{
    "count": 7,
    "next": null,
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    "results": [
        {
            "id": 3641,
            "url": "https://svs.gsfc.nasa.gov/3641/",
            "result_type": "Visualization",
            "release_date": "2009-10-08T00:00:00-04:00",
            "title": "Rotating Phytoplankton 10-year Global Average",
            "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 displays the 10-year global average of 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. || ",
            "hits": 20
        },
        {
            "id": 3642,
            "url": "https://svs.gsfc.nasa.gov/3642/",
            "result_type": "Visualization",
            "release_date": "2009-10-08T00:00:00-04:00",
            "title": "Regions Exhibiting Decreased Phytoplankton Levels and Increased Sea Surface Temperatures",
            "description": "Throughout most of Earth's ocean, as the surface layer of the ocean warms, the water becomes less dense and forms a cap, rather than mixing down to allow cooler, nutrient-rich water to well up. Over time, areas with less mixing show reduced productivity and less phytoplankton. This data visualization highlights regions where a strong correlation between high sea surface temperatures and decreased phytoplankton productivity occurred from 1997-2006. For nearly a decade, the Sea-viewing Wide Field-of-View Sensor (SeaWiFS) has been making global observations of phytoplankton productivity. On December 6, 2006, NASA-funded scientists announced that warming sea surface temperatures over the past decade have caused a global decline in phytoplankton productivity. || ",
            "hits": 12
        },
        {
            "id": 3625,
            "url": "https://svs.gsfc.nasa.gov/3625/",
            "result_type": "Visualization",
            "release_date": "2009-08-26T00:00:00-04:00",
            "title": "Honey Bees Weigh In on Climate",
            "description": "This animation illustrates the relationship between the annual vegetation cycle and seasonal variations in the weights of honey bee hives. The weight of a hive increases in the spring as bees bring back nectar from flowering plants. The change in hive weight over time can be compared with satellite measurements of vegetation. Tracking a large number of hives this way can reveal the effects of changing climate and land use on the interaction of plants and pollinators. Data from this hive in Highland, Maryland and others suggests that for some locations in the U.S., spring is arriving earlier by as much as half a day per year, probably due to a combination of climate and the warming effect of urbanization.This animation has been incorporated into the video \"Feeling the Sting of Climate Change,\" which provides more background and introduces HoneyBeeNet, a central repository for hive weight data from across the U.S. || ",
            "hits": 23
        },
        {
            "id": 3584,
            "url": "https://svs.gsfc.nasa.gov/3584/",
            "result_type": "Visualization",
            "release_date": "2009-06-05T00:00:00-04:00",
            "title": "A Global View of Seasonal NDVI",
            "description": "Satellite data can be used to monitor the health of plant life from space. The Normalized Difference Vegetation Index (NDVI) provides a simple numerical indicator of the health of vegetation which can be used to monitoring changes in vegetation over time. This animation shows the seasonal changes in vegetation by fading between average monthly NDVI data from 2004. The loop begins on September 24 and repeats six times during one full rotation of the globe at a rate of one frame per day. The fade for each month is complete on the 15th of each month. || ",
            "hits": 76
        },
        {
            "id": 3585,
            "url": "https://svs.gsfc.nasa.gov/3585/",
            "result_type": "Visualization",
            "release_date": "2009-03-16T00:00:00-04:00",
            "title": "Stereoscopic SeaWiFS Biosphere Global Rotation: 1997-2006",
            "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. This time period repeats twice during the animation. 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. The nutrient-rich waters contribute to some of the oxygen-poor pockets of the seas called dead zones.This visualization is a stereoscopic version of animation entry:  #3420:SeaWiFS Biosphere Global Rotation from 1997 to 2006 || ",
            "hits": 23
        },
        {
            "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": 9
        },
        {
            "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": 14
        }
    ]
}