In the sixth episode of the Climate History Podcast, ​Dr. Dagomar Degroot interviews one of the world's best-known historians of science: Dr. James Fleming, the Charles A. Dana Professor of Science, Technology, and Society at Colby College. Professor Fleming is perhaps the leading historian of meteorology and climatology. He has degrees in astronomy, atmospheric science, and history, and he is the founder and first president of the International Commission on History of Meteorology. He is editor-in-chief of History of Meteorology, and he has written and reviewed for the IPCC. His extensive publications include Meteorology in America, 1800-1870 (Johns Hopkins, 1990), Historical Perspectives on Climate Change (Oxford, 1998), The Callendar Effect (AMS, 2007), Fixing the Sky (Columbia, 2010), and most recently, Inventing Atmospheric Science (MIT, 2016).

In this episode, Professors Degroot and Fleming  discuss how a plane crash launched Fleming's career, the deep history and future prospects of geoengineering, and the birth of modern atmospheric science in the early twentieth century. 

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In the fifth episode of the Climate History Podcast, Dr. Dagomar Degroot interviews the first returning guest in the history of the podcast, Dr. Sam White of Ohio State University, the co-founder and co-director of the Climate History Network. Professor White is perhaps the leading environmental historian of the "Little Ice Age," a period of global cooling that, according to some definitions, endured from the thirteenth through the nineteenth centuries. 

In 2011, Cambridge University Press published Professor White's first book, The Climate of Rebellion in the Early Modern Ottoman Empire. In it, Professor White argues that falling temperatures and a landmark drought contributed to famines the Ottoman countryside that in turn incited a bloody rebellion. The book won the Middle East Studies Association Albert Hourani award, the Turkish Studies Association Fuat Köprülü award, and the British-Kuwaiti Friendship Society prize for the best book in Middle East and Turkish studies. Professor White has authored a major new book, A Cold Welcome: The Little Ice Age and America’s Colonial Beginnings, which is forthcoming with Harvard University Press. You can click here to watch Professor White discuss the book. 

In this episode, Professors Degroot and White discuss the prospects for climate research in the Trump Administration; the influence of the Little Ice Age on the European colonization of the Americas; and a major new digital mapping initiative that they are developing with the financial and logistical support of Georgetown University and the Ohio State University. 

To listen to this episode, click here to subscribe to our podcast on iTunes. If you don't have iTunes, you can still listen by clicking here.  ​

Bruce Campbell is a highly respected historian of medieval economic history whose research and teaching has bridged many disciplines in the sciences and humanities. In his long and distinguished career at Queen's University, Belfast, he has belonged to the Departments of Geography, Economic History, History, and the School of Geography, Archaeology and Palaeoecology. Recently, he published a major new book: The Great Transition: Climate, Disease and Society in the Late-Medieval World​. The book transforms how historians have understood the quintessential crisis of Western society - its apparent collapse in the fourteenth century - by rooting it in environmental forces that include climate change. 

We are grateful to Professor Campbell for answering our questions. Professors Bathsheba Demuth, Dagomar Degroot, and Tim Newfield all contributed to them. 

HC: For people who haven't read your book, what is the "Great Transition" your title refers to? What makes the fourteenth century so pivotal?

BC: The title of my book refers to the unraveling of one inter-linked pan-Eurasian system of commerce connecting easternmost Asia with westernmost Europe (the system which allowed Marco Polo, his father and uncle, to travel from Venice to Beijing and back) via the caravan routes across the Middle East, and the birth of another based on the newly discovered sea route round Africa, from which eventually sprang Western Europe’s rise to global economic hegemony.

At the same time populations were greatly reduced, economic activity was scaled down, commerce was realigned and political and religious boundaries were redrawn. Nor was this all, for the atmospheric circulation patterns of the Medieval Climate Anomaly gave way to those of the so-called Little Ice Age and the Second Pandemic of Plague erupted and spread throughout the greater part of the Old World. It is the multi-dimensional and inter-linked character of these developments that made this extended transition so "great," plus the fact that no part of the Known World remained unaffected.

