OrbitalHub

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NASA’s ESCAPADE mission—short for Escape and Plasma Acceleration and Dynamics Explorers—marks a bold step into understanding how the solar wind has shaped Mars’ atmospheric history. Unlike any single-satellite mission before it, ESCAPADE sends two identical spacecraft—nicknamed “Blue” and “Gold”—into orbit around Mars to explore, in stereo, the Red Planet’s magnetic environment and the processes that drive its atmospheric loss.

The mission is part of NASA’s SIMPLEx (Small Innovative Missions for Planetary Exploration) program and is managed by the Space Sciences Laboratory at the University of California, Berkeley, with strong participation from Rocket Lab, NASA Goddard, Embry-Riddle Aeronautical University, and Advanced Space LLC. Because Mars has a weak, patchy magnetosphere—thanks to remnant crustal magnetic fields rather than a global magnetic core—ESCAPADE’s twin spacecraft will give scientists a detailed look at how this hybrid field interacts with solar wind particles and channels energy, momentum, and plasma.

ESCAPADE is set to launch aboard Blue Origin’s New Glenn rocket, using a somewhat unconventional trajectory. Rather than launching directly to Mars in a typical Hohmann transfer, the mission will first travel into a “loiter” orbit around Earth–Sun Lagrange Point 2, nearly a million miles from Earth, before looping back and using a gravity assist to reach Mars. This maneuver provides flexibility in launch windows and also gives the spacecraft a chance to observe Earth’s own magnetotail during the early phase of the mission.

Once the two spacecraft arrive at Mars—expected around September 2027 after roughly an 11-month cruise—they will perform orbit insertion maneuvers, first settling into large “capture” orbits and then transitioning to science orbits over time. By mid-2028, ESCAPADE will begin its primary science operations in two distinct phases. The first, called Campaign A, places both spacecraft in nearly identical “string-of-pearls” orbits, with one trailing the other in tight formation. This configuration allows them to take nearly simultaneous measurements of how solar wind conditions change across time and space around Mars.

Then, in Campaign B, the Blue and Gold spacecraft will diverge onto separate orbits—one closer to Mars, the other further out—to sample different regions of the planet’s space environment. This dual-perspective approach promises to disentangle how particles flow in and out of the Martian magnetosphere, how energy and momentum are transported, and the specific mechanisms that drive atmospheric loss. Along the way, ESCAPADE will collect key data not only on ions and electrons but also on plasma density and magnetic fields, giving a 3D picture of Martian space weather in action.

At the heart of each spacecraft are three science instruments: a magnetometer (built at NASA Goddard) mounted on a two-meter boom to measure local magnetic fields; an electrostatic analyzer to detect and characterize particles like ions and electrons; and a Langmuir probe developed by Embry-Riddle to measure plasma density and solar extreme-ultraviolet (EUV) flux. Each spacecraft also has deployable solar arrays—about 4.9 meters wide when extended—to power its systems, which use roughly as much energy as a household kettle.

ESCAPADE isn’t just a science mission—it’s a strategic one. By studying how the solar wind interacts with Mars in real time, the mission addresses fundamental questions about how the planet’s atmosphere has thinned over billions of years. Understanding this process not only informs our knowledge of Mars’ climate history, but also helps future missions—especially crewed missions—anticipate the space weather environment they’ll face.

The dual-spacecraft design is especially powerful: it allows scientists to compare simultaneous observations, capturing the rapid, dynamic dance of particles and fields as they change. This stereo view of Mars’ magnetosphere is something no previous mission has achieved, and it could shed light on how energy and matter escape from Mars in different regions and under different conditions.

Finally, ESCAPADE demonstrates the increasing capability of small missions to carry out high-impact planetary science. Even though each spacecraft is relatively compact—about 209 kg dry, 535 kg fueled—they carry sophisticated instruments and operate in deep space, thanks to partnerships with commercial launch providers (Blue Origin) and spacecraft manufacturers (Rocket Lab). This makes ESCAPADE a model for future low-cost, high-value exploration missions.

