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GGS-311_-_Lecture8(3)

Course: GGS 311, Fall 2011
School: George Mason
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& Accuracy Uncertainty Matt Rice GGS 311 - GMU Fall 2011 National Map Published by Accuracy USGS Standards http://egsc.usgs.gov/isb/pubs/factsheets/fs17199.html#US% 20National Horizontal accuracy For maps on publication National Map Published by Accuracy USGS Standards http://egsc.usgs.gov/isb/pubs/factsheets/fs17199.html#US% 20National Vertical accuracy Vertical accuracy, as...

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& Accuracy Uncertainty Matt Rice GGS 311 - GMU Fall 2011 National Map Published by Accuracy USGS Standards http://egsc.usgs.gov/isb/pubs/factsheets/fs17199.html#US% 20National Horizontal accuracy For maps on publication National Map Published by Accuracy USGS Standards http://egsc.usgs.gov/isb/pubs/factsheets/fs17199.html#US% 20National Vertical accuracy Vertical accuracy, as National Map Published by Accuracy USGS Standards http://egsc.usgs.gov/isb/pubs/factsheets/fs17199.html#US% 20National Conforming Maps: This map complies with Uncertainty & Accuracy Longley et al. Chp. 6 Definitions Conception, measurement and analysis Vagueness, ambiguity, and other problems Statistical models of uncertainty Error propagation Living with uncertainty Introduction Imperfect or uncertain reconciliation and GIS Tension between perfection/ideal and reality It is impossible to make a perfect representation of the world, so uncertainty about it is inevitable Sources of Uncertainty Measurement error: different observers, measuring instruments Specification error: omitted variables Ambiguity, vagueness and the quality of a GIS representation Uncertainty is a catch-all for incomplete representations or quality measures A conceptual view of uncertainty. The three filters, U1, U2, and U3, distort the way in which the complexity of the real world is conceived, represented, and analyzed in a cumulative way. U1: Conceptio n Spatial uncertainty & formulating an approach to a geographic problem: Natural geographic units? In many cases, there are no natural units of geographic analysis Analysis involving more than one variable makes the search for a natural unit more difficult U1: Conception: GIS units/zones & vagueness Vagueness Statistics & vagueness Cartography & vagueness visual communication of vague boundaries or labels Cognition & vagueness confidence intervals with boundaries or labels perception of vagueness, need to categorize data A local assemblage of oak trees or part of an oak woodlandon Ragged Boys Hill, in the New Forest, UK. The Ordnance Survey map of the area suggests that there are trees beyond the perimeter of the woodland area, while the tree symbology suggests that the woods are characterized by varying proportions of deciduous and coniferous trees. (Photo courtesy Jim Champion) U1: Conception: GIS & ambiguity Ambiguity Many linguistic terms used to convey geographic information are inherently ambiguous Geographic prepositions (across, over, in) & translation to other languages Labels for terrain features: mountain, hill, bluff, butte, plateau, abundance, alp, cliff, crag, dome, drift, elevation, eminence, glob, heap, height, hump, mass, mesa, mound, mount, palisade, peak, pike, pile, precipice, pyramid, range, ridge, shock, sierra, stack, ton, U1: Conception: GIS & ambiguity Ambiguity Direct vs. Indirect indicators Direct: clear correspondence with a mapped phenomenon Indirect: perceived surrogate link with the phenomenon of interest Ambiguity is introduced when imperfect indicators of phenomena are used instead of the phenomena themselves. Ambiguity: Classification schemes, definitions, & crossborder data conflation Fuzzy Approache s to In fuzzy set theory, it is possible to have partial Uembership in a set: m ncertaint y membership can vary, e.g. from 0 to 1 this adds a third option to classification: yes, no, and maybe Fuzzy approaches have been applied to the mapping of soils, vegetation cover, and A.X. Zhu, Soil Mapping Using GIS, Expert Knowledge, and Fuzzy Logic Scale & Geographi Identification of c Units homogeneous zones and spheres of