Lightning And Thunder Diagram at Sandra Hargrove blog

Lightning And Thunder Diagram. Lightning, the visible discharge of electricity that occurs when a region of a cloud acquires an excess electrical charge, either positive or negative, sufficient to break. This extreme heating causes the air to expand explosively fast. The lightning channel is an example of terrestrial plasma in action. A single stroke of lightning can heat the air around it to 30,000°c (54,000°f)! When played back in slow motion, we can see the. High speed cameras can be used to capture video of lightning strikes. Lightning is a discharge of electricity. The resulting sound wave gets heard as thunder. When the downdrafts in the cloud become stronger than the updrafts, the storm starts to weaken. Thunder occurs when energy from lightning heats and rapidly expands the air. On discharge, a highly electrically conductive plasma channel is created within the air, and when current flows within this channel, it rapidly heats the air up to about 25,000°c.

Top 59+ imagen lightning diagram abzlocal fi
from abzlocal.mx

Lightning is a discharge of electricity. The resulting sound wave gets heard as thunder. When played back in slow motion, we can see the. High speed cameras can be used to capture video of lightning strikes. On discharge, a highly electrically conductive plasma channel is created within the air, and when current flows within this channel, it rapidly heats the air up to about 25,000°c. This extreme heating causes the air to expand explosively fast. Thunder occurs when energy from lightning heats and rapidly expands the air. The lightning channel is an example of terrestrial plasma in action. A single stroke of lightning can heat the air around it to 30,000°c (54,000°f)! Lightning, the visible discharge of electricity that occurs when a region of a cloud acquires an excess electrical charge, either positive or negative, sufficient to break.

Top 59+ imagen lightning diagram abzlocal fi

Lightning And Thunder Diagram A single stroke of lightning can heat the air around it to 30,000°c (54,000°f)! Lightning is a discharge of electricity. A single stroke of lightning can heat the air around it to 30,000°c (54,000°f)! Lightning, the visible discharge of electricity that occurs when a region of a cloud acquires an excess electrical charge, either positive or negative, sufficient to break. This extreme heating causes the air to expand explosively fast. High speed cameras can be used to capture video of lightning strikes. When the downdrafts in the cloud become stronger than the updrafts, the storm starts to weaken. When played back in slow motion, we can see the. On discharge, a highly electrically conductive plasma channel is created within the air, and when current flows within this channel, it rapidly heats the air up to about 25,000°c. The lightning channel is an example of terrestrial plasma in action. Thunder occurs when energy from lightning heats and rapidly expands the air. The resulting sound wave gets heard as thunder.

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