Air Meteorology | Temperature (Part 1) | Chapter 3 | DGCA CPL

Welcome to Aerominds Training Centre!

In this video, we continue Meteorology with Chapter 3 – Temperature, one of the most fundamental and scoring chapters for DGCA CPL and ATPL exams.

This lesson is specially designed for students who are completely new to aviation and meteorology. Concepts are explained from absolute basics, using simple language, real-life examples, and clear exam-oriented logic, without unnecessary complexity.

In this video, you will clearly understand:

• What a black body is and why Earth and Sun behave like black bodies
• Stefan Boltzmann’s Law, Wien’s Law, and Planck’s Law explained in exam-friendly terms
• Earth’s radiation balance and heat budget
• Distribution of incoming solar radiation in the atmosphere and at the surface
• Albedo and why snow-covered surfaces reflect most solar energy
• Diurnal variation of surface temperature over land and sea
• Coastal effects, sea breeze influence, and wind effects on temperature variation
• Why minimum temperature occurs after sunrise and maximum after noon
• Effect of clouds on daytime heating and nighttime cooling
• Why cloudy nights are warmer and clear nights are colder
• DGCA CPL / ATPL exam relevance, frequently asked MCQs, and common conceptual traps

This video focuses on deep concept clarity and DGCA exam-oriented understanding rather than rote memorisation.

Whether you are a student pilot in India, preparing for DGCA CPL or ATPL examinations, or just starting your aviation journey after 12th, this class will help you build a rock-solid foundation in Meteorology.

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