influence lies at the heart of traditional regional geography as well as contemporary data analysis The regional geography of Russia Relationships typically grow stronger when based on larger geographic units (Source de Blij H.J. and Muller P.O. 2000 Geography: Realms, Regions and Concepts (9th ed) New York: Wiley, p. 113) U2: Measurement/ representation Representati onal models (raster/vector ) filter reality differently Uncertainty can be measured Statistical measures of uncertainty: nominal case How to measure the accuracy of nominal attributes? e.g., a vegetation cover map Field checked B C D E Total A 80 4 0 15 7 106 B 2 17 0 9 2 30 C 12 5 9 4 8 38 D 7 8 0 65 0 80 E 3 2 1 6 38 50 Total Recorded in database A 104 36 10 99 55 304 Example a of confusion matrix. A grand total of 304 parcels have been checked. The rows of the table correspond to the land use class of each parcel as recorded in the database, and the columns correspond to the class as recorded in the field. The numbers appearing on the principal diagonal of the table (from top left to bottom right) reflect correct classification. Confusion Matrix Statistics Percent correctly classified total of diagonal entries divided by the grand total, times 100 209/304*100 = 68.8% but chance (accidental correct classification) would give a score of better than 0 Kappa statistic normalized to range from 0 (chance) to 100 evaluates to 58.3% Sampling for the Confusion Matrix Examining every parcel may not be practical Rarer classes should be sampled more often in order to assess accuracy reliably sampling is often stratified by class An example of a vegetation cover map Methods for estimating the accuracy of classification Interval/Ratio Case Errors distort measurements by small amounts Accuracy refers to the amount of distortion from the true value Precision refers to the variation among repeated measurements and also to the amount of detail in the reporting of a measurement Higher precision, lower accuracy Higher accuracy, lower precision The term precision is often used to refer to the repeatability of measurements. In both diagrams six measurements have been taken of the same position, represented by the center of the circle. On the left, successive measurements have similar values (they are precise), but show a bias away from the correct value (they are inaccurate). On the right, precision is lower but accuracy is higher. Reporting Measurements The amount of detail in a reported measurement (e.g., output from a GIS) should reflect its accuracy 14.4m implies an accuracy of 0.1m 14m implies an accuracy of 1m Excess precision should be removed by rounding Measuring Accuracy Root Mean Square Error is the square root of the average squared error the primary measure of accuracy in map accuracy standards and GIS databases e.g., elevations in a digital elevation model might have an RMSE of 2m the abundances of errors of different magnitudes often closely follow a Gaussian or normal distribution The Gaussian or Normal distribution. The light blue area (between 61 standard deviation) encloses 68% of the area under the curve, so 68% of observations will fall between these limits. A Useful Rule of Thumb for Positional Accuracy Positional accuracy of features on a paper map is roughly 0.5mm on the map e.g., 0.5mm on a map at scale 1:24,000 gives a positional accuracy of 12m this is approximately the U.S. National Map Accuracy Standard and also allows for digitizing error, stretching of the paper, and other common sources of positional error A useful rule of thumb is that positions measured from maps are accurate to about 0.5 mm on the map. Multiplying this by the scale of the map gives the corresponding distance on the ground. Map scale 1:1250 Ground distance corresponding to 0.5 mm map distance 62.5 cm 1:2500 1.25 m 1:5000 2.5 m 1:10,000 5m 1:24,000 12 m 1:50,000 25 m 1:100,000 50 m 1:250,000 125 m 1:1,000,000 500 m 1:10,000,000 5 km U3: Analysis. Uncertainties in data lead to uncertainties in Error the results of analysis PAlmost every input to a ropagatio GIS is subject to error n and uncertainty In principle, every output should have confidence limits or some other expression of uncertainty Three realizations