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Micrometeorology is a branch of meteorology that is concerned with atmospheric phenomena and processes near the ground at scales of tens of meters to several kilometers. Progress in micrometeorologyismade throughexperimentalinvestigationofthesephenomenaandquantitative studyattemptingtobringordertoexperimentaldata. Studiesofsurfa- air ?ux play a crucial role in this endeavor. The current paradigm of micrometeorology builds on two premises: (i) that scale separation exists so that the microscale phenomena can be treated more or less in isolation of phenomena occurring at larger scales, and (ii) that these phenomena are in?uenced by the surface to such an extent that “external factors” can be ignored. Quantitative studies have been based on the assumption of horizontal homogeneity, which inevitably biases the investigation toward over-idealization of the real world by restricting it to perfectly ?at topography and daytime, fair weather conditions. This bias was noted by John Philip 40 years ago: “Experimenters attempt to avoid [advection] by working on sites downwind of extensive ‘homogeneous’ areas. Sometimes advection is invoked to explain otherwise inexplicable observations...” (J. Meteorol. 16, 535).
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The Handbook of Micrometeorology is the most up-to-date reference for micrometeorological issues and methods related to the eddy covariance technique for estimating mass and energy exchange between the terrestrial biosphere and the atmosphere. It is intended to provide micrometeorologists, ecosystem scientists, boundary-layer meteorologists, and students involved in micrometeorology with the state of science on measurement and analysis. The Handbook is the culmination of many detailed discussions of theory, analysis, and practical applications by the leading scientists in the field. It provides useful advice for bringing coherence to estimates of mass and energy exchange for understanding the role of the terrestrial biosphere in global environmental change.
Titel: Handbook of Micrometeorology: A Guide for ...
Verlag: Springer
Erscheinungsdatum: 2004
Einband: Hardcover
Zustand: New
Anbieter: BennettBooksLtd, Los Angeles, CA, USA
Hardcover. Zustand: New. In shrink wrap. Looks like an interesting title! Bestandsnummer des Verkäufers Q-1402022646
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Zustand: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Up-to-date reference on micrometeorologyAddressing both advanced researchers and studentsThe Handbook of Micrometeorology is the most up-to-date reference for micrometeorological issues and methods related to the eddy covariance techniq. Bestandsnummer des Verkäufers 4092955
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Buch. Zustand: Neu. Handbook of Micrometeorology | A Guide for Surface Flux Measurement and Analysis | Xuhui Lee (u. a.) | Buch | xiv | Englisch | 2004 | Springer | EAN 9781402022647 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu Print on Demand. Bestandsnummer des Verkäufers 102377574
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Anbieter: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Deutschland
Buch. Zustand: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Micrometeorology is a branch of meteorology that is concerned with atmospheric phenomena and processes near the ground at scales of tens of meters to several kilometers. Progress in micrometeorologyismade throughexperimentalinvestigationofthesephenomenaandquantitative studyattemptingtobringordertoexperimentaldata. Studiesofsurfa- air ux play a crucial role in this endeavor. The current paradigm of micrometeorology builds on two premises: (i) that scale separation exists so that the microscale phenomena can be treated more or less in isolation of phenomena occurring at larger scales, and (ii) that these phenomena are in uenced by the surface to such an extent that 'external factors' can be ignored. Quantitative studies have been based on the assumption of horizontal homogeneity, which inevitably biases the investigation toward over-idealization of the real world by restricting it to perfectly at topography and daytime, fair weather conditions. This bias was noted by John Philip 40 years ago: 'Experimenters attempt to avoid [advection] by working on sites downwind of extensive 'homogeneous' areas. Sometimes advection is invoked to explain otherwise inexplicable observations.' (J. Meteorol. 16, 535). 268 pp. Englisch. Bestandsnummer des Verkäufers 9781402022647
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Buch. Zustand: Neu. This item is printed on demand - Print on Demand Titel. Neuware -Micrometeorology is a branch of meteorology that is concerned with atmospheric phenomena and processes near the ground at scales of tens of meters to several kilometers. Progress in micrometeorologyismade throughexperimentalinvestigationofthesephenomenaandquantitative studyattemptingtobringordertoexperimentaldata. Studiesofsurfa- air ux play a crucial role in this endeavor. The current paradigm of micrometeorology builds on two premises: (i) that scale separation exists so that the microscale phenomena can be treated more or less in isolation of phenomena occurring at larger scales, and (ii) that these phenomena are in uenced by the surface to such an extent that ¿external factors¿ can be ignored. Quantitative studies have been based on the assumption of horizontal homogeneity, which inevitably biases the investigation toward over-idealization of the real world by restricting it to perfectly at topography and daytime, fair weather conditions. This bias was noted by John Philip 40 years ago: ¿Experimenters attempt to avoid [advection] by working on sites downwind of extensive ¿homogeneous¿ areas. Sometimes advection is invoked to explain otherwise inexplicable observations.¿ (J. Meteorol. 16, 535).Springer-Verlag KG, Sachsenplatz 4-6, 1201 Wien 268 pp. Englisch. Bestandsnummer des Verkäufers 9781402022647
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Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Micrometeorology is a branch of meteorology that is concerned with atmospheric phenomena and processes near the ground at scales of tens of meters to several kilometers. Progress in micrometeorologyismade throughexperimentalinvestigationofthesephenomenaandquantitative studyattemptingtobringordertoexperimentaldata. Studiesofsurfa- air ux play a crucial role in this endeavor. The current paradigm of micrometeorology builds on two premises: (i) that scale separation exists so that the microscale phenomena can be treated more or less in isolation of phenomena occurring at larger scales, and (ii) that these phenomena are in uenced by the surface to such an extent that 'external factors' can be ignored. Quantitative studies have been based on the assumption of horizontal homogeneity, which inevitably biases the investigation toward over-idealization of the real world by restricting it to perfectly at topography and daytime, fair weather conditions. This bias was noted by John Philip 40 years ago: 'Experimenters attempt to avoid [advection] by working on sites downwind of extensive 'homogeneous' areas. Sometimes advection is invoked to explain otherwise inexplicable observations.' (J. Meteorol. 16, 535). Bestandsnummer des Verkäufers 9781402022647
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Hardcover. Zustand: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book. Bestandsnummer des Verkäufers ERICA75814020226465
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