Air temperature

What is Air temperature?

Air temperature is the measure of how hot or cold the air is at a specific location, typically recorded at 1.5 meters above ground level, and expressed in degrees Celsius or Fahrenheit.

Air temperature is one of the most fundamental aspects of weather and climate, influencing weather conditions, agricultural productivity, and energy consumption.

Temperature is affected by multiple environmental and geographical factors, including the time and location of measurement. The Earth's axial tilt plays a major role in seasonal temperature variations, as different regions receive varying amounts of sunlight throughout the year.

Key factors affecting air temperature

  • Sunlight (solar radiation): The primary heat source for the Earth's atmosphere. Areas receiving more direct sunlight (such as the equator) tend to be warmer than those receiving less (such as the poles).
  • Altitude: Higher elevations generally experience lower temperatures because air pressure and density decrease with altitude, reducing heat retention.
  • Cloud cover: Clouds can trap heat at night, keeping temperatures warmer, or block sunlight during the day, making it cooler.
  • Wind and air masses: Moving air masses transport warm or cold air across regions, causing fluctuations in local temperatures.

By understanding these factors, we can better predict weather patterns, adapt to climate variations, and manage temperature-related challenges in industries such as agriculture, energy, and urban planning.

Published:

April 9, 2025

Alternate names:

Atmospheric temperature

Ambient temperature

Current temperature