Electromagnetic Waves
Physics!
All about Orbits
Choose the Technique
Remote Sensing Basics
100

Full range of wave frequencies that characterize solar radiation

Electromagnetic spectrum

100

What does this formula calculate? And what is each variable? (specify the units)

Frequency of a wave

c = speed of light 

lambda = wavelength

100

Reason geostationary satellites appear "stationary"

Satellites in geostationary orbit (GEO) fly above Earth’s equator, moving from west to east, exactly matching Earth’s rotation:

100

This instrument shoots laser pulses into the sky and measures how the light bounces back off tiny particles in the air to figure out wind speed and direction.

Doppler LIDAR ( Light Detection and Ranging)

Doppler lidar is defined as a remote sensing technology that utilizes the Doppler effect to measure atmospheric winds by analyzing the frequency change of laser-produced radiation scattered from moving atmospheric particles. It is particularly effective in clear air and can provide detailed observations of wind and turbulence in confined three-dimensional spaces.

100

Collects data on external stimuli and reflects sunlight

Passive sensor
200

Relationship between wavelength and frequency

The longer the wavelength the lower the frequency. 

200

E = hf says what?

where h = Plank's constant

E = energy of a quantum

Energy is directly proportional to the frequency

200

Revisit period is related to this type of resolution in remote sensing image

Temporal resolution

Length of time it takes for a satellite to return to acquire another image of the same location

200

Scientists may choose this type of orbit to compare like-for-like images over time to investigate how weather patterns emerge, help predict extreme weather events, and to accumulate data on long-term problems like deforestation or rising sea levels.

Sun-synchronous orbit (SSO)

200

2 potential sources of atmospheric interference that energy can encounter 

- Scattering (redirection) and or Absorption (conversion of energy into other forms of energy)

300

List the electromagnetic waves from longest wavelength to shortest wavelength. (clue: the waves are: x-rays, visible light, gamma, microwave, infrared, ultraviolet, microwave)t

Radio, Microwaves, Infrared rays, visible light, ultraviolet rays, x-rays, and gamma rays

300

In this formula for total radiant emittance (Watts per meter square)

What is T in this formula? This is the Stephen-Boltzmann law

T is the temperature of the emitting material

Put simply, higher the temperature higher the emittance

300

Type of orbit pictured here (in orange)

Sun-synchronous orbit 

Type of polar orbit 

Matching Earth’s rotation around the Sun

They pass over the same spot on Earth at the same local time every day

300
Choose this type of orbit for communication

Geostationary orbits

300

what is this showing?

Spectral Bandpasses for all Landsat Sensors - Spectral bands are specific ranges or intervals of wavelengths within the electromagnetic spectrum that sensors are designed to detect and measure.


400

What is the frequency of the visible spectrum in order (specify the units)

0.4 to 0.7 micrometers

 or 400 nm to 700 nm

blue 450-485 nm

green 500-565 nm

red 625-750 nm

400

Wien's displacement has this to say about temperature and wavelength

As the amount of energy increases with temperature, the wavelength of maximum (peak) emission become shorter.

400

ISS is a LEO - am I talking about the star sign of the International Space Station?

No - the International Space Station is a lower earth orbit

400

Not the mythological nymph from the Odyssey, this satellite uses LIDAR to "see" through thin clouids, detect aersols and provide vertical slices of the atmosphere 

CALIPSO -  Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation used laser pulses to create detailed vertical profiles of Earth's atmosphere

400

This reflectance curve says this about the reflectance of vegetation

Vegetation reflects highest in the near infrared band (not in the visible band)

500

The energy carried by an electromagnetic wave

Radiant energy

500

As shown in this figur, the Sun's temperature of 6000 degrees Kelvin causes its blackbody radiation to peak in this portion of the spectrum explainig why passive remote sensing relies heavily on reflected solar energy during daytime.


What is the visible region (or visible light)


The figure demonstrates this principle from Wien's displacement law: as temperature increases from 300 K (Earth) to 6000 K (Sun), the peak emission wavelength does this, shifting from the infrared into the visible spectrum.

Figure also illustrates that the Sun at 6000 K has a spectral radiant emittance peak that is many orders of magnitude higher than Earth at 300 K,

500

This orbital parameter, ranging from 0 for a perfect circle to values approaching 1 for highly elongated paths, is kept near zero for MEO navigation satellites to ensure consistent coverage and signal strength.

What is eccentricity?

500

Use this sensor  to measure sea level rise (Jason-2 had Poseidon-3 for this)

Radar Altimeter -

Radar altimetry is defined as a remote sensing technique that measures the height of the ocean surface and other topographic features using radar signals, enabling the study of surface waves and the relationship between water level and subsurface pressure.

The Poseidon-3 altimeter emits pulses at two frequencies 13.6 and 5.3 GHz to measure the distance from the satellite to the surface

500

NDVI (normalized difference vegetation index) index is calculated in this way using this figure 

normalized values of the

Landsat Normalized Difference Vegetation Index (NDVI) is used to quantify vegetation greenness and is useful in understanding vegetation density and assessing changes in plant health.

NDVI is used to quantify vegetation greenness and is useful in understanding vegetation density and assessing changes in plant health. NDVI is calculated as a ratio between the red (R) and near infrared (NIR) values in traditional fashion: 

(NIR - R) / (NIR + R)

In Landsat 4-7, NDVI = (Band 4 – Band 3) / (Band 4 + Band 3).

In Landsat 8-9, NDVI = (Band 5 – Band 4) / (Band 5 + Band 4).

NDVI is delivered as a single band product, specified as shown in the table below.

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