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        {
            "id": 5620,
            "url": "https://svs.gsfc.nasa.gov/5620/",
            "result_type": "Visualization",
            "release_date": "2026-03-02T12:00:00-05:00",
            "title": "Sea Level Through a Porthole (2026)",
            "description": "As the planet warms and polar ice melts, our global average sea level is rising. Although exact ocean heights vary due to local geography, climate over time, and dynamic fluid interactions with gravity and planetary rotation, scientists observe sea level trends by comparing measurements against a 22 year spatial and temporal mean reference. These visualizations use the visual metaphor of a submerged porthole window to observe how far our oceans rose between 1993 and the end of 2025.",
            "hits": 781
        },
        {
            "id": 5611,
            "url": "https://svs.gsfc.nasa.gov/5611/",
            "result_type": "Visualization",
            "release_date": "2026-01-30T09:00:00-05:00",
            "title": "Global Mean Sea Level 1993-2025",
            "description": "This animation shows the rise in global mean sea level from 1993 to 2023 based on data from a series of five international satellites.",
            "hits": 606
        },
        {
            "id": 5520,
            "url": "https://svs.gsfc.nasa.gov/5520/",
            "result_type": "Visualization",
            "release_date": "2025-03-25T09:00:00-04:00",
            "title": "Sea Level Through a Porthole (2025)",
            "description": "As the planet warms and polar ice melts, our global average sea level is rising. Although exact ocean heights vary due to local geography, climate over time, and dynamic fluid interactions with gravity and planetary rotation, scientists observe sea level trends by comparing measurements against a 22 year spatial and temporal mean reference. These visualizations use the visual metaphor of a submerged porthole window to observe how far our oceans rose between 1993 and 2025. || ",
            "hits": 371
        },
        {
            "id": 5516,
            "url": "https://svs.gsfc.nasa.gov/5516/",
            "result_type": "Visualization",
            "release_date": "2025-03-11T00:00:00-04:00",
            "title": "Global Mean Sea Level 1993-2024",
            "description": "This animation shows the rise in global mean sea level from 1993 to 2024 based on data from a series of five international satellites.",
            "hits": 482
        },
        {
            "id": 5312,
            "url": "https://svs.gsfc.nasa.gov/5312/",
            "result_type": "Visualization",
            "release_date": "2024-06-16T18:00:00-04:00",
            "title": "Slow Reveal Graphs: Global Mean Sea Level 1993-2023",
            "description": "Slow reveal graphs are an instructional routine using scaffolded visuals and discourse to help students (in K-12 and beyond) make sense of data.  This is a slow reveal graph of the SVS visualization of rising Global Mean Sea Level. || ",
            "hits": 65
        },
        {
            "id": 5304,
            "url": "https://svs.gsfc.nasa.gov/5304/",
            "result_type": "Visualization",
            "release_date": "2024-05-30T00:00:00-04:00",
            "title": "Sea Level Through a Porthole (2023) for Science-on-a-Sphere",
            "description": "This visualization watches the global mean sea level change through a circular window. The blue mark on the ruler shows the exact measurements of the Integrated Multi-Mission Ocean Altimeter Data for Climate Research. The level of the animated water changes more smoothly, driven by a 60-day floating average of the same data.When played on a standard 68\" Science-on-a-Sphere display, the measurement markings in the video are accurate to the real world.",
            "hits": 219
        },
        {
            "id": 5221,
            "url": "https://svs.gsfc.nasa.gov/5221/",
            "result_type": "Visualization",
            "release_date": "2024-03-21T12:00:00-04:00",
            "title": "Global Mean Sea Level 1993-2023",
