A Tranquil Sunrise

A Tranquil Sunrise

The sky and water take up equal parts of this image. At the horizon, the Sun colors the sky orange, with its light reflecting off a few distant clouds. A fast boat in the distance cuts a line across the water as it moves from left to right. The boat and the person aboard are in silhouette.
NASA/Joel Kowsky

A fast boat crosses the waters several hours after NASA’s SpaceX Crew-7 splashdown on March 12, 2024. The SpaceX Dragon Endurance spacecraft landed in the Gulf of Mexico off the coast of Pensacola, Florida. The Crew-7 members spent nearly six months in space as part of Expedition 70 on the International Space Station.

Throughout their mission, the Crew-7 members contributed to a host of science and maintenance activities and technology demonstrations. Moghbeli conducted one spacewalk, joined by NASA astronaut Loral O’Hara, replacing one of the 12 trundle bearing assemblies on the port solar alpha rotary joint, which allows the arrays to track the Sun and generate electricity to power the station.

Image Credit: NASA/Joel Kowsky

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Monika Luabeya

Advancing Human Spaceflight Safety

Advancing Human Spaceflight Safety

As NASA continues to pursue new human missions to low Earth orbit, lunar orbit, the lunar surface, and on to Mars, the NESC continues to provide a robust technical resource to address critical challenges.

The NESC Environmental Control and Life Support Systems (ECLSS), Crew Systems, and Extravehicular Activity (EVA) discipline is led by the NASA Technical Fellow for ECLS, Dr. Morgan Abney, ECLSS & Crew Systems Deputy Dave Williams, Extravehicular & Human Surface Mobility Deputy Danielle Morris, and EVA Deputy Colin Campbell. In 2023, this team led assessments and provided support to the Commercial Crew Program, ISS, Orion Multi-Purpose Crew Vehicle, Extravehicular and Human Mobility Program, Gateway International Habitat, and Moon-to-Mars Program. Three of the most notable activities in 2023 are briefly described below.

Mitigation for Water in the Helmet During EVA

During EVA22 in 2013, water was observed in the helmet and assumed to be the result of a “burp” from the drink bag. No further investigation was pursued because water had been observed to some degree (water on visor, wet hair, etc.) on eight previous occasions. The result was a nearly catastrophic event during EVA23, where astronaut Luca Parmitano experienced dangerous quantities of water in his helmet. Both EVA23 and EVA35 in 2016 contributed to identification of drowning as a key risk, which resulted in several water mitigation approaches. Based on these approaches, the program determined the risk level to be acceptable for nominal EVA. However, in March 2022, a crewmember returning from EVA80 noticed water accumulated on the visor of his helmet obstructing ~30-50% of his field of view. Due to the increasing complexity of EVA objectives on EVA80 and forward, the ISS Program identified loss or reduction of visibility as a greater risk than previously recognized and sought to identify methods to prevent even small quantities of liquid water from forming in the helmet during EVA. The NESC was asked to provide support to the activity through modeling of the helmet and two-phase (water and oxygen) flow behavior in microgravity, through model validation testing, and through testing of mitigation hardware identified by the larger team. The model predictions provided a map (Figure 1) of anticipated liquid water formations based on the contact angle between the face or head and the helmet surface. Based on the ISS helmet with no water mitigations, the model predicted that large blobs would most likely form bridges between the helmet and face and that rupture of those bridges would result in the majority of liquid transferring to the face. To mitigate this risk, the ISS EVA80 team devised a solution to add absorbent materials in the path of the oxygen and water entering the helmet. Following EVA23, the helmet absorption pad (HAP) was added for bulk water collection. The improved mitigation strategy based on EVA80 included a HAP extender (HAP-E) and a helmet absorption band (HAB) (Figure 2). The NESC provided modeling of the mitigation hardware and validation testing of the HAB configuration using flow conditions anticipated in ISS operation (Figure 3). The testing provided ground validation of the HAB performance. The HAB and HAP-E have both been implemented in flight.

