atmospheric windows

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Remote Sensing BIT MESRA,RANCHI preeti tiwari mgi/10004/16

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Page 1: Atmospheric windows

Remote SensingBIT MESRA,RANCHI

preeti tiwarimgi/10004/16

Page 2: Atmospheric windows

Outline

• Electromagnetic Radiation• Blackbody Radiation• Atmospheric Windows• Instrument Parameters• Remote Sensing Architectures

Page 3: Atmospheric windows

EM Radiation

• Photon wavelength, frequency and energy c

hE h = 6.626 x 10-34 J sec

Page 4: Atmospheric windows

EM Radiation• Communications• Microwaves: 1 mm to 1 m wavelength. The

microwaves are further divided into different frequency (wavelength) bands: (1 GHz = 109 Hz) – P band: 0.3 - 1 GHz (30 - 100 cm) – L band: 1 - 2 GHz (15 - 30 cm) – S band: 2 - 4 GHz (7.5 - 15 cm) – C band: 4 - 8 GHz (3.8 - 7.5 cm) – X band: 8 - 12.5 GHz (2.4 - 3.8 cm) – Ku band: 12.5 - 18 GHz (1.7 - 2.4 cm) – K band: 18 - 26.5 GHz (1.1 - 1.7 cm) – Ka band: 26.5 - 40 GHz (0.75 - 1.1 cm) – V band: 50 – 75 GHz– W band: 75 – 111 GHz

Page 5: Atmospheric windows

EM Radiation

• Heat energy is the KE of random motion of the particles in matter

• Temperature is the measure of heat energy concentrated in a substance

• Random motion results in COLLISIONS• COLLISIONS cause changes in the

internal energy of the molecules• Internal energy modes relax to ground

state by giving off photons (EM Radiation)

Page 6: Atmospheric windows

Blackbody Radiation• An ideal thermal emitter

– Transforms heat energy into radiant energy at the maximum rate allowed (Thermodynamics)

– Any real material at the same temperature can not emit at a rate in excess of a blackbody

• An ideal thermal absorber

• Planck’s formula1

51 1

2

T

c

ecM C1 = 3.74 x 10-16 Wm2 = 2hc2

C2 = 1.44 x 10-2 mK = hc/k

Page 7: Atmospheric windows

Blackbody Radiation• Wien’s

Displacement Law– Defines

wavelength in a blackbody at which the maximum energy is emitted

TmKx

m

310898.2

Page 8: Atmospheric windows

Blackbody Radiation

• Stefan-Boltzmann Law– Relates the power emitted

by a body to that body’s temperature

44ambsfc TTq

= 5.669 x 10-8 Wm-2K-4

Page 9: Atmospheric windows

Other Than Blackbody Radiation

• Emissivity– Ratio of the spectral

energy radiated by a material to that of a blackbody at the same temperature

– Can depend on• Wavelength• Temperature• Phase (solid/liquid)

44ambsfc TTq

Page 11: Atmospheric windows

Atmospheric Windows

Page 13: Atmospheric windows

Atmospheric WindowM13 ObservationsRotational Transitions in CO

Page 14: Atmospheric windows

Window Transmission

Glass Quartz

Sapphire

Page 15: Atmospheric windows

Instrument ParametersTelescopes: Microwave, Radio, IR, Vis, UV, XRay, Gamma Ray

Page 16: Atmospheric windows

Instrument Parameters

ionMagnificatRr

hf

g

d

f – focal lengthh – altituderd – radius of detector arrayRg – ½ Swath Width

Page 17: Atmospheric windows

Instrument Parameters• Focal Length

Refractive System Reflective System

Page 18: Atmospheric windows

Instrument Parameters

• F-Stop or F-Number

DfF #

D - Aperture

Page 19: Atmospheric windows

Instrument Parameters

• A telescope's spatial (or angular) resolution refers to how well it can distinguish between two objects in space which are separated by a small angular distance.

• The closer two objects can be while still seen as two separate objects, the higher the spatial resolution of the telescope.

• The spatial resolution of a telescope affects how well details can be seen in an image. – A telescope with higher spatial resolution

creates clearer and more detailed images.

Page 20: Atmospheric windows

Instrument Parameters• Diffraction Limited

Resolution– Rayleigh diffraction

criteria– Angular distance from

maximum brightness at the center of the image to the first dark interference ring Dr

22.1

DhhX r 44.22

h can be replaced by slantrange for off Nadir obs.

Page 21: Atmospheric windows

Instrument Parameters

Aberration

Coma

Stigmatism

Page 22: Atmospheric windows

Instrument Parameters

Page 23: Atmospheric windows

Instrument Parameters

Page 24: Atmospheric windows

Instrument Parameters

• Silicon Imager Spectral Response

Page 25: Atmospheric windows

Instrument Parameters

• IR Detectors

Page 26: Atmospheric windows
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Remote Sensing Architectures

Global Ocean Temperatures

Page 28: Atmospheric windows

Remote Sensing Architectures

Mie scattering (small particles)Rayleigh Scattering (large particles)

PassiveActive

Page 29: Atmospheric windows

Remote Sensing Architectures

Cosmic Background Explorer

SPOT Mars Reconnaissance Orbiter

What is the driver for the remote sensing architecture?

Page 30: Atmospheric windows

Remote Sensing Architectures

Landsat 7•a panchromatic band with 15m spatial resolution •on-board, full aperture, 5% absolute radiometric calibration •a thermal IR channel with 60m spatial resolution •an on-board data recorder

Page 31: Atmospheric windows

Remote Sensing Architectures

Chicago

Baghdad

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Remote Sensing Architectures

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Remote Sensing Architecture

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Remote Sensing Architectures

Page 35: Atmospheric windows

Diffuse – Rough Surface Specular – Smooth Surface

Maxwell Model

Page 36: Atmospheric windows

Remote Sensing Architectures

Page 37: Atmospheric windows

Remote Sensing Architectures

• Space Radar– Mauna Loa Volcano

• Rift Zones (Orange)• Smooth Lava Flows (Red)

– Pahoehoe Flows

• Rough Lava Flows (Yellow/White)

– A’a Flows

– Obtained by sensing different Radar bands

Page 38: Atmospheric windows

Space Radar Systems

Page 39: Atmospheric windows

Remote Sensing Architectures

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Remote Sensing Architectures

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Remote Sensing Architectures

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Remote Sensing Architectures

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Remote Sensing Architectures

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Remote Sensing Architectures

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Remote Sensing Architectures• LIDAR

– Light Detection and Ranging

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Remote Sensing Architectures

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Remote Sensing Architectures

• Pushbroom Sensor

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