Turn Around, Don’t Drown: Floods and Flash Floods

April 25, 2024
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Heavy convective (thunderstorm) rainfall was my expertise for over half of my National Weather Service career. The technical term was called Quantitative Precipitation Forecasting (QPF), which in layman’s terms was trying to figure out how much rain would fall in a specific time period, in a specific location. The scope of our forecast area was the lower 48 states, including parts of Mexico and Canada, where rainfall runoff impacts rivers in the USA.

During the spring, we begin to see an increase in the number of thunderstorms, which can produce intense periods of heavy rain. One to two inches of rain in an hour is common from thunderstorms, and they can produce much more than that in extreme events.

There are two types of flooding that we need to be watchful for in the Lake Anna area: River flooding and Flash Flooding. River floods usually develop from relatively long periods of heavy rain and can cover large regions. When heavy rain occurs, some water will soak into the soil, with the rest flowing into rivers. The National Weather Service (NWS) makes rainfall forecasts out to five days and this data is fed into computer models of the rivers. Meteorologists at the Weather Prediction Center produce these forecasts.

After rainfall forecasts are put into river models, the output tells us how high the rivers and streams in the area will rise. In order to verify and track these forecasts the United States Geological Survey (USGS) operates numerous gauges along rivers throughout Virginia that record river heights.

The NWS knows the river heights that cause flooding near the gauge. If the NWS sees a potential for heavy rain to occur, that could push a river up to flood stage, then a flood watch is issued. If we have high confidence that the river will equal or exceed the flood stage, then a flood warning is issued. The gauge closest to the Lake anna area is on the North Anna River, at Partlow, just below the dam.

Fortunately, forecasting river flooding is fairly predictable and watches and warnings usually have enough lead-time so that people can move themselves and their property to higher ground before the water rises too high.

Flash flooding is a type of flooding that is very dangerous and results in more lost lives each year, in the United States, than any other weather phenomena. Flash flooding occurs when intense rains occur in a very short period of time so that the ground can’t absorb the water. Although flash floods usually evolve into river floods, the bigger danger is the rapid rise in water in small streams, creeks, runs and drainage ditches during the intense rainfall. During intense periods of heavy rain, the water in small water drainage areas can rise several feet in a matter of minutes. This results in fast flowing water that can carry cars and people quickly downstream and even wash away buildings in the biggest flash floods. The most serious flash floods usually occur in mountainous areas. The sloped terrain creates even greater runoff and faster rises in streams and rivers. This is what happened in June 1995 in Madison County when rainfall of 20-30 inches fell in about 16 hours. This gets a bit technical, but is a great overview of the Madison County Flash Flood.

There are some things that you can do to protect yourself from flash floods. The first is “DON’T EVER DRIVE YOUR CAR THROUGH WATER THAT’S RUNNING OVER A ROAD”. The danger lies in the fact that the water can eat away at the road and you really don’t know the depth of the water or if the road is washed away. It only takes about 18 inches of water to carry away most cars we drive today. About half of all flash flood deaths are from people in cars that get trapped in flash floods. If you ever come across this situation, “TURN AROUND DON’T DROWN.” Flash floods at night are even more dangerous since your visibility is reduced.


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Heavy convective (thunderstorm) rainfall was my expertise for over half of my National Weather Service career. The technical term was called Quantitative Precipitation Forecasting (QPF), which in layman’s terms was trying to figure out how much rain would fall in a specific time period, in a specific location. The scope of our forecast area was the lower 48 states, including parts of Mexico and Canada, where rainfall runoff impacts rivers in the USA.

During the spring, we begin to see an increase in the number of thunderstorms, which can produce intense periods of heavy rain. One to two inches of rain in an hour is common from thunderstorms, and they can produce much more than that in extreme events.

There are two types of flooding that we need to be watchful for in the Lake Anna area: River flooding and Flash Flooding. River floods usually develop from relatively long periods of heavy rain and can cover large regions. When heavy rain occurs, some water will soak into the soil, with the rest flowing into rivers. The National Weather Service (NWS) makes rainfall forecasts out to five days and this data is fed into computer models of the rivers. Meteorologists at the Weather Prediction Center produce these forecasts.

After rainfall forecasts are put into river models, the output tells us how high the rivers and streams in the area will rise. In order to verify and track these forecasts the United States Geological Survey (USGS) operates numerous gauges along rivers throughout Virginia that record river heights.

The NWS knows the river heights that cause flooding near the gauge. If the NWS sees a potential for heavy rain to occur, that could push a river up to flood stage, then a flood watch is issued. If we have high confidence that the river will equal or exceed the flood stage, then a flood warning is issued. The gauge closest to the Lake anna area is on the North Anna River, at Partlow, just below the dam.

Fortunately, forecasting river flooding is fairly predictable and watches and warnings usually have enough lead-time so that people can move themselves and their property to higher ground before the water rises too high.

Flash flooding is a type of flooding that is very dangerous and results in more lost lives each year, in the United States, than any other weather phenomena. Flash flooding occurs when intense rains occur in a very short period of time so that the ground can’t absorb the water. Although flash floods usually evolve into river floods, the bigger danger is the rapid rise in water in small streams, creeks, runs and drainage ditches during the intense rainfall. During intense periods of heavy rain, the water in small water drainage areas can rise several feet in a matter of minutes. This results in fast flowing water that can carry cars and people quickly downstream and even wash away buildings in the biggest flash floods. The most serious flash floods usually occur in mountainous areas. The sloped terrain creates even greater runoff and faster rises in streams and rivers. This is what happened in June 1995 in Madison County when rainfall of 20-30 inches fell in about 16 hours. This gets a bit technical, but is a great overview of the Madison County Flash Flood.

There are some things that you can do to protect yourself from flash floods. The first is “DON’T EVER DRIVE YOUR CAR THROUGH WATER THAT’S RUNNING OVER A ROAD”. The danger lies in the fact that the water can eat away at the road and you really don’t know the depth of the water or if the road is washed away. It only takes about 18 inches of water to carry away most cars we drive today. About half of all flash flood deaths are from people in cars that get trapped in flash floods. If you ever come across this situation, “TURN AROUND DON’T DROWN.” Flash floods at night are even more dangerous since your visibility is reduced.


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