In episode 53 of Forecast, Mike talks with Julia Pongratz from the Max Planck Institute for Meteorology about the role of land cover and land use change in the climate system. Julia began working on the topic with an unbelievable challenge: simulating the impacts of LCLUC over the past millennium. Now her interests encompass geoengineering, climate mitigation and model intercomparisons, with a focus on understanding the ever-complex interactions among biophysical and biogeochemical feedbacks. Also, Julia assures Mike that, unlike in Maine, the ticks aren’t too horrendous in Germany. Probably. At least in the big cities.
In episode 52 of Forecast, Mike and Marilyn Raphael from the University of California at Los Angeles talk about Antarctic sea ice. Arctic sea ice is, on a relative scale, well understood: observations and models show a massive decline. Antarctic sea ice is weirder. Overall, the extent of Antarctic sea ice is increasing, slightly. But this masks nearby areas with both large increases and decreases. Mike and Marilyn discuss the many mechanisms that might be underlying the interesting and somewhat bedeviling trends, as well as the multitude of ways in which Antarctic sea ice interacts with the broader climate system. We wrap up with a personal discussion of what it’s like being an introvert in science, and some ways to navigate the often-draining interpersonal demands.
In episode 51 of Forecast, Jérôme Chappellaz regales Mike with all manner ice core tales. The early days of discovering that methane varies hugely between glacial and interglacial states; profligate consumption of ice in the early days; the intensely competitive yet fundamentally friendly nature of the field; the ever-present need to take scientific risks; documentary film making. Spontaneity, chance and inspiration dominate the conversation. Jérôme’s insomnia while in Antarctica leads to the crazy dream of Subglacior, a radical development in ice core technology, and a meeting with royalty leads to funding for the Ice Memory project. Perhaps unique among the geosciences, the ice core community and Jérôme in particular are constantly faced with disappearing/melting records, and the pressing need to create an ice archive for the next generation and whatever hammers will be in their toolbox. Leading to … sequencing the history of the Black Plague from ice cores, maybe?
In episode 50 of Forecast, Julien Emile-Geay from the University of Southern California calmly presents a somewhat radical world view. Love of jazz as a means of selecting a grad school; universities as revolutionary institutions; pursuit of science as a subversive activity. Even more unusual: considering data and models not as separate entities, but as co-equal, and integral, facets of research into paleoclimate dynamics. For example, Julien is leading efforts on both massive data compilations, and on the massive Last Millennium Reanalysis. Progress is coming on many fronts, including ENSO dynamics, the always-controversial topic of solar-climate interactions, and low frequency climate variability — what Julien calls the “bassline of the climate soundtrack”.
In this episode of Forecast, Jess tells Mike about the origins of the TEX86 temperature proxy — an index of membrane lipids produced by mesophilic archaea. The origins in the 1980s in extreme ocean environment; discovery of membrane production in a huge range of environments; brute force discovery of the index; the inevitable struggles to understand what it actually represents; an unusually active and sometimes dismissive debate about its usefulness. All proxies have issues, but Jess and her colleagues are converging on the what/when/where for TEX86’s application. For Jess, work on TEX86 (and other methods!) is leading to an improved understanding of the atmospheric dynamics, surface processes, and feedbacks governing past climate variability, particularly in the tropics.
Kevin Anchukaitis from the University of Arizona is probably best known for his work on dendroclimatology, but this is changing quickly. Now, his broader interests in the connections among history, political science, archaeology, statistics, climate modeling, and forward modeling of proxies are increasingly mirrored within the broader field of late Holocene paleoclimate research. Now, it’s possible to bring together this astonishingly wide range of evidence to disentangle, for example, the influence of volcanic eruptions on climate and society. It ends up sounding like a golden age for climate science, if not for the extinct Monteverde golden toad, whose extinction Kevin showed to be due to a fungal disease coupled with natural climate variability. As always, with good science, you have to go where the evidence takes you.
