PRODUCT_ID large_stringclasses 6
values | ROW int64 4.9k 37.2k | COL int64 1.15k 6.31k | LTM_CODE large_stringclasses 6
values | NAC_TILE large_stringclasses 6
values | NAC_FRACTION_NULL float64 | DTM_3M_TILE large_stringclasses 6
values | DTM_3M_FRACTION_NULL float64 0 0 | SLOPE_3M_TILE large_stringclasses 6
values | SLOPE_3M_FRACTION_NULL float64 0 0 | ASPECT_3M_TILE large_stringclasses 6
values | ASPECT_3M_FRACTION_NULL float64 0 0 | METADATA_TILE large_stringclasses 6
values | CENTER_LATITUDE float64 -33.36 25.9 | CENTER_LONGITUDE float64 -165.55 35.1 | UPPER_LEFT_LONGITUDE float64 -165.56 35.1 | UPPER_LEFT_LATITUDE float64 -33.35 25.9 | LOWER_RIGHT_LONGITUDE float64 -165.54 35.2 | LOWER_RIGHT_LATITUDE float64 -33.37 25.9 | BOUNDS_XMIN float64 131k 340k | BOUNDS_XMAX float64 132k 341k | BOUNDS_YMIN float64 640k 2.49M | BOUNDS_YMAX float64 640k 2.49M | EMISSION_ANGLE float64 1.17 21.7 | INCIDENCE_ANGLE float64 42.5 68.3 | PHASE_ANGLE float64 36.5 76.7 | SUB_SOLAR_GROUND_AZIMUTH float64 45.9 269 | SUB_SOLAR_LATITUDE float64 -1.53 1.23 | SUB_SOLAR_LONGITUDE float64 -134.97 74.2 | DATASET large_stringclasses 2
values | ALLOW_NANS_OPTICAL_DTM_SLOPE_ASPECT bool 1
class | __index_level_0__ int64 172k 824k |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
M1160454221 | 18,070 | 4,922 | LTM_16N | nac/M1160454221_r18070_c4922.nc | null | dtm_3m/M1160454221_r18070_c4922.nc | 0 | slope_3m/M1160454221_r18070_c4922.nc | 0 | aspect_3m/M1160454221_r18070_c4922.nc | 0 | metadata/M1160454221_r18070_c4922.txt | 21.130048 | -55.714054 | -55.723098 | 21.138513 | -55.705011 | 21.121582 | 257,823.788462 | 258,335.788462 | 639,844.375677 | 640,356.375677 | 21.695 | 43.525 | 63.955 | 243.964369 | -1.53 | -93.81 | train | false | 172,373 |
M1407958183 | 4,896 | 1,150 | LTM_4S | nac/M1407958183_r4896_c1150.nc | null | dtm_3m/M1407958183_r4896_c1150.nc | 0 | slope_3m/M1407958183_r4896_c1150.nc | 0 | aspect_3m/M1407958183_r4896_c1150.nc | 0 | metadata/M1407958183_r4896_c1150.txt | -25.052221 | -150.557267 | -150.566691 | -25.043862 | -150.547841 | -25.060578 | 289,339.795075 | 289,851.795075 | 1,740,625.276471 | 1,741,137.276471 | 16.915 | 60.095 | 76.735 | 73.573376 | 0.32 | -94.08 | train | false | 382,578 |
M1471423196 | 37,214 | 1,924 | LTM_23N | nac/M1471423196_r37214_c1924.nc | null | dtm_3m/M1471423196_r37214_c1924.nc | 0 | slope_3m/M1471423196_r37214_c1924.nc | 0 | aspect_3m/M1471423196_r37214_c1924.nc | 0 | metadata/M1471423196_r37214_c1924.txt | 25.936254 | 3.847731 | 3.83806 | 25.944415 | 3.857401 | 25.928093 | 136,566.953851 | 137,078.953851 | 787,227.371909 | 787,739.371909 | 19.45 | 56.74 | 74.87 | 252.663057 | 1.23 | -48.94 | train | false | 403,665 |
M1096572724RE | 10,462 | 4,900 | LTM_22S | nac/M1096572724R_r10462_c4900.nc | null | dtm_3m/M1096572724R_r10462_c4900.nc | 0 | slope_3m/M1096572724R_r10462_c4900.nc | 0 | aspect_3m/M1096572724R_r10462_c4900.nc | 0 | metadata/M1096572724R_r10462_c4900.txt | -0.425194 | -11.905744 | -11.914171 | -0.416758 | -11.897317 | -0.433629 | 131,338.712205 | 131,850.712205 | 2,486,833.60942 | 2,487,345.60942 | 1.17 | 68.25 | 67.08 | 269.314994 | -1.14 | -80.08 | train | false | 470,271 |
