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Books > Earth & environment > Earth sciences > Meteorology
General Circulation Models (GCMs) are rapidly assuming widespread
use as powerful tools for predicting global events on time scales
of months to decades, such as the onset of EL Nino, monsoons, soil
moisture saturation indices, global warming estimates, and even
snowfall predictions. While GCMs have been praised for helping to
foretell the current El Nino and its impact on droughts in
Indonesia, its full power is only now being recognized by
international scientists and governments who seek to link GCMs to
help them estimate fish harvests, risk of floods, landslides, and
even forest fires.
This topical textbook provides a bridge between technical and popular texts on global warming within the broader context of climate change. Written at an introductory level, it explains the interacting components of this system: what the greenhouse effect is; and how scientists seek to predict climate change. It makes accessible the technical and heavy science literature to the 'non-science' student.Global warming is one of the major environmental problems facing the world today. But it is an issue surrounded by great contention because it is based largely on scientific prediction and has yet to be proven. Opinion is divided regarding whether global warming will occur and, if it does, what the effects will be. In order to appreciate the uncertainties surrounding this issue, it is necessary to understand the workings of the climate system and the methods by which scientists seek to predict climate change.'Global Warming' aims to make accessible the heavily technical literature to the non-science student, providing a bridge between the highly scientific and the popular non-academic texts. Placing global warming within the broader context of climate change, this textbook details the interacting components of the climatic system, reviewing the importance of changing carbon dioxide levels for the evolution of the Earth's atmosphere and climate. Utilising observed and modelled data, it presents the latest evidence for and against global warming whilst highlighting the difficulties involved with analysing both types of data and introducing areas of controversy within research. The book also addresses the important problem of making policy decisions for the future, based on the uncertain science of global warming.
First Published in 2000. Routledge is an imprint of Taylor & Francis, an informa company.
Statistical and machine learning methods have many applications in the environmental sciences, including prediction and data analysis in meteorology, hydrology and oceanography, pattern recognition for satellite images from remote sensing, management of agriculture and forests, assessment of climate change, and much more. With rapid advances in machine learning in the last decade, this book provides an urgently needed, comprehensive guide to machine learning and statistics for students and researchers interested in environmental data science. It includes intuitive explanations covering the relevant background mathematics, with examples drawn from the environmental sciences. A broad range of topics are covered, including correlation, regression, classification, clustering, neural networks, random forests, boosting, kernel methods, evolutionary algorithms, and deep learning, as well as the recent merging of machine learning and physics. End-of-chapter exercises allow readers to develop their problem-solving skills and online data sets allow readers to practise analysis of real data.
These proceedings are based upon the review lectures, the re search talks and the accompanying discussion from the NATO Advanced Study Institute on "The Dynamical and Chemical Coupling of the Neutral and Ionized Atmosphere" held at Spatind, Norway April 12-22, 1977. In recent years, in spite of the many subdivisions of atmospher ic physics it has become clear that a complete understanding of the subject matter requires an interdisciplinary effort of the scien tists working on a variety of atmospheric phenomena. This Advanced Study Institute was organized in order to meet this demand. A number of eminent scientists were invited to review the major subfields in atmospheric physics and expose the areas where the coupling between the neutral and ionized atmosphere is evident. These review papers were supported by current research results. However, the material covered here is by no means complete con sidering the range of subject matter covered by the title. The re sponsibility for this inadequacy lies with the editors and the pro gram committee, rather than with the individual contributors. Oslo, June 1977. B. Grandal J.A. Holtet. PARTICIPANTS Max-Planck-Institute for Nuclear Physics Arnold, F. P.O.Box 1248, D-0069 Heidelberg F.R.G. Bj centsrn, L. Uppsala Ionospheric Observatory S-755 90 Uppsala Sweden The Institute for Mathematical and Physical Brekke, A."
Understanding and predicting the Earth's climate system,
particularly climate variability and possible human-induced climate
change, presents one of the most difficult and urgent challenges in
science. Climate scientists worldwide have responded to that
challenge over the past decade by creating a wide variety of ever
more sophisticated climate models that are beginning to show
considerable ability to replicate many aspects of the climate
system. At the same time, to fully understand climate change, one
also has to look to past climates. For this purpose five eminent
scholars who span the disciplines of modeling and observation,
including elements of past, present and future climate studies came
together at this Les Houches school. They presented a systematic
development of each of their respective subjects which provided a
comprehensive overview of this vast and complex subject. These core
lectures were supplemented by a set of shorter lectures and of
seminars.
