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        {
            "id": 14648,
            "url": "https://svs.gsfc.nasa.gov/14648/",
            "result_type": "Produced Video",
            "release_date": "2024-08-16T00:00:00-04:00",
            "title": "An Ocean in Bloom",
            "description": "Music: \"Maelstrom Dream,\" \"Skipping Stones On The Lake,\" \"Breaking Through The Clouds,\" \"Awaking Wonder,\" \"Floating Emotions,\" \"Fire in the Chill of Dawn,\" \"Closed Fractures,\" \"Battle For Our Future,\" \"Final Climb,\" \"In Nature,\" Universal Production Music.Complete transcript available.This video can be freely shared and downloaded. While the video in its entirety can be shared without permission, some individual imagery provided by external sources (see list below) is obtained through permission and may not be excised or remixed in other products. For more information on NASA’s media guidelines, visit https://www.nasa.gov/multimedia/guidelines/index.htmlFootage Courtesy Of: FOX 13 News, New World of Communications of Tampa, INC. TM and Copyright 2021, 2022, 2023. All Rights Reserved, Pexels, Pond5, Ralph Arwood, Joseph Rohrs, Dale Danelle, NOAA Fisheries, NASA/SpaceX.You can also find \"An Ocean in Bloom\" on NASA+. || NHQ_2024_0801_AnOceanInBloom_FINALCUT.02846_print.jpg (1024x576) [214.4 KB] || NHQ_2024_0801_AnOceanInBloom_FINALCUT.02846_searchweb.png (320x180) [102.3 KB] || NHQ_2024_0801_AnOceanInBloom_FINALCUT.02846_web.png (320x180) [102.3 KB] || NHQ_2024_0801_AnOceanInBloom_FINALCUT.02846_thm.png (80x40) [6.5 KB] || NHQ_2024_0801_AnOceanInBloom_FINALCUT_EN_US.en_US.vtt [20.8 KB] || NHQ_2024_0801_AnOceanInBloom_FINALCUT_EN_US.en_US.srt [21.9 KB] || NHQ_2024_0801_AnOceanInBloom_FINALCUT.webm (3840x2160) [412.0 MB] || NHQ_2024_0801_AnOceanInBloom_FinalCut_HD.mp4 (1920x1080) [3.2 GB] || NHQ_2024_0801_AnOceanInBloom_FINALCUT.mp4 (3840x2160) [5.6 GB] || ",
            "hits": 72
        },
        {
            "id": 13021,
            "url": "https://svs.gsfc.nasa.gov/13021/",
            "result_type": "B-Roll",
            "release_date": "2018-07-30T00:00:00-04:00",
            "title": "EXPORTS -- B-roll and Media",
            "description": "Footage, animations and stills for the Export Processes in the Ocean from RemoTe Sensing (EXPORTS) mission, leaving from Seattle on Aug. 10. || R/V Roger RevelleCredit: Scripps Institution of Oceanography || REVELLE_siocomm_2.jpg (1200x960) [329.8 KB] || R/V Roger RevelleCredit: Scripps Institution of Oceanography || REVELLE_siocomm_1.jpg (3000x1901) [1.4 MB] || ",
            "hits": 23
        },
        {
            "id": 12332,
            "url": "https://svs.gsfc.nasa.gov/12332/",
            "result_type": "Produced Video",
            "release_date": "2016-08-11T15:00:00-04:00",
            "title": "PACE -- Plankton, Aerosol, Cloud, ocean Ecosystem",
            "description": "The Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) mission will deliver the most comprehensive look at global ocean color measurements in NASA's history. Not only will PACE monitor the health of our ocean, its science data will expand atmospheric studies by sensing our skies over an exceptionally broad spectrum of wavelengths. A strategic climate continuity mission in support of NASA's Plan for a Climate-Centric Architecture for Earth Observations and Applications from Space (2010), PACE wil monitor aerosol particles, clouds, and many factors related to the marine carbon cycle including the phytoplankton pigment, chlorophyll. Moreover, PACE applications will help with many of our most pressing environmental issues such as harmful algal bloom and air quality forecasts. || ",
            "hits": 28
        },
        {
            "id": 30794,
            "url": "https://svs.gsfc.nasa.gov/30794/",
            "result_type": "Hyperwall Visual",
            "release_date": "2016-07-26T00:00:00-04:00",
            "title": "Ocean Acidification: Surface pH",
            "description": "The imagery here shows the output of a computer model that makes predictions of how the pH will change over time based on best estimates of likely CO2 emissions (RCP 8.5) used in the United Nations Intergovernmental Panel on Climate Change's AR5 assessment. The dataset starts in 1861 and runs through 2100.This visualization, originally developed by NOAA Environmental Visualization Laboratory for display on NOAA's Science On a Sphere, is adapted here for use on the NASA hyperwall. || ",
            "hits": 219
        },
        {
            "id": 30697,
            "url": "https://svs.gsfc.nasa.gov/30697/",
            "result_type": "Hyperwall Visual",
            "release_date": "2015-10-23T00:00:00-04:00",
            "title": "Ocean Alkalinity",
