Best & Worst-Case Scenarios for the College Football Playoff Rankings

The first College Football Playoff Rankings will be released on Tuesday at 5 PM Mountain Time. For the first time in program history, BYU will be ranked in the CFP rankings. The rankings started in 2014 when the CFP was created. Today, let’s look at the best-case scenarios and the worst-case scenarios for BYU when the CFP rankings are released on Tuesday night. 

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Worst-Case Scenario

A few weeks ago, we looked back at all initial CFP rankings dating back to 2014 and compared them to the AP polls. The initial CFP rankings were mostly consistent with the AP polls, with one exception: the CFP ranked non-P5 teams lower than the AP poll. Since 2014, at least one non-P5 team dropped three or more spots in the first CFP ranking compared to the AP poll. Memphis in 2015 was the only non-P5 team whose ranking improved – they went from #15 in the AP poll to #13 in the CFP rankings.

Perhaps the most comparable team to BYU is the 2018 UCF team. UCF was 7-0 and ranked #9 in the AP when the first CFP rankings were released. In the first CFP ranking, the Knights were ranked #12. The Knights eventually climbed up to #8, the highest a non-P5 team has ever been ranked.

The worst-case scenario for BYU would include teams like Miami, Northwestern, Indiana or even Oklahoma surpassing the Cougars in the rankings.

Worst-case scenario ranking: #12

Best-Case Scenario

Seven teams are ranked in front of BYU in the AP poll: Alabama, Ohio State, Notre Dame, Clemson, Texas A&M, Florida, and Cincinnati. Of that list, it seems like Cincinnati is the only team that BYU could potentially leapfrog on Tuesday. That feels unlikely, however, as the Bearcats are fresh off a big road victory over UCF.

Best-case scenario ranking: #7

Most Likely

History suggests that at least one P5 team will surpass BYU in the CFP rankings. Miami, Indiana, and Northwestern are the most likely candidates. 

Most likely ranking: #9

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Dinosaur Asteroid Hit Worst-Case Place

We all know the story: 66 million years ago, a giant asteroid crashed into Earth, killing off three quarters of all species, including most of the dinosaurs. Researchers suspect that the impact caused the extinction by kicking up a cloud of dust and tiny droplets called aerosols that plunged the planet into something like a nuclear winter.

“These components in the atmosphere drove global cooling and darkness that would have stopped photosynthesis from occurring, ultimately shutting down the food chain.”

Shelby Lyons, a recent Ph.D. graduate from Penn State University.

But scientists have also found lots of soot in the geologic layers deposited immediately after the asteroid impact. And the soot may have been part of the killing mechanism too—depending on where it came from.

Some of the soot probably came from wildfires that erupted around the planet following the impact. But most of these particles would have lingered in the lower atmosphere for only a few weeks and wouldn’t have had much of an effect on global climate.

But scientists hypothesize that soot may also have come from the very rocks that the asteroid pulverized when it struck. If those rocks contained significant amounts of organic matter—such as the remains of marine organisms—it would have burned up on impact, sending soot shooting up into the stratosphere. In that case, soot would have spread around the globe in a matter of hours and stayed there for years. And it would have radically altered Earth’s climate.

So Lyons and her team set out to identify the source of the soot. They looked at chemicals known as polycyclic aromatic hydrocarbons, or PAHs, which are another by-product of combustion.

“You can find PAHs in meat or veggies that you grill. You can find them from the exhaust of a car. You can also find them in smoke and debris from the wildfires today out west.”

PAHs are made up of fused rings of carbon atoms—think of chicken wire. To determine the origin of the soot, the researchers looked at the structure and chemistry of the PAHs buried along with it. Specifically, the researchers looked for groups of atoms that stick off the rings like spikes. PAHs generated from burning wood don’t have many spikes, but PAHs from burning fossil carbon—like what would have been in the target rocks—have more.

Lyons and her team found that most of the PAHs deposited after the impact were spiky, which suggests that soot from the rocks hit by the asteroid played a major role in the mass extinction.

“There was more dust and more sulfate aerosols than soot, but soot is a stronger blocker of sunlight than either of those two. So a small amount of soot can drive large reductions in sunlight.”

The findings are in the Proceedings of the National Academy of Sciences. [Shelby L. Lyons et al., Organic matter from the Chicxulub crater exacerbated the K–Pg impact winter]

The results suggest that the devastation of this very sooty asteroid impact may be due

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