Geomorphology Weekly Notes 3-1.htm
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<!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 3.2 Final//EN"> <!-- Created from PDF via Acrobat SaveAsXML --> <!-- Mapping table version: 28-February-2003 --> <HTML> <HEAD> <META name="dc.title" content="Energy - Open vs" > <META name="dc.date" content="2009-08-13T10:15:35-04:00" > <META name="dc.date.modified" content="2009-08-13T10:15:40-04:00" > <META name="generator" content="Adobe Acrobat Exchange-Pro 7.8" > </HEAD> <BODY bgcolor=white text=black link=blue vlink=purple alink=fushia > <DIV class="Sect" ><DIV ><P align="justify" ><FONT size="+1" color="#000000"></B>Energy - Open vs. closed systems<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Free vs. Bounded<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Dynamic/ Steady state/ Potential<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Weathering - Solution - Lava Cooling<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Volcanism / Diastrophism = open<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">(Erosion of hillside & sedimentary transport in H20)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Geoid tend to Equilibrium<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Isostacy vs. Eustacy<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Energy balance in systems<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Humans use 40 of Earth Productivity<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">(wind, tides, geothermal heat)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">26% of Evapotranspiration<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Processing Rock, Cement, Placers, Diatomaceous, Earth<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Radioactive Power Plants<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Power - Rate of doing work<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">(Energy overtime ) = kwh or horse power<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Albedo refers to sunlight reflected from a surface<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">30 reflected<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Absorbed<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Evaporated<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">S R = 3000, Energy source on earth<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Heat, gravity, acceleration<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Extraneous Energy - meteor / Asteroid etc.)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Humans concentrate energy<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Solar Constant - Radiant Energy - Atmosphere - Greenhouse and Blanket Effect<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Terrestrial gradients - latitude -Season - Grid<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Altitude-3.0 vs. 5.5/1000<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Mt. Barrier & Deserts<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Diurnal Variation<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Blanket/ Greenhouse - Fog - Dew - Frost<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Hydrologic cycle<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Glacial Storage (180 - 250)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">(20,000 yago) 425-450 ft lower.<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">(Saltation, Suspension, & Solution)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Gravity & Tides vs. Equilibrium<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Coreolis Effect<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Geothermal heat flow - 1 degree/69 mi (20 - 30 km)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Heat release, volcanoes, geysers, hot springs<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Volcanism / Rock cycle<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Mountain Building - Thermal & density energy<FONT size="+1"> </P ></DIV ></DIV ></BODY> </HTML>
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rsadoo. (Aug 17, 2009). Geomorphology Weekly Notes 3-1.htm. Retrieved Nov 06, 2014, from UMass Boston OpenCourseware Web site: http://ocw.umb.edu/environmental-earth-and-ocean-sciences/eeos-302-geomorphology/Geomorphology%20Weekly%20Notes%203-1.htm.