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ACT Science: Conflicting Viewpoints (Drill 5)

Drill 5 · Science · Conflicting Viewpoints

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About This Drill

ACT Science: Conflicting Viewpoints (Drill 5) is a Science practice drill covering Conflicting Viewpoints. It contains 5 original questions created by Brian Stewart, a Barron's test prep author with over 20 years of tutoring experience.

ACT Conflicting Viewpoints questions ask you to analyze and compare two competing explanations. In this drill, two scientists debate the primary driver of Earth's glacial cycles, orbital (Milankovitch) cycles versus atmospheric CO₂ concentration, requiring identification of evidence, assumptions, and evaluation of new data.

Questions & Explanations

Scientists 1 and 2
Over the past 2.6 million years, Earth has cycled between glacial periods (ice ages) and warmer interglacial periods approximately every 100,000 years. Ice cores drilled from Antarctica and Greenland preserve bubbles of ancient atmosphere that allow scientists to reconstruct past temperatures and atmospheric carbon dioxide (CO₂) concentrations. Researchers agree on the following: CO₂ concentrations ranged from approximately 180 parts per million (ppm) during glacial maxima to approximately 280 ppm during interglacials; global average temperatures differed by roughly 4 to 7°C between glacial and interglacial periods; Earth's orbital geometry changes on three well-defined timescales -- eccentricity (~100,000 years), axial tilt or obliquity (~41,000 years), and precession (~23,000 years) -- collectively called Milankovitch cycles; and ice sheets, once formed, reflect sunlight and amplify cooling through a positive feedback called ice-albedo feedback. What drives the initiation and pacing of these glacial cycles is debated. Scientist 1 The primary driver of Earth's glacial cycles is the periodic variation in Earth's orbital geometry -- the Milankovitch cycles. When Earth's orbit, axial tilt, and rotational wobble combine to reduce the amount of summer sunlight reaching high northern latitudes, snow and ice accumulate year over year, initiating glaciation. Spectral analysis of climate records preserved in deep-sea sediments and ice cores reveals cyclical climate variability at periods of approximately 100,000, 41,000, and 23,000 years -- matching precisely the three Milankovitch frequencies. This correspondence between orbital periods and climate cycles is not coincidental: the timing of glacial inceptions and terminations aligns closely with calculated changes in Earth's orbital configuration. Changes in CO₂ and temperature are closely correlated in the ice core record, but CO₂ responds to orbital-driven temperature changes rather than causing them -- it acts as an amplifying feedback rather than the initial trigger. Scientist 2 The primary driver of Earth's glacial cycles is the concentration of atmospheric CO₂. CO₂ is a potent greenhouse gas whose radiative forcing is well-established: each doubling of CO₂ concentration produces a global mean warming of approximately 3°C. The tight correlation between CO₂ and temperature in ice core records reflects a causal relationship: when CO₂ falls, global temperatures drop and ice sheets expand; when CO₂ rises, temperatures increase and ice sheets retreat. While orbital changes modulate the distribution of sunlight, they are insufficient on their own to account for the 4 to 7°C swings between glacial and interglacial states -- the forcing from Milankovitch cycles is too small without the powerful amplification provided by CO₂ and the associated feedbacks of water vapor and ice-albedo. CO₂ changes, driven initially by ocean circulation and carbon cycle processes, set the pace and magnitude of the ice ages. The orbital cycles provide a background rhythm, but CO₂ is the dominant control on glacial climate.

Question 1. Which of the following does Scientist 1 cite as the primary evidence that orbital cycles drive glacial periods?

  • A) Climate records show cyclical variability at periods that match the three Milankovitch frequencies precisely ✓
  • B) CO₂ concentrations were approximately 100 ppm lower during glacial maxima than during interglacials in the data presented
  • C) Each doubling of CO₂ concentration produces a warming of approximately 3°C
  • D) Ice-albedo feedback amplifies the initial cooling caused by CO₂ reduction

Explanation: Scientist 1 states: "Spectral analysis of climate records preserved in deep-sea sediments and ice cores reveals cyclical climate variability at periods of approximately 100,000, 41,000, and 23,000 years -- matching precisely the three Milankovitch frequencies." This pattern match between orbital periods and observed climate cycles is the central evidence for Milankovitch forcing. Option B states a fact both scientists acknowledge but is not Scientist 1's primary argument for orbital driving. Option C is Scientist 2's statement about CO₂ radiative forcing. Option D describes a feedback that Scientist 2 invokes in support of CO₂ forcing.

