{
    "count": 73,
    "next": null,
    "previous": null,
    "results": [
        {
            "id": 10744,
            "url": "https://svs.gsfc.nasa.gov/10744/",
            "result_type": "Produced Video",
            "release_date": "2011-04-30T00:00:00-04:00",
            "title": "The NASA Goddard Space Flight Center - in Stereoscopic 3D!",
            "description": "See Goddard in 3DThis short promotional video highlights some of the best that the Goddard Space Flight Center has to offer - showcasing  the science and technology born from the efforts of the dedicated Goddard family.  Available here are left and right eye movies, as well as anaglyph (red/cyan). To view the 3D version on Youtube: http://youtu.be/08rMlpvUP3w?hd=1To view the 2D version on Youtube: http://youtu.be/2rb-u9cnQeI || GSFC_3D_960x540_2997_anaglyph.00277_print.jpg (1024x576) [68.2 KB] || GSFC_3D_960x540_2997_anaglyph_web.png (320x180) [184.7 KB] || GSFC_3D_960x540_2997_anaglyph_thm.png (80x40) [15.2 KB] || GSFC_3D_960x540_2997_anaglyph.mov (960x540) [22.3 MB] || GSFC_3D_960x540_LEFT.mov (960x540) [19.7 MB] || GSFC_3D_appletv.m4v (960x540) [32.8 MB] || GSFC_3D_1920x1080_LEFT.wmv (1280x720) [31.7 MB] || GSFC_3D_1920x1080_AUDIO_anaglyph.mov (1920x1080) [124.2 MB] || GSFC_3D_1920x1080_H264_RIGHT.mp4 (1920x1080) [205.1 MB] || GSFC_3D_1920x1080_H264_LEFT.mp4 (1920x1080) [205.1 MB] || GSFC_3D_960x540_2997_anaglyph.webmhd.webm (960x540) [13.1 MB] || GSFC_3D_appletv_subtitles.m4v (960x540) [32.8 MB] || GSFC_3D.en_US.srt [857 bytes] || GSFC_3D.en_US.vtt [861 bytes] || ",
            "hits": 61
        },
        {
            "id": 10502,
            "url": "https://svs.gsfc.nasa.gov/10502/",
            "result_type": "Produced Video",
            "release_date": "2009-10-12T00:00:00-04:00",
            "title": "Climate Change and the Global Ocean",
            "description": "We know climate change can affect us, but does climate change alter something as vast, deep and mysterious as our oceans? For years, scientists have studied the world's oceans by sending out ships and divers, deploying data-gathering buoys, and by taking aerial measurements from planes. But one of the better ways to understand oceans is to gain an even broader perspective - the view from space. NASA's Earth observing satellites do more than just take pictures of our planet. High-tech sensors gather data, including ocean surface temperature, surface winds, sea level, circulation, and even marine life. Information the satellites obtain help us understand the complex interactions driving the world's oceans today - and gain valuable insight into how the impacts of climate change on oceans might affect us on dry land.For complete transcript, click here. || Global_Ocean_ipod_320x240.01252_print.jpg (1024x576) [77.3 KB] || Global_Ocean_ipod_320x240_web.png (320x180) [84.7 KB] || Global_Ocean_ipod_320x240_thm.png (80x40) [16.1 KB] || Global_Ocean_appletv.webmhd.webm (960x540) [78.2 MB] || Global_Ocean_broll_prores.mov (1280x720) [5.3 GB] || Global_Ocean_1280x720.mp4 (1280x720) [159.8 MB] || Global_Ocean_appletv.m4v (960x540) [187.1 MB] || Global_Ocean_H264_1280x720_30fps.mov (1280x720) [167.6 MB] || Global_Ocean_youtube_1280x720.mov (1280x720) [79.2 MB] || Global_Ocean_ipod_640x480.m4v (640x360) [59.9 MB] || Global_Ocean_ipod_320x240.m4v (320x180) [25.9 MB] || Global_Ocean.wmv (346x260) [39.1 MB] || ",
            "hits": 54
        },
        {
            "id": 10400,
            "url": "https://svs.gsfc.nasa.gov/10400/",
            "result_type": "Produced Video",
            "release_date": "2009-03-04T00:00:00-05:00",
            "title": "50 Years of Goddard",
            "description": "Pioneer rocket scientist Robert H. Goddard once said, 'It is difficult to say what is impossible, for the dream of yesterday is the hope of today and the reality of tomorrow.' Fifty years after its inception, NASA's Goddard Space Flight Center continues to live by these words, advancing science and engineering to new limits once thought impossible as it explores of the Earth, the sun, the solar system, and the universe. || ",
            "hits": 26
        },
        {
            "id": 3397,
            "url": "https://svs.gsfc.nasa.gov/3397/",
            "result_type": "Visualization",
            "release_date": "2009-01-14T00:00:00-05:00",
            "title": "2008 Sea Surface Surface Temperatures in the Gulf of Mexico",
            "description": "Sea surface temperatures in the Gulf of Mexico rise due to natural summer warming. These warm surface temperatures are a contributing factor to favorable conditions that can lead to the formation of tropical storms and hurricanes in the Gulf of Mexico and off the Eastern Shore of the United States. In general, hurricanes tend to form over warm ocean water whose temperature is 82 degrees Fahrenheit (approximately 27.7 degrees Celsius) or higher. These areas are depicted in yellow, orange, and red. This data was taken by the AMSR-E instrument aboard the Aqua satellite. || ",
            "hits": 25
        },
        {
            "id": 10264,
            "url": "https://svs.gsfc.nasa.gov/10264/",
            "result_type": "Produced Video",
            "release_date": "2008-10-14T00:00:00-04:00",
            "title": "Earth Science Week 2008",
            "description": "Keep your eyes glued to the Goddard Web site through the week of October 12 for daily videos that answer several questions about our home planet. The videos are all part of Earth Science Week: 2008, themed 'No Child Left Inside.' || ",
            "hits": 13
        },
        {
            "id": 3532,
            "url": "https://svs.gsfc.nasa.gov/3532/",
            "result_type": "Visualization",
            "release_date": "2008-09-11T00:00:00-04:00",
            "title": "Current Sea Surface Temperatures Rising in the Gulf of Mexico",
            "description": "Sea surface temperatures in the Gulf of Mexico rise due to natural summer warming. These warm surface temperatures are a contributing factor to favorable conditions that can lead to the formation of tropical storms and hurricanes in the Gulf of Mexico and off the East Coast of the United States. In general, hurricanes tend to form over warm ocean water whose temperature is 82 degrees Fahrenheit (approximately 27.7 degrees Celsius) or higher. These areas are depicted in yellow, orange, and red. This blended microwave- and infrared-wavelength data was taken by the AMSR-E and MODIS instruments aboard the Aqua satellite, and the TMI instrument aboard the TRMM satellite. This animation updates every 24 hours. || ",
            "hits": 87
        },
        {
            "id": 20144,
            "url": "https://svs.gsfc.nasa.gov/20144/",
            "result_type": "Animation",
            "release_date": "2008-07-15T00:00:00-04:00",
            "title": "Aquarius",
            "description": "Aquarius spacecraft in orbit around the Earth || Aquarius 2010 Beauty Shot 3 || aqub000100002_print.jpg (1024x576) [35.4 KB] || aqub0001_web.png (320x180) [223.9 KB] || aqub0001_thm.png (80x40) [15.5 KB] || Aquarius-Beauty3_720p.m2v (1280x720) [21.0 MB] || Aquarius-beauty3.mp4 (1280x720) [5.3 MB] || beauty3 (1280x720) [0 Item(s)] || Aquarius-Beauty3_720p.webmhd.webm (960x540) [2.8 MB] || Aquarius-Beauty3_512x288.m1v (512x288) [3.5 MB] || ",
            "hits": 28
        },
        {
            "id": 3524,
            "url": "https://svs.gsfc.nasa.gov/3524/",
            "result_type": "Visualization",
            "release_date": "2008-07-10T00:00:00-04:00",
            "title": "Biosphere Data Over Northeastern United States (Land Masked)",
            "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 and along the north eastern seaboard of the United States. 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. || ",
            "hits": 8
        },
        {
            "id": 3526,
            "url": "https://svs.gsfc.nasa.gov/3526/",
            "result_type": "Visualization",