of a model simulating the effects of error on a digital elevation model Overlay of two street networks in Goleta, California Living with Uncertainty It is easy to see the importance of uncertainty in GIS but much more difficult to deal with it effectively but we may have no option, especially in disputes that are likely to involve litigation Some Basic Principles Uncertainty is inevitable in GIS Data obtained from others should never be taken as truth efforts should be made to determine quality Uncertainty information may be recorded in metadata Effects on GIS outputs are often much greater than expected there is an automatic tendency to regard outputs from a computer as the truth More Basic Principles Use as many sources of data as possible Be honest and informative in reporting results and cross-check them for accuracy add plenty of caveats and cautions Keep a lab notebook, document your work
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George Mason - GGS - 311
Web GIS / Future of GISDr. Matt RiceGeography and Geoinformation Science311Fall 2011Overview:Future of GISGIS software architectureDataLegal Issues and IPPrivacyPanoramic Map of EurekaCalifornia (l890 1910) availablethrough the Library of Con
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATION SCIENCE 311 INTRODUCTION TO GEOGRAPHIC INFORMATION SYSTEMS Instructor: Dr. Matt Rice Term: Fall 2011 Classroom: Innovation Hall, room 222 Classtime: (GGS 311003: CRN 75396), Tuesday 4:30pm
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATIONSCIENCE 311INTRODUCTION TO GEOGRAPHICINFORMATION SYSTEMSInstructor: Dr. Matt RiceFaculty Office: Research Building I, Room 242Faculty Office Hours: Wednesday, 11:00am-1:00pm or by appointmentEmail: rice@gmu.eduFaculty web
George Mason - GGS - 311
GEOGRAPHY & GEOINFORMATIONSCIENCE 311INTRODUCTION TO GEOGRAPHICINFORMATION SYSTEMSInstructor: Dr. Matt RiceFaculty Office: Research Building I, Room 242Faculty Office Hours: Wednesday, 11:00am-1:00pm or by appointmentEmail: rice@gmu.eduFaculty web
George Mason - GGS - 311
GIS Data CollectionLongley, chp. 9Dr. Matt RiceGeorge Mason UniversityFall 2011OverviewIntroductionPrimary data captureSecondary data captureData transferCapturing attribute dataManaging a data capture projectData CollectionOne of most expens
George Mason - GGS - 311
Data Collection TechniquesRasterVectorSecondaryDigitalremotesensingimagesGPSmeasurementsDigitalaerialphotographsPrimarySurveymeasurementsScannedmapsTopographicsurveysDEMsfrommaps ToponymydatasetsfromatlasesPrimary Data CaptureCapture sp
George Mason - GGS - 311
GGS 311 Introduction to GIS Dr. Matt Rice Midterm Exam Study Sheet Fall 2011 1) Read Chapters 1, 7, 5, 3, 9 completely and pay attention to the bold points they are probably going to appear on the exam, p
George Mason - GGS - 311
GGS 311: Introduction to Geographic InformationSystemsChapter 3: RepresentingGeographyDr. Matt RiceGeorge Mason UniversityFall 2011QuestionWhat coordinate system are theseunits likely associated with?621,161 m E3,349,894 m NUTM?PLSS / Townshi
George Mason - GEOL - 102
2/25/11Archean Eonand the Solar System87% of the Earths history is inthe Precambrian!A little background before weget to the Earthmore background All of the planets were formed around thesame time (~4.7bya). They are formed from the same materia
George Mason - GEOL - 102
ArcheanRemember Precambrian time includes 80% of theearth's history, from 4.5 byr - 700 myr. So for the first 500 myr there is nogeologic record. Original crust was thin and composed mainlyof komatite & basalt. Granites have formed from basalts fr
George Mason - GEOL - 102
Cenozoic EventsCenozoic periodEocene and ModernCenozoic Half of the present sea floor was formedsince the end of the Cretaceous! Atlantic and Indian rifting had increased.East CoastFlorida region Erosion is still dominant. Passive margins. Carb
George Mason - GEOL - 102
4/22/11Cenozoic LifeCenozoicEVIDENCE FOR CENOZOICCLIMATE CHANGE Remember in the Cretaceous, climateswere much warmer than today. Although the oceans and atmosphereare affected by the K/T boundary theclimate soon returned to its greenhousestate i
George Mason - GEOL - 102