M1151623432 | 19,094 | 6,308 | LTM_27S | nac/M1151623432_r19094_c6308.nc | null | dtm_3m/M1151623432_r19094_c6308.nc | 0 | slope_3m/M1151623432_r19094_c6308.nc | 0 | aspect_3m/M1151623432_r19094_c6308.nc | 0 | metadata/M1151623432_r19094_c6308.txt | -17.741449 | 35.143416 | 35.134408 | -17.733152 | 35.152424 | -17.749745 | 340,475.931474 | 340,987.931474 | 1,961,542.847635 | 1,962,054.847635 | 5.93 | 42.53 | 37.13 | 68.956074 | 0.3 | 74.23 | test | false | 759,380 |
M189321511 | 15,560 | 2,424 | LTM_2S | nac/M189321511_r15560_c2424.nc | null | dtm_3m/M189321511_r15560_c2424.nc | 0 | slope_3m/M189321511_r15560_c2424.nc | 0 | aspect_3m/M189321511_r15560_c2424.nc | 0 | metadata/M189321511_r15560_c2424.txt | -33.360693 | -165.550366 | -165.560711 | -33.352448 | -165.540018 | -33.368937 | 311,730.88586 | 312,242.88586 | 1,488,418.670527 | 1,488,930.670527 | 13.285 | 44.805 | 36.46 | 45.945927 | 0.96 | -134.97 | test | false | 824,297 |
SomBench Pre-training Corpus: Multimodal Lunar Tiles
Dataset Summary
This includes a small sample from SomBench: a corpus of co-registered, multimodal lunar image tiles built for large-scale self-supervised (foundation-model) pre-training. It contains a subset of modalities from the low-resolution (WAC-anchored) and high-resolution (NAC-anchored) tracks specifically used in pretraining.
Tiles are anchored to individual LROC Experiment Data Record (EDR) image canvases rather than to a fixed map grid. A sliding window enumerates fixed-shape 512 × 512-pixel patches over each EDR, and every co-registered modality is snapped to that same per-tile boundary. Each tile therefore bundles many physically distinct measurements (optical, topographic, spectral, radar, thermal, gravity) over the same ground patch, covering the same spatial bounds. Anchoring to image canvases also preserves the optical observation context, and overlapping EDR coverage exposes models to the same terrain under different illumination conditions.
The corpus is organized into two parallel tracks that share construction logic but differ in their optical anchor and ground scale:
WAC_LowRes/: anchored to LROC Wide-Angle Camera (WAC) visible imagery at 100 m/pixel; each tile covers ≈ 51.2 × 51.2 km.NAC_HighRes/: anchored to LROC Narrow-Angle Camera (NAC) imagery at 1 m/pixel; each tile covers ≈ 512 × 512 m.
Both tracks use a 512 × 512-pixel tile size for the anchor modality (WAC or NAC). Coarser modalities are resampled, while preserving native resolution as much as possible, to align to the exact bounds of the anchor modality.
Note: The full dataset is available on AWS at s3://nasa-lunar-fm-bench/ and can be accessed using the AWS CLI:
aws s3 ls s3://nasa-lunar-fm-bench/ --no-sign-request
Supported Tasks and Applications
- Self-supervised / foundation-model pre-training: masked image modeling and multimodal SSL over co-registered layers.
- Multimodal representation learning and cross-modal fusion: joint embeddings across optical, topographic, spectral, radar, thermal, and gravity modalities.
