A swath of the Carmel River, upstream from the former San Clemente Dam site, surged with water on January 26, 2017. (Lindsey Hoshaw/KQED)
Tommy Williams—a fisheries biologist whose enthusiasm bubbles forth so swiftly, he’s often interrupting himself mid-sentence—is pacing on the banks of the Carmel River. “Amazing,” he says, snapping pictures of newly formed sandbanks and twigs wedged in between white alder, black cottonwood and willow trunks.
It’s not the trees or twigs that delight him. It’s the thundering flow of a river that has been dammed for the last 94 years—and the sediment (dirt and rocks) that are pushing everything downstream.
A view of the San Clemente Dam, before it was torn down in 2015. (California American Water)
“These trees have been growing in a place that haven’t had this kind of sediment flow here for 100 years,” says Williams, who works in the Santa Cruz office for NOAA Fisheries. “This is rocking their world right now.”
Williams doesn’t even mind that recent high flows have stripped out some of the tree tags he’d tied to branches along the river’s edge to mark fish survey spots. NOAA’s collaborating agency, the USGS, has also lost several rebar survey markers (which designate geological study areas) to the floods.
In fact, Carmel River flows in January were the highest they’ve been since 1998. That’s due to winter storms which soaked the Carmel Basin with 25 inches of rain since the first of the year.
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At its peak, the river water was rushing by at about 75,000 gallons a second. That’s 4.5 million gallons every minute, roughly enough water to fill six Olympic-size swimming pools.
The water sent boulders and broken tree branches crashing onto a service road alongside the river. By mid-January, it became impassable.
Carmel River Flows
In January 2017, Carmel River flows were the highest they’ve been since 1998. (USGS)
“It’s kind of messy,” says Williams. “But messy is okay.”
Actually, “messy” is crucial. The roots of upturned trees capture gravel, which provides essential spawning ground for federally protected steelhead trout. The back eddies and side channels next to the unearthed trees give fish a place to hide from predators like kingfishers and garter snakes. Or rest, as they make their long trek up river to spawn.
Tearing Down a Relic, Restoring a River
The river hasn’t been this messy since Woodrow Wilson was president. All that debris used to be trapped behind the San Clemente Dam, a concrete behemoth built in 1921 that became choked with silt and was eventually declared seismically unsafe in 1991. The dam crossed where the Carmel River and the San Clemente Creek naturally converged.
San Clemente Dam stopped supplying water to Monterey residents in 2002, when it was 90 percent full of silt and there was only a sliver of storage capacity left for water.
Cranes and bulldozers chipped away at it, demolishing the dam in 2015 after state and federal agencies decided it was too hazardous. If it were flooded or if an earthquake struck, up to 250,000 dump trucks worth of sediment could spew forth, suffocating anything living in the river.
The project involved a major river reroute—getting half a mile of the Carmel to flow into an adjacent stream: San Clemente Creek. This allowed engineers to stabilize the built-up sediment behind the dam and cover it with grass and tree saplings.
Trish Chapman, regional manager for the California State Coastal Conservancy, says the removal “seemed so much smarter than just slapping more concrete on a dam that no longer had any function.”
California American Water Company, the agency that owns the dam, could have retrofitted the structure for $49 million, which still would have presented problems as the dam weakened and aged. So for $84 million, the company tore it down.
Expanding Habitat for Steelhead to Spawn
Now the Carmel River is flowing freely again, carrying sediment downstream that was trapped behind the 106-foot wall for almost a century.
Steelhead trout live in the Carmel River. (The National Park Service)
“Did I ever think we’d see dams coming down? Not really,” says Williams. The biologist is also involved in the planned removal of four hydroelectric dams on the Klamath River.
“So it’s a pretty exciting time,” he adds.
Exciting and historic. The San Clemente deconstruction was the largest dam removal in state history.
Demolition of the dam opened 25 miles of upstream tributaries and creeks so that endangered steelhead can start to make their way up river to spawn.
