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    "results": [
        {
            "id": 4272,
            "url": "https://svs.gsfc.nasa.gov/4272/",
            "result_type": "Visualization",
            "release_date": "2015-02-09T00:00:00-05:00",
            "title": "What Would have Happened to the Ozone Layer if Chlorofluorocarbons (CFCs) had not been Regulated? (UPDATED)",
            "description": "World Avoided Ozone Full AnimationThis video is also available on our YouTube channel. || world_avoided_robinson.1830_print.jpg (1024x576) [70.0 KB] || world_avoided_robinson.1830_searchweb.png (180x320) [38.8 KB] || world_avoided_robinson.1830_thm.png (80x40) [4.7 KB] || full_movie (1920x1080) [0 Item(s)] || world_avoided_robinson_1080.mp4 (1920x1080) [26.3 MB] || world_avoided_robinson_1080.webm (1920x1080) [7.2 MB] || world_avoided_robinson_4272.pptx [27.2 MB] || world_avoided_robinson_4272.key [29.8 MB] || world_avoided_robinson_1080.mp4.hwshow || ",
            "hits": 132
        },
        {
            "id": 3667,
            "url": "https://svs.gsfc.nasa.gov/3667/",
            "result_type": "Visualization",
            "release_date": "2010-06-03T00:00:00-04:00",
            "title": "Ship Tracks Reveal Pollution's Effects on Clouds",
            "description": "NASA's MODIS satellite instrument is revealing that humans may be changing our planet's brightness. Pollution in the atmosphere creates smaller, brighter cloud droplets that reflect more sunlight back to space and may have a slight impact on global warming.This narrated visualization illustrates how we can study the effect against a clean backdrop by looking for zones of pollution in otherwise pristine air - in this case the North Pacific Ocean near the Aleutian islands. On an overcast day, the clouds look uniform. However, MODIS' sesor reveals a different picture - long skinny trails of brighter clouds hidden within. As ships travel across the ocean, pollution in the ships' exhaust create more cloud drops that are smaller in size, resulting in even brighter clouds. On clear days, ships can actually create new clouds. Water vapor condenses around the particles of pollution, forming streamers of clouds as the ships travel on. The ship tracks themselves are too small to impact global temperatures, but they help us understand how larger pollution sources such as industrial sites or agricultural burning might be changing clouds on a larger scale. || ",
            "hits": 55
        },
        {
            "id": 3708,
            "url": "https://svs.gsfc.nasa.gov/3708/",
            "result_type": "Visualization",
            "release_date": "2010-05-01T00:00:00-04:00",
            "title": "Five Spheres - Tropospheric Ozone",
            "description": "Satellite data can be used to monitor the health of the atmosphere from space. This animation of atmospheric changes is match framed to animation entries 3707, 3709, 3710, and 3711. This dataset shows tropospheric ozone, which is close to the ground and a component of pollution. This should be distinguished from high altitude (stratospheric) ozone which shields the Earth's surface from ultraviolet radiation.For more information about tropospheric ozone see the links below:http://www.nasa.gov/vision/earth/environment/ozone_resource_page.htmlhttp://www.ozonelayer.noaa.gov/science/basics.htm || ",
            "hits": 22
        },
        {
            "id": 3665,
            "url": "https://svs.gsfc.nasa.gov/3665/",
            "result_type": "Visualization",
            "release_date": "2009-12-13T00:00:00-05:00",
            "title": "Global Transport of Black Carbon",
            "description": "Tiny air pollution particles commonly called soot, but also known as black carbon, are in the air and on the move throughout our planet. Black carbon enters the air when fossil fuels and biofuels, such as coal, wood, and diesel are burned. Since black carbon readily absorbs heat from sunlight, the particles can affect Earth's climate, especially on a regional scale. Though global distribution of soot remains difficult to measure, NASA researchers use satellite data and computer models to better understand how these short-lived particles influence Earth's climate, cryosphere, and clouds. This scientific data visualization uses data from the GEOS5 GOCART climate model to show black carbon's atmospheric concentration from August to November in 2009.A flat map version of this animation is available.This visualziation was created in support of a presentation at the Fall 2009 American Geophysical Union (AGU) conference in San Fransisco, CA. || ",
            "hits": 66
        },
        {
            "id": 3668,
            "url": "https://svs.gsfc.nasa.gov/3668/",
            "result_type": "Visualization",
            "release_date": "2009-12-13T00:00:00-05:00",
            "title": "Atmospheric Black Carbon Density",