- Multi-scale learning: pairing meter-scale NAC context with hundreds-of-meters-to-kilometer static layers within one framework.
- Downstream fine-tuning: the
testsplit is reserved for evaluation and fine-tuning on the SomBench application benchmarks (crater detection, IMP segmentation, ice prospectivity).
Tracks
| Property | WAC_LowRes/ |
NAC_HighRes/ |
|---|---|---|
| Optical anchor | WAC VIS (100 m/px) | NAC (1 m/px) |
| Tile ground extent | 51.2 km × 51.2 km | 512 m × 512 m |
| Tile size (pixels) | 512 × 512 | 512 × 512 |
| Modality directories | ~29 | ~31 |
| Source EDR products | 54,080 WAC EDRs | 1,095 NAC EDRs |
Zones covered (LTM_CODE) |
92 (90 LTM + LPS_N/S) | 80 |
| Tiles | 963,609 | 1,000,113 |
| Dataset size | 38 TB | 1.4 TB |
Directory Layout
Sombench-pretraining-data/
├── WAC_LowRes/ # low-resolution (WAC-anchored)
├── WAC_LowRes.parquet
├── aspect/
├── dtm/
├── metadata/
├── slope/
├── uv/
└── vis/
├── NAC_HighRes/ # high-resolution (NAC-anchored)
├── NAC_HighRes.parquet
├── aspect_3m/
├── dtm_3m/
├── metadata/
├── nac/
└── slope_3m/
The .parquet file in each track has a row for each tile and includes the paths to the paired modalities (e.g. DTM_TILE), metadata associated with the EDR image (e.g. INCIDENCE_ANGLE), and DATASET assignment for training.
Within each modality sub-directory, tiles are stored as one netCDF file per patch, named by the source EDR product id and the sliding-window row/column:
{product_id}_r{row}_c{col}.nc
Modalities
Each modality lives in its own sub-directory (the lowercase "dataset key"). The table lists source, native resolution, and band content. Availability differs by track and by region: some layers exist only at the poles, others only outside the poles. Band counts are structural (from the SomBench paper); native resolutions are the upstream product resolutions before per-tile snapping.
NOTE: This table includes all modalities that are included in SomBench; however, the HuggingFace sample inlcudes only modalities used in pre-training, including 6 WAC_LowRes modalities (
vis,uv,dtm,aspect,slope,metadata) and 5 NAC_HighRes modalities (nac,dtm,aspect,slope,metadata).
| Directory (low / high) | Modality | Source / instrument | Latitude | Native res | Bands | Pixel value units |
|---|---|---|---|---|---|---|
nac (high only) |
NAC panchromatic imagery; high-res anchor | LRO LROC NAC | 90°S–90°N (sparse, non-uniform) | 1 m | 1 | I/F: unitless |
vis (low only) |
WAC visible reflectance (415, 566, 604, 643, 689 nm); low-res anchor | LRO LROC WAC | 90°S–90°N | 100 m | 5 | I/F: unitless |
uv (low only) |
WAC ultraviolet (321, 360 nm) | LRO LROC WAC | 90°S–90°N | 500 m | 2 | I/F: unitless |
wac_mosaic |
WAC global morphologic mosaic (643 nm) | LRO LROC WAC | 90°S–90°N | 100 m | 1 | I/F: unitless |
wac_norm_ref |
WAC normalized multi-band reflectance | LRO LROC WAC | 60°S–60°N | 500 m | 7 | I/F: unitless |
wac_nr_643_hr |
WAC 643 nm high-resolution normalized reflectance | LRO LROC WAC | 90°S–90°N | 100 m | 1 | I/F: unitless |
tio2 |
WAC-derived TiO₂ abundance | LRO LROC WAC | 70°S–70°N | 400 m | 1 | wt% |
dtm / dtm_60m |
SLDEM2015 elevation (topography) | LOLA + Kaguya TC | 90°S–90°N | 60 m | 1 | meters |
slope / slope_60m |
SLDEM2015 slope | LOLA + Kaguya TC | 90°S–90°N | 60 m | 1 | degrees |
aspect / aspect_60m |
