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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Etat : 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. N° de réf. du vendeur 4092955
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Buch. Etat : 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. N° de réf. du vendeur 9781402022647
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Buch. Etat : 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. N° de réf. du vendeur 102377574
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Buch. Etat : 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). N° de réf. du vendeur 9781402022647
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Buch. Etat : 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. N° de réf. du vendeur 9781402022647
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