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A tornado occurred on the afternoon of Tuesday, December 24, in the municipality of Güira de Melena, in Artemisa.
The meteorologist Raydel Ruisanchez shared photos of the phenomenon on his Facebook wall, showing a gray air cloud over a field area.
According to Ruisanchez, it was a weak tornado.
"It can be seen in the images how the column of air reached the surface," he said.
The expert explained that the occurrence of the phenomenon on a local scale was related to instability conditions due to a moist flow from the south in the lower layers of the troposphere, and strong currents from the southwest in the middle and upper layers of the troposphere.
Frequently Asked Questions about the Tornado in Güira de Melena and Meteorological Phenomena in Artemisa
What happened in Güira de Melena before Christmas Eve?
On December 24, a weak tornado was reported in Güira de Melena, Artemisa. This phenomenon occurred due to atmospheric instability caused by a humid flow from the south and strong southwest currents in the troposphere. According to meteorologist Raydel Ruisanchez, the tornado was visible as a gray cloud that reached the surface.
How have the storms affected Güira de Melena in 2024?
Throughout 2024, Güira de Melena has experienced multiple severe weather phenomena, including storms with hail and heavy rains. These events have caused damage to infrastructure and crops, impacting the daily lives of its residents. Additionally, Hurricane Rafael, in November, left a significant trail of destruction in the region.
What has been the impact of Hurricane Rafael in Artemisa?
Hurricane Rafael caused severe damage in Güira de Melena and other municipalities in Artemisa, including the destruction of homes, agricultural losses, and damage to infrastructure such as hospitals and stadiums. Fortunately, no human casualties were reported, but the images of the disaster reveal a devastating scene in the region.
What weather conditions favored the occurrence of the tornado in Güira de Melena?
The tornado in Güira de Melena was the result of local atmospheric instability, influenced by a humid flow from the south in the lower layers of the troposphere and strong currents from the southwest in the middle and upper layers. These conditions facilitated the formation of the meteorological phenomenon, although its intensity was regarded as weak.
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