Smog over downtown San Francisco, February 2009. (Jerome Paz/flickr Creative Commons)
This week, you can watch as Earth passes a threshold not seen for at least a million years. The concentration of carbon dioxide in the air will rise above 400 parts per million. And scientists predict neither you nor your children will ever see it go below 400 ppm again.
The World Meteorological Organization (WMO) said on Monday that this year’s El Niño combined with global warming puts the world “in uncharted territory.”
“This naturally occurring El Niño event and human induced climate change may interact and modify each other in ways which we have never before experienced,” said WMO Secretary-General Michel Jarraud.
‘An Icon of Climate Change’
When scientists talk about atmospheric CO2, their yardstick is the so-called Keeling curve. It’s the record of the air’s composition, made each day at a station run by the Scripps Institution of Oceanography in the pure air high on Mauna Loa volcano, in Hawaii.
This week’s carbon dioxide readings at the Mauna Loa Observatory are updated every day. As they rise above the 400 parts-per-million threshold, scientists warn that they will not return to it in our lifetimes. (Scripps/UC San Diego)
The Keeling curve was started in 1958 under the direction of Keeling’s father, Charles David “Dave” Keeling. Today it’s the longest series of such measurements in the world. It was named a National Historic Chemical Landmark this year.
The Keeling curve is an icon of climate change. What does it show?
In the 1960s, Dave Keeling’s measurements showed that the CO2 level in the air was rising steadily. That long-term increase is the mark of human influence. It comes overwhelmingly from the fossil fuels we burn — largely to generate electricity, but also to smelt metals, produce cement, run motors and so on. Other smaller sources of CO2 are from humans cutting down forests and from large-scale mechanical farming, which removes most of the carbon-rich humus contained in soil.
Since the 1960s, the long-term increase in CO2 has sped up. A little over half of the CO2 we produce is absorbed by the ocean and by growing plants. The rest stays in the air and acts as a greenhouse gas.
NOAA’s Mauna Loa Observatory on Hawaii, a small collection of buildings where scientists take key measurements on air and sunlight. (NOAA)
If CO2 weren’t a greenhouse gas, we might welcome it for promoting plant growth. But because it is one, higher CO2 levels will make Earth steadily warmer until either human ingenuity or geology can bring them back down.
What led to Ralph Keeling’s prediction, and the significance of this week? That stems from another of Dave Keeling’s early discoveries — the CO2 curve also goes through a yearly cycle, rising to a peak around May and falling to a low around October.
The yearly cycle is a signal of natural life. Plants absorb CO2 from the air during the growing season, then release it as they are eaten or die back. Because most of Earth’s land area is in the northern hemisphere, the yearly cycle is dominated by the seasons in the north.
But this year we have a record-breaking El Niño in the cycle, triggering drought in the tropics and hampering plant growth there, and fueling widespread forest fires that pour CO2 into the air. The forest grows back, but not in time for next summer.
Atmospheric CO2 at the Mauna Loa Observatory in the last two years. (Scripps/UC San Diego)
So Ralph Keeling predicts the annual summer dip won’t bring readings back down into the 390s, as it did in 2014 and 2015.
“Will daily values at Mauna Loa ever fall below 400 ppm again in our lifetimes?” Keeling asked. “I’m prepared to project that they won’t, making the current values the last time the Mauna Loa record will produce numbers in the 300s.”
Meanwhile the stubborn long-term climb caused by humans shows no sign of slackening.
Change Can Happen, But Are We Willing?
In the 1700s, before coal began to be burned for industrial processes, CO2 was at about 280 ppm.
The long-term upward trend has never gone down since the Keeling measurements began. The only way to make the climb stop is to burn less carbon and, at the same time, fix more carbon. Burning less means changing our economic system severely and rapidly. It can be done, but the change will be profound.
Rise in atmospheric CO2 at the Mauna Loa Observatory since March 1958. (Scripps/UC San Diego)
Fixing more carbon is a project with many options, most of which involve burying CO2 underground. One promising frontier is working with the natural carbon cycle to increase the world’s biomass. Restoring the soil, by reforming our farming practices, could help turn the Keeling curve back toward 400 and below, once again. That, too, would be a profound change.
Eventually, geology will take care of the atmosphere through the really long-term carbon cycle. First the ocean will stir excess CO2 throughout its deepest waters. That will take on the order of 1,000 years.
Second, the erosion of rocks will fertilize the sea with dissolved carbon minerals, which plankton will use to make their microscopic shells, which will fall to the seafloor as the plankton die and be buried. It’s a roundabout system, but that’s how the Earth works. That will take many thousands of years.
We probably can’t wait that long.
