Climate Change: Evidence and Causes is a jointly produced publication of The US National Academy of Sciences and The Royal Society. Written by a UK-US team of leading climate scientists and reviewed by climate scientists and others, the publication is intended as a brief, readable reference document for decision makers, policy makers, educators, and other individuals seeking authoritative information on the some of the questions that continue to be asked. Climate Change makes clear what is well-established and where understanding is still developing. It echoes and builds upon the long history of climate-related work from both national academies, as well as on the newest climate-change assessment from the United Nations' Intergovernmental Panel on Climate Change. It touches on current areas of active debate and ongoing research, such as the link between ocean heat content and the rate of warming.

In response to a request from Congress, Surface Temperature Reconstructions for the Last 2,000 Years assesses the state of scientific efforts to reconstruct surface temperature records for Earth during approximately the last 2,000 years and the implications of these efforts for our understanding of global climate change. Because widespread, reliable temperature records are available only for the last 150 years, scientists estimate temperatures in the more distant past by analyzing "proxy evidence," which includes tree rings, corals, ocean and lake sediments, cave deposits, ice cores, boreholes, and glaciers. Starting in the late 1990s, scientists began using sophisticated methods to combine proxy evidence from many different locations in an effort to estimate surface temperature changes during the last few hundred to few thousand years. This book is an important resource in helping to understand the intricacies of global climate change.

"The hot dry seasons of the past few years have caused rapid disintegration of glaciers in Glacier National Park, Montana...Sperry Glacier...has lost one-quarter or perhaps one-third of its ice in the past 18 years... If this rapid rate should continue...the glacier would almost disappear in another 25 years..." "Born about 4,000 years ago, the glaciers that are the chief attraction in Glacier National Park are shrinking so rapidly that a person who visited them ten or fifteen years ago would hardly recognize them today as the same ice masses." Do these reports sound familiar? Typical of frequent warnings of the dire consequences to be expected from global warming, such reports often claim modern civilization's use of fossil fuels as being the dominant cause of recent climate warming. You might be surprised to learn the reports above were made nearly thirty years apart! The first in 1923 prior to the record heat of the Dust Bowl years during the 1930s. The second in 1952 during the second decade of a four-decade cooling trend that had some scientists concerned that a new ice age might be on the horizon! Did the remnants of Sperry Glacier disappear during global warming of the late 20th century? According to the US Geological Survey (USGS), today Sperry Glacier "ranks as a moderately sized glacier" in Glacier National Park. What caused the warmer global climate prior to "4,000 years ago" before Glacier National Park's glaciers first appeared? Are you aware that during 2019 the National Park Service quietly began removing its "Gone by 2020" signs from Glacier National Park as its most famous glaciers continued their renewed growth that began in 2010? Was late 20th-century global warming caused by fossil fuel emissions? Was it really more pronounced than early 20th-century warming? Or was late 20th-century warming perfectly natural, in part a response to the concurrent peak strength of one of the strongest solar grand maxima in contemporary history? These and other questions are addressed by "Looking Out the Window." Be a juror in the trial of carbon dioxide in the court of public opinion and let the evidence inform your verdict.

The warming of the Earth has been the subject of intense debate and concern for many scientists, policy-makers, and citizens for at least the past decade. Climate Change Science: An Analysis of Some Key Questions, a new report by a committee of the National Research Council, characterizes the global warming trend over the last 100 years, and examines what may be in store for the 21st century and the extent to which warming may be attributable to human activity.

Professor Kondratyev and his team consider the concept of global warming due to the greenhouse effect and put forward a new approach to the problem of assessing the impact of anthropogenic processes. Considering data on both sources and sinks for atmospheric carbon and various conceptual schemes of the global carbon dioxide cycle, they suggest a new approach to studies of the problem of the greenhouse effect. They assess the role of different types of soil and vegetation in the assimilation of carbon dioxide from the atmosphere, and discuss models of the atmosphere ocean gas exchange and its role in the carbon dioxide cycle, paying special attention to the role of the Arctic Basin. The authors also consider models of other global atmospheric cycles for a range of atmospheric constituents, and conclude by drawing together a range of scenarios on modelling the global carbon cycle.

Emissions of carbon dioxide from the burning of fossil fuels have ushered in a new epoch where human activities will largely determine the evolution of Earth's climate. Because carbon dioxide in the atmosphere is long lived, it can effectively lock the Earth and future generations into a range of impacts, some of which could become very severe. Emissions reductions decisions made today matter in determining impacts experienced not just over the next few decades, but in the coming centuries and millennia. According to Climate Stabilization Targets: Emissions, Concentrations, and Impacts Over Decades to Millennia, important policy decisions can be informed by recent advances in climate science that quantify the relationships between increases in carbon dioxide and global warming, related climate changes, and resulting impacts, such as changes in streamflow, wildfires, crop productivity, extreme hot summers, and sea level rise. One way to inform these choices is to consider the projected climate changes and impacts that would occur if greenhouse gases in the atmosphere were stabilized at a particular concentration level. The book quantifies the outcomes of different stabilization targets for greenhouse gas concentrations using analyses and information drawn from the scientific literature. Although it does not recommend or justify any particular stabilization target, it does provide important scientific insights about the relationships among emissions, greenhouse gas concentrations, temperatures, and impacts. Climate Stabilization Targets emphasizes the importance of 21st century choices regarding long-term climate stabilization. It is a useful resource for scientists, educators and policy makers, among others.