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UGC NET Environmental Science Unit-I: Fundamentals of Environmental Sciences Syllabus

The Unit-I: Fundamentals of Environmental Sciences syllabus for UGC NET Environmental Science in full: 11 chapters and 14 topics, every one listed below, plus 50 Unit-I: Fundamentals of Environmental Sciences flashcards with answers.

11Chapters
14Topics
50Flashcards

Unit-I: Fundamentals of Environmental Sciences syllabus: all 11 chapters

Expand any chapter to see its topics and sub-topics.

  1. Definition, Principles and Scope of Environmental Science

    overview

    No separate topics listed for this chapter.

  2. Structure and Composition of Atmosphere, Hydrosphere, Lithosphere and Biosphere

    overview

    No separate topics listed for this chapter.

  3. Laws of Thermodynamics, Heat Transfer Processes, Mass and Energy Transfer Across Various Interfaces, Material Balance

    overview

    No separate topics listed for this chapter.

  4. Meteorological Parameters

    11 topics
    • Pressure
    • Temperature
    • Precipitation
    • Humidity
    • Mixing Ratio
    • Saturation Mixing Ratio
    • Radiation
    • Wind Velocity
    • Adiabatic Lapse Rate
    • Environmental Lapse Rate
    • Wind Roses
  5. Interaction between Earth, Man and Environment

    overview

    No separate topics listed for this chapter.

  6. Biogeographic Provinces of the World and Agro-climatic Zones of India

    overview

    No separate topics listed for this chapter.

  7. Concept of Sustainable Development

    overview

    No separate topics listed for this chapter.

  8. Natural Resources and Their Assessment

    overview

    No separate topics listed for this chapter.

  9. Remote Sensing and GIS

    3 topics
    • Principles of Remote Sensing and GIS
    • Digital Image Processing and Ground Truthing
    • Application of Remote Sensing and GIS in Land Cover/Land Use Planning and Management (Urban Sprawling, Vegetation Study, Forestry, Natural Resource), Waste Management and Climate Change
  10. Environmental Education and Awareness

    overview

    No separate topics listed for this chapter.

  11. Environmental Ethics

    overview

    No separate topics listed for this chapter.

UGC NET Environmental Science Unit-I: Fundamentals of Environmental Sciences flashcards — 50 questions with answers

  1. What is atmospheric pressure and what instrument measures it?

    Atmospheric pressure is the force exerted per unit area by the weight of the overlying air column. It is measured with a barometer (mercury or aneroid) and expressed in pascals (Pa), millibars (mb/hPa), or atmospheres; standard sea-level pressure is 1013.25 hPa (1 atm).

  2. How does atmospheric pressure vary with altitude?

    Pressure decreases roughly exponentially with height because less air lies above. It falls by about half for every ~5.5 km of ascent, described by the barometric formula P = P0 · exp(-h/H), where H is the scale height (~8 km).

  3. Distinguish between temperature and heat in atmospheric science.

    Temperature is a measure of the average kinetic energy of molecules (intensity of heat). Heat is the total thermal energy transferred between bodies due to a temperature difference. Temperature is measured in °C, °F, or K (0 K = -273.15 °C).

  4. What is precipitation and name its main forms?

    Precipitation is any form of water (liquid or solid) that falls from clouds and reaches the ground. Main forms: rain, drizzle, snow, sleet, hail, and freezing rain. It is measured with a rain gauge in millimetres.

  5. Define absolute humidity, specific humidity, and relative humidity.

    Absolute humidity = mass of water vapour per unit volume of air (g/m³). Specific humidity = mass of water vapour per unit mass of moist air (g/kg). Relative humidity = ratio of actual vapour pressure to saturation vapour pressure at that temperature, expressed as a percentage.

  6. What does relative humidity of 100% indicate?

    It indicates the air is saturated—the actual water vapour content equals the maximum the air can hold at that temperature. Further cooling or addition of vapour leads to condensation (dew, fog, or cloud formation); the dew point equals the air temperature.

  7. Define mixing ratio in atmospheric science and give its formula.

    Mixing ratio (w) is the mass of water vapour per unit mass of dry air, usually in g/kg. Formula: w = mv / md, or w = 0.622 · e/(P − e), where e is vapour pressure and P is total atmospheric pressure.

