{ "count": 17, "next": null, "previous": null, "results": [ { "id": 5060, "url": "https://svs.gsfc.nasa.gov/5060/", "result_type": "Visualization", "release_date": "2023-01-12T10:00:00-05:00", "title": "Global Temperature Anomalies from 1880 to 2022", "description": "This color-coded map in Robinson projection displays a progression of changing global surface temperature anomalies. Normal temperatures are shown in white. Higher than normal temperatures are shown in red and lower than normal temperatures are shown in blue. Normal temperatures are calculated over the 30 year baseline period 1951-1980. The final frame represents the 5 year global temperature anomalies from 2018-2022. || GISTEMP-2022-TemperatureAnomalyBothCelsiusFahrenheit.00899_print.jpg (1024x576) [145.3 KB] || GISTEMP-2022-TemperatureAnomalyBothCelsiusFahrenheit.00899_searchweb.png (180x320) [74.8 KB] || GISTEMP-2022-TemperatureAnomalyBothCelsiusFahrenheit.00899_thm.png (80x40) [6.3 KB] || GISTEMP-2022-TemperatureAnomalyBothCelsiusFahrenheit.mp4 (1920x1080) [57.8 MB] || celsius (1920x1080) [0 Item(s)] || celsius (3840x2160) [0 Item(s)] || ", "hits": 174 }, { "id": 5047, "url": "https://svs.gsfc.nasa.gov/5047/", "result_type": "Visualization", "release_date": "2022-11-30T00:00:00-05:00", "title": "Net Ecosystem Exchange of Carbon Dioxide", "description": "The NASA Carbon Monotoring System's estimate of the Net Ecosystem Exchange of Carbon Dioxide from 2000 to 2018. || co2_nee_5.01750_print.jpg (1024x576) [124.3 KB] || co2_nee_5.01750_searchweb.png (320x180) [43.8 KB] || co2_nee_5.01750_thm.png (80x40) [4.5 KB] || 3840x2160_16x9_30p (3840x2160) [64.0 KB] || co2_nee_5.webm (3840x2160) [14.2 MB] || co2_nee_5.mp4 (3840x2160) [256.2 MB] || ", "hits": 352 }, { "id": 14177, "url": "https://svs.gsfc.nasa.gov/14177/", "result_type": "Produced Video", "release_date": "2022-07-19T11:00:00-04:00", "title": "How Climate Patterns Thousands of Miles Away Affect US Bird Migration", "description": "Stock footage: Pond5Radar video courtesy of Dr. Kyle Horton, Colorado State UniversityUniversal Production Music: “Two Ticks” by Michael Lesirge [PRS] and Tarek Christopher Modi [PRS]This video can be freely shared and downloaded. While the video in its entirety can be shared without permission, some individual imagery provided by pond5.com and CSU is obtained through permission and may not be excised or remixed in other products. For more information on NASA’s media guidelines, visit https://www.nasa.gov/multimedia/guidelines/index.htmlComplete transcript available. || 14177_BirdMigration_Thumb.jpg (1920x1080) [268.4 KB] || 14177_BirdMigration_Thumb_print.jpg (1024x576) [130.4 KB] || 14177_BirdMigration_Thumb_searchweb.png (320x180) [64.3 KB] || 14177_BirdMigration_Thumb_web.png (320x180) [64.3 KB] || 14177_BirdMigration_Thumb_thm.png (80x40) [6.5 KB] || BirdMigration.mov (1920x1080) [4.0 GB] || BirdMigration.webm (960x540) [50.2 MB] || BirdMigration.mp4 (1920x1080) [380.5 MB] || TWITTER_720_BirdMigration.mp4 (1280x720) [35.5 MB] || YOUTUBE_1080_BirdMigration.mp4 (1920x1080) [289.5 MB] || 14177_BirdMigration_EN.US.en_US.srt [3.9 KB] || 14177_BirdMigration_EN.US.en_US.vtt [3.7 KB] || ", "hits": 39 }, { "id": 4464, "url": "https://svs.gsfc.nasa.gov/4464/", "result_type": "Visualization", "release_date": "2018-12-14T00:00:00-05:00", "title": "Using Tree Rings to Study Human Influence on Hydroclimate", "description": "This visualization displays a global drought atlas dating back to 1400, created using data from tree rings. The data is displayed on a flat rectangular map projection with a simple overlay depicting the differences in tree ring sizes for dry and wet years. In the second half of the visualization, a ‘fingerprint’ thumbnail is