            "description": "Black carbon, or soot, is formed from the burning of fossil fuels and biomass and lingers in the atmosphere for days or weeks before being deposited on the land or ocean. The transport and deposition of black carbon has become an important topic related to climate change since it can absorb sunlight and cause an increase in temperature on ice surfaces or in the atmosphere. The movement of black carbon in the atmosphere can be simulated by including existing black carbon data sets in a global model of the atmosphere. This animation shows the simulation of over three months of atmospheric black carbon production and movement from the Goddard Chemistry Aerosol and Transport (GOCART) model, which is driven by output of the GEOS5 global atmosphere simulation. Note the production of black carbon from industrialization in China and biomass burning in Africa, as well as the movement of black carbon across the oceans of the world. || ",
            "hits": 91
        },
        {
            "id": 3586,
            "url": "https://svs.gsfc.nasa.gov/3586/",
            "result_type": "Visualization",
            "release_date": "2009-03-17T00:00:00-04:00",
            "title": "What Would have Happened to the Ozone Layer if Chlorofluorocarbons (CFCs) had not been Regulated?",
            "description": "Led by NASA Goddard scientist Paul Newman, a team of atmospheric chemists simulated 'what might have been' if chlorofluorocarbons (CFCs) and similar ozone-depleting chemicals were not banned through the Montreal Protocol. The comprehensive model — including atmospheric chemical effects, wind changes, and solar radiation changes — simulated what would happen to global concentrations of stratospheric ozone if CFCs were continually added to the atmosphere.The visualizations below present two cases, from several different viewing positions: the 'world avoided' case, where the rate of CFC emission into the atmosphere is assumed to be that of the period before regulation, and the 'projected' case, which assumes the current rate of emission, post-regulation. Both cases extrapolate to the year 2065. || ",
            "hits": 140
        },
        {
            "id": 3492,
            "url": "https://svs.gsfc.nasa.gov/3492/",
            "result_type": "Visualization",
            "release_date": "2009-03-09T12:00:00-04:00",
            "title": "Atlantic Transport of Anthropogenic Aerosol Optical Depth (AOD)  in 2003",
            "description": "In a new NASA study, researchers taking advantage of improvements in satellite sensor capabilities offer the first measurement-based estimate of the amount of pollution. The new measurements from the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument on NASA's Terra satellite substantiate the results of previous model-based studies, and are the most extensive to date. Hongbin Yu, an associate research scientist of the University of Maryland Baltimore County working at NASA's Goddard Space Flight Center in Greenbelt, Md., grew up in China and taught there as a university professor, , where he witnessed first-hand and studied how pollution from nearby power plants affected the local environment. Yu points out, however, that the matter of pollution transport is a global one. \"Our study focused on East Asian pollution transport, but pollution also flows from Europe, North America, the broader Asian region and elsewhere, across bodies of water and land, to neighboring areas and beyond,\" he said. \"So we should not simply blame East Asia for this amount of pollution flowing into North America.\" In fact, a recent model study conducted by Mian Chin, co-author of this study and an atmospheric scientist at NASA Goddard suggests that European pollution also makes significant contribution to the pollution inflow to North America. \"Satellite instruments give us the ability to capture finer measurements, on a nearly daily basis across a broader geographic region and across a longer time frame so that the overall result is a better estimate than any other measurement method we've had in the past,\" said study co-author Lorraine Remer, a physical scientist and member of the MODIS science team at NASA Goddard. The MODIS instrument can distinguish between broad categories of particles in the air, and observes Earth's entire surface every one to two days, enabling it to monitor movement of the East Asian pollution aerosols as they rise into the lower troposphere, the area of the atmosphere where we live and breathe, and make their way across the Pacific and up into the middle and upper regions of the troposphere. Remer added that the research team also found that pollution movements fluctuate during the year, with the East Asian airstream carrying its largest \"load\" in spring and smallest in summer. The most extensive East Asian export of pollution across the Pacific took place in 2003, triggered by record-breaking wildfires across vast forests of East Asia and Russia. Notably, the pollution aerosols also travel across the ocean quickly, journeying into the atmosphere above North American in as little as one week. \"We cannot determine at what level of elevation in the atmosphere the pollution ends up once it crosses over to North America, so we do not have a way in this study to assess what actual impact it has on air quality here,\" said Remer. \"Nevertheless, we realize there is indeed impact. For example, particles like these have been linked to regional weather and climate effects. Since pollution transport is such a broad global issue, it is important moving forward to extend this kind of study to other regions, to see how much pollution is migrating from its source regions to others, when, and how fast,\" said Remer. || ",