            "description": "To document effects of ocean acidification it is important to have an understanding of the processes and parameters that influence alkalinity. Alkalinity is a measure of the ability of seawater to neutralize acids. This visualization shows monthly surface total alkalinity (TA) from August 2011 to May 2015 as derived using data from NASA’s Aquarius mission. Utilization of Aquarius data allows unprecedented global mapping of surface TA as it correlates strongly with salinity and to a lesser extent with temperature.For the first time, Aquarius data are allowing scientists to observe changes in surface alkalinity over time. For example, they have found that the Northern Hemisphere has more spatial and monthly variability in total alkalinity and salinity, while less variability in Southern Ocean alkalinity is due to less salinity variability and upwelling of waters enriched in alkalinity. Increasing surface TA in subtropical regions from increasing salinity and temperature causes the saturation states of calcite and aragonite to decrease, i.e., enhanced dissolution. Thus, based on increasing TA in the subtropical regions over the past few decades, it is expected that it is becoming more difficult for calcifying organisms to make their shells. || ",
            "hits": 93
        },
        {
            "id": 11899,
            "url": "https://svs.gsfc.nasa.gov/11899/",
            "result_type": "Produced Video",
            "release_date": "2015-07-21T13:00:00-04:00",
            "title": "Scientists Link Earlier Melting Of Snow To Dark Aerosols",
            "description": "Tiny particles suspended in the air, known as aerosols, can darken snow and ice causing it to absorb more of the sun’s energy. But until recently, scientists rarely considered the effect of all three major types of light-absorbing aerosols together in climate models.In a new study, NASA scientists used a climate model to examine the impact of this snow-darkening phenomenon on Northern Hemisphere snowpacks, including how it affects snow amount and heating on the ground in spring.The study looked at three types of light-absorbing aerosols – dust, black carbon and organic carbon. Black carbon and organic carbon are produced from the burning of fossil fuels, like coal and oil, as well as biofuels and biomass, such as forests.With their snow darkening effect added to NASA’s GEOS-5 climate model, scientists analyzed results from 2002 to 2011, and compared them to model runs done without the aerosols on snow. They found that the aerosols indeed played a role in absorbing more of the sun’s energy. Over broad places in the Northern Hemisphere, the darkened snow caused some surface temperatures to be up to 10 degrees Fahrenheit warmer than it would be if the snow were pristine. As a result, warmer, snow-darkened areas had less snow in spring than they would have had under pristine snow conditions.According to the study, dust’s snow darkening effect significantly contributed to surface warming in Central Asia and the western Himalayas. Black carbon’s snow darkening effect had a larger impact primarily in Europe, the eastern Himalayas and East Asia. It had a smaller impact in North America. Organic carbon’s snow darkening effect was relatively lower but present in regions such as southeastern Siberia, northeastern East Asia and western Canada.“As we add more of these aerosols to the mix, we are potentially increasing our overall impact on Earth’s climate,” said research scientist Teppei Yasunari at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.Research: Impact of snow darkening via dust, black carbon, and organic carbon on boreal spring climate in the Earth systemJournal: Geophysical Research: Atmospheres, June 15, 2015.Link to paper: http://onlinelibrary.wiley.com/doi/10.1002/2014JD022977/fullHere is the YouTube video. || ",
            "hits": 66
        },
        {
            "id": 11900,
            "url": "https://svs.gsfc.nasa.gov/11900/",
            "result_type": "Produced Video",
            "release_date": "2015-07-21T13:00:00-04:00",
            "title": "Instagram: Scientists Link Earlier Melting Of Snow To Dark Aerosols",
            "description": "Tiny particles suspended in the air, known as aerosols, can darken snow and ice causing it to absorb more of the sun’s energy. But until recently, scientists rarely considered the effect of all three major types of light-absorbing aerosols together in climate models.In a new study, NASA scientists used a climate model to examine the impact of this snow-darkening phenomenon on Northern Hemisphere snowpacks, including how it affects snow amount and heating on the ground in spring.The study looked at three types of light-absorbing aerosols – dust, black carbon and organic carbon. Black carbon and organic carbon are produced from the burning of fossil fuels, like coal and oil, as well as biofuels and biomass, such as forests.With their snow darkening effect added to NASA’s GEOS-5 climate model, scientists analyzed results from 2002 to 2011, and compared them to model runs done without the aerosols on snow. They found that the aerosols indeed played a role in absorbing more of the sun’s energy. Over broad places in the Northern Hemisphere, the darkened snow caused some surface temperatures to be up to 10 degrees Fahrenheit warmer than it would be if the snow were pristine. As a result, warmer, snow-darkened areas had less snow in spring than they would have had under pristine snow conditions.According to the study, dust’s snow darkening effect significantly contributed to surface warming in Central Asia and the western Himalayas. Black carbon’s snow darkening effect had a larger impact primarily in Europe, the eastern Himalayas and East Asia. It had a smaller impact in North America. Organic carbon’s snow darkening effect was relatively lower but present in regions such as southeastern Siberia, northeastern East Asia and western Canada.