overhead. IRWIN: Yeah. Ideally we want to be within plus or minus 20 minutes of an overpass. ADAMSON: Okay. IRWIN: So we've established our routines. So we start 13 to 15 minutes before the satellite overpasses, and we're generally halfway through our collection when the overpass happens. ADAMSON: So you're walking back and forth-- IRWIN: Well, Travis is walking. ADAMSON: Travis does the walking? Okay. IRWIN: Yep. ADAMSON: Well, why don't you tell us how that works? TRAVIS KROPUENSKE: Yeah, I've got one of the ASDs strapped to my back. It's got a fiber optic cable leading to a foreoptic, which I hold out ahead of me out of any shadows. ADAMSON: You're careful not to cast a shadow on it, okay. KROPUENSKE: Yeah. ADAMSON: Glad you thought of that. KROPUENSKE: If I'm picking up shadow, I'm not doing my job. ADAMSON: Yeah. KROPUENSKE: And I'm going to walk these north-south transects that are about 150 meters long. ADAMSON: The instrument measures light as it's reflecting off the ground, and of course, you're not very far off the ground. KROPUENSKE: I mean, I might be a meter and a half at that foreoptic. ADAMSON: And Landsat at the same time is 438 miles above the ground. How does that work? How are we kind of comparing what you're collecting on the ground versus what Landsat is collecting way up in space? KROPUENSKE: We're sampling what Landsat is collecting. I'm just measuring a small portion at the same time. So then here's what we got. What do you got? There's three sensors in there. And it's measuring electromagnetic spectrum from 350 nanometer to 2500 nanometer, and which includes the visible portion. ADAMSON: Okay. KROPUENSKE: And, yeah, you know, every nanometer, we're getting a measurement. IRWIN: Additionally to those instruments, we have these calibration panels that are made of a material called Spectralon that is, it's a near Lambertian material. So they disperse light equally in all directions. We've had them characterized. What that means is, for several different solar geometries we know how the panels behave. And then so during different times of the year, the sun is in different spots for us. So that allows us to deal with those different solar positions throughout the year. ADAMSON: Okay. What do those panels look like? IRWIN: They're essentially, basically a one foot square. They're both at 99% reflectance. So they're quite white. ADAMSON: One foot by one foot. Is that okay to do since the Landsat pixels are 30 meters across? IRWIN: Yeah. So we're not relying on seeing the panels themselves in the, in the imagery. ADAMSON: Yeah, okay. IRWIN: What we're doing is we're getting our foreoptics quite close to the panels themselves. So we're just sampling a very small portion of the panel and the light that's being reflected back. We are pretty confident that we understand the light that is coming off of the panel, and that allows us to have a good calibration transferred to the spectrometers, which we then transfer to our field site. ADAMSON: What's the first thing you do when you get out to the site? IRWIN: First thing we do is, drive out there and pull out our panels and instruments. Set up the panels where they need to be initially. And then we start setting up our instruments. They need around 15 minutes of time to let them warm up and get up to operating temperature. ADAMSON: Okay. IRWIN: And so while that's happening, we're setting up the computers that store the data that the spectrometers are collecting and get our files all ready to go for storing that information. ADAMSON: What if it's cloudy? Then do you still do it or not? IRWIN: We consider this validation work, not calibration work. ADAMSON: Oh, okay. IRWIN: So that's part of the reason why we have a grass field site, because it's not easy. Most of the calibration sites are pseudo invariant, meaning they don't change much. And they like to use targets like deserts-- ADAMSON: Yeah. IRWIN: --where they have a nice bright reflectance, and they're well understood. They use those for calibration. But this is a validation site. And so we do have a tolerance for cloud cover. We kind of have a threshold of 40% cloud cover forecast that is kind of our go no-go decision. ADAMSON: Where do you get your information about whether it's 40% cloud cover or not? IRWIN: So we use the National Weather Service. They have a tabular data forecast for up to seven days out. ADAMSON: So raining is a no-go. IRWIN: Raining is a no-go. Another thing we don't do is when