The old dam impeded the fish’s migration to and from the ocean. There was a fish ladder, but it was the steepest fish ladder in western North America. Over time, the steelhead population dwindled from 1,350 in 1965 to 249 in 2013, the year the dam closed.
By 2016, the California State Coastal Conservancy was already seeing initial signs of recovery.
Fisheries biologist Tommy Williams scans a juvenile steelhead trout for a passive integrated transponder (PIT) tag. PIT tags uniquely identify each fish. (NOAA Fisheries)
Trish Chapman says fisheries biologists surveyed a “reach,” or section of the river they’d restored, and discovered steelhead nests above where the dam had been, evidence that the fish were making it past the old dam site.
“Finding out last year that fish had made it up above the reach that we worked on… that was pretty exciting,” says Chapman.
Williams says it will take years, maybe decades, before the biologists know whether the river has fully repaired itself and the fish are coming back.
“For me, extinction is not an option here,” says Williams. “We have to say, ‘what would we do to try to keep these fish around?'”
For now, that means allowing the river to run its course.
This summer, Williams and his team will return to tag and measure fish after the roaring rush of the river—fueled by winter rains—has finally slowed to a crawl.
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"title": "With Dam Gone, California River Comes Back to Life",
"headTitle": "With Dam Gone, California River Comes Back to Life | KQED",
"content": "\u003cp>\u003cspan style=\"font-size: 4.6875em;float: left;line-height: 0.733em;padding: 0.05em 0.1em 0 0;font-family: times, serif, georgia\">T\u003c/span>ommy Williams—a fisheries biologist whose enthusiasm bubbles forth so swiftly, he’s often interrupting himself mid-sentence—is pacing on the banks of the Carmel River. “Amazing,” he says, snapping pictures of newly formed sandbanks and twigs wedged in between white alder, black cottonwood and willow trunks.\u003c/p>\n\u003cp>It’s not the trees or twigs that delight him. It’s the thundering flow of a river that has been dammed for the last 94 years—and the sediment (dirt and rocks) that are pushing everything downstream.\u003c/p>\n\u003cfigure id=\"attachment_1371003\" class=\"wp-caption alignright\" style=\"max-width: 410px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"wp-image-1371003 \" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-1020x765.jpg\" alt=\"San Clemente Dam_historic\" width=\"410\" height=\"308\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-1020x765.jpg 1020w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-160x120.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-800x600.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-768x576.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-1920x1440.jpg 1920w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-1180x885.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-960x720.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-240x180.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-375x281.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-520x390.jpg 520w\" sizes=\"(max-width: 410px) 100vw, 410px\">\u003cfigcaption class=\"wp-caption-text\">A view of the San Clemente Dam, before it was torn down in 2015. \u003ccite>(California American Water)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>“These trees have been growing in a place that haven’t had this kind of sediment flow here for 100 years,” says Williams, who works in the Santa Cruz office for \u003ca href=\"http://www.nmfs.noaa.gov/\" target=\"_blank\" rel=\"noopener\">NOAA Fisheries\u003c/a>. “This is rocking their world right now.”\u003c/p>\n\u003cp>Williams doesn’t even mind that recent high flows have stripped out some of the tree tags he’d tied to branches along the river’s edge to mark fish survey spots. NOAA’s collaborating agency, the \u003ca href=\"https://www.usgs.gov/\" target=\"_blank\" rel=\"noopener\">USGS\u003c/a>, has also lost several rebar survey markers (which designate geological study areas) to the floods.\u003c/p>\n\u003cp>In fact, Carmel River flows in January were the highest they’ve been since 1998. That’s due to winter storms which soaked the Carmel Basin with 25 inches of rain since the first of the year.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>At its peak, the river water was rushing by at about 75,000 gallons a second. That’s 4.5 million gallons every minute, roughly enough water to fill six Olympic-size swimming pools.\u003c/p>\n\u003cp>The water sent boulders and broken tree branches crashing onto a service road alongside the river. By mid-January, it became impassable.\u003c/p>\n\u003ch4 style=\"text-align: center\">Carmel River Flows\u003c/h4>\n\u003cfigure id=\"attachment_1382063\" class=\"wp-caption aligncenter\" style=\"max-width: 1150px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-1382063\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows.jpg\" alt=\"In January 2017, Carmel River flows were the highest they’ve been since 1998.