“As we add more of these aerosols to the mix, we are potentially increasing our overall impact on Earth’s climate,” said research scientist Teppei Yasunari at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.Research: Impact of snow darkening via dust, black carbon, and organic carbon on boreal spring climate in the Earth systemJournal: Geophysical Research: Atmospheres, June 15, 2015.Link to paper: http://onlinelibrary.wiley.com/doi/10.1002/2014JD022977/fullHere is the YouTube video. || ",
            "hits": 31
        },
        {
            "id": 30584,
            "url": "https://svs.gsfc.nasa.gov/30584/",
            "result_type": "Hyperwall Visual",
            "release_date": "2015-02-13T00:00:00-05:00",
            "title": "AXIOM-1 Ocean chlorophyll, Sea Ice Thickness and Atmospheric Precipitable Water",
            "description": "This animation shows ocean surface chlorophyll concentration, sea ice thickness, and atmospheric precipitable water. || 0001_print.jpg (1024x576) [236.0 KB] || 0001_searchweb.png (320x180) [121.0 KB] || 0001_web.png (320x180) [121.0 KB] || 0001_thm.png (80x40) [8.0 KB] || chl-1920x1080.webm (1920x1080) [15.9 MB] || axiom_chl_720p.mp4 (1280x720) [161.2 MB] || axiom_chl_h265_720p.mp4 (1280x720) [105.5 MB] || chl-1920x1080.mp4 (1920x1080) [889.5 MB] || chl (5760x3240) [128.0 KB] || axiom_chl_h265_2304p.mp4 (4096x2304) [913.8 MB] || chlorophyll_ice_thickness_precip_water_30584.key [896.4 MB] || chlorophyll_ice_thickness_precip_water_30584.pptx [893.1 MB] || axiom_chl_2304p.mp4 (4096x2304) [1.4 GB] || ",
            "hits": 32
        },
        {
            "id": 3908,
            "url": "https://svs.gsfc.nasa.gov/3908/",
            "result_type": "Visualization",
            "release_date": "2012-02-08T00:00:00-05:00",
            "title": "ECCO2 Sea Surface Temperature and Flows",
            "description": "Generated for Science On a Sphere show \"Loop\". This animation depicts the part of Earth's ocean circulation model that involves heat transfer.In the polar latitudes the ocean loses heat to the atmosphere. Near the equator ocean water warms, and because it is less dense, it remains close to the surface. Cast away from the planet's equator by the winds and Earth's rotation, warm equatorial waters travel on or near the surface of the globe outward toward high latitudes. But as water loses heat to the increasingly cold atmosphere far away from the equator it sinks and pushes other water out of the way. Endlessly, this pump known as Meridional Overturning Circulation, circulates water and heat around the globe. Considering that the ocean stores exponentially more heat than the atmosphere and the fact that they're always in direct contact with each other, there's a strong relationship between oceanic heat and atmospheric circulation. || ",
            "hits": 58
        },
        {
            "id": 10695,
            "url": "https://svs.gsfc.nasa.gov/10695/",
            "result_type": "Produced Video",
            "release_date": "2011-06-17T14:00:00-04:00",
            "title": "NASA's Oceanographic Voyage - ICESCAPE",
            "description": "The ICESCAPE mission, or \"Impacts of Climate on Ecosystems and Chemistry of the Arctic Pacific Environment,\" is NASA's first dedicated oceanographic field campaign. From June-July 2010, scientists onboard the U.S. Coast Guard Cutter Healy spent five weeks at sea studying how changing conditions in the Arctic affect the ocean's chemistry and ecosystems. On June 25, 2011, researchers embark on the mission's second and final campaign. The multiyear observations collected from the icebreaker will help us interpret what instruments in space tell us, as well as turn up some new discoveries. || ",
            "hits": 35
        },
        {
            "id": 3454,
            "url": "https://svs.gsfc.nasa.gov/3454/",
            "result_type": "Visualization",
            "release_date": "2007-11-05T00:00:00-05:00",
            "title": "SeaWiFS Biosphere Data over the North Pacific",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997. By monitoring the color of reflected light via satellite, scientists can determine how successfully plant life is photosynthesizing. A measurement of photosynthesis is essentially a measurement of successful growth, and growth means successful use of ambient carbon. This animation represents nearly a decade's worth of data taken by the SeaWiFS instrument, showing the abundance of life in the sea. Dark blue represents warmer areas where there is little life due to lack of nutrients, and greens and reds represent cooler nutrient-rich areas. The nutrient-rich areas include coastal regions where cold water rises from the sea floor bringing nutrients along and areas at the mouths of rivers where the rivers have brought nutrients into the ocean from the land. || ",
