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    "results": [
        {
            "id": 14190,
            "url": "https://svs.gsfc.nasa.gov/14190/",
            "result_type": "Produced Video",
            "release_date": "2019-11-07T00:00:00-05:00",
            "title": "NASA Explorers | Season Three: Fires",
            "description": "Complete transcript available. || S3_Trailer_Thumbnail.png (2136x1102) [999.3 KB] || S3_Trailer_V2.mov (3840x2160) [2.8 GB] || S3_Trailer_V2.mp4 (3840x2160) [44.3 MB] || S3_Trailer_V2.webm (3840x2160) [9.7 MB] || S3_Trailer_Captions.en_US.srt [846 bytes] || S3_Trailer_Captions.en_US.vtt [858 bytes] || ",
            "hits": 22
        },
        {
            "id": 13289,
            "url": "https://svs.gsfc.nasa.gov/13289/",
            "result_type": "Produced Video",
            "release_date": "2019-08-26T11:00:00-04:00",
            "title": "NASA's CAMP2Ex Heads to the Philippines for Monsoon Season",
            "description": "NASA, the Naval Research Laboratory and the Manila Observatory are working together in the Philippines to study how tiny particles in the atmosphere affect cloud formation. || ",
            "hits": 39
        },
        {
            "id": 30483,
            "url": "https://svs.gsfc.nasa.gov/30483/",
            "result_type": "Hyperwall Visual",
            "release_date": "2013-11-12T00:00:00-05:00",
            "title": "2013 Rainfall over the Philippines",
            "description": "In a normal year, 30 percent of the total rainfall near the Philippines, located in the Western Pacific Ocean is caused by tropical cyclones. This visualization shows the estimated total rainfall contributed by named tropical cyclones over the Philippines from January 1 to November 11, 2013. The data used to create the visualization were derived from Tropical Rainfall Measurement Mission (TRMM) measurements. In particular, a TRMM-based, near-real time Multi-satellite Precipitation Analysis (TMPA) was used to analyze only rainfall near tropical cyclones passing close to or over the Philippines. The data show almost four feet of rain fell in parts of the northern and central Philippines.The color scale represents rainfall amounts from 0-44 inches (~0-1100 millimeters). Red indicates areas where rainfall totals were greater than 43 inches. Small white icons with the names of each tropical cyclone show storm tracks. The most notable tropical cyclone was Super Typhoon Haiyan that devastated the central Philippines in November 2013. Super Typhoon Haiyan, Tropical Depression 30W, and Typhoon Rumbia passed over the central Philippines resulting in estimated rainfall totals of more than 43 inches (~1100 millimeters) over the island of Leyte. || ",
            "hits": 32
        },
        {
            "id": 2951,
            "url": "https://svs.gsfc.nasa.gov/2951/",
            "result_type": "Visualization",
            "release_date": "2004-05-27T12:00:00-04:00",
            "title": "Super Typhoon Nida",
            "description": "The MODIS instrument onboard NASA's Aqua and Terra satellites captured this sequence of true-color images of Super Typhoon Nida churning through the Philippine Islands. Packing winds up tof 100 mph and gusts of 122 mph, and caused floods and landslides. Nida has been responsible for at least six deaths in the Philippines and has displaced thousands as it skirted the eastern part of the country before moving towards southern Japan. || ",
            "hits": 36
        },
        {
            "id": 2389,
            "url": "https://svs.gsfc.nasa.gov/2389/",
            "result_type": "Visualization",
            "release_date": "2002-03-04T12:00:00-05:00",
            "title": "Mount Pinatubo Particle Model",
            "description": "The global impact of the June 1991 Mount Pinatubo eruption in the Philippines can be seen in this particle model. Immediately following the eruption large amounts of sulfur dioxide and dust spread through the earth's atmosphere. The colors in this animation reflect the atmospheric height of the particles. Red is high and blue is closer to the earth's surface. || ",
            "hits": 111
        },
        {
            "id": 2193,
            "url": "https://svs.gsfc.nasa.gov/2193/",
            "result_type": "Visualization",
            "release_date": "2001-06-12T12:00:00-04:00",
            "title": "Mt. Pinatubo 10th Anniversary Perspective",
            "description": "This recent false color Landsat-7 image, from January 2001, shows Mt. Pinatubo as it stands today. The caldera is seen in the middle of the image, underneath clouds.Ten years after the blast, vegetation is re-growing on the slopes of the mountain (in green.) Streams of mud, called lahars, (resulting from ash from the eruption mixing with water- seen as the lighter sediment) continue to flow down the sides of the mountains, as well as channels of water (darker streams).  However, as vegetation grows back, the ash becomes more stabilized and less likely to form the destructive lahars. || ",
            "hits": 46
        },
        {
            "id": 2194,
            "url": "https://svs.gsfc.nasa.gov/2194/",
            "result_type": "Visualization",
            "release_date": "2001-06-12T12:00:00-04:00",
            "title": "Mt. Pinatubo 10th Anniversary Perspective (Stills)",
            "description": "This recent false color Landsat-7 image, from January 2001, shows Mt. Pinatubo as it stands today. The caldera is seen in the middle of the image, underneath clouds. Ten years after the blast, vegetation is re-growing on the slopes of the mountain (in green). Streams of mud, called lahars, (resulting from ash from the eruption mixing with water- seen as the lighter sediment) continue to flow down the sides of the mountains, as well as channels of water (darker streams). However, as vegetation grows back, the ash becomes more stabilized and less likely to form the destructive lahars. || ",
            "hits": 22
        }
    ]
}