introduced, which is an indicator for human influences on climate change. A signal-to-noise ratio graph is depicted comparing the fingerprint to both tree ring drought atlas data and observational meteorological data (CRU and Dai) || hydroclimate_comp5_4k_1210_print.jpg (1024x576) [62.1 KB] || hydroclimate_comp5_4k_1210_searchweb.png (320x180) [41.3 KB] || hydroclimate_comp5_4k_1210_thm.png (80x40) [4.9 KB] || hydroclimate_comp5_1080p30.mp4 (1920x1080) [9.4 MB] || TreeRing_hydroclimate_comp (3840x2160) [0 Item(s)] || hydroclimate_comp5_4k_2160p30.mp4 (3840x2160) [25.6 MB] || hydroclimate_comp5_4k_2160p30.webm (3840x2160) [7.6 MB] || hydroclimate_comp5_1080p30.mp4.hwshow [192 bytes] || ", "hits": 46 }, { "id": 4603, "url": "https://svs.gsfc.nasa.gov/4603/", "result_type": "Visualization", "release_date": "2018-05-22T15:00:00-04:00", "title": "Cholera Risk Maps", "description": "Cholera Risk, Pre-Hurricane || cholera_risk_pre.1000_print.jpg (1024x576) [92.1 KB] || cholera_risk_pre.1000_searchweb.png (320x180) [65.9 KB] || cholera_risk_pre.1000_thm.png (80x40) [5.9 KB] || cholera_risk_pre (1920x1080) [0 Item(s)] || cholera_risk_pre_1080p30.mp4 (1920x1080) [18.1 MB] || cholera_risk_pre_1080p30.webm (1920x1080) [6.9 MB] || cholera_risk_pre_1080p30.mp4.hwshow [190 bytes] || ", "hits": 27 }, { "id": 12958, "url": "https://svs.gsfc.nasa.gov/12958/", "result_type": "Produced Video", "release_date": "2018-05-18T14:00:00-04:00", "title": "Using Precipitation Data to Assess Risk of Cholera Outbreaks", "description": "Music: \"A New Hope,\" Al Lethbridge, Atmosphere Music Ltd PRS; \"Spirals within a Sphere,\" Adam Salkeld, Atmosphere Music Ltd PRSComplete transcript available. || cholera_still_print.jpg (1024x695) [243.6 KB] || cholera_still_searchweb.png (320x180) [119.4 KB] || cholera_still_thm.png (80x40) [7.6 KB] || 12958_Cholera_GPM_prores.mov (1920x1080) [3.1 GB] || 12958_Cholera_GPM_twitter_720.mp4 (1280x720) [54.2 MB] || 12958_Cholera_GPM_youtube_720.mp4 (1280x720) [430.0 MB] || 12958_Cholera_GPM_facebook_720.mp4 (1280x720) [337.4 MB] || 12958_Cholera_GPM_youtube_1080.mp4 (1920x1080) [490.1 MB] || 12958_Cholera_GPM_prores.webm (1920x1080) [23.6 MB] || 12958_Cholera_GPM_large.mp4 (1920x1080) [235.1 MB] || 12958_Cholera.en_US.srt [4.2 KB] || 12958_Cholera.en_US.vtt [4.2 KB] || ", "hits": 34 }, { "id": 4601, "url": "https://svs.gsfc.nasa.gov/4601/", "result_type": "Visualization", "release_date": "2017-12-18T11:00:00-05:00", "title": "Jupiter Quasi-Quadrennial Oscillation", "description": "Climate patterns on Jupiter can have striking similarities to those on Earth, making the gas giant a natural laboratory for understanding planetary atmospheres. Complete transcript available.Watch this video on the NASA Goddard YouTube channel.Music provided by Killer Tracks: \"Lights,\" \"Times Waits,\" \"The Space Between\" || JupiterQQOpreview.jpg (1920x1080) [456.5 KB] || TWITTER_720_4601_Jupiter_QQO_Master_APR_twitter_720.mp4 (1280x720) [37.7 MB] || 4601_Jupiter_QQO_Master.webm (960x540) [72.7 MB] || FACEBOOK_720_4601_Jupiter_QQO_Master_APR_facebook_720.mp4 (1280x720) [218.0 MB] || YOUTUBE_HQ_4601_Jupiter_QQO_Master_APR_youtube_hq.mov (1920x1080) [875.9 MB] || 4601_Jupiter_QQO_Master_APR_Output.en_US.srt [3.8 KB] || 4601_Jupiter_QQO_Master_APR_Output.en_US.vtt [3.8 KB] || 4601_Jupiter_QQO_Master_APR.mov (1920x1080) [2.4 GB] || ", "hits": 63 }, { "id": 30754, "url": "https://svs.gsfc.nasa.gov/30754/", "result_type": "Hyperwall Visual", "release_date": "2016-03-17T00:00:00-04:00", "title": "Ocean Color Time Series", "description": "Ocean Color, July 2002 - March 2017 || ocean_color_mollweide_1080p.00001_print.jpg (1024x576) [147.0 KB] || ocean_color_mollweide_1080p.mp4 (1920x1080) [52.3 