Remote Sensing - Vocabulary Flashcards

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Vocabulary flashcards covering key Remote Sensing concepts, satellites, instruments, atmospheric and climate topics, image interpretation, and fundamental physics relevant to the subject.

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76 Terms

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Remote Sensing

The science of acquiring data about an area or object without being in physical contact, often using satellites or aircraft to observe Earth systems.

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Active Sensing

Remote sensing that emits energy (e.g., radar, lidar) and measures the backscatter or reflection from targets.

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Passive Sensing

Remote sensing that measures naturally occurring radiation (e.g., sunlight reflected from surfaces) without emitting its own energy.

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RADAR

Radio Detection and Ranging; an active sensing system using microwaves to locate objects and measure elevation.

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LIDAR

Light Detection and Ranging; uses laser pulses to measure distances and create high-resolution 3D surface maps.

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TM (Thematic Mapper)

Landsat sensor with seven spectral bands used for Earth observation and land mapping.

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ETM+ (Enhanced Thematic Mapper Plus)

Landsat 7 sensor, an eight-band upgrade to TM with improved performance.

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MSS (Multispectral Scanner)

An earlier Landsat sensor that collected data in multiple spectral bands.

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ALI (Advanced Land Imager)

A Landsat-era instrument designed for high-resolution multispectral imagery.

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MODIS

Moderate-resolution Imaging Spectroradiometer; on Terra and Aqua; measures clouds, land, oceans, and atmospheric properties.

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CERES

Clouds and the Earth's Radiant Energy System; measures broadband radiative energy flux on Terra and Aqua.

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SeaWiFS

Sea-viewing Wide Field-of-View Sensor; monitors ocean color and radiative energy flux.

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AVHRR

Advanced Very High Resolution Radiometer; NOAA sensor for earth observation across multiple spectral bands.

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AVIRIS

Airborne Visible/Infrared Imaging Spectrometer; airborne hyperspectral instrument.

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CZCS

Coastal Zone Color Scanner; early satellite sensor for ocean color and chlorophyll.

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MISR

Multi-angle Imaging Spectro Radiometer; measures Earth's surface and atmosphere from multiple viewing angles.

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MSR

Microwave Scanning Radiometer; measures microwave emissions from Earth's surface.

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RAR

Real Aperture Radar; type of radar system used for imaging.

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Landsat (Landsat 7, 8, 9)

Series of Landsat satellites; currently Landsat 7, 8, and 9 in operation with multiple spectral bands.

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Terra

EOS satellite part of the Earth Observing System; focuses on atmosphere, land, and water.

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Aqua

EOS satellite focused on the Earth's water cycle (precipitation, evaporation, etc.).

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Aura

EOS satellite studying ozone, air quality, and climate.

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OCO-2

Orbiting Carbon Observatory 2; studies atmospheric carbon dioxide.

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GCOM-W1 (SHIZUKU)

JAXA satellite studying the water cycle.

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PARASOL

Radiative and microphysical properties of clouds and aerosols; moved to a lower orbit and deactivated in 2013.

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CloudSat

Radar satellite studying clouds and their properties.

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CALIPSO

Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation; studies clouds and aerosols.

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EOS Morning Constellation (EOS-AM)

Second EOS constellation named for its 10:30 AM equatorial crossing; includes EO-1.

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EOS-A-Train

A train of satellites in Sun-synchronous orbit; seven satellites planned/operating for coordinated observations.

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OCO (Orbiting Carbon Observatory)

Failed to achieve orbit; intended to study atmospheric CO2.

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Glory

NASA mission that failed to reach orbit while studying aerosols and climate.

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LEO

Low Earth Orbit; ~200–2,000 km altitude; high-resolution Earth observation, but limited ground coverage per pass.

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MEO

Medium Earth Orbit; ~2,000–35,786 km; larger coverage, moderate latency (e.g., GPS).

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GEO

Geostationary Orbit; ~35,786 km; instruments appear stationary relative to Earth, ideal for weather and communications.

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Geosynchronous Orbit

Orbit with a 24-hour period; may be non-equatorial; appears to trace a figure-eight path from the ground.

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Polar Orbit

Orbit that passes over the poles; enables global coverage and sun-synchronous imaging.

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Non-Polar Orbit

Inclined or equatorial orbit offering regional coverage with potential polar gaps.

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Milankovitch Cycles

Variations in Earth’s orbital parameters—eccentricity, obliquity, and precession—that influence glacial/interglacial cycles.

