Mojave River flows through Barstow for first time since 2011
The Mojave River flows near the Deep Creek area during a winter storm last week. Inflow to the Mojave River at its headwaters peaked at approximately 15,000 cubic feet per second during the storm, according to provisional estimates. [James Quigg, Daily Press]
By Matthew Cabe
Victor Valley Press
BARSTOW — Recent rains allowed surface water in the Mojave River to flow through the city for the first time in eight years, signaling good news for recharge in regional aquifers, according to Mojave Water Agency officials.
MWA Senior Hydrogeologist/Engineer Tony Winkel told the Daily Press inflow to the Mojave River at its headwaters on Thursday peaked at approximately 15,000 cubic feet per second, according to provisional estimates.
That inflow surged through the inlet within the Mojave River Dam, sometimes called the Forks Dam, where the Deep Creek and West Fork tributaries converge.
Winkel said previous storms in recent weeks allowed the river to soak up water “like a big dry sponge.” Because the river can only absorb water so quickly, though, water from last week’s storm subsequently “skirted” along through Barstow, petering out just beyond Minneola Road in Yermo late last week.
“Minneola Road is kind of the upper end of the Baja subarea, but it was kind of a trickle,” Winkel said. “So right at the headwaters, it’s raging. You get down to the tail end of it, it’s just trickling because that much water has soaked in, which is a good thing because that’s water supply.”
Amid the worst drought in California history several years ago, the High Desert finally received some wet weather in 2017. But that water didn’t reach Barstow, which makes last week’s storm significant because it was the city’s “first influx of water since 2011,” Winkel said.
To understand just how much water flowed into the Mojave River on Thursday, MWA Water Conservation and Forecast Manager Nick Schneider said to imagine 15,000 basketballs bouncing through the inlet — in one second.
The analogy isn’t precise, according to Schneider and Winkel because a basketball isn’t exactly one cubic foot. Schneider, however, said the “industry conversion idea” is fair for visualization purposes.
“For the layman, if you think of a basketball, that’s a good way to process it,” Winkel said. “For an engineer, it drove me nuts.”
While 15,000 CFS is impressive and welcome, Winkel said last week’s storm, historically, pales in comparison to older weather events that brought significant inflow at the Mojave River’s headwaters.
On March 4, 1978, inflow peaked above 35,000 CFS, according to data Winkel provided. Some 40 years earlier, during what’s been called the “flood of the century” that ravaged the High Desert in March 1938, inflow peaked at nearly 75,000 CFS.
The data, which included estimates as far back as December 1859, showed at least 16 peak events with a magnitude above 25,000 CFS, including a Jan. 22, 1862, incident during which inflow is estimated at more than 100,000 CFS.
That peak came during the Great Flood of 1862, which started with a series of storms in December 1861 and is considered the largest flood in California’s history. It’s unknown how much damage occurred locally, but Sacramento was underwater for months. Schneider said newly elected Gov. Leland Stanford had to travel by rowboat to and from his inauguration in January.
Winkel said last week’s storm was nowhere near even the peaks seen in the wet winters of 2010 and 2011, which were also below 25,000 CFS. That said, it’s important in its own right because it equals recharge for the High Desert’s water supply, he said.
Consequential weather events occur, on average, every six to eight years, but that cycle isn’t consistent and the peaks are “very variable”, according to Winkel. Still, the High Desert, insofar as water supply is concerned, relies on peak events like the one experienced last week, he said.
“So how significant is it that the water made it to Barstow?” Winkel said. “Very. Because that’s the natural supply that we depend on.”
Specific recharge data for last week’s storm is not yet available because “we’re still in the storm swell,” according to Winkel, who said he’s hoping for more rain this year.
“Aside from the excitement factor of a river that’s actually flowing, which is very exciting because it usually doesn’t, I want to see more for water supply purposes.”
By Matthew Cabe
Victor Valley Press
BARSTOW — Recent rains allowed surface water in the Mojave River to flow through the city for the first time in eight years, signaling good news for recharge in regional aquifers, according to Mojave Water Agency officials.
MWA Senior Hydrogeologist/Engineer Tony Winkel told the Daily Press inflow to the Mojave River at its headwaters on Thursday peaked at approximately 15,000 cubic feet per second, according to provisional estimates.
That inflow surged through the inlet within the Mojave River Dam, sometimes called the Forks Dam, where the Deep Creek and West Fork tributaries converge.
Winkel said previous storms in recent weeks allowed the river to soak up water “like a big dry sponge.” Because the river can only absorb water so quickly, though, water from last week’s storm subsequently “skirted” along through Barstow, petering out just beyond Minneola Road in Yermo late last week.
“Minneola Road is kind of the upper end of the Baja subarea, but it was kind of a trickle,” Winkel said. “So right at the headwaters, it’s raging. You get down to the tail end of it, it’s just trickling because that much water has soaked in, which is a good thing because that’s water supply.”
Amid the worst drought in California history several years ago, the High Desert finally received some wet weather in 2017. But that water didn’t reach Barstow, which makes last week’s storm significant because it was the city’s “first influx of water since 2011,” Winkel said.
To understand just how much water flowed into the Mojave River on Thursday, MWA Water Conservation and Forecast Manager Nick Schneider said to imagine 15,000 basketballs bouncing through the inlet — in one second.
The analogy isn’t precise, according to Schneider and Winkel because a basketball isn’t exactly one cubic foot. Schneider, however, said the “industry conversion idea” is fair for visualization purposes.
“For the layman, if you think of a basketball, that’s a good way to process it,” Winkel said. “For an engineer, it drove me nuts.”
While 15,000 CFS is impressive and welcome, Winkel said last week’s storm, historically, pales in comparison to older weather events that brought significant inflow at the Mojave River’s headwaters.
On March 4, 1978, inflow peaked above 35,000 CFS, according to data Winkel provided. Some 40 years earlier, during what’s been called the “flood of the century” that ravaged the High Desert in March 1938, inflow peaked at nearly 75,000 CFS.
The data, which included estimates as far back as December 1859, showed at least 16 peak events with a magnitude above 25,000 CFS, including a Jan. 22, 1862, incident during which inflow is estimated at more than 100,000 CFS.
That peak came during the Great Flood of 1862, which started with a series of storms in December 1861 and is considered the largest flood in California’s history. It’s unknown how much damage occurred locally, but Sacramento was underwater for months. Schneider said newly elected Gov. Leland Stanford had to travel by rowboat to and from his inauguration in January.
Winkel said last week’s storm was nowhere near even the peaks seen in the wet winters of 2010 and 2011, which were also below 25,000 CFS. That said, it’s important in its own right because it equals recharge for the High Desert’s water supply, he said.
Consequential weather events occur, on average, every six to eight years, but that cycle isn’t consistent and the peaks are “very variable”, according to Winkel. Still, the High Desert, insofar as water supply is concerned, relies on peak events like the one experienced last week, he said.
“So how significant is it that the water made it to Barstow?” Winkel said. “Very. Because that’s the natural supply that we depend on.”
Specific recharge data for last week’s storm is not yet available because “we’re still in the storm swell,” according to Winkel, who said he’s hoping for more rain this year.
“Aside from the excitement factor of a river that’s actually flowing, which is very exciting because it usually doesn’t, I want to see more for water supply purposes.”