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"headTitle": "CO2: Earth Passes Into ‘Uncharted Territory’ | KQED",
"content": "\u003cp>This week, \u003ca href=\"https://scripps.ucsd.edu/programs/keelingcurve/\" target=\"_blank\" rel=\"noopener\">you can watch\u003c/a> as Earth passes a threshold not seen for at least a million years. The concentration of carbon dioxide in the air will rise above 400 parts per million. And scientists predict neither you nor your children will ever see it go below 400 ppm again.\u003c/p>\n\u003cp>The World Meteorological Organization (WMO) said on Monday that this year’s El Niño combined with global warming puts the world “\u003ca href=\"https://www.wmo.int/media/content/el-ni%C3%B1o-expected-strengthen-further-high-impacts-unprecedented-preparation\" target=\"_blank\" rel=\"noopener\">in uncharted territory\u003c/a>.”\u003c/p>\n\u003cp>“This naturally occurring El Niño event and human induced climate change may interact and modify each other in ways which we have \u003ca href=\"https://www.wmo.int/media/content/weather-reports-future-0\" target=\"_blank\" rel=\"noopener\">never before experienced\u003c/a>,” said WMO Secretary-General Michel Jarraud.\u003c/p>\n\u003cp>\u003cstrong>‘An Icon of Climate Change’\u003c/strong>\u003c/p>\n\u003cp>When scientists talk about atmospheric CO\u003csub>2\u003c/sub>, their yardstick is the so-called Keeling curve. It’s the record of the air’s composition, made each day at a station run by the \u003ca href=\"http://scrippsco2.ucsd.edu/\" target=\"_blank\" rel=\"noopener\">Scripps Institution of Oceanography\u003c/a> in the pure air high on Mauna Loa volcano, in Hawaii.\u003c/p>\n\u003cfigure id=\"attachment_364994\" class=\"wp-caption alignright\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-this-week.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-364994\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-this-week-800x480.png\" alt=\"CO2 at Mauna Loa this week\" width=\"800\" height=\"480\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-this-week-800x480.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-this-week-400x240.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-this-week-960x576.png 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-this-week.png 1000w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">This week’s carbon dioxide readings at the Mauna Loa Observatory are updated every day. As they rise above the 400 parts-per-million threshold, scientists warn that they will not return to it in our lifetimes. \u003ccite>(Scripps/UC San Diego)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Ralph Keeling, the custodian of the CO\u003csub>2\u003c/sub> record, made his prediction last week in \u003ca href=\"https://scripps.ucsd.edu/programs/keelingcurve/2015/10/21/is-this-the-last-year-below-400/\" target=\"_blank\" rel=\"noopener\">a blog post on the Keeling Curve website\u003c/a>.\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>The Keeling curve was started in 1958 under the direction of Keeling’s father, Charles David “Dave” Keeling. Today it’s the longest series of such measurements in the world. It was named a \u003ca href=\"http://www.acs.org/content/acs/en/education/whatischemistry/landmarks/landmarksdirectory.html\" target=\"_blank\" rel=\"noopener\">National Historic Chemical Landmark\u003c/a> this year.\u003c/p>\n\u003cp>The Keeling curve is an icon of climate change. What does it show?\u003c/p>\n\u003cp>In the 1960s, Dave Keeling’s measurements showed that the CO\u003csub>2\u003c/sub> level in the air was rising steadily. That long-term increase is the mark of human influence. It comes overwhelmingly \u003ca href=\"http://www.esrl.noaa.gov/gmd/ccgg/trends/ff.html\" target=\"_blank\" rel=\"noopener\">from the fossil fuels we burn\u003c/a> — largely to generate electricity, but also to smelt metals, produce cement, run motors and so on. Other smaller sources of CO\u003csub>2\u003c/sub> are from humans cutting down forests and from large-scale mechanical farming, which removes most of the carbon-rich humus contained in soil.\u003c/p>\n\u003cp>Since the 1960s, the long-term increase in CO\u003csub>2\u003c/sub> has sped up. A little over half of the CO\u003csub>2\u003c/sub> we produce is absorbed by the ocean and by growing plants. The rest stays in the air and acts as a greenhouse gas.\u003c/p>\n\u003cfigure id=\"attachment_365502\" class=\"wp-caption alignright\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/mauna-loa2.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-365502\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/mauna-loa2.jpg\" alt=\"NOAA's Mauna Loa Observatory on Hawaii, a small collection of buildings where scientists take key measurements on air and sunlight.\" width=\"640\" height=\"480\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/mauna-loa2.jpg 640w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/mauna-loa2-400x300.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">NOAA’s Mauna Loa Observatory on Hawaii, a small collection of buildings where scientists take key measurements on air and sunlight. \u003ccite>(NOAA)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>If CO\u003csub>2\u003c/sub> weren’t a greenhouse gas, we might welcome it for promoting plant growth. But because it is one, higher CO\u003csub>2\u003c/sub> levels will make Earth steadily warmer until either human ingenuity or geology can bring them back down.