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Chapter 3 — Temperature

PHY 116 • Introduction to Meteorology • Fall 2026

TEST 2

October 14, 2026

Chapters 3, 4 and 5

NO CALCULATORS ON THE EXAM.

Test 2 Review →

Introduction to Temperature

Temperature is one of the most basic elements of weather and climate.

The daily mean temperature can be determined by averaging the 24 hourly readings or by adding the maximum and minimum temperatures for a 24-hour period and dividing by two.

Daily Mean Temperature
(Maximum + Minimum) ÷ 2

The daily temperature range is the difference between the maximum and minimum temperatures.

Daily Temperature Range
Maximum − Minimum

Monthly Mean Temperature

The sum of the daily mean temperatures divided by the number of days in the month.

Annual Mean Temperature

The average of the 12 monthly mean temperatures.

Annual Temperature Range

The difference between the warmest and coldest monthly mean temperatures.

Daily Temperature Range

The difference between the day's maximum and minimum temperatures.

NWS New York Climate Data →

Controls of Temperature

The controls of temperature are the factors that cause temperature to vary from place to place.

1
Differential Heating
of Land & Water
2
Ocean Currents
3
Altitude
4
Geographic Position
5
Cloud Cover
6
Albedo

Ocean Temperatures

Atlantic Ocean sea surface temperatures

Click the image for a larger view.

View Global Ocean Temperatures →

Ocean Currents

Global ocean currents

Global Temperature Patterns

On maps showing the world distribution of temperature, isotherms are lines connecting points having the same temperature.

Isotherms generally trend east and west and show decreasing temperatures toward the poles. They also reveal the effects of the seasonal migration of the Sun's vertical rays and the influence of ocean currents.

The north-south migration of isotherms is generally more pronounced over continents because land experiences greater temperature changes than water.

Remember: Annual temperature range is generally small near the equator and increases with latitude. Outside the tropics, temperature range also tends to increase with continentality.

Seasonal Lag

The warmest and coldest months do not occur exactly when incoming solar radiation reaches its maximum and minimum.

In the Northern Hemisphere, the greatest solar intensity occurs around the summer solstice, but July and August are generally warmer. Likewise, minimum solar energy occurs around the winter solstice, but January and February are usually colder.

View Current WPC Surface Analysis →

Measuring Temperature

Thermometers measure temperature mechanically or electrically.

Liquid-in-Glass Thermometer

Uses the expansion and contraction of a liquid as temperature changes.

Maximum Thermometer

Traditionally designed to record the highest temperature reached during a period.

Minimum Thermometer

Records the lowest temperature reached during a period.

Thermistor

An electrical thermal resistor used to measure temperature.

A bimetal strip mechanical thermometer can be used in a thermograph, an instrument that continuously records temperature.

Temperature Scales

READ PAGES 70 TO 73. Temperature conversions are important for Chapter 3 and Test 2.
Fahrenheit Ice point: 32°F

Steam point: 212°F
Celsius Ice point: 0°C

Steam point: 100°C
Kelvin Absolute scale.

Ice point approximately: 273 K

Temperature Conversion Formulas

°C → °F
°F = 1.8(°C) + 32

°F → °C
°C = (°F − 32) ÷ 1.8

°C → Kelvin
K = °C + 273

Practice Temperature Conversions

⇄

Example: Celsius to Fahrenheit

16°C:

°F = 1.8 × 16 + 32
°F ≈ 61°F

Temperature Conversion Videos

Degree Days

Three common applications of temperature data are heating degree days, cooling degree days and growing degree days.

65°
REMEMBER THE MAGIC NUMBER OF 65

Heating Degree Days

Each degree that the daily mean temperature is below 65°F contributes to heating degree days.

Cooling Degree Days

Determined from how far the daily mean temperature is above 65°F.

Growing Degree Days

Determined from the difference between the daily mean temperature and the base temperature required for a crop to grow.
READ PAGES 73 AND 74.

View Islip Climate / Heating & Cooling Degree Data →

Heat Index & Wind Chill

Heat Index

The heat index combines air temperature and humidity to describe how hot conditions feel to the human body.

National Weather Service Heat Index Chart

National Weather Service Heat Index Information →

Wind Chill

Wind chill combines air temperature and wind speed to describe how cold conditions feel to exposed skin.

National Weather Service Wind Chill Chart

National Weather Service Wind Chill Information →

Isopleths & Isotherms

An isopleth is a line connecting points having an equal value of a particular quantity.

ISOTHERM: A line connecting points of equal temperature.

Analysis charts may show isotherms in 2-, 4-, 5- or 10-degree increments.

Meteorologists use isotherms to help identify temperature gradients, fronts, warm-air advection, cold-air advection and other important atmospheric features.

Learn More About Isopleths →

What You Need to Know for Test 2

TEST 2 — OCTOBER 14, 2026

Chapters 3, 4 and 5

OPEN THE FULL TEST 2 REVIEW →