Course: SEE211 - Energy, Climate Change and Sustainability
Reference: "Here Comes the Sun" by the Beatles (1969)
Composition: 90% hydrogen (H2), 9% helium (He), and 1% other elements
Fusion Reaction: 41H + 2e = 4He + 2 neutrinos (ν) + 6 gamma rays (γ)
Energy Released: ΔE = 26.7 MeV
Key Parameters:
Amount of Energy
Spectral and Temporal Distributions
Variations Over Time
Solar Constant (Isc): 1.367 kW/m²
Formula for Radiant Power Density Outside Earth's Atmosphere:
Is = Isc * [1 + 0.033 cos(n)]
n: Day of the Year (variation ±3.3% over the year)
Measurement Consistency:
Measured outside Earth's atmosphere, free from atmospheric interference (clouds, dust, gas)
Standard Reference:
Baseline for understanding solar energy modification by Earth's atmosphere
Energy Budget:
Essential for understanding energy absorption, reflection, and emission by Earth
Solar constant value is approximately 1361 watts/m²
Mean extraterrestrial irradiance is ~1.35 kW/m²
Importance in evaluating solar energy systems
Wavelength Range:
Spans UV to IR
Peak Irradiance:
Peaks around 500 nm in visible spectrum
Atmospheric Effects:
Dips in curves due to absorption by atmospheric gases (ozone, CO2, water vapor)
Astronomy:
Studying star spectra, temperature, and composition
Thermodynamics:
Foundation for radiation theory in physics
Technological Applications:
Design in thermal management systems
Climate Science:
Studying Earth's radiation and greenhouse effect
Total solar energy reaching Earth: 1.7x10¹⁷ W (170 petawatts)
Annual solar energy exceeds fossil fuel resources available on Earth
1% irradiance with 10% conversion efficiency meets global energy needs
2022 Energy Statistics:
Solar Flux: 3,850,000 EJ
Wind: 2,250 EJ
Biomass: 3,000 EJ
Electricity: 24,398 TWh (87 EJ)
Components of energy transfer
Incoming sunlight absorption, reflection, emission
Diagram representation of Earth's energy balance
Discussing inherent challenges in solar energy applications
Geographical Location:
High precipitation areas may face more cloud cover
Seasonal Variations:
Planning for seasonal changes in solar power generation
Hybrid Systems:
Utilizing combinations of renewable sources for stability
Summary: Precipitation impacts efficiency but can be beneficial in cleaning panels.
Path length of sunlight through atmosphere affecting radiation intensity
Definitions:
AM0: Outside atmosphere
AM1: Sun at zenith
AM1.5: Standard spectrum for most applications
Intensity of Solar Radiation:
Greater air mass results in lower intensity due to scattering
Absorption and Scattering:
More atmospheric interference at higher air masses
Panel Performance:
Understanding air mass is essential for panel orientation and efficiency
Graph showcasing spectral irradiance regarding solar technology performance
Highlighting solar potential across major cities in India
1600 GW potential per km² noted
Active Systems:
Utilize photovoltaic panels and thermal collectors
Passive Systems:
Involve building materials and design for natural air circulation
Architecture, agriculture, solar lighting, heating, electrical generation
Variety of applications including solar vehicles and cooking
Converting solar radiation into heat for utility and industrial use
Integration into building architecture with advantages in heating water and air
Description of structure and functions of flat panel collectors for heating purposes
Useful heat gain and solar flux regulation
Efficiency in colder climates with design details
Layers function for heat retention and utilization
Utilizing solar energy for efficient air heating applications
Parabolic troughs and power tower designs detailed
Different solar thermal collectors together according to efficiency and temperature ranges
Websites and educational resources provided for comprehensive understanding
Discussion on research opportunities in solar energy technology advancements