            "release_date": "2008-07-10T00:00:00-04:00",
            "title": "Biosphere Data Over United States Eastern Seaboard (Land Masked)",
            "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 and along the eastern seaboard of the United States. 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. || ",
            "hits": 10
        },
        {
            "id": 3527,
            "url": "https://svs.gsfc.nasa.gov/3527/",
            "result_type": "Visualization",
            "release_date": "2008-07-10T00:00:00-04:00",
            "title": "Biosphere Data Across the United States Western Seaboard (Land Masked)",
            "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 and along the Western seaboard of the United States. 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. || ",
            "hits": 8
        },
        {
            "id": 3528,
            "url": "https://svs.gsfc.nasa.gov/3528/",
            "result_type": "Visualization",
            "release_date": "2008-07-10T00:00:00-04:00",
            "title": "Biosphere Data Around the Gulf of Mexico (Land Masked)",
            "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 in and around the Gulf of Mexico. 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. || ",
            "hits": 9
        },
        {
            "id": 3544,
            "url": "https://svs.gsfc.nasa.gov/3544/",
            "result_type": "Visualization",
            "release_date": "2008-07-10T00:00:00-04:00",
            "title": "Biosphere Data Around the Costa Rica Dome (Land Masked)",
            "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.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. || ",
            "hits": 21
        },
        {
            "id": 3488,
            "url": "https://svs.gsfc.nasa.gov/3488/",
            "result_type": "Visualization",
            "release_date": "2008-01-09T00:00:00-05:00",
            "title": "La Niña 2007 Sea Surface Temperature Anomalies",
            "description": "This visualization shows the 2007 La Niña event in the Pacific Ocean.  Sea surface temperature (SST) anomalies from 2007 are shown based on a 3-day moving average using Aqua/AMSR-E SST data. || ",
            "hits": 45
        },
        {
            "id": 3390,
            "url": "https://svs.gsfc.nasa.gov/3390/",
            "result_type": "Visualization",
            "release_date": "2007-03-17T12:00:00-04:00",
            "title": "AMSR-E Sea Surface Temperature",
            "description": "This animation is part of an NSF-funded, international project, Exploring Time. The two-hour television special, broadcast on the Discovery Channel in the spring of 2007, explores how the world changes over different timescales ... from billionths of seconds to billions of years. This animation portrays a 3-day moving average of AMSR-E sea surface temperature (SST) over the western hemisphere from the beginning of 2005 to early December, 2006. In addition, seasonal MODIS land cover shows the advance and retreat of snow over the northern hemisphere.This program was also broadcast in Japan through a partnership with the NHK international broadcasting service and in France through a partnership with the ARTE television network. || ",
            "hits": 61
        },
        {
            "id": 20085,
            "url": "https://svs.gsfc.nasa.gov/20085/",
            "result_type": "Animation",
            "release_date": "2006-10-04T00:00:00-04:00",
            "title": "Ocean Convection at High Altitudes - Normal Condition",
            "description": "Understanding the variability of the density of ocean water is critical to understanding changes in the ocean's circulation, particularly those parts of the circulation that pertain to climate. In the tropics, the sun warms the surface water and causes that water to expand. Because the surface water is now less dense than the cooler water below, the warmest waters remain near the surface. Near the poles, the energy input by the sun is not as strong, and the surface waters are not warmed to the degree they are away from the poles. Here, it is the salinity of the water plays a critical role as to which water is found at the surface as the waters near the surface are not that much different in temperature to the water below.  These animations highlight the crucial role of salinity in high latitude convection (upward and downward movement of water) and climate.This animation, labeled Normal, is a display of the way convection might often occur at high latitudes. Here the water initially is assumed to be almost constant in temperature and salinity from top to bottom. At the times when the air immediately above is colder than the water, there is a transfer of heat from the water to the atmosphere. The surface waters cool, condense, become more dense and ultimately sink. Because the cooling can be very intense at high latitudes, the surface water can cool enough to sink to the bottom. Note in this animation that the convection is depicted to occur in a narrow, almost chimney like area. This is very much the way nature and deep convection behaves at high latitudes. Note later in this animation, the coldest water has made its way to the bottom and it appears the water is moving from right to left near the bottom. This depiction is meant to indicate a movement toward the tropics at these depths. || ",
            "hits": 168
        },
        {
            "id": 20086,
            "url": "https://svs.gsfc.nasa.gov/20086/",
            "result_type": "Animation",
            "release_date": "2006-10-04T00:00:00-04:00",
            "title": "Ocean Convection at High Altitudes - Fresh Condition",
            "description": "Understanding the variability of the density of ocean water is critical to understanding changes in the ocean's circulation, particularly those parts of the circulation that pertain to climate. In the tropics, the sun warms the surface water and causes that water to expand. Because the surface water is now less dense than the cooler water below, the warmest waters remain near the surface. Near the poles, the energy input by the sun is not as strong, and the surface waters are not warmed to the degree they are away from the poles. Here, it is the salinity of the water plays a critical role as to which water is found at the surface as the waters near the surface are not that much different in temperature to the water below.  These animations highlight the crucial role of salinity in high latitude convection (upward and downward movement of water) and climate.This animation, labeled Fresh, illustrates the condition where  the water near the surface is assumed to be much fresher than the saltier water below. Now when a atmosphere cools the surface water, the water sinks, but it does not make it all the way to the bottom. The scenario displayed is one where the condensing effect of the cooling is not strong enough to overcome the effects that salinity has on the density of the water. The less saline the water, the less dense it is. A cold fresh layer of water is constrained near the surface. Sometimes, this layer can even freeze insulating the water from any further cooling by the atmosphere. Note that in this animation there is very little movement of the water at depth back toward the tropics. || ",
            "hits": 161
        },
        {
            "id": 3376,
            "url": "https://svs.gsfc.nasa.gov/3376/",
            "result_type": "Visualization",
            "release_date": "2006-10-02T00:00:00-04:00",
            "title": "Current Tropical Sea Surface Temperatures",
            "description": "Current sea surface temperature (SST) and SST anomaly data. || ",
            "hits": 77
        },
        {
            "id": 3362,
            "url": "https://svs.gsfc.nasa.gov/3362/",
            "result_type": "Visualization",
            "release_date": "2006-06-14T00:00:00-04:00",
            "title": "NASA Scientists Research Tropical Cyclones",
