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<style type="text/css"> <!-- .style1 {font-weight: bold} --> </style> <B>Part II Climates: </strong></U></P > <P align="justify" ><FONT size="+1"></B>Climate is the average of weather over a twenty to thirty year period,<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">-1 .Temperature: by month/year and threshold temperature<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">-2.Rainfall: by month/year and threshold amounts<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">-3 .Soil-environment/temperature/moisture<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">-4.Vegitation: xerophyte (cactus)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">-5.Economic component: mining farming<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Block soil is rich, warms up and cools down fast<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">In the South we have a red soil. Rain is mixing with Iron to create rust FE203.<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Yellow color means baked soil (Yellow River/Yellow Sea)<FONT size="+1"> <br> <br> Climate Classification Coded within Last 100 years developed by Vladimir Koppen<br> <br> <FONT size="+1"><B>A</B><I> Temperature Based Tropical Climates</I><FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Average temperature is above 64<FONT size="+1">°<FONT size="+1"> F (18<FONT size="+1">° <FONT size="+1">C). Notice that tropical climates have no third<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">letter: there is little or no seasonally in temperature, so no third letter is needed. The<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">seasonality in precipitation is taken care of by the second letter.<FONT size="+1"> </P ><P align="justify" ><FONT size="+1"><B><span class="style1"><I>Af</I><FONT size="+1"></span> </P > <P align="justify" ><U><FONT size="+1">Tropical Rainforest</U></B>. Second letter f, no dry season, wet all year. with at least 2.4" (6<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">cm) of rainfall each and every month Selva vegetation covers the area.<FONT size="+1"> <!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="Am" > <META name="dc.date" content="2009-08-07T11:26:32-04:00" > <META name="dc.date.modified" content="2009-08-07T11:26:36-04:00" > <META name="generator" content="Adobe Acrobat Exchange-Pro 7.256" > </HEAD> <BODY bgcolor=white text=black link=blue vlink=purple alink=fushia > <DIV class="Sect" ><DIV ><P align="justify" ><U><FONT size="+1" color="#000000"><B>Am </U></P ><P align="justify" ><U>Monsoon.</U></B> Second letter m, seasonally high rainfall, short but distinct dry season with </P ><P align="justify" >less than 2.4" (6 cm) of rainfall in the driest month. Selva is found here also. </P ><P align="justify" ><U><B>Aw </U></P ><P align="justify" ><U>Savanna.</U></B> Second letter <B>w</B>, dry season in winter with at least one month less than 2.4" (6 </P ><P align="justify" >cm) of rainfall. This can be of a parkland with isolated trees or primarily grassland. </P ><P align="justify" ><B>Dry Climates </P ><P align="justify" ><U>B</U></B> Precipitation Based Dry Climates </P ><P align="justify" ><U>Evapotranspiration</U> (evaporation plus transpiration from plants) equals or exceeds </P ><P align="justify" >precipitation. Because of this, there is no surplus water in the B climate areas, and no </P ><P align="justify" >permanent streams can form there. Streams crossing B climate areas are usually "exotic" </P ><P align="justify" >meaning that they originate in more humid areas. An example of this would be the Nile. </P ><P align="justify" >The B climate is by far the largest climate area. 7 or more of the precipitation falls in </P ><P align="justify" >the summer months; winter precipitation concentration (dry summer) 70 or more of </P ><P align="justify" >precipitation falls during the 6 winter months; neither summer nor winter precipitation </P ><P align="justify" >concentration: fits neither of the above conditions, more or less even precipitation. It is </P ><P align="justify" >important to note that most deserts are not sandy. They may have sandy areas in some </P ><P align="justify" >locations. </P ><P align="justify" ><U><B>Low latitude (hot) desert.</U></B> Second letter <B>W</B>, arid; third letter <B>h</B>, hot. Potential </P ><P align="justify" >Evapotranspiration is more than twice available precipitation. Mean annual temperature </P ><P align="justify" >is over 64° F (18° C).Life is quite sparse and adapted to low rain fall Egypt </P ><P align="justify" ><U><B>BWk </U></P ><P align="justify" ><U>Mid latitude (cool or cold) desert.