there's snow on the field. ADAMSON: Oh, okay. IRWIN: The instrumentation does have limitations in terms of operating temperature. ADAMSON: Ok. IRWIN: I don't think we've done anything below 40 degrees, I would say. ADAMSON: How about weekends and holidays? Landsat doesn't care if it's a holiday or a weekend. IRWIN: That's right. Landsat is imaging the EROS site, assuming cloud free, every eight days. So we'll do weekends. We will do some holidays, depending on how our collection season has been. There are definitely times of year, like, we have a lot better time getting good collections in September than we do in say, March and April. ADAMSON: Yeah, we get more rainy weather in the springtime here. IRWIN: Yes. And June can be variable, and last year we had some challenges in July with wildfire smoke. Got some interesting results that I'm not sure we've been able to tease everything out with yet. Yeah, we're on the northwest corner of the property. Essentially, it's an area that is free of trees and just grass. And it's got some slope to it but it's gradual. ADAMSON: Okay, well, Travis is the one who has to walk in this field. Are you wearing boots or bug spray and things like that? KROPUENSKE: I wear boots just because the site is, you know, there's tripping hazards out there. ADAMSON: Yeah, okay. KROPUENSKE: It's dynamic. New holes show up occasionally. ADAMSON: Have you run across any surprises? You know, critters and things like that? KROPUENSKE: Couple times I've went down. Tripped in a hole. Get up. Keep moving. ADAMSON: Oh, no. KROPUENSKE: In May and June, the fawns will lay really tight in the grass. ADAMSON: You're talking about baby deer. KROPUENSKE: Yes, yes. And so you won't-- They won't move until you are darn near on them. And it startles you. The pheasants are the same way. So that's an interesting challenge. ADAMSON: At least there's nothing dangerous. It's not like we have, you know, poisonous snakes or anything like that. KROPUENSKE: Well, I have a running tick count every collection. ADAMSON: Ticks are probably the most dangerous thing we have here, right? KROPUENSKE: Yeah. ADAMSON: How long has this site been used as a test site for Landsat? IRWIN: When they introduced the Level 2 product for Landsat, so the surface reflectance product, it was decided that we should probably have a way to validate the surface reflectance products. So we started working toward that. In 2021, we first started working with the EROS facilities folks on where we might try to do this. Part of the reason we selected the northwest corner was, again, directed by facilities, because at some point we thought that we may ask them to mow the site to make it more uniform, if you will. ADAMSON: They still don't mow it, though. We're just letting the grass grow. Is that still okay? Does it still work well as a good site? IRWIN: Yeah, I think it's a good site for us. Again, we're trying to do validation. ADAMSON: Yeah. IRWIN: So we want the, if you will, the, the dirty sites. ADAMSON: Yeah, okay. IRWIN: Because, you know, calibration is where you want the best information possible so you can make the sensor work optimally, but validation we're looking for the dirty areas so we know how good our calibration is, if you will. ADAMSON: What benefits does this add to the validation work? I guess the blunt way to put it is, why do this? IRWIN: We're producing a surface reflectance product. People around the world are consuming this product. Landsat is considered the gold standard in terms of its calibration. You know, we want to find out if there are issues, be it in the atmospheric correction algorithm or in any of the specific bands that Landsat measures in different types of land cover. Vegetation is difficult because it's darker and there's not always a lot of return of the signal that the system is measuring. So that's why we're looking at vegetation primarily and trying to ensure that we're delivering good product that's reliable. ADAMSON: Besides Landsat, are there other times that you're out there taking measurements as well? KROPUENSKE: Sentinel goes over every five days. ADAMSON: The European Copernicus Sentinel satellites. KROPUENSKE: Correct. Sentinel 2A-- or, 2B and 2C at this point it is now. ADAMSON: Ah, okay. KROPUENSKE: And when we have a dual overpass, when Sentinel and Landsat are overpassing on the same day, those are kind of a priority collect. You know, we're getting a good cross comparison between two platforms. And