Swarming Proxima Centauri: Coherent Picospacecraft Swarms Over Interstellar Distances

Swarming Proxima Centauri: Coherent Picospacecraft Swarms Over Interstellar Distances

4 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Labeled diagram of the Swarming Proxima Centauri
Graphic depiction of Swarming Proxima Centauri: Coherent Picospacecraft Swarms Over Interstellar Distances
Thomas Eubanks

Thomas Eubanks
Space Initiatives, Inc.

Tiny gram-scale interstellar probes pushed by laser light are likely to be the only technology capable of reaching another star this century. We presuppose availability by mid-century of a laser beamer powerful enough (~100-GW) to boost a few grams to relativistic speed, lasersails robust enough to survive launch, and terrestrial light buckets (~1-sq.km) big enough to catch our optical signals. Then our proposed representative mission, around the third quarter of this century, is to fly by our nearest neighbor, the potentially habitable world Proxima b, with a large autonomous swarm of 1000s of tiny probes.

Given extreme constraints on launch mass (grams), onboard power (milliwatts), and coms aperture (centimeters to meters), our team determined in our work over the last 3 years that only a large swarm of many probes acting in unison can generate an optical signal strong enough to cross the immense distance back to Earth. The 8-year round-trip time lag eliminates any practical control by Earth, therefore the swarm must possess an extraordinary degree of autonomy, for example, in order to prioritize which data is returned to Earth. Thus, the reader will see that coordinating the swarming of individuals into an effective whole is the dominant challenge for our representative mission to Proxima Centauri b. Coordination in turn rests on establishing a mesh network via low-power optical links and synchronizing probes’ on-board clocks with Earth and with each other to support accurate position-navigation-timing (PNT).

Our representative mission begins with a long string of probes launched one at a time to ~0.2c. After launch, the drive laser is used for signaling and clock synchronization, providing a continual time signal like a metronome. Initial boost is modulated so the tail of the string catches up with the head (“time on target”). Exploiting drag imparted by the interstellar medium (“velocity on target”) over the 20-year cruise keeps the group together once assembled. An initial string 100s to 1000s of AU long dynamically coalesces itself over time into a lens-shaped mesh network #100,000 km across, sufficient to account for ephemeris errors at Proxima, ensuring at least some probes pass close to the target.

A swarm whose members are in known spatial positions relative to each other, having state-of-the-art microminiaturized clocks to keep synchrony, can utilize its entire population to communicate with Earth, periodically building up a single short but extremely bright contemporaneous laser pulse from all of them. Operational coherence means each probe sends the same data but adjusts its emission time according to its relative position, such that all pulses arrive simultaneously at the receiving arrays on Earth. This effectively multiplies the power from any one probe by the number N of probes in the swarm, providing orders of magnitude greater data return.

A swarm would tolerate significant attrition en route, mitigating the risk of “putting all your eggs in one basket,” and enabling close observation of Proxima b from multiple vantage points. Fortunately, we don’t have to wait until mid-century to make practical progress – we can explore and test swarming techniques now in a simulated environment, which is what we propose to do in this work. We anticipate our innovations would have a profound effect on space exploration, complementing existing techniques and enabling entirely new types of missions, for example picospacecraft swarms covering all of cislunar space, or instrumenting an entire planetary magnetosphere. Well before mid-century we foresee a number of such missions, starting in Earth or lunar orbit, but in time extending deep into the outer Solar system. For example, such a swarm could explore the rapidly receding interstellar object 1I/’Oumuamua or the solar gravitational lens. These would both be precursors to the ultimate interstellar mission, but also scientifically valuable in their own right.

