Massman William (18 results)

Paperback. Condition: New. Print on Demand. This book explores the complex and multifaceted phenomenon of acid deposition and its significant impact on terrestrial and aquatic ecosystems. The author delves into the history of acid rain research, tracing its origins from anecdotal observations to the establishment of scientific consensus. The book examines the intricate chemical processes involved in the formation of acid rain and explores the sources of sulfur and nitrogen oxides that contribute to its occurrence. The author also investigates the ecological consequences of acid deposition, highlighting its detrimental effects on forests, lakes, and aquatic organisms. By presenting a comprehensive analysis of acid deposition, this book provides valuable insights into the environmental challenges posed by this phenomenon and the scientific efforts to understand and mitigate its impacts. This book is a reproduction of an important historical work, digitally reconstructed using state-of-the-art technology to preserve the original format. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in the book. print-on-demand item.

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Taschenbuch. Condition: Neu. Handbook of Micrometeorology | A Guide for Surface Flux Measurement and Analysis | Xuhui Lee (u. a.) | Taschenbuch | xiv | Englisch | 2010 | Springer | EAN 9789048166275 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.

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Taschenbuch. Condition: 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).

Buch. Condition: 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).

Paperback. Condition: Brand New. 264 pages. 9.50x6.20x0.60 inches. In Stock.

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Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -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 provides useful insight for interpreting estimates of mass and energy exchange and understanding the role of the terrestrial biosphere in global environmental change. 264 pp. Englisch.

Condition: 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.

Condition: 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.

Buch. Condition: 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.

Buch. Condition: 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.

Buch. Condition: 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.

Taschenbuch. Condition: 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 264 pp. Englisch.