Figure 1. Map of predicted water formations within a helmet as a function of face/head and helmet contact angles. Dashed rectangle indicates the expected domain of the ISS helmet with no water mitigations. 
Figure 2. Water mitigation strategy for the ISS helmet: a) sketch of HAP, HAP-E, and HAB, b) side view of early prototype, c) bottom view of early prototype. 
Figure 3. HAB ground validation testing under trickle water flow conditions.

Evaluation of Terrestrial Portable Fire Extinguishers for Microgravity Applications 

The tragic fire of Apollo 1 has, of necessity, instilled in NASA an enduring respect for the risk of fire in spacecraft. As such, robust fire detection and response systems have been a cornerstone of NASA-designed vehicles. Portable fire extinguishers (PFE) are a fundamental fire response capability of spacecraft and both carbon dioxide and water-based PFEs have been used by NASA historically. However, terrestrial-based PFEs, particularly those using new halon-based suppressants, may provide improved capability beyond the NASA state-of-the-art. In 2023, the NESC sought to evaluate the effectiveness of commercial-off-the-shelf (COTS) PFEs in microgravity. The team developed an analytical model to predict the discharge rate of three terrestrial COTS PFEs containing CO2, HFC-227ea, and Novec 1230. The model considered the internal geometry of the PFEs, the material properties of the suppressants and their corresponding PFE tanks, and the effects of microgravity and in-flight perturbations. The results predicted that for PFE tanks containing dip tubes, like those for HFC-227ea and Novec 1230 where nitrogen gas is used as a pressurant, microgravity plays a significant role in the discharge performance due to two-phase flow. Figure 4 shows the various equilibrium configurations based on gravity and perturbations. As a comparison, the analysis predicts >80% discharge of the HFC-227ea in the COTS PFE within ~30 seconds with the remainder discharging over ~0.5-1 hours when discharged in a terrestrial fire (Figure 4A), while only 60-80% discharges in 30 seconds with the remainder discharging over 1-2 hours in microgravity (Figure 4C). 

Figure 4. Equilibrium two-phase configurations of nitrogen (white)-pressurized liquid suppressant (blue). A) PFE held nominally with nozzle up in 1-g with no perturbations, B) PFE held inverted in 1-g or in 0-g where liquid preferentially accumulates away from the dip tube entrance with no perturbations, C) PFE in 0-g at the statistically most probable state with no perturbations, D) PFE in 0-g where nitrogen preferentially accumulates at ends of the PFE with no perturbations, E) PFE in any level gravity with significant perturbations (shaken up), and F) statistically most probable state in 0-g following complete discharge.

Based on this analysis, the use of terrestrially designed PFEs containing gaseous pressurant over a liquid suppressant will likely result in decreased initial discharge of the suppressant and significantly longer total discharge times in microgravity as compared to terrestrial discharge performance. Testing is ongoing to validate the models using a custom-designed PFE test stand (Figures 5 and 6) that enables multi-configuration testing of COTS PFEs. 

Figure 5. (left) PFE test stand for model validation. Design prevents directional load effects to enable accurate mass measurement during PFE discharge. Figure 6. (right) Insulated PFE housing and remote discharge control allows for accurate, real-time thermal measurements during validation testing.

Standardized Abrasion, Cut, and Thermal Testing for Spacesuit Gloves and Materials  

State-of-the-art spacesuit gloves have been optimized for the challenges of ISS. Artemis missions call for high-frequency EVAs at the lunar south pole, where temperatures in the permanently shadowed region (PSR) will expose crew gloves to temperatures lower than ever previously experienced and where frequent and repeated exposure to regolith dust and rocks will present significantly increased risk for abrasion and cuts. With the development of new spacesuits by commercial partners, inexpensive and repeatable test methods are needed to characterize, evaluate, and compare gloves and glove materials for their thermal performance at PSR temperatures and for their resistance to lunar regolith abrasion and cuts. To address these needs, the NESC is leading a team to develop standardized test methods in coordination with ASTM International Committee F47 on Commercial Spaceflight.  