Global Warming: The Hard Science presents a comprehensive,
qualitatively rigorous, and critical discussion of the science
underlying the global warming issue. The major processes in the
climate system needed to understand projected human-induced
climatic change are presented in detail. Observational systems used
to monitor changes in the climate system and the ways in which the
raw data are analyzed in order to produce estimates of current
trends are also critically reviewed.
Atmospheric and climatological studies are becoming more and more
important in day-to-day living. Winds and ocean current owe their
existence to the thermodynamic imbalances that arise from the
differential heating of the Earth and air by the sun. Accounting
for heat exchanges with the atmosphere and ocean is essential in
any predictive model of the ocean and/or atmosphere. Thermodynamic
feedback processes in the atmosphere and ocean are critical to
understanding the overall stability of the Earth's climate and
climate change. Water and its phase changes make the thermodynamics
of the atmosphere and ocean uniquely interesting and
challenging.
Global climate change has emerged as one of today's most challenging and controversial policy issues. In this significant new contribution, a roster of premier scholars examines economic and social aspects of that far-reaching phenomenon. Although the 1997 "summit" in Kyoto focused world attention on climate, it was just one step in an ongoing process. Research by the U.N.'s Intergovernmental Panel on Climate Change (IPCC) has been ongoing since 1988. An extensive IPCC Working Group report published in 1995 examined the economic and social aspects of climate change. In this new volume, eminent economists assess that IPCC report and address the questions that emerge. The result is a reasoned, cogent look at the realities of climate change and some methods (and difficulties) of dealing with them. William Nordhaus's introduction establishes the context for this book. It provides basic scientific background, reviews the IPCC's activities, and explains the genesis of the project. Subsequent contributions fall into two categories. Early chapters review analytical issues critical to social and economic understanding of climate change. For example, Granger Morgan looks at how typical decisionmaking frameworks relate to this topic. Other chapters in this section discuss discounting and intergenerational equity, the possible role of cost-benefit analysis, and the institutional architecture needed to address the problem effectively. A second set of chapters address specific economic questions surrounding climate-change policy. For example, John Weyant and Tom Kram look at the costs of slowing climate change. Weyant agrees with the IPCC that the economic cost is high, relative to othereconomic and environmental policies. There is tremendous uncertainty in these estimates, however, and different approaches to modeling -- economic, engineering, and social-psychological -- yield very different interpretations and prognoses. In another chapter, Robert Mendelsohn examines the costs of not slowing climate change. What impacts can we expect, how might they vary among different nations and regions, and how likely are we to encounter catastrophic results?
Richard John Chorley was known as a leading figure in quantitative geography in the late 20th Century and played an instrumental role in bringing the use of systems theory to geography. This set of 7 reissued works either edited by or written by Chorley offers a great wealth of scholarship on geography and geomorphology.
These proceedings record the results of climate change in many areas which are hyper-arid deserts today but which, almost cyclically, at intervals of thousands or even hundreds of thousands of years, have had a much more humid climate.
This text presents a comprehensive and up-to-date survey of the diverse climate of the British Isles. Examining the ways in which regional climates evolve from the interplay of meteorological conditions and geographies of the British Isles, leading climatologists provide detailed explanations of the climatic characteristics of eleven regions of the British Isles. Climatic distinctiveness and local weather contrasts are described for each region, together with a summary of climatic data from 1961 to the present.
'Dynamic Meteorology: A Basic Course' is an introduction to the physics of the atmosphere. Starting from the basics, it provides students with an awareness of simple mathematics and enthusiastically proceeds to provide a thorough grounding in the fundamentals of meteorology. The authors lead students to a scientifically rigorous understanding of the behaviour of weather systems such as highs, lows, fronts, jet streams and tropical cyclones. From the 'ABC' of the laws of Avogrado, Boyle and Charles to the powerful omega equation and beyond, this is a simple exposition of dynamic meteorology. Why does the wind blow along the lines of isobars rather than across them? Why are low pressure systems on the weather map more intense than high-pressure systems? Why is there much less constraint on the strength of the wind around a cyclone than an anticyclone? An international team of academic experts in meteorology answer these and many other fundamental questions with simple mathematical equations. Covering both northern and southern hemispheres, 'Dynamic Meteorology' equips students of earth and environmental sciences with proper understanding of the essential mathematics necessary to unlock the mysteries of the natural world.
