UTM ↔ Latitude/Longitude Converter
Convert between UTM and latitude/longitude. Direction is auto-detected; the result shows zone, band, easting, northing, hemisphere, central meridian, and EPSG code with a map and full geographic report.
What UTM is
The Universal Transverse Mercator grid system divides the world into 60 vertical zones, each 6° of longitude wide. Each zone gets its own Transverse Mercator projection, giving accurate flat-map metres over a narrow strip. UTM is the default for topographic mapping, surveying, and most GIS work where distances and areas need to come out in metres directly.
A full UTM coordinate carries four parts: a zone number, a band letter, an easting in metres, and a northing in metres. The anatomy diagram below breaks each part down for the Empire State Building's reference UTM string.
The converter below accepts either a UTM string or a lat/lon pair and shows the conversion in the other direction. The deep report at the bottom of the page includes the zone-specific details (central meridian, scale factor, EPSG code) for the point you converted.
Convert UTM ↔ Lat/Lon
Paste either a UTM coordinate or a lat/lon pair. The direction is detected automatically; the result shows the other format along with the resolved point coordinates.
See it on the map
Click anywhere on the map to set the input above to that point's decimal-degree coordinates — the UTM conversion re-runs instantly.
How to use this tool
Enter coordinates in either format
Latitude/longitude can be DD (40.7484, -73.9857), DMS (40°44'54"N, 73°59'09"W), or DDM. UTM should be "zone-band easting northing" — for example "18T 585628 4511322" for the Empire State Building. The band letter encodes the hemisphere; explicit N/S in lat/lon also works.
Read the converted output
A lat/lon input produces the equivalent UTM with zone number, band letter, easting, and northing. A UTM input produces decimal-degree lat/lon. The report below the map adds zone-specific context: central meridian, scale factor, false easting/northing, and the EPSG code for this UTM zone.
Refine with the map
Click anywhere on the map to set the input to that point's decimal coordinates. The conversion re-runs instantly, and the report fetches nearest place and elevation. The URL updates with each conversion so links are shareable.
The structure of a UTM coordinate
A complete UTM position has four parts: a zone number (1–60), a band letter (C–X excluding I and O), an easting in metres, and a northing in metres. The Empire State Building, in canonical form, reads:
18T 585628 mE 4511322 mN │ │ │ │ │ │ │ │ │ │ │ └ northing label │ │ │ │ └ northing in metres (from equator) │ │ │ └ easting label │ │ └ easting in metres (offset from 500,000 false easting) │ └ band letter (T = 40°N to 48°N latitude) └ zone number (1–60, indicating which 6°-wide longitude strip)
Each zone is 6° of longitude wide. Zone 1 starts at 180°W; zone 60 ends at 180°E. The zone number for a given longitude is floor((lon + 180) / 6) + 1. The band letter partitions latitude into 20 strips, 8° tall each, except band X which is 12° tall (covering 72°N–84°N). Bands C–M sit in the Southern hemisphere; N–X in the Northern.
| Part | Range | What it encodes |
|---|---|---|
| Zone | 1 – 60 | 6°-wide longitude strip. Zone 1 is 180°W–174°W; zone 30 is 6°W–0°; zone 60 is 174°E–180°E. |
| Band | C – X (skipping I, O) | 8°-tall latitude strip (band X is 12° tall). Bands C–M are S hemisphere; N–X are N. |
| Easting | ~166,000 – ~834,000 m | Metres east, offset by the 500,000 m "false easting" so the central meridian = 500,000. |
| Northing | 0 – ~9,329,000 m (N); 1,116,000 – 10,000,000 m (S) | Northern: metres north of equator. Southern: metres north of the false origin 10,000,000 m south. |
How UTM ↔ lat/lon math works
The Transverse Mercator projection wraps a cylinder around the Earth along a chosen meridian (the zone's central meridian), then projects every point onto that cylinder. Unrolled flat, the central meridian becomes a vertical line at easting 500,000; everywhere else in the zone gets a curved-but-tractable transformation. The full forward and inverse formulas are 6th- order series in WGS-84 ellipsoidal parameters; the canonical reference is USGS Snyder PP 1395 (1987), still the most cited derivation in geodetic literature.