SLDEM2015 aspect (downslope geographic azimuth, 0/360°: north-facing, 90°: east-facing; sine/cosine encoded) | LOLA + Kaguya TC | 90°S–90°N | 60 m | 2 | aspect: degrees, sine/cosine: unitless |
dtm_3m (high only) |
NAC-stereo DTM elevation | USGS NAC DTM | 90°S–90°N (sparse, non-uniform) | 3 m | 1 | meters |
slope_3m (high only) |
NAC-stereo DTM slope | USGS NAC DTM | 90°S–90°N (sparse, non-uniform) | 3 m | 1 | degrees |
aspect_3m (high only) |
NAC-stereo DTM aspect (downslope geometric azimuth, 0/360°: faces map-up, 90°: faces map-right; sine/cosine encoded) | USGS NAC DTM | 90°S–90°N (sparse, non-uniform) | 3 m | 2 | aspect: degrees, sine/cosine: unitless |
roughness |
LOLA roughness (50 m baseline) | LRO LOLA | 90°S–90°N | 1 km | 1 | meters |
geomap |
USGS Unified Geologic Map (categorical, 43 units) | USGS | 90°S–90°N | 60 m | 1 | unitless |
gravity |
GRAIL free-air gravity disturbance | GRAIL | 90°S–90°N | 20 km | 1 | milligal |
mi_norm_ref |
Kaguya MI normalized reflectance (VIS–NIR) | SELENE/Kaguya MI | 55°S–55°N | 60 m | 8 | I/F: unitless |
mi_mineralogy |
Kaguya MI mineralogy (olivine, OPX, CPX, plagioclase, FeO, plag. grain size, OMAT) | SELENE/Kaguya MI | 55°S–55°N | 60 m | 7 | OMAT: unitless, grain size: microns, FeO: wt%, all others: wt%/100 |
sw_fe |
Kaguya MI space-weathering Fe (smFe, mpFe, npFe) | SELENE/Kaguya MI | 55°S–55°N | 1 km | 3 | wt% |
sp_mineralogy |
Kaguya SP polar mineralogy (olivine, plag., HCP, LCP, FeO, npFe, OMAT) | SELENE/Kaguya SP | 80–90°N; 80–90°S | 1 km | 7 | OMAT: unitless, FeO: wt%, all others: wt%/100 |
minirf_s1 |
Mini-RF radar reflectivity (S-band) | LRO Mini-RF | 90°S–90°N | 90 m | 1 | decibels |
minirf_cpr |
Mini-RF circular polarization ratio (CPR) | LRO Mini-RF | 90°S–90°N | 90 m | 1 | unitless |
treg |
Diviner nighttime regolith temperature anomaly | LRO Diviner | 70°S–70°N | 240 m | 1 | Kelvin |
hpar |
Diviner H-parameter (regolith density scale height) | LRO Diviner | 70°S–70°N | 240 m | 1 | meters |
rock_abundance |
Diviner rock abundance (areal fraction of m-scale rocks) | LRO Diviner | 70°S–70°N | 240 m | 1 | unitless |
tbol |
Diviner bolometric temperature; 24 sub-solar-longitude phases (15° steps) + closest | LRO Diviner | 90°S–90°N | 15 km | 25 | Kelvin |
tbol_poles |
Diviner polar bolometric temperature; 24 phases × summer/winter + closest | LRO Diviner | 80–90°N; 80–90°S | 240 m | 49 | Kelvin |
dice |
Diviner ice stability depth | LRO Diviner | 80–90°N; 80–90°S | 240 m | 1 | centimeters |
psr |
LOLA permanently shadowed regions (PSR) mask | LRO LOLA | 80–90°N; 80–90°S | 20 m | 1 | unitless |
avg_illum |
LOLA average Sun illumination (18.6-yr precession cycle) | LRO LOLA | 75–90°N; 75–90°S | 120 m | 1 | unitless |
albedo |
LOLA 1064 nm normal albedo | LRO LOLA | 50–90°N; 50–90°S | 1 km | 1 | I/F: unitless |
hydrogen |
Lunar Prospector hydrogen abundance | LP Neutron Spectrometer | 60–90°N; 60–90°S | 15 km | 1 | wt% |
metadata |
Associated per-tile metadata (illumination geometry, location, …) | LRO LROC NAC/WAC | 90°S–90°N | - | - | coordinates & angles: degrees |
craters (low only) |
Robbins (2019) crater labels, rasterized to the tile grid | Robbins crater catalog | 90°S–90°N | - | - | unitless |
Regional availability. Most modalities are present in both polar and
non-polar tiles wherever data exists. The exceptions: sp_mineralogy,
tbol_poles, dice, psr, avg_illum, albedo, and hydrogen are
polar-only, while tio2, hpar, and rock_abundance are non-polar-only.