EnMAP, beings it has a variable-- it has a cross track degree of about 30 degrees out from ground track. And so they overpass more often. ADAMSON: EnMAP is a satellite from where? KROPUENSKE: That's the DLR, Germany. ADAMSON: And you do the exact same thing for all those. Is it the same routine? KROPUENSKE: Same routine. ADAMSON: How much of this work is also in preparation for Landsat Next? IRWIN: You can view the-- supporting the Sentinel and EnMAP missions as, in some ways, part of that because Landsat Next architecture will be quite a bit different. And some of the bands will be very similar to the bands that Sentinel uses. So it behooves us to understand those parts of the electromagnetic spectrum as well. EnMAP's a little bit of a different animal. It's the same spatial resolution as Landsat, but it's a hyperspectral mission, which means it's collecting a lot more bands than Landsat will. But as we transition to Landsat Next, we'll also have a lot more bands than we currently do. So again, we're supporting the commissioning of these European instruments by collecting data for them. But it's also potentially beneficial to us. ADAMSON: At this point, since a Landsat pass was coming up, we needed to head out to the field test site. It really couldn't be a nicer day for this, though, right? Is there better conditions than we have today for these kind of collects? IRWIN: This is about as good as it gets in eastern South Dakota. ADAMSON: Yeah, it's probably like 78 degrees. The sky is nice and blue. Not really any clouds to speak of. Nice and dry too. Travis, can you tell me about what you're setting up over here? KROPUENSKE: Sure. We're using two reflectance panels today, and I'm setting up the A panel on the tripod. And inside is roughly a 12 by 12 inch reflectance panel with 99% reflectance. And they do tend to degrade over time, and so we keep them covered until needed. And we try to keep our setup geometries all the same. The same face at the sun all the time. So there's consistency to our setup and to our measurements then. ADAMSON: The same spot that you always set it up? KROPUENSKE: Correct. We've got one face of the box that is pointed at the sun. And it's a consistent measurement. ADAMSON: For those who aren't aware of where EROS is located, we're about 10 miles north of Sioux Falls, South Dakota, sort of in the middle of cornfields and soybean fields. EROS is on a half section of land, so there is some space to accommodate one of these test sites. Okay, to the extent that you can, can you tell me about what you're wearing? KROPUENSKE: Sure. This is an ASD FieldSpec 4 spectral radiometer. I've got it strapped to my back, but it's essentially the same spectroradiometer that is set up as the fixed base unit, except this one is mobile with me. ADAMSON: Okay. KROPUENSKE: It's attached to a laptop, which records the collected data. ADAMSON: It's kind of a heavy backpack. Does that weigh you down? Does that wear you out out here? KROPUENSKE: It's not terrible, but you notice it, I'll say. ADAMSON: Okay, okay. Tell me what you're holding in your right hand right there. KROPUENSKE: Attached to this painting roller stick-- ADAMSON: Okay, we just rig up whatever we can, don't we? KROPUENSKE: We've repurposed it, say. And, we've got an 8-degree foreoptic, which is where we're measuring-- where the light enters to measure. ADAMSON: Okay, great. KROPUENSKE: And I'll hold that out ahead of me, out of my shadow, so we're always getting clean light. I like to think of it as, you know, it's the same as the Landsat satellite, only smaller in my hand. ADAMSON: Only a meter and a half off the ground and just getting a really, really small area at a time. KROPUENSKE: That's right. ADAMSON: But it's measuring the same--the same stuff. KROPUENSKE: We're sampling what Landsat is getting. And hopefully what we're measuring is going to validate what Landsat has. ADAMSON: Why did you call it an 8-degree? What does the 8 degrees mean? KROPUENSKE: That means that there's an 8-degree cone radiating out from the center of that foreoptic. ADAMSON: That measures the cone that you're measuring straight down-- The Air National Guard is also busy. We've got time. We're just waiting for the satellite pass to start anyway. There's the other one. There's usually two. Okay. So this is looking straight down, and then that's the size of the cone as the circle hits the ground. KROPUENSKE: Correct. Correct. ADAMSON: Okay, sounds good. How far do you