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            "id": 30747,
            "url": "https://svs.gsfc.nasa.gov/30747/",
            "result_type": "Hyperwall Visual",
            "release_date": "2016-01-29T10:00:00-05:00",
            "title": "2015 El Niño Disrupts Ocean Chlorophyll",
            "description": "Sea Surface Temperature Anomaly & Ocean Color variations during El Nino vs. La Nina, using the rainbow colorbar for Ocean Color || ocean_color_ssta_swipe_new_rainbow_1080p.00001_print.jpg (1024x576) [116.9 KB] || ocean_color_ssta_swipe_new_rainbow_1080p.mp4 (1920x1080) [2.4 MB] || ocean_color_ssta_swipe_new_rainbow_720p.mp4 (1280x720) [1.4 MB] || ocean_color_ssta_swipe_new_rainbow_720p.webm (1280x720) [3.8 MB] || ocean_color_ssta_swipe_new_rainbow_2304p.mp4 (4096x2304) [7.5 MB] || ocean_color_ssta_swipe_new_rainbow_360p.mp4 (640x360) [530.1 KB] || ",
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        {
            "id": 30745,
            "url": "https://svs.gsfc.nasa.gov/30745/",
            "result_type": "Hyperwall Visual",
            "release_date": "2016-01-14T00:00:00-05:00",
            "title": "All Stirred Up in the Arabian Sea",
            "description": "Ocean bloom off of Oman, Pakistan, and India. || V2015355084000.ArabianSea_hw_print.jpg (1024x626) [245.8 KB] || V2015355084000.ArabianSea_hw_searchweb.png (320x180) [128.3 KB] || V2015355084000.ArabianSea_hw_thm.png (80x40) [16.8 KB] || V2015355084000.ArabianSea_hw.tif (3881x2374) [12.4 MB] || stirred_up_arabian_sea_30745.key [2.9 MB] || stirred_up_arabian_sea_30745.pptx [312.5 KB] || clouds-of-dust-and-clouds-of-phytoplankton-at-the-arabian-sea.hwshow [341 bytes] || ",
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        {
            "id": 2077,
            "url": "https://svs.gsfc.nasa.gov/2077/",
            "result_type": "Visualization",
            "release_date": "2001-03-12T12:00:00-05:00",
            "title": "SeaWiFS: the North Atlantic Bloom",
            "description": "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.  Until now, scientists have only had a continuous record of photosynthesis on land. But following three years of continual data collected by the SeaWiFS instrument, NASA has gathered the first record of photosynthetic productivity in the oceans.  By taking three years of continuous data as a whole, experts have been able to map trends and anomalies in the global circulation of carbon to a degree of detail than has never been done before. It is a baseline measurement to by which all future measurements will be compared. || ",
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            "id": 608,
            "url": "https://svs.gsfc.nasa.gov/608/",
            "result_type": "Visualization",
            "release_date": "1999-11-17T12:00:00-05:00",
            "title": "Side by Side View of the Michigan Bloom - July 24 and Sept. 7, 1999",
            "description": "Two possible explanations for the brightening were advanced in 1999: A large bloom of cyanobacteria such as microcystis or an inorganic precipitation of calcium carbonate triggered by warming surface waters. I never heard whether one or the other choice was validated by researchers on Lake Michigan. A variety of atmospheric aerosols and clouds over the lake also effect the perceived brightness of the water from image to image. || ",
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            "id": 609,
            "url": "https://svs.gsfc.nasa.gov/609/",
            "result_type": "Visualization",
            "release_date": "1999-11-17T12:00:00-05:00",
            "title": "Michigan Lake Changes: Slow Dissolve Between Jul. 24, Aug. 20, Sept. 7, 1999 (With Text)",
            "description": "Two possible explanations for the brightening were advanced in 1999: A large bloom of cyanobacteria such as microcystis or an inorganic precipitation of calcium carbonate triggered by warming surface waters. I never heard whether one or the other choice was validated by researchers on Lake Michigan. A variety of atmospheric aerosols and clouds over the lake also effect the perceived brightness of the water from image to image. || ",
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            "url": "https://svs.gsfc.nasa.gov/610/",
            "result_type": "Visualization",
            "release_date": "1999-11-17T12:00:00-05:00",
            "title": "Michigan Lake Changes: Fast Dissolve Between Jul. 24, Aug 20, and Sept. 7, 1999 (With Text)",
            "description": "Two possible explanations for the brightening were advanced in 1999: A large bloom of cyanobacteria such as microcystis or an inorganic precipitation of calcium carbonate triggered by warming surface waters. I never heard whether one or the other choice was validated by researchers on Lake Michigan. A variety of atmospheric aerosols and clouds over the lake also effect the perceived brightness of the water from image to image. || ",
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            "id": 611,
            "url": "https://svs.gsfc.nasa.gov/611/",
            "result_type": "Visualization",
            "release_date": "1999-11-17T12:00:00-05:00",
            "title": "Michigan Lake Changes: Slow Dissolve Between Jul. 24, Aug. 20, and Sept. 7, 1999 (Without Text)",
            "description": "Two possible explanations for the brightening were advanced in 1999: A large bloom of cyanobacteria such as microcystis or an inorganic precipitation of calcium carbonate triggered by warming surface waters. I never heard whether one or the other choice was validated by researchers on Lake Michigan. A variety of atmospheric aerosols and clouds over the lake also effect the perceived brightness of the water from image to image. || ",
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        },
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            "id": 612,
            "url": "https://svs.gsfc.nasa.gov/612/",
            "result_type": "Visualization",
            "release_date": "1999-11-17T12:00:00-05:00",
            "title": "Michigan Lake Changes: Faster Dissolve Between Jul 24, Aug 20, and Sept 7, 1999 (Without Text)",
            "description": "Two possible explanations for the brightening were advanced in 1999: A large bloom of cyanobacteria such as microcystis or an inorganic precipitation of calcium carbonate triggered by warming surface waters. I never heard whether one or the other choice was validated by researchers on Lake Michigan. A variety of atmospheric aerosols and clouds over the lake also effect the perceived brightness of the water from image to image. || ",
            "hits": 33
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}