Historically, climate fluctuations, such as the Little Ice Age, show that interglacial climate chage in not entirely stable, but responds to even subtle changes in radiative forcing. Through research, it has been made clear that even an abrupt change of climate within years is not just a theoretical possibility but has in fact happened in the prehistoric past. It is therefore clear that in principal it could happen again. Human civilaization has exploded under the mild and relatively stable climatic conditions that have prevailed over the last 11,000 years.
This book focuses on revisiting the past and to study climate and environment in a suite of experiments where boundary conditions are similar but not identical to today so we can learn about the climate-environment system, its sensitivity, thresholds and feedback. The palaeoclimate community holds an important key to scientific information on climate change that provides a basis for appropriate adaptation and mitigation strategies. The authors of this book have taken up this challenge and summarize their results in this special volume. It presents state-of-the-art science on new reconstructions from all spheres of the Earth System and on their synthesis, on methodological advances, and on the current ability of numerical models to simulate low and high frequency changes of climate, environment, and chemical cycling related to interglacials.
* Summarizes important information on climate change, providing a basis for appropriate adaptation and mitigation strategies for human civilization
* Reports on new reconstuctions on methodological advances, numerical models simulating low and high frequence changes, and chemical cycling related to interglacials
* Incorporates palaeovegetaion and numerical modeling of climate and environmental and geochemical parameters to address regional feedback to global change with successful data-models

This rock-based book is an attempt to link deep-water process sedimentology with sandstone petroleum reservoirs. In presenting a consistent process interpretation, the author has relied on his description and interpretation of core and outcrop (1:20 to 1:50 scale) from 35 case studies (which include 32 petroleum reservoirs), totaling more than 30,000 feet (9,145 m), carried out during the past 30 years (1974-2004). This book should serve as an important source of information for students on history, methodology, first principles, advanced concepts, controversies, and practical applications on deep-water sedimentology and petroleum geology
* Discusses the link between deep-water process sedimentology and petroleum geology
* Addresses criteria for recognizing deposits of gravity-driven, thermohaline-driven, wind-driven, and tide-driven processes in deep-water environments
* Provides head-on approach to resolve controversial process-related problems

Dams profoundly impact the geomorphology of rivers by altering the natural patterns of water, sediment and energy flow in rivers. These changes have a largely negative impact on aquatic and riparian ecosystems upstream and downstream of the dam. Natural dams also impact river geomorphology, although with positive and negative repercussions for aquatic and riparian organisms.
In 2002, the 33rd Binghamton Geomorphology Symposium convened under the theme "Dams and Morphology," and featured invited papers and contributed posters on topics of natural dams, artificial dams, and dam removal. Fourteen of these papers have been included in this volume.

Cyclic Development of Sedimentary Basins presents the controversial subject of the cyclic phenomena in the earth's evolutionary history and its reflection in the development of sedimentary basins and its lithic infillings. Galactic rotation of celestial bodies causes cyclicity that is also reflected on a smaller scale in the proper Earth. This book presents the consequences of the earth's cyclic phenomena in the long-term cycles which affect the origin and further evolution of sedimentary basins.
* Basin development
* Cyclicity
* Examples from the world

Surface analysis deals with characterizing and understanding the behavior of molecules which react on the surface between two substances. The latest self--contained volume in this long established and respected series of review articles on applications and instrumental developments in spectroscopy presents a high quality treatment of the frontiers of research occurring in modern spectroscopic methods. The internationally renowned authors have taken care to make their work accessible to experts and non--experts alike.

This volume, also available as part of the collection "Geomorphology: Critical Concepts in Geography" [set ISBN 0-415-27608-X], constitutes an instant archive of esential benchmark papers and makes available in one place key published material on its area.

This volume, also available as part of the collection "Geomorphology: Critical Concepts in Geography" [set ISBN 0-415-27608-X], constitutes an instant archive of esential benchmark papers and makes available in one place key published material on its area.