A sub-directory may still appear in both tracks even where its tiles are
populated for one region only.
Tile File Format
Every tile is a self-describing netCDF4 file (written via h5netcdf with
Bitshuffle + LZ4 chunk compression; one chunk per variable):
- Coordinate vectors: 1-D
xandypixel-center coordinates in the tile's CRS. - Global attributes: full CRS as a WKT string (
crs), per-axis pixel resolution (pix_res_x,pix_res_y), and a comma-separated list of band names (band_names). - Value-range clipping applied at write time from a per-modality registry
(e.g. slope ∈ [0°, 90°], normalized reflectance ∈ [0, 1], albedo ∈ [0, 1], TiO₂ ∈ [0, 100] %).
NaNencodes a genuine data gap and is preserved through clipping; the categoricalgeomaplayer is exempt so class indices are unchanged. - Snapped resolution: because coarse modalities are resampled to align with the anchor grid, the stored pixel size can differ slightly from native (e.g. 60 m → ≈ 56.9 m in the NAC track; 100 m → ≈ 102.4 m). The per-tile CRS and resolution are always recorded in the file's attributes.
Multi-band / multi-phase notes
tbol: all 24 sub-solar-longitude snapshots (15° steps) plus a duplicated "closest" band → 25 bands.tbol_poles: 24 phases × summer/winter (48) plus a "closest" band → 49 bands (polar tiles only).- Multi-band spectral/mineral layers (
mi_norm_ref,mi_mineralogy,wac_norm_ref,sp_mineralogy,sw_fe) are stacked along a band dimension; if any band is missing, the whole layer is recorded as missing for that tile.
Catalogs and Metadata
Each track has a Parquet catalog (WAC_LowRes.parquet and
NAC_HighRes.parquet) with one row per tile and these columns:
- Identification:
PRODUCT_ID(source EDR id),ROW,COL(sliding-window offset),LTM_CODE(LTM zone orLPS_N/LPS_S). - Per-modality:
{MODALITY}_TILE, relative path to the tile's netCDF file (e.g.WAC_VIS_TILE,NAC_TILE,DTM_60M_TILE,TBOL_TILE, …) and{MODALITY}_FRACTION_NULL, the tile's NaN fraction for that layer. (METADATA_TILE, and low-resCRATERS_TILE, have no null-fraction column.) - Geometry:
CENTER_LATITUDE/CENTER_LONGITUDE, cornerUPPER_LEFT_*/LOWER_RIGHT_*lon/lat, and projected boundsBOUNDS_XMIN/XMAX/YMIN/YMAX. - Viewing geometry:
INCIDENCE_ANGLE,EMISSION_ANGLE,PHASE_ANGLE,SUB_SOLAR_GROUND_AZIMUTH,SUB_SOLAR_LATITUDE,SUB_SOLAR_LONGITUDE. - Split & flags:
DATASET(train/val/test) andALLOW_NANS_OPTICAL_DTM_SLOPE_ASPECT, a boolean marking tiles permitted to contain NaN in the optical / DTM / slope / aspect layers (primarily polar tiles admitted with partial data; 4,588 in the low-res track, 3,888 in the high-res track).
Loading on the Hub.
load_dataset(...)and the dataset viewer return this catalog (per-tile paths and metadata), not the netCDF imagery. Fetch each tile from the path in its{MODALITY}_TILEcolumn (e.g. viahuggingface_hub).
