The Southwest Monsoon winds originate from the Indian Ocean (especially the Arabian Sea and Bay of Bengal), bringing moisture to the Indian subcontinent.
Explanation:
Ozone is a secondary pollutant, meaning it is not emitted directly but is formed in the atmosphere through chemical reactions between primary pollutants (like nitrogen oxides and volatile organic compounds) in the presence of sunlight.
Explanation:
A positive NAO phase is characterized by stronger than normal Azores High and Icelandic Low, leading to stronger westerly winds, milder and wetter winters in northern Europe, and colder and drier winters in southern Europe.
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