            "description": "From hot towers to phytoplankton blooms, NASA's cutting-edge hurricane research has been revealing never-before-seen aspects of these giant storms for over a decade. The past three years have seen great progress in the areas of intensity monitoring and 3-D modeling of hurricanes. In 2006, scientists at NASA and other institutions have more tools than ever to study these storms using the very latest in ground, air, and space-based technology. The top left window shows sea surface temperature and clouds. Orange and red colors represent ocean temperatures at 82 degrees Fahrenheit or higher.   This is the temperature required for hurricanes to form. The bottom left window shows wind analysis model data from NASA's Modeling, Analysis, and Prediction (MAP '05) program. The top right window shows Rainfall Accumulation for Hurricane Katrina from the TRMM spacecraft. The bottom right window shows Energy-releasing deep convective clouds (to 16 km) in the eyewall of Hurricane Katrina, called 'Hot Towers',  on August 28 occurred while the storm was intensifying to a category 5 classification. || ",
            "hits": 17
        },
        {
            "id": 10069,
            "url": "https://svs.gsfc.nasa.gov/10069/",
            "result_type": "Produced Video",
            "release_date": "2006-06-07T00:00:00-04:00",
            "title": "Bermuda High",
            "description": "The Bermuda High pressure system sits over the Atlantic during summer.  Acting as a block that hurricanes cannot penetrate, the size and location of this system can determine where hurricanes go. A normal Bermuda High often leads to hurricanes moving up the east coast and out to sea.  During summer 2004 and 2005, the Bermuda High expanded to the south and west, which steered hurricanes into the Gulf of Mexico rather than up the east coast or curving out to sea. Once in the Gulf, most hurricane paths will involve landfall at some location. || ",
            "hits": 235
        },
        {
            "id": 3357,
            "url": "https://svs.gsfc.nasa.gov/3357/",
            "result_type": "Visualization",
            "release_date": "2006-06-01T00:00:00-04:00",
            "title": "2006 Sea Surface Temperatures Rising in the Gulf of Mexico",
            "description": "Sea surface temperatures in the Gulf of Mexico rise due to natural summer warming.  These warm surface temperatures are a contributing factor to favorable conditions that can lead to the formation of tropical storms and hurricanes in the Gulf of Mexico and off the Eastern Shore of the United States.  In general, hurricanes tend to form over warm ocean water whose temperature is 82 degrees Fahrenheit (approximately 27.7 degrees Celsius) or higher.  These areas are depicted in yellow, orange, and red.  This data was taken by the AMSR-E instrument aboard the Aqua satellite.This animation depicts the 2006 seasonal changes. || ",
            "hits": 29
        },
        {
            "id": 3489,
            "url": "https://svs.gsfc.nasa.gov/3489/",
            "result_type": "Visualization",
            "release_date": "2006-06-01T00:00:00-04:00",
            "title": "2007 Sea Surface Temperatures in the Gulf of Mexico",
            "description": "Sea surface temperatures in the Gulf of Mexico rise due to natural summer warming.  These warm surface temperatures are a contributing factor to favorable conditions that can lead to the formation of tropical storms and hurricanes in the Gulf of Mexico and off the Eastern Shore of the United States.  In general, hurricanes tend to form over warm ocean water whose temperature is 82 degrees Fahrenheit (approximately 27.7 degrees Celsius) or higher.  These areas are depicted in yellow, orange, and red.  This data was taken by the AMSR-E instrument aboard the Aqua satellite. || ",
            "hits": 14
        },
        {
            "id": 3358,
            "url": "https://svs.gsfc.nasa.gov/3358/",
            "result_type": "Visualization",
            "release_date": "2006-05-30T00:00:00-04:00",
            "title": "Comparing the 1998-1999 La Niña event to the corresponding 2006 Sea Surface Temperature Anomaly Conditions",
            "description": "Are we seeing another La Niña event in 2006? This animation compares the winter 1998-1999 La Niña event to the corresponding 2006 conditions in the Pacific Ocean. This is done by comparing Sea Surface Temperature (SST) anomalies (i.e., differences from normal SST values) between 1999 and 2006. Blue areas indicate ocean regions 5 degrees Celsius (9 degrees Fahrenheit) cooler than the norm. During the 1998-1999 La Niña event this resulted in a distinct area of deep blue stretching across the Pacific Ocean. Through this comparison, one can see that our current ocean temperature conditions do not reflect those same conditions during the 1998-1999 La Niña event. || ",
            "hits": 34
        },
        {
            "id": 2946,
            "url": "https://svs.gsfc.nasa.gov/2946/",
            "result_type": "Visualization",
            "release_date": "2006-05-15T12:00:00-04:00",
            "title": "Europa's Synthetic Subsurface Heat Transport (Version 2)",
            "description": "Encounters with Jupiter's moon Europa by the Voyager and Galileo spacecraft indicated that a liquid salty ocean might exist below a layer of surface ice that is up to 10 kilometers thick. An ocean general circulation model developed to study the earth's oceans was used to investigate the tidally-forced ocean circulations on Europa. The orbit of Europa is 'gravity locked' so that the same side of Europa always faces Jupiter as is the case with the earth's moon. The icy surface of Europa heaves up and down 50 meters due to the strong tidal forces. This visualization shows the temperature changes induced from the flow fields calculated for a European ocean 50 kilometers deep. The warmest temperatures tend to be near the equator, not because of heating by the sun, but because the currents in the European ocean move the warmest waters to that location. Understanding the thermal and flow fields from these model runs will help to interpret observations from future missions to Europa such as the Jupiter's Icy Moons Orbiter mission proposed for launch in 2012. || ",
            "hits": 66
        },
        {
            "id": 2947,
            "url": "https://svs.gsfc.nasa.gov/2947/",
            "result_type": "Visualization",
            "release_date": "2006-05-15T12:00:00-04:00",
            "title": "Europa's Synthetic Subsurface Heat Transport (Version 1)",
            "description": "Under Europa's icy surface are vast extraterrestrial oceans.  This conceptual animation depicts simulated heat transport of these subsurface oceans.  Please note that the simulated heat transport in this animation is only conceptual and a more accurate representation can be found at animation #2946. || ",
            "hits": 34
        },
        {
            "id": 20044,
            "url": "https://svs.gsfc.nasa.gov/20044/",
            "result_type": "Animation",
            "release_date": "2005-03-11T12:00:00-05:00",
            "title": "Indecisive El Niño",
            "description": "This animation shows El Niño's and La Niña's mulitiple personalites.  The sequence begins with normal jet streams, normal sea surface temperatures, and normal wind patterns. The first change illustrates what occurs when a very strong El Niño strikes surface waters in the Central equatorial Pacific Ocean. Warm water anomalies (red) develop in the Central Pacific Ocean while normal westerly winds weaken and allow easterly winds to push the warm water up against the South American Coast. The second change in the animation illustrates typical La Niña conditions. Cold water anomalies (blue) develop as stronger than normal trade winds bring cold water up to the ocean surface. The third change in the animation illustrates the current, weaker El Niño. Warmer waters develop in the central Pacific Ocean and stay in place due to westerly and easterly wind patterns. || ",
