In early 2006, a weak La Niña event kept the temperatures in the Pacific Ocean along the equator a little cooler than normal.
Pacific Climate Calm
Project scientist Mark Clampin is reflected in the flight mirrors of the Webb Space Telescope at Marshall Space Flight Center.  Portions of the Webb telescope are being built at NASA Goddard.    Credit: Ball Aerospace/NASA  <b><a href="http://www.nasa.gov/centers/goddard/home/index.html" rel="nofollow">NASA Goddard Space Flight Center</a></b> enables NASA’s mission through four scientific endeavors: Earth Science, Heliophysics, Solar System Exploration, and Astrophysics. Goddard plays a leading role in NASA’s accomplishments by contributing compelling scientific knowledge to advance the Agency’s mission.  <b>Follow us on <a href="http://twitter.com/NASA_GoddardPix" rel="nofollow">Twitter</a></b>  <b>Join us on <a href="http://www.facebook.com/pages/Greenbelt-MD/NASA-Goddard/395013845897?ref=tsd" rel="nofollow">Facebook</a></b>  <b>Find us on <a href="http://instagr.am/p/E_05l/" rel="nofollow">Instagram</a></b>
JWST Flight Mirrors
This region of Xanthe Terra has mostly been contracted due to thrust faulting, but this local region shows evidence of extensional faulting, also called normal faulting.  When two normal faults face each other, they create a bathtub-like depression called a "graben."  http://photojournal.jpl.nasa.gov/catalog/PIA20813
Faulting Mars
This ultraviolet image from NASA Galaxy Evolution Explorer is of NGC 5128 Centaurus-A. This unusual galaxy is believed to be the result of a collision of two normal galaxies.
NGC 5128 Centaurus-A
This image shows differences in atmospheric water vapor relative to a normal average year in the Earth upper troposphere about 10 kilometers 6 miles above the surface.
TOPEX/El Niño Watch - El Niño Moisture in the Atmosphere, February 22, 1998
Tethys may not be tiny by normal standards, but when it is captured alongside Saturn, it cant help but seem pretty small in this image from NASA Cassini spacecraft.
Tiny Tethys
This image shows differences in atmospheric water vapor relative to a normal average year in the Earth upper troposphere about 10 kilometers 6 miles above the surface.
Microwave Limb Sounder/El Niño Watch - December, 1997
New data from NASA Jason-2 satellite show near-normal sea surface heights in the equatorial Pacific Ocean persisting for a 16th straight month.
La Nada Climate Pattern Lingers in the Pacific
A giant horseshoe pattern of higher than normal sea-surface heights developing over the last year is beginning to dominate the entire western Pacific and Asiatic oceans.
TOPEX/El Niño Watch - La Niña Persistence May be Part of Larger Climate Pattern, January 8, 2000
Sulfur dioxide, normally a gas at room temperatures, is known to exist on Io surface as a frost, condensing there from the hot gases emanating from the Io volcanoes. This image was taken in 1996 by NASA Galileo spacecraft.
Distribution of Sulfur Dioxide Frost on Io
Using NASA Herschel Space Observatory, astronomers have discovered that comet Hartley 2 possesses a ratio of heavy water to light, or normal, water that matches what found in Earth oceans.
Heavy and Light Just Right
This image of the Pacific Ocean was produced using sea surface height measurements taken by the U.S./French TOPEX/Poseidon satellite. The image shows sea surface height relative to normal ocean conditions on Nov. 10, 1997.
TOPEX/El Niño Watch - Warm Water Pool is Increasing, Nov. 10, 1997
Height measurements taken by NASA U.S.-French TOPEX/Poseidon satellite. The image shows sea surface height relative to normal ocean conditions on July 11, 1998; sea surface height is an indicator of the heat content of the ocean.
TOPEX/El Niño Watch - Satellite shows Pacific Stabilizing, July 11, 1998
This image of the Pacific Ocean was produced using sea surface height measurements taken by NASA U.S./French TOPEX/Poseidon satellite. The image shows sea surface height relative to normal ocean conditions on Dec. 1, 1997.
TOPEX/El Niño Watch - Double
Our planet emits energy as thermal infrared radiation at wavelengths we cannot normally see but can feel -- for example, if we stand close to a hot surface. This map is from NASA ASTER GED.
NASA Spacecraft Maps Earth Global Emissivity
This image taken by NASA Mars Reconnaissance Orbiter shows part of Cerberus Fossae, a long system of extensional normal faults arranged in trough-bounding graben-bounding pairs.
