Such an outbreak like the April 27 one is extremely rare and historic when it happens.
The big question is, how did this happen?
1. JET STREAM
The jet stream was down south, guiding the low pressure center east with the cold front that would produce the tornadoes. The jet stream was unusually strong, and the storm system may have even gotten some of that energy from the jet stream.
The jet stream made for a high wind shear event, favorable for tornadoes in some areas.
Additionally, the jet stream separates warm and cold air. With the cold front bringing the cold air from above the jet stream and the warm front bringing warm air from below the jet stream, it was a very volatile situation to start with.
2. EHI
EHI (Energy Helicity Index) combines wind factors (like helicity, which is a spinning motion) and energy factors (like CAPEs, which produce stronger and more volatile storms) to make a sense of what the potential is for rotating supercells.
The EHI index was incredibly high for the outbreak.
Values may have reached 12.00, which is considered absolutely unbelievable.
This is probably the biggest factor that directly contributed to the tornado outbreak.
3. CAPE
CAPE values indicate potential energy that can be utilized by thunderstorms. The higher the CAPE, the more unstable the atmosphere. CAPE values were witnessed to be up to 4,000 j/kg, possibly even more.
To give you a sense of how unstable 4,000 j/kg is, 2,000 j/kg is considered the threshold for severe thunderstorms for CAPE values.
There were many other things that came into place, but these 3 really stood out from the other factors.
Stay tuned to the Weather Centre for continuing coverage on the aftermath of this horrific incident.
The big question is, how did this happen?
1. JET STREAM
The jet stream was down south, guiding the low pressure center east with the cold front that would produce the tornadoes. The jet stream was unusually strong, and the storm system may have even gotten some of that energy from the jet stream.
The jet stream made for a high wind shear event, favorable for tornadoes in some areas.
Additionally, the jet stream separates warm and cold air. With the cold front bringing the cold air from above the jet stream and the warm front bringing warm air from below the jet stream, it was a very volatile situation to start with.
2. EHI
EHI (Energy Helicity Index) combines wind factors (like helicity, which is a spinning motion) and energy factors (like CAPEs, which produce stronger and more volatile storms) to make a sense of what the potential is for rotating supercells.
The EHI index was incredibly high for the outbreak.
Values may have reached 12.00, which is considered absolutely unbelievable.
This is probably the biggest factor that directly contributed to the tornado outbreak.
3. CAPE
CAPE values indicate potential energy that can be utilized by thunderstorms. The higher the CAPE, the more unstable the atmosphere. CAPE values were witnessed to be up to 4,000 j/kg, possibly even more.
To give you a sense of how unstable 4,000 j/kg is, 2,000 j/kg is considered the threshold for severe thunderstorms for CAPE values.
There were many other things that came into place, but these 3 really stood out from the other factors.
Stay tuned to the Weather Centre for continuing coverage on the aftermath of this horrific incident.
No comments:
Post a Comment