            "hits": 54
        },
        {
            "id": 20045,
            "url": "https://svs.gsfc.nasa.gov/20045/",
            "result_type": "Animation",
            "release_date": "2005-03-11T12:00:00-05:00",
            "title": "El Niño Hurricane Connection",
            "description": "Animation compares the effects of La Niña and El Niño on the formation of Atlantic Hurricanes. El Niño tends to suppress the formation of hurricanes by steering the subtropical jet stream into the hurricanes' path and shearing off the tops of the storms before they develop into full intensity. During La Niña, the jet stream moves north, and hurricanes tend to more easily evolve without interference. || ",
            "hits": 28
        },
        {
            "id": 20046,
            "url": "https://svs.gsfc.nasa.gov/20046/",
            "result_type": "Animation",
            "release_date": "2005-03-11T12:00:00-05:00",
            "title": "La Niña Retreat",
            "description": "Winds Of Death - It is the strong east to west winds that sustain La Niña. The winds cause cool waters to rise to the surface from the ocean depths. When the winds diminish, the supply of cool water is cut off and the ocean begins to warm. || ",
            "hits": 16
        },
        {
            "id": 3043,
            "url": "https://svs.gsfc.nasa.gov/3043/",
            "result_type": "Visualization",
            "release_date": "2004-11-01T12:00:00-05:00",
            "title": "Indecisive El Niño Exhibits 'Split Personality'",
            "description": "The central equatorial Pacific Ocean warmed by about one degree Celsius (1.8 degrees Fahrenheit) between June and August 2004, which can indicate development of a weak to moderate El Niño. Yet in other locations, important signals have been absent, suggesting the climate pattern may be of two minds.  NASA satellites show warm water anomalies concentrated in the central Pacific Ocean in August.  By September, the anomalies are weaker.The SeaWinds instrument on NASA's Quick Scatterometer (QuikScat) satellite has shown stronger than normal trade winds for this time of year on the eastern side of the Pacific basin. Since the 1997 to 1998 El Niño, these trade winds have exhibited a kind of 'split personality' condition during times when the central equatorial Pacific warmed. || ",
            "hits": 131
        },
        {
            "id": 20029,
            "url": "https://svs.gsfc.nasa.gov/20029/",
            "result_type": "Animation",
            "release_date": "2004-06-23T12:00:00-04:00",
            "title": "Ocean Circulation Conveyor Belt Helps Balance Climate",
            "description": "As part of the ocean conveyor belt, warm water from the tropical Atlantic moves poleward near the surface where it gives up some of its heat to the atmosphere.  This process partially moderates the cold temperatures at higher latitudes.  As the warm water gives up its heat it becomes more dense and sinks.  This circulation loop is closed as the cooled water makes its way slowly back toward the tropics at lower depths in the ocean.If the poles warm, it is possible that melt water from glaciers and the polar ice cap can shut off this circulation and interrupt this circulation system.  The melt water is fresher and hence less dense than the ocean water it melts into, and thus the melt water will tend to accumulate near the surface.  This layer of fresh water acts as an insulating barrier between the atmosphere and the normal ocean water.  The water from the tropics can not release its heat to the atmosphere, and the circulation loop is interrupted.  The mechanism has a positive feedback potential in that if the ocean circulation slows, then even less heat will make it to the higher latitudes re-enforcing an effect that will cool the climate at these higher latitudes. || ",
            "hits": 284
        },
        {
            "id": 2901,
            "url": "https://svs.gsfc.nasa.gov/2901/",
            "result_type": "Visualization",
            "release_date": "2004-02-12T12:00:00-05:00",
            "title": "Atmospheric Water Vapor during the 1998 La Niña (WMS)",
            "description": "Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds which both warm and cool the Earth in different circumstances.  A key feature of global atmospheric water vapor convection is the Intertropical Convergence Zone, the low pressure region within five degrees of the equator where the trade winds converge and solar heating of the atmosphere forces the water-laden air to rise in altitude, form clouds, and then precipitate as rain in the afternoon.  This visualization shows the global water vapor distribution in gray and white and the global precipitation in yellow every hour from August 30, 1998 to September 20, 1998.  The afternoon thunderstorms in the tropics are seen as a flashing yellow region that moves from east to west, following the sun.  This is a La Niña period, when the water to the west of South America is cooler than normal, forcing the atmosphere there to cool down and hold less water.  Strong east-to-west winds can be seen in this region, contributing to the high water vapor region that forms further to the west over southeast Asia, the Philippines, and Indonesia, causing increased humidity and rainfall in that region.  This data is from the Goddard Earth Modeling System, a coupled land-ocean-atmosphere model which uses earth and satellite-based observations to simulate the Earth's physical system during events such as La Niña. || ",
            "hits": 47
        },
        {
            "id": 2902,
            "url": "https://svs.gsfc.nasa.gov/2902/",
            "result_type": "Visualization",
            "release_date": "2004-02-12T12:00:00-05:00",
            "title": "Atmospheric Water Vapor during the 1997-1998 El Niño (WMS)",
            "description": "Water vapor is a small but significant constituent of the atmosphere, warming the planet due to the greenhouse effect and condensing to form clouds which both warm and cool the Earth in different circumstances.  A key feature of global atmospheric water vapor convection is the Intertropical Convergence Zone, the low pressure region within five degrees of the equator where the trade winds converge and solar heating of the atmosphere forces the water-laden air to rise in altitude, form clouds, and then precipitate as rain in the afternoon.  This visualization shows the global water vapor distribution in gray and white and the global precipitation in yellow every hour from December 20, 1997 to January 14, 1998.  The afternoon thunderstorms in the tropics are seen as a flashing yellow region that moves from east to west, following the sun.  This is an El Niño period, when the water to the west of South America is warmer than normal, allowing the atmosphere there to heat up and hold more water.  This region feeds a high band of water vapor reaching to the southeastern United States and causes increased humidity and rainfall in that region.  This data is from the Goddard Earth Modeling System, a coupled land-ocean-atmosphere model which uses earth and satellite-based observations to simulate the Earth's physical system during events such as El Niño. || ",
            "hits": 18
        },
        {
            "id": 2751,
            "url": "https://svs.gsfc.nasa.gov/2751/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E SST Global Flat Map:  Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures for an indication of hurricane potential. Scientists say above normal Atlantic Ocean temperatures is one reason for the 'above normal' hurricane forecast. Hurricanes convert heat from the tropical atmosphere and oceans to wind and waves, just as a car engine converts gasoline into motion. These animations show a year in the life of global ocean temperatures, June 2, 2002 to May 11, 2003. Green indicates the coolest water, yellow the warmest. The Advanced Microwave Scanning Radiometer (AMSR-E) on the Aqua satellite saw through the clouds to provide sea surface temperatures. || ",
