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"title": "El Niño: It's One For the Books -- But Not Behaving As Expected",
"headTitle": "El Niño: It’s One For the Books — But Not Behaving As Expected | KQED",
"content": "\u003cp>The prospect of an El Niño event in the Pacific Ocean always generates a stew of excitement, dread, and speculation in California. This largely stems from the fact that two of California’s wettest winters on record — 1982-1983 and 1997-1998 — occurred during the strongest El Niño years in living memory. The popular perception that El Niño always brings a lot of water to the Golden State, though, is not particularly accurate.\u003c/p>\n\u003cp>The key message here: \u003ca href=\"http://ww2.kqed.org/science/2014/09/01/drought-myth-busting-why-el-nino-wont-save-california/\">strong El Niño events are the ones to watch\u003c/a> out for from a California weather perspective, and it’s reasonable to expect that such events greatly increase the odds of wet conditions throughout the state.\u003c/p>\n\u003cfigure id=\"attachment_502362\" class=\"wp-caption alignright\" style=\"max-width: 565px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-502362\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/01/fig1.gif\" alt=\"Subtropical ridging between Hawaii and California has been more prominent so far during 2015-2016 than during the 82/83 or 97/98 events.\" width=\"565\" height=\"437\">\u003cfigcaption class=\"wp-caption-text\">Subtropical “ridging” between Hawaii and California has been more prominent so far during 2015-2016 than during the 82/83 or 97/98 events. \u003ccite>(NCEP via ESRL)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>\u003cstrong>How is this El Niño different from other ‘Big Ones?’\u003cbr>\n\u003c/strong>\u003c/p>\n\u003cp>Depending on how you measure it, the present El Niño is either the strongest or among the strongest events in the observed record going back to at least 1950. Ocean temperatures in the eastern equatorial Pacific Ocean — the most traditional measure of El Niño’s amplitude — have been at or above record-high values for at least several months now. So despite assertions to the contrary, the 2015-2016 El Niño is not “a bust” by any means.\u003c/p>\n\u003cp>But absolute sea surface temperatures don’t always tell the whole story. While the present El Niño is indeed among the strongest ever recorded, the atmospheric response to the warm ocean temperatures this year has been a bit different than we have observed during other big historical events. Over the northeastern Pacific, El Niño acts to deepen the \u003ca href=\"http://earthobservatory.nasa.gov/NaturalHazards/view.php?id=13718\">semi-permanent Gulf of Alaska low-pressure\u003c/a> zone while simultaneously strengthening (and, literally, straightening) the \u003ca href=\"http://www.livescience.com/27825-jet-stream.html\">jet stream\u003c/a> over the eastern Pacific Ocean. This enhanced and “more zonal” (i.e. more west-to-east) jet stream is what tends to bring increased winter precipitation to California (and, sometimes, as we’re seeing now, even the Pacific Northwest) during strong El Niño years.\u003c/p>\n\u003cfigure id=\"attachment_502363\" class=\"wp-caption alignright\" style=\"max-width: 565px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-502363\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/01/fig2.gif\" alt=\"Tropical convection associated with the 2015-2016 El Niño has been centered further north than in previous big events, with subsidence (downward motion) occurring closer to California on its northern flank.\" width=\"565\" height=\"437\">\u003cfigcaption class=\"wp-caption-text\">Tropical convection associated with the 2015-2016 El Niño has been centered farther north than in previous big events, with subsidence (downward motion) occurring closer to California on its northern flank. \u003ccite>(NCEP via ESRL)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Tropical convection associated with the 2015-2016 El Niño has been centered further north than in previous big events, with subsidence (downward motion; yellow/red colors) occurring closer to California on its northern flank\u003c/p>\n\u003cp>[ad fullwidth]\u003c/p>\n\u003cp>These atmospheric effects are the product of a fairly complex chain of events that link the tropical to the mid-latitude atmosphere. Warmer-than-usual ocean temperatures in the eastern tropical Pacific increase thunderstorm activity there, which pumps vast quantities of heat into the upper atmosphere. This tropically warm air at upper levels eventually flows northward and drops back toward the surface of the Earth in the subtropics (at a latitude roughly equivalent to that of Hawaii). This enhanced “\u003ca href=\"https://www.seas.harvard.edu/climate/eli/research/equable/hadley.html\">Hadley circulation\u003c/a>” during El Niño years increases the temperature differential between the warm tropics and cool Gulf of Alaska, which is what causes the jet stream to strengthen.