Video credit: NASA

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When NASA’s Space Launch System (SLS) powers into the sky, it must contend with some of the most extreme and complex aerodynamic conditions ever attempted. The ascent phase—especially during transonic and supersonic transitions and through maximum aerodynamic stress—is a crucible for design and engineering. Rather than rely solely on wind tunnels, NASA has increasingly turned to supercomputer-based computational fluid dynamics (CFD) simulations to model the flows around the twin solid rocket boosters, the core stage, and plume interactions. These simulations feed into aerodynamic databases used across vehicle design, structural loads, control algorithms, and safety margins.

The challenge in modeling the flow around SLS boosters is immense. As the vehicle accelerates, shock waves form, flow separation regions emerge, boundary layers evolve, and the rocket plumes themselves strongly interact with the surrounding airstream. Moreover, during events like booster separation, multiple plumes fire simultaneously—up to 22 different exhaust sources in some analyses, combining output from the core engines, boosters, and separation motors. Resolving those off-body interactions, transient flow features, and the coupling between vehicle aerodynamics and plume dynamics demands very high fidelity simulations. The NASA team has used solvers such as OVERFLOW, FUN3D, and Cart3D to explore a wide envelope of flight conditions.

Running these simulations requires massive computational resources. Each case can consume thousands to tens of thousands of core-hours, depending on flow complexity, grid resolution, and the number of interacting plumes. To build a full aerodynamic database that spans multiple Mach numbers, angles of attack, mass fractions, and thrust conditions, NASA runs hundreds to thousands of individual cases. The supercomputers at the NASA Advanced Supercomputing (NAS) facility, including Pleiades, Electra, and others, serve as the backbone of these efforts. Through careful meshing strategies, solver optimizations, and parallel computing techniques, engineers map out pressure distributions, shear stresses, and load profiles for every relevant component of the booster-core assembly.

These simulation results are not academic exercises—they directly inform the safety and performance of SLS missions. The aerodynamics databases are used by structural engineers to assess bending loads, by guidance and control teams to refine trajectory models, and by separation system designers to ensure that boosters detach cleanly without risking collision with the core. When flight data come in, the models themselves can be validated and refined, closing the loop between simulation and real world performance. As SLS evolves—especially with future variants and heavier payloads—the simulation infrastructure will scale accordingly, enabling continuous improvements in confidence, margin, and mission success.

Video credit: NASA/NAS/Gerrit-Daniel Stich, Michael Barad, Timothy Sandstrom, Derek Dalle

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Launched on April 15, 1999, from Vandenberg Air Force Base in California aboard a Delta II rocket, Landsat 7 marked a new chapter in Earth observation. This satellite, a collaborative endeavor between NASA, the U.S. Geological Survey (USGS), and NOAA, was the seventh in the long-running Landsat program that began in 1972. With a sun-synchronous, near-polar orbit at an altitude of approximately 705 kilometers, Landsat 7 was designed to pass over the same part of the Earth every 16 days, capturing high-resolution imagery under consistent lighting conditions at around 10:00 a.m. local solar time.

The spacecraft itself was engineered by Lockheed Martin and featured a three-axis stabilized platform, which allowed precise orientation in space. It drew power from solar arrays supported by nickel-cadmium batteries and used a hydrazine monopropellant system for orbital maintenance. One of its significant upgrades over previous Landsat missions was the inclusion of a solid-state data recorder capable of storing roughly 378 gigabits of data. This feature allowed the satellite to store imagery until it could downlink it to a ground station, enabling more flexible operations and broader global coverage.

