The Surface Water and Ocean Topography (SWOT) mission is producing NASA's first global survey of Earth's surface water. Given that Earth's warming climate is likely to alter the movement and accessibility of the planet's lakes, rivers, and reservoirs—resulting in significant societal impact—this information is both timely and necessary. Without an adequate inventory of these freshwater resources and the volume of water they store, it will not be possible to assess the effects of environmental change on agriculture, industry, and other sectors critical to livelihoods of people around the globe.
Fortunately, SWOT is up to the task. With its state-of-the-art "radar interferometry" technology, SWOT provides data from hundreds of thousands of lakes, as well as the discharge volumes of medium-to-large rivers. These measurements support a variety of research and help scientists study the dynamics of floodplains and wetlands; assemble a global inventory of water resources, including lakes, transboundary rivers (i.e., those that cross international borders), and reservoirs; and better understand the global water cycle on land.
That might sound like a tall order for one satellite, but Dr. Tamlin Pavelsky, freshwater science lead for NASA's SWOT mission and professor of hydrology at the University of North Carolina at Chapel Hill, reveals how SWOT's unique capabilities provide observations previous hydrology-related missions could not. He also discusses some of the practical applications for SWOT data, shares his suggestions for getting acquainted with SWOT data products, and explains why he finds the SWOT mission so exciting.
How does SWOT differ from and complement previous hydrology-related satellite missions?
There are two answers to your question. The first is that there have been a number of missions that observe different aspects of the water cycle. For example, data from the Gravity Recovery and Climate Experiment (GRACE) mission can be used to measure changes in groundwater storage and the Global Precipitation Measurement (GPM) mission is for precipitation, so in that sense, SWOT is adding to our body of knowledge on the water cycle. It tells us about surface water, about rivers and lakes and some wetlands, how much water is getting stored, how that storage is changing, and how much water is flowing through those water bodies. That's really important for quantifying the water cycle as a whole and SWOT is providing that new component.
The second is that, for the people who study rivers and lakes in particular, we have a long history of repurposing satellites that were really built to answer other questions about the planet's systems. We've used Landsat, which as its name implies, was really mostly built for people who were studying land, but we can use it to see where water is and how it's changing over time. We've repurposed altimeters that were designed for oceanography to get water levels of rivers and lakes, and so on. SWOT is really the first mission that is for surface water. Hydrology is part of the core of the mission, and so that's one of the things that makes SWOT really exciting for me.
So, in regard to studying Earth's water cycle, are you suggesting that SWOT, in conjunction with these other missions, enables scientists to track water as it moves through the entire water cycle?
In many ways, I think the Holy Grail of NASA Earth science is to be able to monitor the water cycle from space to understand how it's changing. For that to happen, we need to be able to track many of the different components of the water cycle and to be able to say, "Here’s what is happening with precipitation." We can see that with GPM. And then we bring in SWOT data and we can see what happens to, say, a flood wave that's moving down a river and maybe makes it out into the ocean. Then we can use SWOT to look at what's happening with topography and maybe we could use one of the sensors on another mission to tell us about its impact on ocean salinity, and then we can use another satellite to estimate to help us estimate evaporation. So, that is definitely a goal.
What can you tell me about SWOT's Ka-band Radar Interferometer (KaRIn) instrument, the observations it provides, and how they benefit the hydrological science community?
KaRIn is really new. There has never been anything like it on an orbital spacecraft. We've had other radars in space, of course, and we've had other radars that could do interferometry in space, but SWOT has a Ka-band radar, which has a wavelength of about a centimeter. Also, most radars look way off to the side whereas SWOT, while it's not quite looking straight down, is just barely off to the side.
What’s the difference between, for example, a one-centimeter wavelength and a six- or seven-centimeter wavelength, or a radar that looks way out here and not here? Well, it turns out these make a big difference. For example, with most other radars that we have in space, water looks dark and land looks bright. With SWOT, water looks bright. We get a lot of returns off of water surfaces and it's the land that looks dark. So, if you want to study what's happening with water, you want those returns off of the water surface. SWOT is just so unique and there were many questions about what we were going to be able to see with it that we simply could not answer before launch. So, it's really been a process of discovery for us.
What are some applications of SWOT data?
I like to say that freshwater is both the source of our superpowers and our kryptonite. On the one hand, it's our most important resource. We use it for agriculture. We use it for industry. We use it for drinking water, transportation, recreation; it's involved in almost everything we do. We have to have it and we need to know how much we have—and that amount changes over time.
At the same time, floods are the most expensive and most dangerous natural disasters worldwide. Droughts, the lack of water, can be incredibly damaging too. So, [freshwater is] both incredibly important and a hazard, and SWOT's going to help us with both of these aspects. We're going to be able to observe how much freshwater we have—the amount of water stored in pretty much every reservoir in the world—and how that amount is changing over time.