2024 Phase I Selection

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Loura Hall

Detoxifying Mars: the biocatalytic elimination of omnipresent perchlorates

Detoxifying Mars: the biocatalytic elimination of omnipresent perchlorates

3 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Artist rendition of a bottle of H2O, Bioreactor and H2O with a planetary surface in the background.
Graphic depiction of Detoxifying Mars: the biocatalytic elimination of omnipresent perchlorates
Lynn Rothschild

Lynn Rothschild
NASA Ames Research Center (ARC)

Water is the lifeblood of human survival and civilization and is critical for our sustained exploration beyond Earth. Fortunately, Mars has plenty of water to sustain our aspirations in the form of subsurface ice. Unfortunately, it is not clean water – it is contaminated by toxic perchlorates. Perchlorate and chlorate are potent oxidizers that cause equipment corrosion and are hazardous to human health even at low concentrations. It is therefore critical that Martian water be detoxified to remove these contaminating solutes before it can be used in propellant production, food production, or human consumption. The scale of anticipated water demand on Mars highlights the shortcomings of traditional water purification approaches, which require either large amounts of consumable materials, high electrical draw, or water pretreatment.

What if we could make the perchlorates just vanish? This is the innovative solution we propose here, taking advantage of the reduction of chlorate and perchlorate to chloride and oxygen being thermodynamically favorable, if kinetically slow. This is the promise of our regenerative perchlorate reduction system, leveraging synthetic biology to take advantage of and improve upon natural perchlorate reducing bacteria. These terrestrial microbes are not directly suitable for off-world use, but their key genes pcrAB and cld, which catalyze the reduction of perchlorates to chloride and oxygen, have been previously identified and well-studied. This proposed work exploits the prior work studying perchlorate-reducing bacteria by engineering this perchlorate reduction pathway into the spaceflight proven Bacillus subtilis strain 168, under the control of a robust, active promoter. This solution is highly sustainable and scalable, and unlike traditional water purification approaches, outright eliminates perchlorates rather than filtering them to dump somewhere nearby.

For Phase I we will explore whether this approach is feasible through these objectives:

  1. Engineer the genes PcrAB and cld into B. subtilis 168 under the control of the strong promoter pVeg and test and quantify the efficacy of perchlorate reduction under the modeled conditions.
  2. Develop B. subtilis strains that secrete the enzymes to test intra- vs extracellular efficacy.
  3. Perform a trade study comparing the performance of biological water detoxification from Objs. 1 & 2 to traditional engineering approaches in terms of mass, power, and crew time.
  4. Delineate a plan to infuse this technology in human Mars missions. Development of our detoxification biotechnology will also lead to more efficient solutions to natural and particularly industrial terrestrial perchlorate contamination on Earth. It will also shine a spotlight on the potential of using life rather than only industrial solutions to address our environmental problems, which may spur further innovations for other terrestrial environmental challenges such as climate change. The system will be launched as inert, dried spores stable at room temperature for years. Upon arrival at Mars, spores will be rehydrated and grown in a bioreactor that meets planetary protection standards. Martian water will be processed by the bioreactor to accomplish perchlorate reduction. Processed water can then be used or further purified as required.

2024 Phase I Selection

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Loura Hall

Add-on to Large-Scale Water Mining Operations on Mars to Screen for Introduced and Alien Life

Add-on to Large-Scale Water Mining Operations on Mars to Screen for Introduced and Alien Life

4 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Artist rendition of labled Water mining ISRU missins on a lunar surface.
Graphic depiction of Add-on to large-scale water mining operations on Mars to screen for introduced and alien life
Steven Benner

Steven Benner
Foundation For Applied Molecular Evolution

As noted at NASA’s 2019 Carlsbad Conference we have good reason to think that:

  • Life started on Mars using the same geo-organic chemistry that started life on Earth.
  • Martian life persists today on Mars, in near-surface ice, low elevations, and caves, all with transient liquid brines, environments that today on Earth host microbial life.
  • Martian life must use informational polymers (like DNA); Darwinian evolution requires these, and Darwinian evolution is the only way matter can organize to give life.
  • While Martian “DNA” may differ (possibly radically) in its chemistry from Terran DNA, the “Polyelectrolyte Theory of the Gene” limits the universe of possible alien DNA structures.
  • Those structures ensure that Martian DNA can be concentrated from Martian water, even if very highly diluted, and even if Martian “DNA” differs from Earth DNA.
  • On Mars as it exists today, information polymers cannot be generated without life (unlike other less reliable biosignatures such as methane), ensuring that life will not be “detected” if it is not present (the “false positive problem”). Nevertheless, as noted by Rummel and Conley, “the Mars community is not convinced that a mission to attempt detection of extant Martian life has a high priority.” Thus, NASA’s current flagship mission to Mars, derived from its 2012 Decadal Survey, involves pedestrian collection of old dry rocks to be cached, eventually to be returned to Earth to study for evidence of past life.

The purpose of this NIAC project is to change this view, and to do so before human arrival planned by NASA, the Chinese National Space Agency, and SpaceX, “by 2040”, “in 2033”, and “before 2030”, according to their respective statements. Human arrival will undoubtedly complicate the search for indigenous Martian life. Thus, from an astrobiological perspective, these planned crewed missions to Mars put a very strict deadline on the search for life on a pristine Mars. However, crewed missions also offer an opportunity that we will exploit. Crewed missions to Mars will use materials found on Mars itself, “in situ”, in particular, near surface water ice. Propellant (methane and oxygen) will be generated from that water and

atmospheric carbon dioxide for the return trip back to Earth. That water ice will be mined on the scale of tens to hundred tons. Further, to maximize the likelihood of safe return of the crew to Earth, robotic operations that mine tons of near surface water-ice will be in place before the first human astronauts arrive. Thus, water mined in preparation for human arrival is correctly seen as an extremely large-scale astrobiological sample, far larger than dry cached rocks. As the mined water-ice is delivered with dust that, through dust storms, survey the entire accessible surface, this humongous sample will effectively enable a highly sensitive survey of the entire accessible Mars surface for life. This NIAC project will provide an “agnostic life finding” (ALF) system capable of extracting genetic polymers (DNA or alien) from

these large ISRU water samples. ALF is agnostic because it exploits what synthetic biology taught us about the limited kinds of Darwinian genetic molecules. ALF also offers tools to partly analyze the polyelectrolytes in situ.

As an add-on system, ALF creates a negligible additional burden (regarding mass and energy consumption) compared to the investment in the water mining operation at this scale. Although small and low cost, this instrument will allow science to place a severe lower limit on the amount of biosphere on the accessible Martian surface. And it will do so before Homo sapiens becomes a multiplanetary species. And “multiplanetary” is the correct term. This add-on ALF system can be used on all celestial bodies where water will be mined to search for and analyze life, indigenous or introduced, Earth-like or alien. This includes Europa, Enceladus, the Moon, and exotic locales on Earth.

2024 Phase I Selection

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Loura Hall

Mars Aerial and Ground Global Intelligent Explorer (MAGGIE)

Mars Aerial and Ground Global Intelligent Explorer (MAGGIE)

2 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

Artist rendition of MAGGIE above a planetary surface
Graphic depiction of Mars Aerial and Ground Global Intelligent Explorer (MAGGIE)
Ge-Cheng Zha