            "hits": 18
        },
        {
            "id": 3491,
            "url": "https://svs.gsfc.nasa.gov/3491/",
            "result_type": "Visualization",
            "release_date": "2008-03-13T12:00:00-04:00",
            "title": "Pacific Anthropogenic Aerosol Optical Depth (AOD)  in 2003",
            "description": "According to measurements taken with a satellite instrument, vast quantities of industrial aerosols and smoke from biomass burning in East Asia and Russia are traveling from one side of the globe to another. Explosive economic growth in Asia has profound implications for the atmosphere worldwide. Data collected by a NASA satellite shows a dense blanket of polluted air over the Northwestern Pacific. This brown cloud is a toxic mix of ash, acids, and airborne particles from car and factory emissions, as well as from low-tech polluters like coal-burning stoves and from forest fires. This image generated by data from NASA's instrument called MODIS (Moderate Resolution Imaging Spectroradiometer) onboard the Terra satellite demonstrates how large and pervasive this transport phenomenon is across vast areas. China's exports fill shelves around the world, but according to a new NASA research paper, China also heavily exports pollution. This week, space agency scientists reveal how Chinese industrialization and Russian forest fires in combination with pollution transported eastward from Europe send roughly 18 teragrams - almost 40 billion pounds-of pollution aerosols into the atmosphere over the Northwestern Pacific every year. The MODIS instrument on NASA's Terra satellite has been tracking the particulate pollution for more than seven years, gathering data as most of it drifted east across the Pacific Ocean. About 4.5 teragrams of particulate pollution each year could reach the western boundary of North America, which is about 15% of local emissions of particulate pollutants from the U.S. and Canada. In the last two decades, China has more than doubled its pollution production. This boom may be contributing to substantial changes in climate and weather in places far from the origin of the particulates. Never in human history-anywhere-has there been industrial growth like that in modern China. But with fast growth comes unintended consequences, and from space evidence of those consequences is starting to emerge. The research relies on measurements of something called \"aerosol optical thickness\". It's a quantitative measurement about how well a slice of atmosphere transmits light. The greater the value of optical thickness for a given location, the less light of a particular wavelength can pass through it. Measurements of aerosol optical thickness describe quantities of tiny particles in a given volume. By measuring how much light can penetrate a region of atmosphere across a variety of wavelengths, scientists can make certain inferences about the quantity and type of particles blocking that light. This visualization shows the seasonal variations of transport of pollution aerosols across the North Pacific. The East Asian airstream carries its largest pollution loading in spring and smallest in summer and fall. With heavy concentrations of aerosols represented by shades of brown, scientists can track the origins and distribution of the particles as they travel in the atmosphere. The sequence also shows a trail of substantial aerosol concentrations from a variety of sources. These sources include heavy industrial activity in East Asia associated with high population density represented in this sequence by gradations of black covering the land surface, and intense Russian forest fires in high latitudes. || ",
            "hits": 26
        },
        {
            "id": 3038,
            "url": "https://svs.gsfc.nasa.gov/3038/",
            "result_type": "Visualization",
            "release_date": "2004-10-29T12:00:00-04:00",
            "title": "The 2004 Antarctic Ozone Hole",
            "description": "A relatively warm Antarctic winter in 2004 kept the thinning of the protective ozone layer over Antarctica, known as the ozone 'hole,' slightly smaller than in 2003. Each year the 'hole' expands over Antarctica, sometimes reaching populated areas of South America and exposing them to ultraviolet rays normally absorbed by ozone. Scientists have new tools to study this annual phenomenon, and the human-produced compounds that contribute to ozone breakdown are decreasing.On September 22, 2004, ozone thinning over Antarctica reached its maximum extent for the year at 24.2 million square kilometers (9.4 million square miles). The largest maximum area on record was 29.2 million square kilometers, in 2000. On October 5, 2004, the ozone layer reached a low value of 99 Dobson Units. || ",
