PROFILE

Profile of Eric Rignot PROFILE Brian Doctrow, Science Writer

Sometimes taking a step back helps to see things more clearly. Eric Rignot, a glaciologist at the Univer- sity of California, Irvine, has found that when studying the behavior of glaciers and ice sheets, it helps to take a giant step back, all of the way into space. His use of satellite radar imaging has provided extraordinarily detailed information about how fast the ice sheets are melting and how much they contribute to sea-level rise. Rignot’s findings have shown the impact of cli- mate change on the ice sheets and how little time there may be to stop it. His work has earned him nu- merous honors, including fellowship in the American Geophysical Union in 2013 and membership in the National Academy of Sciences in 2018.

Finding His Calling Eric Rignot grew up in what he describes as a rugged part of the French countryside, near the city of St. Etienne. Rignot partly attributes his interest in polar environments to the rough winter weather he experi- enced growing up. As a child, he enjoyed reading novels about polar adventures. He also recalls reading about Nobel Prize winners in an encyclopedia as a kid, which exposed him to the explosion of scientific knowledge that emerged in the early 20th century. Eric Rignot. Image credit: Ian Fenty (NASA/JPL-Caltech, Pasadena, CA). This kindled a lifelong fascination with science and the natural world. to realize the value of having an education with a broad As a student, Rignot pursued studies in mathe- foundation, because it gave him the flexibility to branch matics, in part because in the French educational out into new fields. system, math promised to open up the most doors. At the Ecole´ Centrale, Rignot found a scientific mentor “If you’re good in math,” he explains, “you can basically do whatever you want.” Nevertheless, in Sebastien ´ Candel, currently the president of the French Rignot was not introduced to physics until high Academy of Sciences, who encouraged Rignot to pursue school and for a long time wanted to become a research. After graduating from the Ecole´ Centrale in 1985, veterinarian. At age 17, Rignot met an engineer who Rignot was faced with a conundrum. He was interested encouraged him to go to engineering school. “He in aeronautics, but not in working for the defense in- seemed so sure, expressing no doubt that I could be dustry, where most of the jobs in aeronautics were. ‘ successful, that I thought, well, maybe I should try Instead, Rignot studied astronomy and astrophysics at that,’” Rignot recalls. Paris-Sorbonne University, obtaining a Master’sdegree Rignot studied engineering at the Ecole´ Centrale in 1986. However, Candel persuaded him not to pursue Paris, where he took classes in physics, chemistry, “ ‘ ’ math, and economics. At the time, Rignot says, he was a career in astronomy. He told me, Eric, you re going skeptical about the multidisciplinary curriculum. He to compete with the top, brightest minds in the country thought, “I’m going to come out of this engineering [for] maybe one or two spots every year,’” recalls Rignot, school not having any specific skills.” Later, he came who did not consider his odds of success to be good.

Published under the PNAS license. This is a Profile of a member of the National Academy of Sciences to accompany the member’s Inaugural Article, 10.1073/pnas.1812883116.

www.pnas.org/cgi/doi/10.1073/pnas.1821951116 PNAS Latest Articles | 1of3 Downloaded by guest on September 26, 2021 Rignot turned to another of his interests: remote them,” says Rignot. “I was fortunate to be there at that sensing, then an emerging field. Although the Landsat time, have the right push from the right people, such program had been acquiring satellite imagery of Earth as future assistant JPL director Jakob van Zyl, to go for more than a decade, many significant develop- into that direction.” ments were still in the future. would In the early 1990s, the technique of radar interfer- take advantage of Rignot’s background in aeronautics ometry emerged at JPL, led by pioneers, such as ra- and fluid mechanics. dar astronomer Richard Goldstein. In this technique To help prepare for remote sensing research, a single location is imaged at different times, and Rignot came to the University of Southern California, the phase of the reflected radar pulses is recorded. where he obtained additional Master’s degrees in Changes in the height or angle of the ice surface show aeronautical and electrical engineering. Rignot par- up as changes in the phases. The technique is sensi- ticularly enjoyed the freedom that his mentor, Fred- tive enough to measure millimeter-sized deformations erick Browand, offered for him to solve problems in of the ice and provides measurements of the ice ve- his own way and at his own pace. Rignot believes locity, thickness, and rate of discharge into the ocean. that some of the most influential people throughout In 1998, Rignot published an analysis of satel- his career were the ones who gave him this kind of lite radar interferometry data from the Pine Island freedom. Glacier in West (2). As early as the 1970s, Through Candel, Rignot was introduced to Charles researchers had suggested that this region of Ant- Elachi, then an assistant director at NASA’s Jet Pro- arctica might be vulnerable to . How- pulsion Laboratory (JPL) in Pasadena, California. Rignot ever, Pine Island Glacier is remote even by Antarctic got a job at JPL as a radar engineer in 1988. He quickly standards; it is one of the farthest points from any realized that what he really wanted was to be in charge manned station, so observational data on the glacier of his own research program—to “be his own boss”— were minimal. and that to do so, he would need to get a doctorate. Rignot measured the location of the grounding Fortunately for Rignot, JPL had a program that would line—the boundary between ice resting on solid fund his doctoral education, and for two and a half ground and ice floating on water—to within 100 me- years he continued to work at JPL while pursuing his ters, compared with the many tens of kilometers-scale doctorate in electrical engineering at the University accuracy with which it had been previously known. of Southern California , which he received in 1991. An He further found that between 1992 and 1996, the article Rignot published in 1993 with Jakob van Zyl grounding line retreated by more than a kilometer based on his doctoral research on detecting changes per year, suggesting that the ice was thinning much in radar images remains among his most highly cited more rapidly than thought. At the time, conventional papers (1). wisdom held that ice sheets and glaciers changed on a timescale of centuries, but Rignot’s results revealed Observing Glaciers from Space that large changes could occur on time scales of de- At JPL, Rignot worked on a remote sensing technique cades to years. In honor of Rignot’s contributions to known as synthetic-aperture radar, in which a radar glacier dynamics, a glacier in Antarctica near Pine antenna is mounted on a moving platform, such as a Island Glacier was named the Rignot Glacier in 2003. satellite. The continuous motion of the radar antenna increases the effective size of the antenna, thereby From NASA Engineer to University Professor increasing the resolution of the image relative to a Rignot remained at JPL until 2007, when he moved to stationary antenna. A major advantage of radar for the University of California, Irvine. Although he had remote sensing is the ability to see through clouds. As been successful at JPL, Rignot felt isolated intellec- Rignot puts it, “every day is a sunny day.” At the same tually, working mostly by himself. Moreover, it was time, NASA happened to be developing a program to difficult to form a research group with competitive study glaciers and sea ice in the polar regions, and funding, and many regulations restricted his scientific Rignot used synthetic-aperture radar to study changes freedom. In contrast, the University of California, Irvine in the polar ice. At the time, there was little observa- offered him a guaranteed salary, academic freedom, tional data available. “It was clear that nobody knew and the opportunity to form his own research group. for sure what the was doing in “Coming to [University of California, Irvine] made me response to climate warming,” he explains. As a result, reach a completely different level,” says Rignot. “It Rignot felt that it was an area where relatively little broadened my view of Earth science in general, on the investment in effort could yield large returns. “I think connectivity between what I was working [on] and the that’s something that’s stuck for me throughout my bigger picture of the Earth as a system.” career,” says Rignot, “to identify the areas that seem Rignot continues to work for JPL as a consultant. important but where our knowledge was especially He was a contributing author to the Fourth Assess- poor and we needed to explore.” In the beginning, it ment Report (AR-4) of the United Nations Intergov- was not exactly clear how remote sensing would be ernmental Panel on Climate Change (IPCC). “I was useful in studying polar ice. “Pretty soon I realized I’d very excited about AR-4,” he says. “AR-4 was a turning stepped on a gold mine of information about polar point in the IPCC story, where the report came out regions from remote sensing techniques that were very strongly as saying the signal from anthropogenic changing completely the way we were looking at emissions in the climate system was unequivocal.”

