Behind Hurricane Ida’s Record-Shattering Rainfall in New York and the Northeast: Yes, It’s Global Warming

Ida had weakened well below hurricane strength by the time it reached the Northeast, so how did it still cause so much rain?

Two major factors likely contributed to its extended extreme rainfall.

First, Ida’s tropical moisture interacted with developing warm and cold fronts.

Second, evidence is mounting that, as the climate warms, the amount of precipitation from heavy rainstorms is increasing, especially in the central and eastern U.S.

From tropical to extratropical

Weather forecasters saw the disaster in the Northeast coming.

As hurricanes move northward from the tropics, they often transition from their characteristic circular shape to become “extratropical cyclones” with warm and cold fronts extending outward from the low pressure at the center. Even though they no longer have the intense winds that they did in the tropics, they still bring tropical humidity. That moist air is lifted along the fronts, and long-lasting, very heavy rain can result. That was happening as Ida’s remnants moved northward.




Forecasters emphasized the threat of flash flooding well ahead of its arrival, and the National Oceanic and Atmospheric Administration’s Weather Prediction Center issued a rare “high risk” of excessive rainfall outlook for parts of the Northeast a day in advance.

But the widespread, intense rainfall overwhelmed rivers and drainage systems in the highly populated corridor from Philadelphia to New York and Boston. That led to major flash flooding and at least 32 deaths in the region. Newark, New Jersey, recorded 8.41 inches of rain, their most ever in a single day, shattering the old record by over 1.5 inches. Weather stations in New York City saw rain rates over 3 inches per hour. The extreme rainfall arrived with tornadoes in Maryland and New Jersey.

Warmer climate, heavier rainfall

Extreme rain and flash flooding aren’t new to the Northeast, and they often result from hurricanes or their remnants. The remains of Hurricanes Agnes (1972), Floyd (1999), Irene (2011), Lee (2011) and Sandy (2012), among others, all brought widespread rainfall and flooding through the area. Yet, heavy downpours are becoming more common in the region as the climate warms.

The reasons behind this are fairly simple: Warmer air can have more water vapor in it. With every 1 degree Celsius (1.8 F) increase in temperature, there can be about 7% more moisture in the air. This is formally known as the Clausius-Clapeyron relation.

Because the amount of rain that a storm produces is closely connected to the amount of water vapor in the air, this means that, all else being equal, heavy downpours are more likely in a warmer climate. It explains why heavy rain occurs year-round in the tropics, whereas it is much more likely in summer than winter in the U.S.

This is also why the intensity of rainfall is expected to increase as the climate warms. When weather patterns that bring together the ingredients for heavy rainfall, like hurricanes, occur in a warmer world, more moisture is available, and more rain falls. Unfortunately, this is not a linear process: A small bit of added moisture can lead to a lot more rain.




The latest National Climate Assessment, in 2018, described a trend toward increasing precipitation in the Northeast and also warned that aging infrastructure in the region isn’t prepared to handle the water.

Hurricanes are limited to certain areas, but extreme rainfall from other types of storms can occur just about anywhere – think of intense cloudbursts during the summer monsoon in the Desert Southwest, or organized thunderstorm systems like the one that caused deadly flooding in Tennessee in August 2021.

Many communities are already highly vulnerable to the type of extreme precipitation that has been observed historically. Floods have always been a hazard, and intense rainfall can test the infrastructure even in places where it happens often. But as the climate changes, these risks will only increase further.

Russ Schumacher is Associate Professor of Atmospheric Science and Colorado State Climatologist at Colorado State University.

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