MB] || ocean_color_mollweide_720p.mp4 (1280x720) [26.0 MB] || ocean_color_mollweide_1080p.webm (1920x1080) [4.1 MB] || mollweide (4104x2304) [0 Item(s)] || ocean_color_mollweide_2304p.mp4 (4096x2304) [172.6 MB] || ", "hits": 49 }, { "id": 30367, "url": "https://svs.gsfc.nasa.gov/30367/", "result_type": "Hyperwall Visual", "release_date": "2013-10-24T12:00:00-04:00", "title": "Monthly Solar Insolation", "description": "These maps show Earth's average monthly solar insolation, or the rate of incoming sunlight reaching the surface, from July 2006 to the present as derived from Clouds and Earth’s Radiant Energy System (CERES) measurements of radiant energy escaping the top of Earth's atmosphere. The CERES instrument flies onboard NASA’s Terra and Aqua satellites and makes these measurements every day on a global scale. The colors represent the kilowatt-hours of sunlight falling on every square meter of the surface per day, averaged over one month. Energy from the sun warms the surface, creating updrafts of air that carry warmth and moisture up into the atmosphere. Thus, knowing the rate of sunlight reaching the surface helps scientists understand weather and climate patterns. Exposure to sunlight is also a key limit to plant growth, particularly in tropical rainforests. Thus, insolation maps are also useful to scientists studying plant growth patterns in different parts of the world. || ", "hits": 245 }, { "id": 30373, "url": "https://svs.gsfc.nasa.gov/30373/", "result_type": "Hyperwall Visual", "release_date": "2013-10-24T12:00:00-04:00", "title": "Monthly Daytime Land-Surface Temperature", "description": "Scientists monitor land-surface temperature because the warmth rising off Earth's landscapes influences our world's weather and climate patterns. Likewise, land surface temperature is also influenced by changes in weather and climate patterns. These maps show monthly daytime land-surface temperatures from February 2000 to the present using thermal infrared measurements made by the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument aboard NASA's Terra satellite. The measurements shown here represent the temperature of the \"skin\" (or top 1 millimeter) of the land surface during the daytime—including bare land, snow or ice cover, and cropland or forest canopy—and should not be confused with surface air temperature measurements that are given in a typical weather reports. Yellow shows the warmest temperatures (up to 45 degrees Celsius) and light blue shows the coldest temperatures (down to -25 degrees Celsius). Black means no data. || ", "hits": 74 }, { "id": 30374, "url": "https://svs.gsfc.nasa.gov/30374/", "result_type": "Hyperwall Visual", "release_date": "2013-10-24T12:00:00-04:00", "title": "Monthly Nighttime Land Surface Temperature", "description": "Scientists monitor land-surface temperature because the warmth rising off Earth's landscapes influences our world's weather and climate patterns. Likewise, land surface temperature is also influenced by changes in weather and climate patterns. These maps show monthly nighttime land-surface temperatures from February 2000 to the present using thermal infrared measurements made by the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument onboard NASA's Terra satellite. The measurements shown here represent the temperature of the \"skin\" (or top 1 millimeter) of the land surface during the nighttime—including bare land, snow or ice cover, and cropland or forest canopy—and should not be confused with surface air temperature measurements that are given in a typical weather reports. Yellow shows the warmest temperatures (up to 45 degrees Celsius) and light blue shows the coldest temperatures (down to -25 degrees Celsius). Black means no