\u003c/p>\n\u003cp>\u003cstrong>Skipping the Southland\u003c/strong>\u003c/p>\n\u003cp>In late 2015 and early 2016, the atmosphere has responded to the ongoing powerful El Niño much in the way that meteorologists have come to expect. The Pacific warmed; tropical thunderstorms increased; the Hadley cell strengthened; the Pacific jet began to roar. But this year, the Hadley cell has actually strengthened a bit more than expected. The descending air on its northern side has occurred closer to California, which means that enhanced temperature differential is occurring farther to the north than during previous big El Niño events. Subtropical ridging between Hawaii and California has been more pronounced, and the El Niño-strengthened jet stream has set up shop primarily across Northern California and \u003ca href=\"http://www.nbcnews.com/news/us-news/flooding-landslides-after-record-rainfall-pounds-pacific-northwest-n475966\">even the Pacific Northwest\u003c/a>, rather than Southern California. From a global climate perspective, this is a relatively minor detail; if you happen to live in Los Angeles, though, it makes all the difference in the world.\u003c/p>\n\u003cp>The net effect so far in 2015-2016: Northern California and the Pacific Northwest have gotten soaked, while Southern California has been left pretty dry (with a few notable exceptions). While a veritable “parade of storms” has indeed inundated the northern reaches of the state with very heavy precipitation, bringing the best \u003ca href=\"http://ww2.kqed.org/news/2015/12/30/sierra-snowpack-survey-drought\">Sierra Nevada snowpack\u003c/a> in years, leading to huge \u003ca href=\"http://ww2.kqed.org/lowdown/2015/09/21/now-that-summers-over-what-do-californias-reservoirs-look-like-a-real-time-visualization/\">inflows to large reservoirs\u003c/a> in critical watersheds, and even leading to some minor flooding at times, many of California’s most populous cities haven’t witnessed an especially remarkable winter to date. The San Francisco Bay Area and Sacramento region have seen “Water Year” precipitation to date that is pretty close to the long-term average (which seems like a lot relative to the extremely dry years witnessed as of late). The densely populated greater Los Angeles region, on the other hand, is well below average for the season to date (though with significant precipitation this past weekend, its January total may well end up near or above average). From a long-term drought relief perspective, the \u003ca href=\"http://www.cnrfc.noaa.gov/awipsProducts/RNOWRKCLI.php\">season to date\u003c/a> looks pretty good—precipitation is near or above average in most of California’s largest watersheds, and the water stored in the \u003ca href=\"http://cdec.water.ca.gov/cdecapp/snowapp/sweq.action\">critical Sierra Nevada snowpack\u003c/a> is uniformly above average. So far, though, this isn’t quite the blockbuster year that many had hoped for (especially in the south).\u003c/p>\n\u003cfigure id=\"attachment_502364\" class=\"wp-caption alignleft\" style=\"max-width: 531px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-502364\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/01/fig3.gif\" alt=\"While nearly all of California is expected to be above average in terms of season-to-date precipitation after this weekend’s Southern California storm, only the northern 2/3 of the state is above average for the full season to date.\" width=\"531\" height=\"688\">\u003cfigcaption class=\"wp-caption-text\">While nearly all of California is expected to be above average in terms of season-to-date precipitation after this weekend’s Southern California storm, only the northern 2/3 of the state is above average for the full season to date.? \u003ccite>(NOAA via WRCC)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>\u003cstrong>So, What Now?