C264 Climate Change

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Free C264 Climate Change Questions

1.

Explain how the likelihood of extreme warm summer temperatures in the Northern Hemisphere changed from the period of 1951 to 1980 compared to 2005 to 2015.

  • It remained the same.

  • It decreased significantly.

  • It increased dramatically.

  • It fluctuated without a clear trend.

Explanation

Explanation:

Studies of temperature records show that the frequency of extremely warm summer temperatures in the Northern Hemisphere has increased sharply since the mid-20th century. Between 1951 and 1980, such extreme events were relatively rare, but by 2005–2015, their likelihood had risen several times over due to global warming driven by greenhouse gas emissions. This dramatic increase reflects a shifting baseline, meaning what was once considered an exceptional heat event is becoming much more common.

Correct Answer:

It increased dramatically.

Why Other Options Are Wrong:

It remained the same.

This is incorrect because observational data clearly show a strong upward trend in the frequency of extreme heat events, not stability.

It decreased significantly.

The opposite is true; the chance of extreme warm summers has risen, not fallen.

It fluctuated without a clear trend.

Although there is natural variability year to year, the long-term trend shows a clear and pronounced increase rather than random fluctuation.


2.

Why is carbon dioxide the most important increasing greenhouse gas in terms of its effect on global warming?

  • Chlorine atoms released by carbon dioxide catalyze the breakdown of ozone.

  • Carbon dioxide is the only greenhouse gas.

  • Its concentration in the atmosphere has steadily increased since the 1950s.

  • It is disappearing from the atmosphere at an alarming rate.

Explanation

Explanation:

Carbon dioxide (CO₂) is the most significant greenhouse gas driving current climate change because its atmospheric concentration has risen steadily since the industrial revolution, particularly from the 1950s onward, largely due to fossil fuel combustion and deforestation. CO₂ has a long atmospheric lifetime, allowing it to accumulate and exert a persistent warming effect. Although other greenhouse gases like methane and nitrous oxide are potent, CO₂ is more abundant and contributes the largest share to human-induced radiative forcing. This steady rise and its capacity to trap heat make it the principal driver of global warming.

Correct Answer:

Its concentration in the atmosphere has steadily increased since the 1950s.

Why Other Options Are Wrong:

Chlorine atoms released by carbon dioxide catalyze the breakdown of ozone. Carbon dioxide does not release chlorine atoms and is not directly responsible for ozone depletion. Ozone depletion is primarily linked to chlorofluorocarbons (CFCs) and related halogenated compounds. While CO₂ contributes to greenhouse warming, its chemical behavior is distinct from the ozone-destroying reactions driven by chlorine and bromine compounds. Confusing CO₂ with CFCs mixes two separate environmental issues: greenhouse-driven warming and ozone layer thinning.

Carbon dioxide is the only greenhouse gas. This is inaccurate because several other greenhouse gases—such as methane, nitrous oxide, and water vapor—also trap heat in the atmosphere. Although CO₂ is the most important in terms of total contribution to recent warming, the climate system is influenced by a complex mix of gases. Neglecting these others oversimplifies the greenhouse effect and ignores critical contributors like methane, which has a stronger heat-trapping ability per molecule.

It is disappearing from the atmosphere at an alarming rate. The opposite is true. Carbon dioxide is accumulating, not disappearing, and current levels are the highest in at least 800,000 years. Measurements at observatories like Mauna Loa show a continuous upward trend. Suggesting a disappearance misrepresents decades of consistent observational data and undermines the understanding of CO₂’s role in ongoing climate change.


3.

Explain how warming sea water contributes to sea level rise.
 

  • It causes the water to evaporate more quickly.

  • It leads to the melting of polar ice caps.

  • It results in thermal expansion of the water.

  • It increases the salinity of the ocean.

Explanation

Explanation:

As ocean water warms, it expands in volume—a process known as thermal expansion. This expansion is a direct and significant contributor to global sea level rise, independent of the melting of land ice. While melting glaciers and ice sheets also add water to the oceans, thermal expansion from rising ocean temperatures accounts for a substantial portion of the observed sea level increase.

Correct Answer:

It results in thermal expansion of the water.

Why Other Options Are Wrong:

It causes the water to evaporate more quickly.

Although evaporation rates can increase slightly with warmer temperatures, this does not directly cause long-term global sea level rise because the water cycle balances evaporation with precipitation.

It leads to the melting of polar ice caps.

Melting of polar ice adds to sea level, but the question asks specifically how warming sea water itself raises sea level, which is through expansion, not melting distant ice.

It increases the salinity of the ocean.

Warmer water does not inherently increase salinity; in fact, increased ice melt and precipitation can reduce salinity in some areas.


4.

How much mass has the Greenland ice sheet lost since 2002?