Three standardized methods are currently in development. The first method seeks to standardize lunar dust abrasion testing of glove (and suit) materials based on adapted “tumble testing” first proposed at NASA in 1990. The NASA-designed tumbler (Figure 7) enables testing of six samples per run and compares pre- and post-tumbled tensile strength of materials to compare abrasion resistance. The method is highly controlled using a commercially available tumble medium and lunar regolith simulant.  

Because material properties change with temperature, the second method seeks to develop a standardized approach to evaluate the cut resistance of glove materials at relevant cryogenic temperatures. The method is an adaptation of ASTM F2992 Standard Test Method for Measuring Cut Resistance of Materials Used in Protective Clothing with Tomodynamometer (TDM-100) Test Equipment. In order to allow for cut evaluation at cryogenic temperatures, the TDM-100 cut fixture was modified to include channels for liquid nitrogen flow (Figure 8A), thereby cooling the test material to 77 K. 

Figure 7. Hardware used in the tumble test method. Tumbler apparatus (left). Tumbler with panel removed to show lunar regolith simulant and commercially available tumbler media (top right). Tumbler panel showing lunar regolith simulant (bottom right).

The third method seeks to evaluate the thermal performance of gloves down to PSR requirement temperature of 48 K. Historical thermal testing of gloves was conducted with human-in-the-loop (HITL) testing for both radiative and conductive cooling. Conductive cooling was accomplished by having the test subject grab thermally controlled “grasp objects” and maintain contact until their skin temperature reached 283 K (50 ºF) or until they felt sufficient discomfort to end the test themselves. While HITL testing is critical for final certification of gloves, iterative design and development testing would benefit from a faster, less expensive test. To meet this need, the NESC is developing a glove thermal test that uses a custom manikin hand designed by Thermetrics, LLC (Figure 8B). 

Figure 8. A) Mandrel used in cut testing as designed for ambient testing (left) and cryogenic testing (right). Flow channels allow for liquid nitrogen flow to cool the material sample to cryogenic temperatures. B) Prototype of Thermetrics, LLC custom manikin hand for spacesuit glove thermal testing.

The manikin hand is outfitted with temperature and heat flux sensors to monitor heat transfer to the hand. The hand is placed within a spacesuit glove and thermally controlled with internal water flow to simulate human heat generation. The Cryogenic Ice Transfer, Acquisition, Development, and Excavation Laboratory (CITADEL) chamber at JPL is then used to test the glove thermal performance at a range of temperatures from 200 K down to 48 K. Thermal performance is evaluated to mimic historical HITL testing under both radiative and conductive cooling. Conductive cooling is accomplished through a temperature-controlled touch object and is evaluated using two touch pressures. All three methods will be incorporated as ASTM F47 standard test procedures following NASA and ASTM committee review and approvals (targeting 2024).  

ASA astronaut and Expedition 68 Flight Engineer Nicole Mann is pictured in her Extravehicular Mobility Unit (EMU) during an EVA. The NESC has recently contributed to astronaut safety investigations of water accumulating in EMU helmets during EVAs, and developing EMU gloves for use in the harsh conditions of the lunar south pole.

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Meagan Chappell

NASA, Health and Human Services Highlight Cancer Moonshot Progress

NASA, Health and Human Services Highlight Cancer Moonshot Progress

NASA Administrator Bill Nelson delivers remarks during an event with Department of Health and Human Services Secretary Xavier Becerra to highlight how the agencies are making progress toward President Joe Biden and First Lady Jill Biden’s Cancer Moonshot initiative, Thursday, March 21, 2024, in the Earth Information Center at the Mary W. Jackson NASA Headquarters building in Washington. NASA is working with agencies and researchers across the federal government to help cut the nation’s cancer death rate by at least 50% in the next 25 years, a goal of the Cancer Moonshot Initiative.
Credit: NASA/Keegan Barber

During an event at NASA Headquarters in Washington Thursday, NASA Administrator Bill Nelson and U.S. Department of Health and Human Services (HHS) Secretary Xavier Becerra united to note progress their respective agencies are making in space and on Earth toward President Biden and First Lady Jill Biden’s Cancer Moonshot initiative.