Scientists 1 and 2
Over the past 2.6 million years, Earth has cycled between glacial periods (ice ages) and warmer interglacial periods approximately every 100,000 years. Ice cores drilled from Antarctica and Greenland preserve bubbles of ancient atmosphere that allow scientists to reconstruct past temperatures and atmospheric carbon dioxide (CO₂) concentrations. Researchers agree on the following: CO₂ concentrations ranged from approximately 180 parts per million (ppm) during glacial maxima to approximately 280 ppm during interglacials; global average temperatures differed by roughly 4 to 7°C between glacial and interglacial periods; Earth's orbital geometry changes on three well-defined timescales -- eccentricity (~100,000 years), axial tilt or obliquity (~41,000 years), and precession (~23,000 years) -- collectively called Milankovitch cycles; and ice sheets, once formed, reflect sunlight and amplify cooling through a positive feedback called ice-albedo feedback. What drives the initiation and pacing of these glacial cycles is debated. Scientist 1 The primary driver of Earth's glacial cycles is the periodic variation in Earth's orbital geometry -- the Milankovitch cycles. When Earth's orbit, axial tilt, and rotational wobble combine to reduce the amount of summer sunlight reaching high northern latitudes, snow and ice accumulate year over year, initiating glaciation. Spectral analysis of climate records preserved in deep-sea sediments and ice cores reveals cyclical climate variability at periods of approximately 100,000, 41,000, and 23,000 years -- matching precisely the three Milankovitch frequencies. This correspondence between orbital periods and climate cycles is not coincidental: the timing of glacial inceptions and terminations aligns closely with calculated changes in Earth's orbital configuration. Changes in CO₂ and temperature are closely correlated in the ice core record, but CO₂ responds to orbital-driven temperature changes rather than causing them -- it acts as an amplifying feedback rather than the initial trigger. Scientist 2 The primary driver of Earth's glacial cycles is the concentration of atmospheric CO₂. CO₂ is a potent greenhouse gas whose radiative forcing is well-established: each doubling of CO₂ concentration produces a global mean warming of approximately 3°C. The tight correlation between CO₂ and temperature in ice core records reflects a causal relationship: when CO₂ falls, global temperatures drop and ice sheets expand; when CO₂ rises, temperatures increase and ice sheets retreat. While orbital changes modulate the distribution of sunlight, they are insufficient on their own to account for the 4 to 7°C swings between glacial and interglacial states -- the forcing from Milankovitch cycles is too small without the powerful amplification provided by CO₂ and the associated feedbacks of water vapor and ice-albedo. CO₂ changes, driven initially by ocean circulation and carbon cycle processes, set the pace and magnitude of the ice ages. The orbital cycles provide a background rhythm, but CO₂ is the dominant control on glacial climate.

Question 2. Which of the following statements would both Scientist 1 and Scientist 2 most likely accept as accurate?

  • A) Milankovitch orbital cycles alone are sufficient to explain the full 4 to 7°C temperature difference between glacial and interglacial periods
  • B) CO₂ is the initial trigger of glacial cycles and orbital changes play no role
  • C) CO₂ concentrations in the atmosphere were lower during glacial periods than during interglacial periods ✓
  • D) Ice-albedo feedback is the primary driver of glacial cycles and operates independently of both CO₂ and orbital changes

Explanation: The intro paragraph establishes as agreed background: "CO₂ concentrations ranged from approximately 180 ppm during glacial maxima to approximately 280 ppm during interglacials." Both scientists build their arguments around this observed CO₂ variation -- Scientist 1 treats it as a consequence of orbital-driven temperature change, while Scientist 2 treats it as the primary cause. Both accept the empirical fact that CO₂ was lower during glacials. Option A is contradicted by Scientist 2, who explicitly states Milankovitch forcing "is too small without the powerful amplification provided by CO₂." Option B is contradicted by Scientist 1 and overstates Scientist 2's position (S2 says orbital cycles "provide a background rhythm"). Option D is not proposed by either scientist -- both treat ice-albedo as a feedback, not a primary driver.

Scientist 1
Over the past 2.6 million years, Earth has cycled between glacial periods (ice ages) and warmer interglacial periods approximately every 100,000 years. Ice cores drilled from Antarctica and Greenland preserve bubbles of ancient atmosphere that allow scientists to reconstruct past temperatures and atmospheric carbon dioxide (CO₂) concentrations. Researchers agree on the following: CO₂ concentrations ranged from approximately 180 parts per million (ppm) during glacial maxima to approximately 280 ppm during interglacials; global average temperatures differed by roughly 4 to 7°C between glacial and interglacial periods; Earth's orbital geometry changes on three well-defined timescales -- eccentricity (~100,000 years), axial tilt or obliquity (~41,000 years), and precession (~23,000 years) -- collectively called Milankovitch cycles; and ice sheets, once formed, reflect sunlight and amplify cooling through a positive feedback called ice-albedo feedback. What drives the initiation and pacing of these glacial cycles is debated. Scientist 1 The primary driver of Earth's glacial cycles is the periodic variation in Earth's orbital geometry -- the Milankovitch cycles. When Earth's orbit, axial tilt, and rotational wobble combine to reduce the amount of summer sunlight reaching high northern latitudes, snow and ice accumulate year over year, initiating glaciation. Spectral analysis of climate records preserved in deep-sea sediments and ice cores reveals cyclical climate variability at periods of approximately 100,000, 41,000, and 23,000 years -- matching precisely the three Milankovitch frequencies. This correspondence between orbital periods and climate cycles is not coincidental: the timing of glacial inceptions and terminations aligns closely with calculated changes in Earth's orbital configuration. Changes in CO₂ and temperature are closely correlated in the ice core record, but CO₂ responds to orbital-driven temperature changes rather than causing them -- it acts as an amplifying feedback rather than the initial trigger.