  • 2,500 Gt

  • 4,000 Gt

  • 6,500 Gt

  • 1,000 Gt

Explanation

Explanation:

Satellite measurements from NASA’s GRACE (Gravity Recovery and Climate Experiment) and follow-up missions show that the Greenland ice sheet has been losing ice at an accelerating rate since the early 2000s. Cumulative losses from 2002 through the mid-2010s to early 2020s are estimated at roughly 4,000 gigatons (Gt) of ice. This massive loss contributes directly to global sea level rise and reflects the sensitivity of the Greenland ice sheet to warming air and ocean temperatures.

Correct Answer:

4,000 Gt

Why Other Options Are Wrong:

2,500 Gt

This underestimates the observed loss, which exceeds this value according to long-term satellite data.

6,500 Gt

This is higher than current published estimates for the period since 2002, so it overstates the measured loss.

1,000 Gt

This is far too low and does not reflect the substantial and well-documented mass loss from Greenland in the past two decades.


5.

The Earth's atmosphere warmed by about 1ºC over the last 100 years. What rate of change is considered to be normal (natural) warming?

  • 1º to 2ºC per 1000 years

  • 2º to 5ºC per 1000 years

  • 5º to 10ºC per 1000 years

  • 1º to 2ºC per 100 years

Explanation

Explanation:

Natural climate changes in Earth’s history, such as those following ice ages or during gradual interglacial periods, have typically occurred over thousands of years. Paleoclimate records from ice cores and sediment data show that natural warming events usually proceed at a pace of about 1º to 2ºC over an entire millennium. The observed 1ºC rise in just the last century is therefore about ten times faster than the natural background rate, underscoring the influence of human activities like fossil fuel combustion and deforestation.

Correct Answer:

1º to 2ºC per 1000 years

Why Other Options Are Wrong:

2º to 5ºC per 1000 years

This overestimates the natural warming rate. While abrupt climate events such as the end of the last ice age included brief regional spikes, the global average natural trend is closer to 1º to 2ºC per 1000 years. Suggesting 2º to 5ºC as the norm implies a speed of warming that is inconsistent with long-term paleoclimate evidence.

5º to 10ºC per 1000 years

This is far too high for natural conditions. A rate of 5º to 10ºC per millennium would represent an extreme and unprecedented pace outside of catastrophic events like massive volcanic activity or asteroid impacts, which are not considered part of normal background climate change.

1º to 2ºC per 100 years

This rate aligns more closely with the modern human-driven warming we are observing now, not the natural background rate. The fact that we have seen about 1ºC of warming in a single century highlights how current climate change is far more rapid than the natural pace of Earth’s historical climate shifts.


6.

What is the primary purpose of using weather symbols in meteorology?

  • To indicate temperature variations

  • To represent different weather conditions on maps

  • To measure atmospheric pressure

  • To predict future climate changes

Explanation

Explanation:

Weather symbols are standardized graphical representations used on weather maps and forecasts to convey complex meteorological information quickly and clearly. These symbols show conditions such as rain, snow, fog, thunderstorms, and wind direction, enabling meteorologists and the public to interpret current and predicted weather at a glance. Their purpose is communication and visualization, not direct measurement or long-term climate prediction.

Correct Answer:

To represent different weather conditions on maps

Why Other Options Are Wrong:

To indicate temperature variations

While weather maps often include temperature data, symbols are not primarily used to show temperature changes. Temperature is typically represented by numbers or color gradients, not the general weather symbols used for conditions like rain or snow.

To measure atmospheric pressure

Measuring atmospheric pressure requires instruments like barometers. Weather symbols may depict pressure patterns on a map, but they do not measure or directly indicate pressure themselves.

To predict future climate changes

Weather symbols are tools for depicting short-term weather conditions, not for forecasting long-term climate trends. Climate change studies rely on extensive data analysis and modeling, not simple symbolic representations on a weather map.


7.

Prevailing wind months in the Philippines: Amihan (NE)

  • May to October

  • January to June

  • July to December

  • November to April

Explanation

Explanation:

The Amihan is the cool northeast monsoon that brings dry winds to the Philippines. It typically begins around late October or early November and lasts until about April, dominating the country’s weather during the cooler, drier season. This pattern is well documented in Philippine meteorology and is associated with winds originating from the northeast that bring lower humidity and relatively cooler temperatures compared to the wet southwest monsoon (Habagat).

Correct Answer:

November to April

Why Other Options Are Wrong:

May to October. This period corresponds to the Habagat, the southwest monsoon that brings warm, moist air and heavy rainfall, the opposite of the cool, dry Amihan conditions. Associating Amihan with this wet season ignores the established timing of monsoon patterns in the Philippines.

January to June. Although January through April falls within the Amihan season, extending it to June is inaccurate because by May the southwest monsoon is already beginning to dominate, shifting winds and increasing rainfall.