\u003c/strong>\u003c/p>\n\u003cp>El Niño is certainly still with us, and it’s still a top-tier event. For that reason, the smart money’s still on a wetter-than-average season for California on balance. This is especially true since the precipitation during strong El Niño years is often heavily “back-weighted,” with an unusually large fraction of seasonal totals occurring during the second half of the rainy season from February to April. What is less clear, at this point, is whether the northerly-shifted atmospheric response to this El Niño will persist — and whether Southern California will start to make up for lost time. It’s certainly possible, and it’s easy to forget that a surprisingly large fraction of precipitation in the Southland occurs during a \u003ca href=\"http://ww2.kqed.org/science/2015/11/23/flying-into-the-heart-of-the-wests-biggest-storms/\">handful of intense storms\u003c/a> each year (even in strong El Niño years). From a statewide perspective, some substantial drought relief has already occurred this year, but there remain large regions in the southern part of the state that are still extremely dry. The refrain from earlier in the autumn is now more relevant than ever: while El Niño is likely to bring some degree of drought relief, California will likely still be facing long-term drought conditions by the coming summer.\u003c/p>\n\u003cp>\u003cstrong>The Big Picture\u003c/strong>\u003c/p>\n\u003cp>Finally, there has been considerable discussion lately regarding why the atmospheric response to El Niño this year has been different than historically observed (and also than foreseen by some of the flagship seasonal forecast models). It’s impossible to ignore the fact that global temperatures in late 2015 and early 2016 have reached their \u003ca href=\"http://ww2.kqed.org/science/2016/01/20/2015-was-the-warmest-year-on-record-globally-but-not-in-california/\">highest levels in recorded human history\u003c/a>. Part of this very recent warming is likely a product of our record El Niño event, but the rest is pretty clearly attributable to the long-term warming trend associated the with human emission of greenhouse gases. While global mean temperature doesn’t directly affect El Niño teleconnections, per se, the Earth hasn’t been warming in a spatially uniform way. This year in particular, the subtropics and the polar regions have been especially warm relative to other parts of the world. It is possible that this spatial pattern of warming may be playing a role in the particular atmospheric configuration that has resulted from the 2015-2016 El Niño event.\u003c/p>\n\u003cp>Unfortunately, it is virtually impossible to say more than that right now. The pace of climate change attribution science is much slower than that of the atmosphere itself, and it’s hard to make causal inferences from observations alone. Climate models are often the best tool available for climate scientists to test the counterfactual: what would this year have looked like without global warming? Such experiments take a considerable amount of time, so we’ll probably have to wait a while to find out. Stay tuned.\u003c/p>\n\u003cp>[ad floatright]\u003c/p>\n\u003cp>\u003cem>Daniel Swain is an atmospheric scientist at Stanford’s School of Earth, Energy & Environmental Sciences. A version of this post also appears on his \u003ca href=\"http://www.weatherwest.com/\">California Weather\u003c/a> blog.\u003c/em>\u003c/p>\n\n",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003cp>The prospect of an El Niño event in the Pacific Ocean always generates a stew of excitement, dread, and speculation in California. This largely stems from the fact that two of California’s wettest winters on record — 1982-1983 and 1997-1998 — occurred during the strongest El Niño years in living memory. The popular perception that El Niño always brings a lot of water to the Golden State, though, is not particularly accurate.\u003c/p>\n\u003cp>The key message here: \u003ca href=\"http://ww2.kqed.org/science/2014/09/01/drought-myth-busting-why-el-nino-wont-save-california/\">strong El Niño events are the ones to watch\u003c/a> out for from a California weather perspective, and it’s reasonable to expect that such events greatly increase the odds of wet conditions throughout the state.\u003c/p>\n\u003cfigure id=\"attachment_502362\" class=\"wp-caption alignright\" style=\"max-width: 565px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-502362\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/01/fig1.gif\" alt=\"Subtropical ridging between Hawaii and California has been more prominent so far during 2015-2016 than during the 82/83 or 97/98 events.