“We go to space not just to explore the stars, but to improve life here on Earth,” said Nelson. “In that microgravity environment, NASA is studying cancer growth—and the effect of cancer treatments— much faster than we can on Earth. I am grateful for President Biden’s leadership as we continue to make moonshot after moonshot to end cancer as we know it.”

Also participating in the event was Dr. W. Kimryn Rathmell, director of the National Cancer Institute, as well as NASA astronauts Stephen Bowen and Frank Rubio, both of whom each recently served extended science missions 250 miles off the Earth aboard the International Space Station where they conducted cancer-related research.

As the second leading cause of death in the United States, the President and First Lady’s Cancer Moonshot is a national effort to end cancer. Nelson noted several related experiments space station astronauts have conducted aboard the orbital laboratory for the benefit of all including protein crystal growth, nanoparticle drug delivery, tissue engineering, and stem cell research.

In addition to $2.9 billion across HHS in the President’s fiscal year 2025 budget proposal, Becerra discussed his agency’s capabilities to accelerate progress toward the President’s moonshot goals.

“Eliminating cancer as we know it is a goal that unifies the country,” said Becerra. “We all know someone, and most of us love someone, who has battled this terrible disease. As we did during the race to the Moon, we believe our technology and scientific community are capable of making the impossible a reality when it comes to ending cancer as we know it.”

The backdrop for the event was NASA’s Earth Information Center, which provides access to NASA satellites and other data to see how our planet is changing.

NASA is working with HHS and researchers across the federal government to help cut the nation’s cancer death rate by at least 50% in the next 25 years, a goal of the Cancer Moonshot Initiative.

Learn more about Cancer Moonshot at:

https://www.whitehouse.gov/cancermoonshot/

-end-

Faith McKie / Cheryl Warner
Headquarters, Washington
202-358-1600
faith.d.mckie@nasa.gov / cheryl.m.warner@nasa.gov

Renata Miller
Health and Human Services, Washington
202-570-8194
renata.miller@hhs.gov

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Mar 21, 2024

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Lauren E. Low

NASA Analysis Sees Spike in 2023 Global Sea Level Due to El Niño

NASA Analysis Sees Spike in 2023 Global Sea Level Due to El Niño

Sea level rise is affecting coastal communities around the world, especially those like Honolulu, pictured, that are located on islands.
NOAA Teacher at Sea Program, NOAA Ship HI’IALAKAI

A long-term sea level dataset shows ocean surface heights continuing to rise at faster and faster rates over decades of observations.

Global average sea level rose by about 0.3 inches (0.76 centimeters) from 2022 to 2023, a relatively large jump due mostly to a warming climate and the development of a strong El Niño. The total rise is equivalent to draining a quarter of Lake Superior into the ocean over the course of a year.

This NASA-led analysis is based on a sea level dataset featuring more than 30 years of satellite observations, starting with the U.S.-French TOPEX/Poseidon mission, which launched in 1992. The Sentinel-6 Michael Freilich mission, which launched in November 2020, is the latest in the series of satellites that have contributed to this sea level record.

The data shows that global average sea level has risen a total of about 4 inches (9.4 centimeters) since 1993. The rate of this increase has also accelerated, more than doubling from 0.07 inches (0.18 centimeters) per year in 1993 to the current rate of 0.17 inches (0.42 centimeters) per year.

This graph shows global mean sea level (in blue) since 1993 as measured by a series of five satellites. The solid red line indicates the trajectory of this increase, which more than doubled over the past three decades. The dotted red line projects future sea level rise.
NASA/JPL-Caltech

“Current rates of acceleration mean that we are on track to add another 20 centimeters of global mean sea level by 2050, doubling the amount of change in the next three decades compared to the previous 100 years and increasing the frequency and impacts of floods across the world,” said Nadya Vinogradova Shiffer, director for the NASA sea level change team and the ocean physics program in Washington.