| Quantity | Value / source | Meaning |
|---|---|---|
| Reference ellipsoid | WGS-84 (a = 6,378,137 m; 1/f = 298.257223563) | The shape of the Earth assumed by every modern UTM implementation. |
| Scale factor k₀ | 0.9996 | Applied along the central meridian. Reduces distortion at zone edges from 1.0010 to about 1.0006. |
| False easting FE | 500,000 m | Added to every easting so points on both sides of the central meridian are positive. |
| False northing FN (N) | 0 m | Northern-hemisphere northings are measured north of the equator. |
| False northing FN (S) | 10,000,000 m | Southern-hemisphere northings are measured north of a "false equator" 10,000,000 m south of the real one. |
| Forward formula | Snyder PP 1395 §8 (eqs. 8-1 to 8-21) | Lat/lon → easting/northing via series in latitude and longitude difference. |
| Inverse formula | Snyder PP 1395 §8 (eqs. 8-22 to 8-25) | Easting/northing → lat/lon via series in M (meridional arc) and footprint latitude. |
| Working precision | 6th-order series | Round-trip accuracy < 1 mm anywhere inside zone bounds. |
Ten worked examples — both directions
| Point | Decimal Degrees | UTM |
|---|---|---|
| Empire State Building, New York City | 40.7484°N, 73.9857°W | 18T 585628 mE 4511322 mN |
| Eiffel Tower, Paris | 48.8584°N, 2.2945°E | 31U 448252 mE 5411955 mN |
| Sydney Opera House | 33.8568°S, 151.2153°E | 56H 334901 mE 6252289 mN |
| Tokyo Tower | 35.6586°N, 139.7454°E | 54S 386438 mE 3946808 mN |
| Cape Town Harbour | 33.9067°S, 18.4196°E | 34H 261415 mE 6245191 mN |
| Christ the Redeemer, Rio de Janeiro | 22.9519°S, 43.2105°W | 23K 683477 mE 7460687 mN |
| Greenwich Royal Observatory | 51.4769°N, 0.0005°W | 30U 708287 mE 5707127 mN |
| Equator on the 0° meridian (Gulf of Guinea) | 0.0°N, 0.0°E | 31N 166021 mE 0 mN |
| McMurdo Station, Antarctica | 77.8463°S, 166.6683°E | 58C 539204 mE 1358225 mN |
| North Cape, Norway (high-latitude land point) | 71.1717°N, 25.7833°E | 35W 456177 mE 7896987 mN |
The Greenwich row is a useful sanity check: zone 30's central meridian sits at 3°W, so a point at longitude 0° is about 3° east of the central meridian. The easting comes out near 708,287 m — well east of the 500,000 m central-meridian value — confirming the false-easting offset is being applied as expected. Cross the prime meridian by half a metre and the result jumps into zone 31, easting near 291,800 m on the western edge of that zone. Behaviour at zone boundaries is the most common surprise in UTM workflows.
Misconceptions worth getting straight
"Northing and latitude are the same thing"
No. Northing is metres on a flat projection of a 6°-wide Earth strip; latitude is angular degrees from the equator. They track each other closely (one degree of latitude is ~111,320 m), but they aren't identical. The easting/northing pair is Cartesian on the projection; lat/lon is angular on the ellipsoid.
"You can subtract two UTM coordinates to get a distance"
Inside the same zone, yes — that's a key reason UTM exists. √((ΔE)² + (ΔN)²) gives the planar distance to about 1 part in 2,500 worst-case. Across zones, no — the projections differ. For cross-zone distance, convert both points to lat/lon first and use Haversine or Vincenty.
"The band letter just tells you the hemisphere"
It encodes more than that. Bands C–M = Southern; N–X = Northern, yes — but they also identify a specific 8° latitude strip, which most GIS software uses for sanity-checking input. A UTM string with the wrong band letter for its northing will be caught by validators.
"UTM is a coordinate system"
UTM is a projected coordinate system built on top of a geographic coordinate system (WGS-84 lat/lon, in this implementation). The distinction matters: changing the underlying datum (e.g., NAD27 vs WGS-84) changes the UTM result by up to ~200 m. Almost all modern data uses WGS-84 or its near-equivalents (NAD83, ITRF), but legacy NAD27 data is still common in the United States and Canada.
"MGRS is the same as UTM with letters"
Closely related, not identical. MGRS is built on UTM south of 84°N (and UPS north of it), but it adds a 100-km grid-square letter pair, then expresses the in-square offset in fewer digits (with progressively coarser precision). MGRS is the military-grid expression; UTM is the raw metric one.