Question 3. Which of the following findings, if confirmed, would most weaken Scientist 1's hypothesis?

  • A) Ice core records from multiple sites all show CO₂ and temperature rising and falling together across glacial cycles
  • B) Among the three Milankovitch cycles, the eccentricity cycle (~100,000 years) produces the smallest change in total solar energy received by Earth, yet corresponds to the dominant and strongest glacial rhythm in recent Earth history ✓
  • C) Ice-albedo feedback amplifies the initial cooling or warming caused by orbital forcing
  • D) The obliquity cycle of ~41,000 years dominated glacial pacing before approximately 1 million years ago

Explanation: Scientist 1's hypothesis requires that orbital forcing drives glacial cycles. The eccentricity cycle (~100,000 years) produces a very small change in total solar insolation -- far smaller than the obliquity or precession cycles -- yet the 100,000-year cycle is the dominant feature of the glacial record over the past 800,000 years. This mismatch -- the weakest orbital forcing producing the strongest climate response -- is a genuine challenge to pure Milankovitch forcing and suggests that another amplifier (such as CO₂) must be primarily responsible for the magnitude and timing of glacial cycles. Option A shows CO₂-temperature correlation, which Scientist 1 already acknowledges and interprets as CO₂ being a feedback, not a weakness. Option C describes ice-albedo feedback, which Scientist 1 could incorporate into an orbital forcing model. Option D actually supports Milankovitch theory by showing a different orbital cycle (obliquity) dominated at a different time, consistent with changing orbital configurations.

Scientist 2
Over the past 2.6 million years, Earth has cycled between glacial periods (ice ages) and warmer interglacial periods approximately every 100,000 years. Ice cores drilled from Antarctica and Greenland preserve bubbles of ancient atmosphere that allow scientists to reconstruct past temperatures and atmospheric carbon dioxide (CO₂) concentrations. Researchers agree on the following: CO₂ concentrations ranged from approximately 180 parts per million (ppm) during glacial maxima to approximately 280 ppm during interglacials; global average temperatures differed by roughly 4 to 7°C between glacial and interglacial periods; Earth's orbital geometry changes on three well-defined timescales -- eccentricity (~100,000 years), axial tilt or obliquity (~41,000 years), and precession (~23,000 years) -- collectively called Milankovitch cycles; and ice sheets, once formed, reflect sunlight and amplify cooling through a positive feedback called ice-albedo feedback. What drives the initiation and pacing of these glacial cycles is debated. Scientist 2 The primary driver of Earth's glacial cycles is the concentration of atmospheric CO₂. CO₂ is a potent greenhouse gas whose radiative forcing is well-established: each doubling of CO₂ concentration produces a global mean warming of approximately 3°C. The tight correlation between CO₂ and temperature in ice core records reflects a causal relationship: when CO₂ falls, global temperatures drop and ice sheets expand; when CO₂ rises, temperatures increase and ice sheets retreat. While orbital changes modulate the distribution of sunlight, they are insufficient on their own to account for the 4 to 7°C swings between glacial and interglacial states -- the forcing from Milankovitch cycles is too small without the powerful amplification provided by CO₂ and the associated feedbacks of water vapor and ice-albedo. CO₂ changes, driven initially by ocean circulation and carbon cycle processes, set the pace and magnitude of the ice ages. The orbital cycles provide a background rhythm, but CO₂ is the dominant control on glacial climate.

Question 4. Scientist 2 argues that CO₂ is the primary driver of glacial cycles. This argument assumes which of the following?

  • A) Earth's orbital geometry does not change over the timescales relevant to glacial cycles
  • B) CO₂ concentrations were identical during all glacial periods regardless of orbital configuration
  • C) A greenhouse gas can function as the primary driver of a climate cycle even if its atmospheric concentration initially changes in response to temperature rather than causing the temperature change ✓
  • D) Ice-albedo feedback operates only when CO₂ concentrations are below 200 ppm

Explanation: High-precision ice core analyses show that temperature begins rising approximately 800 years before CO₂ concentrations increase at each glacial termination. This means CO₂ initially responds to warming (likely released from the ocean as it warms) rather than triggering it. For Scientist 2's CO₂-as-primary-driver hypothesis to hold despite this timing, Scientist 2 must assume that even if CO₂ initially responds to temperature, it can still amplify and sustain the cycle powerfully enough to be considered the dominant causal factor -- in other words, that being an initial feedback does not disqualify CO₂ from being the primary driver. Option A is false and contradicted by both scientists, who acknowledge Milankovitch cycles exist. Option B is not claimed and would be false. Option D introduces a specific threshold not stated or implied by either scientist.

