Orbital cycles and ice ages
Grade 9 Science Worksheet

Circle the best answer.
A timeline divided into equal cycles. NASA: between 1 and 3 million years ago, ice ages came about every 41,000 years. About how many fit in that 2-million-year span, by Esme's math?
- About 4.9
- About 82
- About 20
- About 49
Earth tilted more and less beside the Sun. NASA: the tilt was at its maximum about 10,000 years ago and reaches its minimum about 10,000 years from now. How does that span compare with the cycle, by Jun's math?
- About 41,000 years, a full cycle
- About 10,000 years, a full cycle
- About 20,000 years, about half the 41,000-year cycle
- About 20 years
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Earth's orbit with January and July marked.
NASA: Earth is about 3.4% closer to the Sun in January than in July, and about 6.8% more sunlight arrives. Why is the sunlight change about double, by Kira's reading?
- The Northern Hemisphere tilts toward the Sun in January
- January days are longer everywhere
- The Sun itself is brighter in January
- Sunlight weakens with the square of distance
NASA: at its most elliptical orbit, about 23% more sunlight arrives at closest approach; today it is about 6.8%. About how many times larger is 23%, by Luz's math?
- About 3.4 times
- About 29.8 times
- About 16 times
- About 0.3 times
EPICA Dome C temperature record (NOAA NCEI)
Years ago Temperature vs last 1,000 years 20,000 −9.4 °C 128,000 +3.4 °C 140,000 −9.1 °C 410,000 +1.6 °C 800,000 −8.9 °C Using the EPICA table, how much warmer was 128,000 years ago than 140,000 years ago, by Noah's math?
- About 3.4 °C
- About 125 °C
- About 5.7 °C
- About 12.5 °C
Using the EPICA table, how big was the change from 20,000 years ago (−9.4 °C) to the last 1,000 years, by Pia's math?
- About 0.94 °C
- About 18.8 °C
- About 9.4 °C warmer in the last 1,000 years
- About 9.4 °C colder in the last 1,000 years
The table's 140,000- and 128,000-year values lie about 12,000 years apart. What does the change show, by Ren's reading?
- An interglacial warm period giving way to a new ice age
- A change within a single century
- A glacial period giving way to a warm interglacial
- No change in climate
In 1976, Hays and colleagues tested Milankovitch's idea with deep-sea sediment cores (NASA). What did they find, by Tala's reading?
- Ice ages came each year
- Orbital cycles matched major climate changes over 450,000 years
- Orbital cycles had no link to climate
- Tilt by itself explained each ice age, with no help from the other cycles
NASA: about 800,000 years ago ice-age cycles lengthened from 41,000 to 100,000 years. What do scientists say about why, by Zee's reading?
- Earth's tilt stopped changing, so the cycle got longer
- Several ideas exist, but there is no clear answer yet
- It is fully explained
- Precession came to an end
Why can orbital changes that alter sunlight modestly still pace large ice ages, by Ari's reading (NASA)?
Ice sheets reflecting sunlight back to space. Ice sheets reflecting sunlight back to space. Sun sunlight ice sheets space - Orbital changes raise the Sun's output
- Growing ice reflects more sunlight, adding more cooling
- Ice absorbs more sunlight as it grows
- Each ice age lasts a few years