MbrlCatalogueTitleDetail

Do you wish to reserve the book?
Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery
Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery
Hey, we have placed the reservation for you!
Hey, we have placed the reservation for you!
By the way, why not check out events that you can attend while you pick your title.
You are currently in the queue to collect this book. You will be notified once it is your turn to collect the book.
Oops! Something went wrong.
Oops! Something went wrong.
Looks like we were not able to place the reservation. Kindly try again later.
Are you sure you want to remove the book from the shelf?
Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery
Oops! Something went wrong.
Oops! Something went wrong.
While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Title added to your shelf!
Title added to your shelf!
View what I already have on My Shelf.
Oops! Something went wrong.
Oops! Something went wrong.
While trying to add the title to your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery
Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery

Please be aware that the book you have requested cannot be checked out. If you would like to checkout this book, you can reserve another copy
How would you like to get it?
We have requested the book for you! Sorry the robot delivery is not available at the moment
We have requested the book for you!
We have requested the book for you!
Your request is successful and it will be processed during the Library working hours. Please check the status of your request in My Requests.
Oops! Something went wrong.
Oops! Something went wrong.
Looks like we were not able to place your request. Kindly try again later.
Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery
Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery
Journal Article

Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery

2025
Request Book From Autostore and Choose the Collection Method
Overview
The 15 January 2022 eruption of the Hunga volcano generated a Lamb wave, a global atmospheric pressure perturbation which propagates purely horizontally at the speed of sound. Far‐field observations of the daytime passage of the Lamb wave by the Geostationary Operational Environmental Satellite‐R (GOES‐R) series, revealed unexpected, synchronized variations in the solar reflectance of low‐level liquid clouds, the most prominent of which is a transient darkening accompanying the overpressure peak. We hypothesize that this darkening is mostly caused by the rapid thermodynamic adjustment of the cloudy environment to the slight, but spatially coherent, warming introduced by the pressure pulse. The corresponding reduction in relative humidity leads to the shrinkage and evaporation of small cloud droplets and hygroscopic particles in the halo region, which, in turn, temporarily reduces the optical thickness of the cloudy column. Plain Language Summary The giant Hunga volcano explosion on 15 January 2022 produced a special atmospheric wave, called the Lamb wave, that traveled around the globe somewhat faster than a jetliner. The Lamb wave increased the atmospheric pressure, slightly warming the air. Geostationary time loop imagery recorded the movement of this wave over the Gulf of Mexico, the Caribbean, and the North Atlantic Ocean during daytime hours. The observations reveal that the passing Lamb wave turned low‐level clouds momentarily darker. We argue that the cloud darkening is caused by the shrinkage of droplets inside and near clouds due to the warming. Key Points The Hunga Lamb wave caused detectable brightness variations in low‐level clouds 12,000 km away The dominant signal is a temporary darkening accompanying the peak overpressure We hypothesize the darkening results from the shrinkage of drops due to a sudden increase in temperature and decrease in relative humidity