Keeling Curve
Vostok Ice Cores
Ice Cores
Year 536
100

What does the Keeling Curve measure?

CO2 Levels in the atmosphere 

100

About how far back in time do the Vostok ice cores provide climate data?

Around 400,000 years

100

What do ice cores allow scientists to study?

Past environmental conditions

100

What caused darkness across Europe, the Middle East, and parts of Asia in 536?

A volcanic eruption  

200

Where does the data from the graph come from?

Mauna Loa, Hawaii

200

The Earth has gone through several changes of high and low levels of CO2. True or False.

True

200

Most ice cores come from this location

Antarctica 

200

Scientists traced the volcanic eruption of 536 to which island nation?

Iceland

300

When the Keeling Curve began in 1958, atmospheric CO₂ was around 315 parts per million (ppm). About what level has it reached in recent years?

420 ppm

300

Where was the Vostok ice core collected?

Antarctica

300

What does a thicker ice layer indicate?

The glacier received more snow that year

300

How much did summer temperatures drop during the year 536?

1.5–2.5°C

400

What year did Charles Keeling begin his continuous CO₂ measurements at Mauna Loa?

1958

400

How do modern CO₂ levels (over 420 ppm) compare to those in the Vostok record?

They are much higher than any in the past 420,000 years

400

What tool do scientists use to collect ice cores?

Hollow drills

400

What chemical element from volcanic eruptions can block sunlight and cool Earth?

Sulfur

500

The small zigzag pattern in the Keeling Curve each year is caused by what natural process?

Plants or photosynthesis

500

During warm interglacial periods in the Vostok record, CO₂ concentrations reached about:

280-300 ppm

500

Which of the following materials might scientists find trapped in ice layers?

Dust, pollen, volcanic ash, and insects

500

Snowfall during summer in 536 was reported in which country?

China