Then, over the weekend, the intensity of the rainfall should gradually ease, but it may become more persistent and widespread late Saturday into early Sunday. This may cause some rivers and streams to crest above flood levels for the second time in the past few weeks.
Even though we think any instances of damaging winds in thunderstorms will be isolated over the next several days, be aware that a few trees could come down because of heavy rain alone, as the soaked ground can disrupt their root systems.
This latest bout of rainy weather arrives after 7.41 inches have already fallen in Washington this month, the eighth wettest May on record.
While June will pick up rain Friday where May left off, the pattern should shift to a drier one early next week.
As in the past two weeks, in which we experienced devastating flash floods in Frederick and Ellicott City, Md., a stubborn frontal boundary separating sultry summer air to the south and cooler Atlantic air to the north, will remain anchored across our region. As shown below, the front is expected to be positioned across far northeastern Maryland on Thursday afternoon.
It’s possible that the front could drape anywhere between the District and the Mason-Dixon Line. Models suggest it will push farther north Friday, placing us deep in the warm sector of an approaching low pressure system and cold front.
On Thursday, regions near and along the boundary will experience the greatest triggering (uplift) potential for sustained showers and thunderstorms. On Friday, the potential becomes more area-wide, as a disturbance in the upper-level flow approaches the region, and the cold front moves through from the west.
With southerly flow and intermittent solar heating, the atmosphere will destabilize during the afternoon and evening of both days, providing the buoyant energy for convective storms. Atmospheric moisture will be plentiful, approaching or perhaps exceeding record levels (precipitable water of up to two inches), as shown below.
As we remain under an upper-level ridge in a weak jet stream pattern, steering flow aloft will be on the weak side, meaning thunderstorm cells could linger over the same regions, increasing local rain totals. For regions that have received a soaking in the past few weeks, this means the soil will absorb less, and the potential for runoff increases.
For all these reasons, the Weather Service has placed our region in its slight risk (10 to 20 percent chance) zone of flash flooding, both Thursday and Friday.
Given the lack of strong wind shear, which intensifies storm wind speeds, we do not expect widespread severe thunderstorms either day. However, there remains the prospect of frequent lightning, and an isolated wet microburst or two in which a pocket of damaging winds hits a relatively small area.
As we get into the weekend, the atmospheric setup remains problematic. The cold front will have moved through, but a pesky feature termed a “cutoff low” is expected to develop over the region and persist for a couple days (shown below; note the swirl of air Sunday morning over the Mid-Atlantic). The air mass will remain quite moist. Rounds of slow-moving showers and thunderstorms may be frequent visitors Saturday. By Saturday night and early Sunday, the rains may become more moderate but widespread.
Models differ quite a bit on how much rain will fall through the weekend, and amounts may vary from location to location. They generally simulate one to two inches — on average — around Washington but will not be able to capture in advance the downpours unleashed in thunderstorm rains, which can rival such amounts in an hour alone. Here’s what the primary models project, specifically, for the District:
- American (GFS): 2.0 inches
- Canadian: 1.3 inches
- European: 1.75 inches
Both the potential rainfall and soaked soils in some of our watersheds could spell larger stream flooding concerns in the Sunday-Monday time frame.