            "description": "This animation shows the rise in global mean sea level from 1993 to 2023 based on data from a series of five international satellites. The spike in sea level from 2022 to 2023 is mostly a consequence of climate change and the development of El Niño conditions in the Pacific Ocean. || seaLevelRise_2024_English.00405_print.jpg (1024x576) [188.5 KB] || seaLevelRise_2024_English.00405_web.png (320x180) [54.4 KB] || seaLevelRise_2024_English.00405_thm.png (80x40) [5.1 KB] || seaLevel_Curves_2024_English.00405_searchweb.png (320x180) [41.9 KB] || English (3840x2160) [0 Item(s)] || seaLevelRise_2024_English.mp4 (3840x2160) [45.0 MB] || Climate-dashboard.hwshow [1.6 KB] || ",
            "hits": 251
        },
        {
            "id": 13746,
            "url": "https://svs.gsfc.nasa.gov/13746/",
            "result_type": "Produced Video",
            "release_date": "2020-11-17T06:00:00-05:00",
            "title": "Measuring the Seas from Space! U.S.-European Satellite Launching THIS SATURDAY Seeks to Answer Vital Climate Questions Live Shots",
            "description": "Click here for: Sentinel-6 Michael Freilich Media Reel. Includes links to associated b-roll Click HERE for lightly edited b-roll showing the launch animation and the satellite in orbit.Click here for the PRESS KITClick here for social media video in SPANISH || Sentinel_6_Banner.png (6254x2093) [3.8 MB] || Sentinel_6_Banner_print.jpg (1024x342) [67.7 KB] || Sentinel_6_Banner_searchweb.png (320x180) [67.5 KB] || Sentinel_6_Banner_thm.png (80x40) [5.4 KB] || ",
            "hits": 40
        },
        {
            "id": 4804,
            "url": "https://svs.gsfc.nasa.gov/4804/",
            "result_type": "Visualization",
            "release_date": "2020-10-13T00:00:00-04:00",
            "title": "Greenland Ice Sheet: Three Futures",
            "description": "This movie shows the evolution of several regions of the Greenland Ice Sheet between 2008 and 2300 based on three different climate scenarios. Each scenario reflects a potential future climate outcome based on current and future greenhouse gas emmisions. The regions shown in a violet color are exposed areas of the Greenland bed that were covered by the ice sheet in 2008. || Greenland_NE_2008_2300_HD_still.2127.jpg (1920x1080) [1.0 MB] || Greenland_NE_2008_2300_HD_still.2127_print.jpg (1024x576) [159.2 KB] || Greenland_NE_2008_2300_HD_still.2127_searchweb.png (320x180) [81.1 KB] || Greenland_NE_2008_2300_HD_still.2127_thm.png (80x40) [7.1 KB] || GreenlandVizV5.webm (1920x1080) [19.7 MB] || Greenland_NE_2008_2300_HD_still.2127.tif (1920x1080) [2.0 MB] || GreenlandVizV5.mp4 (1920x1080) [181.9 MB] || GreenlandViz_FINAL.mov (1920x1080) [5.8 GB] || GreenlandVizV5.mp4.hwshow [378 bytes] || ",
            "hits": 114
        },
        {
            "id": 4823,
            "url": "https://svs.gsfc.nasa.gov/4823/",
            "result_type": "Visualization",
            "release_date": "2020-09-11T00:00:00-04:00",
            "title": "Draining the Oceans",
            "description": "Data visualization of the draining of the Earth's oceans. The visualization simulates an incremental drop of 10 meters of the water’s level on Earth’s surface. As time progresses and the oceans drain, it becomes evident that underwater mountain ranges are bigger in size and trenches are deeper in comparison to those on dry land. While water drains quickly closer to continents, it drains slowly in our planet’s deepest trenches. || OceanDrain_3840x2160_60fps_0837_print.jpg (1024x576) [259.5 KB] || OceanDrain_3840x2160_60fps_0837_print_searchweb.png (320x180) [97.8 KB] || OceanDrain_3840x2160_60fps_0837_print_thm.png (80x40) [7.8 KB] || OceanDrain_1920x1080_30fps.mp4 (1920x1080) [44.2 MB] || OceanDrain_1920x1080_30fps.webm (1920x1080) [4.3 MB] || OceanDrain (3840x2160) [0 Item(s)] || OceanDrain (3840x2160) [0 Item(s)] || OceanDrain_3840x2160_60fps_0837.tif (3840x2160) [31.6 MB] || OceanDrain_3840x2160_30fps.mp4 (3840x2160) [154.1 MB] || OceanDrain_1920x1080_30fps.mp4.hwshow [192 bytes] || ",
            "hits": 702
        },
        {
            "id": 4743,
            "url": "https://svs.gsfc.nasa.gov/4743/",
            "result_type": "Visualization",
            "release_date": "2019-07-30T00:00:00-04:00",
            "title": "Greenland's Jakobshavn Region: Three Simulated Greenland Ice Sheet Response Scenarios: 2008 - 2300",