Cerberus Fossae East of the Head of Athabasca Valles
The cold pool of water in the Pacific known as La Nina is beginning to fade, but ocean conditions have not returned to normal, according to scientists studying images from the U.S.-French TOPEX/Poseidon satellite.  http://photojournal.jpl.nasa.gov/catalog/PIA00031
TOPEX El Niño/La Niña -La Niña Begins to Fade, April 7, 1999
A special maneuver of NASA Terra spacecraft was performed as it traversed the nightside enabling a backward somersault of the spacecraft, allowing the normally Earth-viewing instruments to look at deep space and the waxing gibbous Moon.
MISR Views the Moon
This infrared image, taken by NASA Galileo spacecraft in late June, 1996, of Jupiter Great Red Spot has different colors than what you normally see.
First Near Infrared Mapping Spectrometer NIMS Image of the Great Red Spot
CANDLE FLAME NORMAL 1-G ONE GRAVITY AND MICROGRAVITY 0-G ZERO GRAVITY COMPARISON
GRC-1998-C-00486
X-14 NASA 704 Full Scale Airplane tests in  40x80ft. Wind Tunnel (NORMAL MOUNTING) jet inlets
ARC-1967-A-38763
Comparison of a Candle Flame burning in normal gravity or 1-G (left) and a flame burning in Microgravity.
GRC-1998-C-00485
While the crater in this VIS image was crated by an impact event, the resultant form is not the normal circular shape. There are several factors that can create 'out of round' craters. The most common is subsurface faulting from tectonic activity. Pre-existing subsurface fractures can deflect impact pressures along the fault faces, rather than uniformly radially from the center of impact. Meteor Crater in Arizona has "corners" due to the same tectonic forcing of impact pressures.  Orbit Number: 89615 Latitude: 31.7702 Longitude: 156.612 Instrument: VIS Captured: 2022-02-26 05:06  https://photojournal.jpl.nasa.gov/catalog/PIA25404
Out of Round
Recent sea-level height data from NASA U.S./France Jason altimetric satellite during a 10-day cycle ending February 22, 2005, show that the central equatorial Pacific continues to exhibit an area of higher-than-normal sea surface heights.
El Niño: The Weak, Getting Weaker
Sea-level height data from NASA U.S./France Jason altimetric satellite during a 10-day cycle ending July 27, 2004, show weaker than normal trade winds in the western and central equatorial Pacific have triggered an eastward moving, warm Kelvin wave.
Warm Pacific Water Wave Heads East, But No El Niño Yet
This nighttime view of Saturn north pole reveals a dynamic, active planet at least 75 kilometers 47 miles below the normal cloud tops seen in visible light. Clearly revealed is the bizarre six-sided hexagon feature present at the north pole
Saturn North Pole Hexagon and Aurora
This artist concept shows how a normal spiral galaxy around our local universe left might have looked back in the distant universe, when astronomers think galaxies would have been filled with larger populations of hot, bright stars right.
Galaxies Near and Far Artist Concept
NASA Cassini spacecraft has been monitoring propeller features such as Bleriot since their discovery. The bright dash-like features are regions where a small moonlet has caused ring particles to cluster together more densely than normal.
Propeller, Light and Dark
Recent sea-level height data from NASA Jason-1 altimetric satellite show that continuing weaker-than-normal trade winds in the western and central equatorial Pacific have triggered another strong, eastward moving, warm Kelvin wave.
Jason Celebrates 5th Anniversary as El Niño Builds, Warm Kelvin Wave Surges Toward South America
On January 26, 2001, when India Republic Day is normally celebrated, a devastating earthquake hit the state of Gujarat. These two false-color images were acquired by NASA Terra spacecraft before and after the event, on January 15 and 31.
Dewatering Effects from the Gujarat earthquake
These data, taken during a 10-day collection cycle ending August 18, 2001, show that above-normal sea-surface heights and warmer ocean temperatures still blanket the far-western tropical Pacific and much of the north and south mid-Pacific.
Pacific Decadal Oscillation Still Rules in Pacific; No Niño Anytime Soon
Data taken during a 10-day collection cycle ending March 9, 2001, show that above-normal sea-surface heights and warmer ocean temp. red and white areas still blanket the far-western tropical Pacific and much of the north and south mid-Pacific.
Warm Ocean Temperatures Blanket the Far-Western Pacific
The latest image from NASA Jason oceanography satellite, taken during a 10-day collection cycle ending December 2, 2002, shows the Pacific dominated by two significant areas of higher-than-normal sealevel warmer ocean temperatures.