In this unfolding human and environmental saga the fourteenth century is pivotal because it marks the point of no return, when changes in climate, disease and society accelerated and became irreversible. This makes the century one of the most complex and fascinating in history, when the trajectory of change was altered in ways that determined the course of historical development for centuries to come.

HC: One of the major contributions of the book is that it forcefully argues for connections between disease, conflict, and climate change, in ways that are rarely (if ever) deterministic and rely on some cutting-edge scholarship to show how these factors worked hand in hand to unravel the fabric of medieval Europe. How do you see these three calamities -  disease, conflict, and climate change - as connected? 
​
BC: I am glad that you think the interpretations advanced "are rarely (if ever) deterministic." Certainly, my aim in writing the book was to eschew all forms of determinism, including those that stem from too exclusive a reliance upon economic models of historical change. Of course, climate, disease and society all had their own separate dynamics hence it is often more helpful to think in terms of conjunctures than connections, as expressed by the idea of a perfect storm, when several separate developments coalesced at the same point in time.

​But connections there certainly were, as articulated via the complex web of inter-relationships that connected humans and the natural world. These are the socio-ecological systems referred to in the book with their component elements of climate and society, ecosystems and biology, microbes and humans. ​

HC: Did the presence of one of these elements - the climate, the pathogens, or the social changes - make some of the others more likely? Can we see similar relationships at other points in human history? 

BC: The answer to both questions is yes. How human events unfolded over the course of the fourteenth century would have been entirely different in the absence of climate change and, especially so, in the absence of plague. Each element of this destabilising scenario compounded the effects of the others.

For parallel situations at other points in human history look no further than Geoffrey Parker’s Global Crisis: War, Climate Change and Catastrophe in the Seventeenth Century (2013) and John L. Brooke’s Climate Change and the Course of Global History: A Rough Journey (2014). The latter shows that crises of this sort have recurred throughout human history. If we broaden our analytical remit they come more clearly into focus and enrich the historical narratives we have to tell.

HC: You note the increase in climate variability in the fourteenth century. Do you see some societies as having adaptations that made them better able to deal with this instability?

BC: Away from environmental, political and military margins, Western Europe proved to be remarkably resilient to the increase in climate variability in the fourteenth century. Admittedly, there were stresses and strains and subsistence crises and famines, occasionally, as in the case of the Great Northern European Famine of 1313‑21, on a grand scale, but no tipping point was reached until plague (Yersinia pestis) intervened. In large part this was because of European agriculture’s intrinsically mixed-farming character, with its variable combinations of arable and grass, interchangeable choices of crop types and livestock types, and extensive use of working animals. Properly managed, these were innately sustainable farming systems and even quite serious short-term setbacks, as in 1315-21, could be quite quickly overcome.

It appears to have been otherwise in the case of the irrigation-based rice-growing farming systems of China and southeast Asia, with their narrower range of crops, far smaller pastoral sectors, and heavier dependence upon human labour. For them the failing reliability of the Asian Monsoon from the late thirteenth century proved to be far more challenging and destabilising than anything that northwest Europe had to cope with. The scope for comparative research into these kinds of issues is considerable.

HC: Disease also plays a huge role in your work. That the black plague reshapes demographics is something familiar to many historians, but you go into detail about how the "socio-ecological" context of the mortality crisis affected European responses. Can you explain what work the term "socio-ecological" does for you, and what kinds of variation it accounts for?

​BC: Analysis of ancient DNA has now established beyond reasonable doubt that Yersinia pestis was the pathogen responsible for the Black Death of 1346-53. The bacterium is still active in the world today and, in fact, plague deaths are on the increase, especially in such countries as Madagascar and in plague’s ancient reservoirs of Central Asia. This is attracting a great deal of serious scientific research that has revealed the range of wild mammalian hosts capable of harbouring the infection, the vital role played by fleas and maybe even lice in spreading it, the susceptibility of both to climate-driven variations in ecological conditions, and the role played by levels of human exposure to the relevant insect vectors in determining rates of infection.