\" width=\"1150\" height=\"730\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows.jpg 1150w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-160x102.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-800x508.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-768x488.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-1020x647.jpg 1020w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-960x609.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-240x152.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-375x238.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-520x330.jpg 520w\" sizes=\"(max-width: 1150px) 100vw, 1150px\">\u003cfigcaption class=\"wp-caption-text\">In January 2017, Carmel River flows were the highest they’ve been since 1998. \u003ccite>(USGS)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>“It’s kind of messy,” says Williams. “But messy is okay.”\u003c/p>\n\u003cp>Actually, “messy” is crucial. The roots of upturned trees capture gravel, which provides essential spawning ground for federally protected steelhead trout. The back eddies and side channels next to the unearthed trees give fish a place to hide from predators like kingfishers and garter snakes. Or rest, as they make their long trek up river to spawn.\u003c/p>\n\u003cp>\u003cstrong>Tearing Down a Relic, Restoring a River\u003c/strong>\u003c/p>\n\u003cp>The river hasn’t been this messy since Woodrow Wilson was president. All that debris used to be trapped behind the San Clemente Dam, a concrete behemoth built in 1921 that became choked with silt and was eventually declared seismically unsafe in 1991. The dam crossed where the Carmel River and the San Clemente Creek naturally converged.\u003c/p>\n\u003cp>San Clemente Dam stopped supplying water to Monterey residents in 2002, when it was 90 percent full of silt and there was only a sliver of storage capacity left for water.\u003c/p>\n\u003cp>Cranes and bulldozers chipped away at it, demolishing the dam in 2015 after state and federal agencies decided it was too hazardous. If it were flooded or if an earthquake struck, up to 250,000 dump trucks worth of sediment could spew forth, suffocating anything living in the river.\u003c/p>\n\u003cdiv class=\"sharedaddy show-for-medium-up\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-1375780\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/Dam_desktop.jpg\" alt=\"Dam_desktop\" width=\"1334\" height=\"1075\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop.jpg 1334w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-160x129.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-800x645.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-768x619.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-1020x822.jpg 1020w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-1180x951.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-960x774.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-240x193.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-375x302.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-520x419.jpg 520w\" sizes=\"(max-width: 1334px) 100vw, 1334px\">\u003c/div>\n\u003cdiv class=\"show-for-small-only\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-1375781\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/Dam_mobile.jpg\" alt=\"Dam_mobile\" width=\"752\" height=\"1335\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile.jpg 752w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile-160x284.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile-240x426.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile-375x666.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile-520x923.jpg 520w\" sizes=\"(max-width: 752px) 100vw, 752px\">\u003c/div>\n\u003cp> \u003c/p>\n\u003cp>The project involved a major river reroute—getting half a mile of the Carmel to flow into an adjacent stream: San Clemente Creek. \u003cspan style=\"font-weight: 400\">This allowed engineers to stabilize the built-up sediment behind the dam and cover it with grass and tree saplings.\u003c/span>\u003c/p>\n\u003cp>Trish Chapman, regional manager for the \u003ca href=\"http://scc.ca.gov/\" target=\"_blank\" rel=\"noopener\">California State Coastal Conservancy\u003c/a>, says the removal “seemed so much smarter than just slapping more concrete on a dam that no longer had any function.”\u003c/p>\n\u003cp>\u003ca href=\"https://amwater.com/caaw/\" target=\"_blank\" rel=\"noopener\">California American Water Company\u003c/a>, the agency that owns the dam, could have retrofitted the structure for $49 million, which still would have presented problems as the dam weakened and aged. So for $84 million, the company tore it down.\u003c/p>\n\u003cp>\u003cstrong>Expanding Habitat for Steelhead to Spawn\u003c/strong>\u003c/p>\n\u003cp>Now the Carmel River is flowing freely again, carrying sediment downstream that was trapped behind the 106-foot wall for almost a century.