\u003c/p>\n\u003cp>What led to Ralph Keeling’s prediction, and the significance of this week? That stems from another of Dave Keeling’s early discoveries — the CO\u003csub>2\u003c/sub> curve also goes through a yearly cycle, rising to a peak around May and falling to a low around October.\u003c/p>\n\u003cp>The yearly cycle is a signal of natural life. Plants absorb CO\u003csub>2\u003c/sub> from the air during the growing season, then release it as they are eaten or die back. Because most of Earth’s land area is in the northern hemisphere, the yearly cycle is dominated by the seasons in the north.\u003c/p>\n\u003cp>But this year we have \u003ca href=\"https://wunderground.atavist.com/el-nino-forecast\" target=\"_blank\" rel=\"noopener\">a record-breaking El Niño\u003c/a> in the cycle, triggering drought in the tropics and hampering plant growth there, and fueling widespread forest fires that pour CO\u003csub>2\u003c/sub> into the air. The forest grows back, but not in time for next summer.\u003c/p>\n\u003cfigure id=\"attachment_364992\" class=\"wp-caption alignleft\" style=\"max-width: 398px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-two-years.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-364992\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-two-years-800x454.png\" alt=\"CO2 at L+Mauna Loa, 2014-2015\" width=\"398\" height=\"226\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-two-years-800x454.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-two-years-400x227.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-two-years.png 900w\" sizes=\"(max-width: 398px) 100vw, 398px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Atmospheric CO\u003csub>2\u003c/sub> at the Mauna Loa Observatory in the last two years. \u003ccite>(Scripps/UC San Diego)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>So Ralph Keeling predicts the annual summer dip won’t bring readings back down into the 390s, as it did in 2014 and 2015.\u003c/p>\n\u003cp>“Will daily values at Mauna Loa ever fall below 400 ppm again in our lifetimes?” Keeling asked. “I’m prepared to project that they won’t, making the current values the last time the Mauna Loa record will produce numbers in the 300s.”\u003c/p>\n\u003cp>Meanwhile the stubborn long-term climb caused by humans shows no sign of slackening.\u003c/p>\n\u003cp>\u003cstrong>Change Can Happen, But Are We Willing?\u003cbr>\n\u003c/strong>\u003cbr>\nIn the 1700s, before coal began to be burned for industrial processes, CO\u003csub>2\u003c/sub> was at about 280 ppm.\u003c/p>\n\u003cp>The long-term upward trend has never gone down since the Keeling measurements began. The only way to make the climb stop is to burn less carbon and, at the same time, fix more carbon. Burning less means changing our economic system severely and rapidly. It can be done, but the change will be profound.\u003c/p>\n\u003cfigure id=\"attachment_364991\" class=\"wp-caption alignright\" style=\"max-width: 492px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-since-1958.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-364991\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-since-1958-800x480.png\" alt=\"Full record from Mauna Loa\" width=\"492\" height=\"295\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-since-1958-800x480.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-since-1958-400x240.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-since-1958-960x576.png 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-since-1958.png 1000w\" sizes=\"(max-width: 492px) 100vw, 492px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Rise in atmospheric CO2 at the Mauna Loa Observatory since March 1958. \u003ccite>(Scripps/UC San Diego)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Fixing more carbon is a project with many options, most of which involve burying CO\u003csub>2\u003c/sub> underground. One promising frontier is working with the natural carbon cycle to increase the world’s biomass. Restoring the soil, by reforming our farming practices, could help turn the Keeling curve back toward 400 and below, once again. That, too, would be a profound change.\u003c/p>\n\u003cp>Eventually, geology will take care of the atmosphere through the \u003ci>really\u003c/i> long-term carbon cycle. First the ocean will stir excess CO\u003csub>2\u003c/sub> throughout its deepest waters. That will take on the order of 1,000 years.\u003c/p>\n\u003cp>Second, the erosion of rocks will fertilize the sea with dissolved carbon minerals, which plankton will use to make their microscopic shells, which will fall to the seafloor as the plankton die and be buried. It’s a roundabout system, but that’s how the Earth works. That will take many thousands of years.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>We probably can’t wait that long.\u003c/p>\n\n",
