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標題: Titlebook: Environmental Instrumentation; Leo J. Fritschen,Lloyd W. Gay Textbook 1979 Springer-Verlag New York Inc. 1979 Barometer.Meteorologisches I [打印本頁]

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書目名稱Environmental Instrumentation影響因子(影響力)

書目名稱Environmental Instrumentation影響因子(影響力)學科排名

書目名稱Environmental Instrumentation網(wǎng)絡公開度

書目名稱Environmental Instrumentation網(wǎng)絡公開度學科排名

書目名稱Environmental Instrumentation被引頻次

書目名稱Environmental Instrumentation被引頻次學科排名

書目名稱Environmental Instrumentation年度引用

書目名稱Environmental Instrumentation年度引用學科排名

書目名稱Environmental Instrumentation讀者反饋

書目名稱Environmental Instrumentation讀者反饋學科排名

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Drives in the Secondary Literature,tes more energy than it receives and the environment receives more energy than it radiates. There is, thus, a net transfer of energy from the warm black body to the cooler environment. The basic problem is to determine the direction and rate of this net energy transfer.

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0172-6226 tions linking biological responses to atmospheric variables, (2) development of improved data acquisition and handling equipment, (3) the application of modeling to environmental problems, and (4) the implementation of large, cooperative studies of international scope. The consequences of man‘s poss

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Conclusion: The Transit-Oriented Region,es in this book will find their greatest usefulness in evaluating processes, such as growth, development, photosynthesis, or transpiration, rather than inventory or description of environmental factors.

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https://doi.org/10.1007/978-3-030-23444-7 . is the rate at which the entity . is being transferred per unit of time, . is the area through which the transfer occurs, . is a proportionality coefficient, and . is the change in potential for transfer with change in distance z.

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https://doi.org/10.1007/978-3-030-39423-3but more sensitive sensors are often needed for air pollution monitoring and environmental measurements. For environmental measurements, the anemometers should generate an electrical signal suitable for transmission and recording. Research needs and wind tunnel studies often require sensitive anemometers with frequency responses as high as 10. Hz.

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Internal Objectives: Empirical Evidence,gnals which, in turn, are recorded and interpreted. The conversion has been accomplished by a variety of transducers. The information that is presented to the transducer and passed on by it (in converted form) can be classified as to whether the information is in electrical or nonelectrical form.

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Textbook 1979ing biological responses to atmospheric variables, (2) development of improved data acquisition and handling equipment, (3) the application of modeling to environmental problems, and (4) the implementation of large, cooperative studies of international scope. The consequences of man‘s possible alter

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Soil Heat Flux,rly sums are normally near zero, but daily values can be significant when the soil is heating in the spring or cooling in the fall. Hourly values of the soil heat flux can be large under dry bare soil conditions. Omission of soil heat flux measurements from hourly energy budget analyses will introdu

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Wind Speed and Direction, linear response to a wide range of velocities. The WMO, (1971) contains instrument guidelines for many types of routine meteorological measurements, but more sensitive sensors are often needed for air pollution monitoring and environmental measurements. For environmental measurements, the anemomete

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https://doi.org/10.1007/978-1-4612-6205-3Barometer; Meteorologisches Instrument; Scale; Wind direction; Wind speed; biological; complexity; energy; e

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Environmental Instrumentation978-1-4612-6205-3Series ISSN 0172-6226

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https://doi.org/10.1007/978-3-030-23444-7location to another, and to the potential for transfer that exists at various locations. The general, one-dimensional form of this relation is . where . is the rate at which the entity . is being transferred per unit of time, . is the area through which the transfer occurs, . is a proportionality co

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