\u003c/p>\n\u003cfigure id=\"attachment_1382193\" class=\"wp-caption alignleft\" style=\"max-width: 343px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-1382193\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/Steelhead_trout.jpg\" alt=\"Steelhead trout live in the Carmel River.\" width=\"343\" height=\"343\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout.jpg 450w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-160x160.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-240x240.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-375x375.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-32x32.jpg 32w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-50x50.jpg 50w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-64x64.jpg 64w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-96x96.jpg 96w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-128x128.jpg 128w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-150x150.jpg 150w\" sizes=\"(max-width: 343px) 100vw, 343px\">\u003cfigcaption class=\"wp-caption-text\">Steelhead trout live in the Carmel River. \u003ccite>(The National Park Service)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>“Did I ever think we’d see dams coming down? Not really,” says Williams. The biologist is also involved in the \u003ca href=\"https://ww2.kqed.org/news/2016/10/24/removal-of-klamath-dams-would-be-largest-river-restoration-in-u-s-history/\" target=\"_blank\" rel=\"noopener\">planned removal of four hydroelectric dams\u003c/a> on the Klamath River.\u003c/p>\n\u003cp>“So it’s a pretty exciting time,” he adds.\u003c/p>\n\u003cp>Exciting and historic. The San Clemente deconstruction was the largest dam removal in state history.\u003c/p>\n\u003cp>Demolition of the dam opened 25 miles of upstream tributaries and creeks so that endangered steelhead can start to make their way up river to spawn.\u003c/p>\n\u003cp>The old dam impeded the fish’s migration to and from the ocean. There was a fish ladder, but it was the steepest fish ladder in western North America. Over time, the steelhead population dwindled from 1,350 in 1965 to 249 in 2013, the year the dam closed.\u003c/p>\n\u003cp>By 2016, the California State Coastal Conservancy was already seeing initial signs of recovery.\u003c/p>\n\u003cfigure id=\"attachment_1375543\" class=\"wp-caption alignright\" style=\"max-width: 2272px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-1375543\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo.jpg\" alt=\"Fisheries biologist Tommy Williams scans a juvenile steelhead trout for a passive integrated transponder (PIT) tag. PIT tags uniquely identify the fish and in mark-and-recapture studies, they allow scientists to estimate fish survival rates and population size.\" width=\"2272\" height=\"1704\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo.jpg 2272w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-160x120.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-800x600.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-768x576.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-1020x765.jpg 1020w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-1920x1440.jpg 1920w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-1180x885.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-960x720.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-240x180.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-375x281.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-520x390.jpg 520w\" sizes=\"(max-width: 2272px) 100vw, 2272px\">\u003cfigcaption class=\"wp-caption-text\">Fisheries biologist Tommy Williams scans a juvenile steelhead trout for a passive integrated transponder (PIT) tag. PIT tags uniquely identify each fish. \u003ccite>(NOAA Fisheries)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Trish Chapman says fisheries biologists surveyed a “reach,” or section of the river they’d restored, and discovered steelhead nests above where the dam had been, evidence that the fish were making it past the old dam site.\u003c/p>\n\u003cp>“Finding out last year that fish had made it up above the reach that we worked on… that was pretty exciting,” says Chapman.\u003c/p>\n\u003cp>Williams says it will take years, maybe decades, before the biologists know whether the river has fully repaired itself and the fish are coming back.\u003c/p>\n\u003cp>“For me, extinction is not an option here,” says Williams. “We have to say, ‘what would we do to try to keep these fish around?'”\u003c/p>\n\u003cp>For now, that means allowing the river to run its course.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>This summer, Williams and his team will return to tag and measure fish after the roaring rush of the river—fueled by winter rains—has finally slowed to a crawl.\u003c/p>\n\n",