            "description": "The Greenland Ice Sheet holds enough water to raise the world’s sea level by over 7 meters (23 feet). Rising atmosphere and ocean temperatures have led to an ice loss equivalent to over a centimeter increase in global mean sea-level between 1991 and 2015. Large outlet glaciers, rivers of ice moving to the sea, drain the ice from the interior of Greenland and cause the outer margins of the ice sheet to recede. Improvements in measuring the ice thickness in ice sheets is enabling better simulation of the flow in outlet glaciers, which is key to predicting the retreat of ice sheets into the future.Recently, a simulation of the effects of outlet glacier flow on ice sheet thickness coupled with improved data and comprehensive climate modeling for differing future climate scenarios has been used to estimate Greenland’s contribution to sea-level over the next millennium. Greenland could contribute 5–34 cm (2-13 inches) to sea-level by 2100 and 11–162 cm (4-64 inches) by 2200, with outlet glaciers contributing 19–40 % of the total mass loss. The analysis shows that uncertainties in projecting mass loss are dominated by uncertainties in climate scenarios and surface processes, followed by ice dynamics. Uncertainties in ocean conditions play a minor role, particularly in the long term. Greenland will very likely become ice-free within a millennium without significant reductions in greenhouse gas emissions.Three visualizations of the evolution of the Jakobshavn region of the Greenland Ice Sheet between 2008 and 2300 based on three different climate scenarios are shown below. Each scenario is described briefly in the caption under each visualization. Each of the three visualizations are provided with a date, colorbar and a distance scale as well as without. The regions shown in a violet color are exposed areas of the Greenland bed that were covered by the ice sheet in 2008.The data sets used for these animations are the control (“CTRL”) simulations and were produced with the open-source Parallel Ice Sheet Model . All data sets for this study are publicly available at the NSF Arctic Data Center || ",
            "hits": 34
        },
        {
            "id": 4738,
            "url": "https://svs.gsfc.nasa.gov/4738/",
            "result_type": "Visualization",
            "release_date": "2019-07-24T00:00:00-04:00",
            "title": "Northeast Regional View of Three Simulated Greenland Ice Sheet Response Scenarios: 2008 - 2300",
            "description": "The Greenland Ice Sheet holds enough water to raise the world’s sea level by over 7 meters (23 feet). Rising atmosphere and ocean temperatures have led to an ice loss equivalent to over a centimeter increase in global mean sea-level between 1991 and 2015. Large outlet glaciers, rivers of ice moving to the sea, drain the ice from the interior of Greenland and cause the outer margins of the ice sheet to recede. Improvements in measuring the ice thickness in ice sheets is enabling better simulation of the flow in outlet glaciers, which is key to predicting the retreat of ice sheets into the future.Recently, a simulation of the effects of outlet glacier flow on ice sheet thickness coupled with improved data and comprehensive climate modeling for differing future climate scenarios has been used to estimate Greenland’s contribution to sea-level over the next millennium. Greenland could contribute 5–34 cm (2-13 inches) to sea-level by 2100 and 11–162 cm (4-64 inches) by 2200, with outlet glaciers contributing 19–40 % of the total mass loss. The analysis shows that uncertainties in projecting mass loss are dominated by uncertainties in climate scenarios and surface processes, followed by ice dynamics. Uncertainties in ocean conditions play a minor role, particularly in the long term. Greenland will very likely become ice-free within a millennium without significant reductions in greenhouse gas emissions.Three visualizations of the evolution of the northeastern region of the Greenland Ice Sheet between 2008 and 2300 based on three different climate scenarios are shown below. Each scenario is described briefly in the caption under each visualization. Each of the three visualizations are provided with a date, colorbar and a distance scale as well as without. The regions shown in a violet color are exposed areas of the Greenland bed that were covered by the ice sheet in 2008.The data sets used for these animations are the control (“CTRL”) simulations and were produced with the open-source Parallel Ice Sheet Model . All data sets for this study are publicly available at the NSF Arctic Data Center || ",
