By D M Brink; G R Satchler

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25. J. J. Neale (1994). Ultraviolet radiation, ozone depletion, and marine photosynthesis. Photosyn. , 39, 303-320. 26. D. L. B. Coffin, A. J. S. P. Lesser, M. E. J. W. S. G. Impact of UV-B radiation on pelagic freshwater ecosystems. Arch. Hydrobiol. Beih. Ergebn. , 43,31-69. 27. F. Vincent, S. Roy (1993). Solar ultraviolet-B radiation and aquatic primary production: Damage, protection, and recovery. Environ. , 1, 1-12. 28. F. Xiong, J. Komenda, J. Kopecky, L. Nedbal (1997). Strategies of ultravioletprotection in microscopic algae.

Local solar noon is further modified by the “equation of time”, which gives a variation within the year by about +15 minutes, as a consequence of the elliptical Earth’s orbit around the sun and of the tilt of the Earth’s axis relative to the plane of the orbit. The sun rises and sets when cos z = 0, leading to an expression for the half daylength H of cos H = -tan 0 tan 6 The amount of incoming energy on a horizontal surface at the top of the atmosphere above a given location is then Eo = SO (ro /r)2cos z where r is the instantaneous Earth-sun distance, and ro its mean value.

In every detailed annual organic carbon budget of lake and river ecosystems, organic matter generated by phytoplankton will not support all of the heterotrophic metabolism of the ecosystem. At least several fold support of the total metabolism is by organic subsidies from the land-water interface communities and allochthonous production. From the standpoint of metabolic stability, it is particularly important that most of the organic carbon is dissolved and relatively recalcitrant, widely distributed within the inland waters.

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Angular momentum by D M Brink; G R Satchler

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