            "hits": 24
        },
        {
            "id": 2998,
            "url": "https://svs.gsfc.nasa.gov/2998/",
            "result_type": "Visualization",
            "release_date": "2004-09-09T12:00:00-04:00",
            "title": "MODIS Data May Aid EPA Air Quality Predictions (Wide)",
            "description": "This visualization shows how MODIS data from NASA's Terra and Aqua spacecraft may be able to help EPA in producing air quality index forecasts.Currently, most air quality forecasts are generated from ground based measuring stations; however, these stations generally only exist in heavily populated areas. MODIS data may help EPA provide air quality forcasts over much wider areas and with higher accuracy. In this visualization, the EPA air quality data shows as the thin colored boxes sticking out from the surface. The MODIS data is represented by the colored overlay. An event that began over the northwestern US in September 2003 is shown propagating across the US and into the Midwest. Notice that the movement of the air mass is evident only from the MODIS data.This version of the animation shows a narrow view of the US. This animation was inspired by a similar animation created at the Langley Research Center. || ",
            "hits": 20
        },
        {
            "id": 2999,
            "url": "https://svs.gsfc.nasa.gov/2999/",
            "result_type": "Visualization",
            "release_date": "2004-09-09T12:00:00-04:00",
            "title": "MODIS Data May Aid EPA Air Quality Predictions (Tight)",
            "description": "This visualization shows how MODIS data from NASA's Terra and Aqua spacecraft may be able to help EPA in producing air quality index forecasts.Currently, most air quality forecasts are generated from ground based measuring stations; however, these stations generally only exist in heavily populated areas. MODIS data may help EPA provide air quality forcasts over much wider areas and with higher accuracy. In this visualization, the EPA air quality data shows as the thin colored boxes sticking out from the surface. The MODIS data is represented by the colored overlay. An event that began over the northwestern US in September 2003 is shown propagating across the US and into the Midwest. Notice that the movement of the air mass is evident only from the MODIS data.This version of the animation shows a narrow view of the US. This animation was inspired by a similar animation created at the Langley Research Center. || ",
            "hits": 11
        },
        {
            "id": 2988,
            "url": "https://svs.gsfc.nasa.gov/2988/",
            "result_type": "Visualization",
            "release_date": "2004-09-07T12:00:00-04:00",
            "title": "Antarctic Ozone from TOMS: August 1, 2003 to November 27, 2003",
            "description": "The 2003 Antarctic ozone hole was the second largest ever observed, according to scientists from NASA, the National Oceanic and Atmospheric Administration (NOAA), and the Naval Research Laboratory (NRL). The Antarctic ozone 'hole' is defined as thinning of the ozone layer over the continent to levels significantly below pre-1979 levels. Ozone blocks harmful ultraviolet 'B' rays. Loss of stratospheric ozone has been linked to skin cancer in humans and other adverse biological effects on plants and animals. The size of the 2003 Antarctic ozone hole reached 10.9 million square miles on September 11, 2003, slightly larger than the North American continent, but smaller than the largest ever recorded, on September 10, 2000, when it covered 11.5 million square miles. This animation is an update to animation ID 2809 — this version includes about 2 additional months of data. || ",
            "hits": 23
        },
        {
            "id": 2989,
            "url": "https://svs.gsfc.nasa.gov/2989/",
            "result_type": "Visualization",
            "release_date": "2004-09-07T12:00:00-04:00",
            "title": "The 2003 Antarctic Ozone Hole",
            "description": "TOMS provides dramatic visual evidence of the annual growth and decay of the Antarctic ozone hole. The ozone losses over Antarctica result from reactions with the products of man-made chlorine and bromine compounds. Because of the tilt of the Earth's axis, continuous darkness falls at the South Pole from March 21 to September 21. The dark region in the middle of the July 1 total ozone picture is polar night, where TOMS cannot make measurements. Ozone losses are in blue. Beginning in August, returning sunlight reaches the edges of Antarctica providing chlorine and bromine compounds with energy to rapidly destroy ozone. By mid September, the ozone loss peaks, creating an ozone hole over Antarctic.  or more information see http://www.gsfc.nasa.gov/topstory/2003/1208toms.html || ",
            "hits": 25
        },
        {
            "id": 2980,
            "url": "https://svs.gsfc.nasa.gov/2980/",
            "result_type": "Visualization",
            "release_date": "2004-09-03T12:00:00-04:00",