Ge-Cheng Zha
Coflow Jet, LLC

We propose to develop a novel global mobility Mars exploration platform , Mars Aerial and Ground Intelligent Explorer (MAGGIE). MAGGIE is a compact fixed wing aircraft with ultra-high productivity efficiency powered by solar energy to fly in the Martian atmosphere with vertical take-off/landing (VTOL) capability, which is enabled by advanced deflected slipstream technology with CoFlow Jet (CFJ). The cruise Mach number of MAGGIE is 0.25 with a cruise lift coefficient CL of 3.5, nearly an order of magnitude higher than conventional subsonic aircraft to overcome the low density of the Martian atmosphere. The ultra-high cruise CL with CL/CDc of 9 is made possible by CFJ that overcomes the low Reynolds number effect on Mars. The range of MAGGIE for a fully charged battery per 7.6 sol is 179 km at altitude of 1,000 m. The total range of MAGGIE per Martian year is 16,048 km. The representative mission for MAGGIE presented would conduct three atmospheric and geophysical investigations, all supporting different timescales of the Dynamic Mars science theme. These include a study of the origin and timing of the Martian core dynamo from the weak magnetic fields found in the large impact basins, a regional investigation of the source of methane signals detected by the Tunable Laser Spectrometer on the Mars Science Laboratory in Gale crater, and mapping of subsurface water ice at high resolution in the mid-latitudes where it has been observed from orbit. The conceptual MAGGIE system study indicates that the concept appears to be feasible, but need to be further investigated, designed, and verified under Martian atmospheric conditions in Phase I. MAGGIE would be able to perform the first global-scale atmospheric mission at Mars and revolutionize our capability of exploring almost the entirety of the Martian surface. It is the first concept to enable ongoing exploration of this region of Mars and would provide a substantial leap in capability for NASA’s exploration of the Red Planet. The attractiveness of airborne missions on Mars has been amply demonstrated by the Ingenuity helicopter. MAGGIE would be similarly engaging to the public, both in its audacity, and in the variety of environments it could explore, study, and image. The technology would also enhance VTOL aircraft technology on Earth and other planets.

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Loura Hall

NASA’s Hubble Observes Exoplanet Atmosphere Changing Over 3 Years

NASA’s Hubble Observes Exoplanet Atmosphere Changing Over 3 Years

4 min read

NASA’s Hubble Observes Exoplanet Atmosphere Changing Over 3 Years

By combining several years of observations from NASA’s Hubble Space Telescope along with conducting computer modelling, astronomers have found evidence for massive cyclones and other dynamic weather activity swirling on a hot, Jupiter-sized planet 880 light-years away.

The planet, called WASP-121 b, is not habitable. But this result is an important early step in studying weather patterns on distant worlds, and perhaps eventually finding potentially habitable exoplanets with stable, long-term climates.

A large, yellow-white star fills the center of the image. A
This is an artist’s concept of the exoplanet WASP-121 b, also known as Tylos. The exoplanet’s appearance is based on Hubble simulation data of the object. Using Hubble observations, another team of scientists had previously reported the detection of heavy metals such as magnesium and iron escaping from the upper atmosphere of the ultra-hot Jupiter exoplanet; marking it as the first of such detection. The exoplanet is orbiting dangerously close to its host star, roughly 2.6% of the distance of Earth to the Sun, placing it on the verge of being ripped apart by the star’s tidal forces. The powerful gravitational forces have altered the planet’s shape.

An international team of astronomers assembled and reprocessed Hubble observations of the exoplanet in the years 2016, 2018 and 2019. This provided them with a unique data-set that allowed them to not only analyze the atmosphere of WASP-121 b, but also to compare the state of the exoplanet’s atmosphere across several years. They found clear evidence that the observations of WASP-121 b were varying in time. The team then used sophisticated modelling techniques to demonstrate that these temporal variations could be explained by weather patterns in the exoplanet’s atmosphere.

NASA, ESA, Quentin Changeat (ESA/STScI), Mahdi Zamani (ESA/Hubble)

For the past few decades, detailed telescopic and spacecraft observations of neighboring planets in our solar system show that their turbulent atmospheres are not static but constantly changing, just like weather on Earth. This variability should also apply to planets around other stars, too. But it takes lots of detailed observing and computational modelling to actually measure such changes.

To make the discovery, an international team of astronomers assembled and reprocessed Hubble observations of WASP-121 b taken in 2016, 2018, and 2019.

They found that the planet has a dynamic atmosphere, changing over time. The team used sophisticated modelling techniques to demonstrate that these dramatic temporal variations could be explained by weather patterns in the exoplanet’s atmosphere.

