Unit 2 Capstone Review: Layers, Lapse Rates, Ozone Calculations, and Global Solutions
Welcome to the capstone synthesis and mastery review of Unit 2 in Science for Preparatory 2! In this comprehensive lesson, we consolidate all our physical, chemical, and atmospheric insights: an analytical comparative matrix across the four atmospheric layers (Troposphere, Stratosphere, Mesosphere, Thermosphere), step-by-step problem-solving methods for temperature lapse rates on mountain summits (Delta T = Height in km * 6. 5), formulas for calculating ozone erosion degrees and percentages, a review of the four major ozone-depleting chemicals, and the global mechanisms countering the greenhouse crisis. This rigorous overview guarantees complete conceptual readiness for the standardized digital exams.
1. Comparative Layers Matrix
Consolidated parameters of atmospheric layers:
- Troposphere: 13 km | 100 mb | drops to -60 °C | vertical air currents | 75% of mass, 99% of water vapor.
- Stratosphere: 37 km | 1 mb | rises to 0 °C | horizontal air currents | houses ozone layer (20-40 km), plane highway.
- Mesosphere: 35 km | 0.01 mb | drops to -90 °C (coldest layer) | highly rarefied, meteors burn.
- Thermosphere: 590 km | rises to 1200 °C (hottest layer) | Ionosphere reflects radio waves; Van Allen belts cause Aurora.
2. Formulas & Problem Solving
Mathematical laws for atmospheric sciences:
- Temperature Change:
ΔT = Height (in km) × 6.5. - Summit Temperature:
Temp at summit = Temp at base - ΔT. - Base Temperature:
Temp at base = Temp at summit + ΔT. - Elevation Height (km):
Height = (Temp at base - Temp at summit) / 6.5. - Ozone Erosion Degree:
Erosion = 300 - Measured Ozone (DU). - Ozone Erosion Percentage:
Percentage = (Erosion / 300) × 100%.
Advanced Calculations Clinic:
Solution:
1. Temperature decrease = 2.5 × 6.5 = 16.25 °C.
2. Temperature at summit = 23 - 16.25 = 6.75 °C.
Solution:
1. Degree of erosion = (25 / 100) × 300 = 75 DU.
2. Remaining ozone = 300 - 75 = 225 DU.
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