3rd Grade Science (Next Generation Science Standards) • Earth’s Systems

Comparing Regional Climates — Compare climate characteristics across regions.

Discover why some places are hot and dry while others are cold and snowy all year long.

A microscope with leaf and experiment flask for elementary science discovery
Inside this lesson 10 sections 5 questions 5 figures

SECTION 1

Why Do People Study Climate?

Have you ever wondered why polar bears live in the Arctic but parrots live in tropical jungles? The answer has a lot to do with climate — the usual weather pattern of a place over a long time. People have been studying climate for hundreds of years to understand why different parts of the world feel so different.

Long ago, travelers noticed that some lands were always warm while others were always cold. Scientists began to keep records of temperature and rainfall. Over time, they sorted the world into different climate regions — areas that share similar weather patterns.

~350 BC • Ancient Greece

A Greek thinker named Aristotle split the world into three climate zones: hot near the equator, cold near the poles, and mild in between.

1700s • Thermometer Invented

Scientists built better thermometers and rain gauges. Now they could measure temperature and precipitation with numbers instead of just guessing.

1884 • Köppen Climate System

A scientist named Wladimir Köppen created a system to group climates using temperature and rainfall data. We still use a version of his system today!

Today • Satellites & Computers

Modern satellites orbit Earth and measure climate data from space. Computers help scientists compare climates in every region of the world.

Today, the big question is: How are climates in different regions alike and different? Let's find out!

SECTION 2

Key Ideas About Climate

Before we compare climates, we need to understand a few important ideas. Climate is not the same as weather. Weather is what happens outside right now — like today's rain or sunshine. Climate is the pattern of weather over many years.

1

Temperature

How hot or cold a region usually is. Some places are warm all year. Others have hot summers and cold winters.
2

Precipitation

The water that falls from the sky — like rain, snow, sleet, or hail. Some regions get a lot, and some get very little.
3

Seasons

Some regions have four clear seasons. Others stay almost the same all year long, with just a wet season and a dry season.
4

Location on Earth

Places near the equator get more direct sunlight and are warmer. Places near the poles get less sunlight and are colder.
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KEY TAKEAWAY

Think of climate like your closet. If you live somewhere cold, your closet is full of coats and boots. If you live somewhere hot, it is full of shorts and sandals. Your closet tells the long-term pattern — that is your climate!

SECTION 3

A Picture of Earth's Climate Zones

Earth can be divided into big climate zones based on how much sunlight each area gets. The diagram below shows how the zones wrap around the planet like belts.

Earth's Major Climate ZonesPolar (very cold all year)Temperate (warm summers, cold winters)Tropical (hot and warm all year)Temperate (warm summers, cold winters)Polar (very cold all year)NS← Equator
The tropical zone sits near the equator (the dashed yellow line). The temperate zones are in the middle, and the polar zones are at the top (North Pole) and bottom (South Pole).

Notice how the zones appear in the same order on both sides of the equator. The tropical zone gets the most direct sunlight, so it is the warmest. The polar zones get the least sunlight, so they are the coldest. The temperate zones are in between.

SECTION 4

What Shapes a Region's Climate?

Several things work together to shape a region's climate. Let's look at the main ones.

Distance from the Equator

The equator is an imaginary line around the middle of Earth. Places close to the equator get sunlight that hits more directly, which makes them warmer. Places far from the equator get sunlight at a lower angle, so they are cooler.

Altitude (How High Up)

Altitude means how high above sea level a place is. The higher you go, the colder it gets. That is why mountain tops can have snow even when the land below is warm.

Nearness to Oceans

Oceans heat up and cool down slowly. Places near the ocean usually have milder temperatures — not too hot in summer and not too cold in winter. Places far from the ocean can get very hot in summer and very cold in winter.

Wind and Water Currents

Big winds and ocean currents carry warm or cold air and water around the planet. They can make a region warmer or cooler than you might expect just from its location.

💡

Fun Fact

The city of Quito, Ecuador, sits right on the equator — but it is not super hot! Why? Because it is high up in the mountains (about 2,850 meters). Altitude cools it down.