            "hits": 13
        },
        {
            "id": 3471,
            "url": "https://svs.gsfc.nasa.gov/3471/",
            "result_type": "Visualization",
            "release_date": "2007-10-05T00:00:00-04:00",
            "title": "SeaWiFS Biosphere Data over the North Pacific (Slow Version)",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997.  By monitoring the color of reflected light via satellite, scientists can determine how successfully plant life is photosynthesizing.  A measurement of photosynthesis is essentially a measurement of successful growth, and growth means successful use of ambient carbon. This animation represents nearly a decade's worth of data taken by the SeaWiFS instrument, showing the abundance of life in the sea. Dark blue represents warmer areas where there is little life due to lack of nutrients, and greens and reds represent cooler nutrient-rich areas. The nutrient-rich areas include coastal regions where cold water rises from the sea floor bringing nutrients along and areas at the mouths of rivers where the rivers have brought nutrients into the ocean from the land.This animation is essentially the same as animation #3454 with a few minor changes and runs at a slower speed. || ",
            "hits": 14
        },
        {
            "id": 3494,
            "url": "https://svs.gsfc.nasa.gov/3494/",
            "result_type": "Visualization",
            "release_date": "2007-10-05T00:00:00-04:00",
            "title": "SeaWiFS Biosphere Data over Australia",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997.  By monitoring the color of reflected light via satellite, scientists can determine how successfully plant life is photosynthesizing.  A measurement of photosynthesis is essentially a measurement of successful growth, and growth means successful use of ambient carbon. This animation represents nearly a decade's worth of data taken by the SeaWiFS instrument, showing the abundance of life in the sea. Dark blue represents warmer areas where there is little life due to lack of nutrients, and greens and reds represent cooler nutrient-rich areas. The nutrient-rich areas include coastal regions where cold water rises from the sea floor bringing nutrients along and areas at the mouths of rivers where the rivers have brought nutrients into the ocean from the land. || ",
            "hits": 9
        },
        {
            "id": 3451,
            "url": "https://svs.gsfc.nasa.gov/3451/",
            "result_type": "Visualization",
            "release_date": "2007-04-23T12:00:00-04:00",
            "title": "Global Rotation of SeaWiFS Biosphere Decadal Average with Land",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997. By monitoring the color of reflected light via satellite, scientists can determine how successfully plant life is photosynthesizing. A measurement of photosynthesis is essentially a measurement of successful growth, and growth means successful use of ambient carbon. This animation shows an average of 10 years worth of SeaWiFS data. Dark blue represents warmer areas where there tends to be a lack of nutrients, and greens and reds represent cooler nutrient-rich areas which support life. The nutrient-rich areas include coastal regions where cold water rises from the sea floor bringing nutrients along and areas at the mouths of rivers where the rivers have brought nutrients into the ocean from the land. || ",
            "hits": 8
        },
        {
            "id": 3452,
            "url": "https://svs.gsfc.nasa.gov/3452/",
            "result_type": "Visualization",
            "release_date": "2007-04-23T12:00:00-04:00",
            "title": "Global Rotation of SeaWiFS Biosphere Decadal Average without Land",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997. By monitoring the color of reflected light via satellite, scientists can determine how successfully plant life is photosynthesizing. A measurement of photosynthesis is essentially a measurement of successful growth, and growth means successful use of ambient carbon. This animation shows an average of 10 years worth of SeaWiFS data. Dark blue represents warmer areas where there tends to be a lack of nutrients, and greens and reds represent cooler nutrient-rich areas which support life. The nutrient-rich areas include coastal regions where cold water rises from the sea floor bringing nutrients along and areas at the mouths of rivers where the rivers have brought nutrients into the ocean from the land. || ",
            "hits": 20
        },
        {
            "id": 3752,
            "url": "https://svs.gsfc.nasa.gov/3752/",
            "result_type": "Visualization",
            "release_date": "2007-04-16T00:00:00-04:00",
            "title": "Life's Signature Colors, Captured by Satellite",