</U></B> Second letter <B>W</B>, arid; third letter <B>k</B>, cold (from </P ><P align="justify" >German Kalt). Potential Evapotranspiration is more than twice available precipitation. </P ><P align="justify" >Mean annual temperature is less than 64° F (18° C).Afghanistan </P ><P align="justify" ><U><B>BSh </U></P ><P align="justify" ><U>Low latitude (hot) steppe</U></B>. Second letter <B>S</B>, semi arid; third letter <B>h</B>, hot. Potential </P ><P align="justify" >evapotranspiration is up to twice available precipitation. Mean annual temperature is over </P ><P align="justify" >64° F (18° C). This usually has a short grass and is not suitable for cattle grazing but can </P ><P align="justify" >do sheep or goats. </P ><P align="justify" ><U><B>BSk </U></P ><P align="justify" ><U>Mid latitude (cool or cold) steppe.</U></B> Second letter <B>S</B>, semi arid; third letter <B>k</B>, cold (from </P ><P align="justify" >German Kalt). Potential evapotranspiration is up to twice available precipitation. Mean </P ><P align="justify" >annual temperature is less than 64° F (18° C).This can be an area of dry cereal farming or cattle grazing. </P ><P align="justify" ><FONT color="#CC0000"><B> </P ><P align="justify" >Question?<FONT color="#000000"></B> Why do we find this environment in many western movie<FONT size="+1">s?<FONT size="+1"> </P ></DIV ><DIV ><P align="justify" ><FONT size="+1"><B>C</B> Temperature Based Humid Mesothermal </P ></DIV ></DIV ></BODY> </HTML> <!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="The coldest month is between 27° F and 64° F (-3° C to 18° C)" > <META name="dc.date" content="2009-08-07T11:33:59-04:00" > <META name="dc.date.modified" content="2009-08-07T11:34:02-04:00" > <META name="generator" content="Adobe Acrobat Exchange-Pro 7.256" > </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>The coldest month is between 27° F and 64° F (-3° C to 18° C). At least one month </P ><P align="justify" >averages above 50" F (10° C), so there are definite summer and winter seasons, although </P ><P align="justify" >mild. If snow falls, it does not linger long. Those with a as third letter are hot-summer, </P ><P align="justify" >with the warmest month over 72° F (22°C); those with b as third letter are warm summer, </P ><P align="justify" >with warmest month below 72° F (22° C); those with c as third letter are cool, short </P ><P align="justify" >summer, with less than 4 months over 50° F (10° C).These climates are usually located </P ><P align="justify" >proximal to coasts and may have great amounts of rainfall similar to monsoon locations. </P ><P align="justify" ><U><B>Cfa </U></P ><P align="justify" ><U>Humid subtropical.</U></B> Second letter <B>f</B>, no dry season. Mild, no dry season. Precipitation of </P ><P align="justify" >the driest month averages more than 1.2" (3 cm). It is possible to have snow and frost in </P ><P align="justify" >these locations but the growing season is usually long. </P ><P align="justify" ><U><B>Cfb, Cfc </U></P ><P align="justify" ><U>Marine west coast</U></B>. Second letter <B>f</B>, no dry season. Same as above, but cooler due to </P ><P align="justify" >position on continents with respect to prevailing westerlies. You may find fruit trees, </P ><P align="justify" >viticulture and bocage or maqui type of vegetation here. </P ><P align="justify" ><U><B>Cwa, Cwb </U></P ><P align="justify" ><U>Subtropical monsoon.</U></B> Second letter <B>w</B>, dry winter season. Dry winter (<B>w</B> designation) </P ><P align="justify" >with a wet season in the summer. 70 or more of the precipitation comes during the 6 </P ><P align="justify" >summer months. In the US, this is the location of the redwood forests. </P ><P align="justify" ><U><B>Csa, Csb </U></P ><P align="justify" ><U>Mediterranean.</U></B> Second letter s, dry summer season. Dry summer (s designation) with </P ><P align="justify" >driest summer month less than 1.2" (3 cm). 70 or more of the total precipitation comes </P ><P align="justify" >during the 6 winter months. Citrus trees and truck crops with irrigation are common in </P ><P align="justify" >these environments. You can see this type of climate in the Crimea. </P ><P align="justify" ><U><B>D</U></B> Temperature Based Humid Microthermal </P ><P align="justify" ><U><B>Snow climate.</U></B> The coldest month averages below 27° F (-3° C). The warmest month </P ><P align="justify" >averages above 50° F (10° C). Snow usually falls and stays for at least part of the year. </P ><P align="justify" >Third letter designations <B>a</B>, <B>b</B>, and <B>c</B> are the same as for <B>C</B> climates. <B>D</B> climates with a </P ><P align="justify" >third letter designation of <B>d</B> are very-cold winter climates, with the coldest month below - </P ><P align="justify" >36° F (-38° C).These climates are found at high latitudes in the northern hemisphere or in </P ><P align="justify" >interior continental locations. </P ><P align="justify" ><FONT color="#CC0000"><B>Question?