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"bio": "Andrew Alden earned his geology degree at the University of New Hampshire and moved back to the Bay Area to work at the U.S. Geological Survey for six years. He has \u003ca href=\"http://geology.about.com/\">written on geology for About.com\u003c/a> since its founding in 1997. In 2007, he started the Oakland Geology blog, which won recognition as \"Best of the East Bay\" from the \u003ci>East Bay Express\u003c/i> in 2010. In writing about geology in the Bay Area and surroundings, he hopes to share some of the useful and pleasurable insights that geologists give us—not just facts about the deep past, but an attitude that might be called the \u003ci>deep present\u003c/i>.\r\n\r\nRead his \u003ca href=\"http://science.kqed.org/quest/author/andrew-alden/\">previous contributions\u003c/a> to \u003ca href=\"http://http://science.kqed.org/quest/\">QUEST\u003c/a>, a project dedicated to exploring the Science of Sustainability.",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>This week, \u003ca href=\"https://scripps.ucsd.edu/programs/keelingcurve/\" target=\"_blank\" rel=\"noopener\">you can watch\u003c/a> as Earth passes a threshold not seen for at least a million years. The concentration of carbon dioxide in the air will rise above 400 parts per million. And scientists predict neither you nor your children will ever see it go below 400 ppm again.\u003c/p>\n\u003cp>The World Meteorological Organization (WMO) said on Monday that this year’s El Niño combined with global warming puts the world “\u003ca href=\"https://www.wmo.int/media/content/el-ni%C3%B1o-expected-strengthen-further-high-impacts-unprecedented-preparation\" target=\"_blank\" rel=\"noopener\">in uncharted territory\u003c/a>.”\u003c/p>\n\u003cp>“This naturally occurring El Niño event and human induced climate change may interact and modify each other in ways which we have \u003ca href=\"https://www.wmo.int/media/content/weather-reports-future-0\" target=\"_blank\" rel=\"noopener\">never before experienced\u003c/a>,” said WMO Secretary-General Michel Jarraud.\u003c/p>\n\u003cp>\u003cstrong>‘An Icon of Climate Change’\u003c/strong>\u003c/p>\n\u003cp>When scientists talk about atmospheric CO\u003csub>2\u003c/sub>, their yardstick is the so-called Keeling curve. It’s the record of the air’s composition, made each day at a station run by the \u003ca href=\"http://scrippsco2.ucsd.edu/\" target=\"_blank\" rel=\"noopener\">Scripps Institution of Oceanography\u003c/a> in the pure air high on Mauna Loa volcano, in Hawaii.\u003c/p>\n\u003cfigure id=\"attachment_364994\" class=\"wp-caption alignright\" style=\"max-width: 800px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-this-week.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-364994\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-this-week-800x480.png\" alt=\"CO2 at Mauna Loa this week\" width=\"800\" height=\"480\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-this-week-800x480.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-this-week-400x240.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-this-week-960x576.png 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-this-week.png 1000w\" sizes=\"(max-width: 800px) 100vw, 800px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">This week’s carbon dioxide readings at the Mauna Loa Observatory are updated every day. As they rise above the 400 parts-per-million threshold, scientists warn that they will not return to it in our lifetimes. \u003ccite>(Scripps/UC San Diego)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Ralph Keeling, the custodian of the CO\u003csub>2\u003c/sub> record, made his prediction last week in \u003ca href=\"https://scripps.ucsd.edu/programs/keelingcurve/2015/10/21/is-this-the-last-year-below-400/\" target=\"_blank\" rel=\"noopener\">a blog post on the Keeling Curve website\u003c/a>.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>The Keeling curve was started in 1958 under the direction of Keeling’s father, Charles David “Dave” Keeling. Today it’s the longest series of such measurements in the world. It was named a \u003ca href=\"http://www.acs.org/content/acs/en/education/whatischemistry/landmarks/landmarksdirectory.html\" target=\"_blank\" rel=\"noopener\">National Historic Chemical Landmark\u003c/a> this year.\u003c/p>\n\u003cp>The Keeling curve is an icon of climate change. What does it show?\u003c/p>\n\u003cp>In the 1960s, Dave Keeling’s measurements showed that the CO\u003csub>2\u003c/sub> level in the air was rising steadily. That long-term increase is the mark of human influence. It comes overwhelmingly \u003ca href=\"http://www.esrl.noaa.gov/gmd/ccgg/trends/ff.html\" target=\"_blank\" rel=\"noopener\">from the fossil fuels we burn\u003c/a> — largely to generate electricity, but also to smelt metals, produce cement, run motors and so on. Other smaller sources of CO\u003csub>2\u003c/sub> are from humans cutting down forests and from large-scale mechanical farming, which removes most of the carbon-rich humus contained in soil.\u003c/p>\n\u003cp>Since the 1960s, the long-term increase in CO\u003csub>2\u003c/sub> has sped up. A little over half of the CO\u003csub>2\u003c/sub> we produce is absorbed by the ocean and by growing plants. The rest stays in the air and acts as a greenhouse gas.\u003c/p>\n\u003cfigure id=\"attachment_365502\" class=\"wp-caption alignright\" style=\"max-width: 640px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/mauna-loa2.jpg\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-365502\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/mauna-loa2.jpg\" alt=\"NOAA's Mauna Loa Observatory on Hawaii, a small collection of buildings where scientists take key measurements on air and sunlight.