2/4/11EVOLUTIONLife on EarthTypes of fossilization, againPermineralizationReplacementCarbonizationMolds/casts steinkern Amber Trace fossils Tracks, trails, and burrowsPermineralization Original pore spacesare permeated withgroundwater. Min
George Mason - GEOL - 102
Geologic Time ScalePERIODEPOCHHoloceneNeogeneTertiaryPliocenePaleogenePleistoceneOligoceneMioceneEocenePaleocene0.011.65.323.736.657.8Mesozoic66.4Cretaceous144Jurassic208Triassic245CarboniferousPermianPaleozoicPhanerozoicCen
George Mason - GEOL - 102
Historical GeologyFinal ReviewSpring 2011Current eventsExtinctionKnow 5 largest extinction eventsPermian and Cretaceous extinction eventsMesozoic Tectonics Chapter 13Breakup of PangeaKnow ages of rifting eventsPalisades & Newark formationsDinos
George Mason - GEOL - 102
GeologicTime Scaleagain!Time & GeologyTime v Rock DivisionsEonEraPeriodEpochAgeRock versus TimeEonothemErathemSystemSeriesStageEvolution of geologic time scaleSedgwick and Murchison1Lithology denesComposition of mineral grainsColorTe
George Mason - GEOL - 102
HISTORICAL GEOLOGYGEOLOGY 102, section 002Spring, 2011Instructor: Dr. Stacey Verardosverardo@gmu.edu, 703-993-1045Class hours: Tuesdays and Thursdays 1:30 -2:45pmOffice: David King Hall Room 3037Office Hour: Thursdays, 11am -noonClassroom: Enterpr
George Mason - GEOL - 102
Early ManPrimate groups Prosimmii Tree shrews, lemurs, tarsiers Often nocturnal Anthropoidea Monkeys, apes, humansProsimii & AnthropoideaEarliest primates -Prosimian The earliestrelatives of theprimates werefound in theMesozoic andare simila
George Mason - GEOL - 102
IntroductionTime scaleTime scaleTaxonomicclassicationThis is theversion thatyou will bequizzed on.kingdoms1Factors for fossilization Rapid burial is the best way for successfulfossilization. Most often occur in shallow water with highenergy
George Mason - GEOL - 102
1/18/11HISTORICALGEOLOGYGeology102SowhatisthedierencebetweenGEO101andGEO102? InthisclassyouwilllearnoftheoriginoftheearthandtheevoluJonoftheland,atmosphereandallofitslife. AndthisiswhereyoullneedtolearntheGeologicTimescale. Therewillbeaquizonito
George Mason - GEOL - 102
4/10/11Mesozoic LifeAfter Permian extinction Seas were dominated by an abundance ofmollusks, sea urchins, crustaceans and sh& reptiles. On land, synapsids were replaced byreptiles. crocodiles, turtles, snakes, lizards and dinosaursMesozoicevents
George Mason - GEOL - 102
Mesozoic tectonicsMesozoic era -55-250myrThe breakup of PangaeaRepresents a change tectonically fromcompressional mountain building in theeast and northern parts of the continentto compressional forces on the westernmargin.What was happening ? La
George Mason - GEOL - 102
Rodinia was rifting apartEarly PaleozoicCambrian-SilurianLaurentiaBalticaKazakhstaniaSiberiaChinaGondwana Iapetus Ocean openthen closedRODINIA to PANNOTIANorth America & EuropeCambrianto SilurianDomes and basins1Vendian to OrdovicianCrat
George Mason - GEOL - 102
Late Paleozoic TectonicsLate Paleozoic 410-250 million years ago. Divided into Devonian, Carboniferous,Permian. By the Permian Pangea was assembled. During this time Acadian & Caladonian orogenies Alleghenian & Hercynian orogeniesLatePaleozoicP
George Mason - GEOL - 102
Paleozoic LifeEarly life Fossil record increases with increase infossil hard parts. Vertebrates evolve. Animals move onto land. Vascular plants show up. Also largest mass extinction EVER.Precambrian-Cambrian Invertebrate phylaEarly Cambrian foss
George Mason - GEOL - 102
2/11/11Plate TectonicsJOIDES resolutionP-wavesEARTHQUAKE WAVES P-waves S-waves Surface waves/Long wavesS-waves Oscillate back and forth perpendicular to the directionof wave travel. Change shape of rock. Only in solids. Cause strong movement
George Mason - GEOL - 102
PLEISTOCENE EPOCH1.7myr7 kyr agoExtent of ice during LGMevidenceAn Alps region glaciated valley In 1836 Louis Agassiz, apaleontologist, began to believe thatthe glaciers in the Alps were oncemuch more extensive than today.Glaciated EuropeChanges
George Mason - GEOL - 102
3/3/11Proterozoic2.5bya-540myaProterozoic compared to Archean. Proterozoic has a more modern type ofplate tectonics, sedimentation, and climate. First major Wilson cycle. First large ice age most of Earth cooled. Most BIFs. 42% of Earths history!
