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G' water Replinishment by infiltrated rain. Rainfall infiltrates downward to aquifer. Similar to drainage basins. May come from miles away beneath several surface watersheds for deeper ones. Wells are drilled into the zone of saturation, i.e., the aquifer. This may be a sand or gravel bed or perhaps a fracture zone in a crystalline (igneous or metamorphic) or sedimentary rock, or even saprolite, in some cases. |
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Develops with long term water saturation. Soils in which the upper 12 inches is water saturated for more than 1/8th of the growing season. |
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High Velocity rough bottom |
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Definition
causes of turbulent stream flow. Mountain stream- high gradient down stream. 1.High energy 2. High oxygen 3. Low temp = low biodiversity. |
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random treelike stream system |
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elevation change per unit distance (feet/mile) related to local topography & largely determines speed velocity. Limit to downward erosion. When base level rises upstream the gradient decreases= deposits sediment load. When base level drops downcutting occurs. |
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Meanders, natural levees, cutoffs |
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Definition
characteristics of low gradient rivers. Found in locations with low gradients with wide flood plains. Low gradient rivers. |
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flowing water eco systems. examples: Creeks, rivers |
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Can occur in upland areas with clay rich soils (like gpc campus).poorly drained, with retained sulfur and methane.Can occur on flood plains, hilltops on rare occasions when excessive clay will not allow drainage. On floodplain a wetland may not be next to a creek or river. |
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Roundness of stream pebbles |
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Definition
Is related to stream transport distance and mineral hardness. Sediment size is related to water energy. ex. angular/sub-rounded pebbles. |
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contains large number of small ecosystems |
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standing water ecosystems. examples – ponds, lakes, swamps, marshes, various wetlands types |
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"Over-silted" stream. Too much sand. |
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Rock breakage by faults, joints, fractures |
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Definition
facilitates erosion of streams/rivers. Joints and fractures can do the same thing. |
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Term
Aquatic abiotic components |
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Definition
temperature dissolves oxygen, pH Water depth Water energy/gradient (Lotic only) Water chemistry (dissolved O2, dissolved solids) Water clarity Water temperature Bottom topography and type |
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Evidence of a rapid base level drop/local uplift |
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Process of lake and land ecosystem change |
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Small stream with local spring source |
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vertical limit to downcutting |
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Definition
Topographic basin that catches rainfall |
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youthful stream characteristics |
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Definition
High gradient v shaped valleys (slide 8) |
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Definition
shallow shelflike lake ecosystem with plants. Must be close to surface, protects smaller creatures against larger creatures and is a nursery area. |
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erosion on the outside of a meander bend |
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Definition
top of underground water saturation zone. Is usually not flat. Is a subdued replica of a ground surface. Less recharge area on top of a hill and that means a higher chance of well drying out. As surface water streams have a gradient so does this. Ground water flows in a general direction as ground slow down stream. |
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Definition
short term rainfall and temp. events |
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Definition
periodic changes in pacific circulation. May be driven by Solar activity. Under normal conditions: NE and SE trade winds combine to form E to W moving winds along Inter-Tropical Convergence Zone across Pacific Ocean. Every 3 to 7 years, these winds weaken. |
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Definition
the primary cause of north american deserts. Opposite side of orographic |
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difference between night and day temps. Greenhouse effect shields earth from excessive variations. |
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Definition
wispy high altitude clouds |
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Definition
most common atmospheric gas which is composed of 78%. Important atmospheric functions include shielding earths surface from UV, x-rays, cosmic rays from space while allowing visible and infrared wavelengths to penetrate atmosphere. |
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Definition
vertical atmospheric circulation driven by equatorial heating. Vertical air movement of cells lead to 1. a persistent low pressure zone at equator ( 0 degrees) 2. Persistent mid latitude high pressure zone at 30 degrees north (across Africa) 3. strong persistent polar high causes polar eastarly |
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creates monsoon conditions |
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Definition
Summertime heating of large continents. Generates intense convection that draws warm, moist air inland from Indian Ocean. Orographic lifting caused by Himalayan mtns. results in flooding of ganges river. Flooding issues. |
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Definition