<FONT color="#000000"></B> Why are these climates not found in the southern hemisphere? </P ><P align="justify" ><U><B>Dfa, Dfb, Dfc, Dfd </U></P ><P align="justify" ><U>Snow climate with wet winter, no dry season,</U></B> Third letter designations: a is hot </P ><P align="justify" >summer, <B>b</B> is warm summer, <B>c</B> is cool summer, <B>d</B> is cold winter (subarctic). </P ><P align="justify" ><U><B>Dwa Dwb Dwc Dwd </U></P ><P align="justify" ><U>Snow climate with dry winter.</U></B> Third letter designations: a is hot summer, b is warm </P ><P align="justify" >summer, <B>c</B> is cool summer, <B>d</B> is cold winter (subarctic). </P ></DIV ></DIV ></BODY> </HTML> <!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="Note" > <META name="dc.date" content="2009-08-07T11:37:37-04:00" > <META name="dc.date.modified" content="2009-08-07T11:37:40-04:00" > <META name="generator" content="Adobe Acrobat Exchange-Pro 7.256" > </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>Note. Many of the D climates resemble deserts but with low temperature comes short </P ><P align="justify" >growing seasons and a minimal need of water. </P ><P align="justify" >E Temperature Based Polar </P ><P align="justify" >Average temperature of the warmest month is below 50° F (10° C). Only two letters are </P ><P align="justify" >needed because these climates have no summer. They are routinely cold and usually the </P ><P align="justify" >precipitation comes in the form of snow. Vegetation is hardy and stunted and animals are adapted to the cold and snow . </P ></DIV ><DIV ><P align="justify" ><U><B>H </U></P ><P align="justify" ><U>TC,TT,TF and Paramos </U></P ><P align="justify" ></B><I>Elevation Based Mountain Climates</I><I> </I></P ><P align="justify" >This designation is for those areas in which climatic conditions change so quickly over a </P ><P align="justify" >short horizontal distance due to elevation changes. Mountain climates are variable over a </P ><P align="justify" >short distance, but they must fit into the surrounding general climate. In general, </P ><P align="justify" >mountain climates are colder and wetter with increased altitude, although there are some </P ><P align="justify" >exceptions to the wetter generality. (Sometimes shown as "G" climates on some maps.) </P ><P align="justify" >These have some of the oldest cultures associated with them and have specialized crops </P ><P align="justify" >and farming techniques also </P ><P align="justify" ><U><B>The Changing Climate</U></B> extra reading notes </P ><P align="justify" >-Average Atmospheric Values </P ><P align="justify" >-Variability of elements </P ><P align="justify" >-occurrence of extreme events </P ><P align="justify" >Exchange of energy and moisture within Atmosphere </P ><P align="justify" >-hydrosphere </P ><P align="justify" >-Biosphere </P ><P align="justify" >-Litho sphere </P ><P align="justify" >-cryo sphere </P ><P align="justify" >Climate has varied extensively through time </P ><P align="justify" >Human Activities effect environment </P ></DIV ><DIV ><P align="justify" ><U><B>ET </U></P ><P align="justify" ><U>Tundra</U></B>. The warmest average month is above 32° F (0° C) but less than 50° F (10° C). </P ><P align="justify" >Very short growing season. Permafrost is common to this environment. </P ><P align="justify" ><U><B>EF </U></P ><P align="justify" ><U>Ice cap.</U></B> Permanent snow and ice, average temperature of all months is below 32° F (0° </P ><P align="justify" >C). There is no growing season. Glacier may migrate during the summer months in both </P ><P align="justify" >north and south hemispheric locations. </P ><P align="justify" ><U><B>EM </U></P ><P align="justify" ><U>Island locations at high latitude. Very few locations. Cold and windy suitable for sheep. </U></P ></DIV ></DIV ></BODY> </HTML> <!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="Evidence used to detect change" > <META name="dc.date" content="2009-08-07T11:41:28-04:00" > <META name="dc.date.modified" content="2009-08-07T11:41:32-04:00" > <META name="generator" content="Adobe Acrobat Exchange-Pro 7.256" > </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>Evidence used to detect change </P ><P align="justify" >-Sea floor sediment </P ><P align="justify" >-Oxygen Isotope analysis </P ><P align="justify" >-glacial Ice </P ><P align="justify" >-old Soils </P ><P align="justify" >-tree rings </P ><P align="justify" >-documentation </P ><P align="justify" >Sea floor sediment contains remains of organisms that once lived at the surface. </P ><P align="justify" >-Surface and organisms changed and adapted with climate </P ><P align="justify" >-JOIDES Resolution collects cores from sea floor </P ><P align="justify" ><B>Oxygen Isotope analysis </P ><P align="justify" ></B>-precise measurement of ratio between common Oxygenl6 and heavier </P ><P align="justify" >uncommon </P ><P align="justify" >Oxygen 18 </P ><P align="justify" >-016 evaporates more readily from Oceans leaving greater amounts of) 18 in </P ><P align="justify" >ocean </P ><P align="justify" >Study of Buried soils Paleosols </P ><P align="justify" >Yearly growth of tree rings </P ><P align="justify" >Pollen in Sediment </P ></DIV ><DIV ><P align="justify" ><B><I>Natural Mechanisms of Climate Change </I></P ><P align="justify" ></B>1<B>.Plate Tectonics:</B> continental plates shining </P ><P align="justify" >2.