El Niño Continues to Grow
Lingering just a month ago in the eastern Pacific Ocean, the La Niña phenomenon, with its large volume of chilly water, barely has a pulse this month, according to new satellite data from NASA U.S.-French TOPEX/Poseidon mission.  The data, taken during a 10-day cycle of data collection ending June 18, show that the equatorial Pacific Ocean is warming up and returning to normal (green) as La Niña all but vanishes. The warming trend is most apparent in the equatorial Pacific Ocean, where only a few patches of cooler, low sea levels (seen in blue and purple) remain. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal. Like its counterpart, El Niño, a La Niña condition will influence global climate and weather until it has completely subsided.  As summer begins in the northern hemisphere, lower-than-normal sea surface levels and cool ocean temperatures persist in the northeastern Gulf of Alaska and along the western coast of North America. In contrast, the trend is the opposite over most of the Pacific, where above-normal sea surface heights and warmer ocean temperatures (indicated by the red and white areas) appear to be increasing and dominating the overall Pacific Ocean. Red areas are about 10 centimeters (4 inches) above normal; white areas show the sea surface height is between 14 and 32 centimeters (6 and 13 inches) above normal.  Scientists are not ready to administer last rites to La Niña, though. In the last 12 months, the pool of unusually cold water in the Pacific has shrunk (warmed) several times before cooling (expanding) again. This summer's altimeter data will help them determine whether La Niña has truly dissipated or whether they will see another resurgence of cool water in the Pacific.  http://photojournal.jpl.nasa.gov/catalog/PIA01586
TOPEX/El Niño Watch - La Niña Barely Has a Pulse, June 18, 1999
Effects of thrust reversers on the aerodynamics characteristics of a four-engine jet transport model. 1/4 front view on normal struts with thrust reversers.
Four Engine Jet Transport Model.
This diagram shows the normal pathways of calcium movement in the body and indicates changes (green arrows) seen during preliminary space flight experiments. Calcium plays a central role because 1) it gives strength and structure to bone and 2) all types of cells require it to function normally. To better understand how and why weightlessness induces bone loss, astronauts have participated in a study of calcium kinetics -- that is, the movement of calcium through the body, including absorption from food, and its role in the formation and breakdown of bone.
Biotechnology
Cells from kidneys lose some of their special features in conventional culture but form spheres replete with specialized cell microvilli (hair) and synthesize hormones that may be clinically useful. Ground-based research studies have demonstrated that both normal and neoplastic cells and tissues recreate many of the characteristics in the NASA bioreactor that they display in vivo. Proximal kidney tubule cells that normally have rich apically oriented microvilli with intercellular clefts in the kidney do not form any of these structures in conventional two-dimensional monolayer culture. However, when normal proximal renal tubule cells are cultured in three-dimensions in the bioreactor, both the microvilli and the intercellular clefts form. This is important because, when the morphology is recreated, the function is more likely also to be rejuvenated. The work is sponsored by NASA's Office of Biological and Physical Research. The bioreactor is managed by the Biotechnology Cell Science Program at NASA's Johnson Space Center (JSC).
Microgravity
The latest remote sensing data from NASA's Jason satellite show that the equatorial Pacific sea surface levels are higher, indicating warmer sea surface temperatures in the central and west Pacific Ocean. This pattern has the appearance of La Niña rather than El Niño. This contrasts with the Bering Sea, Gulf of Alaska and U.S. West Coast where lower-than-normal sea surface levels and cool ocean temperatures continue (indicated by blue and purple areas).  The image above is a global map of sea surface height, accurate to within 30 millimeters. The image represents data collected and composited over a 10-day period, ending on Jan 23, 2004. The height of the water relates to the temperature of the water. As the ocean warms, its level rises; and as it cools, its level falls. Yellow and red areas indicate where the waters are relatively warmer and have expanded above sea level, green indicates near normal sea level, and blue and purple areas show where the waters are relatively colder and the surface is lower than sea level. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal.  http://photojournal.jpl.nasa.gov/catalog/PIA05071
Pacific Dictates Droughts and Drenchings
Adolph Spakowski, head of the Photovoltaic Fundamentals Section at the National Aeronautics and Space Administration (NASA) Lewis Research Center, illustrated the difference between conventional silicon solar cells (rear panel) and the new thin-film cells. The larger, flexible thin-film cells in the foreground were evaluated by Lewis energy conversion specialists for possible future space use. The conventional solar cells used on most spacecraft at the time were both delicate and heavy. For example, the Mariner IV spacecraft required 28,000 these solar cells for its flyby of Mars in 1964.     NASA Lewis began investigating cadmium sulfide thin-film solar cells in 1961. The thin-film cells were made by heating semiconductor material until it evaporated. The vapor was then condensed onto an electricity-producing film only one-thousandth of an inch thick. The physical flexibility of the new thin-film cells allowed them to be furled, or rolled up, during launch.    Spakowski led an 18-month test program at Lewis to investigate the application of cadmium sulfide semiconductors on a light metallized substrate. The new thin-film solar cells were tested in a space simulation chamber at a simulated altitude of 200 miles. Sunlight was recreated by a 5000-watt xenon light. Two dozen cells were exposed to 15 minutes of light followed by 15 minutes of darkness to test their durability in the constantly changing illumination of Earth orbit.