\" width=\"565\" height=\"437\">\u003cfigcaption class=\"wp-caption-text\">Subtropical “ridging” between Hawaii and California has been more prominent so far during 2015-2016 than during the 82/83 or 97/98 events. \u003ccite>(NCEP via ESRL)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>\u003cstrong>How is this El Niño different from other ‘Big Ones?’\u003cbr>\n\u003c/strong>\u003c/p>\n\u003cp>Depending on how you measure it, the present El Niño is either the strongest or among the strongest events in the observed record going back to at least 1950. Ocean temperatures in the eastern equatorial Pacific Ocean — the most traditional measure of El Niño’s amplitude — have been at or above record-high values for at least several months now. So despite assertions to the contrary, the 2015-2016 El Niño is not “a bust” by any means.\u003c/p>\n\u003cp>But absolute sea surface temperatures don’t always tell the whole story. While the present El Niño is indeed among the strongest ever recorded, the atmospheric response to the warm ocean temperatures this year has been a bit different than we have observed during other big historical events. Over the northeastern Pacific, El Niño acts to deepen the \u003ca href=\"http://earthobservatory.nasa.gov/NaturalHazards/view.php?id=13718\">semi-permanent Gulf of Alaska low-pressure\u003c/a> zone while simultaneously strengthening (and, literally, straightening) the \u003ca href=\"http://www.livescience.com/27825-jet-stream.html\">jet stream\u003c/a> over the eastern Pacific Ocean. This enhanced and “more zonal” (i.e. more west-to-east) jet stream is what tends to bring increased winter precipitation to California (and, sometimes, as we’re seeing now, even the Pacific Northwest) during strong El Niño years.\u003c/p>\n\u003cfigure id=\"attachment_502363\" class=\"wp-caption alignright\" style=\"max-width: 565px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-502363\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/01/fig2.gif\" alt=\"Tropical convection associated with the 2015-2016 El Niño has been centered further north than in previous big events, with subsidence (downward motion) occurring closer to California on its northern flank.\" width=\"565\" height=\"437\">\u003cfigcaption class=\"wp-caption-text\">Tropical convection associated with the 2015-2016 El Niño has been centered farther north than in previous big events, with subsidence (downward motion) occurring closer to California on its northern flank. \u003ccite>(NCEP via ESRL)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>Tropical convection associated with the 2015-2016 El Niño has been centered further north than in previous big events, with subsidence (downward motion; yellow/red colors) occurring closer to California on its northern flank\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>These atmospheric effects are the product of a fairly complex chain of events that link the tropical to the mid-latitude atmosphere. Warmer-than-usual ocean temperatures in the eastern tropical Pacific increase thunderstorm activity there, which pumps vast quantities of heat into the upper atmosphere. This tropically warm air at upper levels eventually flows northward and drops back toward the surface of the Earth in the subtropics (at a latitude roughly equivalent to that of Hawaii). This enhanced “\u003ca href=\"https://www.seas.harvard.edu/climate/eli/research/equable/hadley.html\">Hadley circulation\u003c/a>” during El Niño years increases the temperature differential between the warm tropics and cool Gulf of Alaska, which is what causes the jet stream to strengthen.\u003c/p>\n\u003cp>\u003cstrong>Skipping the Southland\u003c/strong>\u003c/p>\n\u003cp>In late 2015 and early 2016, the atmosphere has responded to the ongoing powerful El Niño much in the way that meteorologists have come to expect. The Pacific warmed; tropical thunderstorms increased; the Hadley cell strengthened; the Pacific jet began to roar. But this year, the Hadley cell has actually strengthened a bit more than expected. The descending air on its northern side has occurred closer to California, which means that enhanced temperature differential is occurring farther to the north than during previous big El Niño events. Subtropical ridging between Hawaii and California has been more pronounced, and the El Niño-strengthened jet stream has set up shop primarily across Northern California and \u003ca href=\"http://www.nbcnews.com/news/us-news/flooding-landslides-after-record-rainfall-pounds-pacific-northwest-n475966\">even the Pacific Northwest\u003c/a>, rather than Southern California. From a global climate perspective, this is a relatively minor detail; if you happen to live in Los Angeles, though, it makes all the difference in the world.