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Lecture 3

Geography 2320A/B Lecture 3: Lecture 3 Compiled notes pictures
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Department
Geography
Course
Geography 2320A/B
Professor
Gabor Sass
Semester
Fall

Description
One Class Friday s What is documenting understanding the spatial pattern B to the depths of the oceans and high in atmosphere and still And Antarctica found huge Lakes deep under (heat melting the ice) they are lockina forice now species thaf can travel distances migraton (otrds factors Influencing Biogeographic patterns The Geo non- random van Terrestrial Rain 50cm tor some trees Soils topography can shape where soils are. 8ocm on ses of Botas Respond to gradients fundamental Biogeograp (3) Interach on s among species Influence among "ecosystem engineers fluence o such a humans) Temporal dynamic o gographic template ne Class ne Class The Geographic Templat Why d o the tropics have other regions on Earth no adverse weather condihons lots of sunlight precipitation Trees on mountains stop growing at a certain elevation temperature Cyou can Teczina Cnats Two Great Engines Earth moves continents aroun pacts Sun 30% of E co bsorbed b as LW radiati Si lo ab d photo synthesis tant or distrib of species the poles Forests 20% albed. of Incidence ht dispers over Earth (0, equator more Sun higher Surtace. get to the poles. ne Class One Class Friday s What is documenting understanding the spatial pattern B to the depths of the oceans and high in atmosphere and still And Antarctica found huge Lakes deep under (heat melting the ice) they are lockina forice now species thaf can travel distances migraton (otrds factors Influencing Biogeographic patterns The Geo non- random van Terrestrial Rain 50cm tor some trees Soils topography can shape where soils are. 8ocm on ses of Botas Respond to gradients fundamental Biogeograp (3) Interach on s among species Influence among "ecosystem engineers fluence o such a humans) Temporal dynamic o gographic template ne Class ne Class The Geographic Templat Why d o the tropics have other regions on Earth no adverse weather condihons lots of sunlight precipitation Trees on mountains stop growing at a certain elevation temperature Cyou can Teczina Cnats Two Great Engines Earth moves continents aroun pacts Sun 30% of E co bsorbed b as LW radiati Si lo ab d photo synthesis tant or distrib of species the poles Forests 20% albed. of Incidence ht dispers over Earth (0, equator more Sun higher Surtace. get to the poles. ne ClassOne Class d change. Annual E Balance hea transes through convection (wind ocean eam Warm around th inox (both hemispheres have sunlight) solstices Cone hem. has more aunligh (Hadley Ferrel Polar cell we oft winds at certain togations (in N.Hem hit versa in the S. Hem) ountain s on Temp.: Efects of M 4 incr. elevation s decr. temp. lav. o.Lo c/10Dm or Effects of Water Bodie s on Temp d Hoo relates to different SO C 0 W SP capacity x far fic heat have sways. fom bodies of water will higher hure tempera ne Class neClass higher overhead Acct temp's. (H Cocier in higher lat. due to ocean currents tream brings extra warmth to uary Gulf Precipitation more precip. Where there is rising air ITCZ shift on a year y bases (South in Dec in th Summer It is evapora. Effects of Mountains on Recip L reaches dew condensahon point on the font side of a mountain on the back side of the mountains there is no deter the temp. d condensation point latent heat is released in the air when it condenses, Ch the a warm winds moves down the back side of a mountain *driest areas on Earth are 30 N 30 s. (Sahara ono Coasts aroun Great Lakes Cinland drier of precip from the Gulf summer we a lot. *deduce from a picture based o vee tah what part of the world you are in One Clas
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