Plague, in fact, is one of the most ecological of all diseases, but it is also closely associated with human poverty and patterns of mobility and communication. It was much the same in the late-thirteenth and fourteenth centuries. What I have attempted to show is that to understand the origin and spread of the Black Death it is necessary to reconstruct this web of socio-ecological relationships. Recent progress on this front has been impressive but there is still a great deal more to be learned.

HC: What do you think about the recent historical and palaeomicrobiological scholarship that suggests the plague bacterium established enzootic foci in Europe after the Black Death? How does this affect our understanding of late medieval and early modern plague? 

BC: The jury is still out on this one. One school of thought believes that, impelled by short-term climate shocks, plague was repeatedly reintroduced to Europe from reservoirs of infection in Central Asia, although so far only the initial outbreak that started in the Crimea in 1346 has been tracked in detail.

Alternatively, it has been hypothesised that semi-permanent reservoirs of infection became established in Europe, either among urban colonies of rodents in the greatest ports and cities or in their ground-burrowing sylvatic cousins, such as the Alpine marmot. After all, in most parts of the world where enzootic plague foci have become established, it is wild mammals in thinly populated rural areas that maintain it. In such cases, as exemplified by Madagascar, small mutations soon promote the evolution of geographically-specific lineages of the Yersinia pestis genome.

The proof of whether or not enzootic plague foci became established in Europe will therefore hinge upon whether aDNA analysis can identify specifically European variants of the genome. So far no such evidence has been found, but then these are still early days for this most expensive branch of bio-archaeological research. The answer is important because it bears upon the ability of medical historians to explain how plague seemingly managed to sustain itself in Europe for so long, especially given the long intervals between some outbreaks, why it eventually disappeared, and the extent to which plague outbreaks in Europe were driven by fluctuating environmental conditions in Central Asia.

For historians of plague these are the big questions to which satisfactory answers have yet to be found. Meanwhile, there is plenty of more conventional historical research to be done, tracking the course and estimating the impact of the second outbreak of plague in 1360-63, and improving upon Jean Biraben’s pioneering chronology of European plague outbreaks.

HC: New reconstructions of the North Atlantic Oscillation (NAO) have challenged previous reconstructions that showed a persistently positive NAO during the Medieval Climate Anomaly, and a negative NAO in the centuries that followed. The scientific state of the art can change much more quickly than the historical state of the art. What does that mean for histories that draw equally from scientific and documentary evidence? 
​
​BC: Keeping up with the advances in knowledge being made by climatologists and biologists is a real challenge. Medieval historians have not been idle but, you are right, the historical state of the art changes much more slowly. This discrepancy will certainly keep us on our toes and engender a constant process of iterative rethinking. It will also make study of the medieval centuries more dynamic, pertinent and exciting.

​Above all, it challenges us to come up with more and better historical databases and chronologies to enable more rigorous analyses of the interactions between environment and society. In this context, it should not be forgotten that historical archives contain a rich trove of information that can be deployed to shed light on past environmental conditions. Of course the histories we write using the imperfect information available today will soon need to be revised and certainly will eventually be superseded, but this should not deter us from writing them.

HC: Your background is as a Medieval economic historian specializing in England, if I'm correct. How did you move to write a global environmental history?

BC: In fact, my initial training was in geography, which required me to think comparatively and on a large scale and pay due attention to environmental and human agencies and processes. My doctoral research then focused in on three exceptionally well-documented medieval Norfolk manors. This was when I started using manorial accounts to measure crop yields and using manorial court rolls to chart the influence upon the market in customary land of years of dearth and glut. This work left me in no doubt of the magnitude of the impacts upon these crowded and impoverished rural communities of the terrible harvest failures of 1315‑17, the great cattle panzootic of 1319 and, above all, the outbreak of the Black Death in 1349.

Back in the early 1970s it seemed to me that none of the then current historical models was capable of accommodating the environmental dimensions of these disasters. Nor had the detailed climate reconstructions been undertaken that would have allowed me to place these events in their broader socio-ecological context. But my interest was aroused and the proxy climate series are now available that have enabled me to write what is intended to be less a global environmental history than an economic history of a formative era, taking full account of the contribution made by global environmental process.

