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High-Frequency Radar

High-Frequency Radar

A live snapshot of lake surface currents, 24 hours a day.

High Frequency Radar

New to the Great Lakes, HF radar measures surface currents like no other platform can: over large areas.

When studying currents, researchers are typically limited to a device that measures only one point in the water.

By capturing extremely detailed, near-surface water direction and speed information, this platform allows observers to:

  • Locate people or pets during search and rescue operations
  • Track vessels
  • Monitor movements of hazardous spills or harmful algal blooms
  • Understand how water moves through complex waterways, like in the Straits of Mackinac

Photos by Nathan Shaiyan, Michigan Technological University, unless otherwise noted.

Data collected May 2022: Arrows indicate the direction and speed of the surface current.

HF radar will be available on Seagull soon.

Data Visualization of High Frequency Radar

HF radars are shore-based remote sensing systems made up of antennas, generally used in pairs and placed close to the water’s edge.

The antennas send out pulses of high-frequency radio waves that bounce off the water’s surface and back to the antenna. By measuring how the waves bounce back, the radar is able to create a map detailing the speed and direction of surface currents.

Because saltwater allows HF radar to work over much larger areas, coastal waters have long benefited from HF radar, but the Great Lakes are just beginning to use it. Even the reduced range, reaching 10-15 miles in some tests by Dr. Lorelle Meadows, can be enough for many areas.

The first HF radar in the Great Lakes is located in the Straits of Mackinac where, operated by Michigan Technological University Great Lakes Research Center, a single radar pair covers the waters on the west side of the Mackinac Bridge.

Learn more about the project.

Latest Data

From UGLOS. HF radar will also be available via Seagull soon.

During winter check NOAA Great Lakes Environmental Research Lab for current ice conditions that can interfere with measurement.

HF radars are shore-based remote sensing systems made up of antennas, generally used in pairs and placed close to the water’s edge.

The antennas send out pulses of high-frequency radio waves that bounce off the water’s surface and back to the antenna. By measuring how the waves bounce back, the radar is able to create a map detailing the speed and direction of surface currents.

Because saltwater allows HF radar to work over much larger areas, coastal waters have long benefited from HF radar, but the Great Lakes are just beginning to use it. Even the reduced range, reaching 10-15 miles in some tests by Dr. Lorelle Meadows, can be enough for many areas.

The first HF radar in the Great Lakes is located in the Straits of Mackinac where, operated by Michigan Technological University Great Lakes Research Center, a single radar pair covers the waters on the west side of the Mackinac Bridge.

Learn more about the project.

A map shows the placement of the high-frequency radar at both ends of the Mackinac Bridge, alongside two buoys that also monitor the waterway

Pair distance: 6.6 kilometers (4.1 miles)

Total area covered: 20 square kilometers (7.7 square miles)

Radar: 42 MHz

Transmit power: 40 watts

Map refresh: every 30 minutes

MTU researchers also monitor the Straits while aboard the S/V Osprey and using two two buoys (45175 and 45194). Image by MTU

Mockup of Great Lakes and Buoy data on a computer and phone
Seagull Logo Homepage White Outline

HF radar will also be available on Seagull soon.

See it on UGLOS now.

GLOS