            "hits": 15
        },
        {
            "id": 2752,
            "url": "https://svs.gsfc.nasa.gov/2752/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E Sea Surface Temperature in the Atlantic Used to Forecast 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures for an indication of hurricane potential. Scientists say above normal Atlantic Ocean temperatures is one reason for the 'above normal' hurricane forecast. Hurricanes convert heat from the tropical atmosphere and oceans to wind and waves, just as a car engine converts gasoline into motion. These animations show a year in the life of global ocean temperatures, June 2, 2002 to May 11, 2003. Green indicates the coolest water, yellow the warmest. The Advanced Microwave Scanning Radiometer (AMSR-E) on the Aqua satellite saw through the clouds to provide sea surface temperatures. || ",
            "hits": 15
        },
        {
            "id": 2753,
            "url": "https://svs.gsfc.nasa.gov/2753/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR_E Pacific Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures for an activity predictions for 2003 in part to changing conditions in the Pacific Ocean, such as the demise of El Niño. This sequence traces the evolution of the warmer-than-normal waters associated with the weak El Niño that developed in the late fall of 2002.  By January, the warm conditions began to dissipate.  Fewer than normal hurricanes generally form when El Niño is present.  Researchers say the Pacific may transition to the colder-than-normal La Niña phase.  Areas in red represent warmer than normal and areas in blue represent cooler than normal. || ",
            "hits": 18
        },
        {
            "id": 2754,
            "url": "https://svs.gsfc.nasa.gov/2754/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E Atlantic Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures for an indication of hurricane potential. Scientists say above normal Atlantic Ocean temperatures is one reason for the 'above normal' hurricane forecast. Hurricanes convert heat from the tropical atmosphere and oceans to wind and waves, just as a car engine converts gasoline into motion. These animations show a year in the life of global ocean temperatures, June 2, 2002 to May 11, 2003. Green indicates the coolest water, yellow the warmest. The Advanced Microwave Scanning Radiometer (AMSR-E) on the Aqua satellite saw through the clouds to provide sea surface temperatures. || ",
            "hits": 5
        },
        {
            "id": 2755,
            "url": "https://svs.gsfc.nasa.gov/2755/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E Pacific Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures for an activity predictions for 2003 in part to changing conditions in the Pacific Ocean, such as the demise of El Niño. This sequence traces the evolution of the warmer-than-normal waters associated with the weak El Niño that developed in the late fall of 2002.  By January, the warm conditions began to dissipate.  Fewer than normal hurricanes generally form when El Niño is present.  Researchers say the Pacific may transition to the colder-than-normal La Niña phase.  Areas in red represent warmer than normal and areas in blue represent cooler than normal. || ",
            "hits": 19
        },
        {
            "id": 2756,
            "url": "https://svs.gsfc.nasa.gov/2756/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E Global Anomalous Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season",
            "description": "This animation show a year in the life of anomalous global ocean temperatures, June 2, 2002, to May 11, 2003.  Green indicates the coolest water, yellow the warmest. The Advanced Microwave Scanning Radiometer (AMSR-E) on the Aqua satellite is able to take measurements through clouds to provide this sea surface temperature data. || ",
            "hits": 9
        },
        {
            "id": 2757,
            "url": "https://svs.gsfc.nasa.gov/2757/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E Anomalous Atlantic Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures for an indication of hurricane potential. Scientists say above normal Atlantic Ocean temperatures is one reason for the 'above normal' hurricane forecast. Hurricanes convert heat from the tropical atmosphere and oceans to wind and waves, just as a car engine converts gasoline into motion. These animations show a year in the life of global ocean temperatures, June 2, 2002, to May 11, 2003. Blue indicates the coolest water, red the warmest. The Advanced Microwave Scanning Radiometer (AMSR-E) on the Aqua satellite is able to take measurements through clouds to provide sea surface temperatures. || ",
            "hits": 15
        },
        {
            "id": 2758,
            "url": "https://svs.gsfc.nasa.gov/2758/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E Anomalous Atlantic Sea Surface Temperature Data Used to Forecast 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures for an indication of hurricane potential. Scientists say above normal Atlantic Ocean  temperatures is one reason for the 'above normal' hurricane forecast. Hurricanes convert heat from the tropical atmosphere and oceans to wind and waves,  just as a car engine converts gasoline into motion. These animations show a year in the life of global ocean temperatures, June 2, 2002, to May 11, 2003.  Blue indicates the coolest water anomaly, red the warmest anomaly.The Advanced Microwave Scanning Radiometer (AMSR-E) on the Aqua satellite takes measurements through clouds to provide sea surface temperatures. || ",
            "hits": 14
        },
        {
            "id": 2759,
            "url": "https://svs.gsfc.nasa.gov/2759/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E Anomalous Pacific Sea Surface Temperature Data Used to predict 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures to predict the upcoming year's tropical cyclone activity. This sequence tracks warmer-than-normal waters and colder-than-normal waters in the Pacific Ocean. In 2003, experts have predicted a 'normal to below normal' number of tropical cyclones. Researchers say the Pacific may transition to the colder-than-normal La Niña phase. Fewer than normal hurricanes generally form when El Niño is present. Areas in red represent warmer than normal and areas in blue represent cooler than normal. || ",
            "hits": 25
        },
        {
            "id": 2760,
            "url": "https://svs.gsfc.nasa.gov/2760/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "AMSR-E Anomalous Pacific Sea Surface Temperature Data Used to predict 2003 Hurricane Season",
            "description": "Researchers and forecasters often study sea surface temperatures to predict the upcoming year's tropical cyclone activity.   This sequence tracks warmer-than-normal waters and colder-than-normal waters in the Pacific Ocean.  In 2003, experts have  predicted a 'normal to below normal' number of tropical cylones.  Researchers say the Pacific may transition to the colder-than-normal La Niña phase.  Fewer than normal hurricanes generally form when El Niño is present.  Areas in red represent warmer than normal and areas in blue represent cooler than normal. || ",
            "hits": 17
        },
        {
            "id": 2705,
            "url": "https://svs.gsfc.nasa.gov/2705/",
            "result_type": "Visualization",
            "release_date": "2003-02-26T12:00:00-05:00",
            "title": "Terra/Aqua Snow Sequence January/February 2003",
            "description": "This is a sequence of snow images from the Terra and Aqua Satellites in January and February 2003. || ",
            "hits": 15
        },
        {