walk, do you figure? KROPUENSKE: 150 times eight is eight, 1200 meters, plus I'll forget about the little side steps in here. ADAMSON: Definitely more than a kilometer anyway, is what it comes down to. You're getting a little bit of a hike in here today. But the terrain looks pretty easy. KROPUENSKE: It's not bad. There's just, you know, I like to keep an eye on the ground because it can be dynamic. ADAMSON: It's not exactly flat. There's just a little slope. KROPUENSKE: Yeah, not a terrible uphill. We've got a little minor ditch through that adds some flavor. ADAMSON: Okay. Do you walk the same path, the same transect? Do you have that kind of figured out? You have to walk this path every time? It's not like worn down though. KROPUENSKE: It's not terribly worn down. The grass is somewhat resilient. It, it seems to handle that. I try to stay consistent. Being my survey background, I'm always counting my steps. And I can't really go anywhere without counting steps. ADAMSON: Travis started by getting a reading of the white panels. What's the purpose of that? IRWIN: So the purpose of that is to provide another known reference point as he's collecting. And then as he goes along, we'll have him collect this panel again occasionally. ADAMSON: Okay. IRWIN: And then we can do a, assuming the atmosphere stays the same, we can do a linear interpolation between the two white panel collects. ADAMSON: Sure thing. Okay. There's a couple other instruments out there. Can we talk about what those are? Are they related to what you're doing today? IRWIN: So those are what we call ground viewing radiometers. They were designed and built by the University of Arizona, one of our university cooperators. They are an eight-band instrument. They're essentially doing the same thing that we're doing, except they're measuring just one spot. And each of those has a field of view on the ground that's roughly a foot and a half that it's staring at. So they all have solar panels on them and some other instruments, like a moisture sensor. And so they know essentially when it's light out, when it's warm enough to operate and when it's raining. And so, you know, given the proper conditions, they will take a measurement every 2 to 5 minutes, depending on how we program them to do that. That data is all collected and processed over the internet, cellular information. And University of Arizona processes it for us and passes it back, and they give us a reflectance value. The challenge with those things is they're literally only looking at three different spots on the ground throughout the field, where we're trying to get a more comprehensive view by walking transects through the field. ADAMSON: Okay. Well, we're kind of gathering lots of data anyway. Lots of different types of data. That's kind of the point here, isn't it? IRWIN: Yeah, we're also experimenting with UAS, through our colleagues at the National Uncrewed Systems office in Denver, again to see if we can expand this sort of work to areas that are less accessible for walking. We also have university partners at SDSU analyzing similar technologies to the ground-bearing radiometers that are small portable radiometers that a farmer could use in his field and are low cost. And so they're looking at putting a calibration on those and seeing if they can do the same thing that way. KROPUENSKE: 479 ends B. ADAMSON: I'm going to go follow Travis a minute. Well, he's got a little bit of a path here to walk down. I wouldn't say he's walking fast, but he's moving along pretty good. There are a few little pathways kind of cut through here, like you've been here before. KROPUENSKE: Yep, maintaining our consistency. ADAMSON: Okay. Very good, very good. The, what do you call it at the end, the foreoptic? KROPUENSKE: That's correct. ADAMSON: Okay, he's got that off to the right side a little bit, so it's out of shadow. You're trying to walk at about the same speed all the time, too, right? KROPUENSKE: That is right. We've got roughly a five by five pixel area. And we try to get the same amount of shots per pixel. ADAMSON: Oh, okay. KROPUENSKE: And sometimes the instrument will mess up and so I count my paces, so I kind of know where it missed. And I can go back if needed. ADAMSON: Oh, okay. Okay. I'm messing up your count now, I realize. Sorry about that. KROPUENSKE: Oh, you're fine. ADAMSON: You're just gathering as much data as you can. You can kind of check while you're out here to make sure it's good. KROPUENSKE: