Laserfiche WebLink
<br />, <br /> <br />it approximates the end of the growIng season; c) There is a mini.nn.nn <br />probable error due to the effect of ice in the records of winter flow <br />if the discharge for the winter period (November to April) is computed <br />together at one time; d) The winter or base flow period coincides <br />with reduced metabolic functions and decreased demands for vital life <br />elements by most aquatic organisms (e.g., oxygen, food, removal of <br />waste products, and increased tolerance to pollution); e) A low flow <br />winter period ~tches the downstream migration habits of many fishes <br />(warmwater and coldwater), when they travel to deeper more permanent <br />water to spend the winter. This is also the spawning and incubation <br />season for most salmonids, when they naturally seek less water by <br />moving into headwater or tributary streams and onto redds in shoal <br />or shallow riffle areas; and f) Higher summer flow regimens provided <br />by this method coincide with the frost-free, recreation season and <br />the major growth period for most aquatic plants and animals, when their <br />requirements for dissolved gases, space, food, and removal of septic <br />waste products are naturally higher (the attendant increased width, <br />depth, and velocities in the stream all serve to enhance the availa- <br />bility of elements vital to these recreation uses and critical life <br />functions). These phenomena may be seasonally reversed for anadromous <br />fishes using the coastal streams of Alaska, the Canadian Provinces, and <br />our west coast states and flow regimens should be adjusted accordingly. <br /> <br />4 <br /> <br />Using the ~ntana Method, it is easy to adjust to above or below <br />normal water years and maintain stream flows that are appropriate <br />portions of monthly, quarterly, or annual instream supplies of water. <br />This helps fish, wildlife, and aquatic resources share surpluses and <br /> <br />15 <br />