            "id": 2691,
            "url": "https://svs.gsfc.nasa.gov/2691/",
            "result_type": "Visualization",
            "release_date": "2003-02-03T12:00:00-05:00",
            "title": "Sea Surface Temperature Anomalies",
            "description": "Sea surface temperature (SST) anomalies show the development of the 2002/2003 El Niño based on data from NASA's Aqua spacecraft. || Sea surface temperature anomalies from 2002/2003 || a002691.00040_print.png (720x480) [667.4 KB] || sst_pre.jpg (320x218) [16.0 KB] || a002691.webmhd.webm (960x540) [4.2 MB] || 720x486_4x3_29.97p (720x486) [16.0 KB] || a002691.dv (720x480) [58.4 MB] || sst.mpg (352x240) [2.2 MB] || a002691_320.m1v (320x240) [3.1 MB] || ",
            "hits": 20
        },
        {
            "id": 2692,
            "url": "https://svs.gsfc.nasa.gov/2692/",
            "result_type": "Visualization",
            "release_date": "2003-02-03T12:00:00-05:00",
            "title": "Sea Surface Temperature Anomalies (with dates)",
            "description": "Sea surface temperature (SST) anomalies show the development of the 2002/2003 El Niño based on data from NASA's Aqua spacecraft. || ",
            "hits": 8
        },
        {
            "id": 2693,
            "url": "https://svs.gsfc.nasa.gov/2693/",
            "result_type": "Visualization",
            "release_date": "2003-02-03T12:00:00-05:00",
            "title": "Sea Surface Wind Anomalies",
            "description": "Sea surface wind anomalies show the development of the 2002/2003 El Niño based on data from NASA's QuikSCAT spacecraft. The wind data has been processed using the Variational Analysis Method (VAM). || ",
            "hits": 9
        },
        {
            "id": 2694,
            "url": "https://svs.gsfc.nasa.gov/2694/",
            "result_type": "Visualization",
            "release_date": "2003-02-03T12:00:00-05:00",
            "title": "Sea Surface Wind Anomalies (with dates)",
            "description": "Sea surface wind anomalies show the development of the 2002/2003 El Niño based on data from NASA's QuikSCAT spacecraft. The wind data has been processed using the Variational Analysis Method (VAM). || ",
            "hits": 12
        },
        {
            "id": 2695,
            "url": "https://svs.gsfc.nasa.gov/2695/",
            "result_type": "Visualization",
            "release_date": "2003-02-03T12:00:00-05:00",
            "title": "SST Anomalies + Wind Anomalies",
            "description": "Sea surface temperature (SST) anomalies and sea surface wind anomalies show the development of the 2002/2003 El Niño based on data from NASA's Aqua and QuikSCAT spacecraft.  The wind data has been processed using the Variational Analysis Method (VAM). || ",
            "hits": 14
        },
        {
            "id": 2696,
            "url": "https://svs.gsfc.nasa.gov/2696/",
            "result_type": "Visualization",
            "release_date": "2003-02-03T12:00:00-05:00",
            "title": "SST Anomalies + Wind Anomalies (with dates)",
            "description": "Sea surface temperature (SST) anomalies and sea surface wind anomalies show the development of the 2002/2003 El Niño based on data from NASA's Aqua and QuikSCAT spacecraft. The wind data has been processed using the Variational Analysis Method (VAM). || ",
            "hits": 12
        },
        {
            "id": 2697,
            "url": "https://svs.gsfc.nasa.gov/2697/",
            "result_type": "Visualization",
            "release_date": "2003-02-03T12:00:00-05:00",
            "title": "Sea Surface Wind Anomalies in the North Atlantic",
            "description": "Sea surface wind anomalies (based on QuikSCAT data) from 31 December 2002 illustrate the wind patterns that exist during a North Atlantic Oscillation.  The wind data has been processed using the Variational Analysis Method (VAM). || ",
            "hits": 11
        },
        {
            "id": 2698,
            "url": "https://svs.gsfc.nasa.gov/2698/",
            "result_type": "Visualization",
            "release_date": "2003-02-03T12:00:00-05:00",
            "title": "Sea Surface Wind Anomalies in North Atlantic (with Date)",
            "description": "Sea surface wind anomalies (based on QuikSCAT data) from 31 December 2003 illustrate the wind patterns that exist during a North Atlantic Oscillation. The wind data has been processed using the Variational Analysis Method (VAM). || ",
            "hits": 17
        },
        {
            "id": 2432,
            "url": "https://svs.gsfc.nasa.gov/2432/",
            "result_type": "Visualization",
            "release_date": "2002-04-22T12:00:00-04:00",
            "title": "Sea Surface Temperature Anomaly from July 5, 2001 to March 10, 2002",
            "description": "This animation depicts the difference between the actual sea surface temperature and the average climatology data. Blue areas indicate temperatures colder than average while red areas indicate regions that are warmer. Temperature values between -4 degrees and +3 degrees are mapped to gradient color ramps, and regions with less than one degree deviation from average are shown as gray. || ",
            "hits": 17
        },
        {
            "id": 2423,
            "url": "https://svs.gsfc.nasa.gov/2423/",
            "result_type": "Visualization",
            "release_date": "2002-04-12T12:00:00-04:00",
            "title": "Great Zoom out of Baltimore, MD: Maryland Science Center (for the Volvo Ocean Race presentation)",
            "description": "Using data from different spacecraft and some powerful computer technology, visualizers at the Goddard Space Flight Center present you with a collection of American cities in a way you have never seen them before. Starting with our camera high above the Earth, we rush in towards the surface at what would be an impossible speed for any known vehicle. Passing though layers of atmosphere, the colors of our destinations shimmer with their own unique characteristics, and suddenly we find ourselves floating in virtual space just above the ground. This particular zoom also incorporates a fly through the clouds revealing the Terra/MODIS 'wonderglobe' with clouds. || ",
            "hits": 18
        },
        {
            "id": 2398,
            "url": "https://svs.gsfc.nasa.gov/2398/",
            "result_type": "Visualization",
            "release_date": "2002-03-07T12:00:00-05:00",
            "title": "Global Sea Surface Temperature from MODIS between July 2001 and February 2002",
            "description": "This animation shows the sea surface temperature in the Pacific Ocean in false color from July 2001 to the middle of February 2002 || a002398.00100_print.png (720x480) [467.1 KB] || sstdaily_pre.jpg (320x240) [10.6 KB] || a002398.webmhd.webm (960x540) [3.0 MB] || a002398.dv (720x480) [47.3 MB] || sstdaily.mpg (320x240) [1.4 MB] || ",
            "hits": 36
        },
        {
            "id": 2399,
            "url": "https://svs.gsfc.nasa.gov/2399/",
            "result_type": "Visualization",
            "release_date": "2002-03-07T12:00:00-05:00",
            "title": "A Close View of Sea Surface Temperature Anomaly for February 15, 2002",
            "description": "This image shows the difference between the actual sea surface temperature data and the average climatology data in the eastern portion of the Pacific Ocean for February 15, 2002. || closeanomaly.jpg (2880x1944) [2.2 MB] || closeanomaly_web.png (320x216) [156.3 KB] || closeanomaly_thm.png (80x40) [7.4 KB] || closeanomaly_searchweb.png (320x180) [107.0 KB] || closeanomaly.tif (2880x1944) [12.4 MB] || ",
            "hits": 14
        },
        {
            "id": 2400,
            "url": "https://svs.gsfc.nasa.gov/2400/",
            "result_type": "Visualization",
            "release_date": "2002-03-07T12:00:00-05:00",
            "title": "A Pacific View of Sea Surface Temperature from MODIS for February 15, 2002",
