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Questions and Answers

What is the difference between constant and variable components in hydrometeorology?

  • Constant components vary over time, while variable components remain the same.
  • Constant components are only observed in the atmosphere, and variable components are exclusive to water bodies.
  • Constant components fluctuate with weather patterns, whereas variable components are stable.
  • Constant components have proportions that remain the same, while variable components amounts vary. (correct)
  • What altitude range corresponds to the stratosphere in the Earth's atmosphere?

  • 80-300 km
  • 45-80 km
  • 0-10 km
  • 10-45 km (correct)
  • Which of the following is NOT an application of hydrometeorology?

  • Irrigation system design
  • Study of precipitation and evaporation
  • Development of machine learning algorithms (correct)
  • Flood and drought problem analysis
  • Which process is crucial for creating effective cropping calendars in hydrometeorology?

    <p>Precipitation patterns</p> Signup and view all the answers

    What contributes to the determination of suitable cropping systems in hydrometeorology?

    <p>Precipitation, runoff, and evaporation interactions</p> Signup and view all the answers

    Study Notes

    Introduction to Hydrometeorology

    • Hydrometeorology is the study of the Earth's waters and the atmosphere.
    • Hydrology is the study of the Earth's waters, including their occurrence, circulation, distribution, properties, and reaction with the environment.
    • Meteorology is the study of the atmosphere.

    Sources of Water

    • Atmospheric water: Precipitation
    • Surface water: Lakes, rivers, seas, oceans
    • Subsurface water: Groundwater

    Waters of the Earth

    • World water supply (fresh and saline): 97.5% saline, 2.5% fresh
    • World water supply (fresh only): 0.4% lakes, rivers, etc., 30.9% groundwater, 68.7% snow and ice

    Residence Time

    • Reservoir: A term describing the time a water molecule stays in a certain body or area. Measuring the time a water molecule spends in a certain reservoir.
    • Oceans: 1370 km³ x 10,000,000, 97.25%, 40 years
    • Ice Caps and Glaciers: 29 km³ x 10,000,000, 2.05%, 40 years
    • Groundwater: 9.5 km³ x 10,000,000, 0.68%, 200 (shallow) / 10,000 (deep) years
    • Lakes: 0.125 km³ x 10,000,000, 0.01%, 100 years
    • Soil Moisture: 0.065 km³ x 10,000,000, 0.005%, 100 years
    • Atmosphere: 0,013 km³ x 10,000,000, 0.001%, 0.2 years
    • Streams and Rivers: 0.0017 km³ x 10,000,000, 0.0001%, 0.04 years
    • Biosphere: 0.0006 km³ x 10,000,000, 0.00004%, ——- years

    Earth's Atmosphere

    • An envelope of gases surrounding the Earth, held by gravity
    • Composed of clean dry air, water vapor, and impurities

    Composition of Earth's Atmosphere

    • Constant Components (always the same): Nitrogen (78.08%), Oxygen (20.95%), Argon (0.93%), Neon, Helium, Krypton (trace)
    • Variable Components (vary): Water vapor (0-4%), Carbon dioxide (0.039%), Methane (trace), Sulfur dioxide (trace), Ozone (trace), Nitrogen oxides (trace)

    Water Vapor

    • Changes phase easily (solid, liquid, gas)
    • 0-4% by volume
    • Important for heat transfer in the atmosphere
    • Less abundant in polar regions compared to equatorial regions

    Layers of the Atmosphere

    • Troposphere: Weather and climate occur here (ground level to 10 km)
    • Stratosphere: 10 to 50 km
    • Mesosphere: 50 to 90 km
    • Thermosphere: 90 to 120 km
    • Exosphere: >120 km

    Hydrologic Cycle

    • Deals with water storage, movement/transport, and transformation on Earth.
    • The cycle is not continuous or steady, with erratic movement.
    • Drought, torrential rains, and El Niño/La Niña episodes are examples of variability.

    Components of the Hydrologic Cycle

    • Water storage: Atmosphere (water vapor), Soil (soil moisture), Surface water (seas, oceans, streams, lakes, wetlands), Plants and animals, Groundwater
    • Water transport: Evaporation, Transpiration, Precipitation, Runoff, Infiltration, Groundwater flow
    • Water transformation: Liquid to gas (evaporation, transpiration), Gas to liquid (precipitation), Gas to solid (solid forms of precipitation), Solid to liquid (snowmelt)
    • Key components: evaporation, evapotranspiration, precipitation, infiltration, runoff/streamflow, groundwater

    Applications of Hydrometeorology

    • Studying processes like precipitation, runoff, and evaporation
    • Addressing problems like floods and droughts
    • Weather forecasting
    • Cropping calendar preparation
    • Determining suitable cropping systems
    • Irrigation design
    • Dam, culvert, and reservoir construction
    • Soil conservation practice design

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