what is different between cyclones and thenderstorms
Answers & Comments
Aneelmalhi
Thunderstorms are formed due to convective activity with a good convergence of wind in a local area. During summer, heat over land increases resulting in rising of hot air into atmosphere forming cumulonimbus clouds. This grows into a thunderstorm
Cyclones are formed by low pressure area in tropical seas. Normally low pressure areas where cyclones spread over hundreds of kilometers. Tropical seas have relatively high sea surface temperatures, moisture content and when less wind shear accompanies, the convergence of winds around the low pressure area forms a cyclone and lets it grow.
Thunderstorms are formed due to convective activity with a good convergence of wind in a local area. During summer, heat over land increases resulting in rising of hot air into atmosphere forming cumulonimbus clouds. This grows into a thunderstorm.
Cyclones are formed by low pressure area in tropical seas. Normally low pressure areas where cyclones spread over hundreds of kilometers. Tropical seas have relatively high sea surface temperatures, moisture content and when less wind shear accompanies, the convergence of winds around the low pressure.
Answers & Comments
Cyclones are formed by low pressure area in tropical seas. Normally low pressure areas where cyclones spread over hundreds of kilometers. Tropical seas have relatively high sea surface temperatures, moisture content and when less wind shear accompanies, the convergence of winds around the low pressure area forms a cyclone and lets it grow.
Thunderstorms are formed due to convective activity with a good convergence of wind in a local area. During summer, heat over land increases resulting in rising of hot air into atmosphere forming cumulonimbus clouds. This grows into a thunderstorm.
Cyclones are formed by low pressure area in tropical seas. Normally low pressure areas where cyclones spread over hundreds of kilometers. Tropical seas have relatively high sea surface temperatures, moisture content and when less wind shear accompanies, the convergence of winds around the low pressure.