Seasonal Effects

Global sea level saw a significant jump from 2022 to 2023 due mainly to a switch between La Niña and El Niño conditions. A mild La Niña from 2021 to 2022 resulted in a lower-than-expected rise in sea level that year. A strong El Niño developed in 2023, helping to boost the average amount of rise in sea surface height.

La Niña is characterized by cooler-than-normal ocean temperatures in the equatorial Pacific Ocean. El Niño involves warmer-than-average ocean temperatures in the equatorial Pacific. Both periodic climate phenomena affect patterns of rainfall and snowfall as well as sea levels around the world.

“During La Niña, rain that normally falls in the ocean falls on the land instead, temporarily taking water out of the ocean and lowering sea levels,” said Josh Willis, a sea level researcher at NASA’s Jet Propulsion Laboratory in Southern California. “In El Niño years, a lot of the rain that normally falls on land ends up in the ocean, which raises sea levels temporarily.”

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. Credit: NASA’s Scientific Visualization Studio

A Human Footprint

Seasonal or periodic climate phenomena can affect global average sea level from year to year. But the underlying trend for more than three decades has been increasing ocean heights as a direct response to global warming due to the excessive heat trapped by greenhouse gases in Earth’s atmosphere.

“Long-term datasets like this 30-year satellite record allow us to differentiate between short-term effects on sea level, like El Niño, and trends that let us know where sea level is heading,” said Ben Hamlington, lead for NASA’s sea level change team at JPL.

These multidecadal observations wouldn’t be possible without ongoing international cooperation, as well as scientific and technical innovations by NASA and other space agencies. Specifically, radar altimeters have helped produce ever-more precise measurements of sea level around the world. To calculate ocean height, these instruments bounce microwave signals off the sea surface, recording the time the signal takes to travel from a satellite to Earth and back, as well as the strength of the return signal.

The researchers also periodically cross-check those sea level measurements against data from other sources. These include tide gauges, as well as satellite measurements of factors like atmospheric water vapor and Earth’s gravity field that can affect the accuracy of sea level measurements. Using that information, the researchers recalibrated the 30-year dataset, resulting in updates to sea levels in some previous years. That includes a sea level rise increase of 0.08 inches (0.21 centimeters) from 2021 to 2022.

When researchers combine space-based altimetry data of the oceans with more than a century of observations from surface-based sources, such as tide gauges, the information dramatically improves our understanding of how sea surface height is changing on a global scale. When these sea level measurements are combined with other information, including ocean temperature, ice loss, and land motion, scientists can decipher why and how seas are rising.

Learn more about sea level and climate change:

https://sealevel.nasa.gov/

News Media Contacts

Jane J. Lee / Andrew Wang
Jet Propulsion Laboratory, Pasadena, Calif.
818-354-0307 / 626-379-6874
jane.j.lee@jpl.nasa.gov / andrew.wang@jpl.nasa.gov

2024-031

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Naomi Hartono

Soyuz MS-25 Launch Scrubbed

Soyuz MS-25 Launch Scrubbed

The Soyuz rocket is raised vertical Monday, March 18, 2024, at launch pad Site 31 of the Baikonur Cosmodrome in Kazakhstan. Credit: NASA/Bill Ingalls
The Soyuz rocket is raised vertical Monday, March 18, 2024, at launch pad Site 31 of the Baikonur Cosmodrome in Kazakhstan. Credit: NASA/Bill Ingalls

The March 21 launch of the crewed Soyuz-25 spacecraft to the International Space Station with NASA astronaut Tracy C. Dyson, Roscosmos cosmonaut Oleg Novitskiy, and spaceflight participant Marina Vasilevskaya of Belarus was scrubbed. The next available launch opportunity is Saturday, March 23. More information on the viability of that date is forthcoming, pending details on what caused today’s launch abort.


Learn more about station activities by following the space station blog, @space_station and @ISS_Research on X, as well as the ISS Facebook and ISS Instagram accounts.

Get weekly updates from NASA Johnson Space Center at: https://roundupreads.jsc.nasa.gov/

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Abby Graf