When to use UTM, when not to
| Use case | UTM? | Why |
|---|---|---|
| Topographic mapping over a region < 6° wide | Yes | Designed exactly for this — metres are metres, low distortion. |
| Land surveying, infrastructure engineering | Yes | Standard in most national survey frameworks outside the US. |
| US engineering / cadastral work | Maybe — also see State Plane | State Plane is the US national standard, with smaller zones and lower distortion. |
| Cross-continent route planning | No | Crosses zone boundaries; geodetic (lat/lon + Vincenty) is correct. |
| Polar work (above 84°N / below 80°S) | No | Use UPS — UTM is undefined. |
| Web map rendering | No | Web maps use Web Mercator (EPSG:3857), not UTM. |
| GPS field collection | Yes | Most field GPS hardware can output UTM directly. |
| Geocoding addresses | No | Geocoders return lat/lon; convert to UTM as the final step if needed. |
How to verify a UTM coordinate
Three sanity checks any UTM result should pass:
- Easting is between ~166,000 and ~834,000 m.Outside this range, the point is in the wrong zone (and a re-projection to the neighbouring zone is needed) or the false easting was forgotten.
- Northing matches the band letter. Bands C–M require Southern-hemisphere northings (1,116,000 to 10,000,000 m); N–X require Northern (0 to 9,329,000 m). Cross-checking is a common validator step.
- Round-trip the conversion. Convert your UTM back to lat/lon, and confirm it matches your starting lat/lon to within a millimetre. Any larger discrepancy is a sign of either zone error or datum mismatch.
For complex projects — mixed UTM/lat-lon data, or any work crossing zones — keep a copy of the lat/lon (WGS-84) as the authoritative source. UTM is a derived representation; lat/lon is the underlying truth.
How this converter is built
The math runs entirely in the browser: forward and inverse formulas live in src/lib/coords/utm.ts, implementing Snyder PP 1395 §8 verbatim with the WGS-84 ellipsoid. Direction is auto-detected from the input string — a regex match on <digits><letter> <digits> <digits>triggers the UTM-to-lat/lon path; anything else is parsed as lat/lon. The map below the converter uses MapLibre GL with MapTiler tiles and renders the result point as a draggable pin. Clicking the map sets the input to that point's decimal-degree coordinates and re-runs the conversion. The deep report sub-fetches nearest place (Mapbox v6, server-side proxy with no-store cache) and elevation (USGS 3DEP for US, OpenTopoData SRTM30m elsewhere) — both per CLAUDE.md §19.2 and §19.4. No coordinates are ever logged or retained.
Related tools
- Coordinate converter (all six formats)— DD, DMS, DDM, UTM, MGRS, Plus Code in one place
- MGRS converter— UTM with 100-km grid squares and military precision
- Plus Codes (Open Location Code)— Open-source location code from Google
- DMS ↔ Decimal Degrees— Angular notation conversion
- Elevation— USGS 3DEP / SRTM30m with accuracy band
- Address ↔ coordinates— Forward geocoding with Mapbox confidence bands
Related articles
- The UTM coordinate system explained— Pillar article on UTM zones, bands, and projection math
- Coordinate formats explained— The six common notations and when each is used
- What is a map projection?— How curved Earth becomes flat map — Transverse Mercator
- What is a geodetic datum?— WGS-84 vs NAD27 vs NAD83 — why the datum matters for UTM
- Decimal degrees vs DMS— Why modern systems use decimal degrees
Frequently asked questions
What is UTM?
Universal Transverse Mercator — a worldwide grid of 60 zones, each 6° of longitude wide, using the Transverse Mercator projection. Within each zone, positions are expressed as an easting and northing in metres, plus the zone number and band letter that locate the strip. UTM is the default for topographic mapping, infrastructure surveying, and most national mapping outside the US. See /learn/utm-coordinate-system for the pillar explanation.
What does the band letter mean?
It encodes latitude as one of 20 letters (C–X, omitting I and O), each covering an 8° latitude band (band X is 12° tall). Bands C–M are in the Southern hemisphere; N–X in the Northern. Most software uses the hemisphere flag (N or S) alone, but the band letter is a common human-readable convention and a useful validator: an out-of-band northing will fail a band-letter sanity check.