data. || ", "hits": 47 }, { "id": 11376, "url": "https://svs.gsfc.nasa.gov/11376/", "result_type": "Produced Video", "release_date": "2013-09-27T08:00:00-04:00", "title": "IPCC Projections of Temperature and Precipitation in the 21st Century", "description": "New data visualizations from the NASA Center for Climate Simulation and NASA's Scientific Visualization Studio show how climate models – those used in the new report from the United Nations' Intergovernmental Panel on Climate Change (IPCC) – estimate how temperature and precipitation patterns could change throughout the 21st century. For the IPCC's Physical Science Basis and Summary for Policymakers reports, scientists referenced an international climate modeling effort to study how the Earth might respond to four different scenarios of how much carbon dioxide and other greenhouse gases would be emitted into the atmosphere throughout the 21st century. The Summary for Policymakers, the first official piece of the group's Fifth Assessment Report, was released Fri., Sept. 27.That modeling effort, called the Coupled Model Intercomparison Project Phase 5 (CMIP5), includes dozens of climate models from institutions around the world, including from NASA's Goddard Institute for Space Studies.To produce visualizations that show temperature and precipitation changes similar to those included in the IPCC report, the NASA Center for Climate Simulation calculated mean model results for each of the four emissions scenarios. The final products are visual representations how much temperature and precipitation patterns would change through 2100 compared to the historical average from the end of the 20th century. The changes shown compare the model projections to the average temperature and precipitation benchmarks observed from 1971-2000. This baseline is different from the IPCC report, which uses a 1986-2005 baseline. Because the reference period from 1986-2005 was slightly warmer than 1971-2000, the visualizations are slightly different than those in the report, even though the same model data is used. || ", "hits": 124 }, { "id": 4073, "url": "https://svs.gsfc.nasa.gov/4073/", "result_type": "Visualization", "release_date": "2013-05-09T12:00:00-04:00", "title": "Greenhouse Warming Linked to Shifts in Rainfall", "description": "Global warming may increase the risk for extreme rainfall and drought according to a NASA-led modeling study. The study shows for the first time how rising carbon dioxide concentrations could affect the entire range of rainfall types on Earth. Analysis of information from 14 climate models indicates wet regions of the world, such as the equatorial Pacific Ocean and the Asian monsoon regions, will likely see increases in heavy precipitation because of warming resulting from projected increases in carbon dioxide levels. Arid land areas outside the tropics and many regions with moderate rainfall could become drier. The models project for every 1 degree Fahrenheit of carbon dioxide-induced warming, heavy rainfall will increase globally by 3.9 percent and light rain will increase globally by 1 percent. However, total global rainfall is not projected to change much because moderate rainfall will decrease globally by 1.4 percent.This visualization shows an average rainfall month for June,July, and August. The movie will display areas with no rain (brown), moderate rain (tan), and heavy rain (blue). Very Heavy rainfall (dark blue) is defined as months that receive an average of 0.95 of an inch of rain per day (24 mm/day) every day for the months of June, July, and August. Heavy rainfall is defined as months that receive an average of more than about 0.35 of an inch per day (9 mm/day). Light rain is defined as months that