​Of course, in 2010 when I began this book project I had no idea that it would lead me to ponder the influences of varying levels of solar irradiance upon ocean-atmosphere interactions in the Pacific Ocean or those of alternating droughts and pluvials upon the enzootic foci of plague in Arid Central Asia. The academic challenge of so doing has been daunting, occasionally almost overwhelmingly so, but it has more than repaid the effort and the book will, I hope, encourage others to challenge its findings and take the subject and this approach further.

HC: Do you see any lessons from this period for the present?

BC: History, as we know, never repeats itself but there are always lessons to be learnt from it. The serious risks posed by climate, disease and conflict have not gone away. What the ‘Great Transition’ demonstrates is the intrinsic instability of climate systems, the weather extremes that can materialise seemingly out of the blue, the punitive power of microbes when unchecked by science, the economically disruptive impacts of armed conflict, and the sheer bad luck of several extreme events occurring at much the same time. Above all, the fourteenth century shows that the status quo of centuries can be overturned. ​

For the fourth episode of the Climate History Podcast, Dr. Dagomar Degroot interviews one of the world's leading environmental historians: Dr. John R. McNeill of Georgetown University. Professor McNeill has authored or co-authored six books, and edited or co-edited twelve. He is perhaps best known for Something New Under the Sun: An Environmental History of the Twentieth-Century World, which won the book prizes of the Forest History Society and the World History Association. He also wrote Mosquito Empires: Ecology and War in the Greater Caribbean, 1640-1914, which was awarded the Beveridge Award of the American Historical Association. McNeill has authored or coauthored well over 50 articles in journals that span the scientific and humanistic disciplines, ranging from Science to Environmental History. He is a past recipient of a MacArthur Grant, a Toynbee Prize, and a Guggenheim Fellowship, among many other awards. 

In this episode, Professors Degroot and McNeill discuss the "Anthropocene:" the proposed geological epoch distinguished by humanity's profound transformation of Earth's environment. McNeill is currently a member of the Anthropocene Working Group for the Subcommission on Quaternary Stratigraphy. This body of experts recently recommended that International Union of Geological Sciences consider the Anthropocene a new geological epoch, with a starting date of around 1950. Professor Degroot therefore asks Professor McNeill about alternative starting dates, criticisms of the Anthropocene concept, and the special place of climate change in debates about humanity's recent reshaping of the Earth. 

To listen to this episode, click here to subscribe to our podcast on iTunes. If you don't have iTunes, you can still listen by clicking here.  

Contributing editor Benoit Lecavalier recently conducted an extensive interview with Valérie Masson-Delmotte, one of the world's leading climate scientists and the lead coordinating author for Working Group One, the Physical Scientific Basis, in the next IPCC Assessment Report. To read Part I, on climate science, click here.​

Valérie Masson-Delmotte is an internationally renowned climate scientist. She was a lead author for the "paleoclimate" section of the fourth assessment report published by the Intergovernmental Panel on Climate Change (IPCC). She was the lead coordinating author for the "information from paleoclimate archives" section in the IPCC's fifth and most recent assessment report. For the IPCC's upcoming sixth assessment report, she is a lead coordinating author for the entire Working Group One, the Physical Scientific Basis, which oversees all other scientific chapters.

At the recent Second Open Science Conference of the International Partnerships in Ice Core Sciences, in Tasmania, our contributing editor, Benoit Lecavalier, conducted a lengthy interview with Dr. ​Masson-Delmotte. Later this month, we will publish Part II, on  public outreach on the future of the IPCC. 

Benoit Lecavalier (BL): The historical climate record covers a period of direct measurements that inform us about past states of the climate system. How was our knowledge of the climate extended into the past?