New Thin-Film Solar Cells Compared to Normal Solar Cells
STS109-331-010 (9 March 2002) ---  The Hubble Space Telescope (HST) heads back toward its normal routine, after  a week of servicing and upgrading by  the STS-109 astronaut crew on board the Space Shuttle Columbia.
Deployed view of the Hubble Space Telescope
X-14 NASA 704 Full Scale Airplane tests in  40x80ft. Subsonic Wind Tunnel (NORMAL MOUNTING) with Sy Sewell, NASA (left) and Ed Varette, Army (right)
ARC-1967-AC-38761
Attendees gather next to the X-57 Maxwell aircraft during a knowledge sharing meeting at NASA’s Armstrong Flight Research Center in Edwards, California looking at a display of the battery assembly that normally sits inside the aircraft.
X-57 Maxwell Technical Interchange Meeting
STS109-331-005 (9 March 2002) ---  The Hubble Space Telescope (HST) heads back toward its normal routine, after  a week of servicing and upgrading by  the STS-109 astronaut crew on board the Space Shuttle Columbia.
Deployed view of the Hubble Space Telescope
The English confrontation with Indian rockets came in 1780 at the Battle of Guntar. The closely massed, normally unflinching British troops broke and ran when the Indian army laid down a rocket barrage in their midst.
Early Rockets
X-14 NASA 704 Full Scale Airplane tests in  40x80ft. Wind Tunnel (NORMAL MOUNTING) with Sy Sewell, NASA (left) and Ed Varette, Army (right)
ARC-1967-AC-38759
S99-08178 (28 July 1999) --- Normally  housing NASA's fleet of T-38 jet trainers, this Ellington Field hangar  was filled instead with well wishers for the returning crew of STS-93 on the  morning of July 28, 1999.
STS-93 crew return at Ellington Field
The U.S./European Jason-3 satellite has produced its first map of sea surface height, which corresponds well to data from its predecessor, Jason-2. Higher-than-normal sea levels are red; lower-than-normal sea levels are blue. El Niño is visible as the red blob in the eastern equatorial Pacific.  Extending the timeline of ocean surface topography measurements begun by the Topex/Poseidon and Jason 1 and 2 satellites, Jason 3 will make highly detailed measurements of sea-level on Earth to gain insight into ocean circulation and climate change.   http://photojournal.jpl.nasa.gov/catalog/PIA20532
Jason-3 Produces First Global Map of Sea Surface Height
Images from the U.S./European Jason-3 satellite show sea surface height with respect to the seasonal cycle and the long-term trend. Blue/magenta colors indicate lower-than-normal sea levels, while yellow/red colors indicate higher-than-normal sea levels. The April 9, 2018 image (left panel) shows most of the ocean at neutral heights (green). A month later (right panel), a red patch is visible along the equator in the Central Pacific. The red area is a downwelling Kelvin wave, traveling eastward along the equator.  https://photojournal.jpl.nasa.gov/catalog/PIA22473
Downwelling Kelvin Wave in the Pacific
Some climate forecast models indicate there is an above average chance that there could be a weak to borderline El Niño by the end of November 2003. However, the trade winds, blowing from east to west across the equatorial Pacific Ocean, remain strong. Thus, there remains some uncertainty among climate scientists as to whether the warm temperature anomaly will form again this year. The latest remote sensing data from NASA's Jason satellite show near normal conditions across the equatorial Pacific. There are currently no visible signs in sea surface height of an impending El Niño.  This equatorial quiet contrasts with the Bering Sea, Gulf of Alaska and U.S. West Coast where lower-than-normal sea surface levels and cool ocean temperatures continue (indicated by blue and purple areas).  The image above is a global map of sea surface height, accurate to within 30 millimeters. The image represents data collected and composited over a 10-day period, ending on Nov. 3, 2003. The height of the water relates to the temperature of the water. As the ocean warms, its level rises; and as it cools, its level falls. Yellow and red areas indicate where the waters are relatively warmer and have expanded above sea level, green indicates near normal sea level, and blue and purple areas show where the waters are relatively colder and the surface is lower than sea level. The blue areas are between 5 and 13 centimeters (2 and 5 inches) below normal, whereas the purple areas range from 14 to 18 centimeters (6 to 7 inches) below normal.  http://photojournal.jpl.nasa.gov/catalog/PIA04878
A Mostly Quiet Pacific