George Mason - GEOL - 102
Rocks & MineralsCriteria to be a mineral Occurs naturally as an inorganic solid. Has a specic internal structure. Has a specic chemical composition can exchange occasionally. Has specic physical properties. Minerals can be composed of one element
George Mason - GEOL - 102
Sedimentary ArchivesWhat determines which type ofsedimentary rock forms indifferent environs?Sedimentary EnvironmentsTectonic settingType of rock being weatheredType of transportClimateAmount of pressure & temperatureTimeSedimentary Environment
George Mason - GEOL - 102
Review Sheet for Historical GeologyExam OneSpring 2011Know the TIME SCALEKnow current eventsScience of Historical GeologyChapter 1Scientific MethodUniformitarianismThe 6 KingdomsTaxonomic ClassifiicationsTypes of FossilizationPermineralization
George Mason - GEOL - 102
Review Sheet for Historical GeologyExam TwoCURRENT EVENTSArchean and the Solar System -chapter 8Archean most of Earths History4.6 bya to 700 mya80% of Earths historySolar Nebular HypothesisKnow the planets!Terrestrial & GaseousMeteorites, Astero
George Mason - GEOL - 302
American Mineralogist, Volume 93, pages 16931720, 2008Review PaPeRMineral evolutionRobeRt M. Hazen,1,* DoMinic PaPineau,1 wouteR bleekeR,2 RobeRt t. Downs,3JoHn M. FeRRy,4 tiMotHy J. Mccoy,5 DiMitRi a. sveRJensky,4 anD Hexiong yang3Geophysical Labora
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Thevesoilformingfactors AllinteracttoformthedierenttypesofsoilThevesoilformingfactors Parentalmaterial Canberock Bedrock Residualsoils Transportedmaterialnotinplace TransportedsoilsThevesoilformingfactors LimestonesandstonebasaltThevesoilform
George Mason - GEOL - 306
CATION EXCHANGECAPACITYCLAY MINERALSAnd clay sized fractionThe very very smallveryKaolinite a clay mineral stacks ofhexagonalsheets shownhere are acharacteristicof many clayminerals. Bar is 50m1/1,000,000 m 1/1000 mmhttp:/www.reading.ac.uk
George Mason - GEOL - 306
soilorganicsSpodosolMyakka.TheOcialStateSoilofFloridaAEBhCarbon(cyclelater) dominantlyaddingCtothesoil soweretalkingmoreabouttheupperhorizonAofthesoildominantly.SOMsoilorganicmaFer OrganicmaFerisessenGaltoproducGvesoils improvesphysicala
George Mason - GEOL - 306
MacronutrientsNitrogenxingnodulesh4p:/blog.lib.umn.edu/denis036/thisweekinevoluAon/2007/08/cooperaAon_gets_complex_1.htmlESSENTIALELEMENTS Wearelearningthatsoilsareverycomplexmedium manyreacAonsoccurring thesystemasawholeinaconstantstateofux.Add
George Mason - GEOL - 306
Soil in the newsSome bad- But also some good thingsThe future rests on the soilbeneath our feet.http:/s.ngm.com/2008/09/soil/img/soil-615.jpgPopulation factsPopulationPopulation The world's population will reach 7billion people late this year, a