  8. What is the saturation mixing ratio and how does it depend on temperature?

    Saturation mixing ratio (ws) is the mass of water vapour per unit mass of dry air when the air is saturated at a given temperature and pressure. It increases strongly with temperature (warm air holds far more vapour) and decreases with increasing pressure.

  9. How is relative humidity expressed using mixing ratios?

    Relative humidity (RH) = (w / ws) × 100, where w is the actual mixing ratio and ws is the saturation mixing ratio at the same temperature and pressure.

  10. What is the dew point temperature?

    The dew point is the temperature to which air must be cooled, at constant pressure and water-vapour content, for it to become saturated (RH = 100%). Below it, condensation occurs. A small gap between air temperature and dew point indicates high humidity.

  11. Define solar (electromagnetic) radiation and its primary source.

    Radiation is energy transferred as electromagnetic waves requiring no medium. The Sun is the primary source, emitting mostly shortwave radiation (visible, UV, near-IR). Earth re-emits absorbed energy as longwave (terrestrial/infrared) radiation.

  12. State the Stefan–Boltzmann law of radiation.

    The total energy radiated per unit surface area of a black body is proportional to the fourth power of its absolute temperature: E = σT⁴, where σ = 5.67 × 10⁻⁸ W m⁻² K⁻⁴. Hotter bodies radiate far more energy.

  13. State Wien's displacement law.

    The wavelength of peak emission of a black body is inversely proportional to its absolute temperature: λmax = b/T, where b = 2.898 × 10⁻³ m·K. The hot Sun peaks in visible light; the cooler Earth peaks in the infrared.

  14. What is the solar constant?

    The solar constant is the average solar radiation received per unit area at the top of Earth's atmosphere on a surface perpendicular to the Sun's rays, at the mean Earth–Sun distance. Its value is approximately 1361–1366 W/m².

  15. Differentiate albedo from emissivity.

    Albedo is the fraction of incident shortwave (solar) radiation reflected by a surface (0–1; e.g. fresh snow ~0.8, ocean ~0.06). Emissivity is the efficiency with which a surface emits longwave radiation relative to a black body (0–1).

  16. What is wind velocity and what instruments measure wind?

    Wind velocity is the rate and direction of horizontal air movement (a vector: speed + direction). Wind speed is measured with an anemometer (m/s, km/h, or knots) and direction with a wind vane; direction is named for where the wind comes FROM.

  17. What primarily drives wind, and name two forces that modify its direction.

    Wind is driven by horizontal pressure gradients (air moving from high to low pressure). Its direction is modified by the Coriolis force (due to Earth's rotation) and friction near the surface; centripetal force matters in curved flow.

  18. Define the Dry Adiabatic Lapse Rate (DALR) and give its value.

    The DALR is the rate at which an unsaturated (dry) air parcel cools as it rises adiabatically (no heat exchange) due to expansion. Its value is approximately 9.8 °C per 1000 m (about 10 °C/km), and it is constant.

  19. Define the Saturated (Moist) Adiabatic Lapse Rate (SALR/MALR).

    The SALR is the rate at which a saturated rising air parcel cools. It is lower than the DALR (averages ~5–6 °C/km, range 4–9 °C/km) because latent heat released during condensation partly offsets the cooling. It varies with temperature and moisture.

  20. What is the Environmental Lapse Rate (ELR) and its average value?

    The ELR is the actual observed rate of temperature decrease with height in the surrounding stationary atmosphere. Its average (normal) value in the troposphere is about 6.5 °C per 1000 m, but it varies with location, time, and weather.

Show the other 30 Unit-I: Fundamentals of Environmental Sciences flashcards
  1. How are the lapse rates used to determine atmospheric stability?

    Compare the Environmental Lapse Rate (ELR) with the adiabatic rates. If ELR < SALR → absolutely stable; if ELR > DALR → absolutely unstable; if SALR < ELR < DALR → conditionally unstable. Stable air suppresses vertical mixing and traps pollutants.

  2. What is a temperature inversion and why is it significant for pollution?

    A temperature inversion is when temperature increases with height (opposite to normal), making the lower air denser and very stable. It suppresses vertical mixing, trapping pollutants near the ground and causing smog/haze episodes.

  3. What is a wind rose and what information does it display?

    A wind rose is a circular (polar) diagram that shows the frequency distribution of wind direction and speed at a location over a period. Spokes/petals point to the directions winds blow from; their length shows frequency and colour bands show speed classes.