\" width=\"640\" height=\"480\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/mauna-loa2.jpg 640w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/mauna-loa2-400x300.jpg 400w\" sizes=\"(max-width: 640px) 100vw, 640px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">NOAA’s Mauna Loa Observatory on Hawaii, a small collection of buildings where scientists take key measurements on air and sunlight. \u003ccite>(NOAA)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>If CO\u003csub>2\u003c/sub> weren’t a greenhouse gas, we might welcome it for promoting plant growth. But because it is one, higher CO\u003csub>2\u003c/sub> levels will make Earth steadily warmer until either human ingenuity or geology can bring them back down.\u003c/p>\n\u003cp>What led to Ralph Keeling’s prediction, and the significance of this week? That stems from another of Dave Keeling’s early discoveries — the CO\u003csub>2\u003c/sub> curve also goes through a yearly cycle, rising to a peak around May and falling to a low around October.\u003c/p>\n\u003cp>The yearly cycle is a signal of natural life. Plants absorb CO\u003csub>2\u003c/sub> from the air during the growing season, then release it as they are eaten or die back. Because most of Earth’s land area is in the northern hemisphere, the yearly cycle is dominated by the seasons in the north.\u003c/p>\n\u003cp>But this year we have \u003ca href=\"https://wunderground.atavist.com/el-nino-forecast\" target=\"_blank\" rel=\"noopener\">a record-breaking El Niño\u003c/a> in the cycle, triggering drought in the tropics and hampering plant growth there, and fueling widespread forest fires that pour CO\u003csub>2\u003c/sub> into the air. The forest grows back, but not in time for next summer.\u003c/p>\n\u003cfigure id=\"attachment_364992\" class=\"wp-caption alignleft\" style=\"max-width: 398px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-two-years.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-364992\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-two-years-800x454.png\" alt=\"CO2 at L+Mauna Loa, 2014-2015\" width=\"398\" height=\"226\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-two-years-800x454.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-two-years-400x227.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-two-years.png 900w\" sizes=\"(max-width: 398px) 100vw, 398px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Atmospheric CO\u003csub>2\u003c/sub> at the Mauna Loa Observatory in the last two years. \u003ccite>(Scripps/UC San Diego)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>So Ralph Keeling predicts the annual summer dip won’t bring readings back down into the 390s, as it did in 2014 and 2015.\u003c/p>\n\u003cp>“Will daily values at Mauna Loa ever fall below 400 ppm again in our lifetimes?” Keeling asked. “I’m prepared to project that they won’t, making the current values the last time the Mauna Loa record will produce numbers in the 300s.”\u003c/p>\n\u003cp>Meanwhile the stubborn long-term climb caused by humans shows no sign of slackening.\u003c/p>\n\u003cp>\u003cstrong>Change Can Happen, But Are We Willing?\u003cbr>\n\u003c/strong>\u003cbr>\nIn the 1700s, before coal began to be burned for industrial processes, CO\u003csub>2\u003c/sub> was at about 280 ppm.\u003c/p>\n\u003cp>The long-term upward trend has never gone down since the Keeling measurements began. The only way to make the climb stop is to burn less carbon and, at the same time, fix more carbon. Burning less means changing our economic system severely and rapidly. It can be done, but the change will be profound.\u003c/p>\n\u003cfigure id=\"attachment_364991\" class=\"wp-caption alignright\" style=\"max-width: 492px\">\u003ca href=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-since-1958.png\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\" wp-image-364991\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2015/11/CO2-since-1958-800x480.png\" alt=\"Full record from Mauna Loa\" width=\"492\" height=\"295\" srcset=\"https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-since-1958-800x480.png 800w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-since-1958-400x240.png 400w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-since-1958-960x576.png 960w, https://cdn.kqed.org/wp-content/uploads/sites/35/2015/11/CO2-since-1958.png 1000w\" sizes=\"(max-width: 492px) 100vw, 492px\">\u003c/a>\u003cfigcaption class=\"wp-caption-text\">Rise in atmospheric CO2 at the Mauna Loa Observatory since March 1958. \u003ccite>(Scripps/UC San Diego)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Fixing more carbon is a project with many options, most of which involve burying CO\u003csub>2\u003c/sub> underground. One promising frontier is working with the natural carbon cycle to increase the world’s biomass. Restoring the soil, by reforming our farming practices, could help turn the Keeling curve back toward 400 and below, once again. That, too, would be a profound change.\u003c/p>\n\u003cp>Eventually, geology will take care of the atmosphere through the \u003ci>really\u003c/i> long-term carbon cycle. First the ocean will stir excess CO\u003csub>2\u003c/sub> throughout its deepest waters. That will take on the order of 1,000 years.\u003c/p>\n\u003cp>Second, the erosion of rocks will fertilize the sea with dissolved carbon minerals, which plankton will use to make their microscopic shells, which will fall to the seafloor as the plankton die and be buried. It’s a roundabout system, but that’s how the Earth works. That will take many thousands of years.\u003c/p>\n\u003cp>\u003c/p>\n\u003cp>We probably can’t wait that long.\u003c/p>\n\n\u003c/div>\u003c/p>",
