Why It’s Going To Get Hot And Dry All Over At The Same Time

Why It’s Going To Get Hot And Dry All Over At The Same Time

The kind of hot, dry conditions that can shrink crop yields, destabilize food prices, and lay the groundwork for devastating wildfires are increasingly striking multiple regions simultaneously as a result of a warming climate, according to a new study.

Climate change has doubled the odds that a region will suffer a year that is both warm and dry compared to the average for that place during the middle of the 20th century, the researchers report. It’s also becoming more likely that dry and severely warm conditions will hit key agricultural regions in the same year, potentially making it harder for surpluses in one location to compensate for low yields in another.

“When we look in the historical data at the key crop and pasture regions, we find that before anthropogenic climate change, there were very low odds that any two regions would experience those really severe conditions simultaneously,” says climate scientist Noah Diffenbaugh, a professor in the School of Earth, Energy & Environmental Sciences at Stanford University and senior author of the paper, which appears in Science Advances.

“The global marketplace provides a hedge against localized extremes, but we’re already seeing an erosion of that climate buffer as extremes have increased in response to global warming,” Diffenbaugh says.

Why It’s Going To Get Hot And Dry All Over At The Same TimeBefore anthropogenic climate change, there were very low odds that any two key crop or pasture regions would experience severe heat and dry conditions simultaneously. (Credit: Diffenbaugh Lab/Stanford)

Smaller harvests

The new study points to a future in which multiple regions are at risk of experiencing low crop yields simultaneously. That’s because, while some crops can thrive in a warm growing season, others—particularly grains—grow and mature too quickly when temperatures rise, consecutive dry days pile up, and warmth persists overnight.

As a result, hot-dry conditions tend to produce smaller harvests of major commodities, including wheat, rice, corn, and soybeans.

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“When these extremes occur simultaneously, it exacerbates the adverse impacts beyond what any of them would have caused separately.”

The implications extend beyond agriculture. Those same hot, dry conditions can also exacerbate fire risk, drying out vegetation in the summer and autumn and fueling intense, fast-spreading wildfires like those that burned through more than 240,000 acres in California in November 2018.

The basic trend of global warming—1 degree Celsius or 1.8 degrees Fahrenheit since the late 19th century—lends an intuitive logic to the study’s core findings.

“If it’s getting warmer everywhere, then it’s more likely to be hot in two places at once, and it’s probably also more likely to be hot when it’s also dry in two places at once,” Diffenbaugh says

Double trouble

Despite that simple intuition, accounting for ongoing, interdependent changes in both precipitation and temperature in different locations through time presents a statistical challenge. As a result, many past analyses have looked at warm and dry events as independent phenomena, or at different regions as independent from one another.

That approach may underestimate the added risk due to human-caused global warming, as well as the social, ecological, and economic benefits of curbing emissions.

“When these extremes occur simultaneously, it exacerbates the adverse impacts beyond what any of them would have caused separately,” says lead author Ali Sarhadi, a postdoctoral scholar in Diffenbaugh’s Climate and Earth System Dynamics Group.

Researchers used historical data from the past century to quantify the odds that different regions experience hot and dry conditions in the same year. Before 1980, there was less than a 5 percent chance that two region pairs would experience extreme temperatures in a year that was also dry in both regions. However, in the past two decades, the odds have increased to as much as 20 percent for some region pairs.

For example, the odds that China and India—two of the world’s largest agricultural producers and the two most populous nations—both experience low precipitation and extremely warm temperatures in the same year were less than 5 percent before 1980 but are more than 15 percent today, Diffenbaugh says.

“So, what used to be a rare occurrence can now be expected to occur with some regularity, and we have very strong evidence that global warming is the cause,” he explains.

Climate agreement

The authors also analyzed climate model projections of possible future global warming scenarios and found that within a few decades, if the world continues on its current emissions trajectory, the odds that average temperatures will rise well beyond the range normally experienced in the middle of the 20th century could climb upward of 75 percent in many regions.

Achieving the goals the United Nations’ Paris climate agreement outlined is likely to substantially reduce those risks, Sarhadi says. While the White House has announced its intention to withdraw the United States from the agreement, achieving the emissions reduction targets in the 200-nation pact would allow the world to dramatically reduce the likelihood of compounding hot, dry conditions hitting multiple croplands across the world.

“There are still options for mitigating these changes,” he says.

Future risk

The framework built for this study represents a vital step in pinning down the risk associated with multiple climate extremes coming together in one region, where they can often compound one another.

What were the chances, for example, that high temperatures, high winds, and low humidity combined to create mega fire conditions in the past, and how have those odds changed as a result of global warming? That’s the sort of question the team’s framework will be able to answer. It’s a gravely urgent one for officials now reckoning with fires of historic scale and intensity in California.

“A lot of the events that stress infrastructure, and our disaster prevention and response systems, occur when multiple ingredients come together in the same place at the same time,” Diffenbaugh says.

High storm surges and wind speeds with heavy rain can make the difference between a passing storm and a calamitous tropical cyclone; wind patterns and moisture levels in different parts of the atmosphere influence the severity of a rainstorm and associated flood risk.

A key challenge for decision-makers is understanding what to expect in a changing climate. That means honing in on joint probabilities, which are at the core of calculations that engineers, policy-makers, humanitarian aid providers, and insurers use to allocate resources, set building codes, and design evacuation plans and other disaster responses.

“People are making practical decisions based on the probabilities of different combinations of conditions,” Diffenbaugh says. “The default is to use the historical probabilities, but our research shows that assuming that those historical probabilities will continue into the future doesn’t accurately reflect the current or future risk.”

The Department of Energy and Stanford University funded the work.

Source: Stanford University

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