  4. What does the longest spoke on a wind rose indicate, and one application?

    The longest spoke indicates the prevailing (most frequent) wind direction. Wind roses are used in air-pollution dispersion studies, airport runway alignment, and siting of industries, wind farms, and landfills relative to settlements.

  5. Define remote sensing.

    Remote sensing is the science of acquiring information about an object, area, or phenomenon by recording reflected or emitted electromagnetic radiation using sensors mounted on platforms (satellites, aircraft, drones) without physical contact with the target.

  6. What are the basic components/stages of a remote sensing system?

    The components are: (1) an energy source/illumination, (2) interaction of radiation with the atmosphere, (3) interaction with the target, (4) recording of energy by the sensor, (5) transmission/reception/processing, and (6) interpretation/analysis and application.

  7. Distinguish between active and passive remote sensing.

    Passive sensors record natural radiation reflected or emitted by the target (e.g. optical/thermal sensors using sunlight). Active sensors generate their own energy and measure the returned signal (e.g. RADAR, LiDAR), enabling day/night and all-weather operation.

  8. What is spectral reflectance (signature) and why is it useful?

    Spectral reflectance is the proportion of incident energy a surface reflects across different wavelengths. Each feature has a characteristic reflectance curve (spectral signature)—e.g. healthy vegetation strongly reflects near-IR—allowing features to be identified and distinguished.

  9. List the four types of resolution in remote sensing.

    Spatial resolution (smallest distinguishable ground area/pixel size), Spectral resolution (number and width of wavelength bands), Radiometric resolution (sensitivity to energy differences/bit depth), and Temporal resolution (revisit frequency of a location).

  10. What is the 'atmospheric window' in remote sensing?

    Atmospheric windows are wavelength ranges where the atmosphere is largely transparent (low absorption/scattering), allowing radiation to pass through to sensors. The visible, parts of the infrared, and microwave regions are key windows used in remote sensing.

  11. Define a Geographic Information System (GIS).

    A GIS is a computer-based system for capturing, storing, managing, analysing, and displaying spatially referenced (geographic) data. It links attribute data to geographic location, enabling spatial query, overlay, and modelling for decision-making.

  12. What are the main components of a GIS?

    The five components are: Hardware, Software, Data (spatial + attribute), People (users/experts), and Methods/Procedures. Data is often considered the most important and expensive component.

  13. Compare raster and vector data models in GIS.

    Raster represents space as a grid of cells/pixels, each holding a value—good for continuous data (imagery, elevation). Vector represents features as points, lines, and polygons with coordinates—good for discrete features (roads, boundaries) and precise mapping.

  14. What is a data layer (overlay) in GIS and why is it powerful?

    A layer is a themed dataset (e.g. roads, land use, soils) referenced to common coordinates. Overlay analysis stacks and combines layers spatially to reveal relationships and produce new information—a core GIS analytical capability for suitability and planning.

  15. Differentiate spatial data from attribute data in GIS.

    Spatial data describes the location, shape, and geometry of features (where things are—coordinates). Attribute data describes the characteristics or properties of those features (what they are—e.g. name, population, land-use type), stored in linked tables.

  16. What is digital image processing in remote sensing?

    Digital image processing is the computer-based manipulation and analysis of digital remote-sensing images (arrays of pixels with DN values) to correct distortions, enhance features, and extract thematic information. Main steps: pre-processing, enhancement, transformation, and classification.

  17. What is image rectification/geometric correction?

    Geometric correction (rectification) removes geometric distortions (from sensor, platform, Earth curvature/rotation) and aligns the image to a map coordinate system (georeferencing), so pixels correspond to true ground positions. It often uses ground control points and resampling.

  18. Name three common image enhancement techniques.

    (1) Contrast stretching (expanding the range of DN values to improve visibility), (2) Spatial filtering (low-pass smoothing or high-pass edge enhancement), and (3) Band ratioing / band combinations (e.g. creating indices or false-colour composites).

  19. Differentiate supervised and unsupervised image classification.

    Supervised classification uses analyst-defined training samples of known classes to teach the algorithm (e.g. maximum likelihood). Unsupervised classification automatically groups pixels into spectral clusters (e.g. ISODATA, K-means) which the analyst then labels.

  20. What is ground truthing (ground verification) in remote sensing?

    Ground truthing is the collection of in-situ reference data (field observations, GPS points, measurements) to verify, calibrate, and validate the interpretation/classification of remotely sensed imagery, ensuring accuracy of the derived maps.