At the heart of Landsat 7’s success was its sole scientific instrument: the Enhanced Thematic Mapper Plus (ETM+). This powerful sensor was a “whisk-broom” scanner, capturing data across eight spectral bands. Six of these bands covered the visible, near-infrared, and shortwave infrared portions of the electromagnetic spectrum with a resolution of 30 meters. A thermal infrared band operated at 60 meters resolution, while a high-resolution panchromatic band offered detail at 15 meters. Each scene covered an area of roughly 183 by 170 kilometers.

One of ETM+’s distinguishing features was its rigorous calibration. Equipped with a full-aperture solar calibrator and internal lamps, ETM+ maintained its radiometric accuracy to within five percent. This exceptional calibration made it the gold standard for satellite remote sensing, enabling cross-calibration with other Earth-observing missions such as NASA’s Terra and EO-1 satellites.

However, Landsat 7’s mission was not without challenges. On May 31, 2003, the satellite’s scan line corrector (SLC)—a mechanism that compensated for the motion of the satellite to ensure complete image coverage—failed. This hardware malfunction introduced zigzag-shaped data gaps that affected roughly 22 to 30 percent of each image. Despite the setback, Landsat 7 continued to operate, and the data it captured remained valuable. Scientists developed methods to fill in the gaps using data from adjacent passes, allowing continued scientific use and analysis.

Originally designed for a five-year mission, Landsat 7 exceeded expectations by remaining active for over two decades. In 2017, the final station-keeping maneuvers were performed to maintain the satellite’s orbital parameters. As fuel levels dropped, the satellite’s orbit began to drift slightly, but its imaging capabilities remained intact. In April 2022, the satellite was placed in a lower orbit to support calibration of other Earth-observing systems, and it continued to acquire data intermittently until January 2024. On June 4, 2025, the mission officially came to an end.

Throughout its operational life, Landsat 7 played a vital role in Earth sciences. It provided consistent, high-resolution imagery that supported a wide range of applications, including environmental monitoring, land use planning, disaster response, water resource management, agriculture, and climate change research. The data collected were used in studies that tracked deforestation in the Amazon, urban sprawl in North America, and agricultural patterns in sub-Saharan Africa, among countless other projects.

One of Landsat 7’s most transformative impacts came in 2008, when USGS made its entire Landsat archive—including Landsat 7 data—available to the public at no cost. This decision revolutionized the field of remote sensing, opening the doors to researchers, educators, governments, and businesses worldwide. The number of Landsat scene downloads skyrocketed, leading to an explosion in published scientific studies and practical applications.

Beyond its imagery, Landsat 7 served as a radiometric benchmark. Its ETM+ sensor was so well-calibrated that it became a reference instrument, helping to ensure consistency and accuracy across other satellite missions. This legacy continued with Landsat 8, launched in 2013, and Landsat 9, which entered service in 2021. Even in its final years, Landsat 7 contributed to efforts to standardize Earth observation through proposed servicing missions and calibration support.

Landsat 7’s mission may have ended, but its legacy endures. For over 20 years, it provided humanity with a clearer picture of our changing planet, setting new standards in satellite imaging and democratizing access to Earth observation data. As scientists and decision-makers confront the challenges of climate change, food security, and sustainable development, the insights first captured by Landsat 7 continue to inform policy and shape our understanding of the world.

Video credit: NASA Goddard

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NASA’s Lucy mission, launched on October 16, 2021, is the first space mission specifically designed to study the Trojan asteroids, a unique group of asteroids that orbit the Sun in two large swarms around Jupiter—one leading and one trailing the gas giant. These celestial bodies are believed to be remnants from the early solar system, offering valuable clues about the formation of the planets. Named after the fossilized human ancestor “Lucy,” whose discovery shed light on human evolution, this spacecraft similarly seeks to uncover the ancient history of the solar system.

The Lucy mission has four primary scientific goals:

Surface Geology – Analyze surface features to determine the history of cratering, layering, and possible past activity like volcanism.

Surface Composition – Identify the composition of the asteroids’ surfaces to infer the origins of their materials.

Interior and Bulk Properties – Measure mass, density, and structure of each asteroid to understand their internal makeup.

