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    "results": [
        {
            "id": 5173,
            "url": "https://svs.gsfc.nasa.gov/5173/",
            "result_type": "Visualization",
            "release_date": "2023-10-10T00:00:00-04:00",
            "title": "Earth's Radiation Balance, 2000-2023",
            "description": "A plotted view of planetary heat uptake since the beginning of the CERES data record showing an oscillating, monthly mean (yellow) and twelve-month running average (red line). These data show how much energy is added (absorbed) by Earth during the CERES period. || planetary_heat_anomaly.1800_print.jpg (1024x576) [69.7 KB] || planetary_heat_anomaly.1800_searchweb.png (320x180) [21.2 KB] || planetary_heat_anomaly.1800_thm.png (80x40) [3.0 KB] || phu_2023 (3840x2160) [0 Item(s)] || planetary_heat_anomaly_2160p60.mp4 (3840x2160) [4.2 MB] || ",
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        {
            "id": 14228,
            "url": "https://svs.gsfc.nasa.gov/14228/",
            "result_type": "Produced Video",
            "release_date": "2022-10-31T11:00:00-04:00",
            "title": "Clouds 101",
            "description": "Complete transcript available. || Screen_Shot_2022-10-19_at_1.52.39_PM_print.jpg (1024x578) [66.1 KB] || Screen_Shot_2022-10-19_at_1.52.39_PM.png (2844x1607) [3.9 MB] || Clouds_101_Lock.00001_searchweb.png (320x180) [34.8 KB] || Screen_Shot_2022-10-19_at_1.52.39_PM_searchweb.png (320x180) [66.0 KB] || Screen_Shot_2022-10-19_at_1.52.39_PM_web.png (320x180) [66.4 KB] || Screen_Shot_2022-10-19_at_1.52.39_PM_thm.png (80x40) [8.7 KB] || Clouds_101_audio_otter_ai.en_US.srt [9.6 KB] || Clouds_101_audio_otter_ai.en_US.vtt [9.6 KB] || Clouds_101_Lock.mp4 (1920x1080) [974.5 MB] || ",
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        },
        {
            "id": 4935,
            "url": "https://svs.gsfc.nasa.gov/4935/",
            "result_type": "Visualization",
            "release_date": "2021-04-16T00:00:00-04:00",
            "title": "CERES Radiation Balance",
            "description": "A plotted view of planetary heat uptake since the beginning of the CERES data record showing an oscillating, monthly mean (yellow) and twelve-month running average (red line). These data show how much energy is added (absorbed) by Earth during the CERES period. || CERES_2021_update_final.01650_print.jpg (1024x576) [69.5 KB] || CERES_2021_update_final.01650_searchweb.png (320x180) [23.5 KB] || CERES_2021_update_final.01650_thm.png (80x40) [3.3 KB] || CERES_2021_update_final.mp4 (1920x1080) [9.2 MB] || CERES_2021_update_final.webm (1920x1080) [6.2 MB] || CERES_2021_update_final.mp4.hwshow [194 bytes] || ",
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        },
        {
            "id": 13557,
            "url": "https://svs.gsfc.nasa.gov/13557/",
            "result_type": "Produced Video",
            "release_date": "2020-02-24T11:00:00-05:00",
            "title": "Placing the Recent Hiatus Period in an Energy Balance Perspective",
            "description": "GLOBAL OBSERVATIONS OF EARTH’S ENERGY BALANCE With the launch of NASA’s Terra Satellite Earth Observing System on Dec. 18, 1999, and subsequent ‘first light’ of the Cloud’s and the Earth’s Energy Radiant System (CERES) instrument on February 26, 2000, NASA gave birth to what ultimately would become the first long-term global observational record of Earth’s energy balance. This key indicator of the climate system describes the delicate and complex balance between how much of the sun’s energy reaching Earth is absorbed and how much thermal infrared radiation is emitted back to space. “Absorbed solar radiation fuels the climate system and life on our planet,” said Norman Loeb, CERES Principal Investigator. “The Earth sheds heat by emitting outgoing radiation.” || ",
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        },
        {
            "id": 4794,
            "url": "https://svs.gsfc.nasa.gov/4794/",
            "result_type": "Visualization",
            "release_date": "2020-02-21T08:00:00-05:00",
            "title": "CERES Radiation Balance",