This map shows sea level measured by the Sentinel-6 Michael Freilich satellite from June 5 to15. Red areas are regions where sea level is higher than normal, and blue areas indicate areas where it's lower than normal.  The measurements are part of a set of data streams that become available to the public hours to a couple of days after the satellite collects them. The difference in when the products become available balances accuracy with delivery timeliness for tasks like forecasting the weather or helping to monitor the formation of hurricanes. The satellite, named after former NASA Earth Science Division Director Michael Freilich, collects its measurements for about 90% of the world's oceans.  The spacecraft is one of two satellites that compose the Copernicus Sentinel-6/Jason-CS (Continuity of Service) mission. The second satellite, Sentinel-6B, is slated for launch in 2025. Together, they are the latest in a series of spacecraft starting with TOPEX/Poseidon in 1992 and continuing with the Jason series of satellites that have been gathering precise ocean height measurements for nearly 30 years.  Shortly after launch in Nov. 2020, Sentinel-6 Michael Freilich moved into position, trailing the current reference sea level satellite Jason-3 by 30 seconds. Scientists and engineers then spent time cross-calibrating the data collected by both satellites to ensure the continuity of measurements between the two. Once assured of the data quality, Sentinel-6 Michael Freilich will then become the primary sea level satellite.  https://photojournal.jpl.nasa.gov/catalog/PIA24533
Sentinel-6 Michael Freilich Sea Surface Height
Testing of the Little Joe booster on its launcher. The launcher is positioned at its normal launch angle of 80 degrees. Joseph Shortal wrote (vol. 3, p. 33):  The Little Joe booster was assembled at Wallops on its special launcher in a vertical attitude. It is shown in the  on the left  with the work platform in place. The launcher was located on a special concrete slab in Launching Area 1. The capsule was lowered onto the booster by crane.... After the assembly was completed, the scaffolding was disassembled and the launcher pitched over to its normal launch angle of 80 degrees.... Little Joe had a diameter of 80 inches and an overall length, including the capsule and escape tower of 48 feet. The total weight at launch was about 43,000 pounds. The overall span of the stabilizing fins was 21.3 feet.   Although in comparison with the overall Mercury Project, Little Joe was a simple undertaking, the fact that an attempt was made to condense a normal two-year project into a 6-month one with in house labor turned it into a major undertaking for Langley.  -- Published in Joseph A. Shortal, History of Wallops Station: Origins and Activities Through 1949, (Wallops Island, VA: National Aeronautics and Space Administration, Wallops Station, nd), Comment Edition.
Mercury: testing of the Little Joe booster
Paul Ducheyne, a principal investigator in the microgravity materials science program and head of the University of Pernsylvania's Center for Bioactive Materials and Tissue Engineering, is leading the trio as they use simulated microgravity to determine the optimal characteristics of tiny glass particles for growing bone tissue. The result could make possible a much broader range of synthetic bone-grafting applications. Even in normal gravity, bioactive glass particles enhance bone growth in laboratory tests with flat tissue cultures. Ducheyne and his team believe that using the bioactive microcarriers in a rotating bioreactor in microgravity will produce improved, three-dimensional tissue cultures. The work is sponsored by NASA's Office of Biological and Physical Research. The bioreactor is managed by the Biotechnology Cell Science Program at NASA's Johnson Space Center (JSC). NASA-sponsored bioreactor research has been instrumental in helping scientists to better understand normal and cancerous tissue development. In cooperation with the medical community, the bioreactor design is being used to prepare better models of human colon, prostate, breast and ovarian tumors. Cartilage, bone marrow, heart muscle, skeletal muscle, pancreatic islet cells, liver and kidney are just a few of the normal tissues being cultured in rotating bioreactors by investigators. Credit: NASA and University of Pennsylvania Center for Bioactive Materials and Tissue Engineering.
Microgravity
This chart details Skylab's Ultraviolet (UV) X-Ray Solar Photography experiment (S020) in an Apollo Telescope Mount facility. It was designed to photograph normal and explosive areas within the solar atmosphere in the UV and x-ray spectra. The Marshall Space Flight Center had program management responsibility for the development of Skylab hardware and experiments.
Skylab
STS109-348-004 (3 March 2002) ---  The Hubble Space Telescope (HST), with  its normal routine temporarily interrupted, is berthed in the cargo bay of the Space Shuttle Columbia prior to  a week of servicing and upgrading by  the STS-109 astronaut crew.  A thin blue  line of airglow pin-points Earth's horizon at sunrise.