George Mason - GEOL - 306
SOILORGANICMATTERSOMPeatIsleofLewis,ScotlandSOM EspeciallyinOandA Nutrients Importantfor Supportmicroandmacroorganisms CEC TheyarepartofSOM Holdingwater Tilth. FormaGonofpedsstructure MostofthisnextweekCarboncycle Wewillcoverthisnextweek
George Mason - GEOL - 306
AGoodrichsoilneeds Soil acomplex,breathingen8ty Soil Plants chemistry9macronutrients Neededforplantstogrow C,H,O,N Crucial96%ofaplant K,Ca,Mg,P(phosphorus)S(sulfur)7micoelements Fe,Cl,Mn(Manganese),B(Boron),Cu,Mo(Molybdenum),Zn Lessthan0.010
George Mason - GEOL - 306
SoilPhysicalproper/es.SoilsamplingSoilsampling EarthDay2007 Sunnyside therepresenta5vesoilfortheDistrictofColumbia U.S.Na5onalArboretum.SoilsamplingSoil TextureSoil Texture = %Sand, Silt & Clay in a soil. Soil texture is the single most impor
George Mason - GEOL - 306
GEOLOGY306SOILSCIENCESPRING2011http:/mason.gmu.edu/~jnord/geol306/PREREQUISITE GEOL 101 and CHEM 103 or 211CLASS MEETS Monday 4:30 p.m. to 7:10 p.m. - Enterprise Hall 276Dr. Julia Nord, 3055 David King HallINSTRUCTOREmail Address - jnord@gmu.eduOF
George Mason - GEOL - 306
Soil Taxonomy- more detailsPurpose of Soil Taxonomy:1. Organize knowledge about soils2. Understand relationships among different soils3. Establish groups or classes for practical purposes.a. predicting behaviorb. identifying best usesc. estimating
George Mason - GEOL - 306
Soil solution- Not pure waterWater striderHydrological cycle water in living thingsImportance to plants Maintain turgidity Carry dissolved nutrients Required for Ps Lost in transpiration to cool plant and keep nutrients moving upImportance to p
George Mason - GEOL - 306
ROCKCYCLEIGNEOUSROCKGraniteh*p:/web.uct.ac.za/depts/geolsci/dlr/rocks/gran9.jpg VIOOLSDRIFBATHOLITHSAA1900Ma ADAMELLITE(TwoFeldsparGranite):Orthoclase(phenocrysHc)PlagioclaseQuartzBioHteMagneHteROCK asolidaggregateofoneormoremineralsormineralli
George Mason - GEOL - 306
SEDIMENTARYROCKSWhiteClisofDover(chalk)h5p:/cache.eb.com/eb/image?id=74594&rendTypeId=4RockcycleWEATHERING producessolidparKcles (primaryandsecondary) +ionsinsoluKonTRANSPORTATION movessolidparKcles (primaryandsecondary) +ionsinsoluKonDEPOS
George Mason - GEOL - 306
TwelveSoilordersPicturesfromNRCSNaturalResourcesConserva8onServiceh:p:/soils.usda.gov/technical/classica8on/orders/En8solrecentSoilsthathaveli:leornoevidenceofdevelopmentofpedogenichorizons.Manyaresandyorveryshallow.MountainsetcIncep8solL.Incept
George Mason - GEOL - 306
ROCKCYCLEWEATHERING thephysicalbreakdown(disintegra5on)andchemicalaltera5on(decomposi5on)ofrocksatornearEarth'ssurface Slowbutconstant Plentyof5meSURFICIALorEXTERNALPROCESSES Aectsthetop150feetjust!WEATHERINGsceneryWEATHERINGscenery TheBrides
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