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"info": "Possible is hosted by entrepreneur Reid Hoffman and writer Aria Finger. Together in Possible, Hoffman and Finger lead enlightening discussions about building a brighter collective future. The show features interviews with visionary guests like Trevor Noah, Sam Altman and Janette Sadik-Khan. Possible paints an optimistic portrait of the world we can create through science, policy, business, art and our shared humanity. It asks: What if everything goes right for once? How can we get there? Each episode also includes a short fiction story generated by advanced AI GPT-4, serving as a thought-provoking springboard to speculate how humanity could leverage technology for good.",
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"info": "1A is home to the national conversation. 1A brings on great guests and frames the best debate in ways that make you think, share and engage.",
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"officialWebsiteLink": "https://the1a.org/",
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"info": "Every weekday, \u003cem>All Things Considered\u003c/em> hosts Robert Siegel, Audie Cornish, Ari Shapiro, and Kelly McEvers present the program's trademark mix of news, interviews, commentaries, reviews, and offbeat features. Michel Martin hosts on the weekends.",
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"title": "American Suburb: The Podcast",
"tagline": "The flip side of gentrification, told through one town",
"info": "Gentrification is changing cities across America, forcing people from neighborhoods they have long called home. Call them the displaced. Now those priced out of the Bay Area are looking for a better life in an unlikely place. American Suburb follows this migration to one California town along the Delta, 45 miles from San Francisco. But is this once sleepy suburb ready for them?",
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"order": 19
},
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"baycurious": {
"id": "baycurious",
"title": "Bay Curious",
"tagline": "Exploring the Bay Area, one question at a time",
"info": "KQED’s new podcast, Bay Curious, gets to the bottom of the mysteries — both profound and peculiar — that give the Bay Area its unique identity. And we’ll do it with your help! You ask the questions. You decide what Bay Curious investigates. And you join us on the journey to find the answers.",
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"order": 4
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"info": "The day's top stories from BBC News compiled twice daily in the week, once at weekends.",
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"tuneIn": "https://tunein.com/radio/BBC-World-Service-p455581/",
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"code-switch-life-kit": {
"id": "code-switch-life-kit",
"title": "Code Switch / Life Kit",
"info": "\u003cem>Code Switch\u003c/em>, which listeners will hear in the first part of the hour, has fearless and much-needed conversations about race. Hosted by journalists of color, the show tackles the subject of race head-on, exploring how it impacts every part of society — from politics and pop culture to history, sports and more.\u003cbr />\u003cbr />\u003cem>Life Kit\u003c/em>, which will be in the second part of the hour, guides you through spaces and feelings no one prepares you for — from finances to mental health, from workplace microaggressions to imposter syndrome, from relationships to parenting. The show features experts with real world experience and shares their knowledge. Because everyone needs a little help being human.\u003cbr />\u003cbr />\u003ca href=\"https://www.npr.org/podcasts/510312/codeswitch\">\u003cem>Code Switch\u003c/em> offical site and podcast\u003c/a>\u003cbr />\u003ca href=\"https://www.npr.org/lifekit\">\u003cem>Life Kit\u003c/em> offical site and podcast\u003c/a>\u003cbr />",
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"id": "commonwealth-club",
"title": "Commonwealth Club of California Podcast",
"info": "The Commonwealth Club of California is the nation's oldest and largest public affairs forum. As a non-partisan forum, The Club brings to the public airwaves diverse viewpoints on important topics. The Club's weekly radio broadcast - the oldest in the U.S., dating back to 1924 - is carried across the nation on public radio stations and is now podcasting. Our website archive features audio of our recent programs, as well as selected speeches from our long and distinguished history. This podcast feed is usually updated twice a week and is always un-edited.",
"airtime": "THU 10pm, FRI 1am",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Commonwealth-Club-Podcast-Tile-360x360-1.jpg",
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"source": "Commonwealth Club of California"
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"info": "KQED’s live call-in program discussing local, state, national and international issues, as well as in-depth interviews.",
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"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Forum-Podcast-Tile-703x703-1.jpg",
"imageAlt": "KQED Forum with Mina Kim and Alexis Madrigal",
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"source": "kqed",
"order": 10
},
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"google": "https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5tZWdhcGhvbmUuZm0vS1FJTkM5NTU3MzgxNjMz",
