Explores the role of the ocean in fast climate changes in the past and conceivable future. The first half of the 16 papers present data interpretation, hypotheses based on data analyses, and ideas that shed new light on past climates and their evolution. The remaining papers describe climate system models that focus on the global ocean, starting with simpler, ocean-only models that develop into full, three-dimensional models of entire climate systems. Topics include the key climate transitions during the Quaternary period, stochastic resonance in the North Atlantic, and the relationship between glacial- to-interglacial changes of ocean circulation and eolian sediment transport. No index. c. Book News Inc.
This book is designed for first- and second-year universitystudents (and their instructors) in earth science, environmentalscience, and physical geography degree programmes worldwide. Thesummaries at the end of each section constitute essential readingfor policy makers and planners. It provides a simple but masterlyaccount, with a minimum of equations, of how the Earth’sclimate system works, of the physical processes that have givenrise to the long sequence of glacial and interglacial periods ofthe Quaternary, and that will continue to cause the climate toevolve. Its straightforward and elegant description, with anabundance of well chosen illustrations, focuses on different timescales, and includes the most recent research in climate science bythe United Nations Intergovernmental Panel on Climate Change(IPCC). It shows how it is human behaviour that will determinewhether or not the present century is a turning point to a newclimate, unprecedented on Earth in the last several millionyears.
Tackling the issue of global warming head-on for a teen audience, Bridget Heos examines the science behind it, the history of climate change on our planet, and the ways in which humans have affected the current crisis we face. It’s Getting Hot in Here illustrates how interconnected we are not just with everyone else on the planet, but with the people who came before us and the ones who will inherit the planet after us. This eye-opening approach to one of today’s most pressing issues focuses on the past human influences, the current state of affairs, the grim picture for the future—and how young readers can help to make a positive change.
Reconstructing climatic changes in deserts and their margins at a variety of scales in space and time, this book draws upon evidence from land and sea, including desert dunes, wind-blown dust, river and lake sediments, glacial moraines, plant and animal fossils, isotope geochemistry, speleothems, soils, and prehistoric archaeology. The book summarises the Cenozoic evolution of the major deserts of the Americas, Eurasia, Africa and Australia and the causes of historic floods and droughts. The book then considers the causes and consequences of desertification and proposes four key conditions for achieving ecologically sustainable use of natural resources in arid and semi-arid areas. Climate Change in Deserts is an invaluable reference for researchers and advanced students interested in the climate and geomorphology of deserts: geographers, geologists, ecologists, archaeologists, soil scientists, hydrologists, climatologists and natural resource managers.
To understand climate change today, we first need to know how Earth’s climate changed over the past 450 million years. Finding answers depends upon contributions from a wide range of sciences, not just the rock record uncovered by geologists. In Earth’s Climate Evolution, Colin Summerhayes analyzes reports and records of past climate change dating back to the late 18th century to uncover key patterns in the climate system. The book will transform debate and set the agenda for the next generation of thought about future climate change. The book takes a unique approach to the subject providing a description of the greenhouse and icehouse worlds of the past 450 million years since land plants emerged, ignoring major earlier glaciations like that of Snowball Earth, which occurred around 600 million years ago in a world free of land plants. It describes the evolution of thinking in palaeoclimatology and introduces the main players in the field and how their ideas were received and, in many cases, subsequently modified. It records the arguments and discussions about the merits of different ideas along the way. It also includes several notes made from the author’s own personal involvement in palaeoclimatological and palaeoceanographic studies, and from his experience of working alongside several of the major players in these fields in recent years. This book will be an invaluable reference for both undergraduate and postgraduate students taking courses in related fields and will also be of interest to historians of science and/or geology, climatology and oceanography. It should also be of interest to the wider scientific and engineering community, high school science students, policy makers, and environmental NGOs. Reviews: "Outstanding in its presentation of the facts and a good read in the way that it intersperses the climate story with the author's own experiences. [This book] puts the climate story into a compelling geological history." -Dr. James Baker "The book is written in very clear and concise prose, [and takes] original, enlightening, and engaging approach to talking about 'ideas' from the perspective of the scientists who promoted them." -Professor Christopher R. Scotese "A thrilling ride through continental drift and its consequences." - Professor Gerald R. North "Written in a style and language which can be easily understood by laymen as well as scientists." - Professor Dr Jörn Thiede "What makes this book particularly distinctive is how well it builds in the narrative of change in ideas over time." - Holocene book reviews, May 2016 "This is a fascinating book and the author’s biographical approach gives it great human appeal." - E Adlard
Glaciers in the Andes are particularly important natural archives of present and past climatic and environmental changes, in significant part because of the N-S trend of this topographic barrier and its influence on the atmospheric circulation of the southern hemisphere. Strong gradients in the seasonality and amount of precipitation exist between the equator and 30° S. Large differences in amount east and west of the Andean divide also occur, as well as a change from tropical summer precipitation (additionally modified by the seasonal shift of the circulation belts) to winter precipitation in the west wind belt (e. g. , Yuille, 1999; Garraud and Aceituno, 2001). The so-called 'dry axis' lies between the tropical and extra tropical precipitation regimes (Figure 1). The high mountain desert within this axis responds most sensitively to the smallest changes in effective moisture. An important hydro-meteorological feature on a seasonal to inter-annual time-scale is the occurrence of EN SO events, which strongly control the mass balance of glaciers in this area (e. g. , Wagnon et ai. , 2001; Francou et ai. , in press). The precipitation pattern is an important factor for the interpretation of climatic and environmental records extracted from ice cores, because much of this information is related to conditions at the actual time of precipitation, and this is especially so for stable isotope records. Several ice cores have recently been drilled to bedrock in this area. From Huascanin (Thompson et ai. , 1995), Sajama (Thompson et ai.
Reducing the Vulnerability of Agriculture and Forestry
Author: James Salinger
Publisher: Springer Science & Business Media
This book reviews the latest assessments of climate variability and climate change, and their impacts on agriculture and forestry, and recommends appropriate adaptation strategies for reducing the vulnerability of agriculture and forestry to climate variability and climate change. Among other solutions, the text offers management strategies to mitigate greenhouse gas emissions from different agroecosystems, and proposes the use of seasonal climate forecasts to reduce climate risk.