{
    "count": 14,
    "next": null,
    "previous": null,
    "results": [
        {
            "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": 10
        },
        {
            "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": 12
        },
        {
            "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": 11
        },
        {
            "id": 3459,
            "url": "https://svs.gsfc.nasa.gov/3459/",
            "result_type": "Visualization",
            "release_date": "2007-09-15T00:00:00-04:00",
            "title": "Multivariate ENSO Index Correlation with Ocean Net Primary Production Data over the North Atlantic",
            "description": "The SeaWiFS instrument aboard the Seastar satellite has been collecting ocean data since 1997. A check up of the Earth's planetary health reveals that the lowest rung in the ocean food chain is shrinking. For the past 20 years (early 1980s to present), phytoplankton concentrations declined as much as 30 percent in northern oceans. Scientists from NASA, the National Oceanic and Atmospheric Administration (NOAA), and Oregon State University say warmer ocean temperatures and low winds may be depriving the tiny ocean plants of necessary nutrients. However, they still do not know if the loss of phytoplankton is a long-term trend or a climate oscillation. Scientists can monitor ocean and planetary health through phytoplankton. Since the whole ocean food chain depends on the health and productivity of phytoplankton, a significant change could indicate a shift in our climate. Phytoplankton consists of many diverse species of microscopic free-floating ocean plants that form the base of the ocean's food chain. These plants thrive on sunlight and nutrients. Limit either one and phytoplankton will not grow. This animation shows the Multivariate ENSO Index (MEI) in red and the net primary production NPP anomaly in units of Tgrams carbon per month in green. The MEI is a multivariate index that incorporates sea level pressure, surface zonal and meridional wind components, sea surface temperature, surface air temperature, and cloudiness (Wolter and Timlin, 1998). The MEI index is calculated for the tropical Pacific (i.e., between 10 degrees North and 10 degrees South, from Asia to the Americas) with units of kg m-3. The Net Primary Production (NPP) data was generated from the Vertically Generalized Production Model (VGPM). The VGPM data set is available at the following URL: http://web.science.oregonstate.eduocean.productivity/ . As the sea surface temperature warms, the production levels decrease. || ",
            "hits": 61
        },
        {
            "id": 3420,
            "url": "https://svs.gsfc.nasa.gov/3420/",
            "result_type": "Visualization",
            "release_date": "2007-04-23T12:00:00-04:00",
            "title": "SeaWiFS Biosphere Global Rotation from 1997 to 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. 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": 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": 13
        },
        {
            "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": 17
        },
        {
            "id": 3387,
            "url": "https://svs.gsfc.nasa.gov/3387/",
            "result_type": "Visualization",
            "release_date": "2006-12-05T00:00:00-05:00",
            "title": "SeaWiFS Biosphere from 1997 to 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. 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. A recent study indicates there is a correlation between this ocean nutrients and changes in sea surface temperature (SST). The results show that when SSTs warm, marine plant life in the form of microscopic phytoplankton declines. When SSTs cool, marine plant life flourishes. Changes in phytoplankton growth influence fishery yields and the amount of carbon dioxide the oceans remove from the atmosphere. This could have major implications on the future of our ocean's food web and how it relates to climate change. Once the animation pulls out to a full global view, the remaining animation can be compared to the 'MODIS Sea Surface Temperature from 2002 to 2006' animation. || ",
            "hits": 15
        },
        {
            "id": 3388,
            "url": "https://svs.gsfc.nasa.gov/3388/",
            "result_type": "Visualization",
            "release_date": "2006-12-05T00:00:00-05:00",
            "title": "MODIS Sea Surface Temperature from 2002 to 2006",
            "description": "A recent study indicates there is a correlation between ocean nutrients and changes in sea surface temperature (SST). The results show that when ocean water warms, marine plant life in the form of microscopic phytoplankton tend to decline. When water cools, plant life flourishes. Changes in phytoplankton growth influence fishery yields and the amount of carbon dioxide the oceans remove from the atmosphere. This could have major implications on the future of our ocean's food web and how it relates to climate change.The temperature data in this visualization comes from the Moderate Resolution Imaging Spectroradiometer (MODIS) onboard NASA's Terra and Aqua spacecraft.In order to see the correlation between SST and SeaWiFS data, this animation can be compared to the latter part of the 'SeaWiFS Biosphere from 1997 to 2006' animation. || ",
            "hits": 20
        },
        {
            "id": 3389,
            "url": "https://svs.gsfc.nasa.gov/3389/",
            "result_type": "Visualization",
            "release_date": "2006-12-05T00:00:00-05:00",
            "title": "MODIS Sea Surface Temperature Highlighting the Gulf Stream (2002 to 2006)",
            "description": "A recent study indicates a correlation between ocean nutrients and changes sea surface temperature (SST). The results show that when SSTs warm, marine plant life in the form of microscopic phytoplankton declines. Similarly, when SSTs cool, marine plant life seems to flourish. Changes in phytoplankton growth influence fishery yields and the amount of carbon dioxide the oceans remove from the atmosphere. This could have major implications on the future of our ocean's food web and how it relates to climate change.The temperature data in this visualization comes from the Moderate Resolution Imaging Spectroradiometer (MODIS) onboard NASA's Terra and Aqua spacecraft. || ",
            "hits": 14
        },
        {
            "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": 46
        },
        {
            "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": 7
        },
        {
            "id": 3510,
            "url": "https://svs.gsfc.nasa.gov/3510/",
            "result_type": "Visualization",
            "release_date": "2006-12-05T00:00:00-05:00",
            "title": "MODIS Sea Surface Temperature from 2002 to 2006 around Australia",
            "description": "A recent study indicates there is a correlation between ocean nutrients and changes in sea surface temperature (SST). The results show that when ocean water warms, marine plant life in the form of microscopic phytoplankton tend to decline. When water cools, plant life flourishes. Changes in phytoplankton growth influence fishery yields and the amount of carbon dioxide the oceans remove from the atmosphere. This could have major implications on the future of our ocean's food web and how it relates to climate change.The temperature data in this visualization comes from the Moderate Resolution Imaging Spectroradiometer (MODIS) onboard NASA's Terra and Aqua spacecraft.In order to see the correlation between SST and SeaWiFS data, this animation can be compared to 'SeaWiFS Biosphere Data over Australia'. Please click here to see this other animation. || ",
            "hits": 7
        },
        {
            "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": 20
        }
    ]
}