HST in Columbia's payload bay during sunrise
S115-E-05484 (11 Sept. 2006) --- Astronaut Christopher J. Ferguson, STS-115 pilot, temporarily sits in the port station on the flight deck, normally occupied by astronaut Brent W. Jett Jr., the commander for this flight of the Space Shuttle Atlantis.
Ferguson looks at crew procedures on the FD of the Space Shuttle Atlantis during STS-115
This 1970 photograph shows Skylab's Ultraviolet (UV)/X-Ray Solar Photography instrument, an Apollo Telescope Mount (ATM) facility designed to photograph normal and explosive areas in the solar atmosphere in the x-ray and UV spectra. The Marshall Space Flight Center had program management responsibility for the development of Skylab hardware and experiments.
Skylab
The First Robotics Rocket City Regional Competition was held at the Von Braun Civic Center in Huntsville, Alabama on March 16, 2018. High school robotics teams from throughout the U.S., as well as a team from Brazil, competed. Costumed students were the normal at this event and lent it much color.
The First Robotics Rocket City Regional Competition
S63-03964 (1963) --- Al Rochford, Crew Systems, Manned Space Center, assists astronaut L. Gordon Cooper Jr., in checking his life vest, normally stowed in a pocket in the lower left leg. Photo credit: NASA
ROCHFORD, AL - ASTRONAUT COOPER, GORDON L. - LIFE VEST CHECK - PRELAUNCH ACTIVITIES - MERCURY-ATLAS (MA)-9 - MSC
Lunar Landing Walking Simulator: Researchers at Langley study the ability of astronauts to walk, run and perform other tasks required during lunar exploration. The Reduced Gravity Simulator gave researchers the opportunity to look at the effects of one-sixth normal gravity on self-locomotion. Several Apollo astronauts practiced lunar waling at the facility.
Lunar Landing Walking Simulator
iss069e011049 (May 17, 2023) --- From left, Expedition 69 Flight Engineers Frank Rubio of NASA and Sultan Alneyadi of UAE (United Arab Emirates) return the station’s Treadmill 2 to its normal configuration inside the International Space Station's Tranquility module after an inspection and cleaning of its electronic components.
Astronauts Frank Rubio of NASA and Sultan Alneyadi of UAE
iss064e053473 (April 7, 2021) --- NASA astronaut and Expedition 64 Flight Engineer Shannon Walker poses for a portrait inside the U.S. Quest airlock that is normally filled with U.S. spacesuit components when spacewalks are planned at the International Space Station.
iss064e053473
KENNEDY SPACE CENTER, FLA. -  Seen in the photo is one end of the airlock that is installed in the payload bay of orbiter Discovery.  The airlock is normally located inside the middeck of the spacecraft’s pressurized crew cabin. The airlock is sized to accommodate two fully suited flight crew members simultaneously. Support functions include airlock depressurization and repressurization, extravehicular activity equipment recharge, liquid-cooled garment water cooling, EVA equipment checkout, donning and communications. The outer hatch isolates the airlock from the unpressurized payload bay when closed and permits the EVA crew members to exit from the airlock to the payload bay when open.
KENNEDY SPACE CENTER, FLA. - Seen in the photo is one end of the airlock that is installed in the payload bay of orbiter Discovery. The airlock is normally located inside the middeck of the spacecraft’s pressurized crew cabin. The airlock is sized to accommodate two fully suited flight crew members simultaneously. Support functions include airlock depressurization and repressurization, extravehicular activity equipment recharge, liquid-cooled garment water cooling, EVA equipment checkout, donning and communications. The outer hatch isolates the airlock from the unpressurized payload bay when closed and permits the EVA crew members to exit from the airlock to the payload bay when open.
KENNEDY SPACE CENTER, FLA. -  A worker in the Orbiter Processing Facility checks the open hatch of the airlock in Discovery’s payload bay. The airlock is normally located inside the middeck of the spacecraft’s pressurized crew cabin. The airlock is sized to accommodate two fully suited flight crew members simultaneously. Support functions include airlock depressurization and repressurization, extravehicular activity equipment recharge, liquid-cooled garment water cooling, EVA equipment checkout, donning and communications. The outer hatch isolates the airlock from the unpressurized payload bay when closed and permits the EVA crew members to exit from the airlock to the payload bay when open.
KENNEDY SPACE CENTER, FLA. - A worker in the Orbiter Processing Facility checks the open hatch of the airlock in Discovery’s payload bay. The airlock is normally located inside the middeck of the spacecraft’s pressurized crew cabin. The airlock is sized to accommodate two fully suited flight crew members simultaneously. Support functions include airlock depressurization and repressurization, extravehicular activity equipment recharge, liquid-cooled garment water cooling, EVA equipment checkout, donning and communications. The outer hatch isolates the airlock from the unpressurized payload bay when closed and permits the EVA crew members to exit from the airlock to the payload bay when open.