Valérie Masson-Delmotte (VMD): First, I would like to say that the instrumental period is in fact sometimes rather short. A few areas go back three centuries, like the meteorological records in England, while on the global scale the records extend back approximately 150 years at best. In some tropical regions, the precipitation records only go back 50 years. While measurements of Antarctic sea ice only begin with satellite measurements starting in ~1979. The instrumental records are very short, and so it is important to complement them with the use of either early instrumental measurements from the historical archives -  for example historical information such as harvest dates, and dates for freezing over lakes and rivers found in Europe, Japan, or China.

Finally, we have to use indirect information from natural archives, where in fact you have continuous recording of environmental parameters related to the mean climate state and variability. Starting basically at the beginning of the 20th century, people have developed methods to make use of all sorts of archives. First from continents, because they were easier to reach, came tree rings and lake sediments, then deep sea sediments, corals, and ice cores.

BL: Can you elaborate on how tree rings bridge the gap between the instrumental and historical period with natural archives, and specifically how they represent a proxy for climate?

VMD: In trees you can measure tree ring widths or density. What I do myself is the measuring of the relative abundance of heavy to light molecules, the atoms in some molecules. I also use the cellulose in the tree rings. In fact, the information on climate that you get depends on the tree's location. It is mostly related to what would be the strongest stress factor for tree growth. In cold areas at the tree line limit, it is temperature, mostly summer temperature, while in some places it can be the availability of moisture.

The tree ring signal therefore depends on the location, and so when people are focusing on temperature then they will look for high elevation and latitude tree ring records where temperature is the key control. These tree ring records are then only selected to build a chronology. We stack the tree ring records and obtain tree samples from different ages with overlap periods with younger trees and older trees to correct for age effects related to the aging of the trees.

Then the tree ring record must be calibrated, which is hard work. We must relate the parameters measured in the tree ring to a climate parameter and it implies a lot of statistical analysis to yield a robust methodology. Then a number of trees are agglomerated for a given region to produce a regional signal, to remove dependence on a single tree in the event that say, an insect attack compromised a tree. Ultimately it is about playing with a large number of records and then agglomerating them at the regional or even hemispheric scale. Depending on the place, tree ring records provide climatic information that can go back in time at the scale of one to two thousand years.

BL: If we want to extend the record even farther back in time, we might look at ice cores. What types of measurements are conducted on ice cores and how do those proxies relate to environmental conditions?

VMD: An ice core is basically a record of atmospheric deposition, so you have information on what remains of past snowfall after it has been eroded by winds. Furthermore, you have information on temperature through a number of direct and indirect parameters. The direct information arises when you drill an ice core  - you are left with a hole in the ice and you can measure a temperature profile down this borehole. Any change in surface temperature will be imprinted but filtered by diffusion processes in this temperature profile. Therefore, borehole temperatures are probably the most direct information. When you have summer temperatures above zero degrees you have melt and refreezing and so melt layers form, a crucial piece of information on past temperature from ice core.

Myself, I work on water stable isotopes, again measuring heavy to light water molecules directly in the water from the ice cores. And these are reflecting past changes in moisture transport from ocean and continental evaporation areas towards the central part of the ice sheets. Since the 1960s, we have greatly expanded our physical understanding of how hydrogen and oxygen isotope fractionation relates to past surface temperatures from theoretical models. We can also simulate it in atmospheric models.

BL: We have temperature reconstructions from borehole temperatures, summer melt layers, and water isotopes from ice core studies, we also have additional information from the air trapped in the ice cores. What can be said of the ancient gases trapped in air bubbles, such as CO2?

VMD: The instrumental records on atmospheric CO2 go back to the 1960s. We don’t have high quality CO2 records from Greenland ice cores, but we do have them for Antarctica. The issue is that Greenland is closer to the continents. It receives a lot of organic matter and dust from the nearby continents. There are chemical reactions taking place in the Greenland ice that make the preservation of the atmospheric composition of CO2 problematic. Instead, we rely on the analysis of the air trapped in the firn of Antarctic and in the ice cores. However, Greenland ice core remain very useful for methane and other gases, but not for CO2 unfortunately.

BL: Ice cores yield a great deal of information on past climates. What are some novel inferences that have come out of ice cores in the past several years?