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"excerpt": "After nearly 100 years, the Carmel River runs unobstructed again and set a record for high flow levels in January.\r\n",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>\u003cspan style=\"font-size: 4.6875em;float: left;line-height: 0.733em;padding: 0.05em 0.1em 0 0;font-family: times, serif, georgia\">T\u003c/span>ommy Williams—a fisheries biologist whose enthusiasm bubbles forth so swiftly, he’s often interrupting himself mid-sentence—is pacing on the banks of the Carmel River. “Amazing,” he says, snapping pictures of newly formed sandbanks and twigs wedged in between white alder, black cottonwood and willow trunks.\u003c/p>\n\u003cp>It’s not the trees or twigs that delight him. It’s the thundering flow of a river that has been dammed for the last 94 years—and the sediment (dirt and rocks) that are pushing everything downstream.\u003c/p>\n\u003cfigure id=\"attachment_1371003\" class=\"wp-caption alignright\" style=\"max-width: 410px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"wp-image-1371003 \" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-1020x765.jpg\" alt=\"San Clemente Dam_historic\" width=\"410\" height=\"308\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-1020x765.jpg 1020w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-160x120.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-800x600.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-768x576.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-1920x1440.jpg 1920w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-1180x885.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-960x720.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-240x180.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-375x281.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/San-Clemente-Dam_historic-520x390.jpg 520w\" sizes=\"(max-width: 410px) 100vw, 410px\">\u003cfigcaption class=\"wp-caption-text\">A view of the San Clemente Dam, before it was torn down in 2015. \u003ccite>(California American Water)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>“These trees have been growing in a place that haven’t had this kind of sediment flow here for 100 years,” says Williams, who works in the Santa Cruz office for \u003ca href=\"http://www.nmfs.noaa.gov/\" target=\"_blank\" rel=\"noopener\">NOAA Fisheries\u003c/a>. “This is rocking their world right now.”\u003c/p>\n\u003cp>Williams doesn’t even mind that recent high flows have stripped out some of the tree tags he’d tied to branches along the river’s edge to mark fish survey spots. NOAA’s collaborating agency, the \u003ca href=\"https://www.usgs.gov/\" target=\"_blank\" rel=\"noopener\">USGS\u003c/a>, has also lost several rebar survey markers (which designate geological study areas) to the floods.\u003c/p>\n\u003cp>In fact, Carmel River flows in January were the highest they’ve been since 1998. That’s due to winter storms which soaked the Carmel Basin with 25 inches of rain since the first of the year.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>At its peak, the river water was rushing by at about 75,000 gallons a second. That’s 4.5 million gallons every minute, roughly enough water to fill six Olympic-size swimming pools.\u003c/p>\n\u003cp>The water sent boulders and broken tree branches crashing onto a service road alongside the river. By mid-January, it became impassable.\u003c/p>\n\u003ch4 style=\"text-align: center\">Carmel River Flows\u003c/h4>\n\u003cfigure id=\"attachment_1382063\" class=\"wp-caption aligncenter\" style=\"max-width: 1150px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-1382063\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows.jpg\" alt=\"In January 2017, Carmel River flows were the highest they’ve been since 1998.\" width=\"1150\" height=\"730\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows.jpg 1150w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-160x102.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-800x508.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-768x488.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-1020x647.jpg 1020w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-960x609.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-240x152.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-375x238.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/USGS_graph_Carmel_River_Flows-520x330.jpg 520w\" sizes=\"(max-width: 1150px) 100vw, 1150px\">\u003cfigcaption class=\"wp-caption-text\">In January 2017, Carmel River flows were the highest they’ve been since 1998. \u003ccite>(USGS)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>“It’s kind of messy,” says Williams. “But messy is okay.”\u003c/p>\n\u003cp>Actually, “messy” is crucial. The roots of upturned trees capture gravel, which provides essential spawning ground for federally protected steelhead trout. The back eddies and side channels next to the unearthed trees give fish a place to hide from predators like kingfishers and garter snakes. Or rest, as they make their long trek up river to spawn.