Arctic and North Pole temperature map

The globe looks straight down on the North Pole. Cold air pools over Greenland and the frozen ocean, while the edges of the Arctic Ocean and northern Siberia show how fast conditions change.

© OpenStreetMap contributors · NASA · GEBCO · Natural Earth · GeoNames · NOAA GFS · GEFS-Aerosols

GlobeLayers — live 3D weather globe

GlobeLayers is a live 3D weather globe. Spin it, zoom in, and read today's weather anywhere on Earth, straight from open forecast data.

Layers

Data & freshness

Weather layers come from the NOAA GFS model at 0.25° resolution; air quality comes from NOAA GEFS-Aerosols. Four times a day, each new model run brings a 48-hour forecast in 3-hour steps, and the globe blends smoothly between steps. The banner shows the model run; the timeline shows the time you are looking at.

Sources & credits

NOAA GFS and GEFS-Aerosols (public domain) · NASA Blue Marble · GEBCO bathymetry and relief · © OpenStreetMap contributors · Natural Earth · GeoNames (CC BY 4.0).

Privacy

GlobeLayers uses cookie-free audience measurement by Cloudflare Web Analytics. No personal data is collected and there are no advertising trackers. The “My location” button uses your device's location only in your browser: it is never sent or stored.

Arctic and North Pole temperature map

This view looks down at the North Pole and shows the air temperature at two metres above the surface, in degrees Celsius, from the NOAA GFS model. Unlike Antarctica, the Arctic is an ocean covered in sea ice and surrounded by land.

Because the ice sits on water, the air above it is not as cold as on the southern plateau. In winter the coldest areas lie over Siberia, northern Canada and the high ice sheet of Greenland, where values drop well below minus 40 degrees. Over open water near the ice edge, the air is much warmer.

Follow the forecast for sudden changes. When a strong low-pressure system pushes into the Arctic from the Atlantic or the Pacific, a surge of mild air can raise temperatures by tens of degrees in a day or two, and the map shows it as a patch of lighter colour. Cold air can also spill south from the pole into mid-latitudes.

Summer brings long days with constant sunlight and temperatures close to freezing over the ocean. The grid is 0.25 degrees, and each of the four daily runs covers 48 hours in 3-hour steps.

GlobeLayers
How to use