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The Equatorial Glaciers of New Guinea includes the Results of the 1971-1973 Australian Universities' Expeditions to Irian Jaya: Survey, Glaciology, Meteorology, Biology and Paleoenvironments.
An enthralling exploration of the biologically richest island on Earth, featuring more than 200 spectacular color images by award-winning National Geographic photographer Tim Laman In this beautiful book, Bruce Beehler, a renowned author and expert on New Guinea, and award-winning National Geographic photographer Tim Laman take the reader on an unforgettable journey through the natural and cultural wonders of the world's grandest island. Skillfully combining a wealth of information, a descriptive and story-filled narrative, and more than 200 stunning color photographs, the book unlocks New Guinea's remarkable secrets like never before. Lying between the Equator and Australia's north coast, and surrounded by the richest coral reefs on Earth, New Guinea is the world's largest, highest, and most environmentally complex tropical island—home to rainforests with showy rhododendrons, strange and colorful orchids, tree-kangaroos, spiny anteaters, ingenious bowerbirds, and spectacular birds of paradise. New Guinea is also home to more than a thousand traditional human societies, each with its own language and lifestyle, and many of these tribes still live in isolated villages and serve as stewards of the rainforests they inhabit. Accessible and authoritative, New Guinea provides a comprehensive introduction to the island's environment, animals, plants, and traditional rainforest cultures. Individual chapters cover the island's history of exploration; geology; climate and weather; biogeography; plantlife; insects, spiders, and other invertebrates; freshwater fishes; snakes, lizards, and frogs; birdlife; mammals; paleontology; paleoanthropology; cultural and linguistic diversity; surrounding islands and reefs; the pristine forest of the Foja Mountains; village life; and future sustainability. Complete with informative illustrations and a large, detailed map, New Guinea offers an enchanting account of the island's unequalled natural and cultural treasures.
Glaciers in the tropics and their environmental consequences.
Like a star chart this volume orientates the reader to the key issues and debates in Pacific and Australasian biogeography, palaeoecology and human ecology. A feature of this collection is the diversity of approaches ranging from interpretation of the biogeographic significance of plant and animal distributional patterns, pollen analysis from peats and lake sediments to discern Quaternary climate change, explanation of the patterns of faunal extinction events, the interplay of fire on landscape evolution, and models of the environmental consequences of human settlement patterns. The diversity of approaches, geographic scope and academic rigor are a fitting tribute to the enormous contributions of Geoff Hope. As made apparent in this volume, Hope pioneered multidisciplinary understanding of the history and impacts of human cultures in the Australia- Pacific region, arguably the globe's premier model systems for understanding the consequences of humans colonization on ecological systems. The distinguished scholars who have contributed to this volume also demonstrate Hope's enduring contribution as an inspirational research leader, collaborator and mentor. Terra Australis leave no doubt that history matters, not only for land management, but more importantly, in alerting settler and indigenous societies alike to their past ecological impacts and future environmental trajectories.
The evidence for the Little Ice Age, the most important fluctuation in global climate in historical times, is most dramatically represented by the advance of mountain glaciers in the sixteenth and seventeenth centuries and their retreat since about 1850. The effects on the landscape and the daily life of people have been particularly apparent in Norway and the Alps. This major book places an extensive body of material relating to Europe, in the form of documentary evidence of the history of the glaciers, their portrayal in paintings and maps, and measurements made by scientists and others, within a global perspective. It shows that the glacial history of mountain regions all over the world displays a similar pattern of climatic events. Furthermore, fluctuations on a comparable scale have occurred at intervals of a millennium or two throughout the last ten thousand years since the ice caps of North America and northwest Europe melted away. This is the first scholarly work devoted to the Little Ice Age, by an author whose research experience of the subject has been extensive. This book includes large numbers of maps, diagrams and photographs, many not published elsewhere, and very full bibliographies. It is a definitive work on the subject, and an excellent focus for the work of economic and social historians as well as glaciologists, climatologists, geographers, and specialists in mountain environment.
First published in 1977, the second volume of Climate: Present, Past and Future covers parts 3 and 4 of Professor Hubert Lamb’s seminal and pioneering study of climatology. Part 3 provides a survey of evidence of types of climates over the last million years, and of methods of dating that evidence. Through the earlier stages of the Earth’s development the book traces what is known of the various geographies presented by the drifting continents and indicates what can be learnt about climatic regimes and the causes of climatic change. From the last ice age to the present our knowledge of the succession of climates is summarized, indicating prevailing temperatures, rainfalls, wind and ocean current patterns where possible. Part 4 considers events during the fifteen years prior to the book’s initial publication, leading on to the problems of estimating the most probable future course of climatic development, and the influence of Man’s activities on climate. Alongside the reissue of volume 1, this Routledge Revival will be essential reading for anyone interested in both the causes and workings of climate and in the history of climatology itself.
Since The Little Ice Age was published in 1988, interest in climatic history has grown rapidly and research in the area has flourished. A vast amount of new data has become available from sources such as ice cores, speleothems and tree rings. The picture that we have of past climates and glacier oscillations has extended further into the past and has become more detailed. However, the knowledge of climate change on the decennial and centennial timescale, to which glacier history can contribute, is scarce and is in demand when attempting to predict future change, especially with regard to global warming. New chapters and material have been included throughout the book, which tend to confirm and elaborate on the conclusions of the first edition. The glacial evidence has been presented in the context of the oceanographic and icecap studies that have provided such exciting results. Little Ice Ages is structured in three parts: Part 1 details the evidence for glacier variations in the last thousand years in different parts of the world and the associated climatic fluctuations. Part 2 brings together the evidence for the timing of glacier variations in the course of the Holocene. Part 3 views the Holocene record in a longer time context, especially as it appears in ice cores, and goes on to consider the likely causes of climatic variability on a Little Ice Age timescale and some of its physical, biological and human consequences. It becomes apparent in Little Ice Ages that the glacier record provides a valuable indication of the nature of climatic fluctuations on the land areas of the globe. The record points to periods of cooling which were more numerous and less continuous than was believed to be the case twenty years ago. There appears to be no single explanation for the variability. Volcanism, solar variability and ocean currents have all played their parts and prediction continues to present many problems. Some authorities have thrown doubt on the existence of the Little Ice Age, but Little Ice Age makes the case for a climatic sequence that can usefully be called the Little Ice Age and which had predecessors occurring at intervals of several centuries throughout much of the last 10,000 years.