Bazaar
Hurricane Lane Fell Apart as it Approached Hawaii. So What Happened? | Weather.com
Advertisement
Advertisement

Latest Hurricane News

Hurricane Lane Fell Apart as it Approached Hawaii. So What Happened?

At a Glance

  • Hurricane Lane weakened dramatically as it moved closer to Hawaii.
  • Wind shear and dry air led to its demise.
  • Interaction with Hawaii's mountainous terrain might have also played a role.
  • Significant flooding occurred on the Big Island, but the impacts from strong winds and storm surge could have been worse.

Hurricane Lane rapidly fell apart as it approached Hawaii, and although it brought flooding rainfall, the threat of damaging winds and storm surge was greatly reduced.

Lane's appearance on satellite imagery deteriorated rapidly from a well-defined Category 5 hurricane to a disheveled tropical storm over the course of a few days late last week. But why did this weakening occur and spare Hawaii from additional severe impacts?

(MORE: Recapping Hurricane Lane)

image
Infrared satellite imagery showing the demise of Lane from a Category 5 hurricane to a tropical storm Aug. 22-25, 2018.

First and foremost, Lane encountered a wall of wind shear as it moved closer to Hawaii. Wind shear, a change in wind speed and/or direction with height, is an enemy to hurricanes since it can shred them apart when strong and persistent.

You can see Lane move from an area of light wind shear (blue and green shadings) to higher wind shear (orange and red shadings) in the animation below from Aug. 22-24.

image
Orange and red shadings depict increased winds in the upper atmosphere, which help to shred apart hurricanes and tropical storms. (CIMSS/SSEC)

Those strong winds also imported dry air, another nemesis of hurricanes, into the core of Lane, according to a tweet from Philippe Papin, an atmospheric scientist at the U.S. Naval Research Laboratory.

The wind shear and dry air attacked Lane's core, or eyewall, leading to the degradation of its center of circulation as shown in this animation.

Advertisement

As a side note, when Lane was just outside this zone of wind shear, that band of strong winds aloft might have actually helped intensify the hurricane. Strong winds in the upper atmosphere just west of a hurricane can help improve ventilation in the storm and allow it to strengthen.

When Lane entered that zone of strong winds, however, it was over.

Another potential factor in Lane's weakening is the interaction of its circulation with Hawaii's mountainous terrain. The low-level wind flow around the hurricane might have been disrupted by the tall peaks, assisting in Lane's demise.

Forecasters always knew Lane would encounter wind shear, but the question was how quickly it would surrender to the strong winds and begin to fall apart.

That had implications for how close Lane would get to the Hawaiian Islands. Slower weakening would allow Lane to come closer to Hawaii while rapid weakening would keep it farther south.

Thankfully, Lane weakened faster and therefore turned to the west (left) before reaching the islands. Weaker circulations tend to follow the path of prevailing winds in the lower atmosphere, which, in this case, were from the east.

Although the heavy rain from Lane produced significant flooding and landslides on the Big Island, impacts from strong winds and storm surge could have been much worse across the island chain had Lane held intact longer.

Advertisement
Hidden Weather Icon Masks
Hidden Weather Icon Symbols