\u003c/p>\n\u003cp>\u003cstrong>Tearing Down a Relic, Restoring a River\u003c/strong>\u003c/p>\n\u003cp>The river hasn’t been this messy since Woodrow Wilson was president. All that debris used to be trapped behind the San Clemente Dam, a concrete behemoth built in 1921 that became choked with silt and was eventually declared seismically unsafe in 1991. The dam crossed where the Carmel River and the San Clemente Creek naturally converged.\u003c/p>\n\u003cp>San Clemente Dam stopped supplying water to Monterey residents in 2002, when it was 90 percent full of silt and there was only a sliver of storage capacity left for water.\u003c/p>\n\u003cp>Cranes and bulldozers chipped away at it, demolishing the dam in 2015 after state and federal agencies decided it was too hazardous. If it were flooded or if an earthquake struck, up to 250,000 dump trucks worth of sediment could spew forth, suffocating anything living in the river.\u003c/p>\n\u003cdiv class=\"sharedaddy show-for-medium-up\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-1375780\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/Dam_desktop.jpg\" alt=\"Dam_desktop\" width=\"1334\" height=\"1075\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop.jpg 1334w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-160x129.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-800x645.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-768x619.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-1020x822.jpg 1020w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-1180x951.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-960x774.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-240x193.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-375x302.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_desktop-520x419.jpg 520w\" sizes=\"(max-width: 1334px) 100vw, 1334px\">\u003c/div>\n\u003cdiv class=\"show-for-small-only\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-1375781\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/Dam_mobile.jpg\" alt=\"Dam_mobile\" width=\"752\" height=\"1335\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile.jpg 752w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile-160x284.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile-240x426.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile-375x666.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Dam_mobile-520x923.jpg 520w\" sizes=\"(max-width: 752px) 100vw, 752px\">\u003c/div>\n\u003cp> \u003c/p>\n\u003cp>The project involved a major river reroute—getting half a mile of the Carmel to flow into an adjacent stream: San Clemente Creek. \u003cspan style=\"font-weight: 400\">This allowed engineers to stabilize the built-up sediment behind the dam and cover it with grass and tree saplings.\u003c/span>\u003c/p>\n\u003cp>Trish Chapman, regional manager for the \u003ca href=\"http://scc.ca.gov/\" target=\"_blank\" rel=\"noopener\">California State Coastal Conservancy\u003c/a>, says the removal “seemed so much smarter than just slapping more concrete on a dam that no longer had any function.”\u003c/p>\n\u003cp>\u003ca href=\"https://amwater.com/caaw/\" target=\"_blank\" rel=\"noopener\">California American Water Company\u003c/a>, the agency that owns the dam, could have retrofitted the structure for $49 million, which still would have presented problems as the dam weakened and aged. So for $84 million, the company tore it down.\u003c/p>\n\u003cp>\u003cstrong>Expanding Habitat for Steelhead to Spawn\u003c/strong>\u003c/p>\n\u003cp>Now the Carmel River is flowing freely again, carrying sediment downstream that was trapped behind the 106-foot wall for almost a century.\u003c/p>\n\u003cfigure id=\"attachment_1382193\" class=\"wp-caption alignleft\" style=\"max-width: 343px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-1382193\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/Steelhead_trout.jpg\" alt=\"Steelhead trout live in the Carmel River.\" width=\"343\" height=\"343\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout.jpg 450w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-160x160.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-240x240.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-375x375.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-32x32.jpg 32w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-50x50.jpg 50w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-64x64.jpg 64w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-96x96.jpg 96w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-128x128.jpg 128w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Steelhead_trout-150x150.jpg 150w\" sizes=\"(max-width: 343px) 100vw, 343px\">\u003cfigcaption class=\"wp-caption-text\">Steelhead trout live in the Carmel River. \u003ccite>(The National Park Service)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>“Did I ever think we’d see dams coming down? Not really,” says Williams. The biologist is also involved in the \u003ca href=\"https://ww2.kqed.org/news/2016/10/24/removal-of-klamath-dams-would-be-largest-river-restoration-in-u-s-history/\" target=\"_blank\" rel=\"noopener\">planned removal of four hydroelectric dams\u003c/a> on the Klamath River.