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},
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"id": "freakonomics-radio",
"title": "Freakonomics Radio",
"info": "Freakonomics Radio is a one-hour award-winning podcast and public-radio project hosted by Stephen Dubner, with co-author Steve Levitt as a regular guest. It is produced in partnership with WNYC.",
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"officialWebsiteLink": "http://freakonomics.com/",
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"meta": {
"site": "radio",
"source": "WNYC"
},
"link": "/radio/program/freakonomics-radio",
"subscribe": {
"npr": "https://rpb3r.app.goo.gl/4s8b",
"apple": "https://itunes.apple.com/us/podcast/freakonomics-radio/id354668519",
"tuneIn": "https://tunein.com/podcasts/WNYC-Podcasts/Freakonomics-Radio-p272293/",
"rss": "https://feeds.feedburner.com/freakonomicsradio"
}
},
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"id": "fresh-air",
"title": "Fresh Air",
"info": "Hosted by Terry Gross, \u003cem>Fresh Air from WHYY\u003c/em> is the Peabody Award-winning weekday magazine of contemporary arts and issues. One of public radio's most popular programs, Fresh Air features intimate conversations with today's biggest luminaries.",
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"officialWebsiteLink": "https://www.npr.org/programs/fresh-air/",
"meta": {
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"link": "/radio/program/fresh-air",
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"apple": "https://itunes.apple.com/WebObjects/MZStore.woa/wa/viewPodcast?s=143441&mt=2&id=214089682&at=11l79Y&ct=nprdirectory",
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"title": "Here & Now",
"info": "A live production of NPR and WBUR Boston, in collaboration with stations across the country, Here & Now reflects the fluid world of news as it's happening in the middle of the day, with timely, in-depth news, interviews and conversation. Hosted by Robin Young, Jeremy Hobson and Tonya Mosley.",
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"rss": "https://feeds.npr.org/510051/podcast.xml"
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},
"how-i-built-this": {
"id": "how-i-built-this",
"title": "How I Built This with Guy Raz",
"info": "Guy Raz dives into the stories behind some of the world's best known companies. How I Built This weaves a narrative journey about innovators, entrepreneurs and idealists—and the movements they built.",
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"officialWebsiteLink": "https://www.npr.org/podcasts/510313/how-i-built-this",
"airtime": "SUN 7:30pm-8pm",
"meta": {
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"link": "/radio/program/how-i-built-this",
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},
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"id": "inside-europe",
"title": "Inside Europe",
"info": "Inside Europe, a one-hour weekly news magazine hosted by Helen Seeney and Keith Walker, explores the topical issues shaping the continent. No other part of the globe has experienced such dynamic political and social change in recent years.",
"airtime": "SAT 3am-4am",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Inside-Europe-Podcast-Tile-300x300-1.jpg",
"meta": {
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"source": "Deutsche Welle"
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"link": "/radio/program/inside-europe",
"subscribe": {
"apple": "https://itunes.apple.com/us/podcast/inside-europe/id80106806?mt=2",
"tuneIn": "https://tunein.com/radio/Inside-Europe-p731/",
"rss": "https://partner.dw.com/xml/podcast_inside-europe"
}
},
"latino-usa": {
"id": "latino-usa",
"title": "Latino USA",
"airtime": "MON 1am-2am, SUN 6pm-7pm",
"info": "Latino USA, the radio journal of news and culture, is the only national, English-language radio program produced from a Latino perspective.",
"imageSrc": "https://ww2.kqed.org/radio/wp-content/uploads/sites/50/2018/04/latinoUsa.jpg",
"officialWebsiteLink": "http://latinousa.org/",
"meta": {
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"link": "/radio/program/latino-usa",
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"apple": "https://itunes.apple.com/WebObjects/MZStore.woa/wa/viewPodcast?s=143441&mt=2&id=79681317&at=11l79Y&ct=nprdirectory",
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"rss": "https://feeds.npr.org/510016/podcast.xml"
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},
"live-from-here-highlights": {
"id": "live-from-here-highlights",
"title": "Live from Here Highlights",
"info": "Chris Thile steps to the mic as the host of Live from Here (formerly A Prairie Home Companion), a live public radio variety show. Download Chris’s Song of the Week plus other highlights from the broadcast. Produced by American Public Media.",
"airtime": "SAT 6pm-8pm, SUN 11am-1pm",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Live-From-Here-Podcast-Tile-360x360-1.jpg",
"officialWebsiteLink": "https://www.livefromhere.org/",
"meta": {
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"source": "american public media"
},
"link": "/radio/program/live-from-here-highlights",
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"tuneIn": "https://tunein.com/radio/Live-from-Here-Highlights-p921744/",
"rss": "https://feeds.publicradio.org/public_feeds/a-prairie-home-companion-highlights/rss/rss"
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},