VMD: What I like about ice cores is that we have local information, the amount of accumulation/precipitation, local temperature, then you have original information from the chemical analysis of the ice core, transport of sea salt, transport of dust from the continent, biomass burning from the continents, what we call aerosols, and then we can have more remote information. By looking at water isotopes, we have information on the evaporation conditions of water, not local but at the moisture source. We also have information on climate forcing through the deposition of volcanic aerosols, and through the impact of solar activity on cosmogenic aerosols. This allows us to reconstruct the external drivers of climate change.

Finally, we have global information through the analysis of the atmosphere composition. This helps us place our current changes in a broader context, and it facilitates our understanding of how the global biogeochemical cycles work, from the past methane and CO2 cycle. The new information that arose from the long 800,000 year-old Antarctic ice core, which shed light on glacial-interglacial cycles, demonstrated relationships between atmospheric composition and climate, as well as between ice volume, sea level, and climate. We also have a lot of information on abrupt events of the last glacial periods which are characteristic of spontaneous climate variability, not related to the position of the Earth around the sun, which is the first-order driver of glacial-interglacial changes. These abrupt climate events arise from the internal reorganization of the climate system. We describe these events in more and more detail using data and models but we don’t know exactly the cause.

More recently, a lot of information has arisen that compares the current interglacial with earlier and warmer ones. This helps us understand what happens when the climate is warmer than it is now. This research is not really about analogues but about case studies where you know what is the perturbation to the climate system. Based on this, you can test climate feedbacks under similar ranges of actions or "forcings" [climate influences]. Like what happened when climate in the atmosphere was two to four degrees celsius warmer than today, we have information of the past on that.

We can use this data to test climate models, which is I think very important. Climate models developed for today based on process analyses and physics can be further validated by testing them on case studies for extreme cold and extreme warm conditions, to make sure that the models have the right feedbacks. At the moment, it appears we can start testing the models not only for the mean states but also for transient changes, like glacial-interglacial transitions.

Finally, working on the last 2000 years is very important, it is a challenge for paleoclimatologists because we are looking for a small signal in a lot of noisy data. What is emerging is a detailed picture of regional changes around Antarctica and Greenland, changes in atmospheric and ocean circulation, the response to volcanic forcing, and modes of variability. All of these things will also be at play in the future in addition to being superimposed on the human influence to the system.

​This interview has been lightly edited for readability. Stay tuned for Part II, later this month. ​

For the third episode of the Climate History Podcast, Dr. Dagomar Degroot interviews two leading archaeologists of the medieval and early modern Arctic: Dr. Thomas McGovern of the City University of New York, and Dr. George Hambrecht of the University of Maryland College Park. Since 1972, Professor McGovern has travelled the world for archaeological fieldwork. He has spent much of his time in the far north, especially in Greenland, Iceland, the Faeroes, and Shetland. He is one of the founders of the North Atlantic Biocultural Organization (NABO), and he is associate director of the Human Ecodynamics Research Center at the CUNY Graduate Center. He has an extraordinary record of groundbreaking publications on the history of Arctic peoples, and he has won many awards from the National Science Foundation, the Ford Foundation, the National Geographic Society, and other leading organizations. 

Professor Hambrecht is part of a new generation of interdisciplinary archaeologists of far north. He explores interactions between the political, environmental, and biological dimensions of the transformative early modern period. He is especially interested in historical and zooarchaeology in Iceland, the Subarctic, and the Arctic North Atlantic. He has done extensive fieldwork to reconstruct how Icelandic farmers coped with the onset of the Little Ice Age. He leads teams of interdisciplinary researchers in projects that have recently won support from the National Science Foundation. ​

In this episode, professors Degroot, McGovern, and Hambrecht discuss the perils of doing fieldwork in the Far North; the struggles of the Norse in Greenland and Iceland at the onset of the Little Ice Age; the threat of climate change to the archaeological record of northern peoples; and the possibilities (and challenges) of interdisciplinary approaches to Arctic research. 