The team found that WASP-121 b’s atmosphere shows notable differences between observations. Most dramatically, there could be massive weather fronts, storms, and massive cyclones that are repeatedly created and destroyed due to the large temperature difference between the star-facing side and dark side of the exoplanet. They also detected an apparent offset between the exoplanet’s hottest region and the point on the planet closest to the star, as well as variability in the chemical composition of the exoplanet’s atmosphere (as measured via spectroscopy).

The team reached these conclusions by using computational models to help explain observed changes in the exoplanet’s atmosphere. “The remarkable details of our exoplanet atmosphere simulations allows us to accurately model the weather on ultra-hot planets like WASP-121 b,” explained Jack Skinner, a postdoctoral fellow at the California Institute of Technology in Pasadena, California, and co-leader of this study. “Here we make a significant step forward by combining observational constraints with atmosphere simulations to understand the time-varying weather on these planets.”


This visualization shows the temperature forecast spanning 130 exoplanet-days, across sunrise, noon, sunset, and midnight for the exoplanet WASP-121 b, also known as Tylos. The brighter yellow regions depict areas in the day side of the exoplanet where temperatures soar well above 2,100 degrees Kelvin (3,320 degrees Fahrenheit); due to the close proximity to its host star, roughly 2.6% of the distance of Earth to the Sun. Due to the extreme temperature difference between the day and night sides, astronomers suspect evaporated iron and other heavy metals escaping into the higher layers of atmosphere on the day side partially fall back onto lower layers, making it rain iron at night. Some of the heavy metals also escape the planet’s gravity from the upper atmosphere.

It only takes WASP-121 b roughly 31 hours to complete an orbit around its star.

An international team of astronomers assembled and reprocessed Hubble observations of the exoplanet in the years 2016, 2018, and 2019. This provided them with a unique data-set that allowed them to not only analyze the atmosphere of WASP-121 b, but also to compare the state of the exoplanet’s atmosphere across several years. They found clear evidence that the observations of WASP-121 b were varying in time. The team then used sophisticated modelling techniques to demonstrate that these temporal variations could be explained by weather patterns in the exoplanet’s atmosphere, as seen here.

The international team of astronomers in this study consists of: Q. Changeat (European Space Agency (ESA), Space Telescope Science Institute (STScI), University College London); J.W. Skinner (California Institute of Technology, Brandeis University); J. Y-K. Cho, (Brandeis University, Center for Computational Astrophysics/Flatiron Institute); J. Nättilä (Center for Computational Astrophysics/ Flatiron Institute, Columbia University); I.P. Waldmann (University College London); A.F. Al-Refaie (University College London); A. Dyrek (Université Paris Cité, Université Paris-Saclay); B. Edwards (Netherlands Institute for Space Research, University College London); T. Mikal-Evans (Max Planck Institute for Astronomy); M. Joshua (Blue Skies Space Ltd.); G. Morello (Chalmers University of Technology, Instituto de Astrofísica de Canarias); N. Skaf (National Astronomical Observatory of Japan, Université de Paris, University College London); A. Tsiaras (University College London); O. Venot (Université de Paris Cité, Université Paris Est Creteil); and K.H. Yip (University College London). Credit: NASA, ESA, Quentin Changeat (ESA/STScI), Mahdi Zamani (ESA/Hubble)

“This is a hugely exciting result as we move forward for observing weather patterns on exoplanets,” said one of the principal investigators of the team, Quentin Changeat, a European Space Agency Research Fellow at the Space Telescope Science Institute in Baltimore, Maryland. “Studying exoplanets’ weather is vital to understanding the complexity of exoplanet atmospheres on other worlds, especially in the search for exoplanets with habitable conditions.”

WASP-121 b is so close to its parent star that the orbital period is only 1.27 days. This close proximity means that the planet is tidally locked so that the same hemisphere always faces the star, in the same way that our Moon always has the same side pointed at Earth. Daytime temperatures approach 3,450 degrees Fahrenheit (2,150 degrees Kelvin) on the star-facing side of the planet.