\u003c/p>\n\u003cp>The net effect so far in 2015-2016: Northern California and the Pacific Northwest have gotten soaked, while Southern California has been left pretty dry (with a few notable exceptions). While a veritable “parade of storms” has indeed inundated the northern reaches of the state with very heavy precipitation, bringing the best \u003ca href=\"http://ww2.kqed.org/news/2015/12/30/sierra-snowpack-survey-drought\">Sierra Nevada snowpack\u003c/a> in years, leading to huge \u003ca href=\"http://ww2.kqed.org/lowdown/2015/09/21/now-that-summers-over-what-do-californias-reservoirs-look-like-a-real-time-visualization/\">inflows to large reservoirs\u003c/a> in critical watersheds, and even leading to some minor flooding at times, many of California’s most populous cities haven’t witnessed an especially remarkable winter to date. The San Francisco Bay Area and Sacramento region have seen “Water Year” precipitation to date that is pretty close to the long-term average (which seems like a lot relative to the extremely dry years witnessed as of late). The densely populated greater Los Angeles region, on the other hand, is well below average for the season to date (though with significant precipitation this past weekend, its January total may well end up near or above average). From a long-term drought relief perspective, the \u003ca href=\"http://www.cnrfc.noaa.gov/awipsProducts/RNOWRKCLI.php\">season to date\u003c/a> looks pretty good—precipitation is near or above average in most of California’s largest watersheds, and the water stored in the \u003ca href=\"http://cdec.water.ca.gov/cdecapp/snowapp/sweq.action\">critical Sierra Nevada snowpack\u003c/a> is uniformly above average. So far, though, this isn’t quite the blockbuster year that many had hoped for (especially in the south).\u003c/p>\n\u003cfigure id=\"attachment_502364\" class=\"wp-caption alignleft\" style=\"max-width: 531px\">\u003cimg loading=\"lazy\" decoding=\"async\" class=\"size-full wp-image-502364\" src=\"http://ww2.kqed.org/science/wp-content/uploads/sites/35/2016/01/fig3.gif\" alt=\"While nearly all of California is expected to be above average in terms of season-to-date precipitation after this weekend’s Southern California storm, only the northern 2/3 of the state is above average for the full season to date.\" width=\"531\" height=\"688\">\u003cfigcaption class=\"wp-caption-text\">While nearly all of California is expected to be above average in terms of season-to-date precipitation after this weekend’s Southern California storm, only the northern 2/3 of the state is above average for the full season to date.? \u003ccite>(NOAA via WRCC)\u003c/cite>\u003c/figcaption>\u003c/figure>\n\u003cp>\u003cstrong>So, What Now?\u003c/strong>\u003c/p>\n\u003cp>El Niño is certainly still with us, and it’s still a top-tier event. For that reason, the smart money’s still on a wetter-than-average season for California on balance. This is especially true since the precipitation during strong El Niño years is often heavily “back-weighted,” with an unusually large fraction of seasonal totals occurring during the second half of the rainy season from February to April. What is less clear, at this point, is whether the northerly-shifted atmospheric response to this El Niño will persist — and whether Southern California will start to make up for lost time. It’s certainly possible, and it’s easy to forget that a surprisingly large fraction of precipitation in the Southland occurs during a \u003ca href=\"http://ww2.kqed.org/science/2015/11/23/flying-into-the-heart-of-the-wests-biggest-storms/\">handful of intense storms\u003c/a> each year (even in strong El Niño years). From a statewide perspective, some substantial drought relief has already occurred this year, but there remain large regions in the southern part of the state that are still extremely dry. The refrain from earlier in the autumn is now more relevant than ever: while El Niño is likely to bring some degree of drought relief, California will likely still be facing long-term drought conditions by the coming summer.