Why is there a 500,000 false easting?
So that points on either side of the zone's central meridian both have positive easting. Without the offset, the central meridian sits at 0 and points west would be negative, which is awkward in surveying notation. The "false easting" of 500,000 m gives every zone a comfortable 0–1,000,000 range with the central meridian at the middle.
Why does UTM not work at the poles?
The Transverse Mercator projection introduces unacceptable scale distortion above 84°N and below 80°S. Polar regions are covered by the Universal Polar Stereographic (UPS) system instead. This converter returns an error for input outside the ±84° band — polar projects need a UPS-aware tool.
How precise is the UTM conversion?
Sub-millimetre round-trip. The formulas (USGS Snyder PP 1395 §8) are implemented as 6th-order series in WGS-84 ellipsoidal parameters. Easting and northing are displayed as integer metres, but the underlying math uses full double-precision floats. For survey-grade work the output is directly usable.
How does UTM differ from State Plane?
UTM uses worldwide 6°-wide zones; State Plane uses much smaller per-state zones designed to hold scale distortion below 1 part in 10,000. State Plane is the US standard for engineering and cadastral work; UTM is the standard for cross-state, federal, and international work. Both can coexist on the same project — UTM as the cross-region reference, State Plane for in-state engineering.
How does UTM differ from MGRS?
MGRS is built on UTM (south of 84°N) and UPS (north of it), but it adds a 100-km grid-square letter pair after the zone-band, then expresses the in-square offset in fewer digits. UTM gives you metres; MGRS gives you progressively coarser precision-on-demand (1 km, 100 m, 10 m, 1 m). Use UTM for engineering precision, MGRS for military communications.
Can I convert UTM in one zone to a neighbouring zone?
Yes — convert UTM → lat/lon, then lat/lon → UTM in the new zone. This converter does it automatically: a UTM input gives you the lat/lon, which can then be re-projected to any zone via /tools/coordinate-converter. Direct UTM-to-UTM zone shifts without a lat/lon round-trip are mathematically unstable near zone boundaries.
Sources
- USGS Snyder PP 1395 — J. P. Snyder, "Map Projections — A Working Manual", USGS Professional Paper 1395 (1987). The canonical UTM forward/inverse formulas (§8). · https://pubs.usgs.gov/pp/1395/report.pdf · Accessed .
- NGA TR 8358.2 — NGA Technical Report 8358.2 — The Universal Grids and the Transverse Mercator and Polar Stereographic Map Projections (the defence-standard definition). · https://earth-info.nga.mil/index.php?dir=coordsys&action=specs-univ-grids · Accessed .
- NIMA TR 8350.2 (WGS 84) — NIMA Technical Report 8350.2 — Department of Defense World Geodetic System 1984. Defines the ellipsoid the UTM math assumes. · https://earth-info.nga.mil/php/download.php?file=coord-wgs84 · Accessed .
- ISO 19111:2019 — ISO 19111:2019 — Geographic information — Referencing by coordinates. The standard that defines projected vs geographic CRS. · https://www.iso.org/standard/74039.html · Accessed .
- NGS NCAT — NGS Coordinate Conversion and Transformation Tool — US government UTM ↔ lat/lon utility used to spot-check this converter. · https://geodesy.noaa.gov/NCAT/ · Accessed .
- EPSG Registry — EPSG Geodetic Parameter Dataset — codes 32601–32660 (UTM north) and 32701–32760 (UTM south) are the canonical IDs for each UTM zone on WGS-84. · https://epsg.org/ · Accessed .
- USGS 3DEP — USGS 3D Elevation Program — the source the report uses for US elevation lookups (sub-2 m vertical accuracy). · https://www.usgs.gov/3d-elevation-program · Accessed .
- OpenTopoData SRTM30m — OpenTopoData public API serving NASA SRTM 30 m — the source for non-US elevation lookups. · https://www.opentopodata.org/datasets/srtm/ · Accessed .
- Mapbox Geocoding v6 — Mapbox Geocoding API v6 — used by the nearest-place lookup in the report. · https://docs.mapbox.com/api/search/geocoding-v6/ · Accessed .
- NGA — Universal Transverse Mercator (UTM) — NGA reference page describing UTM grid usage in defence-mapping context (zones, bands, MGRS relationship). · https://earth-info.nga.mil/index.php?dir=coordsys&action=coordsys · Accessed .