The METADATA_TILE column (and the metadata modality
directory) carries associated per-tile metadata (illumination geometry, location,
etc.).
Splits
Splits are assigned at the grid-cell (LTM zone) level to prevent spatial leakage:
- Zone partition: unique
LTM_CODEgrid cells are randomly partitioned into train / validation / test at a target of 75 % / 15 % / 10 % of cells. Whole zones go to a single split, so nearby tiles never straddle splits. - Buffer exclusion: tiles that straddle two zones are dropped to guarantee strict spatial separation.
- Zone/partition assignments are applied consistently across both tracks.
Released split sizes (DATASET column of the catalogs):
| Split | WAC_LowRes |
NAC_HighRes |
|---|---|---|
| Train | 754,529 | 750,557 |
| Val | 115,548 | 157,153 |
| Test | 93,532 | 92,403 |
| Total | 963,609 | 1,000,113 |
Train + validation are intended for pre-training; test is reserved for downstream evaluation and fine-tuning. Because zones vary in tile count, the realized tile ratio differs from the 75/15/10 cell ratio.
Coverage and Projections
Tiles span from the equator to ±82° latitude in 90 Lunar Transverse Mercator (LTM) zones plus two
Lunar Polar Stereographic (LPS) caps (|φ| ≥ 82°), using WKT definitions from McClernan et al. (2025).
Non-polar windows are rejected if the required anchor modality contains any
NaN; polar windows are admitted with any valid data to maximize coverage, so
polar tiles more often contain partial NaN. Tiles that straddle two zones are
dropped, keeping split boundaries clean.
Known Limitations
Heterogeneous spatial resolution, illumination-driven appearance changes, label
scarcity/class imbalance, and tens-of-meters absolute geolocation uncertainty all
apply. In practice: expect resampling artifacts where coarse modalities are
snapped to the anchor bounds; treat NaN as a genuine data gap (especially in
polar tiles, which are admitted with partial coverage); and use the
ALLOW_NANS_OPTICAL_DTM_SLOPE_ASPECT flag when building NaN-free training sets.
See the SomBench paper for the full discussion and recommended
practices.
Citations
@article{fraccaro2026lfm,
title = {Multimodal-Multiresolution Foundation Model for Lunar Remote Sensing},
author = {Fraccaro, Paolo and Nyirjesy, Gabby and Szwarcman, Daniela and Patil, Himanshu
and Gaur, Vishal and Lal, Rohit and Slank, Rachel A. and Dawson, Geoffrey
and Debary, Hiyam and Dionelis, Nikolaos and Barker, Michael K. and Annex, Andrew
and Viswanathan, Vishnu and Morse, Zachary and Schaefer, Ethan I. and Kumar, Ankur
and Watson, Campbell D. and Dawson-Rigas, Rebekah I. and Maskey, Manil
and Roy, Sujit and Ramachandran, Rahul and Bernab\'e-Moreno, Juan},
year = {2026}
howpublished = {\url{https://huggingface.co/collections/nasa-ibm-ai4science/nasa-ibm-lunar-fm-and-downstream-models}}
}
@misc{sombench2026collection,
author = {Patil, Himanshu and Nyirjesy, Gabby and Slank, Rachel A. and Gaur, Vishal
and Szwarcman, Daniela and Fraccaro, Paolo and Dionelis, Nikolaos and Barker, Michael K.
and Annex, Andrew and Viswanathan, Vishnu and Morse, Zachary and Schaefer, Ethan I.
and Debary, Hiyam and Kumar, Ankur and Lal, Rohit and Dawson, Geoffrey
and Watson, Campbell and Dawson-Rigas, Rebekah I. and Maskey, Manil
and Bernab\'e-Moreno, Juan and Ramachandran, Rahul and Roy, Sujit},
title = {{SomBench}: Benchmark Dataset for Advancing Machine Learning in Lunar Science},
year = {2026},
howpublished = {\url{https://huggingface.co/collections/nasa-ibm-ai4science/lunar-fm-ml-ready-benchmark-dataset-sombench}}
}
License
Released under the Creative Commons Attribution 4.0 International (CC BY 4.0) license.
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