receive an average of less than 0.01 of an inch per day. Moderate rainfall is defined as months that receive an average of between about 0.04 to 0.09 of an inch per day. || ", "hits": 274 }, { "id": 10742, "url": "https://svs.gsfc.nasa.gov/10742/", "result_type": "Produced Video", "release_date": "2011-08-25T12:00:00-04:00", "title": "NPP Resource Reel", "description": "The NPOESS Preparatory Project (NPP) represents a critical first step in building the next-generation weather satellite system. Goddard Space Flight Center is leading NASA's effort to launch a satellite that will carry the first of the new sensors developed for this next-generation system, previously called the National Polar-orbiting Operational Environmental Satellite System (NPOESS) and now the Joint Polar Satellite System (JPSS). || ", "hits": 39 }, { "id": 10392, "url": "https://svs.gsfc.nasa.gov/10392/", "result_type": "Produced Video", "release_date": "2009-02-19T00:00:00-05:00", "title": "Volcanic Ash Still Image", "description": "Aerosols are complex particles; they can occur in nature but can also be generated by humans. One source of naturally-occurring aerosols is volcanoes. Large-scale volcanic activity may last only a few days, but the massive outpouring of gases and ash can influence climate patterns for years. Sulfuric gases convert to sulfate aerosols, sub-micron droplets containing about 75 percent sulfuric acid. Following eruptions, these aerosol particles can linger as long as three to four years in the stratosphere. Still image courtesy of United States Geological Survey. || ", "hits": 59 }, { "id": 20114, "url": "https://svs.gsfc.nasa.gov/20114/", "result_type": "Animation", "release_date": "2007-09-07T00:00:00-04:00", "title": "Greenhouse Gases Effect on Global Warming", "description": "The 'greenhouse effect' is the warming of climate that results when the atmosphere traps heat radiating from Earth toward space. Certain gases in the atmosphere resemble glass in a greenhouse, allowing sunlight to pass into the 'greenhouse,' but blocking Earth's heat from escaping into space. The gases that contribute to the greenhouse effect include water vapor, carbon dioxide (CO2), methane, nitrous oxides, and chlorofluorocarbons (CFCs).On Earth, human activities are changing the natural greenhouse. Over the last century the burning of fossil fuels like coal and oil has increased the concentration of atmospheric CO2. This happens because the coal or oil burning process combines carbon (C) with oxygen (O2) in the air to make CO2. To a lesser extent, the clearing of land for agriculture, industry, and other human activities have increased the concentrations of other greenhouse gases like methane (CH4), and further increased (CO2).The consequences of changing the natural atmospheric greenhouse are difficult to predict, but certain effects seem likely: - On average, Earth will become warmer. Some regions may welcome warmer temperatures, but others may not. - Warmer conditions will probably lead to more evaporation and precipitation overall, but individual regions will vary, some becoming wetter and others dryer. - A stronger greenhouse effect will probably warm the oceans and partially melt glaciers and other ice, increasing sea level. Ocean water also will expand if it warms, contributing to further sea level rise. - Meanwhile, some crops and other plants may respond favorably to increased atmospheric CO2, growing more vigorously and using water more efficiently. At the same time, higher temperatures and shifting climate patterns may change the areas where crops grow best and affect the makeup of natural plant communities. || ", "hits": 1473 }, { "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": 43 } ] }