\u003c/p>\n\u003cp>\u003cstrong>The Big Picture\u003c/strong>\u003c/p>\n\u003cp>Finally, there has been considerable discussion lately regarding why the atmospheric response to El Niño this year has been different than historically observed (and also than foreseen by some of the flagship seasonal forecast models). It’s impossible to ignore the fact that global temperatures in late 2015 and early 2016 have reached their \u003ca href=\"http://ww2.kqed.org/science/2016/01/20/2015-was-the-warmest-year-on-record-globally-but-not-in-california/\">highest levels in recorded human history\u003c/a>. Part of this very recent warming is likely a product of our record El Niño event, but the rest is pretty clearly attributable to the long-term warming trend associated the with human emission of greenhouse gases. While global mean temperature doesn’t directly affect El Niño teleconnections, per se, the Earth hasn’t been warming in a spatially uniform way. This year in particular, the subtropics and the polar regions have been especially warm relative to other parts of the world. It is possible that this spatial pattern of warming may be playing a role in the particular atmospheric configuration that has resulted from the 2015-2016 El Niño event.\u003c/p>\n\u003cp>Unfortunately, it is virtually impossible to say more than that right now. The pace of climate change attribution science is much slower than that of the atmosphere itself, and it’s hard to make causal inferences from observations alone. Climate models are often the best tool available for climate scientists to test the counterfactual: what would this year have looked like without global warming? Such experiments take a considerable amount of time, so we’ll probably have to wait a while to find out. Stay tuned.\u003c/p>\n\u003cp>\u003c/p>\u003c/div>",
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"content": "\u003cdiv class=\"post-body\">\u003cp>\u003c/p>\n\u003cp>\u003cem>Daniel Swain is an atmospheric scientist at Stanford’s School of Earth, Energy & Environmental Sciences. A version of this post also appears on his \u003ca href=\"http://www.weatherwest.com/\">California Weather\u003c/a> blog.\u003c/em>\u003c/p>\n\n\u003c/div>\u003c/p>",
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"info": "What kind of no sabo word is Hyphenación? For us, it’s about living within a hyphenation. Like being a third-gen Mexican-American from the Texas border now living that Bay Area Chicano life. Like Xorje! Each week we bring together a couple of hyphenated Latinos to talk all about personal life choices: family, careers, relationships, belonging … everything is on the table. ",
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"info": "The Political Mind of Jerry Brown brings listeners the wisdom of the former Governor, Mayor, and presidential candidate. Scott Shafer interviewed Brown for more than 40 hours, covering the former governor's life and half-century in the political game – and Brown has some lessons he'd like to share. ",
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"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.",
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"mindshift": {
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"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>",
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"order": 12
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"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?",
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"tagline": "Politics from a personal perspective",
"info": "Political Breakdown is a new series that explores the political intersection of California and the nation. Each week hosts Scott Shafer and Marisa Lagos are joined with a new special guest to unpack politics -- with personality — and offer an insider’s glimpse at how politics happens.",
"airtime": "THU 6:30pm-7pm",
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"possible": {
"id": "possible",
"title": "Possible",
"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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"pri-the-world": {
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"title": "PRI's The World: Latest Edition",
"info": "Each weekday, host Marco Werman and his team of producers bring you the world's most interesting stories in an hour of radio that reminds us just how small our planet really is.",
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"imageSrc": "https://cdn.kqed.org/wp-content/uploads/2024/04/The-World-Podcast-Tile-360x360-1.jpg",
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},
"radiolab": {
"id": "radiolab",
"title": "Radiolab",
"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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},
"reveal": {
"id": "reveal",
"title": "Reveal",
"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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