KENNEDY SPACE CENTER, FLA. -  Seen in the photo is one end of the airlock that is installed in the payload bay of orbiter Discovery.  The airlock is normally located inside the middeck of the spacecraft’s pressurized crew cabin. The airlock is sized to accommodate two fully suited flight crew members simultaneously. Support functions include airlock depressurization and repressurization, extravehicular activity equipment recharge, liquid-cooled garment water cooling, EVA equipment checkout, donning and communications. The outer hatch isolates the airlock from the unpressurized payload bay when closed and permits the EVA crew members to exit from the airlock to the payload bay when open.
KENNEDY SPACE CENTER, FLA. - Seen in the photo is one end of the airlock that is installed in the payload bay of orbiter Discovery. The airlock is normally located inside the middeck of the spacecraft’s pressurized crew cabin. The airlock is sized to accommodate two fully suited flight crew members simultaneously. Support functions include airlock depressurization and repressurization, extravehicular activity equipment recharge, liquid-cooled garment water cooling, EVA equipment checkout, donning and communications. The outer hatch isolates the airlock from the unpressurized payload bay when closed and permits the EVA crew members to exit from the airlock to the payload bay when open.
Astronaut John Blaha replaces an exhausted media bag and filled waste bag with fresh bags to continue a bioreactor experiment aboard space station Mir in 1996. NASA-sponsored bioreactor research has been instrumental in helping scientists to better understand normal and cancerous tissue development. In cooperation with the medical community, the bioreactor design is being used to prepare better models of human colon, prostate, breast and ovarian tumors. Cartilage, bone marrow, heart muscle, skeletal muscle, pancreatic islet cells, liver and kidney are just a few of the normal tissues being cultured in rotating bioreactors by investigators. This image is from a video downlink. The work is sponsored by NASA's Office of Biological and Physical Research. The bioreactor is managed by the Biotechnology Cell Science Program at NASA's Johnson Space Center (JSC).
Microgravity
The heart of the bioreactor is the rotating wall vessel, shown without its support equipment. Volume is about 125 mL. The work is sponsored by NASA's Office of Biological and Physical Research. The bioreactor is managed by the Biotechnology Cell Science Program at NASA's Johnson Space Center (JSC). NASA-sponsored bioreactor research has been instrumental in helping scientists to better understand normal and cancerous tissue development. In cooperation with the medical community, the bioreactor design is being used to prepare better models of human colon, prostate, breast and ovarian tumors. Cartilage, bone marrow, heart muscle, skeletal muscle, pancreatic islet cells, liver and kidney are just a few of the normal tissues being cultured in rotating bioreactors by investigators.
Microgravity
The NASA Bioreactor provides a low turbulence culture environment which promotes the formation of large, three-dimensional cell clusters. Due to their high level of cellular organization and specialization, samples constructed in the bioreactor more closely resemble the original tumor or tissue found in the body. NASA-sponsored bioreactor research has been instrumental in helping scientists to better understand normal and cancerous tissue development. In cooperation with the medical community, the bioreactor design is being used to prepare better models of human colon, prostate, breast and ovarian tumors. Cartilage, bone marrow, heart muscle, skeletal muscle, pancreatic islet cells, liver and kidney are just a few of the normal tissues currently being cultured in rotating bioreactors by investigators
Microgravity
The NASA Bioreactor provides a low turbulence culture environment which promotes the formation of large, three-dimensional cell clusters. Due to their high level of cellular organization and specialization, samples constructed in the bioreactor more closely resemble the original tumor or tissue found in the body. NASA-sponsored bioreactor research has been instrumental in helping scientists to better understand normal and cancerous tissue development. In cooperation with the medical community, the bioreactor design is being used to prepare better models of human colon, prostate, breast and ovarian tumors. Cartilage, bone marrow, heart muscle, skeletal muscle, pancreatic islet cells, liver and kidney are just a few of the normal tissues currently being cultured in rotating bioreactors by investigators.
Microgravity
Astronomers are studying the unusual appearance of Saturn's rings. The top portion of this Hubble Space Telescope snapshot shows Saturn with its rings barely visible. Normally, astronomers see Saturn with its rings tilted, but because the Earth was almost in the plane of Saturn's rings, they appear edge-on. Positioned above the ring plane, the Sun is causing the rings to cast a shadow on Saturn. The bottom photograph shows Saturn with its rings slightly tilted, and displays a faint narrow ring, the F-ring, just outside the main ring, which is normally invisible from Earth. The moon called Dion, on the lower right, is casting a long, thin shadow across the whole ring system due to the setting of the sun on the ring plane.
