## Abstract Stream temperature is a complex function of energy inputs including solar radiation and latent and sensible heat transfer. In streams where groundwater inputs are significant, energy input through advection can also be an important control on stream temperature. For an individual stream
โฆ LIBER โฆ
Controls on biochemical oxygen demand in the upper Klamath River, Oregon
โ Scribed by Annett B. Sullivan; Dean M. Snyder; Stewart A. Rounds
- Book ID
- 116356123
- Publisher
- Elsevier Science
- Year
- 2010
- Tongue
- English
- Weight
- 587 KB
- Volume
- 269
- Category
- Article
- ISSN
- 0009-2541
No coin nor oath required. For personal study only.
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## Abstract For most cold region rivers, winter snowpack accumulation is the main contributor to spring runโoff events. This study investigated the synoptic controls on snowpack variability in the upper reaches of the Peace River Basin. An examination of snowpack accumulation at Grande Prairie, Alb