Displaying items by tag: mathew barlow

Hurricane Debby made landfall near the town of Steinhatchee, Florida, at 7 a.m. Aug. 5, 2024, as a Category 1 storm. As it moved northeast, the storm stalled over the U.S. Southeast and delivered torrential rainfall. Some areas of South Carolina and Georgia recorded more than 20 inches of rain as the storm crawled northeast toward a second landfall (this time as a strong tropical storm) near Myrtle Beach, S.C.  NOAA

A warming climate means more water vapor, which means bigger and wetter tropical storms

(This story was originally published by The Conversation.)

Tropical Storm Debby was moving so slowly, Olympians could have outrun it as it moved across the Southeast in early August 2024. That gave its rainfall time to deluge cities and farms over large parts of Florida, Georgia and the Carolinas. More than a foot of rain had fallen in some areas by early Aug. 7, with more days of rain forecast there and into the Northeast.

Mathew Barlow, a climate scientist at UMass Lowell, explains how storms like Debby pick up so much moisture, what can cause them to slow or stall and what climate change has to do with it.

What causes hurricanes to stall?

Hurricanes are steered by the weather systems they interact with, including other storms moving across the U.S. and the Bermuda High over the Atlantic Ocean.

A hurricane may be moving slowly because there are no weather systems close enough to pull the hurricane along, or there might be a high-pressure system to the north of the hurricane that blocks its forward movement. In this case, a high-pressure system over the western U.S. was slowing Debby’s forward progress and the Bermuda High — which is a large, clockwise circulation of winds that generally runs up the East Coast — wasn’t close enough to be a factor.

That’s similar to what happened with the remnants of Hurricane Harvey in 2017, one of the best-known examples of a stalled hurricane. High pressure over the U.S. blocked its forward movement, allowing it to drop more than 50 inches of rain on parts of Texas.

Slower-moving storms have longer to rain over the same area, and that can dramatically increase the risk of flooding, as the Southeast is experiencing with Debby. 

An area of high pressure lingered in the upper atmosphere over the U.S. Midwest and Northeast in June 2024. This pushed warm air toward the surface and trapped it there—a weather phenomenon meteorologists call a heat dome. The heat wave reached the Southern Appalachians, as seen in this model generated from NASA Earth Observatory data.  NASA

How climate change is heating up the weather, and what we can do about it

This article was originally published by The Conversation.

The heat wave that left more than 100 million people sweating across the eastern U.S. in June 2024 hit so fast and was so extreme that forecasters warned a flash drought could follow across wide parts of the region.

Prolonged high temperatures can quickly dry soils, triggering a rapid onset drought that can affect agriculture, water resources and energy supplies. Many regions under the June heat dome quickly developed abnormally dry conditions.

(The average temperature of June was about 7 degrees above normal in Knoxville as reported by Weather Underground).

The human impacts of the heat wave have also been widespread. In Ohio and Pennsylvania, emergency room visits for heat-related illnesses surged. Several Massachusetts schools without air conditioning closed to protect kids and teachers. In New York and New Jersey, electric wires sagged in the heat, shutting down trains into and out of New York City and leaving commuters stranded.