Descriptive Micrometeorology

Descriptive Micrometeorology

Author: R. E. Munn

Publisher: Elsevier

Published: 2013-09-12

Total Pages: 260

ISBN-13: 1483282252

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Descriptive Micrometeorology compiles views and findings in micrometeorology, which is concerned with the surface boundary layer or thin slice of atmosphere extending from the ground up to a height of approximately 50 meters. This book describes the micrometeorology of soil, short vegetation, forest, water, ice, snow, and built-up urban surfaces. The properties and influence of the planetary boundary layer are not included. The topics discussed include the energy balance at the earth-atmosphere boundary, radiative flux divergence, factors influencing air temperatures, and Kolmogorov similarity theory. The Eddy correlation method for measuring evaporation, radiation balance of snow and ice surfaces, heat storage and horizontal advection in water, and changes in wind patterns are also covered. This publication is intended for meteorologists, but is also a good reference for chemists, engineers, geographers, botanists, hydrologists, health physicists, glaciologists, town planners, limnologists, oceanographers, air pollution control officers, foresters, and ecologists interested in the surface boundary layer.


Boundary-Layer Meteorology 25th Anniversary Volume, 1970–1995

Boundary-Layer Meteorology 25th Anniversary Volume, 1970–1995

Author: John R. Garratt

Publisher: Springer Science & Business Media

Published: 1996-09-30

Total Pages: 434

ISBN-13: 9780792341918

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The journal Boundary-Layer Meteorology was started in 1970 and has become the premier vehicle for the publication of research papers in its field. Dr R.E. Munn served as Editor-in-Chief until recently. The special 25th Anniversary volume, on which this book is based, was compiled from review and other articles solicited and selected as a `Festschrift' to honour Ted Munn's achievement as editor of the journal over that time. Articles by leading contributors to the field include reviews of field studies (Askervein, HEXOS, Cabauw) and their impacts; numerical modelling (large-eddy simulation of the surface layer, frontal structures); analyses and critical discussions (of the von Karman constant, bulk aerodynamic formulations, air-sea interaction, vegetation canopies); and reviews or previews of progress in our understanding of the atmospheric boundary layer, turbulence simulation, Lagrangian descriptions of turbulent diffusion and remote sensing of the boundary layer. The collection provides an excellent perspective on the state of the subject and where it is headed. It should provide fascinating and stimulating reading for researchers and students of boundary-layer meteorology and related areas.


Introduction to Micrometeorology

Introduction to Micrometeorology

Author: Paul S. Arya

Publisher: Academic Press

Published: 1989-01-09

Total Pages: 331

ISBN-13: 0080959822

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This up-to-date textbook is highly recommended for introductory courses offered at undergraduate and graduate levels. Coverage begins with basic fluid and thermodynamical laws and concepts, then moves on to cover such major topics as momentum and heat exchanges with homogeneous surfaces, nonhomogeneous boundary layers, fundamentals of turbulence, and more. This book introduces the reader to theoretical concepts and quantitative relations through qualitative descriptions based upon observations.


The Climate Near the Ground

The Climate Near the Ground

Author: Rudolf Geiger

Publisher: Rowman & Littlefield

Published: 2009

Total Pages: 648

ISBN-13: 9780742555600

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This revised and updated edition of Rudolf Geiger's classic text provides a clear and vivid description of the surface microclimate, its physical basis, and its interactions with the biosphere. The book explains the principles of microclimatology and illustrates how they apply to a wide array of subfields. Those new to the field will find it especially valuable as a guide to understanding and quantifying the vast and ever-increasing literature on the subject. Designed as an introductory text for students in environmental science, this book will also be an essential reference for scientists seeking a clear understanding of the nature and physical basis of the climate near the ground, and its interactions with the biosphere.


Surface Climates of Canada

Surface Climates of Canada

Author: Timothy R. Oke

Publisher: McGill-Queen's Press - MQUP

Published: 1998-01-15

Total Pages: 396

ISBN-13: 0773563571

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In the opening chapters contributors lay out the large-scale context of the physical climate of Canada, introducing the processes, balances, and dynamic linkages between the surface and atmosphere that create and maintain the diversity of surface climates found in Canada as well as outlining the nature of the physical processes that operate near the ground's surface. Individual chapters are dedicated to snow and ice - the almost universal surface cover in Canada - and the other major natural surface environments of Canada: ocean and coastal zones, fresh water lakes, wetlands, arctic islands, low arctic and subarctic lands, forests, and alpine environments. The final part of the book considers those surface environments that have been strongly influenced by human activity, such as agricultural lands and urban environments, and examines the prospects for future climate change. Bringing together for the first time a wide range of scholarship by leading climatologists, The Surface Climates of Canada will be an indispensable tool for understanding Canada's surface climates and the processes responsible for their creation and control. Contributors include Brian D. Amiro (AECL), W.G. Bailey (Simon Fraser), Richard Bello (York), Terry J. Gillespie (Guelph), Barry E. Goodison (Atmospheric Environment Service), F. Kenneth Hare (emeritus professor, Toronto), L.D. Danny Harvey (Toronto), Owen Hertzman (Dalhousie), Peter M. Lafleur (Trent), J. Harry McCaughey (Queen's), Linda Mortsch (Environment Canada), R. Ted Munn (Toronto), D. Scott Munro (Toronto), Atsumu Ohmura (Swiss Federal Institute of Technology), Timothy R. Oke (UBC), John W. Pomeroy (Environment Canada), Alexander W. Robertson (Canadian Forest Service), Nigel T. Roulet (McGill), Wayne R. Rouse (McMaster), Ian R. Saunders (Simon Fraser), William M. Schertzer (Environment Canada), Hans-Peter Schmid (Indiana), David L. Spittlehouse (BC Ministry of Forests), Douw G. Steyn (UBC), John L. Walmsley (Atmospheric Environment Service), John D. Wilson (Alberta), Ming-Ko Woo (McMaster).


Grassland Simulation Model

Grassland Simulation Model

Author: G. S. Innis

Publisher: Springer Science & Business Media

Published: 2012-12-06

Total Pages: 317

ISBN-13: 1461299292

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Perspectives on the ELM Model and Modeling Efforts This volume is the major open-literature description of a comprehensive, pioneering ecological modeling effort. The ELM model is one of the major outputs of the United States Grassland Biome study, a contribution to the International Biological Program (IBP). Writing this introduction provides wel come personal opportunity to (i) review briefly the state of the art at the beginning of the ELM modeling effort in 1971, (ii) to discuss some aspects of the ELM model's role in relation to other models and other phases of the Grassland Biome study, and (iii) to summarize the evolution of ELM or its components since 1973. Pre-Program Historical Perspective My first major contacts with ecological simulation modeling were in 1960 when I was studying intraseasonal herbage dynamics and nutrient production on foothill grasslands in southcentral Montana, making year-round measurements of the aboveground live vegetation, the standing dead, and the litter. Limitations in funding and the rockiness of the foothill soils prevented measuring the dynamics of the root biomass, both live and dead. Herbage biomass originates in live shoots from which it could be translocated into live roots or the live shoots could transfer to standing dead or to litter. Standing dead vegetation must end up in the litter and the live roots eventually transfer to dead roots. Obviously, the litter and the dead roots must decay away.