<B>Volcanic Activity:</B> reducing solar radiation, changing landscape </P ><P align="justify" >3.<B>Solar Variability:</B> variations in output, sunspot surplus can cause global temperature to </P ><P align="justify" >rise </P ><P align="justify" >4.<B>Variations in Earth's orbit:</B> Milonkovitch cycle:axial tilt change(obliquity), </P ><P align="justify" >wobble(precession) shape oforbit(eccentricity) </P ><P align="justify" ><B>Human Impact on global Climate </P ><P align="justify" ></B>-use of fire </P ><P align="justify" >-overgrazing </P ><P align="justify" >-modifying surface albedo </P ><P align="justify" >-Addition of C02 in the atmosphere </P ><P align="justify" >-Addition of trace gasses </P ><P align="justify" >-Methane </P ><P align="justify" >-Nitrous Oxide </P ><P align="justify" >-CFC's </P ><P align="justify" >-These all lead to global warming trends </P ><P align="justify" >-Sea level rise </P ><P align="justify" >-Melting of glaciers </P ><P align="justify" >-increase in ocean volume due to temperature expansion of water </P ><P align="justify" >molecules </P ><P align="justify" >-shoreline erosion </P ></DIV ></DIV ></BODY> </HTML> <!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="Climate of Urban areas/Cities different from surrounding or non urban areas" > <META name="dc.date" content="2009-08-07T11:44:18-04:00" > <META name="dc.date.modified" content="2009-08-07T11:44:21-04:00" > <META name="generator" content="Adobe Acrobat Exchange-Pro 7.256" > </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>Climate of Urban areas/Cities different from surrounding or non urban areas </P ><P align="justify" >-Cloudier </P ><P align="justify" >-Foggier </P ><P align="justify" >-Warmer </P ><P align="justify" >-Wetter </P ><P align="justify" ><B>Urban Heat Island </P ><P align="justify" ></B>-Highest temperatures are seen where building density is highest, and industry is </P ><P align="justify" >present </P ><P align="justify" ><B><I>end of reading notes </I></P ><P align="justify" ></B>Eastern Massachusetts is a <B>Cfa</B> climate </P ><P align="justify" >Western Ma is like a <B>D</B> climate </P ><P align="justify" >Characteristics of Climate Types </P ><P align="justify" ><B>A </P ><P align="justify" ></B>every month has temp over <B>64</B> degrees F </P ><P align="justify" >Selva </P ><P align="justify" ><B>Tropical evergreen </B>dense hardwoods </P ><P align="justify" >Vines connecting to ground <B>liana</B> </P ><P align="justify" >Bottom story is <B>fern</B> </P ><P align="justify" >bananas, cacao, nuts, fruits rubber </P ><P align="justify" >plantations </P ><P align="justify" >Soil is Tierra (red) </P ><P align="justify" ><B>B </P ><P align="justify" >Steppes, Desert </P ><P align="justify" ></B>Mining, raw materials </P ><P align="justify" >indigenous peoples, nomad </P ><P align="justify" >Camels, sheep, goat </P ><P align="justify" >short grasses </P ><P align="justify" ><B>C </P ><P align="justify" ></B>Influenced by the sea </P ><P align="justify" >one or months above 50 degrees F </P ><P align="justify" ><B>Deciduous</B> leaf trees </P ><P align="justify" >Pedocal Soil, Podzol soil </P ><P align="justify" >Fruit trees ex.) pecan, apples, walnuts, peaches </P ><P align="justify" ><B>D </P ><P align="justify" ></B>One or month above 50 degrees F and one or month below 32 degrees F </P ><P align="justify" ><B>Evergreen</B> and <B>Taiga trees</B> </P ><P align="justify" >Coniferous forest </P ><P align="justify" >paper pulp </P ><P align="justify" ><B>E </P ><P align="justify" ></B>Average Temp of warmest month is less than 50 degrees F </P ></DIV ></DIV ></BODY> </HTML> <!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="Ice cap" > <META name="dc.date" content="2009-08-07T11:45:20-04:00" > <META name="dc.date.modified" content="2009-08-07T11:45:23-04:00" > <META name="generator" content="Adobe Acrobat Exchange-Pro 7.256" > </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>Ice cap. Frozen tundra, <B>permafrost.<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">H<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Paramous</B> is highest elevation: devoid of vegetation<FONT size="+1"> </P ><P align="justify" ><FONT size="+1"><B>Tierra Fria<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Tierra Templada<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Tierra Caliente Lowest elevation<FONT size="+1"> </P ></DIV ></DIV ></BODY> </HTML>
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