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49 Cards in this Set

  • Front
  • Back

Digital images

A numeric representation of 2D raster images

Color or (CIR) images have at least three bands:

Blue


Green


Red

Converting analog images to digital

Film images ---> computer

Linear array CCD

scanning an image - scans one line of pixels at a time


image ---> computer file


light moves across image - light is reflected to sensor - sensor records high number for light areas, low number for dark areas

analog frame camera

image represents an area on the ground "frame"



digital frame camera area array

digital


color images require 3 sets of sensors (red, green, blue)


each sensor records 1 pixel


image represents an area on the ground - acquired at one time

scanning mirror bases scanners

scans across a line one pixel at a time


depends on motion of platform to advance to next line - whisk broom


MSS - LANDSAT - multi-spectral scanner 1972

thematic mapper



TM - Landsat


bidirectional scanning



push broom linear array

has a line of detectors- acquires a line at a time


motion of platform to move the scanner along - no moving parts on instrument


operational land imager (OLI) --> landsat 8

imaging spectrometers

collects many different wavelength bands ---> 200

spectral resolution

enough info in appropriate wavelengths?



spatial resolution

how are the features you want to identify relative to the resolution of the imagery? (pixel size)



temporal resolution

how often does the sensor record information in your area?

radiometric resolution

sensitivity of sensor to differences in signal strength - 8-bit (256 different steps)

aerial photo single frames

wide variety of purposes


many different agencies


historical imagery - mostly pre 1980s


many different scales - mostly B&W panchromatic, some true color, some CIR


scans of hard copies

NAPP

National Aerial Photography Program


began in 1987 - 5 year repeat, acquire imagery of whole US


cloud free


20,000+ a.g.l (above ground level) 6 in focal length ---> 1:40,000


flown N to S through east and west halves 7.5 min. topo quads - 60% end lap

USDA FSA imagery

farm service agency


aerial photography field office


film scans at $13/frame

georeferencing and rectification

-georeferencing - real world coordinates attached to images

orthophotos

an aerial photo processed to have the metric qualities of a map

processing

mosaicking


available tiled seamless

compression and file format

zip


gz


tiff or tif - full resolution imagery compression built in


jpg (jpeg or jfif)


jpeg


mrSID

digital imagery sources

Earth explorer


-orthophotos


NAIP


DOQ - digital orthophoto quadrangler


state, county, regionals


Ohio - OSIP



NAIP

National Agricultural Imagery program


3 year cycle


leaf-on imagery


NRCS - geospatial data gateway

leaf pigments

plant leaves have pigments in them that absorb light


plants take in carbon dioxide & water ---> transform those to energy (sugars) using the energy from light ---> absorb light


photosynthesis ---> chlorophyll




low absorbance in green wavelengths---> reflects green


pigments affect spectra in visible wavelengths - not much in IR wavelengths

leaf structure

the structure of the cells in the leaf control the amount of NIR light that is reflected


spongy mesophyll




internal scattering of NIR


- interfaces between cell wall & air


- not connected to leaf pigment

biomass

number of leaf layers affects the amount of NIR that's reflected

leaf moisture content

how much water is in the leaf?


Water absorbs energy in several parts of the middle IR


- water absorbs in the water absorption bands


-leaves reflect less light in IR when moist, more light when dry

color film

object reflects: blue green red infrared


blue green red ****

Color infrared film (CIR)

object reflects: blue green red infrared


**** blue green red

interpretation of vegetation features - types of plants

deciduous (broad leaf)


coniferous (needle leaf)


- deciduous trees reflect more NIR light than coniferous trees


shrubs


herbaceous plants - tend to reflect more in NIR than deciduous

temporal aspects

when (seasonally) plants will look like what on an image - i.e. leaf-on, leaf-off imagery, etc.



vegetation indices - simple ratio

NIR reflectance/red reflectance




- high numbers for vegetation


- lower numbers for other cover types



vegetation indices - normalized difference vegetation index (NDVI)

NIR - red/NIR + red




- high values in vegetation


lower values for other cover types

leaf - off imagery

acquired before leaves are on trees - often in April

leaf- on imagery

acquired during growing season - often july or august

three pathways associated with water

surface


water column


bottom

diffuse reflection


(water surface)

many different directions


rough surface



specular reflection


(water surface)

all reflected in one direction


smooth surface


(water tends to have a smooth surface at the scale of the wavelength of light)

reflection from water column

infrared wavelengths --->


water absorbs a lot of incident energy in the IR wavelengths


- middle IR especially


- near IR as well


- water does not reflect much IR light

water reflectance

water is not a good reflector at any wavelength


reflects more in shorter wavelengths than longer wavelengths in visible


turbid water reflects more than clear water - turbid water does reflect in NIR




- high suspended solids peak in red wave length


- clear water has peak in blue or green

reflection from bottom of water body

for clear water bodies, relatively shallow water will produce reflection from the bottom


in blue wavelengths can get water depth penetration of 5 - 10 m in clear water

interpreting water features

detection of water bodies


-best done in IR wavelengths


-water doesn't reflect


-other things do

spectral characteristics of soil

most soil curves show increasing reflectance with wavelength


factors


-texture


-moisture content


-organic matter content


-iron oxide content

soil texture

relative percentage of sand, silt, clay particles in soil


particles of different sizes


sand: largest


silt: medium


clay: very small


as particle size decreases, spectral reflectance increases

moisture content

how much water is there between soil particles?


higher moisture content --> lower reflectance


shape of curves shows water absorption bands for wetter soils

organic matter

amount of plant derived material mixed in the soil


high organic matter soils are dark


low organic matter soils are light

iron oxides

soils high in iron oxides are reddish in color

spectral characteristics: concrete & asphalt



concrete - consistently bright


asphalt - relatively dark, but can vary

land use/ land cover classification

land use - residential, commercial, industrial


land cover - the material that is covering the land - grass, trees, water, asphalt, bare soil...




urban categories:


-residential


-commercial, service, institutional


-industrial


-transportation, utilities


-open space