This volume, also available as part of the collection "Geomorphology: Critical Concepts in Geography" [set ISBN 0-415-27608-X], constitutes an instant archive of esential benchmark papers and makes available in one place key published material on its area.

The book deals with push moraines on Spitsbergen. The main body is a translation of the original German report by Karl Gripp on a 1927 expedition. The quality of Gripp's work is evaluated to see whether it stands the test of time. It is found that it is very modern, every year people still go into the field with the same research questions. It is also found that most likely Gripp's report contains the first description of features that we now take for granted, for instance the description of looped moraines to detect surges. Push moraines are still being studied and to show where we stand now two papers have been added that analyse two particular examples, Holmstrombreen and Sefstrombreen. The two examples are geographically close together, but reflect two completely different settings: terrestrial Holmstrombreen and tidewater Sefstrombreen.

Since a few years we know of the De Geer Archive, a collection of glass negatives of Spitsbergen, relating to De Geer's expeditions between 1882 and 1910. The negatives have only emerged recently and a collection of prints relating to Holmstrombreen and Sefstrombreen is included here. Together with a third paper incorporated in the book, this time an evaluation of De Geer's photos and maps of the Sefstrombreen surge, this material shows the importance of incorporating historical documentation in our studies.

This book, first published in 1985, arises from the 14th Binghamton Geomorphology Symposium. The chapters here illustrate the use of models in various areas of research in geomorphology.

The study of landforms is becoming increasingly scientific. This book, first published in 1971, attempts to do justice to the work done in the last few decades, but strives to avoid a too uncritical acceptance of contemporary trends. The author first examines the fundamental characteristics and basic postulates of geomorphology. He then seeks to define the systematic stages through which the study of the landforms of a given area might proceed. Examples are drawn from a wide geographical range with emphasis on presenting examples of actual observations and measurements. The final section presents concise descriptions of simple and inexpensive methods of acquiring field data in landform study.

This book, first published in 1985, conveys the flavours of geomorphology and the bases of its ideas. It portrays the positive features of pluralism in geomorphology, and focuses on processes operative and their associated landforms; the distinctive geological settings of karst, volcanicity and tectonic activity; and technological advances.

This book, first published in 1977, is a concise, fully illustrated introduction to modern geomorphology. Geomorphologists pay much attention to the measurement of present day processes in attempting to develop explanations of landscape evolution, and this book reflects this approach by deliberately emphasising processes in humid environments.

This book, first published in 1986, collects the articles presented to the 16th Binghamton Geomorphology Symposium and is a ground-breaking work in the study of hillslope processes. Hillslope processes are studied in a variety of disciplines other than geomorphology, such as hydrology, pedology, agricultural engineering, civil engineering and engineering geology - the study is truly an interdisciplinary science.

This book, first published in 1982, forms the proceedings volume of the 11th Binghamton Geomorphology Symposium. Chapters cover various coastline phenomena, glacial and periglacial processes, carbonate terrains, and specific applications of geomorphic knowledge and techniques.

This book, first published in 1987, contains a collection of papers presented at the 18th Binghamton Symposium, focusing on the topic of catastrophic flooding. These papers make the case for the careful collection and interpretation of data from which the importance and effects of catastrophic flooding may be deduced. Questions tackled include: what are the causes and effects of catastrophic flooding? What parameters should be used to measure them? What effect do they have on erosional and depositional landforms? Can modelling be used to predict their flow dynamics?

This book, first published in 1983, incorporates a wealth of reference material - keys, nomograms, tables, charts - likely to be needed in the field for actual fieldwork. The widest possible coverage of material is provided in anticipation of problems that individual specialists will encounter on the periphery of their main areas of interest.

This book, first published in 1992, contains the proceedings of the 22nd Binghamton Geomorphology Symposium, and highlights the quantity and diversity of periglacial geomorphic research being undertaken in Arctic and alpine environments. The articles explore a variety of geomorphic processes and examine the potential impacts of global change on the nature and extent of permafrost and seasonal ice phenomena.