"marketplace": {
"id": "marketplace",
"title": "Marketplace",
"info": "Our flagship program, helmed by Kai Ryssdal, examines what the day in money delivered, through stories, conversations, newsworthy numbers and more. Updated Monday through Friday at about 3:30 p.m. PT.",
"airtime": "MON-FRI 4pm-4:30pm, MON-WED 6:30pm-7pm",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Marketplace-Podcast-Tile-360x360-1.jpg",
"officialWebsiteLink": "https://www.marketplace.org/",
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"source": "American Public Media"
},
"link": "/radio/program/marketplace",
"subscribe": {
"apple": "https://itunes.apple.com/WebObjects/MZStore.woa/wa/viewPodcast?s=143441&mt=2&id=201853034&at=11l79Y&ct=nprdirectory",
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},
"mindshift": {
"id": "mindshift",
"title": "MindShift",
"tagline": "A podcast about the future of learning and how we raise our kids",
"info": "The MindShift podcast explores the innovations in education that are shaping how kids learn. Hosts Ki Sung and Katrina Schwartz introduce listeners to educators, researchers, parents and students who are developing effective ways to improve how kids learn. We cover topics like how fed-up administrators are developing surprising tactics to deal with classroom disruptions; how listening to podcasts are helping kids develop reading skills; the consequences of overparenting; and why interdisciplinary learning can engage students on all ends of the traditional achievement spectrum. This podcast is part of the MindShift education site, a division of KQED News. KQED is an NPR/PBS member station based in San Francisco. You can also visit the MindShift website for episodes and supplemental blog posts or tweet us \u003ca href=\"https://twitter.com/MindShiftKQED\">@MindShiftKQED\u003c/a> or visit us at \u003ca href=\"/mindshift\">MindShift.KQED.org\u003c/a>",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Mindshift-Podcast-Tile-703x703-1.jpg",
"imageAlt": "KQED MindShift: How We Will Learn",
"officialWebsiteLink": "/mindshift/",
"meta": {
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"source": "kqed",
"order": 13
},
"link": "/podcasts/mindshift",
"subscribe": {
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"google": "https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5tZWdhcGhvbmUuZm0vS1FJTkM1NzY0NjAwNDI5",
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}
},
"morning-edition": {
"id": "morning-edition",
"title": "Morning Edition",
"info": "\u003cem>Morning Edition\u003c/em> takes listeners around the country and the world with multi-faceted stories and commentaries every weekday. Hosts Steve Inskeep, David Greene and Rachel Martin bring you the latest breaking news and features to prepare you for the day.",
"airtime": "MON-FRI 3am-9am",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/Morning-Edition-Podcast-Tile-360x360-1.jpg",
"officialWebsiteLink": "https://www.npr.org/programs/morning-edition/",
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"onourwatch": {
"id": "onourwatch",
"title": "On Our Watch",
"tagline": "Deeply-reported investigative journalism",
"info": "For decades, the process for how police police themselves has been inconsistent – if not opaque. In some states, like California, these proceedings were completely hidden. After a new police transparency law unsealed scores of internal affairs files, our reporters set out to examine these cases and the shadow world of police discipline. On Our Watch brings listeners into the rooms where officers are questioned and witnesses are interrogated to find out who this system is really protecting. Is it the officers, or the public they've sworn to serve?",
"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/On-Our-Watch-Podcast-Tile-703x703-1.jpg",
"imageAlt": "On Our Watch from NPR and KQED",
"officialWebsiteLink": "/podcasts/onourwatch",
"meta": {
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"source": "kqed",
"order": 12
},
"link": "/podcasts/onourwatch",
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"google": "https://podcasts.google.com/feed/aHR0cHM6Ly9mZWVkcy5ucHIub3JnLzUxMDM2MC9wb2RjYXN0LnhtbD9zYz1nb29nbGVwb2RjYXN0cw",
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"stitcher": "https://www.stitcher.com/show/on-our-watch",
"rss": "https://feeds.npr.org/510360/podcast.xml"
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},
"on-the-media": {
"id": "on-the-media",
"title": "On The Media",
"info": "Our weekly podcast explores how the media 'sausage' is made, casts an incisive eye on fluctuations in the marketplace of ideas, and examines threats to the freedom of information and expression in America and abroad. For one hour a week, the show tries to lift the veil from the process of \"making media,\" especially news media, because it's through that lens that we see the world and the world sees us",
"airtime": "SUN 2pm-3pm, MON 12am-1am",
"imageSrc": "https://ww2.kqed.org/radio/wp-content/uploads/sites/50/2018/04/onTheMedia.png",
"officialWebsiteLink": "https://www.wnycstudios.org/shows/otm",
"meta": {
"site": "news",
"source": "wnyc"
},
"link": "/radio/program/on-the-media",
"subscribe": {
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"tuneIn": "https://tunein.com/radio/On-the-Media-p69/",
"rss": "http://feeds.wnyc.org/onthemedia"
}
},
"our-body-politic": {
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