It become hazy when strong wind blow on a hot dry day give reason.
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Air flowing from areas of high pressure to low pressure creates winds. Air moving at ... This causes the air to become dense and sink, which creates a high pressure cell
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The Loo (Hindi: लू, Urdu: لُو, Punjabi Gurmukhi: ਲੂ) is a strong, dusty, hot and dry summer windfrom the west which blows over the western Indo-Gangetic Plain region of North India and Pakistan.[1] It is especially strong in the months of May and June. Due to its very high temperatures (45 °C–50 °C or 115 °F–120 °F), exposure to it often leads to fatal heatstrokes.[1]
Since it causes extremely low humidity and high temperatures, the Loo also has a severe drying effect on vegetation leading to widespread browning in the areas affected by it during the months of May and June.[2]
Since it causes extremely low humidity and high temperatures, the Loo also has a severe drying effect on vegetation leading to widespread browning in the areas affected by it during the months of May and June.[2]
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