            "description": "Think of Earth's great life forms and images of cheetahs, whales and dinosaurs come to mind. Towering redwood trees, majestic plains of grasses on Asian steppes: Earth's living glow fills the eye with diversity, resilience, and endless Darwinian invention.But arguably one of the most essential populations on Earth would have no chance if pitted against others in a contest based on looks alone. More than any other kind of life, the Earth lives and breathes because of the profound success of lowly phytoplankton.Phytoplankton is a broad, catch-all name for a wide category of simple organisms living primarily in the world's oceans. Floating in vast fields of billions of tiny individual plants, these essential life forms make up a colossal proportion of the Earth's total biomass. It's also vital to the overall web of life on Earth. Phytoplankton serves not only as the base of the aquatic food chain, but also as the principal source of atmospheric oxygen worldwide.As global climate continues to change, a complex set of forces begins to push and pull on the ability of phytoplankton populations to thrive. Changing global ocean temperatures have enormous influences, as does changing ocean chemistry. But while this may present itself as a subject of purely academic interest, phytoplankton populations may present one of the most vital bellwethers for practical changes beginning to take hold of a planet in transition.NASA's SeaWiFS spacecraft is one of the most powerful tools in keeping up with these trends. A small, low cost vehicle and instrument package, SeaWiFS monitors the colors of the world everyday. As a proxy for bioproductivity, color is the key to understanding how these oceanic lifeforms are faring...and changing. || ",
            "hits": 13
        },
        {
            "id": 3450,
            "url": "https://svs.gsfc.nasa.gov/3450/",
            "result_type": "Visualization",
            "release_date": "2006-12-05T00:00:00-05:00",
            "title": "SeaWiFS Biosphere Data over the North Atlantic",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997. By monitoring the color of reflected light via satellite, scientists can determine how successfully plant life is photosynthesizing. A measurement of photosynthesis is essentially a measurement of successful growth, and growth means successful use of ambient carbon. This animation represents nearly a decade's worth of data taken by the SeaWiFS instrument, showing the abundance of life in the sea. Dark blue represents warmer areas where there is little life due to lack of nutrients, and greens and reds represent cooler nutrient-rich areas. The nutrient-rich areas include coastal regions where cold water rises from the sea floor bringing nutrients along and areas at the mouths of rivers where the rivers have brought nutrients into the ocean from the land. || ",
            "hits": 14
        },
        {
            "id": 3468,
            "url": "https://svs.gsfc.nasa.gov/3468/",
            "result_type": "Visualization",
            "release_date": "2006-12-05T00:00:00-05:00",
            "title": "SeaWiFS Biosphere Data over the North Atlantic (Slow Version)",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997. By monitoring the color of reflected light via satellite, scientists can determine how successfully plant life is photosynthesizing. A measurement of photosynthesis is essentially a measurement of successful growth, and growth means successful use of ambient carbon. This animation represents nearly a decade's worth of data taken by the SeaWiFS instrument, showing the abundance of life in the sea. Dark blue represents warmer areas where there is little life due to lack of nutrients, and greens and reds represent cooler nutrient-rich areas. The nutrient-rich areas include coastal regions where cold water rises from the sea floor bringing nutrients along and areas at the mouths of rivers where the rivers have brought nutrients into the ocean from the land.This animation is essentially the same as animation #3450 with a few minor changes and runs at half the speed. || ",
            "hits": 13
        },
        {
            "id": 3599,
            "url": "https://svs.gsfc.nasa.gov/3599/",
            "result_type": "Visualization",
            "release_date": "2006-12-05T00:00:00-05:00",
            "title": "Phytoplankton Blooms through the Eyes of SeaWiFS Data",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997. By monitoring the color of reflected light via satellite, scientists can determine how successfully plant life is photosynthesizing. A measurement of photosynthesis is essentially a measurement of successful growth, and growth means successful use of ambient carbon. This animation represents nearly a decade's worth of data taken by the SeaWiFS instrument, showing the abundance of life in the sea. Dark blue represents warmer areas where there is little life due to lack of nutrients, and greens and reds represent cooler nutrient-rich areas. The nutrient-rich areas include coastal regions where cold water rises from the sea floor bringing nutrients along and areas at the mouths of rivers where the rivers have brought nutrients into the ocean from the land. Dark gray indicate areas where no data was collected. || ",
            "hits": 21
        }
    ]
}