            "hits": 15
        },
        {
            "id": 4739,
            "url": "https://svs.gsfc.nasa.gov/4739/",
            "result_type": "Visualization",
            "release_date": "2019-07-24T00:00:00-04:00",
            "title": "Northwest Regional View of Three Simulated Greenland Ice Sheet Response Scenarios: 2008 - 2300",
            "description": "The Greenland Ice Sheet holds enough water to raise the world’s sea level by over 7 meters (23 feet). Rising atmosphere and ocean temperatures have led to an ice loss equivalent to over a centimeter increase in global mean sea-level between 1991 and 2015. Large outlet glaciers, rivers of ice moving to the sea, drain the ice from the interior of Greenland and cause the outer margins of the ice sheet to recede. Improvements in measuring the ice thickness in ice sheets is enabling better simulation of the flow in outlet glaciers, which is key to predicting the retreat of ice sheets into the future.Recently, a simulation of the effects of outlet glacier flow on ice sheet thickness coupled with improved data and comprehensive climate modeling for differing future climate scenarios has been used to estimate Greenland’s contribution to sea-level over the next millennium. Greenland could contribute 5–34 cm (2-13 inches) to sea-level by 2100 and 11–162 cm (4-64 inches) by 2200, with outlet glaciers contributing 19–40 % of the total mass loss. The analysis shows that uncertainties in projecting mass loss are dominated by uncertainties in climate scenarios and surface processes, followed by ice dynamics. Uncertainties in ocean conditions play a minor role, particularly in the long term. Greenland will very likely become ice-free within a millennium without significant reductions in greenhouse gas emissions.Three visualizations of the evolution of the northwest region of the Greenland Ice Sheet between 2008 and 2300 based on three different climate scenarios are shown below. Each scenario is described briefly in the caption under each visualization. Each of the three visualizations are provided with a date, colorbar and a distance scale as well as without. The regions shown in a violet color are exposed areas of the Greenland bed that were covered by the ice sheet in 2008.The data sets used for these animations are the control (“CTRL”) simulations and were produced with the open-source Parallel Ice Sheet Model . All data sets for this study are publicly available at the NSF Arctic Data Center || ",
            "hits": 18
        },
        {
            "id": 4721,
            "url": "https://svs.gsfc.nasa.gov/4721/",
            "result_type": "Visualization",
            "release_date": "2019-06-19T14:00:00-04:00",
            "title": "Three Simulated Greenland Ice Sheet Response Scenarios: 2008 - 2300",
            "description": "The Greenland Ice Sheet holds enough water to raise the world’s sea level by over 7 meters (23 feet). Rising atmosphere and ocean temperatures have led to an ice loss equivalent to over a centimeter increase in global mean sea-level between 1991 and 2015.  Large outlet glaciers, rivers of ice moving to the sea, drain the ice from the interior of Greenland and cause the outer margins of the ice sheet to recede. Improvements in measuring the ice thickness in ice sheets is enabling better simulation of the flow in outlet glaciers, which is key to predicting the retreat of ice sheets into the future.Recently, a simulation of the effects of outlet glacier flow on ice sheet thickness coupled with improved data and comprehensive climate modeling for differing future climate scenarios has been used to estimate Greenland’s contribution to sea-level over the next millennium. Greenland could contribute 5–34 cm (2-13 inches) to sea-level by 2100 and 11–162 cm (4-64 inches) by 2200, with outlet glaciers contributing 19–40 % of the total mass loss. The analysis shows that uncertainties in projecting mass loss are dominated by uncertainties in climate scenarios and surface processes, followed by ice dynamics. Uncertainties in ocean conditions play a minor role, particularly in the long term. Greenland will very likely become ice-free within a millennium without significant reductions in greenhouse gas emissions.Three visualizations of the evolution of the Jakobshavn region of the Greenland Ice Sheet between 2008 and 2300 based on three different climate scenarios are shown below.   