Satellites and Rings – Search for small moons and ring systems, which may help scientists understand how Trojan asteroids have evolved.

By studying these diverse objects, Lucy is expected to provide insights into planetary formation processes and the dynamics of the early solar system.

Lucy’s mission trajectory is one of the most complex ever attempted. It involves multiple gravity assists and a looping journey through the inner solar system to reach different groups of Trojan asteroids. After launching from Cape Canaveral aboard an Atlas V rocket, Lucy began a 12-year journey involving three Earth gravity assists:

First Earth flyby: October 2022

Second Earth flyby: December 2024

Third Earth flyby: December 2030

These assists help shape Lucy’s path to visit eight asteroids in total—a record for a single NASA mission. These include:

Donaldjohanson (Main Belt asteroid, 2025) – Named after the discoverer of the Lucy hominid fossil.

Eurybates and its satellite Queta (leading Trojan swarm, 2027)

Polymele (2027)

Leucus (2028)

Orus (2028)

Patroclus and Menoetius (binary pair in the trailing Trojan swarm, 2033)

The spacecraft’s ability to fly by both leading and trailing Trojan camps is made possible by its unique and precisely calculated orbit, using Earth’s gravity to slingshot itself across vast distances.

To fulfill its objectives, Lucy is equipped with a suite of three main science instruments:

L’LORRI (Lucy LOng Range Reconnaissance Imager): A high-resolution telescopic camera designed to capture detailed images of the surface features of the Trojan asteroids, similar to what New Horizons used for Pluto.

L’Ralph: This instrument includes both a color visible camera and an infrared spectrometer to analyze surface composition and detect ices, organics, and minerals.

L’TES (Lucy Thermal Emission Spectrometer): Measures the heat emitted from asteroid surfaces, helping scientists estimate the texture and composition of the materials.

In addition to these, Lucy uses a high-gain antenna and radio tracking to precisely measure the gravitational tug of the asteroids during flybys—key for calculating mass and internal structure.

The mission timeline is as follows:

Launch: October 16, 2021

Earth Flyby 1: October 2022 (completed successfully)

Main Belt asteroid Donaldjohanson flyby: April 2025

Trojan flybys (Eurybates, Queta, Polymele, Leucus, Orus): 2027–2028

Return to Earth for gravity assist: December 2030

Patroclus and Menoetius (binary system) flyby: March 2033

End of Primary Mission: Late 2033 (though the spacecraft may continue as an extended mission platform depending on health and power)

NASA’s Lucy mission is a bold and pioneering effort to study some of the oldest and most distant relics of our solar system. Through its ambitious trajectory and carefully selected instruments, Lucy will give scientists an unprecedented look into the origins and evolution of our planetary neighborhood. By exploring a diverse array of Trojan asteroids—each with its own unique story—Lucy stands to revolutionize our understanding of how the planets formed and why our solar system looks the way it does today.

Video credit: NASA Goddard

Komatsu dicit:

Here is a sneak peak of Komatsu on the moon. At the dawn of space exploration, Komatsu is taking on a challenge to develop a machine whose line of job is construction on the moon! The study of lunar construction equipment utilises the results of research and development commissioned by the Project for Promoting the Development of Innovative Technologies for Outer Space Autonomous Construction (A Japanese government project lead-managed by MLIT with the collaboration of MEXT).

Video credit: Komatsu

Sierra Space dicit:

We have successfully completed our sixth stress test and fourth Ultimate Burst Pressure (UBP) test for our LIFE® 10 commercial space station technology, achieving a rupture at 255 psi, the highest pressure yet. This test exceeded NASA’s Factor of Safety recommendations, demonstrating a safety factor greater than 16x in Low Earth Orbit (LEO) and 23x in lunar environments. Our team continues to lead in the development of expandable structures for various space applications, as we build the world’s first commercial space station.

Video credit: Sierra Space