Titlebook: Micrometeorology; Thomas Foken Textbook 20172nd edition The Editor(s) (if applicable) and The Author(s), under exclusive license to Spring

巨碩

Thomas Foken selection of the meanings of homographs. In some research (e.g., Marcel, 1980; Schvaneveldt, Meyer, & Becker, 1976), the context has taken the form of a single word that is intended to bias the interpretation of a homograph. The effects of this bias on the subsequent recognition of a target are the

Coterminous

Thomas Foken selection of the meanings of homographs. In some research (e.g., Marcel, 1980; Schvaneveldt, Meyer, & Becker, 1976), the context has taken the form of a single word that is intended to bias the interpretation of a homograph. The effects of this bias on the subsequent recognition of a target are the

眼界

General Basics, are defined and presented in relation to the subject matter of this book. Besides an historical outline, the energy and water balance equations at the Earth’s surface and the transport processes are discussed. The first chapter of the book focus on the micrometeorological basics, which are then exp

CT-angiography

Basic Equations of Atmospheric Turbulence,asic equations. These include the equations of mean and turbulent motions, describing the transport and for energy and matter, and the conservation equation for the turbulence kinetic energy. To illustrate the importance of micrometeorological equations and parameterizations for modelling on all sca

Chromatic

Specifics of the Near-Surface Turbulence, obstacles, steady-state conditions, and others. Such conditions are rarely found in the nature, since the Earth’s surface is never completely flat and surface properties vary. Furthermore, all processes are not steady-state because of changing cloudiness and the diurnal cycle of irradiation. In thi

ALERT

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含沙射影

巧思

Microclimatology, such as mountain and valley winds, land-sea wind circulations, and katabatic winds. These phenomena are the subjects of many textbooks. Therefore, the following chapter does not provide a comprehensive overview, but rather discusses some typical microclimatological phenomena. These phenomena are pr

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