SECTION 5

Comparing Four Major Climate Types

Let's look closely at four climate types you can find on Earth. Each one has its own temperature and precipitation pattern, and each one supports different plants and animals.

Four Climate Types ComparedTropical🌡️ Hot all year🌧️ Lots of rain🌴 RainforestsAvg temp: 25−28°CRain: very highEx: Amazon, HawaiiDesert🌡️ Very hot days🏜️ Very little rain🌵 Cacti & sandAvg temp: 30−40°CRain: very lowEx: Sahara, ArizonaTemperate🌡️ Four seasons🌦️ Medium rain🍂 Forests & fieldsAvg temp: 10−20°CRain: mediumEx: New York, LondonPolar🌡️ Cold all year❄️ Snow & ice🐧 Tundra & iceAvg temp: −20−0°CRain: low (snow)Ex: Antarctica, ArcticTemperature Scale (warmest → coldest)HotWarmMildColdPrecipitation Scale (most → least)Tropical (most)Temperate (medium)Desert & Polar (least)
This diagram compares four climate types by temperature and precipitation. Notice how tropical climates are hot with lots of rain, while polar climates are cold with very little precipitation.
Climate TypeTemperaturePrecipitationExample Plants
TropicalHot all year (25−28°C)Very high rainPalm trees, ferns
DesertVery hot days, cool nightsVery little rainCacti, small shrubs
TemperateWarm summers, cold wintersMedium rain & snowOak trees, grass
PolarCold all year (below 0°C)Low (mostly snow)Moss, lichens

Summary of four major climate types

SECTION 6

Worked Example: Comparing Two Cities

Let's practice comparing the climates of two real cities: Miami, Florida and Anchorage, Alaska. Follow along step by step!

Comparing Miami and Anchorage

  1. 1

    Step 1 — Find Each City's Location

    Miami is in the southern United States, close to the tropics. Anchorage is in Alaska, far to the north, close to the polar zone.
    Miami = near tropics; Anchorage = near polar zone
  2. 2

    Step 2 — Compare Temperature

    Miami's average temperature in January is about 20°C (68°F). Anchorage's average in January is about −8°C (18°F). Miami stays warm most of the year. Anchorage has long, cold winters.
    Miami is much warmer than Anchorage
  3. 3

    Step 3 — Compare Precipitation

    Miami gets about 150 cm (60 inches) of rain per year, mostly in summer. Anchorage gets about 40 cm (16 inches) of precipitation, and much of it falls as snow.
    Miami gets more rain; Anchorage gets less, mostly snow
  4. 4

    Step 4 — Compare Seasons

    Miami has a wet season and a dry season, but it stays warm in both. Anchorage has four seasons with a very short summer and a very long winter.
    Miami: wet/dry seasons; Anchorage: four seasons with long winter
  5. 5

    Step 5 — State Your Conclusion

    Miami has a tropical-like climate that is hot and rainy. Anchorage has a cold climate with long winters and less precipitation. Their climates are very different because of how far they are from the equator.
    Location on Earth is the main reason their climates are so different.

SECTION 7

What Climates Have in Common — and What Makes Them Different

Even though climates can look very different, every climate has the same basic parts: temperature, precipitation, and seasons. The table below shows what is similar and different across climate types.

FeatureSimilarities Across ClimatesDifferences Across Climates
TemperatureAll regions have a measurable average temperature.Ranges from below −40°C (polar) to above 40°C (desert).
PrecipitationAll regions receive some form of precipitation.Can be rain, snow, sleet, or hail, in very different amounts.
SeasonsAll regions have patterns that repeat each year.Some have 4 seasons, some have 2, some stay nearly the same.
Plants & AnimalsAll climates support some form of life.Tropical has the most species; polar and desert have fewer.

How climates are alike and different

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KEY TAKEAWAY

Think of climate types like flavors of ice cream. Vanilla and chocolate are both ice cream (they share a base), but they taste very different. In the same way, all climates have temperature and precipitation, but the amounts and patterns make each one unique!