            "description": "Sea surface temperature in the Pacific Ocean is shown in false color for February 15, 2002 || pacificsst.jpg (2880x1944) [1.3 MB] || pacificsst_web.png (320x216) [108.3 KB] || pacificsst_thm.png (80x40) [6.1 KB] || pacificsst_searchweb.png (320x180) [96.7 KB] || pacificsst.tif (2880x1944) [8.7 MB] || Video slate image reads \"A Pacific View of Sea Surface Temperature from MODIS for February 15, 2002\". || a002400_slate.jpg (720x528) [133.4 KB] || a002400_slate_web.png (320x234) [111.3 KB] || ",
            "hits": 9
        },
        {
            "id": 2401,
            "url": "https://svs.gsfc.nasa.gov/2401/",
            "result_type": "Visualization",
            "release_date": "2002-03-07T12:00:00-05:00",
            "title": "A Pacific View of Sea Surface Temperature Anomaly for February 15, 2002",
            "description": "This anomaly image shows the difference between the actual sea surface temperature and the average climatology data in the Pacific Ocean for February 15, 2002. || pacificanomaly.jpg (2880x1944) [2.2 MB] || pacificanomaly_web.png (320x216) [153.8 KB] || pacificanomaly_thm.png (80x40) [7.3 KB] || pacificanomaly_searchweb.png (320x180) [121.5 KB] || pacificanomaly.tif (2880x1944) [12.3 MB] || ",
            "hits": 12
        },
        {
            "id": 2395,
            "url": "https://svs.gsfc.nasa.gov/2395/",
            "result_type": "Visualization",
            "release_date": "2002-03-05T12:00:00-05:00",
            "title": "Pulse of the Planet",
            "description": "Akin to a living creature, Earth's land, air, oceans, ice, and life fit together into a complex, interlocking system.  Space affords a unique vantage point from which to observe the daily, seasonal, and annual changes in Earth's systems. Using data from advanced satellites, NASA visualizations portray a majestic, and sometimes violent, natural world and also capture the influences humans have on the planet.Over 80 NASA-related earth science animations created over the past 8 years implementing realtime and non-realtime techniques have been used on this visual journey.  Tools used included IDL, Lightwave3D, Final Cut Pro, Performer, Vis5D, and custom software. || ",
            "hits": 77
        },
        {
            "id": 2392,
            "url": "https://svs.gsfc.nasa.gov/2392/",
            "result_type": "Visualization",
            "release_date": "2002-02-28T12:00:00-05:00",
            "title": "NSIPP cloud cover: Dec 1997 - Jan 1998 (El Niño)",
            "description": "Simulation of cloud cover over Antarctica and South America during the 1997-1998 El Niño. || a002392.00100_print.png (720x480) [351.9 KB] || nsipp-clouds-1997_12-400x400-0-br3M-fps24_pre.jpg (320x320) [16.7 KB] || nsipp-clouds-1997_12-400x400-0-br3M-fps24_thm.png (80x40) [3.4 KB] || nsipp-clouds-1997_12-640x480-0-br4_5M-fps24_pre.jpg (320x240) [12.7 KB] || nsipp-clouds-1997_12-960x640-0-br4_5M-fps24_pre.jpg (320x213) [11.6 KB] || nsipp-clouds-1997_12-960x640-0-br4_5M-fps24_pre_searchweb.jpg (320x180) [71.7 KB] || nsipp-clouds-1997_12-960x640-0-br4_5M-fps24.mpg (960x640) [16.1 MB] || nsipp-clouds-1997_12-960x640-0-br4_5M-fps24.webmhd.webm (960x540) [9.1 MB] || nsipp-clouds-1997_12-640x480-0-br4_5M-fps24.mpg (640x480) [16.0 MB] || a002392.dv (720x480) [105.1 MB] || nsipp-clouds-1997_12-400x400-0-br3M-fps24.mpg (400x400) [10.7 MB] || ",
            "hits": 17
        },
        {
            "id": 2393,
            "url": "https://svs.gsfc.nasa.gov/2393/",
            "result_type": "Visualization",
            "release_date": "2002-02-28T12:00:00-05:00",
            "title": "NSIPP cloud cover: Oct 1998 - Nov 1998 (La Niña)",
            "description": "Simulation of cloud cover over Antarctica and South America during the 1998 La Niña. || a002393.00100_print.png (720x480) [346.4 KB] || nsipp-clouds-1998_10-400x400-0-br3M-fps24_pre.jpg (320x320) [16.5 KB] || nsipp-clouds-1998_10-400x400-0-br3M-fps24_thm.png (80x40) [3.4 KB] || nsipp-clouds-1998_10-640x480-0-br4_5M-fps24_pre.jpg (320x240) [12.5 KB] || nsipp-clouds-1998_10-960x640-0-br4_5M-fps24_pre.jpg (320x213) [11.5 KB] || nsipp-clouds-1998_10-960x640-0-br4_5M-fps24_pre_searchweb.jpg (320x180) [71.6 KB] || nsipp-clouds-1998_10-960x640-0-br4_5M-fps24.mpg (960x640) [14.5 MB] || nsipp-clouds-1998_10-960x640-0-br4_5M-fps24.webmhd.webm (960x540) [7.8 MB] || nsipp-clouds-1998_10-640x480-0-br4_5M-fps24.mpg (640x480) [14.4 MB] || a002393.dv (720x480) [96.8 MB] || nsipp-clouds-1998_10-400x400-0-br3M-fps24.mpg (400x400) [9.6 MB] || ",
            "hits": 12
        },
        {
            "id": 2394,
            "url": "https://svs.gsfc.nasa.gov/2394/",
            "result_type": "Visualization",
            "release_date": "2002-02-28T12:00:00-05:00",
            "title": "NSIPP Cloud Cover: Feb 2002",
            "description": "Simulation of cloud cover over Antarctica and South America during February 2002. || a002394.00100_print.png (720x480) [349.6 KB] || nsipp-clouds-2002_02-400x400-0-br3M-fps24_thm.png (80x40) [3.4 KB] || nsipp-clouds-2002_02-400x400-0-br3M-fps24_pre.jpg (320x320) [16.8 KB] || nsipp-clouds-2002_02-640x480-0-br4_5M-fps24_pre.jpg (320x240) [12.8 KB] || nsipp-clouds-2002_02-960x640-0-br4_5M-fps24_pre.jpg (320x213) [11.6 KB] || nsipp-clouds-2002_02-960x640-0-br4_5M-fps24_pre_searchweb.jpg (320x180) [71.8 KB] || nsipp-clouds-2002_02-960x640-0-br4_5M-fps24.mpg (960x640) [16.1 MB] || nsipp-clouds-2002_02-960x640-0-br4_5M-fps24.webmhd.webm (960x540) [8.8 MB] || nsipp-clouds-2002_02-640x480-0-br4_5M-fps24.mpg (640x480) [16.0 MB] || a002394.dv (720x480) [104.8 MB] || nsipp-clouds-2002_02-400x400-0-br3M-fps24.mpg (400x400) [10.7 MB] || ",
            "hits": 9
        },
        {
            "id": 2366,
            "url": "https://svs.gsfc.nasa.gov/2366/",
            "result_type": "Visualization",
            "release_date": "2002-02-06T12:00:00-05:00",
            "title": "NSIPP North America Forecast December 1, 2001 - November 30, 2002: Sea Surface Temperature Anomaly",
            "description": "Sea surface temperature anomalies forecasted in the northern Pacific for December 2001 through November 2002, from the NASA Seasonal-to-Interannual Prediction Project || a002366.00005_print.png (720x480) [437.7 KB] || a002366_thm.png (80x40) [4.4 KB] || a002366_pre.jpg (320x238) [7.6 KB] || a002366_pre_searchweb.jpg (320x180) [51.8 KB] || a002366.webmhd.webm (960x540) [7.0 MB] || a002366.dv (720x480) [130.3 MB] || a002366.mpg (352x240) [5.4 MB] || ",
            "hits": 14
        },
        {
            "id": 2367,
            "url": "https://svs.gsfc.nasa.gov/2367/",
            "result_type": "Visualization",
            "release_date": "2002-02-06T12:00:00-05:00",
            "title": "NSIPP N. America Forecast Dec. 1, 2001 - Nov. 30, 2002: Sea Surface Temp. Anomaly, Water Vapor, Soil Moisture",
            "description": "Sea surface temperature anomalies, atmospheric water vapor, and soil moisture forecasted in the northern Pacific and North America for December 2001 through November 2002, from the NASA Seasonal-to-Interannual Prediction Project || a002367.00005_print.png (720x480) [447.9 KB] || a002367_thm.png (80x40) [4.5 KB] || a002367_pre.jpg (320x238) [7.1 KB] || a002367_pre_searchweb.jpg (320x180) [49.4 KB] || a002367.webmhd.webm (960x540) [6.0 MB] || a002367.dv (720x480) [130.3 MB] || a002367.mpg (352x240) [5.7 MB] || ",
            "hits": 10
        },
        {
            "id": 2368,
            "url": "https://svs.gsfc.nasa.gov/2368/",
            "result_type": "Visualization",
            "release_date": "2002-02-06T12:00:00-05:00",
            "title": "NSIPP North America Forecast Dec. 1, 2001 - Nov. 30, 2002: Sea Surface Temperature Anomaly, Water Vapor",