A concise textbook emphasizing sedimentary processes and flow in alluvial channels, this title provides comprehensive treatment of flow-bed transport interaction. It emphasizes water flows (basic principles and characterization), fluvial sediment, processes of erosion and sediment transport, bedforms that result from flow-bed sediment interactions in sand and gravel, flow and sedimentary processes in curved, braided and confluent channels, as well as aquatic habits.;The text provides a comprehensive synthesis of current knowledge about physical processes in alluvial channels, with an emphasis on the recent work on flow-bed sediment transport interactions. It is designed for students with an interest in fluvial studies as a part of physical geography, earth sciences, environmental sciences and ecology courses.

The book, written from the perspective of pedologists and agronomists, is a study of the Earth's crust which is subjected to climatic agents and inhabited by living creatures. These phenomena in concert, slowly transform soil through the interaction of physical, climatic and biological processes.

This volume is a collection of papers produced within the framework of the Italian National Antarctic Research Programme (PNRA) on the monitoring and control of environmental contamination. The volume represents a contribution of the PNRA to the study of planetary contamination and to the understanding of the processes of global change.;The research focuses on the measurement and analysis of trace elements and organic micropollutants in the following matrices: snow/firn, seawater, soils, sediments, suspended particulate matter, pack ice, atmosphere, and biota.;The results presented extend beyond the development of specific analytical methodologies, to explicitly tackle significant environmental issues concerning global changes. Particularly relevant are the results concerning time changes of CFCs in the troposphere and lead concentration in Antarctic snow in Victoria Land, the presence of organic micropollutants in various Antarctica matrices, and the seasonal evolution of trace elements and organics in seawater.

Effective management of a water well requires that the water well can meet a set of performance indicators. These can include criteria related to water quality, yield, economics and asset life. Water well deterioration due to fouling and corrosion impacts the ability of a well system to meet these criteria. Managing well deterioration processes involves understanding the nature of these processes and having in place water well maintenance strategies to deal with them. Managing water well deterioration fills a need within the literature for an academically based informative text that incorporates practical advice. The focus on a problem-oriented approach to diagnosing well deterioration makes the book a useful practical handbook. It integrates concepts from hydrogeology, hydrochemistry and microbiology to give a thorough understanding of water well deterioration processes. Scenarios have been developed to illustrate common causes of water well fouling. A feature of the book is the treatment of both corrossion and fouling issues in depth. Case studies selected from around the world are uses to illustrate approaches to the diagnosis and remediation of well deterioration. These scientifically orientated perspectives on water well deterioration are embedded within a management framework to provide a comprehensive approach to dealing with water well deterioration.

The proceedings contain five invited lectures and 99 papers relevant to landslide occurrence and problems from Europe, Asia, America, Africa and Australia and New Zealand. The five special invited lectures deal with a variety of important aspects of landslides.

This text brings together meteorology and the theory of glacier flow, providing a fundamental understanding of how glaciers respond to climate change. Attention is paid to the microclimate of glaciers and the physical processes regulating the exchange of energy and mass between glacier surface and atmosphere. Simple analytical and numerical models are used to:
investigate glaciers sensitivity to climate change
estimate response times
make an interpretation of historical glacier records
assess the contribution of glacier melt to sea-level rise
Modern developments in glacier research, including satellite measurements are discussed in detail, making this a valuable reference source.

This volume describes mountains from all over the world, with an emphasis on mountain landforms, but also looks at their rocks, structure and age. This leads to a deduction on the mechanism which formed them, causing the authors to reject the pre-conceived and well known hypothesis that plate tectonics and folding creates mountains. The book approaches mountains from facts about mountain landscapes rather than theory. It illustrates that almost everywhere, mountains arose by vertical uplift of a former plain, and by a mixture of cracking and warping by earth movements, and erosion by rivers and glaciers, the present mountainous landscapes were created. It also gives evidence that this uplift only occured in the last few million years, a time scale which does not fit the plate tectonics theory. Another part of the evidence, shows that mountain uplift correlates very well with climatic change. Mountain building could have been responsible for the onset of the ice age. It certainly resulted in the creation of new environments.