            "description": "The Clouds and the Earth’s Energy Radiant System (CERES) instrument is a key component of NASA’s Earth Observing System, with six active CERES instruments on satellites orbiting Earth and taking data.  For Earth’s temperature to be stable over long periods of time, absorbed solar and emitted thermal radiation must be equal. Increases in greenhouse gases, like carbon dioxide and methane, trap emitted thermal radiation from the surface and reduce how much is lost to space, resulting in a net surplus of energy into the Earth system. Most of the extra energy ends up being stored as heat in the ocean and the remainder warms the atmosphere and land, and melts snow and ice. As a consequence, global mean surface temperature increases and sea levels rise. Much like a pulse or heartbeat, CERES monitors reflected solar and emitted thermal infrared radiation, which together with solar irradiance measurements is one of Earth’s ‘vital signs.’ Better understanding Earth’s energy balance enables us to be informed and adapt to a changing world. || ",
            "hits": 253
        },
        {
            "id": 4245,
            "url": "https://svs.gsfc.nasa.gov/4245/",
            "result_type": "Visualization",
            "release_date": "2014-12-17T13:00:00-05:00",
            "title": "Link between Sea-Ice Fraction and Absorbed Solar Radiation over the Arctic Ocean",
            "description": "NASA satellite instruments have observed a marked increase in solar radiation absorbed in the Arctic since the year 2000 – a trend that aligns with the drastic decrease in Arctic sea ice during the same period.  This visual shows the Arctic Sea Ice Change and the corresponding Absorbed Solar Radiation Change during June, July, and August from 2000 through 2014.This video is also available on our YouTube channel. || seaice_solarAbsorption_0344_print.jpg (1024x576) [117.1 KB] || SeaIceSolarAbsorptionChange.webm (1920x1080) [1.2 MB] || 1920x1080_16x9_60p (1920x1080) [0 Item(s)] || SeaIceSolarAbsorptionChange.mp4 (1920x1080) [12.1 MB] || composite (1920x1080) [0 Item(s)] || source (1920x1080) [0 Item(s)] || SeaIceSolarAbsorptionChange.m4v (640x360) [2.1 MB] || ",
            "hits": 63
        },
        {
            "id": 3925,
            "url": "https://svs.gsfc.nasa.gov/3925/",
            "result_type": "Visualization",
            "release_date": "2012-07-22T00:00:00-04:00",
            "title": "NPP Ceres Shortwave Radiation",
            "description": "The CERES experiment is one of the highest priority scientific satellite instruments developed for NASA's Earth Observing System (EOS). The doors are open on NASA's Suomi NPP satellite and the newest version of the Clouds and the Earth's Radiant Energy System (CERES) instrument is scanning Earth for the first time, helping to assure continued availability of measurements of the energy leaving the Earth-atmosphere system.CERES products include both solar-reflected and Earth-emitted radiation from the top of the atmosphere to the Earth's surface. Cloud properties are determined using simultaneous measurements by other EOS and NPP instruments such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Visible and Infrared Sounder (VIRS). Analyses using CERES data, build upon the foundation laid by previous missions such as NASA Earth Radiation Budget Experiment (ERBE), leading to a better understanding of the role of clouds and the energy cycle in global climate change. The sun's radiant energy is the fuel that drives Earth's climate engine. The Earth-atmosphere system constantly tries to maintain a balance between the energy that reaches the Earth from the sun and the energy that flows from Earth back out to space. Energy received from the sun is mostly in the visible (or shortwave) part of the electromagnetic spectrum. About 30% of the solar energy that comes to Earth is reflected back to space. The ratio of reflected-to-incoming energy is called \"albedo\" from the Latin word meaning whiteness. The solar radiation absorbed by the Earth causes the planet to heat up until it is radiating (or emitting) as much energy back into space as it absorbs from the sun. The Earth's thermal emitted radiation is mostly in the infrared (or longwave part of the spectrum. The balance between incoming and outgoing energy is called the Earth's radiation budget. This global view shows CERES top-of-atmosphere (TOA) shortwave radiation from Jan 26 and 27, 2012. Thick cloud cover tends to reflect a large amount of incoming solar energy back to space (blue/green/white image). For more information on the Clouds and Earth's Radiant Energy System (CERES) see http://ceres.larc.nasa.gov || ",
            "hits": 55
        },
        {
            "id": 3926,
            "url": "https://svs.gsfc.nasa.gov/3926/",