The team used four sets of Hubble archival observations of WASP-121 b. The complete data-set included observations of WASP-121 b transiting in front of its star (taken in June 2016); WASP-121 b passing behind its star, also known as a secondary eclipse (taken in November 2016); and the brightness of WASP-121 b as a function of its phase angle to the star (the varying amount of light received at Earth from an exoplanet as it orbits its parent star, similar to our Moon’s phase-cycle). These data were taken in March 2018 and February 2019, respectively.

“The assembled data-set represents a significant amount of observing time for a single planet and is currently the only consistent set of such repeated observations,” said Changeat. The information that we extracted from those observations was used to infer the chemistry, temperature, and clouds of the atmosphere of WASP-121 b at different times. This provided us with an exquisite picture of the planet changing over time.”

Hubble’s capabilities also are evident in the broad expanse of science programs it will enable through its Cycle 31 observations, which began on December 1. About two-thirds of Hubble’s time will be devoted to imaging studies, while the remainder is allotted to spectroscopy studies, like those used for WASP-121 b. More details about Cycle 31 science are in a recent announcement.


This visualization shows the weather patterns on the exoplanet WASP-121 b, also known as Tylos. This video has been slowed to observe the patterns in the exoplanet’s atmosphere in closer detail.

An international team of astronomers assembled and reprocessed Hubble observations of the exoplanet in the years 2016, 2018, and 2019. This provided them with a unique data-set that allowed them to not only analyze the atmosphere of WASP-121 b, but also to compare the state of the exoplanet’s atmosphere across several years. They found clear evidence that the observations of WASP-121 b were varying in time. The team then used sophisticated modelling techniques to demonstrate that these temporal variations could be explained by weather patterns in the exoplanet’s atmosphere, as seen here.

The science team’s models found that their results could be explained by quasi-periodic weather patterns: specifically, massive cyclones that are repeatedly created and destroyed due to the huge temperature difference between the star-facing and dark side of the exoplanet. This result represents a significant step forward in potentially observing weather patterns on exoplanets.

The international team of astronomers in this study consists of: Q. Changeat (European Space Agency (ESA), Space Telescope Science Institute (STScI), University College London); J.W. Skinner (California Institute of Technology, Brandeis University); J. Y-K. Cho, (Brandeis University, Center for Computational Astrophysics/Flatiron Institute); J. Nättilä (Center for Computational Astrophysics/ Flatiron Institute, Columbia University); I.P. Waldmann (University College London); A.F. Al-Refaie (University College London); A. Dyrek (Université Paris Cité, Université Paris-Saclay); B. Edwards (Netherlands Institute for Space Research, University College London); T. Mikal-Evans (Max Planck Institute for Astronomy); M. Joshua (Blue Skies Space Ltd.); G. Morello (Chalmers University of Technology, Instituto de Astrofísica de Canarias); N. Skaf (National Astronomical Observatory of Japan, Université de Paris, University College London); A. Tsiaras (University College London); O. Venot (Université de Paris Cité, Université Paris Est Creteil); and K.H. Yip (University College London). Credit: NASA, ESA, Quentin Changeat (ESA/STScI), Mahdi Zamani (ESA/Hubble)

LEARN MORE:

The Hubble Space Telescope is a project of international cooperation between NASA and ESA. NASA’s Goddard Space Flight Center in Greenbelt, Maryland, manages the telescope. The Space Telescope Science Institute (STScI) in Baltimore, Maryland, conducts Hubble and Webb science operations. STScI is operated for NASA by the Association of Universities for Research in Astronomy, in Washington, D.C.

Media Contacts:

Claire Andreoli
NASA’s Goddard Space Flight CenterGreenbelt, MD
claire.andreoli@nasa.gov

Ray Villard
Space Telescope Science Institute, Baltimore, MD

Bethany Downer
ESA/Hubble

Science Contact:

Quentin Changeat
ESA/STScI

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Last Updated
Jan 04, 2024
Editor
Andrea Gianopoulos
Location
Goddard Space Flight Center

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