Hawaiian Vog

Volcanic Haze in Hawaii

Hawaiian Vog

Hawaiian vog forms when volcanic gases from Kilauea react with sunlight, oxygen and moisture, creating hazy air that can affect visibility and breathing comfort.

Vog is air pollution caused by active volcanoes. The name comes from "volcanic smog." Volcanoes in Hawaii can emit sulfur dioxide into the atmosphere, where it reacts with oxygen, moisture, sunlight and particles in the air to form vog.

The most affected areas can change depending on volcanic activity, wind direction and weather. During typical trade wind patterns, emissions from Kilauea can move downwind across parts of the Big Island of Hawaii, including areas south and west of the volcano. When winds shift, vog can affect different districts and sometimes other islands.

In the past, gas plumes from Kilauea came from places such as Halema'uma'u Crater, Pu'u 'O'o and ocean-entry areas where lava flows reached the sea. Today, emission sources depend on current volcanic activity, which can change over time. Visitors and residents should check current volcano and air-quality updates during active eruption periods.

In general, the Big Island has higher vog levels than elsewhere, and the area around Kailua-Kona can be affected when winds carry volcanic emissions across the island. Areas from Volcano Village to Hilo can also experience vog or volcanic gas impacts depending on wind direction and eruption conditions.

Many people do not notice vog at low levels. It may appear as haze, reduced visibility or a grayish layer near the horizon. Vog can be noticeable when driving through or near Hawaii Volcanoes National Park, especially during active volcanic gas emissions.

Vog levels range from light to heavy. Some people are more sensitive to vog than others. Reactions can include eye, nose, throat or skin irritation, coughing, mucus buildup, headache, fatigue, dizziness, difficulty breathing or worsened asthma symptoms. Vog is especially a concern for people with asthma, COPD, heart disease or other respiratory conditions.

Vog conditions can change quickly because volcanic emissions, wind direction and weather patterns vary. Air-quality monitors and forecast models can help estimate conditions, but exact vog levels are difficult to predict far in advance.

For people who may be exposed to higher levels of vog, it can help to stay indoors, close windows and doors, avoid heavy outdoor activity, drink water and use air conditioning on recirculate mode if available. People with breathing or heart conditions should follow medical guidance and monitor local air-quality conditions during heavy vog days.

Frequently Asked Questions

What is Hawaiian vog?

Hawaiian vog is volcanic smog that forms when sulfur dioxide and other volcanic gases react with sunlight, oxygen, moisture and particles in the air.

Where is vog most common in Hawaii?

Vog is most common on the Big Island because it sits closest to Kilauea. Kailua-Kona and other downwind districts can experience hazy conditions when winds carry volcanic emissions across the island.

Is vog harmful to breathe?

Low levels may not bother most people, but vog can irritate the throat, eyes and lungs. People with asthma, COPD, heart disease or other respiratory conditions may feel symptoms more strongly.

Can vog affect other Hawaiian Islands?

Yes. Vog usually affects the Big Island the most, but changing winds can carry haze and fine particles to Maui, Oahu and other islands at times.

How can I protect myself from vog?

Stay indoors during heavy vog, close windows and doors, use air conditioning on recirculate mode, avoid heavy outdoor activity and monitor local air quality if you have breathing concerns.

Can vog levels be forecast?

Vog can be estimated with air-quality monitors and forecast models, but exact conditions are hard to predict because volcanic emissions, wind direction and weather patterns can change quickly.

Is vog the same as laze?

No. Vog forms from volcanic gases in the air. Laze forms when hot lava enters the ocean and creates an acidic steam plume with tiny volcanic glass particles.