30+ year average of atmospheric events. Sun provides the energy that drives the Earth’s climate. Variations in Solar activity and the Earth’s orbit primarily affect this. |
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counter clockwise circulation rising air |
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air mass uplift by encounter with mountains. opp. side rain shadow effect. |
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condition that causes earth's seasons. Variations in earth's surface temperatures and climate are due to earth's axis in relation to the sun and unequal distribution of land vs. water and differential thermal characteristics of land and water. Seasonal changes happen largely because of this |
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release of water vapor from trees/plants |
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lowest layer of atmosphere. "Weather maker". Turbulent, rich in water vapor/droplets. |
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Definition
contains atmospheric ozone, ozone shield. steady wind but little turbulence. Ozone not present as layer but prevalent 10 - 15 ft above earth's surface. Ozone is more dense and effective but unstable. Thinning seems seasonal, greatest in September. |
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middle latitude high pressure zone |
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Definition
persistent falling air at 30 degrees latitude |
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tropical zone of low pressure convection |
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Term
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Definition
horizontal/ latitudinal wind belts. 0 to 30 degree North – Northeast Trade Winds 30 degree to 60 degree North – Westerlies Wind Belt – Jet Stream 60 degree to 90 degree North – Polar Easterlies There is interaction between jet stream and polar easterlies. |
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water vapor and condensation nuclei |
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N hemisphere, clockwise ocean circulation. Combined actions of horizontal wind belts and hadley cells and earths rotation leads to this. Clockwise rotation of ocean currents in n. hemisphere. ex. gulf stream carries heat from subtropics northward carries enough to warm NW coastline of north america. |
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Udder shaped clouds beneath "supercells" |
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Definition
clockwise circulation, falling air |
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Definition
No floodplains, high gradient, high energy, low diversity, v-shaped valleys, mature floodplains, moderate gradient, local meanders, greater diversity. |
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Definition
Wide floodplains, low gradient, meanders and related features. |
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lower energy/moderate. Drought triggered drop in local base level causing downcutting. |
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How humans change base levels |
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Definition
Building dams. As lake fills, the local base level rises upstream. Gradient decreases = deposition. |
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Usually "out of sight out of mind" unless our individual home or city depends on one or more wells for irrigation or water supply. Ground water furnishes 50% of US population's drinking water and 25% of industry's needs. Helps to store freshwater that sustains streamflow, after run off effects of the last rain end. |
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Definition
body of rock or sediment that can hold and transmit usable quantities of ground water. |
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impermeable zones or layers of rock or sediment that do not pass water easily. Also called "confining" bed. |
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The importance of proper well completion – Apparent lack of near surface grouting and concrete surface pad = potential contamination of unconfined (shallow) aquifer. Coastal plain needs larger surface pad. |
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Definition
Aquifer that is “open” to the un-saturated zone, i.e., it is not overlain by an aquitard. The water must be pumped to reach the surface. Is directly recharged by rainfall. |
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Definition
Overlain by an aquitard and pressurized by "up-gradient" water. Wells into confined aquifer are called artesin wells. |
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Definition
Reason why wind blows. Caused by earth's rotation, uneven distribution of landmass. Properties of heat transfer between air/water/land. Solar energy |
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Air rising counter clockwise. Weather maker. Most favorable for rain/snow. |
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Clockwise falling air, fewer clouds. Divergence at surface. |
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Definition
dynamic move-ment of water through the atmosphere, over & below the land surface, through the life cycles of plants and animals, and to and from the oceans & other water bodies. Components: Evaporation/Transpiration Condensation Precipitation Runoff/Infiltration |
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Solar heat Methane Orbital eccentricity Ocean currents Axial tilt Ocean heat Axial wobble Plate Tectonics Water vapor Continent locations Water droplets Land elevations Carbon dioxide Chemical weathering Vulcanism Bolide impacts All of these drivers are of differing impact and all are subject to change. Some are random events, some are susceptible to cycles, some are affected by both random events and cycles of activity. |
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Some climate drivers combine to produce a greater effect. |
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Some climate drivers cancel each other out. |
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composed of minute water droplets and/or ice crystals. Components/Processes needed : Moist air Condensation nuclei Uplift mechanism – Convection, Cyclonic, Weather Front, Orographic
localized flooding |
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