The camera zooms in slowly as the ice sheet retreats and pulls out to a view of the entire ice sheet in the year 2300. Each scenario is described briefly in the caption under each visualization. Each of the three visualizations are provided with a date, colorbar and a distance scale as well as without.  The regions shown in a violet color are exposed areas of the Greenland bed that were covered by the ice sheet in 2008.The data sets used for these animations are the control (“CTRL”) simulations and were produced with the open-source Parallel Ice Sheet Model (www.pism-docs.org). All data sets for this study are publicly available at https://arcticdata.io (doi:10.18739/A2Z60C21V). || ",
            "hits": 64
        },
        {
            "id": 4722,
            "url": "https://svs.gsfc.nasa.gov/4722/",
            "result_type": "Visualization",
            "release_date": "2019-06-19T14:00:00-04:00",
            "title": "Jakobshavn Regional View of Three Simulated Greenland Ice Sheet Response Scenarios: 2008 - 2300",
            "description": "The Greenland Ice Sheet holds enough water to raise the world’s sea level by over 7 meters (23 feet). Rising atmosphere and ocean temperatures have led to an ice loss equivalent to over a centimeter increase in global mean sea-level between 1991 and 2015.  Large outlet glaciers, rivers of ice moving to the sea, drain the ice from the interior of Greenland and cause the outer margins of the ice sheet to recede.  Improvements in measuring the ice thickness in ice sheets is enabling better simulation of the flow in outlet glaciers, which is key to predicting the retreat of ice sheets into the future.Recently, a simulation of the effects of outlet glacier flow on ice sheet thickness coupled with improved data and comprehensive climate modeling for differing future climate scenarios has been used to estimate Greenland’s contribution to sea-level over the next millennium. Greenland could contribute 5–34 cm (2-13 inches) to sea-level by 2100 and 11–162 cm (4-64 inches) by 2200, with outlet glaciers contributing 19–40 % of the total mass loss. The analysis shows that uncertainties in projecting mass loss are dominated by uncertainties in climate scenarios and surface processes, followed by ice dynamics.  Uncertainties in ocean conditions play a minor role, particularly in the long term. Greenland will very likely become ice-free within a millennium without significant reductions in greenhouse gas emissions.Three visualizations of the evolution of the Jakobshavn region of the Greenland Ice Sheet between 2008 and 2300 based on three different climate scenarios are shown below. Each scenario is described briefly in the caption under each visualization.  Each of the three visualizations are provided with a date, colorbar and a distance scale as well as without. The regions shown in a violet color are exposed areas of the Greenland bed that were covered by the ice sheet in 2008.The data sets used for these animations are the control (“CTRL”) simulations and were produced with the open-source Parallel Ice Sheet Model (www.pism-docs.org). All data sets for this study are publicly available at https://arcticdata.io (doi:10.18739/A2Z60C21V). || ",
            "hits": 31
        },
        {
            "id": 4727,
            "url": "https://svs.gsfc.nasa.gov/4727/",
            "result_type": "Visualization",
            "release_date": "2019-06-19T14:00:00-04:00",
            "title": "Greenland View of Three Simulated Greenland Ice Sheet Response Scenarios: 2008 - 2300",