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Eccentricity

Shape of Earth's orbit around the Sun; variations influence seasonal contrast over long timescales.

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Obliquity

Axial tilt of the Earth; affects insolation distribution and seasons.

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Precession

Wobble of Earth's axis; shifts the timing of seasons relative to eccentricity and obliquity.

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Keeling Curve

Long-term record of atmospheric CO2 concentrations from Mauna Loa, showing rising levels and seasonal cycles.

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Global Warming

Increase in Earth's near-surface air and ocean temperatures due to enhanced greenhouse gas concentrations.

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Greenhouse Gases

Atmospheric gases (e.g., H2O, CO2, CH4, O3) that trap heat and warm the planet.

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Radiative Forcing

Measure of the influence of a factor (e.g., greenhouse gases) on the energy balance of the climate system.

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Global Dimming

Reduction in solar radiation reaching Earth's surface due to atmospheric aerosols and other factors.

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Carbon Cycle

Cycle of carbon among atmosphere, biosphere, oceans, and soils, including sources and sinks.

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Hydrological Cycle

Water cycle: evaporation, condensation, precipitation, infiltration, runoff, and storage processes.

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Ozone Layer

Stratospheric layer rich in ozone that absorbs harmful UV radiation.

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Ozone Depletion

Reduction of ozone concentration due to chemical pollutants, notably CFCs, via catalytic reactions.

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Montreal Protocol

International agreement (1989) to phase out ozone-depleting substances like CFCs.

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CCN

Cloud Condensation Nuclei; particles on which water vapor condenses to form clouds.

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Twomey Effect

Increase in cloud reflectivity (albedo) with higher aerosol concentrations, enhancing cooling.

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NDVI

Normalized Difference Vegetation Index; NDVI = (NIR − Red) / (NIR + Red); indicates vegetation density/health.

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EVI

Enhanced Vegetation Index; improves NDVI by reducing canopy background noise; uses NIR, Red, Blue with coefficients.

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Albedo

Fraction of incoming solar radiation reflected by a surface; higher for bright surfaces.

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Emissivity

Efficiency with which a real surface emits thermal radiation relative to a blackbody.

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Blackbody vs Graybody

Blackbody: ideal absorber/emitter; Graybody: emits less than a perfect blackbody (emissivity < 1).

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Planck Function

Equation describing spectral radiance of a blackbody as a function of wavelength and temperature.

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Stefan-Boltzmann Law

Total radiant exitance of a blackbody is proportional to the fourth power of its temperature.

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Wein’s Law

Relates peak wavelength of emitted radiation to the object's temperature; shorter wavelength for hotter objects.

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Peak vs Dominant Wavelength

Peak wavelength: wavelength with maximum emission; Dominant wavelength: wavelength corresponding to perceived color.

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Atmospheric Windows

Wavelength ranges where Earth's atmosphere is relatively transparent to EM radiation.

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Atmospheric Scattering (Rayleigh, Mie)

Scattering of light by particles in the atmosphere; Rayleigh (small particles), Mie (larger particles).

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True Color Image

An image where DN values are mapped to colors representing real-world visible colors.

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False Color Composite (FCC)

An image where colors are assigned to spectral bands that do not correspond to natural colors to highlight features.

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Contrast

Difference in brightness between an object and its surroundings; higher contrast aids detection.

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Resolution (Spatial, Spectral, Radiometric, Temporal)

Spatial: smallest discernible detail; Spectral: ability to distinguish wavelengths; Radiometric: sensitivity to energy differences; Temporal: frequency of data capture.

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Pixel

The smallest element of a digital image representing a sample of the scene’s energy.

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DN (Digital Number)

Digital value assigned to a pixel representing detected radiance before scaling.

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Scale

Ratio of image measurements to real-world measurements; affects area/length calculations.

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NDVI Equation (Channel reference)

NDVI = (NIR − Red) / (NIR + Red); used to assess vegetation health.

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Surface Area Estimation (Finding Area)

Technique to estimate irregular areas by dividing into simple shapes and summing their areas.

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NDVI vs EVI Usage

NDVI is common for vegetation; EVI improves performance in dense canopies and atmospheric corrections.

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Ocean Acidification

Decrease in ocean pH due to CO2 dissolving and forming carbonic acid, affecting marine life.

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Coral Bleaching

Discoloration and loss of coral symbiotic algae due to stress (e.g., warming water).