ORION LUNAR PERILUNE: 7,440 KM | VELOCITY: 1.48 KM/S
LAT: 20.4° S LON: 128.9° E
TARGET: Tsiolkovsky Basin
ALBEDO RATIO: 0.138 (Mare Basalt)
Hover or drag across lunar surface to survey coordinates
CH-04 Lunar Far-Side Perilune Observation Log 521m Archive
"Houston, Orion. The contrast across Tsiolkovsky is striking—the central peak rises dramatically from the dark mare floor. Anorthositic highlands are much brighter than Apollo photographs suggested."
00:14 / 01:45
Preliminary Science Catalog (Curated Observations)
Record ID MET (Hrs) Target Feature Instrument Coordinates Science Payload / Key Finding Status
Ready. Select an observation or toggle spectral bands to view.

Understanding the Artemis II Lunar Science Data Drop

NASA's publication of 814GB of preliminary science observations represents the first human-crewed translunar data suite returned since Apollo 17 in 1972. Incorporating 984 calibrated high-resolution multispectral frames, 521 minutes of crew voice commentary, and continuous intra-vehicular active dosimeter logs, this dataset establishes the geological and radiological baseline for the Artemis III lunar south polar landing.

1. Multispectral Bands and Far-Side Geological Stratigraphy

During the free-return trajectory, the Orion spacecraft attained a perilune altitude of approximately 7,440 kilometers above the lunar far side. Unlike automated orbiters (such as the Lunar Reconnaissance Orbiter or Clementine), the Artemis II optical survey leveraged hand-held and externally mounted multispectral sensors paired with real-time crew target acquisition.

True Color (400–700 nm)

Reconstructed photometrically to match human eye retinal sensitivity at perilune, resolving sub-kilometer albedo variations across the highland impact melts and crater rims.

Near-Infrared Pyroxene Map (750–950 nm)

Isolates the 1.0 μm ferrous iron (Fe²⁺) absorption band in silicate minerals, distinguishing pristine anorthosite massifs from low-calcium pyroxene impact ejecta.

UV/Visible Ratio (320/415 nm)

Direct proxy for titanium dioxide (TiO₂) and ilmenite abundance in lunar mare basalts, aiding resource characterization for future in-situ propellant production.

2. Active Radiological Dosimetry: Van Allen Belts to Cislunar Space

A central scientific milestone of Artemis II is the comprehensive radiation telemetry captured by the Hybrid Electronic Radiation Assessor (HERA) and crew personal dosimeters. The mission traversed both the inner proton belt and outer electron radiation belts during trans-lunar injection (TLI), providing the first real-time bio-dosimetry on a human lunar crew inside the Orion radiation shelter configuration.

The recorded maximum cumulative dosage remained well below mission threshold constraints, demonstrating the shielding efficacy of the Orion water stowage transfer bags positioned against the cabin bulkhead during solar particle event (SPE) drills.

Frequently Asked Inquiries

Why does Artemis II carry scientific payloads if it does not land?
Artemis II is primarily a crewed flight test of Orion's environmental control and life support systems (ECLSS), but its trajectory offers a rare vantage point: high-phase-angle multispectral imaging of far-side craters like Tsiolkovsky and high-altitude space weather dosimetry outside Earth's protective magnetosphere.
How is crew voice audio utilized for planetary science?
Astronaut geological descriptions provide instantaneous qualitative ground-truth for feature illumination, color differentiation, and boulder field dispersion that automated sensors may compress or overexpose. Audio transcripts are time-synchronized with optical timestamps.
Can independent researchers access the full 814GB raw dataset?
Yes. The data drop is hosted via NASA's Planetary Data System (PDS) and the Artemis Preliminary Lunar Science Report portal, with full CDF (Common Data Format), FITS, and uncompressed WAV audio packages available for peer-reviewed research.