SECTION 8

Climate and the Bigger Picture

In this lesson, we compared climates today. But scientists also study how climates change over time. As you learn more science, you will explore why Earth's climates have shifted in the past and how they might change in the future.

What You Learned TodayWhat You Will Learn Later
Climates can be sorted into zones like tropical, desert, temperate, and polar.How oceans and the atmosphere move heat around the whole planet.
Temperature and precipitation are the two main ways to compare climates.How greenhouse gases in the atmosphere affect Earth's temperature.
Distance from the equator is a big factor in a region's climate.How people can affect climate through their actions and choices.

Today's lesson compared to future topics

Understanding how to compare regional climates is the first step. Once you can describe and compare, you can start to ask bigger questions — like Why is this climate changing? and What can we do about it?

SECTION 9

Practice Problems

Try these five questions to test what you have learned. They go from easier to harder. Give each one a try before looking at the answer!

Question 1: CONCEPTUAL

What is the difference between weather and climate? Give an example of each.
Show answer
Weather is what is happening outside right now — for example, "It is raining today." Climate is the pattern of weather over many years — for example, "Seattle gets a lot of rain every year." Weather changes day to day, but climate describes what you can usually expect in a place.

Question 2: BASIC IDENTIFICATION

A city has an average temperature of 27°C all year and gets heavy rain almost every day. Which climate type does this city most likely belong to: tropical, desert, temperate, or polar?
Show answer
This city most likely has a tropical climate. Tropical climates are hot all year with average temperatures around 25−28°C, and they receive a lot of rain. Deserts are hot but dry. Temperate regions have changing seasons. Polar regions are very cold. The combination of constant warmth and heavy rain points to a tropical climate.

Question 3: INTERMEDIATE

City A has hot summers (30°C) and cold winters (−5°C). City B stays around 26°C all year. Both cities get about the same amount of rain. Name one way their climates are similar and two ways they are different.
Show answer
Similar: Both cities get about the same amount of precipitation each year. Different #1: City A has a big temperature change between summer and winter, while City B stays warm all year. Different #2: City A likely has four seasons, while City B likely has a wet season and a dry season. City A sounds like a temperate climate, and City B sounds like a tropical climate.

Question 4: APPLIED

Imagine you are packing for two trips. Trip 1 is to a tropical rainforest. Trip 2 is to the Arctic tundra. What would you pack for each trip, and why? Use what you know about each climate to explain.
Show answer
For the tropical rainforest you would pack light, breathable clothes, a rain jacket, and bug spray because it is hot and rainy with lots of insects. For the Arctic tundra you would pack heavy winter coats, thick boots, gloves, and warm hats because it is extremely cold all year and there is snow and ice on the ground. The difference in packing shows how different the two climates are in temperature and precipitation.

Question 5: CRITICAL THINKING

A mountain sits right on the equator. At the bottom it is hot and full of tropical plants. At the top it is freezing with snow. How is this possible if the mountain is in the tropical zone? Use what you learned about altitude and the equator to explain.
Show answer
Even though the mountain is at the equator (where sunlight is strong and direct), altitude also affects temperature. The higher you go on a mountain, the colder the air gets. So the bottom of the mountain is hot like a typical tropical area, but the top is so high up that the temperature drops below freezing. This shows that distance from the equator is not the only thing that shapes climate — altitude is another important factor. This is why you can find snow near the equator on tall mountains like those in Ecuador or Kenya.

SUMMARY

Lesson Summary

Summary

Climate is the long-term weather pattern of a region, measured mainly by temperature and precipitation. Earth has several major climate zones. The tropical zone near the equator is hot and rainy. Desert climates are hot and dry. Temperate climates have changing seasons with moderate rain. Polar climates are very cold all year with little precipitation.

A region's climate depends on its distance from the equator, its altitude, how close it is to the ocean, and wind and ocean currents. By comparing these features across different regions, you can explain why some places are hot and wet while others are cold and dry. Understanding climate helps us predict what plants and animals can live in a region and how people there live their daily lives.

Varsity Tutors • 3rd Grade Science • Comparing Regional Climates