By Gaylon S. Campbell
From stories of the 1st edition:
"well prepared . . . prompt as an introductory textual content for undergraduates" -- AAAS technology Books and Films
"well written and illustrated" -- Bulletin of the yank Meteorological Society
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Additional resources for An Introduction to Environmental Biophysics
A. N. Hull, and T. M. L. Wigley (1974) Comments on ,. " J. Appl. Meteor. 13 :606-608. 4 Taylor, S. , and G. L. Ashcroft (1972) Physical Edaphology: The Physics of Irrigated and Nonirrigated Soils. San Francisco: W. H. Freeman. 4]. 2 What is the rate of water loss from your skin surface just after you get out of the swimming pool? 2. 43 kJ/g. 3 What is the water potential or component in each of the following? a. Gravitational potential at the base of a 50-m tree with z = 0 at the top of the tree b.
Finally an equilibrium will be established when the number of molecules escaping from the liquid water equals the number being recaptured by the liquid. If the liquid temperature were increased, the random kinetic energy of the molecules would increase, and more water would escape. At equilibrium, the vapor density or concentration would be higher over the warmer water. This equilibrium vapor density, established between liquid water and water vapor in a closed system, is known as the saturation vapor density for the particular temperature of the system.
02 X 1()23) of photons is often calculated. A mole of photons is called an Einstein (E). 2 x 105 J/E. The photon flux from a source can be found by dividing the energy flux at each wavelength of the source by the photon energy at the wavelength and summing over all wavelengths. If the spectrum of a source is reasonably continuous over a given waveband, the photon flux in that waveband can be calculated from the average energy over the waveband divided by the photon energy at the median wavelength.
An Introduction to Environmental Biophysics by Gaylon S. Campbell
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