2of3 | www.pnas.org/cgi/doi/10.1073/pnas.1821951116 Doctrow Downloaded by guest on September 26, 2021 The 2007 Nobel Peace Prize was attributed to the times greater than in the 1980s. In addition to the well- authors of IPCC AR-4, along with former US Vice studied contribution of West Antarctica to sea-level President Al Gore. Rignot subsequently was the lead rise, Rignot also found a significant contribution from author of the Fifth Assessment Report in 2014. East Antarctica, which has received comparatively little Around that time, the development of modern attention. regional atmospheric climate models enabled Rignot “Sea-level rise is probably one of the most telling to determine the mass balance—the net loss or gain in stories of climate change for humans,” says Rignot. mass—of both the Greenland and Antarctic Ice Sheets “Anyone can relate to the fact that their property is going over time, and thus their contributions to sea-level to be underwater, that people will have to migrate from rise, at the level of individual glaciers (3, 4). These where they live to go somewhere else, and that it’s studies revealed that the contributions of the Green- going to cost billions of dollars to displace infra- land and Antarctic ice sheets to global sea-level rise structures. Whether you’re poor or wealthy, you’re were increasing over time and likely to be the domi- going to be affected by it, although the folks who nant contributions to sea-level rise in the 21st century will suffer foremost are poor populations.” For (5). Furthermore, the melting of several West Antarctic Rignot, the message of his findings is clear. “These glaciers appeared to be irreversible (6). ice sheets are responding to climate change faster, In his Inaugural Article (7), Rignot and his col- sooner, and in a bigger way than anyone expected, leagues combined historical satellite data with climate and the fact that East Antarctica is a participant is model outputs to reconstruct the another signal that there is an urgent need to curb our mass balance over the past four decades. They found carbon emissions to avoid the most catastrophic sce- that the rate of mass loss during 2009–2017 was six narios of climate change,” he says.

1 Rignot EJM, van Zyl JJ (1993) Change detection techniques for ERS-1 SAR data. IEEE Trans Geosci Remote Sens 31:896–906. 2 Rignot EJ (1998) Fast recession of a West Antarctic glacier. Science 281:549–551. 3 Rignot E, et al. (2008) Recent Antarctic ice mass loss from radar interferometry and regional climate modeling. Nat Geosci 1:106–110. 4 Rignot E, Box JE, Burgess E, Hanna E (2008) Mass balance of the Greenland ice sheet from 1958 to 2007. Geophys Res Lett 35:L20502. 5 Rignot E, Velicogna I, van den Broeke MR, Monaghan A, Lenaerts JTM (2011) Acceleration of the contribution of the Greenland and Antarctic ice sheets to . Geophys Res Lett 38:L05503. 6 Rignot E, Mouginot J, Morlighem M, Seroussi H, Scheuchl B (2014) Widespread, rapid grounding line retreat of Pine Island, Thwaites, Smith, and Kohler glaciers, West Antarctica, from 1992 to 2011. Geophys Res Lett 41:3502–3509. 7 Rignot E, et al. (2019) Four decades of Antarctic Ice Sheet mass balance from 1979–2017. Proc Natl Acad Sci USA, 10.1073/ pnas.1812883116.

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