People find science for all kinds of reasons. Some are born to it, but usually not. Most people find science by bumping into it at a bar, getting help from it while fixing a flat tire, seeing it alight on a leaf, iridescent, or watching it pass by on a subway car going the other way.
For Kaustubh Thirumalai (Kau), the stage was set with burnout on chemical engineering in India coupled with a side job reviewing comics and black metal for a friend’s website. Then, almost randomly searching for an interesting internship, he hooked up with Prosenjit Ghosh, for whom he worked as a local fixer, helping to procure parts for the construction of a mass spec. After that, it was geosciences, full-on: a move to the US, interests in the techniques and concepts of paleoclimate, and an ever-expanding network of collaborators. But still comics and metal! Just now with a splash of trace metals — little bundles of strontium and company, waiting to be discovered.
Intro music is from the album Terminal Redux by Vektor, ranked by Kau as the #1 metal album of 2016. Extro music is Quartz, by Kau himself. All music used by permission — thanks Dave and Kau! Photos are by Kau, used by permission.
Sometimes papers in Nature are incomprehensible to anyone other than a hard-core specialist. Yes, we use press releases, News & Views, and other reporting to make the leap to our broader readership. But for bringing science to the general public, no amount of Carl Sagans, Neil deGrasse Tysons, or Bill Nyes is going to get the job done. You need journalists. Journalists like Rob Meyer from The Atlantic, who are producing an astonishing amount of great content on topics like the Paris Agreement, fracking regulations, and Antarctica. Rob talks me through his path from music major to twitter procrastinator to Atlantic writer. I flip the usual Nature-related questions around to Rob: how do you select stories, frame them for your audience, and discuss the policy implication? And what is the rationale for the New York Times hiring Bret Stephens? Definitely a story there.
The causes of heat waves are kind of like the controls on a car. We know that pressure systems, land-atmosphere interactions, and modes of variability like ENSO act to control extremes, just as we know that the steering wheel, moderated by the brake and gas pedals, controls the direction and velocity of the car. But imagine driving a car blindfolded. Yes, you know what the controls do, but the chances of hitting something hard are pretty high if you keep the gas pedal down, careening across even the most familiar of roads. For extremes, the moment-to-moment, season-to-season occurrence of extremes will remain challenging to predict, like the exact moment at which you’ll veer out of your lane, but the coming impact of blindly increasing emissions is more certain. Sarah Perkins-Kirkpatrick from the University of New South Wales endured the horrendous heat of Australia’s 2017 summer – pregnant, in a badly insulated house with wobbly air conditioning – and is studying heat waves and how they will change in a persistently warming climate. As Sarah tells Mike, the news is almost uniformly not good. Unless the foot comes off the gas pedal, the car is going to hit the wall: rare events in today’s climate are likely to become seasonally persistent; different emission pathways might delay but won’t alter the ultimate arrival of catastrophic heat. Of course, society could adapt, and Australians could end up living the bulk of their lives in air conditioned spaces, at the cost of further emission increases, radical changes to lifestyle, and eye-popping expense. Is this the world we want? Let’s hope not, but the mitigation equivalent of self-driving cars is not going to magically appear. It’s just us.
The field of environmental economics in general — and climate economics in particular — is exploding. And my guest on episode 44 of Forecast, Solomon Hsiang from UC Berkeley, is helping to crack open some of the recalcitrant oyster shells of the field. How does climate influence conflict, migration and economic productivity? We talk through some of the big challenges in addressing these topics: the frequent impossibility of running experiments and the accompanying use of quasi-experiments; the growing use of — at last! — data; how incredibly hard it is to disentangle the influence of single factors — like climate — in a complicated human system. In many ways economics is decades behind physical sciences. As Sol explains, we’ve now for the most part forgotten about the initial debates regarding fluid dynamics, but economics is still very much at the phase of figuring out elementary processes. Sometimes this means that the major findings reside in statistical approaches, without clear mechanistic understanding. But Sol and his colleagues are working towards linking microscale human decisions to aggregate societal processes, and it is this sort of understanding that will, and indeed already is, proving important in a policy context.