            "description": "The Greenland Ice Sheet holds enough water to raise the world’s sea level by over 7 meters (23 feet). Rising atmosphere and ocean temperatures have led to an ice loss equivalent to over a centimeter increase in global mean sea-level between 1991 and 2015. Large outlet glaciers, rivers of ice moving to the sea, drain the ice from the interior of Greenland and cause the outer margins of the ice sheet to recede. Improvements in measuring the ice thickness in ice sheets is enabling better simulation of the flow in outlet glaciers, which is key to predicting the retreat of ice sheets into the future.Recently, a simulation of the effects of outlet glacier flow on ice sheet thickness coupled with improved data and comprehensive climate modeling for differing future climate scenarios has been used to estimate Greenland’s contribution to sea-level over the next millennium. Greenland could contribute 5–34 cm (2-13 inches) to sea-level by 2100 and 11–162 cm (4-64 inches) by 2200, with outlet glaciers contributing 19–40 % of the total mass loss. The analysis shows that uncertainties in projecting mass loss are dominated by uncertainties in climate scenarios and surface processes, followed by ice dynamics. Uncertainties in ocean conditions play a minor role, particularly in the long term. Greenland will very likely become ice-free within a millennium without significant reductions in greenhouse gas emissions.Three visualizations of the evolution of the Greenland Ice Sheet between 2008 and 2300 based on three different climate scenarios are shown below. Each scenario is described briefly in the caption under each visualization. Each of the three visualizations are provided with a date and colorbar as well as without.  The regions shown in a violet color are exposed areas of the Greenland bed that were covered by the ice sheet in 2008.The data sets used for these animations are the control (“CTRL”) simulations and were produced with the open-source Parallel Ice Sheet Model (www.pism-docs.org). All data sets for this study are publicly available at https://arcticdata.io (doi:10.18739/A2Z60C21V). || ",
            "hits": 106
        },
        {
            "id": 13233,
            "url": "https://svs.gsfc.nasa.gov/13233/",
            "result_type": "Produced Video",
            "release_date": "2019-06-19T14:00:00-04:00",
            "title": "Modeling the Future of the Greenland Ice Sheet",
            "description": "Music: Tides by Jon Cotton [PRS], Ben Niblett [PRS]Complete transcript available. || Greenland_Still_Two.jpg (1920x1080) [941.0 KB] || Greenland_Still_Two_searchweb.png (320x180) [152.3 KB] || Greenland_Still_Two_thm.png (80x40) [8.8 KB] || 13233_Greenland_Outlet_FINAL.mp4 (1920x1080) [253.2 MB] || 13233_Greenland_Outlet_FINAL.mov (1920x1080) [3.4 GB] || 13233_Greenland_Outlet_FINAL.webm (1920x1080) [17.2 MB] || 13233_Greenland_Outlet_FINAL_VX-303985.webm (960x540) [54.0 MB] || GreenlandOutletModel_Fine_V2.en_US.srt [2.9 KB] || GreenlandOutletModel_Fine_V2.en_US.vtt [2.9 KB] || ",
            "hits": 99
        },
        {
            "id": 11976,
            "url": "https://svs.gsfc.nasa.gov/11976/",
            "result_type": "Produced Video",
            "release_date": "2015-08-26T17:00:00-04:00",
            "title": "Sea Level Rise Live Shots",
            "description": "Sea Level Rising Inteview with Tom Wagner || YOUTUBE_HQ_Tom_Wagner_-_Sea_Levels_youtube_hq_print.jpg (1024x576) [128.8 KB] || WEBM_Tom_Wagner_-_Sea_Levels_1.webm (960x540) [82.0 MB] || WMV_Tom_Wagner_-_Sea_Levels_1_HD.wmv (1280x720) [39.7 MB] || APPLE_TV_Tom_Wagner_-_Sea_Levels_1_appletv.m4v (1280x720) [112.3 MB] || APPLE_TV_Tom_Wagner_-_Sea_Levels_1_appletv_subtitles.m4v (1280x720) [112.4 MB] || YOUTUBE_HQ_Tom_Wagner_-_Sea_Levels_1_youtube_hq.mov (1280x720) [369.3 MB] || NASA_TV_Tom_Wagner_-_Sea_Levels_1.mpeg (1280x720) [687.0 MB] || WEBM_Tom_Wagner_-_Sea_Levels.en_US.vtt [4.5 KB] || WEBM_Tom_Wagner_-_Sea_Levels_1.en_US.srt [4.6 KB] || WEBM_Tom_Wagner_-_Sea_Levels_1.en_US.vtt [4.5 KB] || NASA_PODCAST_Tom_Wagner_-_Sea_Levels_1_ipod_sm.mp4 (320x240) [36.7 MB] || Tom_Wagner_-_Sea_Levels_1.mov (1280x720) [2.6 GB] || ",
            "hits": 38
        },
        {
            "id": 4306,
            "url": "https://svs.gsfc.nasa.gov/4306/",
            "result_type": "Visualization",
            "release_date": "2015-06-25T00:00:00-04:00",
            "title": "FROZEN: The Full Story",