            "title": "Ground Level UV Exposure",
            "description": "A large ozone hole means more ultraviolet exposure. TOMS tracks solar ultraviolet (UV-B radiation) measured at 290-320 nanometer wavelengths. Loss of stratospheric ozone has been linked to skin cancer in humans. Increased UV-B exposures for Southern continents can seriously impact phytoplankton and other species. Red is for high UV exposure and blue is for low UV exposure. || ",
            "hits": 34
        },
        {
            "id": 2957,
            "url": "https://svs.gsfc.nasa.gov/2957/",
            "result_type": "Visualization",
            "release_date": "2004-06-28T12:00:00-04:00",
            "title": "China Dust Storm Pollutes Air in the Eastern United States in April 2001 (Flatmap)",
            "description": "A large dust storm develops over China on April 6 and 7, 2001. This animation shows the dust moving over China, Russia, Japan, the Pacific Ocean, and Canada, settling over the United States. || ",
            "hits": 22
        },
        {
            "id": 2956,
            "url": "https://svs.gsfc.nasa.gov/2956/",
            "result_type": "Visualization",
            "release_date": "2004-06-14T12:00:00-04:00",
            "title": "China Dust Storm during April 2001 (WMS)",
            "description": "A major dust storm occurred in April 2001 over parts of China and Mongolia. Dust from this storm was transported all the way to the coast of the United States.  Although dust from the Sahara Desert is routinely transported across the Atlantic to the east coast of the United States, Asian dust rarely makes the distance across the Pacific to the west coast.  These airborne microscopic dust and smoke particles, or aerosols, were measured by the TOMS instrument on the Earth Probe satellite.  For governments struggling to meet national air quality standards, knowing more about the sources and movement of pollution across national borders has become an important issue. || ",
            "hits": 25
        },
        {
            "id": 2940,
            "url": "https://svs.gsfc.nasa.gov/2940/",
            "result_type": "Visualization",
            "release_date": "2004-05-17T12:00:00-04:00",
            "title": "TOMS Ozone Holds Key to Ozone Trends",
            "description": "Chemicals and transport process have led to changes in the stratospheric ozone.  Scientists need measurements of many different chemical species to puzzle out the observed changes.  Aura data will improve our capability to predict ozone changes and help untangle the roles of transport and chemistry in determining ozone trends.  This sequence starts with the actual size of our thin fragile part of our atmosphere that carries ozone.  Then, the atmosphere is magnified.  Inside, is a dynamic and active system of chemicals that moves ozone throughout our atmosphere. || ",
            "hits": 11
        },
        {
            "id": 2941,
            "url": "https://svs.gsfc.nasa.gov/2941/",
            "result_type": "Visualization",
            "release_date": "2004-05-17T12:00:00-04:00",
            "title": "TOMS Ozone Holds Key to Ozone Trends (with Height Indicator)",
            "description": "Chemicals and transport process have led to changes in the stratospheric ozone. Scientists need measurements of many different chemical species to puzzle out the observed changes. Aura data will improve our capability to predict ozone changes and help untangle the roles of transport and chemistry in determining ozone trends. This sequence starts with the actual size of our thin fragile part of our atmosphere that carries ozone. Then, the atmosphere is magnified. Inside, is a dynamic and active system of chemicals that moves ozone throughout our atmosphere. || ",
            "hits": 21
        },
        {
            "id": 2942,
            "url": "https://svs.gsfc.nasa.gov/2942/",
            "result_type": "Visualization",
            "release_date": "2004-05-17T12:00:00-04:00",
            "title": "TOMS Ozone Holds Key to Ozone Trends (with Dates)",
            "description": "Chemicals and transport process have led to changes in the stratospheric ozone. Scientists need measurements of many different chemical species to puzzle out the observed changes. Aura data will improve our capability to predict ozone changes and help untangle the roles of transport and chemistry in determining ozone trends. This sequence starts with the actual size of our thin fragile part of our atmosphere that carries ozone. Then, the atmosphere is magnified. Inside, is a dynamic and active system of chemicals that moves ozone throughout our atmosphere. || ",
            "hits": 9
        },
        {
            "id": 2903,
            "url": "https://svs.gsfc.nasa.gov/2903/",
            "result_type": "Visualization",
            "release_date": "2004-02-12T12:00:00-05:00",
            "title": "Ozone Measurements from 2000 through 2003 (WMS)",