Scientists 1 and 2
Over the past 2.6 million years, Earth has cycled between glacial periods (ice ages) and warmer interglacial periods approximately every 100,000 years. Ice cores drilled from Antarctica and Greenland preserve bubbles of ancient atmosphere that allow scientists to reconstruct past temperatures and atmospheric carbon dioxide (CO₂) concentrations. Researchers agree on the following: CO₂ concentrations ranged from approximately 180 parts per million (ppm) during glacial maxima to approximately 280 ppm during interglacials; global average temperatures differed by roughly 4 to 7°C between glacial and interglacial periods; Earth's orbital geometry changes on three well-defined timescales -- eccentricity (~100,000 years), axial tilt or obliquity (~41,000 years), and precession (~23,000 years) -- collectively called Milankovitch cycles; and ice sheets, once formed, reflect sunlight and amplify cooling through a positive feedback called ice-albedo feedback. What drives the initiation and pacing of these glacial cycles is debated. Scientist 1 The primary driver of Earth's glacial cycles is the periodic variation in Earth's orbital geometry -- the Milankovitch cycles. When Earth's orbit, axial tilt, and rotational wobble combine to reduce the amount of summer sunlight reaching high northern latitudes, snow and ice accumulate year over year, initiating glaciation. Spectral analysis of climate records preserved in deep-sea sediments and ice cores reveals cyclical climate variability at periods of approximately 100,000, 41,000, and 23,000 years -- matching precisely the three Milankovitch frequencies. This correspondence between orbital periods and climate cycles is not coincidental: the timing of glacial inceptions and terminations aligns closely with calculated changes in Earth's orbital configuration. Changes in CO₂ and temperature are closely correlated in the ice core record, but CO₂ responds to orbital-driven temperature changes rather than causing them -- it acts as an amplifying feedback rather than the initial trigger. Scientist 2 The primary driver of Earth's glacial cycles is the concentration of atmospheric CO₂. CO₂ is a potent greenhouse gas whose radiative forcing is well-established: each doubling of CO₂ concentration produces a global mean warming of approximately 3°C. The tight correlation between CO₂ and temperature in ice core records reflects a causal relationship: when CO₂ falls, global temperatures drop and ice sheets expand; when CO₂ rises, temperatures increase and ice sheets retreat. While orbital changes modulate the distribution of sunlight, they are insufficient on their own to account for the 4 to 7°C swings between glacial and interglacial states -- the forcing from Milankovitch cycles is too small without the powerful amplification provided by CO₂ and the associated feedbacks of water vapor and ice-albedo. CO₂ changes, driven initially by ocean circulation and carbon cycle processes, set the pace and magnitude of the ice ages. The orbital cycles provide a background rhythm, but CO₂ is the dominant control on glacial climate.

Question 5. High-precision analysis of an Antarctic ice core reveals that at each of the last eight glacial terminations, Antarctic temperature began rising approximately 800 years before atmospheric CO₂ concentrations increased. This finding most strongly supports the hypothesis of:

  • A) Scientist 1 only, because the temperature increase precedes the CO₂ increase, suggesting CO₂ is responding to an earlier warming trigger rather than causing it ✓
  • B) Scientist 2 only, because the close timing of temperature and CO₂ confirms that CO₂ is driving temperature
  • C) Both scientists equally, because both predict a tight correlation between CO₂ and temperature
  • D) Neither scientist, because neither hypothesis makes a prediction about the relative timing of temperature and CO₂ changes

Explanation: If temperature rises approximately 800 years before CO₂ at every glacial termination, then CO₂ cannot be the initial trigger of warming -- something else must warm the planet first, and CO₂ then rises in response (likely as oceans warm and release dissolved CO₂). This is precisely what Scientist 1 predicts: orbital changes drive initial warming, and CO₂ "acts as an amplifying feedback rather than the initial trigger." This temporal ordering supports Scientist 1's causal framework. Scientist 2's hypothesis that CO₂ drives temperature is directly challenged -- if CO₂ comes after temperature, it could not have caused the temperature rise that preceded it. Option B misrepresents the finding: a lag of CO₂ behind temperature is the opposite of what a CO₂-driven hypothesis predicts. Option C is wrong because the finding specifically addresses the causal order, where the two scientists differ.