            "description": "On March 27, 2009, NASA released FROZEN, a twelve-minute show about the Earth's frozen regions designed for Science On a Sphere.  Science On a Sphere was created by NOAA and displays movies on a spherical screen, which is ideal for a show about the Earth or the planets.  The audience can view the show from any side of the sphere and can see any part of the Earth.  Making a movie for this system is challenging, and FROZEN was an exciting project to create.  Until now, only the \"trailer\" for FROZEN has been available for viewing from our site.  Here, for the first time, is an on-line version of the complete show, presented in several different formats that show different aspects of the movie. || ",
            "hits": 63
        },
        {
            "id": 11380,
            "url": "https://svs.gsfc.nasa.gov/11380/",
            "result_type": "Produced Video",
            "release_date": "2013-10-21T12:00:00-04:00",
            "title": "Ask A Climate Scientist – a Pause in Warming?",
            "description": "Is there a pause in global warming? This question was posed to Jet Propulsion Laboratory scientist Josh Willis as part of NASA's Ask A Climate Scientist campaign.Josh gets asked a lot if there has been a pause in global warming, because temperatures aren't increasing as fast as they were a decade ago. No, he says, global warming is definitely still increasing. We see more heat being trapped in the oceans, and sea levels are rising. Look at the sea level record for the last decade. It's going up like gangbusters, hasn't slowed down. There's not really a pause in global warming. Sometimes there's natural fluctuations and we warm up a little faster in one decade and a little slower in another decade, but global warming, human-caused climate change? Josh says, \"that's definitely going right on up in there. We haven't slowed down at all.\" See more of NASA's answers to your questions on climate science. || ",
            "hits": 25
        },
        {
            "id": 10753,
            "url": "https://svs.gsfc.nasa.gov/10753/",
            "result_type": "Produced Video",
            "release_date": "2011-05-13T12:00:00-04:00",
            "title": "Zoom in to Smith Island, MD",
            "description": "As sea levels rise, islands in the Chesapeake Bay are disappearing under water. || ",
            "hits": 81
        },
        {
            "id": 10596,
            "url": "https://svs.gsfc.nasa.gov/10596/",
            "result_type": "Produced Video",
            "release_date": "2010-04-02T00:00:00-04:00",
            "title": "IceBridge 2010, a liveshot with Lora Koenig",
            "description": "Live interview with NASA Goddard cryospheric scientist Lora Koenig regarding Operation IceBridge and the 2010 Arctic sea ice maximum. || Koenig_OIB_LS_2010_SVS.00327_print.jpg (1024x576) [67.0 KB] || Koenig_OIB_LS_2010_SVS_web.png (320x180) [207.5 KB] || Koenig_OIB_LS_2010_SVS_thm.png (80x40) [16.1 KB] || Koenig_OIB_LS_2010.webmhd.webm (960x540) [56.4 MB] || Koenig_OIB_LS_2010.m4v (960x720) [138.4 MB] || Koenig_OIB_LS_2010.mov (1280x720) [4.1 GB] || Koenig_OIB_LS_2010_youtube_HQ.mov (1280x720) [115.0 MB] || Koenig_OIB_LS_2010_youtube.mov (1280x720) [53.3 MB] || Koenig_OIB_LS_2010_Goddard_Shorts.m4v (640x360) [42.0 MB] || Koenig_OIB_LS_2010_nasa_podcast.m4v (320x180) [17.6 MB] || Koenig_OIB_LS_2010_NASA_PORTAL.wmv (346x260) [36.3 MB] || Koenig_OIB_LS_2010_SVS.mpg (512x288) [36.0 MB] || ",
            "hits": 12
        },
        {
            "id": 3656,
            "url": "https://svs.gsfc.nasa.gov/3656/",
            "result_type": "Visualization",
            "release_date": "2009-10-17T00:00:00-04:00",
            "title": "Sea Level Rise \"What Ifs\" in the Southeastern United States",
            "description": "This visualization shows the Southeastern United States with population data over the land. Darker areas over land indicate higher population densities. Sea level scenarios are shown starting with 0 meters of sea level rise (current sea level) and proceeding through 9 meters of rise. Blue areas moving inland indicate where the coastline would be at various levels.We will likely see some sea level rise in our lifetimes, but the middle-to-higher levels in this visualization are unlikely in the next 100 years.This visualization is based on Shuttle Radar Topography Mission (SRTM) data. This data primarily measured canopy heights. So, this visualization is showing where water might reach the tops of the trees in various areas. || ",
