Climate Since Ad 1500

First Published in 2004. Climate Since A.D. 1500 presents a unique perspective on the 'Little Ice Age' and the climate of the twentieth century. Leading scientists explore historical documents, dendroclimatic data and ice core records from all over the world, presenting an invaluable compilation for all those concerned with past climate and the risks of man-made climatic change in the future. This revised edition includes a new chapter summarizing the wealth of literature on climatic change over the past few years and a new and expanded index.

Supported by in-depth scientific evidence, Singer and Avery present the compelling concept that global temperatures have been rising mostly or entirely because of a natural cycle. Unstoppable Global Warming explains why we're warming, why it's not very dangerous, and why we can't stop it anyway.

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.

​This book is an update of the first BACC assessment, published in 2008. It offers new and updated scientific findings in regional climate research for the Baltic Sea basin. These include climate changes since the last glaciation (approx. 12,000 years ago), changes in the recent past (the last 200 years), climate projections up until 2100 using state-of-the-art regional climate models and an assessment of climate-change impacts on terrestrial, freshwater and marine ecosystems. There are dedicated new chapters on sea-level rise, coastal erosion and impacts on urban areas. A new set of chapters deals with possible causes of regional climate change along with the global effects of increased greenhouse gas concentrations, namely atmospheric aerosols and land-cover change. The evidence collected and presented in this book shows that the regional climate has already started to change and this is expected to continue. Projections of potential future climates show that the region will probably become considerably warmer and wetter in some parts, but dryer in others. Terrestrial and aquatic ecosystems have already shown adjustments to increased temperatures and are expected to undergo further changes in the near future. The BACC II Author Team consists of 141 scientists from 12 countries, covering various disciplines related to climate research and related impacts. BACC II is a project of the Baltic Earth research network and contributes to the World Climate Research Programme.

Since the greenhouse effect emerged as a predictable threat, necessitating the evalu ation of its future impact on the environment in the various parts of the globe, interest in the climate changes during the Holocene has gained momentum. The background can be summarized by the sentence: The past is a key to the future. As a matter of fact, this sentence is in the opposite direction, on the dimension of time, to the principle adopted by the founders of the science of geology. They proposed that geological processes in the present should be used as a key for understanding the past. Another reason for the interest in the history of the climate of the Holocene can be described as the renaissance of a modified deterministic approach to the inter relation between physical and human geography. This relates in the first place to the fact that various investigations, especially as carried out by Hubert Lamb, showed that the sequence of climate changes previously suggested by Blytt and Sernander for Europe and adopted by most Holocene climatologists was far too general, and that there were more climate changes during recent history than previously taken account of. In the second place it was found out that these changes had had an impact on the history of human communities. Thus, one can conclude that once the taboo on geographical determinism (i. e.

History and Climate Change is a balanced and comprehensive overview of the links between climate and man's advance from early to modern times. It draws upon demographic, economic, urban, religious and military perspectives. It is a synthesis of the many historical and scientific theories, which have arisen regarding man's progress through the ages. Central to the book is the question of whether climate variation is a fundamental trigger mechanism from which other historical sequences develop, or one amongst a number of other factors, decisive only when a regime/society is poised for change. Evidence for prolonged climate change is not that extensive. But it is clear that climatic variation has regularly played a part in historical development. Paricular attention is here paid to Europe since AD 211. Cold and warmth, wetness and aridity can create contrary reactions within societies, which can be interpreted in vary different ways by scholars from differenct disciplines. Does climate change exacerbate famine and epidemics? Did climate fluctuation play a part in pivotal historical events such as the mass exodus of Hsuing-nu from China, the pressure of the Huns on the Romans and the genesis of the Crusades? Did the bitter Finnish winter of 1939-40 ensure the ultimate defeat of Hitler? These episodes, and many others are discussed throughout the book in the authors distinctive style, with maps and photographs to illustrate the examples given.

This Handbook re-examines the concept of early modern history in a European and global context. The term 'early modern' has been familiar, especially in Anglophone scholarship, for four decades and is securely established in teaching, research, and scholarly publishing. More recently, however, the unity implied in the notion has fragmented, while the usefulness and even the validity of the term, and the historical periodisation which it incorporates, have been questioned. The Oxford Handbook of Early Modern European History, 1350-1750 provides an account of the development of the subject during the past half-century, but primarily offers an integrated and comprehensive survey of present knowledge, together with some suggestions as to how the field is developing. It aims both to interrogate the notion of 'early modernity' itself and to survey early modern Europe as an established field of study. The overriding aim will be to establish that 'early modern' is not simply a chronological label but possesses a substantive integrity. Volume I examines 'Peoples and Place', assessing structural factors such as climate, printing and the revolution in information, social and economic developments, and religion, including chapters on Orthodoxy, Judaism and Islam.