To listen to this episode, click here to subscribe to our podcast on iTunes. If you don't have iTunes, you can still listen by clicking here.

Photo credit: Benoit S. Lecavalier (2014).

In the second episode of the Climate History Podcast, Dr. Dagomar Degroot interviews the co-founder and co-administrator of the Climate History Network: Dr. Sam White of Ohio State University. Professor White is one of the most innovative and respected environmental historians of the "Little Ice Age," a period of climatic cooling that, according to some definitions, affected most of the world from the fourteenth through the nineteenth centuries. 

Professor White's first book, The Climate of Rebellion in the Early Modern Ottoman Empire, was published by Cambridge University Press in 2011. In it, Professor White uses interdisciplinary methods and sources to explore how climatic cooling and drying shaped the history of the Ottoman Empire. The book won the Middle East Studies Association Albert Hourani award, the Turkish Studies Association Fuat Köprülü award, and the British-Kuwaiti Friendship Society prize for the best book in Middle East and Turkish studies. Professor White has also written award-winning articles, including one entitled "From Globalized Pigs to Capitalist Pigs: A Study in Animals Cultures and Evolutionary History," which was published in the journal Environmental History in 2011. It won the American Society for Environmental History Leopold-Hildy Prize and the Agricultural History Association Wayne D. Rasmussen Award. More recently, Professor White has received major fellowships to write a book that traces how climate change influenced the early settlement of North America. It is currently under contract with Harvard University Press. 

For our first episode, our founder, Dr. Dagomar Degroot of Georgetown University, interviewed one of the world's best-known and most respected historians: Dr. Geoffrey Parker, of Ohio State University. Professor Parker has authored, edited, or co-edited 37 books and more than 100 articles and book chapters. Recently, he released a groundbreaking new book called Global Crisis, which explores how a cooling climate disrupted societies across the seventeenth-century world. Global Crisis has won awards that include the prestigious Heineken Prize, given by the Royal Netherlands Academy of Arts and Sciences, and the British Academy Medal, given by the British Academy for the Humanities and Social Sciences. We were thrilled to have Professor Parker as the first guest on our podcast.

To listen to our inaugural episode, click here to subscribe to our podcast on iTunes. If you don't have iTunes, you can still listen by clicking here.   

Photo credit: Iceberg off Greenland, by Benoit S. Lecavalier (2014).

Granted, most natural history museums have exhibits dedicated to climate history and global warming. The Smithsonian's National Museum of Natural History in Washington, D. C., for example, features a spectacular exhibit that links climate change to the fate of early hominids (above). The American Museum of Natural History in New York has an alcove just beneath the Hayden Planetarium that describes global warming and explains how scholars reconstruct past climates. But no permanent museum gathers all of this information in one place, in a way that skips over disciplinary boundaries and alerts the public about the importance of action, today.


Miranda Massie and a group of like-minded experts are trying to change all that. Massie is the executive director of the Climate Museum Launch Project. Her initiative seeks to open a climate change museum in New York City, which she hopes will attract some one million visitors per year. We are delighted that she took the time to answer our questions.  

DD: Will your museum explore how humans have evolved with climate change, from prehistory to the present? Or will this be a museum of global warming? 

MM: The main focus will be on solutions to anthropogenic climate change, with concentric circles of context. One of those circles will be devoted to the history of the planet’s climate and its relationship to life, including human life.

DD: To what extent will disaster and decline – keywords in the quest for action on global warming - play a role in your museum? 

MM: While we must be honest about growing risks, this is very much a museum about resilience, adaptation, and mitigation—about our shared ability to escape the danger our shared abilities and proclivities have created.  

DD: How close is the Museum of Climate Change to becoming a reality? What still needs to be done? How can people help? 

MM: Much closer than it was when we started fifteen months ago, with longer left to go. We’ve gotten as far as we have because so many people have offered support and expertise, and we very much welcome more. It is a huge help for people to spread the word through social media and in person. And we gratefully welcome your readers’ further thoughts on how we can, with their engagement and support, get closer to the red ribbon moment. I can be reached at mmassie@cmlp.org.