This book is a collection of papers presented in the 30th International Geological Congress, held in Beijing, on structure of the lithosphere and deep processes. The papers deal with topics on the measurement of P-wave velocities in rocks, and elastic properties of crust and upper mantle.
This volume presents the results on contemporary geodynamic model, crustal stress field, active faults, folds and volcanoes. It discusses the tectonophysical environments of earthquake generation and the methodology of earthquake prediction.
Global climate and the effects of global warming are commanding unprecendented interest as climates grow more dynamic and changeable. How does global warming change patterns of climate? Why is the weather and climate of the British Isles so variable? Regional Climates of the British Isles presents a comprehensive survey of the diverse climate of the British Isles. Examining the ways in which regional climates evolve from the interplay of meteorological conditions and geography of the British Isles, leading climatologists provide detailed explanations of the climatic characteristics of 11 regions of the British Isles. Climatic distinctiveness and local weather contrasts are described for each region, together with a summary of climatic data from 1961 to the present. Reviewing the history and causes of climatic change and evaluating regional models, Regional Climates of the British Isles offers an analysis of climatic variations. Examining future climatic change and its likely consequences, the authors acknowledge the need for regionally diverse responses to the greenhouse effect.
A comprehensive and unique account of the creation of artificially
ionized layers in the middle and upper atmosphere, using powerful
radio waves. Major physical mechanisms associated with the
formation of the ionized region are studied in detail. The main
part of the author's research is devoted to problems associated
with the breakdown mechanisms for radio frequency discharges in
air. A special chapter deals with breakdown in intersecting pulsed
beams and the effects of recombination, diffusion and atmospheric
winds on the stability of the structure. The kinetics of the plasma
produced are also described.
This book focuses on different aspects of initiatives-to check pollution and to reduce consumption of fossil fuels-by the Association of Southeast Asian Nations (ASEAN). The chapters examine climate change projections for ASEAN, the relationship between income inequality and environmental sustainability, greening initiatives pursued by microfinance institutions, farmers' awareness and perceptions of climate change, potential introduction of hydrogen fuel cell vehicles in Malaysia, the impact of Euro-4 automobile emission regulations on the development of technological capabilities and the threats and vulnerability people face from climate change and national disasters. The United Nations Framework Convention for Climate Change's Conference of Parties meetings to cap temperature rise to 1.5 degrees Celsius over the next century has set the steering and the interventions essential for mitigating global warming. There is increasing recognition that initiatives must be taken across the globe regardless of the state of development of each individual country, and so this book has important practical implications. This book was originally published as a special issue of the Journal of the Asia Pacific Economy.
Stratospheric processes play a signi?cant role in regulating the weather and c- mate of the Earth system. Solar radiation, which is the primary source of energy for the tropospheric weather systems, is absorbed by ozone when it passes through the stratosphere, thereby modulating the solar-forcing energy reaching into the t- posphere. The concentrations of the radiatively sensitive greenhouse gases present in the lower atmosphere, such as water vapor, carbon dioxide, and ozone, control the radiation balance of the atmosphere by the two-way interaction between the stratosphere and troposphere. The stratosphere is the transition region which interacts with the weather s- tems in the lower atmosphere and the richly ionized upper atmosphere. Therefore, this part of the atmosphere provides a long list of challenging scienti?c problems of basic nature involving its thermal structure, energetics, composition, dynamics, chemistry, and modeling. The lower stratosphere is very much linked dynamically, radiatively, and chemically with the upper troposphere, even though the temperature characteristics of these regions are different. The stratosphere is a region of high stability, rich in ozone and poor in water - por and temperature increases with altitude. The lower stratospheric ozone absorbs the harmful ultraviolet (UV) radiation from the sun and protects life on the Earth. On the other hand, the troposphere has high concentrations of water vapor, is low in ozone, and temperature decreases with altitude. The convective activity is more in the troposphere than in the stratospher |
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