History of Hubble Space Telescope (HST)
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge
 High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 NASA Exploration Rover Challenge
NASA has completes the final test to qualify Orion’s parachute system for flights with astronauts, checking off an important milestone on the path to send humans on missions to the Moon and beyond on Sept. 12, 2018...Over the course of eight tests at the U.S. Army’s Yuma Proving Ground in Arizona, engineers have evaluated the performance of Orion’s parachute system during normal landing sequences as well as several failure scenarios and a variety of potential aerodynamic conditions to ensure astronauts can return safely from deep space missions.
NASA Completes Orion Parachute Tests for Missions with Astronaut
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge
KENNEDY SPACE CENTER, FLA. -  On Launch Pad 39A, astronaut-suited workers take part in an emergency egress scenario. The four-hour exercise simulated normal launch countdown operations, with the added challenge of a fictitious event causing an evacuation of the vehicle and launch pad.  It tested the team’s rescue approaches on the Fixed Service Structure, slidewire basket evacuation, triage care and transportation of injured personnel to hospitals, as well as communications and coordination.
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 High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 NASA Exploration Rover Challenge
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge event
 High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 NASA Exploration Rover Challenge
 High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 NASA Exploration Rover Challenge
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge event
KENNEDY SPACE CENTER, FLA. - Employees at NASA Kennedy Space Center move equipment into the Thermal Protection System facility that has recently been repaired.  The upper floor of the facility, where soft material was processed, was damaged during the 2004 hurricanes and the equipment was temporarily moved to the RLV Hangar.  While the TPS facility was being repaired, normal work activity was done in the hangar.
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High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge
 High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 NASA Exploration Rover Challenge
KENNEDY SPACE CENTER, FLA. - One of the blanket sewing machines used on Thermal Protection System materials has been returned to the TPS facility.  It was moved to the RLV Hangar at NASA Kennedy Space Center after the 2004 hurricanes damaged the upper floor, where soft material was processed, of the TPS facility.   While the TPS facility was being repaired, normal work activity was done in the hangar.
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High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge event
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge event
 High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 NASA Exploration Rover Challenge
 High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 NASA Exploration Rover Challenge
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge
iss064e030517 (2/9/2021) --- A view of the  Plant Water Management (PWM) investigation aboard the International space Station (ISS). Plant Water Management demonstrates a hydroponic method for ensuring adequate hydration and aeration to the root zone in order to sustain plants from germination through harvest. Low-gravity capillary fluidics deliver water in single and multiple plant production chambers, and researchers compare growth of individual plants in microgravity and normal gravity.
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High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge
jsc2024e067103 (2/2/2024) --- Martha and Josh Morris Mathematics and Engineering Elementary students Lizzy, Lynnley, Isaac, and Cooper work on ways to calculate the strength of concrete in microgravity. Their experiment, Will Normal Strength Concrete (NSC) Keep its Structure in Microgravity?, is part of the Nanoracks-National Center for Earth and Space Science Education-Surveyor-Student Spaceflight Experiments Program Mission 18 to ISS (Nanoracks-NCESSE-Surveyor-SSEP).
Preflight Imagery for Nanoracks-NCESSE-Surveyor-SSEP
 High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 NASA Exploration Rover Challenge
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge event
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge event
S72-30704 (1972) --- Astronaut Bruce McCandless II, backup pilot for Skylab 2, tests the balance and control of an astronaut maneuvering unit (AMU) test model at Martin Marietta Corporation's Denver division. The jet-powered backpack can fly for 30 minutes and can be worn over normal clothing or spacesuit. Photo credit: NASA
Astronaut Bruce McCandless tests astronaut maneuvering unit
Dr. Timothy G. Hammond of the Department of Internal Medicine, Nephrology Section, Tulane University Medical Center, New Orleans, LA, is one of NASA's principal investigators conducting research with the NASA Bioreactor project directed by Johrnson Space Center. Hammond's investigations include Production of 1-25- diOH D3 by Renal Epithelial Cells in Simulated Microgravity Culture and Differentiation of Cultured Normal Human Renal Epithelial Cells in Microgravity. Photo credit: Tulane University.
Microgravity
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge event
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge event
High school and university students competed in the 2018 Human Exploration Rover Challenge event at the U.S. Space and Rocket Center in Huntsville, Alabama. Students came from across the U.S. as well as several foreign countries such as Brazil, Germany, India, and Mexico. This event, which is normally a 2 day event, was shortened to 1 day in 2018 due to adverse weather conditions.
2018 Human Exploration Rover Challenge