            "result_type": "Visualization",
            "release_date": "2012-07-22T00:00:00-04:00",
            "title": "NPP Ceres Longwave Radiation",
            "description": "The CERES experiment is one of the highest priority scientific satellite instruments developed for NASA's Earth Observing System (EOS). The doors are open on NASA's Suomi NPP satellite and the newest version of the Clouds and the Earth's Radiant Energy System (CERES) instrument is scanning Earth for the first time, helping to assure continued availability of measurements of the energy leaving the Earth-atmosphere system.CERES products include both solar-reflected and Earth-emitted radiation from the top of the atmosphere to the Earth's surface. Cloud properties are determined using simultaneous measurements by other EOS and NPP instruments such as the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Visible and Infrared Sounder (VIRS). Analyses using CERES data, build upon the foundation laid by previous missions such as NASA Earth Radiation Budget Experiment (ERBE), leading to a better understanding of the role of clouds and the energy cycle in global climate change.The sun's radiant energy is the fuel that drives Earth's climate engine. The Earth-atmosphere system constantly tries to maintain a balance between the energy that reaches the Earth from the sun and the energy that flows from Earth back out to space. Energy received from the sun is mostly in the visible (or shortwave) part of the electromagnetic spectrum. About 30% of the solar energy that comes to Earth is reflected back to space. The ratio of reflected-to-incoming energy is called \"albedo\" from the Latin word meaning whiteness. The solar radiation absorbed by the Earth causes the planet to heat up until it is radiating (or emitting) as much energy back into space as it absorbs from the sun. The Earth's thermal emitted radiation is mostly in the infrared (or longwave part of the spectrum. The balance between incoming and outgoing energy is called the Earth's radiation budget.This global view shows CERES top-of-atmosphere (TOA) longwave radiation from Jan 26 and 27, 2012. Heat energy radiated from Earth (in watts per square meter) is shown in shades of yellow, red, blue and white. The brightest-yellow areas are the hottest and are emitting the most energy out to space, while the dark blue areas and the bright white clouds are much colder, emitting the least energy. Increasing temperature, decreasing water vapor, and decreasing clouds will all tend to increase the ability of Earth to shed heat out to space.For more information on the Clouds and Earth's Radiant Energy System (CERES) see  http://ceres.larc.nasa.gov || ",
            "hits": 116
        },
        {
            "id": 10893,
            "url": "https://svs.gsfc.nasa.gov/10893/",
            "result_type": "Produced Video",
            "release_date": "2012-01-12T11:00:00-05:00",
            "title": "Aqua Podcast Series",
            "description": "This page will soon feature six videos about the Aqua satellite mission, starting with an introductory video, followed by weekly additions of videos highlighting the AIRS, AMSR-E, MODIS, and CERES instruments, and concluding with a video featuring applications of Aqua data. || ",
            "hits": 10
        },
        {
            "id": 10514,
            "url": "https://svs.gsfc.nasa.gov/10514/",
            "result_type": "Produced Video",
            "release_date": "2009-12-11T18:00:00-05:00",
            "title": "Terra@10: Terra 10th Anniversary Video",
            "description": "The Earth-observing satellite Terra celebrates its tenth anniversary in 2009. This video highlights how Terra has helped us better understand our home planet. The satellite's five instruments - ASTER, CERES, MISR, MODIS and MOPITT - reveal how our our world is changing. For complete transcript, click here. || Terra10_ipodlarge.08402_print.jpg (1024x576) [38.3 KB] || Terra10_ipodlarge_web.png (320x180) [47.8 KB] || Terra10_ipodlarge_thm.png (80x40) [4.3 KB] || Terra10_Apple_TV.webmhd.webm (960x540) [71.4 MB] || Terra10_Youtube.mov (1280x720) [72.8 MB] || Terra10_Apple_TV.m4v (960x720) [179.0 MB] || Terra10_H.264.mov (1280x720) [146.6 MB] || Terra10_ipodlarge.m4v (640x360) [55.7 MB] || Terra10.mpg (512x288) [118.8 MB] || Terra10_ipodsmall.m4v (320x180) [24.0 MB] || Terra10.wmv (346x260) [18.2 MB] || ",
            "hits": 16
        }
    ]
}