The seasons on Earth are caused by the tilt of Earth’s axis and its orbit around the Sun. Here’s how these factors contribute:

1. Tilt of Earth’s Axis:
   • Earth’s axis is tilted at an angle of about 23.5 degrees relative to its orbit around the Sun. This tilt means that different parts of Earth receive varying amounts of sunlight throughout the year.
2. Earth’s Orbit:
   • As Earth orbits the Sun, the tilt causes the Northern and Southern Hemispheres to experience different seasons at different times of the year. The orbit is elliptical, but Earth’s axial tilt plays the primary role in creating the seasons.

The Four Seasons:

• Spring: Occurs when the Earth’s axis is not tilted toward or away from the Sun, resulting in roughly equal day and night lengths (the vernal equinox).
• Summer: The hemisphere tilted toward the Sun receives more direct sunlight, leading to warmer temperatures.
• Autumn (Fall): The Earth’s axis is again not tilted toward or away from the Sun, leading to another period of equal day and night lengths (the autumnal equinox).
• Winter: The hemisphere tilted away from the Sun receives less direct sunlight, leading to colder temperatures.

Key Points:

• Northern Hemisphere experiences summer when it is tilted toward the Sun (around June to September) and winter when it is tilted away (around December to March).
• Southern Hemisphere experiences opposite seasons to the Northern Hemisphere due to its opposite tilt.

The Earth’s axial tilt causes the variation in sunlight during the year, which, in turn, causes the changing seasons.

Temperature is measured scientifically using thermometers or similar instruments based on well-established physical principles. These devices rely on the thermal properties of materials to quantify temperature accurately. Below are the most common methods and tools used for scientific temperature measurement:

1. Thermometers

a. Liquid-in-Glass Thermometers:

Contains mercury or alcohol that expands and contracts with temperature.

Used in meteorology and basic laboratory applications.

b. Digital Thermometers:

Use electronic sensors, such as thermistors or resistance temperature detectors (RTDs), to measure temperature.

Common for medical, industrial, and environmental measurements.

2. Resistance Temperature Detectors (RTDs)

Measure temperature by detecting changes in the electrical resistance of metals (usually platinum).

Accurate and widely used in laboratories and industries.

3. Thermocouples

Measure temperature based on the voltage generated at the junction of two dissimilar metals.

Effective for a wide temperature range, including extreme conditions like furnaces or cryogenics.

4. Infrared (IR) Thermometers

Measure thermal radiation emitted by objects to determine their temperature.

Non-contact method used in industries, healthcare (like fever detection), and astronomy.

5. Pyrometers

Specialized instruments used to measure extremely high temperatures, such as in molten metals or kilns.

Often based on thermal radiation principles.

6. Calorimetry

Used in scientific research to measure temperature changes during chemical reactions or phase transitions.

Relies on the heat transfer principle.

7. Advanced Techniques

a. Spectroscopy-Based Methods:

Used in astrophysics and plasma physics by analyzing light emitted by objects.

b. Cryogenic Sensors:

Specialized sensors like Cernox and silicon diodes for ultra-low temperatures.

Units of Measurement

Temperature is measured using standardized units:

Kelvin (K): SI unit, used in scientific research.

Celsius (°C): Used in daily life and most scientific contexts.

Fahrenheit (°F): Primarily used in the United States.

By employing these tools and methods, scientists can measure temperature with precision across a vast range of environments.