            "description": "Sea surface temperature anomalies and atmospheric water vapor forecasted in the northern Pacific and over North America for December 2001 through November 2002, from the NASA Seasonal-to-Interannual Prediction Project || a002368.00095_print.png (720x480) [438.0 KB] || a002368_thm.png (80x40) [4.5 KB] || a002368_pre.jpg (320x238) [7.4 KB] || a002368_pre_searchweb.jpg (320x180) [48.1 KB] || a002368.webmhd.webm (960x540) [7.0 MB] || a002368.dv (720x480) [130.3 MB] || a002368.mpg (352x240) [5.7 MB] || ",
            "hits": 14
        },
        {
            "id": 2132,
            "url": "https://svs.gsfc.nasa.gov/2132/",
            "result_type": "Visualization",
            "release_date": "2001-05-01T12:00:00-04:00",
            "title": "NSIPP: North America Soil Moisture",
            "description": "An animation of soil moisture from December 1999 through June 2000 for North America from the NSIPP global climate model || a002132.00095_print.png (720x480) [460.5 KB] || a002132_thm.png (80x40) [4.5 KB] || a002132_pre.jpg (320x238) [7.4 KB] || a002132_pre_searchweb.jpg (320x180) [54.1 KB] || a002132.webmhd.webm (960x540) [3.1 MB] || a002132.dv (720x480) [157.4 MB] || a002132.mp4 (640x480) [8.3 MB] || a002132.mpg (352x240) [5.7 MB] || ",
            "hits": 10
        },
        {
            "id": 2057,
            "url": "https://svs.gsfc.nasa.gov/2057/",
            "result_type": "Visualization",
            "release_date": "2001-01-19T12:00:00-05:00",
            "title": "El Niño-La Niña Sea Surface Temperature Anomalies from NSIPP: January 1998 through September 2001",
            "description": "A view of El Niño and La Niña through Pacific sea surface temperature anomalies from 1998 through 2001. || ",
            "hits": 38
        },
        {
            "id": 1244,
            "url": "https://svs.gsfc.nasa.gov/1244/",
            "result_type": "Visualization",
            "release_date": "2000-08-28T12:00:00-04:00",
            "title": "NSIPP: Global Soil Moisture",
            "description": "An Animation of global soil moisture from December 1999 through June 2000 from the NSIPP global climate model || a001244.00005_print.png (720x480) [391.0 KB] || a001244_pre.jpg (320x242) [8.3 KB] || a001244.webmhd.webm (960x540) [3.6 MB] || a001244.dv (720x480) [157.7 MB] || a001244.mp4 (640x480) [8.2 MB] || a001244.mpg (352x240) [5.6 MB] || ",
            "hits": 5
        },
        {
            "id": 1245,
            "url": "https://svs.gsfc.nasa.gov/1245/",
            "result_type": "Visualization",
            "release_date": "2000-08-28T12:00:00-04:00",
            "title": "NSIPP: North America Water Vapor and Soil Moisture",
            "description": "An animation of atmospheric water vapor and soil moisture from December 1999 through June 2000 for North America from the NSIPP global climate model || a001245.00005_print.png (720x480) [512.7 KB] || a001245_pre.jpg (320x238) [8.2 KB] || a001245.webmhd.webm (960x540) [5.3 MB] || a001245.dv (720x480) [157.4 MB] || a001245.mp4 (640x480) [8.5 MB] || a001245.mpg (352x240) [5.8 MB] || ",
            "hits": 13
        },
        {
            "id": 1246,
            "url": "https://svs.gsfc.nasa.gov/1246/",
            "result_type": "Visualization",
            "release_date": "2000-08-28T12:00:00-04:00",
            "title": "NSIPP Global Water Vapor, Soil Moisture, and Sea Surface Temperature Anomaly",
            "description": "An animation of global sea surface temperature anomaly, soil moisture, and atmospheric water vapor from June 2000 through June 2001 from the NSIPP global climate model || a001246.00005_print.png (720x480) [505.5 KB] || a001246_thm.png (80x40) [8.0 KB] || a001246_pre.jpg (320x218) [18.3 KB] || a001246_pre_searchweb.jpg (320x180) [98.0 KB] || a001246.webmhd.webm (960x540) [13.6 MB] || a001246.dv (720x480) [278.5 MB] || a001246.mp4 (640x480) [14.7 MB] || a001246.mpg (352x240) [10.2 MB] || ",
            "hits": 5
        },
        {
            "id": 1247,
            "url": "https://svs.gsfc.nasa.gov/1247/",
            "result_type": "Visualization",
            "release_date": "2000-08-28T12:00:00-04:00",
            "title": "NSIPP: Time-Dependent Three-Dimensional Sea Surface Temperature Isosurfaces in the Pacific",
            "description": "A animation of three-dimensional sea surface temperature isosurfaces in the Pacific between -15 degrees and +15 degrees latitude.  Data is derived from the NSIPP global climate model. || a001247.00005_print.png (720x480) [392.7 KB] || a001247_thm.png (80x40) [5.3 KB] || a001247_pre.jpg (320x218) [11.3 KB] || a001247_pre_searchweb.jpg (320x180) [54.3 KB] || a001247.webmhd.webm (960x540) [18.3 MB] || a001247.dv (720x480) [267.6 MB] || a001247.mp4 (640x480) [14.5 MB] || a001247.mpg (352x240) [10.2 MB] || ",
            "hits": 10
        },
        {
            "id": 1248,
            "url": "https://svs.gsfc.nasa.gov/1248/",
            "result_type": "Visualization",
            "release_date": "2000-08-28T12:00:00-04:00",
            "title": "NSIPP: Three-Dimensional Sea Surface Temperature Isosurfaces",
            "description": "A series of three-dimensional isosurfaces of constant temperature are overlaid on a three dimensional bathymetry dataset of the Earths ocean basins.  Higher temperatures are in red and lower temperatures are in blue.  Data is derived from the NSIPP global climate model. || a001248.00095_print.png (720x480) [417.7 KB] || a001248_thm.png (80x40) [6.8 KB] || a001248_pre.jpg (320x218) [14.2 KB] || a001248_pre_searchweb.jpg (320x180) [81.0 KB] || a001248.webmhd.webm (960x540) [3.2 MB] || a001248.dv (720x480) [83.8 MB] || a001248.mp4 (640x480) [4.6 MB] || a001248.mpg (352x240) [2.4 MB] || ",
            "hits": 5
        },
        {
            "id": 1249,
            "url": "https://svs.gsfc.nasa.gov/1249/",
            "result_type": "Visualization",
            "release_date": "2000-08-28T12:00:00-04:00",
            "title": "NSIPP North American Water Vapor, Soil Moisture, and Sea Surface Temperature Anomaly",
            "description": "An animation of sea surface temperature anomaly, soil moisture, and atmospheric water vapor for North America from June 2000 through June 2001 from the NSIPP global climate model || a001249.00005_print.png (720x480) [572.3 KB] || a001249_thm.png (80x40) [7.7 KB] || a001249_pre.jpg (320x218) [17.7 KB] || a001249_pre_searchweb.jpg (320x180) [88.8 KB] || a001249.webmhd.webm (960x540) [13.6 MB] || a001249.dv (720x480) [278.5 MB] || a001249.mp4 (640x480) [15.3 MB] || a001249.mpg (352x240) [10.3 MB] || ",
            "hits": 11
        },
        {
            "id": 1250,
            "url": "https://svs.gsfc.nasa.gov/1250/",
            "result_type": "Visualization",
            "release_date": "2000-08-28T12:00:00-04:00",
            "title": "NSIPP Global SST Anomaly and Soil Moisture",
            "description": "An animation of global sea surface temperature anomaly and soil moisture from June 2000 through June 2001 from the NSIPP global climate model || a001250.00095_print.png (720x480) [474.9 KB] || a001250_thm.png (80x40) [7.9 KB] || a001250_pre.jpg (320x218) [23.7 KB] || a001250_pre_searchweb.jpg (320x180) [106.2 KB] || a001250.webmhd.webm (960x540) [3.4 MB] || a001250.dv (720x480) [54.7 MB] || a001250.mp4 (640x480) [2.8 MB] || a001250.mpg (352x240) [1.6 MB] || ",
            "hits": 52
        },
        {
            "id": 1251,
            "url": "https://svs.gsfc.nasa.gov/1251/",
            "result_type": "Visualization",
            "release_date": "2000-08-28T12:00:00-04:00",
            "title": "NSIPP: Ray-casted Global Sea Surface Temperature",
            "description": "A rotating cartesian projection of the Earth showing three-dimensional sea surface temperature data from the NSIPP global climate model.  High temperatures are in red. || a001251.00095_print.png (720x480) [396.2 KB] || a001251_thm.png (80x40) [5.4 KB] || a001251_pre.jpg (320x238) [7.6 KB] || a001251_pre_searchweb.jpg (320x180) [57.4 KB] || a001251.webmhd.webm (960x540) [1.8 MB] || a001251.dv (720x480) [66.6 MB] || a001251.mp4 (640x480) [3.6 MB] || a001251.mpg (352x240) [1.8 MB] || ",
            "hits": 6
        }
    ]
}