            "description": "This visualization shows the total ozone concentrations for the Earth from January 1, 2000 through December 31, 2003, as measured by theTOMS instrument on the Earth Probe satellite. Low ozone (less than 200 Dobson units) is depicted as regions of dark blue, with high ozone (greater that 330 Dobson units) depicted as yellow and red. The most visible and dynamic feature of the ozone distribution is the ozone hole that forms over Antarctica during September of each year. The amount of ozone in the stratosphere over Antarctica is reduced during this period due to unique atmospheric conditions which chemically reduce the amount of ozone in the region and prevent that ozone from mixing with the higher ozone concentrations just outside the hole. Ozone blocks harmful ultraviolet 'B' rays, and loss of statospheric ozone has been linked to skin cancer in humans and other adverse biological effects in plants and animals. This visualization explicitly shows the TOM ozone data coverage and does not interpolate data into regions of the Earth that the instrument did not observe. Since TOMS measures ozone by observing the characteristics of sunlight reflected from the Earth's surface, no measurements are available for the poles during the polar winter, i.e., around January for the North Pole and July for the South Pole. Also, there is an unobserved region between successive satellite orbits around the equator. Finally, the instrument has periods where technical issues make measurement impossible for a matter of hours or days. This visualization shows that the dynamics of the ozone layer remain visible despite these measurement issues. || ",
            "hits": 16
        },
        {
            "id": 2904,
            "url": "https://svs.gsfc.nasa.gov/2904/",
            "result_type": "Visualization",
            "release_date": "2004-02-12T12:00:00-05:00",
            "title": "Global Ozone from 2000 through 2003 (WMS)",
            "description": "This visualization shows the total ozone concentrations for the Earth from January 1, 2000 through December 31, 2003. Low ozone (less than 200 Dobson units) is depicted as regions of dark blue, with high ozone (greater than 330 Dobson units) depicted as yellow and red. The most visible and dynamic feature of the ozone distribution is the ozone hole that forms over Antarctica during September of each year. The amount of ozone in the stratosphere over Antarctica is reduced during this period due to unique atmospheric conditions which chemically reduce the amount of ozone in the region and prevent that ozone from mixing with the higher ozone concentrations just outside the hole. Ozone blocks harmful ultraviolet 'B' rays, and loss of statospheric ozone has been linked to skin cancer in humans and other adverse biological effects in plants and animals. The 2000 Antarctic ozone hole reached 11.5 million square miles on September 10, 2000, the largest hole ever recorded, slightly larger than the North American continent. The 2002 ozone hole was much smaller than normal, dividing into two parts on September 24 before dissipating completely, while the 2003 hole was the second largest observed, reaching 10.9 million square miles on September 11. This data was measured by the TOMS instrument on the Earth Probe satellite. TOMS experienced some days during this period for which data was not measured due to instrument problems. || ",
            "hits": 42
        },
        {
            "id": 2859,
            "url": "https://svs.gsfc.nasa.gov/2859/",
            "result_type": "Visualization",
            "release_date": "2003-12-03T12:00:00-05:00",
            "title": "China Dust Storm seen by Earth Probe/TOMS in April of 2001",
            "description": "A thick shroud of dust appears over China on April 6 and 7, 2001. The densest portion of the aerosol pollution travels east over China, Russia, Japan, the Pacific Ocean, Canada, and the United States. || ",
            "hits": 11
        },
        {
            "id": 2860,
            "url": "https://svs.gsfc.nasa.gov/2860/",
            "result_type": "Visualization",
            "release_date": "2003-12-03T12:00:00-05:00",
            "title": "China Dust Storm seen by Terra/MODIS and Earth Probe/TOMS in April of 2001",
            "description": "A thick shroud of dust appears over China on April 6-7, 2001. The densest portion of the aerosol pollution travels east over China, Russia, Japan, the Pacific Ocean, Canada, and The United States. || ",
            "hits": 19
        },
        {
            "id": 2855,
            "url": "https://svs.gsfc.nasa.gov/2855/",
            "result_type": "Visualization",
            "release_date": "2003-11-10T12:00:00-05:00",
            "title": "Maximum Ozone Hole Area for 2003",
            "description": "This still shows the maximum stratospheric ozone hole over the Antarctic for 2003. || Stratospheric Ozone for September 24, 2003. || still_hires_24Sept2003.jpg (2560x1920) [202.0 KB] || still_hires_24Sept2003_web.jpg (320x240) [6.6 KB] || still_hires_24Sept2003_thm.png (80x40) [3.1 KB] || still_hires_24Sept2003_web_searchweb.jpg (320x180) [52.2 KB] || still_hires_24Sept2003.tif (2560x1920) [5.0 MB] || ",
            "hits": 6
        }
    ]
}