Why This Weekend's Record Flooding in Louisiana Was So Extreme

An aerial photo of Hammond, Louisiana on Saturday. Image: AP
An aerial photo of Hammond, Louisiana on Saturday. Image: AP

Historic, record flooding gripped southeastern Louisiana this weekend after neighborhoods from Baton Rouge to Livingston were swamped under an absolute torrent of rainfall. As of this morning, 20,000 people have been rescued from their homes, and the danger is far from over.

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Meteorologically speaking, this event has been unfolding for more than a week, thanks to a slow-moving, low-pressure tropical air mass fed by high sea surface temperatures, and record humidity. All of these factors should be taken in the context of climate change, which is making extreme single-day rainfall events and catastrophic floods more likely.

More on climate later—let’s start with the basics. It’s mid-summer and the Gulf of Mexico is hot. Last week, sea surface temperatures in the eastern Gulf skirted an all-time record high of 90 degrees Fahrenheit (32 degrees Celsius); up to five degrees warmer than usual for this time of the year.

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Image: National Hurricane Center/NOAA
Image: National Hurricane Center/NOAA

Put heat and water together, and you get evaporation. The dew point, or temperature at which water vapor condenses, has been hovering oppressively close to the temperature of the ocean itself, meaning water is simply pouring into the atmosphere. Weather Underground meteorologist Jeff Masters noted that “precipitable water”—the amount of water in the atmosphere from the surface to the jet stream—was in the top percentile of historic values along the Gulf Coast last week. Meteorologist Eric Holthaus noted that a weather balloon measured near-record levels of moisture over New Orleans on Friday.

High temperatures and high humidity create the ideal environment for very wet storm systems to develop, and last week nature obliged. “This isn’t a terribly atypical pattern,” Mark Hoekzema, chief meteorologist at Earth Networks, told Gizmodo. “This time of year, tropical easterlies give us these tropical waves that march across the Caribbean, drifting northward onto the US coast.”

Hoekzema explained that when a few of these low-pressure air masses crossed Florida and entered the Gulf Coast region last week, they essentially became trapped. “You had a couple of these systems stall out on the Gulf Coast,” he said. “With very slow movement, you can get excessive amount of rain.”

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While technically not a tropical cyclone, the storm system shared some physical characteristics with hurricanes, including counter-clockwise rotation that allowed it to pull loads of moisture inland from the Gulf of Mexico. The result was a volley of torrential downpours—up to several inches per hour—with some parts of Louisiana clocking 24-hour precipitation totals that exceed the 500 year recurrence interval. We’re talking levels of rainfall that, statistically speaking, occur every thousand years or so.

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Rainfall totals over Louisiana for the past three days. Image: NWS/NOAA
Rainfall totals over Louisiana for the past three days. Image: NWS/NOAA

All in all, between last Tuesday and this morning, neighborhoods around Livingston and Baton Rouge saw more than two feet of precipitation. The especially hard-hit community of Watson picked up more rainfall in the past few days than Los Angeles has seen since 2012.

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With torrential rain came flooding. Rivers in southeastern Louisiana rose rapidly on Friday and over the weekend, with at least nine river gauges setting new record highs. In Denham Springs, the Amite River gauge bested the historic high set during a 1983 flood event by more than five feet. As neighborhoods were inundated, tens of thousands of residents were forced to evacuate their homes.

While the weather is now improving, certain flooded river sections aren’t expected to crest until later today. “We are not in control as far as how fast these floodwaters will recede, and in fact they are still going up in some places,” Louisiana state governor John Bel Edwards said.

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Image: NWS/NOAA
Image: NWS/NOAA

The situation is no doubt exceptional—but the flooding in Louisiana is also a clear example of something we can expect to see more often as greenhouse gases heat up our planet’s atmosphere, allowing it to hold and dump more water. As an analysis by Climate Signals notes, the United States has seen a 20 percent uptick in the amount of precipitation falling in the heaviest downpours over the past century. Torrential, single-day storm events are on the rise, particularly in the southeastern United States, where the frequency of extreme rainfall has risen nearly 30 percent since the late 1950s.

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Meteorologists like to say that no single weather event can be tied to climate change. But in year that has brought a historic, $22 billion dollar flood to eastern China, a 1,000 year rainstorm to Baltimore, and some of the worst flooding Texas has ever seen—not to mention extreme heat waves and megafires galore—it’s hard to ignore the fact that the statistical realities of weather are changing.

Maddie Stone is a freelancer based in Philadelphia.

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DISCUSSION

Give the “it’s because of global warming crap a break”. In the 80's Louisiana was hit by two very similar events. One was in 1985 when hurricane Juan stalled over south central LA because of an incoming cold front. Juan made land fall three times in one week. Each time being pushed back into the gulf to strengthen and come back inland. We had over 24" of rain across S. LA. that week. Another time during the ‘80s we had 24" in one day. Rained to hard you could see the other side of the street. I-10 was shutdown between Lake Charles and Lafayette because of heavy flooding.

Both times the flooding was spread across much of south LA.

This time more homes are impacted because over the last 30 years people have been building nice and expensive homes in scenic locations near the rivers and bayous. This results in more and higher $$$ damage from similar flooding events. There have also been thousands of acres of parking lots and drainage systems built that serve to get the water out of communities faster. These carry water to the river that are only feet above sea level, even 50 miles inland. So, rivers swell and shoreline developments floods. In the past water flowed to the major rivers slowing, giving time for the rivers to carry the extra water to the gulf. The rivers would swell back then but it sometimes took weeks for the peak water levels to occur. For this event, peak river levels occurred in days.

It’s also possible that coastal erosion is a contributing factor for the weather event. Much of the coastal marsh loss is due to the levee system built to contain the Mississippi. Instead we have the unintended consequent of preventing soil from the midwest US from being deposited in the coastal wet lands. Instead, the river and soil jets out into the gulf, creating the dead zone we see today.