Northeast monsoon

Target entity: Northeast monsoon
Context triple: [Arabian Sea, climateInfluencedBy, Northeast monsoon]

• A. Southwest monsoon
  The Southwest monsoon is a seasonal wind and rainfall system that brings warm, moisture-laden air from the Indian Ocean and Arabian Sea to South Asia, producing the region’s primary rainy season.
• B. Indian Monsoon Current
  The Indian Monsoon Current is a seasonally reversing ocean current in the northern Indian Ocean driven by the South Asian monsoon winds, significantly influencing regional climate and marine circulation.
• C. Madden–Julian Oscillation
  The Madden–Julian Oscillation is a large-scale tropical atmospheric pattern characterized by eastward-moving pulses of enhanced and suppressed rainfall that strongly influence global weather and climate variability on intraseasonal timescales.
• D. La Niña
  La Niña is the cool phase of the El Niño–Southern Oscillation climate pattern, characterized by unusually cold ocean temperatures in the central and eastern equatorial Pacific and associated shifts in global weather.
• E. Bora wind
  The Bora wind is a cold, dry, and often violent northeasterly wind that blows from the interior highlands toward the Adriatic Sea, especially affecting coastal areas like Trieste.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Northeast monsoon
Target entity description: The Northeast monsoon is a seasonal wind and rainfall pattern that brings cooler, dry or sometimes heavy rain-bearing air from the Asian continent toward the Indian Ocean, significantly affecting weather in South and Southeast Asia.

• A. Southwest monsoon
  The Southwest monsoon is a seasonal wind and rainfall system that brings warm, moisture-laden air from the Indian Ocean and Arabian Sea to South Asia, producing the region’s primary rainy season.
• B. Indian Monsoon Current
  The Indian Monsoon Current is a seasonally reversing ocean current in the northern Indian Ocean driven by the South Asian monsoon winds, significantly influencing regional climate and marine circulation.
• C. Madden–Julian Oscillation
  The Madden–Julian Oscillation is a large-scale tropical atmospheric pattern characterized by eastward-moving pulses of enhanced and suppressed rainfall that strongly influence global weather and climate variability on intraseasonal timescales.
• D. La Niña
  La Niña is the cool phase of the El Niño–Southern Oscillation climate pattern, characterized by unusually cold ocean temperatures in the central and eastern equatorial Pacific and associated shifts in global weather.
• E. Bora wind
  The Bora wind is a cold, dry, and often violent northeasterly wind that blows from the interior highlands toward the Adriatic Sea, especially affecting coastal areas like Trieste.
• F. None of above. chosen