Yeah, yeah, we've got a little bit of time. We could correct something minor, but-- ADAMSON: Okay. KROPUENSKE: We'd hate to lose a full collect, you know. ADAMSON: Right. Especially on a nice, clear day like this. But you do have to watch your step at the same time, don't you? KROPUENSKE: Yeah. The laptop isn't the best transparent device. ADAMSON: The laptop's right in front of you. KROPUENSKE: Yeah. Some of the burrowing critters are-- they'll get active, and all of a sudden there might be a obstacle in your path. ADAMSON: Yeah, you probably get used to these pathways out here, but the wild animals, they don't really care. KROPUENSKE: No, no, they don't understand. ADAMSON: Okay, I'll leave you to it. Keep walking. What were you doing with your phone there, Jeff? IRWIN: So I take photos periodically throughout the collection so that if anything looks anomalous in the data processing, they can go back to the photo and see if we had clouds move through or something else. ADAMSON: Just a little more verification to be ready for. Okay. How do we know what time Landsat is passing over? IRWIN: There is actually a Landsat Acquisition Tool out there on the web where you can go and find out anywhere in the world what time Landsat will be overpassing your part of the world. ADAMSON: Okay. That's public information, right? IRWIN: That's public information. ADAMSON: That's all you're using, right? IRWIN: Yes. ADAMSON: It's not like you can look up and see it. IRWIN: No, no, it's doing an orbit every 90 minutes. So, I don't know what that translates into miles per hour over the ground, but it's pretty fast. ADAMSON: It is fast. I'm always telling people it moves about 17,000 miles per hour. IRWIN: Okay. ADAMSON: Travis, on the other hand, isn't going that fast. How long is this pass going to last? IRWIN: It's going to take us roughly 26 to 28 minutes to collect the entire field. ADAMSON: Okay. At the same time Landsat's passing over. It's not like it's taking the image of this area for 26 minutes. IRWIN: No, I'm just saying it's going to take us 26 minutes. ADAMSON: It takes you that long. That's it. Okay. IRWIN: Right. ADAMSON: The actual Landsat pass is only about 15 minutes over North America, something like that. IRWIN: I believe that's correct, yeah. ADAMSON: Okay. You're not getting tired yet, are you? KROPUENSKE: Not yet. ADAMSON: Okay. Good, good. KROPUENSKE: We're in the last mile. ADAMSON: Last mile? The homestretch. Here you go. KROPUENSKE: 469 ends A. IRWIN: Got it. ADAMSON: What did those numbers mean, Jeff? IRWIN: So those are the numbers of measurements that he took during the transects and over the panel. And we'll use those to process the data. I don't know if he told you or not, but he's got a little GPS puck on his shoulder. ADAMSON: No. IRWIN: And that's how we correct for where the measurements are located at in the field. ADAMSON: Okay. How accurate is that GPS? IRWIN: Plus or minus 10 meters. ADAMSON: Okay. Okay. That's still pretty good. IRWIN: Yeah. ADAMSON: Okay. That gives you enough accuracy for that. IRWIN: Yeah. We're trying to compare to a 30-meter Landsat pixel. ADAMSON: Definitely you're within that. All right. So I don't want to jinx it here or anything, but what if you find something that doesn't match in the data? What if you find some surprises in the data? IRWIN: We don't like surprises. So then, yeah, we have to dig in and track it down and try to figure out what happened, what went wrong, what it was. We don't often get surprises. ADAMSON: It'll go back to the Cal/Val team anyway to look into, to investigate? IRWIN: Travis will process the data after we get back in. It takes about a half a day to do that. And then we pass it off to more of our analysts who grab the imagery and look at the reflectance measurements from the imagery and compare that to what we collected on the ground. ADAMSON: Yeah. Okay, sounds good. Thank you to Jeff and Travis for letting me tag along and pester them with questions while they did their data collection at the EROS test site during a Landsat overpass. That data collection helps validate the carefully calibrated Landsat data to ensure its reliability. And thank you, listeners. Check out our social media accounts to watch for all future episodes. You can also subscribe to us on Apple and YouTube podcasts. VARIOUS VOICES: This podcast, this podcast, this podcast, this podcast, this podcast is a product of the U.S. Geological Survey, Department of Interior.