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WATER CYCLE Condensation Precipitation Transpiration Infiltration Evaporation Ground water WATER BUDGET V. FINANCIAL BUDGET Evaporation, transpiration, Continuous cycle of evapotranspiration , condensation, and precipitation. Affected by temperature, vegetation, wind, precipitation and Water budget -Vary by location Incoming (increase): Precipitation Condensation Outgoing (Decrease): Evapotranspiration Financial budget Incoming: Paycheck Misc. income Outgoing: Expenses GEOGRAPHY WATER BUDGETS IN C R EA S ED WAT ER BUDGETS D EC R EA S E WAT ER BUDGETS Wet areas: Rain forests, Swamps, Marshes Dry areas: Deserts, Plains, Mountainous areas (rain shadow) Low evaporation and more rain High evaporation (more direct sunlight) less rain MICHIGAN’S WATER BUDGET WATER USAGE COMMON RIVER FEATURES Describe common river system features • • Headwaters Beginning of a stream (high elevation) Watershed • Bend/curve in a river • Land that allows runoff water to enter a stream/river • Tributary Divide • Cutbank • Point Bar • Delta Land that separates water sheds • Floodplain Valley that can be covered by water in flood conditions Oxbow Lake that is left after river changes direction (old meander) Feeder stream • Meander Outside section of meander, high erosion area Inside section of meander, eroded material (sediment) deposited here Fan shaped deposit at the mouth of a stream (before enters the sea) DIAGRAM headwaters divide watershed tributary oxbow cutbank Floodplain delta meander point bar Headward: 3 WAYS THAT RIVERS ERODE SEDIMENT process of lengthening and branching of a stream where the run off first occurs * carries away sediment from the slopes of the watershed Downcutting: process that deepens the channel of a stream or valley by removing material from the stream's bed or the valley's floor. *erodes sediments down creating deeper channel Meandering: moving water in a stream erodes the outer banks and widens its valley, and the inner part of the river has less energy and deposits silt. *erodes side to side to side SEDIMENT CARRIED BY STREAMS (STREAM LOAD) Bed Load: Coarse sand, gravel and pebbles Sliding, rolling or Saltation Suspended Load: Particles of fine sand and silt Moving water keeps them suspended (very small) Dissolved load: Mineral matter transported Transported in dissolved liquid solution STREAM GRADIENT Stream gradient :is the grade measured by the ratio of drop in elevation of a stream per unit horizontal distance, usually expressed as feet per mile or meters/kilometers. Change in elevation Gradient = -------------------------------------- Change in distance Young Streams/ Rivers Narrow channels Small flood plains Downcutting Deep slopes Waterfalls Distance Velocity= -------------------------------- Time Older Rivers • Wide channels • Large flood plains • lateral erosion • gentle slopes FLOODING - overflow of water that submerges land which is usually dry. Natural flooding: heavy rain fall Snow melting Hurricanes Human based: Dams Destruction of wetlands (natural flood protection) Pavement GROUND WATER Porosity: is a measure of the void (i.e., "empty") spaces in a material. High= gravel Low=clay GROUNDWATER Permeability: is a measure of the ability of a porous material (rock, or sediment) to allow fluids to pass through it. In other words how quickly water passes through open spaces (pores). ZONES OF GROUNDWATER Zone of Aeration: Space between Earth’s surface and water table, spaces or pores filled with air. (unsaturated zone) ZONES OF GROUNDWATER Zone of Saturation : All pores are filled with water. Water table: upper surface or start of saturation zone GROUND WATER Aquifer: is an underground layer of waterbearing permeable rock or unconsolidated materials (sandstone, limestone) GROUND WATER Aquitard: is a zone within the earth that restricts the flow of groundwater from one aquifer to another. (shale) WELLS Ordinary well: water is pumped to surface from below the water table Artesian well: water flows from far away, no pumping needed Superior Michigan Huron Ontario St. Clair Erie