  21. What is an accuracy assessment and the error (confusion) matrix?

    Accuracy assessment compares classified-map results against ground-truth reference data to measure correctness. An error/confusion matrix cross-tabulates classified vs reference classes, yielding producer's accuracy, user's accuracy, overall accuracy, and the Kappa coefficient.

  22. What is NDVI and what does it indicate?

    The Normalized Difference Vegetation Index = (NIR − Red)/(NIR + Red). It ranges from −1 to +1; high positive values indicate dense, healthy green vegetation, while low/negative values indicate bare soil, water, or built-up surfaces. It is widely used in vegetation studies.

  23. Distinguish land cover from land use.

    Land cover refers to the physical/biophysical material on the Earth's surface (forest, water, grass, built-up, bare soil). Land use refers to how humans utilise the land (agriculture, residential, industrial, recreation). RS/GIS produces LULC (Land Use/Land Cover) maps.

  24. How are remote sensing and GIS used to study urban sprawl?

    Multi-temporal satellite images are classified to map built-up areas over different years; change-detection in GIS quantifies the rate, direction, and pattern of urban expansion into surrounding rural/green land, supporting urban planning and growth management.

  25. Give two applications of RS and GIS in forestry.

    (1) Mapping forest cover, type, and density and monitoring deforestation/afforestation through change detection; (2) Estimating biomass/carbon stock, assessing forest health, and detecting/monitoring forest fires and encroachment.

  26. How do RS and GIS support natural resource management?

    They enable inventory and mapping of resources (water, soil, minerals, vegetation), monitoring of their condition and change over time, suitability analysis for sustainable use, watershed management, and identification of groundwater potential and degraded lands.

  27. How are RS and GIS applied in solid waste management?

    They are used for suitable landfill/dumpsite site selection via multi-criteria overlay (considering land use, water bodies, settlements, roads, geology), monitoring existing dumpsites, optimising collection/transport routes, and assessing environmental impact of waste sites.

  28. How do remote sensing and GIS contribute to climate change studies?

    They monitor large-scale indicators—glacier/ice-sheet retreat, sea-level and sea-surface temperature, deforestation, land-use change, greenhouse-gas and aerosol concentrations, vegetation/phenology shifts—and model impacts and vulnerability for mitigation and adaptation planning.

  29. What is a false colour composite (FCC) and why is it used for vegetation?

    An FCC assigns near-infrared, red, and green bands to the red, green, and blue display channels respectively. Healthy vegetation, which reflects NIR strongly, appears bright red, making it easy to discriminate vegetation type, vigour, and stress.

  30. What is change detection in remote sensing and GIS?

    Change detection is the process of identifying differences in the state of a feature or area by analysing co-registered images acquired at different times. It quantifies what has changed, where, and how much—used for LULC change, deforestation, urban growth, and disaster assessment.

UGC NET Environmental Science Unit-I: Fundamentals of Environmental Sciences FAQ

What is in the UGC NET Environmental Science Unit-I: Fundamentals of Environmental Sciences syllabus?

UGC NET Environmental Science Unit-I: Fundamentals of Environmental Sciences is split into 11 chapters: Definition, Principles and Scope of Environmental Science, Structure and Composition of Atmosphere, Hydrosphere, Lithosphere and Biosphere, Laws of Thermodynamics, Heat Transfer Processes, Mass and Energy Transfer Across Various Interfaces, Material Balance, Meteorological Parameters, Interaction between Earth, Man and Environment, Biogeographic Provinces of the World and Agro-climatic Zones of India, Concept of Sustainable Development, Natural Resources and Their Assessment, Remote Sensing and GIS, Environmental Education and Awareness and Environmental Ethics. Together they contain 14 topics.

How many chapters are in UGC NET Environmental Science Unit-I: Fundamentals of Environmental Sciences?

11 chapters, containing 14 topics. The largest chapter is Meteorological Parameters, with 11 topics.

Are there flashcards for UGC NET Environmental Science Unit-I: Fundamentals of Environmental Sciences?

Yes — a 50-card Unit-I: Fundamentals of Environmental Sciences deck, printed in full in the flashcards section of this page and available in the Examius app with spaced repetition. The free plan covers one exam of your choice, including its flashcards; Examius Pro, a one-time purchase, unlocks every other exam and deck.