July to December. The early part of this span (July to October) is firmly within the Habagat rainy season. While November and December mark the onset of Amihan, placing the entire range from July is misleading and does not match the climatological record.


8.

What effect has the global warming trend had on the likelihood of extreme cold temperatures?

  • Increased the likelihood of extreme cold temperatures

  • Decreased the likelihood of extreme cold temperatures

  • Had no effect on extreme cold temperatures

  • Made extreme cold temperatures more common in the Northern Hemisphere

Explanation

Explanation:

Global warming raises the average temperature of the atmosphere and oceans, which reduces the probability of extremely cold events. While occasional cold outbreaks can still occur due to natural variability and shifting jet stream patterns, their frequency and severity have decreased over the past several decades. Observational data and climate models consistently show a decline in the occurrence of extreme cold spells as global mean temperatures rise, even as heat waves become more common and intense.

Correct Answer:

Decreased the likelihood of extreme cold temperatures

Why Other Options Are Wrong:

Increased the likelihood of extreme cold temperatures. This contradicts well-documented global temperature records and climate projections, which show fewer and less severe extreme cold events overall as greenhouse gas concentrations rise.

Had no effect on extreme cold temperatures. Evidence shows a clear downward trend in extreme cold events globally. Claiming no effect overlooks the statistically significant changes identified in multiple climate studies.

Made extreme cold temperatures more common in the Northern Hemisphere. Although occasional polar vortex disruptions can lead to cold snaps, these are isolated events within a broader pattern of warming. The long-term data demonstrate an overall decrease, not an increase, in extreme cold in the Northern Hemisphere.


9.

Explain why certain regions of Earth may show more obvious changes due to climate change compared to others.

  • Some regions have more extreme weather patterns.

  • Changes are only visible in urban areas.

  • All regions are affected equally by climate change.

  • Only polar regions are changing.

Explanation

Explanation:

Climate change does not affect every part of Earth uniformly. Local factors such as geography, ocean currents, prevailing winds, and feedback mechanisms cause certain areas to warm or experience altered precipitation patterns more dramatically than others. For example, polar regions warm faster because of the ice–albedo feedback, while low-lying coastal areas are more vulnerable to sea level rise. Mountain regions may show greater changes in snowpack and glacier retreat. These variations mean that climate impacts are unevenly distributed across the planet.

Correct Answer:

Some regions have more extreme weather patterns.

Why Other Options Are Wrong:

Changes are only visible in urban areas.

Although cities can experience heat islands that intensify warming, climate change is a global phenomenon affecting rural, oceanic, and wilderness regions as well. Limiting visible changes to urban settings ignores widespread evidence of shifting ecosystems, melting glaciers, and altered rainfall patterns in remote areas far from cities. Urbanization can amplify local effects, but it is not the only place where changes are measurable or obvious.

All regions are affected equally by climate change.

This is inaccurate because extensive data show that warming and precipitation shifts vary widely across regions. The Arctic warms about twice as fast as the global average, while some oceanic regions warm more slowly. Differences in altitude, ocean currents, and local climate systems mean that climate change impacts are highly uneven. Therefore, it is incorrect to claim equal effects everywhere.

Only polar regions are changing.

Polar regions indeed warm rapidly, but they are not the only places showing clear signs of climate change. Tropical coral reefs are bleaching, droughts are intensifying in subtropical zones, and monsoon patterns are shifting in Asia and Africa. Focusing solely on the poles disregards significant and well-documented changes in temperate and tropical areas.


10.

Since what year have the Greenland and Antarctic ice sheets been observed to be melting?

  • 1990

  • 2000

  • 2002

  • 2010

Explanation

Explanation:

Comprehensive satellite observations began in 2002 with the launch of NASA’s GRACE (Gravity Recovery and Climate Experiment) mission. These satellites provided precise measurements of changes in the mass of the Greenland and Antarctic ice sheets, revealing a consistent and accelerating trend of ice loss from that point onward. While some evidence of earlier melting exists from field studies, 2002 marks the start of continuous, global-scale monitoring that conclusively documents their sustained melt.

Correct Answer:

2002

Why Other Options Are Wrong:

1990. Although some regional studies detected signs of ice loss before the 2000s, there was no comprehensive, high-precision satellite monitoring of total ice sheet mass in 1990. The ability to measure widespread melting with confidence began later with dedicated satellite missions, so 1990 cannot be cited as the definitive observational start.

2000. By 2000, satellite technology had advanced, but systematic, large-scale measurements of the ice sheets’ mass changes were not yet in place. Observations before 2002 lacked the resolution and global coverage needed to accurately quantify melt rates, making 2000 premature for reliable, continuous records.

2010. Waiting until 2010 overlooks nearly a decade of confirmed data showing substantial mass loss in both Greenland and Antarctica. GRACE satellites had already documented significant melting trends well before 2010, so this date understates the length and extent of observed ice sheet decline.


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