\u003c/p>\n\u003cp>“So it’s a pretty exciting time,” he adds.\u003c/p>\n\u003cp>Exciting and historic. The San Clemente deconstruction was the largest dam removal in state history.\u003c/p>\n\u003cp>Demolition of the dam opened 25 miles of upstream tributaries and creeks so that endangered steelhead can start to make their way up river to spawn.\u003c/p>\n\u003cp>The old dam impeded the fish’s migration to and from the ocean. There was a fish ladder, but it was the steepest fish ladder in western North America. Over time, the steelhead population dwindled from 1,350 in 1965 to 249 in 2013, the year the dam closed.\u003c/p>\n\u003cp>By 2016, the California State Coastal Conservancy was already seeing initial signs of recovery.\u003c/p>\n\u003cfigure id=\"attachment_1375543\" class=\"wp-caption alignright\" style=\"max-width: 2272px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-1375543\" src=\"https://ww2.kqed.org/science/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo.jpg\" alt=\"Fisheries biologist Tommy Williams scans a juvenile steelhead trout for a passive integrated transponder (PIT) tag. PIT tags uniquely identify the fish and in mark-and-recapture studies, they allow scientists to estimate fish survival rates and population size.\" width=\"2272\" height=\"1704\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo.jpg 2272w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-160x120.jpg 160w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-800x600.jpg 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-768x576.jpg 768w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-1020x765.jpg 1020w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-1920x1440.jpg 1920w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-1180x885.jpg 1180w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-960x720.jpg 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-240x180.jpg 240w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-375x281.jpg 375w, https://cdn.kqed.org/wp-content/uploads/sites/35/2017/02/Tommy-Williams_photo-520x390.jpg 520w\" sizes=\"(max-width: 2272px) 100vw, 2272px\">\u003cfigcaption class=\"wp-caption-text\">Fisheries biologist Tommy Williams scans a juvenile steelhead trout for a passive integrated transponder (PIT) tag. PIT tags uniquely identify each fish. \u003ccite>(NOAA Fisheries)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Trish Chapman says fisheries biologists surveyed a “reach,” or section of the river they’d restored, and discovered steelhead nests above where the dam had been, evidence that the fish were making it past the old dam site.\u003c/p>\n\u003cp>“Finding out last year that fish had made it up above the reach that we worked on… that was pretty exciting,” says Chapman.\u003c/p>\n\u003cp>Williams says it will take years, maybe decades, before the biologists know whether the river has fully repaired itself and the fish are coming back.\u003c/p>\n\u003cp>“For me, extinction is not an option here,” says Williams. “We have to say, ‘what would we do to try to keep these fish around?'”\u003c/p>\n\u003cp>For now, that means allowing the river to run its course.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>This summer, Williams and his team will return to tag and measure fish after the roaring rush of the river—fueled by winter rains—has finally slowed to a crawl.\u003c/p>\n\n\u003c/div>\u003c/p>",
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"radiolab": {
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"info": "A two-time Peabody Award-winner, Radiolab is an investigation told through sounds and stories, and centered around one big idea. In the Radiolab world, information sounds like music and science and culture collide. Hosted by Jad Abumrad and Robert Krulwich, the show is designed for listeners who demand skepticism, but appreciate wonder. WNYC Studios is the producer of other leading podcasts including Freakonomics Radio, Death, Sex & Money, On the Media and many more.",
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"info": "Created by The Center for Investigative Reporting and PRX, Reveal is public radios first one-hour weekly radio show and podcast dedicated to investigative reporting. Credible, fact based and without a partisan agenda, Reveal combines the power and artistry of driveway moment storytelling with data-rich reporting on critically important issues. The result is stories that inform and inspire, arming our listeners with information to right injustices, hold the powerful accountable and improve lives.Reveal is hosted by Al Letson and showcases the award-winning work of CIR and newsrooms large and small across the nation. In a radio and podcast market crowded with choices, Reveal focuses on important and often surprising stories that illuminate the world for our listeners.",
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},
"selected-shorts": {
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"title": "Selected Shorts",
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