            "hits": 21
        },
        {
            "id": 10503,
            "url": "https://svs.gsfc.nasa.gov/10503/",
            "result_type": "Produced Video",
            "release_date": "2009-10-12T00:00:00-04:00",
            "title": "Melting Ice, Rising Seas",
            "description": "Sea level rise is an indicator that our planet is warming. Much of the world's population lives on or near the coast, and rising seas are something worth watching. Sea level can rise for two reasons, both linked to a warming planet. When ice on land, such as mountain glaciers or the ice sheets of Greenland or Antarctica, melt, that water contributes to sea level rise. And when our oceans get warmer - another indicator of climate change - the water expands, also making sea level higher. Using satellites, lasers, and radar in space, and dedicated researchers on the ground, NASA is studying the Earth's ice and water to better understand how sea level rise might affect us all.For complete transcript, click here. || Melting_Seas_ipod_640x480.03027_print.jpg (1024x576) [80.7 KB] || Melting_Seas_ipod_640x480_web.png (320x180) [156.6 KB] || Melting_Seas_ipod_640x480_thm.png (80x40) [16.6 KB] || Melting_Seas_appletv_1280x720.webmhd.webm (960x540) [67.9 MB] || Melting_Seas_H264_1280x720_30fps.mov (1280x720) [128.9 MB] || Melting_Seas_1280x720.mp4 (1280x720) [125.1 MB] || Melting_Seas_broll_prores.mov (1280x720) [4.4 GB] || Melting_Seas_youtube_1280x720.mov (1280x720) [69.1 MB] || Melting_Seas_appletv_1280x720.m4v (960x540) [160.0 MB] || Melting_Seas_ipod_640x480.m4v (640x360) [49.7 MB] || Melting_Seas_ipod_320x240.m4v (320x180) [21.1 MB] || Rising_Seas.wmv (346x260) [38.5 MB] || ",
            "hits": 115
        },
        {
            "id": 10403,
            "url": "https://svs.gsfc.nasa.gov/10403/",
            "result_type": "Produced Video",
            "release_date": "2009-03-12T12:00:00-04:00",
            "title": "FROZEN: A Spherical Movie About the Cryosphere",
            "description": "NASA's home for spherical films on Magic Planet.  Download the Magic Planet-ready movie file here.Released on March 27, 2009, FROZEN is NASA's second major production for the Science On a Sphere platform, a novel cinema-in-the-round technology developed by the Space Agency's sibling NOAA. Viewers see the Earth suspended in darkness as if it were floating in space. Moving across the planet's face, viewers see the undulating wisps of clouds, the ephemeral sweep of fallen snow, the churning crash of shifting ice, and more.FROZEN brings the Earth alive. Turning in space, the sphere becomes a portal onto a virtual planet, complete with churning, swirling depictions of huge natural forces moving below. FROZEN features the global cryosphere, those places on Earth where the temperature doesn't generally rise above water's freezing point. As one of the most directly observable climate gauges, the changing cryosphere serves as a proxy for larger themes.But just as thrilling as this unusual—and unusually realistic—look at the planet's structure and behavior is the sheer fun and fascination of looking at a spherically shaped movie. FROZEN bends the rules of cinema, revealing new ways to tell exciting, valuable stories of all kinds. The movie may be FROZEN, but the experience itself rockets along. || ",
            "hits": 85
        },
        {
            "id": 3487,
            "url": "https://svs.gsfc.nasa.gov/3487/",
            "result_type": "Visualization",
            "release_date": "2008-06-01T00:00:00-04:00",
            "title": "Draining the Oceans",
            "description": "Three fifths of the Earth's surface is under the ocean, and the ocean floor is as rich in detail as the land surface with which we are familiar. This animation simulates a drop in sea level that gradually reveals this detail. As the sea level drops, the continental shelves appear immediately. They are mostly visible by a depth of 140 meters, except for the Arctic and Antarctic regions, where the shelves are deeper. The mid-ocean ridges start to appear at a depth of 2000 to 3000 meters. By 6000 meters, most of the ocean is drained except for the deep ocean trenches, the deepest of which is the Marianas Trench at a depth of 10,911 meters. || ",
            "hits": 2197
        }
    ]
}